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en.wikipedia.org/wiki/Giza_pyramid_complex

 

The Giza pyramid complex (also called the Giza necropolis) in Egypt is home to the Great Pyramid, the Pyramid of Khafre, and the Pyramid of Menkaure, along with their associated pyramid complexes and the Great Sphinx. All were built during the Fourth Dynasty of the Old Kingdom of ancient Egypt, between c. 2600 – c. 2500 BC. The site also includes several temples, cemeteries, and the remains of a workers' village.

 

The site is at the edge of the Western Desert, approximately 9 km (5.6 mi) west of the Nile River in the city of Giza, and about 13 km (8.1 mi) southwest of the city centre of Cairo. It forms the northernmost part of the 16,000 ha (160 km2; 62 sq mi) Pyramid Fields of the Memphis and its Necropolis UNESCO World Heritage Site, inscribed in 1979. The pyramid fields include the Abusir, Saqqara, and Dahshur pyramid complexes, which were all built in the vicinity of Egypt's ancient capital of Memphis.[1] Further Old Kingdom pyramid fields were located at the sites Abu Rawash, Zawyet El Aryan, and Meidum.

 

The Great Pyramid and the Pyramid of Khafre are the largest pyramids built in ancient Egypt, and they have historically been common as emblems of Ancient Egypt in the Western imagination They were popularised in Hellenistic times, when the Great Pyramid was listed by Antipater of Sidon as one of the Seven Wonders of the World. It is by far the oldest of the Ancient Wonders and the only one still in existence.

 

Literature on ancient Giza is vast; for an overview with further references, see Manuelian[3] or Lehner and Hawass.

 

Maadi settlements

The earliest settlement of the Giza plateau predates the pyramid complexes. Four jars from the Maadi culture were found at the foot of the Great Pyramid, likely from a disturbed earlier settlement. Further Maadi settlement near the site was uncovered during work on the Greater Cairo Wastewater Project. Recent reassessment of the radiocarbon dating puts the Maadi culture's eponymous settlement to c. 3800 – c. 3400 BC, which is also the likely maximum possible range for the Giza remains.

 

The Giza pyramid complex consists of the Great Pyramid (also known as the Pyramid of Cheops or Khufu and constructed c. 2580 – c. 2560 BC), the somewhat smaller Pyramid of Khafre (or Chephren) a few hundred metres to the south-west, and the relatively modest-sized Pyramid of Menkaure (or Mykerinos) a few hundred metres farther south-west. The Great Sphinx lies on the east side of the complex. Consensus among Egyptologists is that the head of the Great Sphinx is that of Khafre. Along with these major monuments are a number of smaller satellite edifices, known as "queens" pyramids, causeways, and temples.[8] Besides the archaeological structures, the ancient landscape has also been investigated.

 

Khufu's complex

Khufu's pyramid complex consists of a valley temple, now buried beneath the village of Nazlet el-Samman; diabase paving and nummulitic limestone walls have been found but the site has not been excavated. The valley temple was connected to a causeway that was largely destroyed when the village was constructed. The causeway led to the Mortuary Temple of Khufu, which was connected to the pyramid. Of this temple, the basalt pavement is the only thing that remains. The king's pyramid has three smaller queen's pyramids associated with it and three boat pits.  The boat pits contained a ship, and the two pits on the south side of the pyramid contained intact ships when excavated. One of these ships, the Khufu ship, has been restored and was originally displayed at the Giza Solar boat museum, then subsequently moved to the Grand Egyptian Museum.

 

Khufu's pyramid still has a limited number of casing stones at its base. These casing stones were made of fine white limestone quarried at Tura.

 

Khafre's complex

Main articles: Pyramid of Khafre and Great Sphinx of Giza

Khafre's pyramid complex consists of a valley temple, the Sphinx temple, a causeway, a mortuary temple, and the king's pyramid. The valley temple yielded several statues of Khafre. Several were found in a well in the floor of the temple by Mariette in 1860. Others were found during successive excavations by Sieglin (1909–1910), Junker, Reisner, and Hassan. Khafre's complex contained five boat-pits and a subsidiary pyramid with a serdab. 

 

Khafre's pyramid appears larger than the adjacent Khufu Pyramid by virtue of its more elevated location, and the steeper angle of inclination of its construction—it is, in fact, smaller in both height and volume. Khafre's pyramid retains a prominent display of casing stones at its apex.

 

Menkaure's complex

Menkaure's pyramid complex consists of a valley temple, a causeway, a mortuary temple, and the king's pyramid. The valley temple once contained several statues of Menkaure. During the 5th Dynasty, a smaller ante-temple was added on to the valley temple. The mortuary temple also yielded several statues of Menkaure. The king's pyramid, completed c. 2510 BC, has three subsidiary or queen's pyramids.  Of the four major monuments, only Menkaure's pyramid is seen today without any of its original polished limestone casing

 

Sphinx

The Sphinx dates from the reign of king Khafre. During the New Kingdom, Amenhotep II dedicated a new temple to Hauron-Haremakhet and this structure was added onto by later rulers.

 

Tomb of Queen Khentkaus I

Main article: Pyramid of Khentkaus I

Khentkaus I was buried in Giza. Her tomb is known as LG 100 and G 8400 and is located in the Central Field, near the valley temple of Menkaure. The pyramid complex of Queen Khentkaus includes her pyramid, a boat pit, a valley temple, and a pyramid town.

 

Construction

Main article: Egyptian pyramid construction techniques

Most construction theories are based on the idea that the pyramids were built by moving huge stones from a quarry and dragging and lifting them into place. Disagreements arise over the feasibility of the different proposed methods by which the stones were conveyed and placed.

 

In building the pyramids, the architects might have developed their techniques over time. They would select a site on a relatively flat area of bedrock—not sand—which provided a stable foundation. After carefully surveying the site and laying down the first level of stones, they constructed the pyramids in horizontal levels, one on top of the other.

 

For the Great Pyramid, most of the stone for the interior seems to have been quarried immediately to the south of the construction site. The smooth exterior of the pyramid was made of a fine grade of white limestone that was quarried across the Nile. These exterior blocks had to be carefully cut, transported by river barge to Giza, and dragged up ramps to the construction site. Only a few exterior blocks remain in place at the bottom of the Great Pyramid. During the Middle Ages (5th century to 15th century), people may have taken the rest away for building projects in the city of Cairo.

 

To ensure that the pyramid remained symmetrical, the exterior casing stones all had to be equal in height and width. Workers might have marked all the blocks to indicate the angle of the pyramid wall and trimmed the surfaces carefully so that the blocks fit together. During construction, the outer surface of the stone was smooth limestone; excess stone has eroded over time.

 

New insights into the closing stages of the Great Pyramid building were provided by the recent find of Wadi el-Jarf papyri, especially the diary of inspector Merer, whose team was assigned to deliver the white limestone from Tura quarries to Giza. The journal was already published, as well as a popular account of the importance of this discovery.

 

Purpose

The pyramids of Giza and others are thought to have been constructed to house the remains of the deceased pharaohs who ruled Ancient Egypt. A portion of the pharaoh's spirit called his ka was believed to remain with his corpse. Proper care of the remains was necessary in order for the "former Pharaoh to perform his new duties as king of the dead". It is theorized the pyramid not only served as a tomb for the pharaoh, but also as a storage pit for various items he would need in the afterlife. "The people of Ancient Egypt believed that death on Earth was the start of a journey to the next world." The embalmed body of the King was entombed underneath or within the pyramid to protect it and allow his transformation and ascension to the afterlife.

 

Astronomy

The sides of all three of the Giza pyramids were astronomically oriented to the cardinal directions within a small fraction of a degree. According to the disputed Orion correlation theory, the arrangement of the pyramids is a representation of the constellation Orion.

 

Workers' village

The work of quarrying, moving, setting, and sculpting the huge amount of stone used to build the pyramids might have been accomplished by several thousand skilled workers, unskilled laborers and supporting workers. Bakers, carpenters, water carriers, and others were also needed for the project. Along with the methods used to construct the pyramids, there is also wide speculation regarding the exact number of workers needed for a building project of this magnitude. When Greek historian Herodotus visited Giza in 450 BC, he was told by Egyptian priests that "the Great Pyramid had taken 400,000 men 20 years to build, working in three-month shifts 100,000 men at a time." Evidence from the tombs indicates that a workforce of 10,000 laborers working in three-month shifts took around 30 years to build a pyramid.

 

The Giza pyramid complex is surrounded by a large stone wall, outside which Mark Lehner and his team discovered a town where the pyramid workers were housed. The village is located to the southeast of the Khafre and Menkaure complexes. Among the discoveries at the workers' village are communal sleeping quarters, bakeries, breweries, and kitchens (with evidence showing that bread, beef, and fish were dietary staples), a copper workshop, a hospital, and a cemetery (where some of the skeletons were found with signs of trauma associated with accidents on a building site). The metal processed at the site was the so-called arsenical copper. The same material was also identified among the copper artefacts from the "Kromer" site, from the reigns of Khufu and Khafre.

 

The workers' town appears to date from the middle 4th Dynasty (2520–2472 BC), after the accepted time of Khufu and completion of the Great Pyramid. According to Lehner and the AERA team:

 

The development of this urban complex must have been rapid. All of the construction probably happened in the 35 to 50 years that spanned the reigns of Khafre and Menkaure, builders of the Second and Third Giza Pyramids.

Using pottery shards, seal impressions, and stratigraphy to date the site, the team further concludes:

 

The picture that emerges is that of a planned settlement, some of the world's earliest urban planning, securely dated to the reigns of two Giza pyramid builders: Khafre (2520–2494 BC) and Menkaure (2490–2472 BC).

Radiocarbon data for the Old Kingdom Giza plateau and the workers' settlement were published in 2006, and then re-evaluated in 2011.

 

Cemeteries

As the pyramids were constructed, the mastabas for lesser royals were constructed around them. Near the pyramid of Khufu, the main cemetery is G 7000, which lies in the East Field located to the east of the main pyramid and next to the Queen's pyramids. These cemeteries around the pyramids were arranged along streets and avenues. Cemetery G 7000 was one of the earliest and contained tombs of wives, sons, and daughters of these 4th Dynasty rulers. On the other side of the pyramid in the West Field, the royals' sons Wepemnofret and Hemiunu were buried in Cemetery G 1200 and Cemetery G 4000, respectively. These cemeteries were further expanded during the 5th and 6th Dynasties.

 

West Field

Main article: Giza West Field

The West Field is located to the west of Khufu's pyramid. It is divided into smaller areas such as the cemeteries referred to as the Abu Bakr Excavations (1949–1950, 1950–1951, 1952, and 1953), and several cemeteries named based on the mastaba numbers such as Cemetery G 1000, Cemetery G 1100, etc. The West Field contains Cemetery G1000 – Cemetery G1600, and Cemetery G 1900. Further cemeteries in this field are: Cemeteries G 2000, G 2200, G 2500, G 3000, G 4000, and G 6000. Three other cemeteries are named after their excavators: Junker Cemetery West, Junker Cemetery East, and Steindorff Cemetery.

 

East Field

Main article: Giza East Field

The East Field is located to the east of Khufu's pyramid and contains cemetery G 7000. This cemetery was a burial place for some of the family members of Khufu. The cemetery also includes mastabas from tenants and priests of the pyramids dated to the 5th Dynasty and 6th Dynasty.

 

Cemetery GIS

This cemetery dates from the time of Menkaure (Junker) or earlier (Reisner), and contains several stone-built mastabas dating from as late as the 6th Dynasty. Tombs from the time of Menkaure include the mastabas of the royal chamberlain Khaemnefert, the King's son Khufudjedef (master of the royal largesse), and an official named Niankhre.

 

Central Field

Main article: Central Field, Giza

The Central Field contains several burials of royal family members. The tombs range in date from the end of the 4th Dynasty to the 5th Dynasty or even later.[

 

Tombs dating from the Saite and later period were found near the causeway of Khafre and the Great Sphinx. These tombs include the tomb of a commander of the army named Ahmose and his mother Queen Nakhtubasterau, who was the wife of Pharaoh Amasis II.

 

South Field

The South Field includes mastabas dating from the 1st Dynasty to 3rd Dynasty as well as later burials. Of the more significant of these early dynastic tombs are one referred to as "Covington's tomb", otherwise known as Mastaba T, and the large Mastaba V which contained artifacts naming the 1st Dynasty pharaoh Djet. Other tombs date from the late Old Kingdom (5th and 6th Dynasty). The south section of the field contains several tombs dating from the Saite period and later. 

 

Tombs of the pyramid builders

In 1990, tombs belonging to the pyramid workers were discovered alongside the pyramids, with an additional burial site found nearby in 2009. Although not mummified, they had been buried in mudbrick tombs with beer and bread to support them in the afterlife. The tombs' proximity to the pyramids and the manner of burial supports the theory that they were paid laborers who took pride in their work and were not slaves, as was previously thought. Evidence from the tombs indicates that a workforce of 10,000 laborers working in three-month shifts took around 30 years to build a pyramid. Most of the workers appear to have come from poor families. Specialists such as architects, masons, metalworkers, and carpenters were permanently employed by the king to fill positions that required the most skill.

 

Shafts

There are multiple burial-shafts and various unfinished shafts and tunnels located in the Giza complex that were discovered and mentioned prominently by Selim Hassan in his report Excavations at Giza 1933–1934. He states: "Very few of the Saitic [referring to the Saite Period) shafts have been thoroughly examined, for the reason that most of them are flooded."

 

Osiris Shaft

The Osiris Shaft is a narrow burial-shaft leading to three levels for a tomb and below it a flooded area. It was first mentioned by Hassan, and a thorough excavation was conducted by a team led by Hawass in 1999. It was opened to tourists in November 2017.

 

New Kingdom and Late Period

During the New Kingdom Giza was still an active site. A brick-built chapel was constructed near the Sphinx during the early 18th Dynasty, probably by King Thutmose I. Amenhotep II built a temple dedicated to Hauron-Haremakhet near the Sphinx. As a prince, the future pharaoh Thutmose IV visited the pyramids and the Sphinx; he reported being told in a dream that if he cleared the sand that had built up around the Sphinx, he would be rewarded with kingship. This event is recorded in the Dream Stele, which he had installed between the Sphinx's front legs.

 

During the early years of his reign, Thutmose IV, together with his wife Queen Nefertari, had stelae erected at Giza.

 

Pharaoh Tutankhamun had a structure built, which is now referred to as the king's resthouse.

 

During the 19th Dynasty, Seti I added to the temple of Hauron-Haremakhet, and his son Ramesses II erected a stela in the chapel before the Sphinx and usurped the resthouse of Tutankhamun. 

 

During the 21st Dynasty, the Temple of Isis Mistress-of-the-Pyramids was reconstructed. During the 26th Dynasty, a stela made in this time mentions Khufu and his Queen Henutsen.

 

Division of the 1903–1905 excavation of the Giza Necropolis

In 1903, rights to excavate the West Field and Pyramids of the Giza Necropolis were divided by three institutions from Italy, Germany, and the United States of America.

 

Background

Prior to the division of the Giza Plateau into three institutional concessions in 1903, amateur and private excavations at the Giza Necropolis had been permitted to operate. The work of these amateur archaeologists failed to meet high scientific standards. Montague Ballard, for instance, excavated in the Western Cemetery (with the hesitant permission of the Egyptian Antiquities Service) and neither kept records of his finds nor published them.

 

Italian, German, and American Concessions at Giza

In 1902, the Egyptian Antiquities Service under Gaston Maspero resolved to issue permits exclusively to authorized individuals representing public institutions. In November of that year, the Service awarded three scholars with concessions on the Giza Necropolis. They were the Italian Ernesto Schiaparelli from the Turin Museum, the German Georg Steindorff from the University of Leipzig who had funding from Wilhelm Pelizaeus, and the American George Reisner from the Hearst Expedition. Within a matter of months, the site had been divided between the concessionaires following a meeting at the Mena House Hotel involving Schiaparelli, Ludwig Borchardt (Steindorff's representative in Egypt), and Reisner.

 

Division of the West Field

By the turn of the 20th century, the three largest pyramids on the Giza plateau were considered mostly exhausted by previous excavations, so the Western Cemetery and its collection of private mastaba tombs were thought to represent the richest unexcavated part of the plateau. George Reisner's wife, Mary, drew names from a hat to assign three long east-west plots of the necropolis among the Italian, German, and American missions. Schiaparelli was assigned the southernmost strip, Borchardt the center, and Reisner the northernmost.

 

Division of the Pyramids

Rights to excavate the Pyramids were then also negotiated between Schiaparelli, Borchardt, and Reisner. Schiaparelli gained rights to excavate the Great Pyramid of Khufu along with its three associated queens' pyramids and most of its Eastern Cemetery. Borchardt received Khafre's pyramid, its causeway, the Sphinx, and the Sphinx's associated temples. Reisner claimed Menkaure's pyramid as well as its associated queens' pyramids and pyramid temple, along with a portion of Schiaparelli's Eastern Cemetery. Any future disputes were to be resolved by Inspector James Quibell, as per a letter from Borchardt to Maspero.

 

Immediate Aftermath

This arrangement lasted until 1905, when, under the supervision of Schiaparelli and Francesco Ballerini, the Italian excavations ceased at Giza. As the Italians were more interested in sites which might yield more papyri, they turned their concession of the southern strip of the Western Cemetery over to the Americans under Reisner.

 

Modern usage

In 1978, the Grateful Dead played a series of concerts later released as Rocking the Cradle: Egypt 1978. In 2007, Colombian singer Shakira performed at the complex to a crowd of approximately 100,000 people. The complex was used for the final draw of the 2019 Africa Cup of Nations and the 2021 World Men's Handball Championship.

 

Egypt's Minister of Tourism unveiled plans for a €17,000,000 revamp of the complex by the end of 2021, in order to boost tourism in Egypt as well as make the site more accessible and tourist-friendly. According to Lonely Planet, the refurbishment includes a new visitors' centre, an environmentally-friendly electric bus, a restaurant (the 9 Pyramids Lounge), as well as a cinema, public toilets, site-wide signage, food trucks, photo booths, and free Wi-Fi. The new facility is part of a wider plan to renovate the 4,500 year old site.

The United States Astronaut Hall of Fame, located inside the Kennedy Space Center Visitor Complex Heroes & Legends building on Merritt Island, Florida, honors American astronauts and features the world's largest collection of their personal memorabilia, focusing on those astronauts who have been inducted into the Hall. Exhibits include Wally Schirra's Sigma 7 space capsule from the fifth crewed Mercury mission and the Gemini IX spacecraft flown by Gene Cernan and Thomas P. Stafford in 1966.

 

In the 1980s, the six then-surviving Mercury Seven astronauts conceived of establishing a place where US space travelers could be remembered and honored, along the lines of halls of fame for other fields. The Mercury Seven Foundation and Astronaut Scholarship Foundation were formed, and have a role in the ongoing operations of the Hall of Fame. The foundation's first executive director was former Associated Press space reporter Howard Benedict.

 

The Astronaut Hall of Fame was opened on October 29, 1990, by the U.S. Space Camp Foundation, which was the first owner of the facility. It was located next to the Florida branch of Space Camp.

 

The Hall of Fame closed for several months in 2002 when U.S. Space Camp Foundation's creditors foreclosed on the property due to low attendance and mounting debt. That September, an auction was held and the property was purchased by Delaware North Park Services on behalf of NASA and the property was added to the Kennedy Space Center Visitor Complex. The Hall of Fame re-opened December 14, 2002.

 

The Hall of Fame, which was originally located just west of the NASA Causeway, closed to the public on November 2, 2015, in preparation for its relocation to the Kennedy Space Center Visitor Complex 6 miles (9.7 km) to the east on Merritt Island. Outside of the original building was a full-scale replica of a Space Shuttle orbiter named Inspiration (originally named "Shuttle To Tomorrow" where visitors could enter and view a program). Inspiration served only as an outdoor, full scale, static display which visitors could not enter. After the Hall of Fame was transferred to the KSC Visitor Complex, Inspiration was acquired by LVX System and was placed in storage at the Shuttle Landing Facility at the Kennedy Space Center; in 2016, the shuttle was loaded on to a barge to be taken for refurbishment before going on an educational tour.

 

The building was purchased at auction by visitor complex operator Delaware North and renamed the ATX Center, and for a time housed educational programs including Camp Kennedy Space Center and the Astronaut Training Experience. Those programs have since been moved to the KSC Visitor Complex, and as of December 2019, the structure was being offered for lease. In July 2020, Lockheed Martin announced it would lease the building to support work on the NASA Orion crew capsule.

 

Inductees into the Hall of Fame are selected by a blue ribbon committee of former NASA officials and flight controllers, historians, journalists, and other space authorities (including former astronauts) based on their accomplishments in space or their contributions to the advancement of space exploration. Except for 2002, inductions have been held every year since 2001.

 

As its inaugural class in 1990, the Hall of Fame inducted the United States' original group of astronauts: the Mercury Seven. In addition to being the first American astronauts, they set several firsts in American spaceflight, both auspicious and tragic. Alan Shepard was the first American in space and later became one of the twelve people to walk on the Moon. John Glenn was the first American to orbit the Earth and after his induction went on, in 1998, to become the oldest man to fly in space, aged 77. Gus Grissom was the first American to fly in space twice and was the commander of the ill-fated Apollo 1, which resulted in the first astronaut deaths directly related to preparation for spaceflight.

 

Thirteen astronauts from the Gemini and Apollo programs were inducted in the second class of 1993. This class included the first and last humans to walk on the Moon, Neil Armstrong and Eugene Cernan; Ed White, the first American to walk in space (also killed in the Apollo 1 accident); Jim Lovell, commander of the famously near-tragic Apollo 13; and John Young, whose six flights included a moonwalk and command of the first Space Shuttle mission.

 

The third class was inducted in 1997 and consisted of the 24 additional Apollo, Skylab, and ASTP astronauts. Notable members of the class were Roger Chaffee, the third astronaut killed in the Apollo 1 fire and the only unflown astronaut in the Hall; Harrison Schmitt, the first scientist and next-to-last person to walk on the Moon; and Jack Swigert and Fred Haise, the Apollo 13 crewmembers not previously inducted.

 

The philosophy regarding the first three groups of inductees was that all astronauts who flew in NASA's "pioneering" programs (which would include Mercury, Gemini, Apollo, Apollo Applications Program (Skylab), and Apollo-Soyuz Test Project) would be included simply by virtue of their participation in a spaceflight in these early programs. The first group (the inaugural class of 1990) would only include the original Mercury astronauts (most of whom would go on to fly in later programs). The second group of inductees would include those astronauts who began their spaceflight careers during Gemini (all of whom would go on to fly in later programs). The third group of inductees would include those astronauts who began their spaceflight careers during Apollo, Skylab, and ASTP (some of whom would go on to fly in the Space Shuttle program). Since it would not be practical (or meaningful) to induct all astronauts who ever flew in space, all subsequent inductees (Space Shuttle program and beyond) are considered based on their accomplishments and contributions to the human spaceflight endeavor which would set them apart from their peers.

 

Over four dozen astronauts from the Space Shuttle program have been inducted since 2001. Among these are Sally Ride, the first American woman in space; Story Musgrave, who flew six missions in the 1980s and 90s; and Francis Scobee, commander of the ill-fated final Challenger mission.

 

The 2010 class consisted of Guion Bluford Jr., Kenneth Bowersox, Frank Culbertson and Kathryn Thornton. The 2011 inductees were Karol Bobko and Susan Helms. The 2012 inductees were Franklin Chang-Diaz, Kevin Chilton and Charles Precourt. Bonnie Dunbar, Curt Brown and Eileen Collins were inducted in 2013, and Shannon Lucid and Jerry Ross comprised the 2014 class.

 

Those inducted in 2015 were John Grunsfeld, Steven Lindsey, Kent Rominger, and Rhea Seddon. In 2016, inductees included Brian Duffy and Scott E. Parazynski. Ellen Ochoa and Michael Foale were announced as the 2017 class of the United States Astronaut Hall of Fame. Scott Altman and Thomas Jones followed in 2018. The 2019 inductees were James Buchli and Janet L. Kavandi.

 

Michael López-Alegría, Scott Kelly and Pamela Melroy were the 2020 inductees, inducted in a November 2021 ceremony. The 2022 inductees were Christopher Ferguson, David Leestma, and Sandra Magnus. Roy Bridges Jr. and Mark Kelly were the 2023 inductees.

 

The Hall of Heroes is composed of tributes to the inductees. Among the Hall of Fame's displays is Sigma 7, the Mercury spacecraft piloted by Wally Schirra which orbited the Earth six times in 1962, and the Gemini 9A capsule flown by Gene Cernan and Thomas P. Stafford in 1966. An Astronaut Adventure room includes simulators for use by children.

 

The spacesuit worn by Gus Grissom during his 1961 Liberty Bell 7 Mercury flight is on display and has been the subject of a dispute between NASA and Grissom's heirs and supporters since 2002. The spacesuit, along with other Grissom artifacts, were loaned to the original owners of the Hall of Fame by the Grissom family when it opened. After the Hall of Fame went into bankruptcy and was taken over by a NASA contractor in 2002, the family requested that all their items be returned. All of the items were returned to Grissom's family except the spacesuit, because both NASA and the Grissoms claim ownership of it. NASA claims Grissom checked out the spacesuit for a show and tell at his son's school, and then never returned it, while the Grissoms claim Gus rescued the spacesuit from a scrap heap.

 

The John F. Kennedy Space Center (KSC, originally known as the NASA Launch Operations Center), located on Merritt Island, Florida, is one of the National Aeronautics and Space Administration's (NASA) ten field centers. Since December 1968, KSC has been NASA's primary launch center of human spaceflight. Launch operations for the Apollo, Skylab and Space Shuttle programs were carried out from Kennedy Space Center Launch Complex 39 and managed by KSC.[4] Located on the east coast of Florida, KSC is adjacent to Cape Canaveral Space Force Station (CCSFS). The management of the two entities work very closely together, share resources and operate facilities on each other's property.

 

Though the first Apollo flights and all Project Mercury and Project Gemini flights took off from the then-Cape Canaveral Air Force Station, the launches were managed by KSC and its previous organization, the Launch Operations Directorate. Starting with the fourth Gemini mission, the NASA launch control center in Florida (Mercury Control Center, later the Launch Control Center) began handing off control of the vehicle to the Mission Control Center in Houston, shortly after liftoff; in prior missions it held control throughout the entire mission.

 

Additionally, the center manages launch of robotic and commercial crew missions and researches food production and In-Situ Resource Utilization for off-Earth exploration. Since 2010, the center has worked to become a multi-user spaceport through industry partnerships, even adding a new launch pad (LC-39C) in 2015.

 

There are about 700 facilities and buildings grouped across the center's 144,000 acres (580 km2). Among the unique facilities at KSC are the 525-foot (160 m) tall Vehicle Assembly Building for stacking NASA's largest rockets, the Launch Control Center, which conducts space launches at KSC, the Operations and Checkout Building, which houses the astronauts dormitories and suit-up area, a Space Station factory, and a 3-mile (4.8 km) long Shuttle Landing Facility. There is also a Visitor Complex open to the public on site.

 

Since 1949, the military had been performing launch operations at what would become Cape Canaveral Space Force Station. In December 1959, the Department of Defense transferred 5,000 personnel and the Missile Firing Laboratory to NASA to become the Launch Operations Directorate under NASA's Marshall Space Flight Center.

 

President John F. Kennedy's 1961 goal of a crewed lunar landing by 1970 required an expansion of launch operations. On July 1, 1962, the Launch Operations Directorate was separated from MSFC to become the Launch Operations Center (LOC). Also, Cape Canaveral was inadequate to host the new launch facility design required for the mammoth 363-foot (111 m) tall, 7,500,000-pound-force (33,000 kN) thrust Saturn V rocket, which would be assembled vertically in a large hangar and transported on a mobile platform to one of several launch pads. Therefore, the decision was made to build a new LOC site located adjacent to Cape Canaveral on Merritt Island.

 

NASA began land acquisition in 1962, buying title to 131 square miles (340 km2) and negotiating with the state of Florida for an additional 87 square miles (230 km2). The major buildings in KSC's Industrial Area were designed by architect Charles Luckman. Construction began in November 1962, and Kennedy visited the site twice in 1962, and again just a week before his assassination on November 22, 1963.

 

On November 29, 1963, the facility was given its current name by President Lyndon B. Johnson under Executive Order 11129. Johnson's order joined both the civilian LOC and the military Cape Canaveral station ("the facilities of Station No. 1 of the Atlantic Missile Range") under the designation "John F. Kennedy Space Center", spawning some confusion joining the two in the public mind. NASA Administrator James E. Webb clarified this by issuing a directive stating the Kennedy Space Center name applied only to the LOC, while the Air Force issued a general order renaming the military launch site Cape Kennedy Air Force Station.

 

Located on Merritt Island, Florida, the center is north-northwest of Cape Canaveral on the Atlantic Ocean, midway between Miami and Jacksonville on Florida's Space Coast, due east of Orlando. It is 34 miles (55 km) long and roughly six miles (9.7 km) wide, covering 219 square miles (570 km2). KSC is a major central Florida tourist destination and is approximately one hour's drive from the Orlando area. The Kennedy Space Center Visitor Complex offers public tours of the center and Cape Canaveral Space Force Station.

 

The KSC Industrial Area, where many of the center's support facilities are located, is 5 miles (8 km) south of LC-39. It includes the Headquarters Building, the Operations and Checkout Building and the Central Instrumentation Facility. The astronaut crew quarters are in the O&C; before it was completed, the astronaut crew quarters were located in Hangar S[39] at the Cape Canaveral Missile Test Annex (now Cape Canaveral Space Force Station). Located at KSC was the Merritt Island Spaceflight Tracking and Data Network station (MILA), a key radio communications and spacecraft tracking complex.

 

Facilities at the Kennedy Space Center are directly related to its mission to launch and recover missions. Facilities are available to prepare and maintain spacecraft and payloads for flight. The Headquarters (HQ) Building houses offices for the Center Director, library, film and photo archives, a print shop and security. When the KSC Library first opened, it was part of the Army Ballistic Missile Agency. However, in 1965, the library moved into three separate sections in the newly opened NASA headquarters before eventually becoming a single unit in 1970. The library contains over four million items related to the history and the work at Kennedy. As one of ten NASA center libraries in the country, their collection focuses on engineering, science, and technology. The archives contain planning documents, film reels, and original photographs covering the history of KSC. The library is not open to the public but is available for KSC, Space Force, and Navy employees who work on site. Many of the media items from the collection are digitized and available through NASA's KSC Media Gallery or through their more up-to-date Flickr gallery.

 

A new Headquarters Building was completed in 2019 as part of the Central Campus consolidation. Groundbreaking began in 2014.

 

The center operated its own 17-mile (27 km) short-line railroad. This operation was discontinued in 2015, with the sale of its final two locomotives. A third had already been donated to a museum. The line was costing $1.3 million annually to maintain.

 

The Kennedy Space Center Visitor Complex, operated by Delaware North since 1995, has a variety of exhibits, artifacts, displays and attractions on the history and future of human and robotic spaceflight. Bus tours of KSC originate from here. The complex also includes the separate Apollo/Saturn V Center, north of the VAB and the United States Astronaut Hall of Fame, six miles west near Titusville. There were 1.5 million visitors in 2009. It had some 700 employees.

 

It was announced on May 29, 2015, that the Astronaut Hall of Fame exhibit would be moved from its current location to another location within the Visitor Complex to make room for an upcoming high-tech attraction entitled "Heroes and Legends". The attraction, designed by Orlando-based design firm Falcon's Treehouse, opened November 11, 2016.

 

In March 2016, the visitor center unveiled the new location of the iconic countdown clock at the complex's entrance; previously, the clock was located with a flagpole at the press site. The clock was originally built and installed in 1969 and listed with the flagpole in the National Register of Historic Places in January 2000. In 2019, NASA celebrated the 50th anniversary of the Apollo program, and the launch of Apollo 10 on May 18. In summer of 2019, Lunar Module 9 (LM-9) was relocated to the Apollo/Saturn V Center as part of an initiative to rededicate the center and celebrate the 50th anniversary of the Apollo Program.

 

The John F. Kennedy Space Center (KSC, originally known as the NASA Launch Operations Center), located on Merritt Island, Florida, is one of the National Aeronautics and Space Administration's (NASA) ten field centers. Since December 1968, KSC has been NASA's primary launch center of American spaceflight, research, and technology. Launch operations for the Apollo, Skylab and Space Shuttle programs were carried out from Kennedy Space Center Launch Complex 39 and managed by KSC. Located on the east coast of Florida, KSC is adjacent to Cape Canaveral Space Force Station (CCSFS). The management of the two entities work very closely together, share resources and operate facilities on each other's property.

 

Though the first Apollo flights and all Project Mercury and Project Gemini flights took off from the then-Cape Canaveral Air Force Station, the launches were managed by KSC and its previous organization, the Launch Operations Directorate. Starting with the fourth Gemini mission, the NASA launch control center in Florida (Mercury Control Center, later the Launch Control Center) began handing off control of the vehicle to the Mission Control Center in Houston, shortly after liftoff; in prior missions it held control throughout the entire mission.

 

Additionally, the center manages launch of robotic and commercial crew missions and researches food production and in-situ resource utilization for off-Earth exploration. Since 2010, the center has worked to become a multi-user spaceport through industry partnerships, even adding a new launch pad (LC-39C) in 2015.

 

There are about 700 facilities and buildings grouped throughout the center's 144,000 acres (580 km2). Among the unique facilities at KSC are the 525-foot (160 m) tall Vehicle Assembly Building for stacking NASA's largest rockets, the Launch Control Center, which conducts space launches at KSC, the Operations and Checkout Building, which houses the astronauts dormitories and suit-up area, a Space Station factory, and a 3-mile (4.8 km) long Shuttle Landing Facility. There is also a Visitor Complex on site that is open to the public.

 

Since 1949, the military had been performing launch operations at what would become Cape Canaveral Space Force Station. In December 1959, the Department of Defense transferred 5,000 personnel and the Missile Firing Laboratory to NASA to become the Launch Operations Directorate under NASA's Marshall Space Flight Center.

 

President John F. Kennedy's 1961 goal of a crewed lunar landing by 1970 required an expansion of launch operations. On July 1, 1962, the Launch Operations Directorate was separated from MSFC to become the Launch Operations Center (LOC). Also, Cape Canaveral was inadequate to host the new launch facility design required for the mammoth 363-foot (111 m) tall, 7,500,000-pound-force (33,000 kN) thrust Saturn V rocket, which would be assembled vertically in a large hangar and transported on a mobile platform to one of several launch pads. Therefore, the decision was made to build a new LOC site located adjacent to Cape Canaveral on Merritt Island.

 

NASA began land acquisition in 1962, buying title to 131 square miles (340 km2) and negotiating with the state of Florida for an additional 87 square miles (230 km2). The major buildings in KSC's Industrial Area were designed by architect Charles Luckman. Construction began in November 1962, and Kennedy visited the site twice in 1962, and again just a week before his assassination on November 22, 1963.

 

On November 29, 1963, the facility was named by President Lyndon B. Johnson under Executive Order 11129. Johnson's order joined both the civilian LOC and the military Cape Canaveral station ("the facilities of Station No. 1 of the Atlantic Missile Range") under the designation "John F. Kennedy Space Center", spawning some confusion joining the two in the public mind. NASA Administrator James E. Webb clarified this by issuing a directive stating the Kennedy Space Center name applied only to the LOC, while the Air Force issued a general order renaming the military launch site Cape Kennedy Air Force Station.

 

Located on Merritt Island, Florida, the center is north-northwest of Cape Canaveral on the Atlantic Ocean, midway between Miami and Jacksonville on Florida's Space Coast, due east of Orlando. It is 34 miles (55 km) long and roughly six miles (9.7 km) wide, covering 219 square miles (570 km2). KSC is a major central Florida tourist destination and is approximately one hour's drive from the Orlando area. The Kennedy Space Center Visitor Complex offers public tours of the center and Cape Canaveral Space Force Station.

 

From 1967 through 1973, there were 13 Saturn V launches, including the ten remaining Apollo missions after Apollo 7. The first of two uncrewed flights, Apollo 4 (Apollo-Saturn 501) on November 9, 1967, was also the first rocket launch from KSC. The Saturn V's first crewed launch on December 21, 1968, was Apollo 8's lunar orbiting mission. The next two missions tested the Lunar Module: Apollo 9 (Earth orbit) and Apollo 10 (lunar orbit). Apollo 11, launched from Pad A on July 16, 1969, made the first Moon landing on July 20. The Apollo 11 launch included crewmembers Neil Armstrong, Michael Collins, and Buzz Aldrin, and attracted a record-breaking 650 million television viewers. Apollo 12 followed four months later. From 1970 to 1972, the Apollo program concluded at KSC with the launches of missions 13 through 17.

 

On May 14, 1973, the last Saturn V launch put the Skylab space station in orbit from Pad 39A. By this time, the Cape Kennedy pads 34 and 37 used for the Saturn IB were decommissioned, so Pad 39B was modified to accommodate the Saturn IB, and used to launch three crewed missions to Skylab that year, as well as the final Apollo spacecraft for the Apollo–Soyuz Test Project in 1975.

 

As the Space Shuttle was being designed, NASA received proposals for building alternative launch-and-landing sites at locations other than KSC, which demanded study. KSC had important advantages, including its existing facilities; location on the Intracoastal Waterway; and its southern latitude, which gives a velocity advantage to missions launched in easterly near-equatorial orbits. Disadvantages included: its inability to safely launch military missions into polar orbit, since spent boosters would be likely to fall on the Carolinas or Cuba; corrosion from the salt air; and frequent cloudy or stormy weather. Although building a new site at White Sands Missile Range in New Mexico was seriously considered, NASA announced its decision in April 1972 to use KSC for the shuttle. Since the Shuttle could not be landed automatically or by remote control, the launch of Columbia on April 12, 1981 for its first orbital mission STS-1, was NASA's first crewed launch of a vehicle that had not been tested in prior uncrewed launches.

 

In 1976, the VAB's south parking area was the site of Third Century America, a science and technology display commemorating the U.S. Bicentennial. Concurrent with this event, the U.S. flag was painted on the south side of the VAB. During the late 1970s, LC-39 was reconfigured to support the Space Shuttle. Two Orbiter Processing Facilities were built near the VAB as hangars with a third added in the 1980s.

 

KSC's 2.9-mile (4.7 km) Shuttle Landing Facility (SLF) was the orbiters' primary end-of-mission landing site, although the first KSC landing did not take place until the tenth flight, when Challenger completed STS-41-B on February 11, 1984; the primary landing site until then was Edwards Air Force Base in California, subsequently used as a backup landing site. The SLF also provided a return-to-launch-site (RTLS) abort option, which was not utilized. The SLF is among the longest runways in the world.

 

On October 28, 2009, the Ares I-X launch from Pad 39B was the first uncrewed launch from KSC since the Skylab workshop in 1973.

 

Beginning in 1958, NASA and military worked side by side on robotic mission launches (previously referred to as unmanned), cooperating as they broke ground in the field. In the early 1960s, NASA had as many as two robotic mission launches a month. The frequent number of flights allowed for quick evolution of the vehicles, as engineers gathered data, learned from anomalies and implemented upgrades. In 1963, with the intent of KSC ELV work focusing on the ground support equipment and facilities, a separate Atlas/Centaur organization was formed under NASA's Lewis Center (now Glenn Research Center (GRC)), taking that responsibility from the Launch Operations Center (aka KSC).

 

Though almost all robotics missions launched from the Cape Canaveral Space Force Station (CCSFS), KSC "oversaw the final assembly and testing of rockets as they arrived at the Cape." In 1965, KSC's Unmanned Launch Operations directorate became responsible for all NASA uncrewed launch operations, including those at Vandenberg Space Force Base. From the 1950s to 1978, KSC chose the rocket and payload processing facilities for all robotic missions launching in the U.S., overseeing their near launch processing and checkout. In addition to government missions, KSC performed this service for commercial and foreign missions also, though non-U.S. government entities provided reimbursement. NASA also funded Cape Canaveral Space Force Station launch pad maintenance and launch vehicle improvements.

 

All this changed with the Commercial Space Launch Act of 1984, after which NASA only coordinated its own and National Oceanic and Atmospheric Administration (NOAA) ELV launches. Companies were able to "operate their own launch vehicles" and utilize NASA's launch facilities. Payload processing handled by private firms also started to occur outside of KSC. Reagan's 1988 space policy furthered the movement of this work from KSC to commercial companies. That same year, launch complexes on Cape Canaveral Air Force Force Station started transferring from NASA to Air Force Space Command management.

 

In the 1990s, though KSC was not performing the hands-on ELV work, engineers still maintained an understanding of ELVs and had contracts allowing them insight into the vehicles so they could provide knowledgeable oversight. KSC also worked on ELV research and analysis and the contractors were able to utilize KSC personnel as a resource for technical issues. KSC, with the payload and launch vehicle industries, developed advances in automation of the ELV launch and ground operations to enable competitiveness of U.S. rockets against the global market.

 

In 1998, the Launch Services Program (LSP) formed at KSC, pulling together programs (and personnel) that already existed at KSC, GRC, Goddard Space Flight Center, and more to manage the launch of NASA and NOAA robotic missions. Cape Canaveral Space Force Station and VAFB are the primary launch sites for LSP missions, though other sites are occasionally used. LSP payloads such as the Mars Science Laboratory have been processed at KSC before being transferred to a launch pad on Cape Canaveral Space Force Station.

 

On 16 November 2022, at 06:47:44 UTC the Space Launch System (SLS) was launched from Complex 39B as part of the Artemis 1 mission.

 

As the International Space Station modules design began in the early 1990s, KSC began to work with other NASA centers and international partners to prepare for processing before launch onboard the Space Shuttles. KSC utilized its hands-on experience processing the 22 Spacelab missions in the Operations and Checkout Building to gather expectations of ISS processing. These experiences were incorporated into the design of the Space Station Processing Facility (SSPF), which began construction in 1991. The Space Station Directorate formed in 1996. KSC personnel were embedded at station module factories for insight into their processes.

 

From 1997 to 2007, KSC planned and performed on the ground integration tests and checkouts of station modules: three Multi-Element Integration Testing (MEIT) sessions and the Integration Systems Test (IST). Numerous issues were found and corrected that would have been difficult to nearly impossible to do on-orbit.

 

Today KSC continues to process ISS payloads from across the world before launch along with developing its experiments for on orbit. The proposed Lunar Gateway would be manufactured and processed at the Space Station Processing Facility.

 

The following are current programs and initiatives at Kennedy Space Center:

Commercial Crew Program

Exploration Ground Systems Program

NASA is currently designing the next heavy launch vehicle known as the Space Launch System (SLS) for continuation of human spaceflight.

On December 5, 2014, NASA launched the first uncrewed flight test of the Orion Multi-Purpose Crew Vehicle (MPCV), currently under development to facilitate human exploration of the Moon and Mars.

Launch Services Program

Educational Launch of Nanosatellites (ELaNa)

Research and Technology

Artemis program

Lunar Gateway

International Space Station Payloads

Camp KSC: educational camps for schoolchildren in spring and summer, with a focus on space, aviation and robotics.

 

The KSC Industrial Area, where many of the center's support facilities are located, is 5 miles (8 km) south of LC-39. It includes the Headquarters Building, the Operations and Checkout Building and the Central Instrumentation Facility. The astronaut crew quarters are in the O&C; before it was completed, the astronaut crew quarters were located in Hangar S at the Cape Canaveral Missile Test Annex (now Cape Canaveral Space Force Station). Located at KSC was the Merritt Island Spaceflight Tracking and Data Network station (MILA), a key radio communications and spacecraft tracking complex.

 

Facilities at the Kennedy Space Center are directly related to its mission to launch and recover missions. Facilities are available to prepare and maintain spacecraft and payloads for flight. The Headquarters (HQ) Building houses offices for the Center Director, library, film and photo archives, a print shop and security. When the KSC Library first opened, it was part of the Army Ballistic Missile Agency. However, in 1965, the library moved into three separate sections in the newly opened NASA headquarters before eventually becoming a single unit in 1970. The library contains over four million items related to the history and the work at Kennedy. As one of ten NASA center libraries in the country, their collection focuses on engineering, science, and technology. The archives contain planning documents, film reels, and original photographs covering the history of KSC. The library is not open to the public but is available for KSC, Space Force, and Navy employees who work on site. Many of the media items from the collection are digitized and available through NASA's KSC Media Gallery Archived December 6, 2020, at the Wayback Machine or through their more up-to-date Flickr gallery.

 

A new Headquarters Building was completed in 2019 as part of the Central Campus consolidation. Groundbreaking began in 2014.

 

The center operated its own 17-mile (27 km) short-line railroad. This operation was discontinued in 2015, with the sale of its final two locomotives. A third had already been donated to a museum. The line was costing $1.3 million annually to maintain.

 

The Neil Armstrong Operations and Checkout Building (O&C) (previously known as the Manned Spacecraft Operations Building) is a historic site on the U.S. National Register of Historic Places dating back to the 1960s and was used to receive, process, and integrate payloads for the Gemini and Apollo programs, the Skylab program in the 1970s, and for initial segments of the International Space Station through the 1990s. The Apollo and Space Shuttle astronauts would board the astronaut transfer van to launch complex 39 from the O&C building.

The three-story, 457,000-square-foot (42,500 m2) Space Station Processing Facility (SSPF) consists of two enormous processing bays, an airlock, operational control rooms, laboratories, logistics areas and office space for support of non-hazardous Space Station and Shuttle payloads to ISO 14644-1 class 5 standards. Opened in 1994, it is the largest factory building in the KSC industrial area.

The Vertical Processing Facility (VPF) features a 71-by-38-foot (22 by 12 m) door where payloads that are processed in the vertical position are brought in and manipulated with two overhead cranes and a hoist capable of lifting up to 35 short tons (32 t).

The Hypergolic Maintenance and Checkout Area (HMCA) comprises three buildings that are isolated from the rest of the industrial area because of the hazardous materials handled there. Hypergolic-fueled modules that made up the Space Shuttle Orbiter's reaction control system, orbital maneuvering system and auxiliary power units were stored and serviced in the HMCF.

The Multi-Payload Processing Facility is a 19,647 square feet (1,825.3 m2) building used for Orion spacecraft and payload processing.

The Payload Hazardous Servicing Facility (PHSF) contains a 70-by-110-foot (21 by 34 m) service bay, with a 100,000-pound (45,000 kg), 85-foot (26 m) hook height. It also contains a 58-by-80-foot (18 by 24 m) payload airlock. Its temperature is maintained at 70 °F (21 °C).[55]

The Blue Origin rocket manufacturing facility is located immediately south of the KSC visitor complex. Completed in 2019, it serves as the company's factory for the manufacture of New Glenn orbital rockets.

 

Launch Complex 39 (LC-39) was originally built for the Saturn V, the largest and most powerful operational launch vehicle until the Space Launch System, for the Apollo crewed Moon landing program. Since the end of the Apollo program in 1972, LC-39 has been used to launch every NASA human space flight, including Skylab (1973), the Apollo–Soyuz Test Project (1975), and the Space Shuttle program (1981–2011).

 

Since December 1968, all launch operations have been conducted from launch pads A and B at LC-39. Both pads are on the ocean, 3 miles (4.8 km) east of the VAB. From 1969 to 1972, LC-39 was the "Moonport" for all six Apollo crewed Moon landing missions using the Saturn V, and was used from 1981 to 2011 for all Space Shuttle launches.

 

Human missions to the Moon required the large three-stage Saturn V rocket, which was 363 feet (111 meters) tall and 33 feet (10 meters) in diameter. At KSC, Launch Complex 39 was built on Merritt Island to accommodate the new rocket. Construction of the $800 million project began in November 1962. LC-39 pads A and B were completed by October 1965 (planned Pads C, D and E were canceled), the VAB was completed in June 1965, and the infrastructure by late 1966.

 

The complex includes: the Vehicle Assembly Building (VAB), a 130,000,000 cubic feet (3,700,000 m3) hangar capable of holding four Saturn Vs. The VAB was the largest structure in the world by volume when completed in 1965.

a transporter capable of carrying 5,440 tons along a crawlerway to either of two launch pads;

a 446-foot (136 m) mobile service structure, with three Mobile Launcher Platforms, each containing a fixed launch umbilical tower;

the Launch Control Center; and

a news media facility.

 

Launch Complex 48 (LC-48) is a multi-user launch site under construction for small launchers and spacecraft. It will be located between Launch Complex 39A and Space Launch Complex 41, with LC-39A to the north and SLC-41 to the south. LC-48 will be constructed as a "clean pad" to support multiple launch systems with differing propellant needs. While initially only planned to have a single pad, the complex is capable of being expanded to two at a later date.

 

As a part of promoting commercial space industry growth in the area and the overall center as a multi-user spaceport, KSC leases some of its properties. Here are some major examples:

 

Exploration Park to multiple users (partnership with Space Florida)

Shuttle Landing Facility to Space Florida (who contracts use to private companies)

Orbiter Processing Facility (OPF)-3 to Boeing (for CST-100 Starliner)

Launch Complex 39A, Launch Control Center Firing Room 4 and land for SpaceX's Roberts Road facility (Hanger X) to SpaceX

O&C High Bay to Lockheed Martin (for Orion processing)

Land for FPL's Space Coast Next Generation Solar Energy Center to Florida Power and Light (FPL)

Hypergolic Maintenance Facility (HMF) to United Paradyne Corporation (UPC)

 

The Kennedy Space Center Visitor Complex, operated by Delaware North since 1995, has a variety of exhibits, artifacts, displays and attractions on the history and future of human and robotic spaceflight. Bus tours of KSC originate from here. The complex also includes the separate Apollo/Saturn V Center, north of the VAB and the United States Astronaut Hall of Fame, six miles west near Titusville. There were 1.5 million visitors in 2009. It had some 700 employees.

 

It was announced on May 29, 2015, that the Astronaut Hall of Fame exhibit would be moved from its current location to another location within the Visitor Complex to make room for an upcoming high-tech attraction entitled "Heroes and Legends". The attraction, designed by Orlando-based design firm Falcon's Treehouse, opened November 11, 2016.

 

In March 2016, the visitor center unveiled the new location of the iconic countdown clock at the complex's entrance; previously, the clock was located with a flagpole at the press site. The clock was originally built and installed in 1969 and listed with the flagpole in the National Register of Historic Places in January 2000. In 2019, NASA celebrated the 50th anniversary of the Apollo program, and the launch of Apollo 10 on May 18. In summer of 2019, Lunar Module 9 (LM-9) was relocated to the Apollo/Saturn V Center as part of an initiative to rededicate the center and celebrate the 50th anniversary of the Apollo Program.

 

Historic locations

NASA lists the following Historic Districts at KSC; each district has multiple associated facilities:

 

Launch Complex 39: Pad A Historic District

Launch Complex 39: Pad B Historic District

Shuttle Landing Facility (SLF) Area Historic District

Orbiter Processing Historic District

Solid Rocket Booster (SRB) Disassembly and Refurbishment Complex Historic District

NASA KSC Railroad System Historic District

NASA-owned Cape Canaveral Space Force Station Industrial Area Historic District

There are 24 historic properties outside of these historic districts, including the Space Shuttle Atlantis, Vehicle Assembly Building, Crawlerway, and Operations and Checkout Building.[71] KSC has one National Historic Landmark, 78 National Register of Historic Places (NRHP) listed or eligible sites, and 100 Archaeological Sites.

 

Further information: John F. Kennedy Space Center MPS

Other facilities

The Rotation, Processing and Surge Facility (RPSF) is responsible for the preparation of solid rocket booster segments for transportation to the Vehicle Assembly Building (VAB). The RPSF was built in 1984 to perform SRB operations that had previously been conducted in high bays 2 and 4 of the VAB at the beginning of the Space Shuttle program. It was used until the Space Shuttle's retirement, and will be used in the future by the Space Launch System[75] (SLS) and OmegA rockets.

Includes teams from Deuel, Hot Springs, Madison, Parkston/Ethan/Hanson/Mt. Vernon. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.

©2021 SDPB

 

In a mono mood on Worthing seafront today - sunny with a bracing wind

A calm evening on the River Adur

The Ajanta Caves (Ajiṇṭhā leni; Marathi: अजिंठा लेणी) in Aurangabad district of Maharashtra, India are about 30 rock-cut Buddhist cave monuments which date from the 2nd century BCE to about 480 or 650 CE. The caves include paintings and sculptures described by the government Archaeological Survey of India as "the finest surviving examples of Indian art, particularly painting", which are masterpieces of Buddhist religious art, with figures of the Buddha and depictions of the Jataka tales. The caves were built in two phases starting around the 2nd century BCE, with the second group of caves built around 400–650 CE according to older accounts, or all in a brief period of 460 to 480 according to the recent proposals of Walter M. Spink. The site is a protected monument in the care of the Archaeological Survey of India, and since 1983, the Ajanta Caves have been a UNESCO World Heritage Site.

 

The caves are located in the Indian state of Maharashtra, near Jalgaon and just outside the village of Ajinṭhā 20°31′56″N 75°44′44″E), about 59 kilometres from Jalgaon railway station on the Delhi – Mumbai line and Howrah-Nagpur-Mumbai line of the Central Railway zone, and 104 kilometres from the city of Aurangabad. They are 100 kilometres from the Ellora Caves, which contain Hindu and Jain temples as well as Buddhist caves, the last dating from a period similar to Ajanta. The Ajanta caves are cut into the side of a cliff that is on the south side of a U-shaped gorge on the small river Waghur, and although they are now along and above a modern pathway running across the cliff they were originally reached by individual stairs or ladders from the side of the river 35 to 110 feet below.

 

The area was previously heavily forested, and after the site ceased to be used the caves were covered by jungle until accidentally rediscovered in 1819 by a British officer on a hunting party. They are Buddhist monastic buildings, apparently representing a number of distinct "monasteries" or colleges. The caves are numbered 1 to 28 according to their place along the path, beginning at the entrance. Several are unfinished and some barely begun and others are small shrines, included in the traditional numbering as e.g. "9A"; "Cave 15A" was still hidden under rubble when the numbering was done. Further round the gorge are a number of waterfalls, which when the river is high are audible from outside the caves.

 

The caves form the largest corpus of early Indian wall-painting; other survivals from the area of modern India are very few, though they are related to 5th-century paintings at Sigiriya in Sri Lanka. The elaborate architectural carving in many caves is also very rare, and the style of the many figure sculptures is highly local, found only at a few nearby contemporary sites, although the Ajanta tradition can be related to the later Hindu Ellora Caves and other sites.

 

HISTORY

Like the other ancient Buddhist monasteries, Ajanta had a large emphasis on teaching, and was divided into several different caves for living, education and worship, under a central direction. Monks were probably assigned to specific caves for living. The layout reflects this organizational structure, with most of the caves only connected through the exterior. The 7th-century travelling Chinese scholar Xuanzang informs us that Dignaga, a celebrated Buddhist philosopher and controversialist, author of well-known books on logic, lived at Ajanta in the 5th century. In its prime the settlement would have accommodated several hundred teachers and pupils. Many monks who had finished their first training may have returned to Ajanta during the monsoon season from an itinerant lifestyle.

 

The caves are generally agreed to have been made in two distinct periods, separated by several centuries.

 

CAVES OF THE FIRST (SATAVAHANA) PERIOD

The earliest group of caves consists of caves 9, 10, 12, 13 and 15A. According to Walter Spink, they were made during the period 100 BCE to 100 CE, probably under the patronage of the Satavahana dynasty (230 BCE – c. 220 CE) who ruled the region. Other datings prefer the period 300 BCE to 100 BCE, though the grouping of the earlier caves is generally agreed. More early caves may have vanished through later excavations. Of these, caves 9 and 10 are stupa halls of chaitya-griha form, and caves 12, 13, and 15A are vihāras (see the architecture section below for descriptions of these types). The first phase is still often called the Hinayāna phase, as it originated when, using traditional terminology, the Hinayāna or Lesser Vehicle tradition of Buddhism was dominant, when the Buddha was revered symbolically. However the use of the term Hinayana for this period of Buddhism is now deprecated by historians; equally the caves of the second period are now mostly dated too early to be properly called Mahayana, and do not yet show the full expanded cast of supernatural beings characteristic of that phase of Buddhist art. The first Satavahana period caves lacked figurative sculpture, emphasizing the stupa instead, and in the caves of the second period the overwhelming majority of images represent the Buddha alone, or narrative scenes of his lives.

 

Spink believes that some time after the Satavahana period caves were made the site was abandoned for a considerable period until the mid-5th century, probably because the region had turned mainly Hindu

 

CAVES OF THE LATER OR VAKATAKA PERIOD

The second phase began in the 5th century. For a long time it was thought that the later caves were made over a long period from the 4th to the 7th centuries CE, but in recent decades a series of studies by the leading expert on the caves, Walter M. Spink, have argued that most of the work took place over the very brief period from 460 to 480 CE, during the reign of Emperor Harishena of the Vakataka dynasty. This view has been criticized by some scholars, but is now broadly accepted by most authors of general books on Indian art, for example Huntington and Harle.

 

The second phase is still often called the Mahāyāna or Greater Vehicle phase, but scholars now tend to avoid this nomenclature because of the problems that have surfaced regarding our understanding of Mahāyāna.

 

Some 20 cave temples were simultaneously created, for the most part viharas with a sanctuary at the back. The most elaborate caves were produced in this period, which included some "modernization" of earlier caves. Spink claims that it is possible to establish dating for this period with a very high level of precision; a fuller account of his chronology is given below. Although debate continues, Spink's ideas are increasingly widely accepted, at least in their broad conclusions. The Archaeological Survey of India website still presents the traditional dating: "The second phase of paintings started around 5th – 6th centuries A.D. and continued for the next two centuries". Caves of the second period are 1–8, 11, 14–29, some possibly extensions of earlier caves. Caves 19, 26, and 29 are chaitya-grihas, the rest viharas.

 

According to Spink, the Ajanta Caves appear to have been abandoned by wealthy patrons shortly after the fall of Harishena, in about 480 CE. They were then gradually abandoned and forgotten. During the intervening centuries, the jungle grew back and the caves were hidden, unvisited and undisturbed, although the local population were aware of at least some of them.

 

REDISCOVERY

On 28 April 1819, a British officer for the Madras Presidency, John Smith, of the 28th Cavalry, while hunting tiger, accidentally discovered the entrance to Cave No. 10 deep within the tangled undergrowth. There were local people already using the caves for prayers with a small fire, when he arrived. Exploring that first cave, long since a home to nothing more than birds and bats and a lair for other larger animals, Captain Smith vandalized the wall by scratching his name and the date, April 1819. Since he stood on a five-foot high pile of rubble collected over the years, the inscription is well above the eye-level gaze of an adult today. A paper on the caves by William Erskine was read to the Bombay Literary Society in 1822. Within a few decades, the caves became famous for their exotic setting, impressive architecture, and above all their exceptional, all but unique paintings. A number of large projects to copy the paintings were made in the century after rediscovery, covered below. In 1848 the Royal Asiatic Society established the "Bombay Cave Temple Commission" to clear, tidy and record the most important rock-cut sites in the Bombay Presidency, with John Wilson, as president. In 1861 this became the nucleus of the new Archaeological Survey of India. Until the Nizam of Hyderabad built the modern path between the caves, among other efforts to make the site easy to visit, a trip to Ajanta was a considerable adventure, and contemporary accounts dwell with relish on the dangers from falls off narrow ledges, animals and the Bhil people, who were armed with bows and arrows and had a fearsome reputation.

 

Today, fairly easily combined with Ellora in a single trip, the caves are the most popular tourist destination in Mahrashtra, and are often crowded at holiday times, increasing the threat to the caves, especially the paintings. In 2012, the Maharashtra Tourism Development Corporation announced plans to add to the ASI visitor centre at the entrance complete replicas of caves 1, 2, 16 & 17 to reduce crowding in the originals, and enable visitors to receive a better visual idea of the paintings, which are dimly-lit and hard to read in the caves. Figures for the year to March 2010 showed a total of 390,000 visitors to the site, divided into 362,000 domestic and 27,000 foreign. The trends over the previous few years show a considerable growth in domestic visitors, but a decline in foreign ones; the year to 2010 was the first in which foreign visitors to Ellora exceeded those to Ajanta.

 

PAINTINGS

Mural paintings survive from both the earlier and later groups of caves. Several fragments of murals preserved from the earlier caves (Caves 9 and 11) are effectively unique survivals of court-led painting in India from this period, and "show that by Sātavāhana times, if not earlier, the Indian painter had mastered an easy and fluent naturalistic style, dealing with large groups of people in a manner comparable to the reliefs of the Sāñcī toraņa crossbars".

 

Four of the later caves have large and relatively well-preserved mural paintings which "have come to represent Indian mural painting to the non-specialist", and fall into two stylistic groups, with the most famous in Caves 16 and 17, and apparently later paintings in Caves 1 and 2. The latter group were thought to be a century or more later than the others, but the revised chronology proposed by Spink would place them much closer to the earlier group, perhaps contemporary with it in a more progressive style, or one reflecting a team from a different region. The paintings are in "dry fresco", painted on top of a dry plaster surface rather than into wet plaster.

 

All the paintings appear to be the work of painters at least as used to decorating palaces as temples, and show a familiarity with and interest in details of the life of a wealthy court. We know from literary sources that painting was widely practised and appreciated in the courts of the Gupta period. Unlike much Indian painting, compositions are not laid out in horizontal compartments like a frieze, but show large scenes spreading in all directions from a single figure or group at the centre. The ceilings are also painted with sophisticated and elaborate decorative motifs, many derived from sculpture. The paintings in cave 1, which according to Spink was commissioned by Harisena himself, concentrate on those Jataka tales which show previous lives of the Buddha as a king, rather than as an animal or human commoner, and so show settings from contemporary palace life.

 

In general the later caves seem to have been painted on finished areas as excavating work continued elsewhere in the cave, as shown in caves 2 and 16 in particular. According to Spink's account of the chronology of the caves, the abandonment of work in 478 after a brief busy period accounts for the absence of painting in caves such as 4 and 17, the later being plastered in preparation for paintings that were never done.

 

COPIES

The paintings have deteriorated significantly since they were rediscovered, and a number of 19th-century copies and drawings are important for a complete understanding of the works. However, the earliest projects to copy the paintings were plagued by bad fortune. In 1846, Major Robert Gill, an Army officer from Madras presidency and a painter, was appointed by the Royal Asiatic Society to replicate the frescoes on the cave walls to exhibit these paintings in England. Gill worked on his painting at the site from 1844 to 1863 (though he continued to be based there until his death in 1875, writing books and photographing) and made 27 copies of large sections of murals, but all but four were destroyed in a fire at the Crystal Palace in London in 1866, where they were on display.

 

Another attempt was made in 1872 when the Bombay Presidency commissioned John Griffiths, then principal of the Bombay School of Art, to work with his students to make new copies, again for shipping to England. They worked on this for thirteen years and some 300 canvases were produced, many of which were displayed at the Imperial Institute on Exhibition Road in London, one of the forerunners of the Victoria and Albert Museum. But in 1885 another fire destroyed over a hundred paintings that were in storage. The V&A still has 166 paintings surviving from both sets, though none have been on permanent display since 1955. The largest are some 3 × 6 metres. A conservation project was undertaken on about half of them in 2006, also involving the University of Northumbria. Griffith and his students had unfortunately painted many of the paintings with "cheap varnish" in order to make them easier to see, which has added to the deterioration of the originals, as has, according to Spink and others, recent cleaning by the ASI.

 

A further set of copies were made between 1909 and 1911 by Christiana Herringham (Lady Herringham) and a group of students from the Calcutta School of Art that included the future Indian Modernist painter Nandalal Bose. The copies were published in full colour as the first publication of London's fledgling India Society. More than the earlier copies, these aimed to fill in holes and damage to recreate the original condition rather than record the state of the paintings as she was seeing them. According to one writer, unlike the paintings created by her predecessors Griffiths and Gill, whose copies were influenced by British Victorian styles of painting, those of the Herringham expedition preferred an 'Indian Renascence' aesthetic of the type pioneered by Abanindranath Tagore.

 

Early photographic surveys were made by Robert Gill, who learnt to use a camera from about 1856, and whose photos, including some using stereoscopy, were used in books by him and Fergusson (many are available online from the British Library), then Victor Goloubew in 1911 and E.L. Vassey, who took the photos in the four volume study of the caves by Ghulam Yazdani (published 1930–1955).

 

ARCHITECTURE

The monasteries mostly consist of vihara halls for prayer and living, which are typically rectangular with small square dormitory cells cut into the walls, and by the second period a shrine or sanctuary at the rear centred on a large statue of the Buddha, also carved from the living rock. This change reflects the movement from Hinayana to Mahāyāna Buddhism. The other type of main hall is the narrower and higher chaitya hall with a stupa as the focus at the far end, and a narrow aisle around the walls, behind a range of pillars placed close together. Other plainer rooms were for sleeping and other activities. Some of the caves have elaborate carved entrances, some with large windows over the door to admit light. There is often a colonnaded porch or verandah, with another space inside the doors running the width of the cave.

 

The central square space of the interior of the viharas is defined by square columns forming a more or less square open area. Outside this are long rectangular aisles on each side, forming a kind of cloister. Along the side and rear walls are a number of small cells entered by a narrow doorway; these are roughly square, and have small niches on their back walls. Originally they had wooden doors. The centre of the rear wall has a larger shrine-room behind, containing a large Buddha statue. The viharas of the earlier period are much simpler, and lack shrines. Spink in fact places the change to a design with a shrine to the middle of the second period, with many caves being adapted to add a shrine in mid-excavation, or after the original phase.

 

The plan of Cave 1 shows one of the largest viharas, but is fairly typical of the later group. Many others, such as Cave 16, lack the vestibule to the shrine, which leads straight off the main hall. Cave 6 is two viharas, one above the other, connected by internal stairs, with sanctuaries on both levels.

 

The four completed chaitya halls are caves 9 and 10 from the early period, and caves 19 and 26 from the later period of construction. All follow the typical form found elsewhere, with high ceilings and a central "nave" leading to the stupa, which is near the back, but allows walking behind it, as walking around stupas was (and remains) a common element of Buddhist worship (pradakshina). The later two have high ribbed roofs, which reflect timber forms, and the earlier two are thought to have used actual timber ribs, which have now perished. The two later halls have a rather unusual arrangement (also found in Cave 10 at Ellora) where the stupa is fronted by a large relief sculpture of the Buddha, standing in Cave 19 and seated in Cave 26. Cave 29 is a late and very incomplete chaitya hall.

 

The form of columns in the work of the first period is very plain and un-embellished, with both chaitya halls using simple octagonal columns, which were painted with figures. In the second period columns were far more varied and inventive, often changing profile over their height, and with elaborate carved capitals, often spreading wide. Many columns are carved over all their surface, some fluted and others carved with decoration all over, as in cave 1.

 

The flood basalt rock of the cliff, part of the Deccan Traps formed by successive volcanic eruptions at the end of the Cretaceous, is layered horizontally, and somewhat variable in quality, so the excavators had to amend their plans in places, and in places there have been collapses in the intervening centuries, as with the lost portico to cave 1. Excavation began by cutting a narrow tunnel at roof level, which was expanded downwards and outwards; the half-built vihara cave 24 shows the method. Spink believes that for the first caves of the second period the excavators had to relearn skills and techniques that had been lost in the centuries since the first period, which were then transmitted to be used at later rock-cut sites in the region, such as Ellora, and the Elephanta, Bagh, Badami and Aurangabad Caves.

 

The caves from the first period seem to have been paid for by a number of different patrons, with several inscriptions recording the donation of particular portions of a single cave, but according to Spink the later caves were each commissioned as a complete unit by a single patron from the local rulers or their court elites. After the death of Harisena smaller donors got their chance to add small "shrinelets" between the caves or add statues to existing caves, and some two hundred of these "intrusive" additions were made in sculpture, with a further number of intrusive paintings, up to three hundred in cave 10 alone.

 

A grand gateway to the site, at the apex of the gorge's horsehoe between caves 15 and 16, was approached from the river, and is decorated with elephants on either side and a nāga, or protective snake deity.

 

ICONOGRAPHY OF THE CAVES

In the pre-Christian era, the Buddha was represented symbolically, in the form of the stupa. Thus, halls were made with stupas to venerate the Buddha. In later periods the images of the Buddha started to be made in coins, relic caskets, relief or loose sculptural forms, etc. However, it took a while for the human representation of the Buddha to appear in Buddhist art. One of the earliest evidences of the Buddha's human representations are found at Buddhist archaeological sites, such as Goli, Nagarjunakonda, and Amaravati. The monasteries of those sites were built in less durable media, such as wood, brick, and stone. As far as the genre of rock-cut architecture is concerned it took many centuries for the Buddha image to be depicted. Nobody knows for sure at which rock-cut cave site the first image of the Buddha was depicted. Current research indicates that Buddha images in a portable form, made of wood or stone, were introduced, for the first time, at Kanheri, to be followed soon at Ajanta Cave 8 (Dhavalikar, Jadhav, Spink, Singh). While the Kanheri example dates to 4th or 5th century CE, the Ajanta example has been dated to c. 462–478 CE (Spink). None of the rock-cut monasteries prior to these dates, and other than these examples, show any Buddha image although hundreds of rock-cut caves were made throughout India during the first few centuries CE. And, in those caves, it is the stupa that is the object of veneration, not the image. Images of the Buddha are not found in Buddhist sailagrhas (rock-cut complexes) until the times of the Kanheri (4th–5th century CE) and Ajanta examples (c. 462–478 CE).

 

The caves of the second period, now all dated to the 5th century, were typically described as "Mahayana", but do not show the features associated with later Mahayana Buddhism. Although the beginnings of Mahāyāna teachings go back to the 1st century there is little art and archaeological evidence to suggest that it became a mainstream cult for several centuries. In Mahayana it is not Gautama Buddha but the Bodhisattva who is important, including "deity" Bodhisattva like Manjushri and Tara, as well as aspects of the Buddha such as Aksobhya, and Amitabha. Except for a few Bodhisattva, these are not depicted at Ajanta, where the Buddha remains the dominant figure. Even the Bodhisattva images of Ajanta are never central objects of worship, but are always shown as attendants of the Buddha in the shrine. If a Bodhisattva is shown in isolation, as in the Astabhaya scenes, these were done in the very last years of activities at Ajanta, and are mostly 'intrusive' in nature, meaning that they were not planned by the original patrons, and were added by new donors after the original patrons had suddenly abandoned the region in the wake of Emperor Harisena's death.

 

The contrast between iconic and aniconic representations, that is, the stupa on one hand and the image of the Buddha on the other, is now being seen as a construct of the modern scholar rather than a reality of the past. The second phase of Ajanta shows that the stupa and image coincided together. If the entire corpus of the art of Ajanta including sculpture, iconography, architecture, epigraphy, and painting are analysed afresh it will become clear that there was no duality between the symbolic and human forms of the Buddha, as far as the 5th-century phase of Ajanta is concerned. That is why most current scholars tend to avoid the terms 'Hinayana' and 'Mahayana' in the context of Ajanta. They now prefer to call the second phase by the ruling dynasty, as the Vākāţaka phase.

 

CAVES

CAVE 1

Cave 1 was built on the eastern end of the horse-shoe shaped scarp, and is now the first cave the visitor encounters. This would when first made have been a less prominent position, right at the end of the row. According to Spink, it is one of the latest caves to have been excavated, when the best sites had been taken, and was never fully inaugurated for worship by the dedication of the Buddha image in the central shrine. This is shown by the absence of sooty deposits from butter lamps on the base of the shrine image, and the lack of damage to the paintings that would have been happened if the garland-hooks around the shrine had been in use for any period of time. Although there is no epigraphic evidence, Spink believes that the Vākāţaka Emperor Harishena was the benefactor of the work, and this is reflected in the emphasis on imagery of royalty in the cave, with those Jakata tales being selected that tell of those previous lives of the Buddha in which he was royal.

 

The cliff has a more steep slope here than at other caves, so to achieve a tall grand facade it was necessary to cut far back into the slope, giving a large courtyard in front of the facade. There was originally a columned portico in front of the present facade, which can be seen "half-intact in the 1880s" in pictures of the site, but this fell down completely and the remains, despite containing fine carving, were carelessly thrown down the slope into the river, from where they have been lost, presumably carried away in monsoon torrents.

 

This cave has one of the most elaborate carved façades, with relief sculptures on entablature and ridges, and most surfaces embellished with decorative carving. There are scenes carved from the life of the Buddha as well as a number of decorative motifs. A two pillared portico, visible in the 19th-century photographs, has since perished. The cave has a front-court with cells fronted by pillared vestibules on either side. These have a high plinth level. The cave has a porch with simple cells on both ends. The absence of pillared vestibules on the ends suggest that the porch was not excavated in the latest phase of Ajanta when pillared vestibules had become a necessity and norm. Most areas of the porch were once covered with murals, of which many fragments remain, especially on the ceiling. There are three doorways: a central doorway and two side doorways. Two square windows were carved between the doorways to brighten the interiors.

 

Each wall of the hall inside is nearly 12 m long and 6.1 m high. Twelve pillars make a square colonnade inside supporting the ceiling, and creating spacious aisles along the walls. There is a shrine carved on the rear wall to house an impressive seated image of the Buddha, his hands being in the dharmachakrapravartana mudra. There are four cells on each of the left, rear, and the right walls, though due to rock fault there are none at the ends of the rear aisle. The walls are covered with paintings in a fair state of preservation, though the full scheme was never completed. The scenes depicted are mostly didactic, devotional, and ornamental, with scenes from the Jataka stories of the Buddha's former existences as a bodhisattva), the life of the Gautama Buddha, and those of his veneration. The two most famous individual painted images at Ajanta are the two over-life size figures of the protective bodhisattvas Padmapani and Vajrapani on either side of the entrance to the Buddha shrine on the wall of the rear aisle (see illustrations above). According to Spink, the original dating of the paintings to about 625 arose largely or entirely because James Fegusson, a 19th-century architectural historian, had decided that a scene showing an ambassador being received, with figures in Persian dress, represented a recorded embassy to Persia (from a Hindu monarch at that) around that date.

 

CAVE 2

Cave 2, adjacent to Cave 1, is known for the paintings that have been preserved on its walls, ceilings, and pillars. It looks similar to Cave 1 and is in a better state of preservation.

 

Cave 2 has a porch quite different from Cave one. Even the façade carvings seem to be different. The cave is supported by robust pillars, ornamented with designs. The front porch consists of cells supported by pillared vestibules on both ends. The cells on the previously "wasted areas" were needed to meet the greater housing requirements in later years. Porch-end cells became a trend in all later Vakataka excavations. The simple single cells on porch-ends were converted into CPVs or were planned to provide more room, symmetry, and beauty.

 

The paintings on the ceilings and walls of this porch have been widely published. They depict the Jataka tales that are stories of the Buddha's life in former existences as Bodhisattva. Just as the stories illustrated in cave 1 emphasize kingship, those in cave 2 show many "noble and powerful" women in prominent roles, leading to suggestions that the patron was an unknown woman. The porch's rear wall has a doorway in the center, which allows entrance to the hall. On either side of the door is a square-shaped window to brighten the interior.

 

The hall has four colonnades which are supporting the ceiling and surrounding a square in the center of the hall. Each arm or colonnade of the square is parallel to the respective walls of the hall, making an aisle in between. The colonnades have rock-beams above and below them. The capitals are carved and painted with various decorative themes that include ornamental, human, animal, vegetative, and semi-divine forms.

 

Paintings appear on almost every surface of the cave except for the floor. At various places the art work has become eroded due to decay and human interference. Therefore, many areas of the painted walls, ceilings, and pillars are fragmentary. The painted narratives of the Jataka tales are depicted only on the walls, which demanded the special attention of the devotee. They are didactic in nature, meant to inform the community about the Buddha's teachings and life through successive rebirths. Their placement on the walls required the devotee to walk through the aisles and 'read' the narratives depicted in various episodes. The narrative episodes are depicted one after another although not in a linear order. Their identification has been a core area of research since the site's rediscovery in 1819. Dieter Schlingloff's identifications have updated our knowledge on the subject.

 

CAVE 4

The Archeological Survey of India board outside the caves gives the following detail about cave 4: "This is the largest monastery planned on a grandiose scale but was never finished. An inscription on the pedestal of the buddha's image mentions that it was a gift from a person named Mathura and paleographically belongs to 6th century A.D. It consists of a verandah, a hypostylar hall, sanctum with an antechamber and a series of unfinished cells. The rear wall of the verandah contains the panel of Litany of Avalokiteśvara".

 

The sanctuary houses a colossal image of the Buddha in preaching pose flanked by bodhisattvas and celestial nymphs hovering above.

 

CAVES 9-10

Caves 9 and 10 are the two chaitya halls from the first period of construction, though both were also undergoing an uncompleted reworking at the end of the second period. Cave 10 was perhaps originally of the 1st century BCE, and cave 9 about a hundred years later. The small "shrinelets" called caves 9A to 9D and 10A also date from the second period, and were commissioned by individuals.

 

The paintings in cave 10 include some surviving from the early period, many from an incomplete programme of modernization in the second period, and a very large number of smaller late intrusive images, nearly all Buddhas and many with donor inscriptions from individuals. These mostly avoided over-painting the "official" programme and after the best positions were used up are tucked away in less prominent positions not yet painted; the total of these (including those now lost) was probably over 300, and the hands of many different artists are visible.

 

OTHER CAVES

Cave 3 is merely a start of an excavation; according to Spink it was begun right at the end of the final period of work and soon abandoned. Caves 5 and 6 are viharas, the latter on two floors, that were late works of which only the lower floor of cave 6 was ever finished. The upper floor of cave 6 has many private votive sculptures, and a shrine Buddha, but is otherwise unfinished. Cave 7 has a grand facade with two porticos but, perhaps because of faults in the rock, which posed problems in many caves, was never taken very deep into the cliff, and consists only of the two porticos and a shrine room with antechamber, with no central hall. Some cells were fitted in.

 

Cave 8 was long thought to date to the first period of construction, but Spink sees it as perhaps the earliest cave from the second period, its shrine an "afterthought". The statue may have been loose rather than carved from the living rock, as it has now vanished. The cave was painted, but only traces remain.

 

SPINK´S DETAILED CHRONOLOGY

Walter M. Spink has over recent decades developed a very precise and circumstantial chronology for the second period of work on the site, which unlike earlier scholars, he places entirely in the 5th century. This is based on evidence such as the inscriptions and artistic style, combined with the many uncompleted elements of the caves. He believes the earlier group of caves, which like other scholars he dates only approximately, to the period "between 100 BCE – 100 CE", were at some later point completely abandoned and remained so "for over three centuries", as the local population had turned mainly Hindu. This changed with the accession of the Emperor Harishena of the Vakataka Dynasty, who reigned from 460 to his death in 477. Harisena extended the Central Indian Vakataka Empire to include a stretch of the east coast of India; the Gupta Empire ruled northern India at the same period, and the Pallava dynasty much of the south.

 

According to Spink, Harisena encouraged a group of associates, including his prime minister Varahadeva and Upendragupta, the sub-king in whose territory Ajanta was, to dig out new caves, which were individually commissioned, some containing inscriptions recording the donation. This activity began in 462 but was mostly suspended in 468 because of threats from the neighbouring Asmaka kings. Work continued on only caves 1, Harisena's own commission, and 17–20, commissioned by Upendragupta. In 472 the situation was such that work was suspended completely, in a period that Spink calls "the Hiatus", which lasted until about 475, by which time the Asmakas had replaced Upendragupta as the local rulers.

 

Work was then resumed, but again disrupted by Harisena's death in 477, soon after which major excavation ceased, except at cave 26, which the Asmakas were sponsoring themselves. The Asmakas launched a revolt against Harisena's son, which brought about the end of the Vakataka Dynasty. In the years 478–480 major excavation by important patrons was replaced by a rash of "intrusions" – statues added to existing caves, and small shrines dotted about where there was space between them. These were commissioned by less powerful individuals, some monks, who had not previously been able to make additions to the large excavations of the rulers and courtiers. They were added to the facades, the return sides of the entrances, and to walls inside the caves. According to Spink, "After 480, not a single image was ever made again at the site", and as Hinduism again dominated the region, the site was again abandoned, this time for over a millennium.

 

Spink does not use "circa" in his dates, but says that "one should allow a margin of error of one year or perhaps even two in all cases".

 

IMPACT ON MODERN INDIAN PAINTINGS

The Ajanta paintings, or more likely the general style they come from, influenced painting in Tibet and Sri Lanka.

 

The rediscovery of ancient Indian paintings at Ajanta provided Indian artists examples from ancient India to follow. Nandlal Bose experimented with techniques to follow the ancient style which allowed him to develop his unique style. Abanindranath Tagore also used the Ajanta paintings for inspiration.

 

WIKIPEDIA

Kew Gardens is the world's largest collection of living plants. Founded in 1840 from the exotic garden at Kew Park in the London Borough of Richmond upon Thames, UK, its living collections include more than 30,000 different kinds of plants, while the herbarium, which is one of the largest in the world, has over seven million preserved plant specimens. The library contains more than 750,000 volumes, and the illustrations collection contains more than 175,000 prints and drawings of plants. It is one of London's top tourist attractions. In 2003, the gardens were put on the UNESCO list of World Heritage Sites.

 

Kew Gardens, together with the botanic gardens at Wakehurst Place in Sussex, are managed by the Royal Botanic Gardens, Kew (brand name Kew), an internationally important botanical research and education institution that employs 750 staff, and is a non-departmental public body sponsored by the Department for Environment, Food and Rural Affairs.

 

The Kew site, which has been dated as formally starting in 1759, though can be traced back to the exotic garden at Kew Park, formed by Lord Capel John of Tewkesbury, consists of 121 hectares (300 acres) of gardens and botanical glasshouses, four Grade I listed buildings and 36 Grade II listed structures, all set in an internationally significant landscape.

 

Kew Gardens has its own police force, Kew Constabulary, which has been in operation since 1847.

 

History

Kew, the area in which Kew Gardens are situated, consists mainly of the gardens themselves and a small surrounding community. Royal residences in the area which would later influence the layout and construction of the gardens began in 1299 when Edward I moved his court to a manor house in neighbouring Richmond (then called Sheen). That manor house was later abandoned; however, Henry V built Sheen Palace in 1501, which, under the name Richmond Palace, became a permanent royal residence for Henry VII. Around the start of the 16th century courtiers attending Richmond Palace settled in Kew and built large houses. Early royal residences at Kew included Mary Tudor's house, which was in existence by 1522 when a driveway was built to connect it to the palace at Richmond. Around 1600, the land that would become the gardens was known as Kew Field, a large field strip farmed by one of the new private estates.

 

The exotic garden at Kew Park, formed by Lord Capel John of Tewkesbury, was enlarged and extended by Augusta, Dowager Princess of Wales, the widow of Frederick, Prince of Wales. The origins of Kew Gardens can be traced to the merging of the royal estates of Richmond and Kew in 1772. William Chambers built several garden structures, including the lofty Chinese pagoda built in 1761 which still remains. George III enriched the gardens, aided by William Aiton and Sir Joseph Banks. The old Kew Park (by then renamed the White House), was demolished in 1802. The "Dutch House" adjoining was purchased by George III in 1781 as a nursery for the royal children. It is a plain brick structure now known as Kew Palace.

 

Some early plants came from the walled garden established by William Coys at Stubbers in North Ockendon. The collections grew somewhat haphazardly until the appointment of the first collector, Francis Masson, in 1771. Capability Brown, who became England's most renowned landscape architect, applied for the position of master gardener at Kew, and was rejected.

 

In 1840 the gardens were adopted as a national botanical garden, in large part due to the efforts of the Royal Horticultural Society and its president William Cavendish. Under Kew's director, William Hooker, the gardens were increased to 30 hectares (75 acres) and the pleasure grounds, or arboretum, extended to 109 hectares (270 acres), and later to its present size of 121 hectares (300 acres). The first curator was John Smith.

 

The Palm House was built by architect Decimus Burton and iron-maker Richard Turner between 1844 and 1848, and was the first large-scale structural use of wrought iron. It is considered " the world's most important surviving Victorian glass and iron structure." The structure's panes of glass are all hand-blown. The Temperate House, which is twice as large as the Palm House, followed later in the 19th century. It is now the largest Victorian glasshouse in existence. Kew was the location of the successful effort in the 19th century to propagate rubber trees for cultivation outside South America.

 

In February 1913, the Tea House was burned down by suffragettes Olive Wharry and Lilian Lenton during a series of arson attacks in London.[19] Kew Gardens lost hundreds of trees in the Great Storm of 1987. From 1959 to 2007 Kew Gardens had the tallest flagpole in Britain. Made from a single Douglas-fir from Canada, it was given to mark both the centenary of the Canadian Province of British Columbia and the bicentenary of Kew Gardens. The flagpole was removed after damage by weather and woodpeckers.

 

In July 2003, the gardens were put on the list of World Heritage Sites by UNESCO.

 

Features

Treetop walkway

A new treetop walkway opened in 2008. This walkway is 18 metres (59 ft) high and 200 metres (660 ft) long and takes visitors into the tree canopy of a woodland glade. Visitors can ascend and descend by stairs or by a lift. The floor of the walkway is made from perforated metal and flexes as it is walked upon. The entire structure sways in the wind.

  

Sackler Crossing

The Sackler Crossing bridge, made of granite and bronze, opened in May 2006. Designed by Buro Happold and John Pawson, it crosses the lake and is named in honour of philanthropists Dr Mortimer and Theresa Sackler.

 

The minimalist-styled bridge is designed as a sweeping double curve of black granite. The sides of the bridge are formed of bronze posts that give the impression, from certain angles, of forming a solid wall whereas from others, and to those on the bridge, they are clearly individual entities that allow a view of the water beyond.

 

The bridge forms part of a path designed to encourage visitors to visit more of the gardens than had hitherto been popular and connects the two art galleries, via the Temperate and Evolution Houses and the woodland glade, to the Minka House and the Bamboo Garden.

 

The crossing won a special award from the Royal Institute of British Architects in 2008.

 

Vehicular tour

Kew Explorer is a service that takes a circular route around the gardens, provided by two 72-seater road trains that are fuelled by Calor Gas to minimise pollution. A commentary is provided by the driver and there are several stops.

   

Compost heap

Kew has one of the largest compost heaps in Europe, made from green and woody waste from the gardens and the manure from the stables of the Household Cavalry. The compost is mainly used in the gardens, but on occasion has been auctioned as part of a fundraising event for the gardens.

 

The compost heap is in an area of the gardens not accessible to the public, but a viewing platform, made of wood which had been illegally traded but seized by Customs officers in HMRC, has been erected to allow visitors to observe the heap as it goes through its cycle.

 

Guided walks

Free tours of the gardens are conducted daily by trained volunteers.

 

Plant houses

 

Alpine House

A narrow semicircular building of glass and steel latticework stands at the right, set amid an area of worked rock with a line of deciduous trees in the rear left, under a blue sky filled with large puffy white clouds. In front of it, curving slightly away to the left, is a wooden platform with benches on it and a thin metal guardrail in front of a low wet area with bright red flowers

 

In March 2006, the Davies Alpine House opened, the third version of an alpine house since 1887. Although only 16 metres (52 ft) long the apex of the roof arch extends to a height of 10 metres (33 ft) in order to allow the natural airflow of a building of this shape to aid in the all-important ventilation required for the type of plants to be housed.

 

The new house features a set of automatically operated blinds that prevent it overheating when the sun is too hot for the plants together with a system that blows a continuous stream of cool air over the plants. The main design aim of the house is to allow maximum light transmission. To this end the glass is of a special low iron type that allows 90 per cent of the ultraviolet light in sunlight to pass. It is attached by high tension steel cables so that no light is obstructed by traditional glazing bars.

 

To conserve energy the cooling air is not refrigerated but is cooled by being passed through a labyrinth of pipes buried under the house at a depth where the temperature remains suitable all year round. The house is designed so that the maximum temperature should not exceed 20 °C (68 °F).

 

Kew's collection of Alpine plants (defined as those that grow above the tree-line in their locale – ground level at the poles rising to over 2,000 metres (6,562 feet)), extends to over 7000. As the Alpine House can only house around 200 at a time the ones on show are regularly rotated.

  

The Nash Conservatory

Originally designed for Buckingham Palace, this was moved to Kew in 1836 by King William IV. With an abundance of natural light, the building is used various exhibitions, weddings, and private events. It is also now used to exhibit the winners of the photography competition.

  

Kew Orangery

The Orangery was designed by Sir William Chambers, and was completed in 1761. It measures 28 by 10 metres (92 by 33 ft). It was found to be too dark for its intended purpose of growing citrus plants and they were moved out in 1841. After many changes of use, it is currently used as a restaurant.

  

The Palm House and Parterre

The Palm House (1844–1848) was the result of cooperation between architect Decimus Burton and iron founder Richard Turner,[28] and continues upon the glass house design principles developed by John Claudius Loudon[29][30] and Joseph Paxton. A space frame of wrought iron arches, held together by horizontal tubular structures containing long prestressed cables,[30][31] supports glass panes which were originally[28] tinted green with copper oxide to reduce the significant heating effect. The 19m high central nave is surrounded by a walkway at 9m height, allowing visitors a closer look upon the palm tree crowns. In front of the Palm House on the east side are the Queen's Beasts, ten statues of animals bearing shields. They are Portland stone replicas of originals done by James Woodford and were placed here in 1958.[32]

  

Princess of Wales Conservatory

Kew's third major conservatory, the Princess of Wales Conservatory, designed by architect Gordon Wilson, was opened in 1987 by Diana, Princess of Wales in commemoration of her predecessor Augusta's associations with Kew. In 1989 the conservatory received the Europa Nostra award for conservation.[34] The conservatory houses ten computer-controlled micro-climatic zones, with the bulk of the greenhouse volume composed of Dry Tropics and Wet Tropics plants. Significant numbers of orchids, water lilies, cacti, lithops, carnivorous plants and bromeliads are housed in the various zones. The cactus collection also extends outside the conservatory where some hardier species can be found.

 

The conservatory has an area of 4499 square metres. As it is designed to minimise the amount of energy taken to run it, the cooler zones are grouped around the outside and the more tropical zones are in the central area where heat is conserved. The glass roof extends down to the ground, giving the conservatory a distinctive appearance and helping to maximise the use of the sun's energy.

 

During the construction of the conservatory a time capsule was buried. It contains the seeds of basic crops and endangered plant species and key publications on conservation.

 

Rhizotron

 

The Rhizotron

A rhizotron opened at the same time as the "treetop walkway", giving visitors the opportunity to investigate what happens beneath the ground where trees grow. The rhizotron is essentially a single gallery containing a set of large bronze abstract castings which contain LCD screens that carry repeating loops of information about the life of trees.

 

Temperate House

 

Inside the Temperate House

The Temperate House, currently closed for restoration, is a greenhouse that has twice the floor area of the Palm House and is the world's largest surviving Victorian glass structure. When in use it contained plants and trees from all the temperate regions of the world. It was commissioned in 1859 and designed by architect Decimus Burton and ironfounder Richard Turner. Covering 4880 square metres, it rises to a height of 19 metres. Intended to accommodate Kew's expanding collection of hardy and temperate plants, it took 40 years to construct, during which time costs soared. The building was restored during 2014 - 15 by Donald Insall Associates, based on their conservation management plan.

 

There is a viewing gallery in the central section from which visitors were able to look down on that part of the collection.

 

Waterlily House

The Waterlily House is the hottest and most humid of the houses at Kew and contains a large pond with varieties of water lily, surrounded by a display of economically important heat-loving plants. It closes during the winter months.

 

It was built to house the Victoria amazonica, the largest of the Nymphaeaceae family of water lilies. This plant was originally transported to Kew in phials of clean water and arrived in February 1849, after several prior attempts to transport seeds and roots had failed. Although various other members of the Nymphaeaceae family grew well, the house did not suit the Victoria, purportedly because of a poor ventilation system, and this specimen was moved to another, smaller, house.

 

The ironwork for this project was provided by Richard Turner and the initial construction was completed in 1852. The heat for the house was initially obtained by running a flue from the nearby Palm House but it was later equipped with its own boiler.

 

Ornamental buildings

 

The Pagoda

In the south-east corner of Kew Gardens stands the Great Pagoda (by Sir William Chambers), erected in 1762, from a design in imitation of the Chinese Ta. The lowest of the ten octagonal storeys is 15 m (49 ft) in diameter. From the base to the highest point is 50 m (164 ft).

 

Each storey finishes with a projecting roof, after the Chinese manner, originally covered with ceramic tiles and adorned with large dragons; a story is still propagated that they were made of gold and were reputedly sold by George IV to settle his debts. In fact the dragons were made of wood painted gold, and simply rotted away with the ravages of time. The walls of the building are composed of brick. The staircase, 253 steps, is in the centre of the building. The Pagoda was closed to the public for many years, but was reopened for the summer months of 2006 and is now open permanently. During the Second World War holes were cut in each floor to allow for drop-testing of model bombs.

  

The Japanese Gateway (Chokushi-Mon)

Built for the Japan-British Exhibition (1910) and moved to Kew in 1911, the Chokushi-Mon ("Imperial Envoy's Gateway") is a four-fifths scale replica of the karamon (gateway) of the Nishi Hongan-ji temple in Kyoto. It lies about 140 m west of the Pagoda and is surrounded by a reconstruction of a traditional Japanese garden.

  

The Minka House

Following the Japan 2001 festival, Kew acquired a Japanese wooden house called a minka. It was originally erected in around 1900 in a suburb of Okazaki. Japanese craftsmen reassembled the framework and British builders who had worked on the Globe Theatre added the mud wall panels.

 

Work on the house started on 7 May 2001 and, when the framework was completed on 21 May, a Japanese ceremony was held to mark what was considered an auspicious occasion. Work on the building of the house was completed in November 2001 but the internal artefacts were not all in place until 2006.

 

The Minka house is located within the bamboo collection in the west central part of the gardens.

  

Queen Charlotte's Cottage

Within the conservation area is a cottage that was given to Queen Charlotte as a wedding present on her marriage to George III. It has been restored by Historic Royal Palaces and is separately administered by them.

It is open to the public on weekends and bank holidays during the summer.

 

Kew Palace

Kew Palace is the smallest of the British royal palaces. It was built by Samuel Fortrey, a Dutch merchant in around 1631. It was later purchased by George III. The construction method is known as Flemish bond and involves laying the bricks with long and short sides alternating. This and the gabled front give the construction a Dutch appearance.

To the rear of the building is the "Queen's Garden" which includes a collection of plants believed to have medicinal qualities. Only plants that were extant in England by the 17th century are grown in the garden.

The building underwent significant restoration, with leading conservation architects Donald Insall Associates, before being reopened to the public in 2006.

It is administered separately from Kew Gardens, by Historic Royal Palaces.

In front of the palace is a sundial, which was given to Kew Gardens in 1959 to commemorate a royal visit. It was sculpted by Martin Holden and is based on an earlier sculpture by Thomas Tompion, a celebrated 17th century clockmaker.

 

Galleries and Museums

 

The Shirley Sherwood Gallery of Botanic Art

The Shirley Sherwood Gallery of Botanic Art opened in April 2008, and holds paintings from Kew's and Dr Shirley Sherwood's collections, many of which had never been displayed to the public before. It features paintings by artists such as Georg D. Ehret, the Bauer brothers, Pierre-Joseph Redouté and Walter Hood Fitch. The paintings and drawings are cycled on a six-monthly basis. The gallery is linked to the Marianne North Gallery (see above).

 

Near the Palm House is a building known as "Museum No. 1" (even though it is the only museum on the site), which was designed by Decimus Burton and opened in 1857. Housing Kew's economic botany collections including tools, ornaments, clothing, food and medicines, its aim was to illustrate human dependence on plants. The building was refurbished in 1998. The upper two floors are now an education centre and the ground floor houses the "Plants+People" exhibition which highlights the variety of plants and the ways that people use them.

 

Admission to the galleries and museum is free after paying admission to the gardens. The International Garden Photographer of the Year Exhibition is an annual event with an indoor display of entries during the summer months.

 

The Marianne North Gallery of Botanic Art

The Marianne North Gallery was built in the 1880s to house the paintings of Marianne North, an MP's daughter who travelled alone to North and South America, South Africa and many parts of Asia, at a time when women rarely did so, to paint plants. The gallery has 832 of her paintings. The paintings were left to Kew by the artist and a condition of the bequest is that the layout of the paintings in the gallery may not be altered.

 

The gallery had suffered considerable structural degradation since its creation and during a period from 2008 to 2009 major restoration and refurbishment took place, with works lead by with leading conservation architects Donald Insall Associates. During the time the gallery was closed the opportunity was also taken to restore the paintings to their original condition. The gallery reopened in October 2009.

 

The gallery originally opened in 1882 and is the only permanent exhibition in Great Britain dedicated to the work of one woman.

 

Plant collections

 

The plant collections include the Aquatic Garden, which is near the Jodrell laboratory. The Aquatic Garden, which celebrated its centenary in 2009, provides conditions for aquatic and marginal plants. The large central pool holds a selection of summer-flowering water lilies and the corner pools contain plants such as reed mace, bulrushes, phragmites and smaller floating aquatic species.

 

The Arboretum, which covers over half of the total area of the site, contains over 14,000 trees of many thousands of varieties. The Bonsai Collection is housed in a dedicated greenhouse near the Jodrell laboratory. The Cacti Collection is housed in and around the Princess of Wales Conservatory. The Carnivorous Plant collection is housed in the Princess of Wales Conservatory. The Grass Garden was created on its current site in the early 1980s to display ornamental and economic grasses; it was redesigned and replanted between 1994 and 1997. It is currently undergoing a further redesign and planting. Over 580 species of grasses are displayed.

 

The Herbaceous Grounds (Order Beds) were devised in the late 1860s by Sir Joseph Hooker, then director of the Royal Botanic Gardens, so that botany students could learn to recognise plants and experience at first hand the diversity of the plant kingdom. The collection is organised into family groups. Its name arose because plant families were known as natural orders in the 19th century. Over the main path is a rose pergola built in 1959 to mark the bicentennial of the Gardens. It supports climber and rambling roses selected for the length and profusion of flowering.

 

The Orchid Collection is housed in two climate zones within the Princess of Wales Conservatory. To maintain an interesting display the plants are changed regularly so that those on view are generally flowering. The Rock Garden, originally built of limestone in 1882, is now constructed of Sussex sandstone from West Hoathly, Sussex. The rock garden is divided into six geographic regions: Europe, Mediterranean and Africa, Australia and New Zealand, Asia, North America, and South America. There are currently 2,480 different "accessions" growing in the garden.

 

The Rose Garden, based upon original designs by William Nesfield, is behind the Palm House, and was replanted between 2009 and 2010 using the original design from 1848. It is intended as an ornamental display rather than a collection of a particularly large number of varieties. Other collections and specialist areas include the rhododendron dell, the azalea garden, the bamboo garden, the juniper collection, the berberis dell, the lilac garden, the magnolia collection, and the fern collection.

  

The Palm House and lake to Victoria Gate

The world's smallest water-lily, Nymphaea thermarum, was saved from extinction when it was grown from seed at Kew, in 2009.

 

Herbarium

The Kew herbarium is one of the largest in the world with approximately 7 million specimens used primarily for taxonomic study. The herbarium is rich in types for all regions of the world, especially the tropics.

 

Library and archives

The library and archives at Kew are one of the world's largest botanical collections, with over half a million items, including books, botanical illustrations, photographs, letters and manuscripts, periodicals, and maps. The Jodrell Library has been merged with the Economic Botany and Mycology Libraries and all are now housed in the Jodrell Laboratory.

 

Forensic horticulture

Kew provides advice and guidance to police forces around the world where plant material may provide important clues or evidence in cases. In one famous case the forensic science department at Kew were able to ascertain that the contents of the stomach of a headless corpse found in the river Thames contained a highly toxic African bean.

 

Economic Botany

 

The Sustainable Uses of Plants group (formerly the Centre for Economic Botany), focus on the uses of plants in the United Kingdom and the world's arid and semi-arid zones. The Centre is also responsible for curation of the Economic Botany Collection, which contains more than 90,000 botanical raw materials and ethnographic artefacts, some of which are on display in the Plants + People exhibit in Museum No. 1. The Centre is now located in the Jodrell Laboratory.

 

Jodrell Laboratory

The original Jodrell laboratory, named after Mr T. J. Phillips Jodrell who funded it, was established in 1877 and consisted of four research rooms and an office. Originally research was conducted into plant physiology but this was gradually superseded by botanical research. In 1934 an artists' studio and photographic darkroom were added, highlighting the importance of botanical illustration. In 1965, following increasing overcrowding, a new building was constructed and research expanded into seed collection for plant conservation. The biochemistry section also expanded to facilitate research into secondary compounds that could be derived from plants for medicinal purposes. In 1994 the centre was expanded again, tripling in size, and a decade later it was further expanded by the addition of the Wolfson Wing.

 

Kew Constabulary

Main article: Kew Constabulary

The gardens have their own police force, Kew Constabulary, which has been in operation since 1847. Formerly known as the Royal Botanic Gardens Constabulary, it is a small, specialised constabulary of two sergeants and 12 officers, who patrol the grounds in a green painted electric buggy. The Kew Constables are attested under section 3 of the Parks Regulation Act 1872, which gives them the same powers as the Metropolitan Police within the land belonging to the gardens.

 

Media

A number of films, documentaries and short videos have been made about Kew Gardens.

 

They include:

 

a short colour film World Garden by cinematographer Geoffrey Unsworth in 1942

three series of A Year at Kew (2007), filmed for BBC television and released on DVD

Cruickshank on Kew: The Garden That Changed the World, a 2009 BBC documentary, presented by Dan Cruickshank, exploring the history of the relationship between Kew Gardens and the British Empire

David Attenborough's 2012 Kingdom of Plants 3D

a 2003 episode of the Channel 4 TV series Time Team, presented by Tony Robinson, that searched for the remains of George III's palace

a 2004 episode of the BBC Four series Art of the Garden which looked at the building of the Great Palm House in the 1840s.

"Kew on a Plate", a TV programme showing the kinds of produce grown at Kew Gardens and how they can be prepared in a kitchen.

In 1921 Virginia Woolf published her short story "Kew Gardens", which gives brief descriptions of four groups of people as they pass by a flowerbed.

 

Access and transport

 

Elizabeth Gate

Kew Gardens is accessible by a number of gates. Currently, there are four gates into Kew Gardens that are open to the public: the Elizabeth Gate, which is situated at the west end of Kew Green, and was originally called the Main Gate before being renamed in 2012 to commemorate the Diamond Jubilee of Elizabeth II; the Brentford Gate, which faces the River Thames; the Victoria Gate (named after Queen Victoria), situated in Kew Road, which is also the location of the Visitors' Centre; and the Lion Gate, also situated in Kew Road.

 

Other gates that are not open to the public include Unicorn Gate, Cumberland Gate and Jodrell Gate (all in Kew Road) and Isleworth Gate (facing the Thames).

  

Victoria Gate

Kew Gardens station, a London Underground and National Rail station opened in 1869 and served by both the District line and the London Overground services on the North London Line, is the nearest train station to the gardens – only 400 metres (1,300 ft) along Lichfield Road from the Victoria Gate entrance. Built by the London and South Western Railway, the Historic England listed building is one of the few remaining original 19th-century stations on the North London Line, and the only station on the London Underground with a pub on the platform (though the platform entrance is now closed off). Kew Bridge station, on the other side of the Thames, 800 metres from the Elizabeth Gate entrance via Kew Bridge, is served by South West Trains from Clapham Junction and Waterloo.

 

London Buses route 65, between Ealing Broadway and Kingston, stops near the Lion Gate and Victoria Gate entrances; route 391, between Fulham and Richmond, stops near Kew Gardens station; while routes 237 and 267 stop at Kew Bridge station.

 

London River Services operate from Westminster during the summer, stopping at Kew Pier, 500 metres (1,600 ft) from Elizabeth Gate. Cycle racks are located just inside the Victoria Gate, Elizabeth Gate and Brentford Gate entrances. There is a 300-space car park outside Brentford Gate, reached via Ferry Lane, as well as some free, though restricted, on-street parking on Kew Road.

 

en.wikipedia.org/wiki/Kew_Gardens

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A high pollution day in Shanghai meant views from the Japanese restaurant at the top of one of the high towers were very limited. Such smogs are very common, mostly due to coal burning factories and power plants in the surrounding area. When the index is high - outdoor exercise is discouraged. Today's index was 180, anything over 75 is unhealthy. aqicn.org/city/shanghai

Oxon Cove Park and Oxon Cove Farm is a national historic district that includes a living farm museum operated by the National Park Service, and located at Oxon Hill, Prince George's County, Maryland. It was listed on the National Register of Historic Places in 2003.

 

The park provides an excellent resource for environmental studies, wildlife observing, fishing, and other recreational activities made possible by easy access to the Potomac River. Fourteen buildings and two structures are located in the historic district and associated with the property's sequential development as a plantation, an institutional agricultural complex, and a farm museum.

 

The Oxon Hill Farm includes the Mount Welby home, Farm Museum, barns, a stable, feed building, livestock buildings and a visitor activity barn. Farm animals include cows, horses and chickens. Visitors can view the animals up close daily and learn about the workings of a farm. The Farm Museum building displays historical farm equipment dating from the late 19th century.

 

The district also includes a hexagonal frame outbuilding; ca. 1830 brick root cellar; ca. 1973 frame hog house; ca. 1890 frame horse and pony barn; ca. 1991 frame chicken house; ca. 1970 steel-frame implement shed; ca. 1980 frame visitor barn; ca. 1970 steel-frame windmill; ca. 1940 frame hay barn; ca. 1890 frame feed building; ca. 1830 brick stable; ca. 1970 frame tool shed; ca. 1980 frame "sorghum sirip" shed; and a ca. 1980 frame dairy barn, and ca. 1940 tile silo. From the 1890s to 1950s, under the ownership of St. Elizabeth's Hospital, the site was used as a therapeutic treatment center for the mentally ill known as Godding Croft. The Oxon Cove Farm historic district is located on the crest of a ridge overlooking the Potomac River, north of I-95.

 

The principal dwelling, known as "Mount Welby," is a ca. 1807-1811 two-story three-bay brick structure laid in Flemish bond with Italianate detailing and sheltered by a shed roof, and visible to motorists crossing the interstate Woodrow Wilson Bridge. The house was built by Irish immigrant Dr. Samuel DeButts. It was entrusted to the National Park Service in 1959 in order to protect its resources from increased development. From 1891 to 1950, the property was used as a therapeutic farm by St. Elizabeths Hospital, and was known as Godding Croft.

 

The house is operated as a historic house museum, with exhibits about period life in the early 19th century for the owners and slaves on the plantation. Other exhibits focus on the home's role at Godding Croft.

 

en.wikipedia.org/wiki/Oxon_Cove_Park_and_Oxon_Hill_Farm

 

en.wikipedia.org/wiki/Wikipedia:Text_of_Creative_Commons_...

Kew Gardens is the world's largest collection of living plants. Founded in 1840 from the exotic garden at Kew Park in the London Borough of Richmond upon Thames, UK, its living collections include more than 30,000 different kinds of plants, while the herbarium, which is one of the largest in the world, has over seven million preserved plant specimens. The library contains more than 750,000 volumes, and the illustrations collection contains more than 175,000 prints and drawings of plants. It is one of London's top tourist attractions. In 2003, the gardens were put on the UNESCO list of World Heritage Sites.

 

Kew Gardens, together with the botanic gardens at Wakehurst Place in Sussex, are managed by the Royal Botanic Gardens, Kew (brand name Kew), an internationally important botanical research and education institution that employs 750 staff, and is a non-departmental public body sponsored by the Department for Environment, Food and Rural Affairs.

 

The Kew site, which has been dated as formally starting in 1759, though can be traced back to the exotic garden at Kew Park, formed by Lord Capel John of Tewkesbury, consists of 121 hectares (300 acres) of gardens and botanical glasshouses, four Grade I listed buildings and 36 Grade II listed structures, all set in an internationally significant landscape.

 

Kew Gardens has its own police force, Kew Constabulary, which has been in operation since 1847.

 

History

Kew, the area in which Kew Gardens are situated, consists mainly of the gardens themselves and a small surrounding community. Royal residences in the area which would later influence the layout and construction of the gardens began in 1299 when Edward I moved his court to a manor house in neighbouring Richmond (then called Sheen). That manor house was later abandoned; however, Henry V built Sheen Palace in 1501, which, under the name Richmond Palace, became a permanent royal residence for Henry VII. Around the start of the 16th century courtiers attending Richmond Palace settled in Kew and built large houses. Early royal residences at Kew included Mary Tudor's house, which was in existence by 1522 when a driveway was built to connect it to the palace at Richmond. Around 1600, the land that would become the gardens was known as Kew Field, a large field strip farmed by one of the new private estates.

 

The exotic garden at Kew Park, formed by Lord Capel John of Tewkesbury, was enlarged and extended by Augusta, Dowager Princess of Wales, the widow of Frederick, Prince of Wales. The origins of Kew Gardens can be traced to the merging of the royal estates of Richmond and Kew in 1772. William Chambers built several garden structures, including the lofty Chinese pagoda built in 1761 which still remains. George III enriched the gardens, aided by William Aiton and Sir Joseph Banks. The old Kew Park (by then renamed the White House), was demolished in 1802. The "Dutch House" adjoining was purchased by George III in 1781 as a nursery for the royal children. It is a plain brick structure now known as Kew Palace.

 

Some early plants came from the walled garden established by William Coys at Stubbers in North Ockendon. The collections grew somewhat haphazardly until the appointment of the first collector, Francis Masson, in 1771. Capability Brown, who became England's most renowned landscape architect, applied for the position of master gardener at Kew, and was rejected.

 

In 1840 the gardens were adopted as a national botanical garden, in large part due to the efforts of the Royal Horticultural Society and its president William Cavendish. Under Kew's director, William Hooker, the gardens were increased to 30 hectares (75 acres) and the pleasure grounds, or arboretum, extended to 109 hectares (270 acres), and later to its present size of 121 hectares (300 acres). The first curator was John Smith.

 

The Palm House was built by architect Decimus Burton and iron-maker Richard Turner between 1844 and 1848, and was the first large-scale structural use of wrought iron. It is considered " the world's most important surviving Victorian glass and iron structure." The structure's panes of glass are all hand-blown. The Temperate House, which is twice as large as the Palm House, followed later in the 19th century. It is now the largest Victorian glasshouse in existence. Kew was the location of the successful effort in the 19th century to propagate rubber trees for cultivation outside South America.

 

In February 1913, the Tea House was burned down by suffragettes Olive Wharry and Lilian Lenton during a series of arson attacks in London.[19] Kew Gardens lost hundreds of trees in the Great Storm of 1987. From 1959 to 2007 Kew Gardens had the tallest flagpole in Britain. Made from a single Douglas-fir from Canada, it was given to mark both the centenary of the Canadian Province of British Columbia and the bicentenary of Kew Gardens. The flagpole was removed after damage by weather and woodpeckers.

 

In July 2003, the gardens were put on the list of World Heritage Sites by UNESCO.

 

Features

Treetop walkway

A new treetop walkway opened in 2008. This walkway is 18 metres (59 ft) high and 200 metres (660 ft) long and takes visitors into the tree canopy of a woodland glade. Visitors can ascend and descend by stairs or by a lift. The floor of the walkway is made from perforated metal and flexes as it is walked upon. The entire structure sways in the wind.

  

Sackler Crossing

The Sackler Crossing bridge, made of granite and bronze, opened in May 2006. Designed by Buro Happold and John Pawson, it crosses the lake and is named in honour of philanthropists Dr Mortimer and Theresa Sackler.

 

The minimalist-styled bridge is designed as a sweeping double curve of black granite. The sides of the bridge are formed of bronze posts that give the impression, from certain angles, of forming a solid wall whereas from others, and to those on the bridge, they are clearly individual entities that allow a view of the water beyond.

 

The bridge forms part of a path designed to encourage visitors to visit more of the gardens than had hitherto been popular and connects the two art galleries, via the Temperate and Evolution Houses and the woodland glade, to the Minka House and the Bamboo Garden.

 

The crossing won a special award from the Royal Institute of British Architects in 2008.

 

Vehicular tour

Kew Explorer is a service that takes a circular route around the gardens, provided by two 72-seater road trains that are fuelled by Calor Gas to minimise pollution. A commentary is provided by the driver and there are several stops.

   

Compost heap

Kew has one of the largest compost heaps in Europe, made from green and woody waste from the gardens and the manure from the stables of the Household Cavalry. The compost is mainly used in the gardens, but on occasion has been auctioned as part of a fundraising event for the gardens.

 

The compost heap is in an area of the gardens not accessible to the public, but a viewing platform, made of wood which had been illegally traded but seized by Customs officers in HMRC, has been erected to allow visitors to observe the heap as it goes through its cycle.

 

Guided walks

Free tours of the gardens are conducted daily by trained volunteers.

 

Plant houses

 

Alpine House

A narrow semicircular building of glass and steel latticework stands at the right, set amid an area of worked rock with a line of deciduous trees in the rear left, under a blue sky filled with large puffy white clouds. In front of it, curving slightly away to the left, is a wooden platform with benches on it and a thin metal guardrail in front of a low wet area with bright red flowers

 

In March 2006, the Davies Alpine House opened, the third version of an alpine house since 1887. Although only 16 metres (52 ft) long the apex of the roof arch extends to a height of 10 metres (33 ft) in order to allow the natural airflow of a building of this shape to aid in the all-important ventilation required for the type of plants to be housed.

 

The new house features a set of automatically operated blinds that prevent it overheating when the sun is too hot for the plants together with a system that blows a continuous stream of cool air over the plants. The main design aim of the house is to allow maximum light transmission. To this end the glass is of a special low iron type that allows 90 per cent of the ultraviolet light in sunlight to pass. It is attached by high tension steel cables so that no light is obstructed by traditional glazing bars.

 

To conserve energy the cooling air is not refrigerated but is cooled by being passed through a labyrinth of pipes buried under the house at a depth where the temperature remains suitable all year round. The house is designed so that the maximum temperature should not exceed 20 °C (68 °F).

 

Kew's collection of Alpine plants (defined as those that grow above the tree-line in their locale – ground level at the poles rising to over 2,000 metres (6,562 feet)), extends to over 7000. As the Alpine House can only house around 200 at a time the ones on show are regularly rotated.

  

The Nash Conservatory

Originally designed for Buckingham Palace, this was moved to Kew in 1836 by King William IV. With an abundance of natural light, the building is used various exhibitions, weddings, and private events. It is also now used to exhibit the winners of the photography competition.

  

Kew Orangery

The Orangery was designed by Sir William Chambers, and was completed in 1761. It measures 28 by 10 metres (92 by 33 ft). It was found to be too dark for its intended purpose of growing citrus plants and they were moved out in 1841. After many changes of use, it is currently used as a restaurant.

  

The Palm House and Parterre

The Palm House (1844–1848) was the result of cooperation between architect Decimus Burton and iron founder Richard Turner,[28] and continues upon the glass house design principles developed by John Claudius Loudon[29][30] and Joseph Paxton. A space frame of wrought iron arches, held together by horizontal tubular structures containing long prestressed cables,[30][31] supports glass panes which were originally[28] tinted green with copper oxide to reduce the significant heating effect. The 19m high central nave is surrounded by a walkway at 9m height, allowing visitors a closer look upon the palm tree crowns. In front of the Palm House on the east side are the Queen's Beasts, ten statues of animals bearing shields. They are Portland stone replicas of originals done by James Woodford and were placed here in 1958.[32]

  

Princess of Wales Conservatory

Kew's third major conservatory, the Princess of Wales Conservatory, designed by architect Gordon Wilson, was opened in 1987 by Diana, Princess of Wales in commemoration of her predecessor Augusta's associations with Kew. In 1989 the conservatory received the Europa Nostra award for conservation.[34] The conservatory houses ten computer-controlled micro-climatic zones, with the bulk of the greenhouse volume composed of Dry Tropics and Wet Tropics plants. Significant numbers of orchids, water lilies, cacti, lithops, carnivorous plants and bromeliads are housed in the various zones. The cactus collection also extends outside the conservatory where some hardier species can be found.

 

The conservatory has an area of 4499 square metres. As it is designed to minimise the amount of energy taken to run it, the cooler zones are grouped around the outside and the more tropical zones are in the central area where heat is conserved. The glass roof extends down to the ground, giving the conservatory a distinctive appearance and helping to maximise the use of the sun's energy.

 

During the construction of the conservatory a time capsule was buried. It contains the seeds of basic crops and endangered plant species and key publications on conservation.

 

Rhizotron

 

The Rhizotron

A rhizotron opened at the same time as the "treetop walkway", giving visitors the opportunity to investigate what happens beneath the ground where trees grow. The rhizotron is essentially a single gallery containing a set of large bronze abstract castings which contain LCD screens that carry repeating loops of information about the life of trees.

 

Temperate House

 

Inside the Temperate House

The Temperate House, currently closed for restoration, is a greenhouse that has twice the floor area of the Palm House and is the world's largest surviving Victorian glass structure. When in use it contained plants and trees from all the temperate regions of the world. It was commissioned in 1859 and designed by architect Decimus Burton and ironfounder Richard Turner. Covering 4880 square metres, it rises to a height of 19 metres. Intended to accommodate Kew's expanding collection of hardy and temperate plants, it took 40 years to construct, during which time costs soared. The building was restored during 2014 - 15 by Donald Insall Associates, based on their conservation management plan.

 

There is a viewing gallery in the central section from which visitors were able to look down on that part of the collection.

 

Waterlily House

The Waterlily House is the hottest and most humid of the houses at Kew and contains a large pond with varieties of water lily, surrounded by a display of economically important heat-loving plants. It closes during the winter months.

 

It was built to house the Victoria amazonica, the largest of the Nymphaeaceae family of water lilies. This plant was originally transported to Kew in phials of clean water and arrived in February 1849, after several prior attempts to transport seeds and roots had failed. Although various other members of the Nymphaeaceae family grew well, the house did not suit the Victoria, purportedly because of a poor ventilation system, and this specimen was moved to another, smaller, house.

 

The ironwork for this project was provided by Richard Turner and the initial construction was completed in 1852. The heat for the house was initially obtained by running a flue from the nearby Palm House but it was later equipped with its own boiler.

 

Ornamental buildings

 

The Pagoda

In the south-east corner of Kew Gardens stands the Great Pagoda (by Sir William Chambers), erected in 1762, from a design in imitation of the Chinese Ta. The lowest of the ten octagonal storeys is 15 m (49 ft) in diameter. From the base to the highest point is 50 m (164 ft).

 

Each storey finishes with a projecting roof, after the Chinese manner, originally covered with ceramic tiles and adorned with large dragons; a story is still propagated that they were made of gold and were reputedly sold by George IV to settle his debts. In fact the dragons were made of wood painted gold, and simply rotted away with the ravages of time. The walls of the building are composed of brick. The staircase, 253 steps, is in the centre of the building. The Pagoda was closed to the public for many years, but was reopened for the summer months of 2006 and is now open permanently. During the Second World War holes were cut in each floor to allow for drop-testing of model bombs.

  

The Japanese Gateway (Chokushi-Mon)

Built for the Japan-British Exhibition (1910) and moved to Kew in 1911, the Chokushi-Mon ("Imperial Envoy's Gateway") is a four-fifths scale replica of the karamon (gateway) of the Nishi Hongan-ji temple in Kyoto. It lies about 140 m west of the Pagoda and is surrounded by a reconstruction of a traditional Japanese garden.

  

The Minka House

Following the Japan 2001 festival, Kew acquired a Japanese wooden house called a minka. It was originally erected in around 1900 in a suburb of Okazaki. Japanese craftsmen reassembled the framework and British builders who had worked on the Globe Theatre added the mud wall panels.

 

Work on the house started on 7 May 2001 and, when the framework was completed on 21 May, a Japanese ceremony was held to mark what was considered an auspicious occasion. Work on the building of the house was completed in November 2001 but the internal artefacts were not all in place until 2006.

 

The Minka house is located within the bamboo collection in the west central part of the gardens.

  

Queen Charlotte's Cottage

Within the conservation area is a cottage that was given to Queen Charlotte as a wedding present on her marriage to George III. It has been restored by Historic Royal Palaces and is separately administered by them.

It is open to the public on weekends and bank holidays during the summer.

 

Kew Palace

Kew Palace is the smallest of the British royal palaces. It was built by Samuel Fortrey, a Dutch merchant in around 1631. It was later purchased by George III. The construction method is known as Flemish bond and involves laying the bricks with long and short sides alternating. This and the gabled front give the construction a Dutch appearance.

To the rear of the building is the "Queen's Garden" which includes a collection of plants believed to have medicinal qualities. Only plants that were extant in England by the 17th century are grown in the garden.

The building underwent significant restoration, with leading conservation architects Donald Insall Associates, before being reopened to the public in 2006.

It is administered separately from Kew Gardens, by Historic Royal Palaces.

In front of the palace is a sundial, which was given to Kew Gardens in 1959 to commemorate a royal visit. It was sculpted by Martin Holden and is based on an earlier sculpture by Thomas Tompion, a celebrated 17th century clockmaker.

 

Galleries and Museums

 

The Shirley Sherwood Gallery of Botanic Art

The Shirley Sherwood Gallery of Botanic Art opened in April 2008, and holds paintings from Kew's and Dr Shirley Sherwood's collections, many of which had never been displayed to the public before. It features paintings by artists such as Georg D. Ehret, the Bauer brothers, Pierre-Joseph Redouté and Walter Hood Fitch. The paintings and drawings are cycled on a six-monthly basis. The gallery is linked to the Marianne North Gallery (see above).

 

Near the Palm House is a building known as "Museum No. 1" (even though it is the only museum on the site), which was designed by Decimus Burton and opened in 1857. Housing Kew's economic botany collections including tools, ornaments, clothing, food and medicines, its aim was to illustrate human dependence on plants. The building was refurbished in 1998. The upper two floors are now an education centre and the ground floor houses the "Plants+People" exhibition which highlights the variety of plants and the ways that people use them.

 

Admission to the galleries and museum is free after paying admission to the gardens. The International Garden Photographer of the Year Exhibition is an annual event with an indoor display of entries during the summer months.

 

The Marianne North Gallery of Botanic Art

The Marianne North Gallery was built in the 1880s to house the paintings of Marianne North, an MP's daughter who travelled alone to North and South America, South Africa and many parts of Asia, at a time when women rarely did so, to paint plants. The gallery has 832 of her paintings. The paintings were left to Kew by the artist and a condition of the bequest is that the layout of the paintings in the gallery may not be altered.

 

The gallery had suffered considerable structural degradation since its creation and during a period from 2008 to 2009 major restoration and refurbishment took place, with works lead by with leading conservation architects Donald Insall Associates. During the time the gallery was closed the opportunity was also taken to restore the paintings to their original condition. The gallery reopened in October 2009.

 

The gallery originally opened in 1882 and is the only permanent exhibition in Great Britain dedicated to the work of one woman.

 

Plant collections

 

The plant collections include the Aquatic Garden, which is near the Jodrell laboratory. The Aquatic Garden, which celebrated its centenary in 2009, provides conditions for aquatic and marginal plants. The large central pool holds a selection of summer-flowering water lilies and the corner pools contain plants such as reed mace, bulrushes, phragmites and smaller floating aquatic species.

 

The Arboretum, which covers over half of the total area of the site, contains over 14,000 trees of many thousands of varieties. The Bonsai Collection is housed in a dedicated greenhouse near the Jodrell laboratory. The Cacti Collection is housed in and around the Princess of Wales Conservatory. The Carnivorous Plant collection is housed in the Princess of Wales Conservatory. The Grass Garden was created on its current site in the early 1980s to display ornamental and economic grasses; it was redesigned and replanted between 1994 and 1997. It is currently undergoing a further redesign and planting. Over 580 species of grasses are displayed.

 

The Herbaceous Grounds (Order Beds) were devised in the late 1860s by Sir Joseph Hooker, then director of the Royal Botanic Gardens, so that botany students could learn to recognise plants and experience at first hand the diversity of the plant kingdom. The collection is organised into family groups. Its name arose because plant families were known as natural orders in the 19th century. Over the main path is a rose pergola built in 1959 to mark the bicentennial of the Gardens. It supports climber and rambling roses selected for the length and profusion of flowering.

 

The Orchid Collection is housed in two climate zones within the Princess of Wales Conservatory. To maintain an interesting display the plants are changed regularly so that those on view are generally flowering. The Rock Garden, originally built of limestone in 1882, is now constructed of Sussex sandstone from West Hoathly, Sussex. The rock garden is divided into six geographic regions: Europe, Mediterranean and Africa, Australia and New Zealand, Asia, North America, and South America. There are currently 2,480 different "accessions" growing in the garden.

 

The Rose Garden, based upon original designs by William Nesfield, is behind the Palm House, and was replanted between 2009 and 2010 using the original design from 1848. It is intended as an ornamental display rather than a collection of a particularly large number of varieties. Other collections and specialist areas include the rhododendron dell, the azalea garden, the bamboo garden, the juniper collection, the berberis dell, the lilac garden, the magnolia collection, and the fern collection.

  

The Palm House and lake to Victoria Gate

The world's smallest water-lily, Nymphaea thermarum, was saved from extinction when it was grown from seed at Kew, in 2009.

 

Herbarium

The Kew herbarium is one of the largest in the world with approximately 7 million specimens used primarily for taxonomic study. The herbarium is rich in types for all regions of the world, especially the tropics.

 

Library and archives

The library and archives at Kew are one of the world's largest botanical collections, with over half a million items, including books, botanical illustrations, photographs, letters and manuscripts, periodicals, and maps. The Jodrell Library has been merged with the Economic Botany and Mycology Libraries and all are now housed in the Jodrell Laboratory.

 

Forensic horticulture

Kew provides advice and guidance to police forces around the world where plant material may provide important clues or evidence in cases. In one famous case the forensic science department at Kew were able to ascertain that the contents of the stomach of a headless corpse found in the river Thames contained a highly toxic African bean.

 

Economic Botany

 

The Sustainable Uses of Plants group (formerly the Centre for Economic Botany), focus on the uses of plants in the United Kingdom and the world's arid and semi-arid zones. The Centre is also responsible for curation of the Economic Botany Collection, which contains more than 90,000 botanical raw materials and ethnographic artefacts, some of which are on display in the Plants + People exhibit in Museum No. 1. The Centre is now located in the Jodrell Laboratory.

 

Jodrell Laboratory

The original Jodrell laboratory, named after Mr T. J. Phillips Jodrell who funded it, was established in 1877 and consisted of four research rooms and an office. Originally research was conducted into plant physiology but this was gradually superseded by botanical research. In 1934 an artists' studio and photographic darkroom were added, highlighting the importance of botanical illustration. In 1965, following increasing overcrowding, a new building was constructed and research expanded into seed collection for plant conservation. The biochemistry section also expanded to facilitate research into secondary compounds that could be derived from plants for medicinal purposes. In 1994 the centre was expanded again, tripling in size, and a decade later it was further expanded by the addition of the Wolfson Wing.

 

Kew Constabulary

Main article: Kew Constabulary

The gardens have their own police force, Kew Constabulary, which has been in operation since 1847. Formerly known as the Royal Botanic Gardens Constabulary, it is a small, specialised constabulary of two sergeants and 12 officers, who patrol the grounds in a green painted electric buggy. The Kew Constables are attested under section 3 of the Parks Regulation Act 1872, which gives them the same powers as the Metropolitan Police within the land belonging to the gardens.

 

Media

A number of films, documentaries and short videos have been made about Kew Gardens.

 

They include:

 

a short colour film World Garden by cinematographer Geoffrey Unsworth in 1942

three series of A Year at Kew (2007), filmed for BBC television and released on DVD

Cruickshank on Kew: The Garden That Changed the World, a 2009 BBC documentary, presented by Dan Cruickshank, exploring the history of the relationship between Kew Gardens and the British Empire

David Attenborough's 2012 Kingdom of Plants 3D

a 2003 episode of the Channel 4 TV series Time Team, presented by Tony Robinson, that searched for the remains of George III's palace

a 2004 episode of the BBC Four series Art of the Garden which looked at the building of the Great Palm House in the 1840s.

"Kew on a Plate", a TV programme showing the kinds of produce grown at Kew Gardens and how they can be prepared in a kitchen.

In 1921 Virginia Woolf published her short story "Kew Gardens", which gives brief descriptions of four groups of people as they pass by a flowerbed.

 

Access and transport

 

Elizabeth Gate

Kew Gardens is accessible by a number of gates. Currently, there are four gates into Kew Gardens that are open to the public: the Elizabeth Gate, which is situated at the west end of Kew Green, and was originally called the Main Gate before being renamed in 2012 to commemorate the Diamond Jubilee of Elizabeth II; the Brentford Gate, which faces the River Thames; the Victoria Gate (named after Queen Victoria), situated in Kew Road, which is also the location of the Visitors' Centre; and the Lion Gate, also situated in Kew Road.

 

Other gates that are not open to the public include Unicorn Gate, Cumberland Gate and Jodrell Gate (all in Kew Road) and Isleworth Gate (facing the Thames).

  

Victoria Gate

Kew Gardens station, a London Underground and National Rail station opened in 1869 and served by both the District line and the London Overground services on the North London Line, is the nearest train station to the gardens – only 400 metres (1,300 ft) along Lichfield Road from the Victoria Gate entrance. Built by the London and South Western Railway, the Historic England listed building is one of the few remaining original 19th-century stations on the North London Line, and the only station on the London Underground with a pub on the platform (though the platform entrance is now closed off). Kew Bridge station, on the other side of the Thames, 800 metres from the Elizabeth Gate entrance via Kew Bridge, is served by South West Trains from Clapham Junction and Waterloo.

 

London Buses route 65, between Ealing Broadway and Kingston, stops near the Lion Gate and Victoria Gate entrances; route 391, between Fulham and Richmond, stops near Kew Gardens station; while routes 237 and 267 stop at Kew Bridge station.

 

London River Services operate from Westminster during the summer, stopping at Kew Pier, 500 metres (1,600 ft) from Elizabeth Gate. Cycle racks are located just inside the Victoria Gate, Elizabeth Gate and Brentford Gate entrances. There is a 300-space car park outside Brentford Gate, reached via Ferry Lane, as well as some free, though restricted, on-street parking on Kew Road.

 

en.wikipedia.org/wiki/Kew_Gardens

Includes teams from Brookings, SF Lincoln, SF Roosevelt, RC Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.

©2021 SDPB

 

Includes teams from O'Gorman, Yankton, Pierre T.F. Riggs, Huron. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.

©2021 SDPB

 

Employee break room kitchen that includes a range and oven that have added safety shutoff and fire suppression features at the Sandhills Medical Foundation facility, where a U.S. Department of Agriculture USDA Rural Development RD Community Facilities Direct Loans and Guaranteed Loans Program provided $2,964,500.00 for the 12,150-square-foot expansion in Lugoff, SC, on August 10, 2022.

The expansion more than mirrors the previous facility. It increases medical and emergency power generation. USDA media by Lance Cheung.

 

For more information about the Community Facilities Loans and Grants Program, please go to rd.usda.gov/programs-services/community-facilities/community-facilities-direct-loan-grant-program

I include this shot at this time because a wildfire very near this site (a few miles) is still ongoing! Our Thompson Ridge brush truck and fire crew was joined by several others in this general region to fight the fire. It was hot and dry... but not windy. The initial (volunteer) responders did a super job containing the fire to about 5 acres until additional support including the USFS arrived. No areal support was provided. The blaze is now under guarded watch to monitor the remaining "hot spots."

 

THANKS TO THE RAPID RESPONSE BY MANY OF OUR NEIGHBORS AND FRIENDS, THESE ANIMALS STILL HAVE NATURAL PLACES LIKE THIS TO BROWSE AND BE SAFE... (and so do we)! KUDOS TO OUR FIRST RESPONDERS!!!

 

These young deer were members of a small feeding group. (There are at least 6 deer visible in this image.) It appeared to me that they were all young, and all female. Perhaps the oldest was three years.

 

IMG_0638; Mule Deer

One of the extraordinary Edwardian machines during practice for the S F Edge Trophy at the 74th Members' Meeting, Goodwood

Includes teams from Brookings, SF Lincoln, SF Roosevelt, RC Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.

©2021 SDPB

 

Another cold, but bright sunny Winter's day. The water was very still on the this morning - at the peak of the high tide

Includes: dark blue jacket and classic panths, pink shirt, vest is variable. Suitable for Iplehouse EID man (superhero type) and dolls with same sizes. Available for order in various colours and configuration.

Includes: dark blue jacket and classic panths, pink shirt, vest is variable. Suitable for Iplehouse EID man (superhero type) and dolls with same sizes. Available for order in various colours and configuration.

Common names include ragwort, common ragwort, tansy ragwort, benweed, St. James-wort, ragweed, stinking nanny/ninny/willy, staggerwort, dog standard, cankerwort, stammerwort, mare's fart and cushag.

 

In the western US it is generally known as tansy ragwort, or tansy, though its resemblance to the true tansy is superficial.

 

Thanks to Wikipedia for the info!

From a walk around Woods Mill. There were several of these Small Skipers about.

17/8/16 #1325. Ponies on the beach near Lancing Sailing Club after a gallop in the sea on a beautifully calm and warm Summer's evening

 

Horses #40 for the treasure hunt

From a wander along the Adur at high tide. I'm told that this is a Rock Pipit. It was fluttering around near the beach end of the Ferry Bridge

The Arrows' display on Friday at the Goodwood Festival of Speed. Shot from the Porsche stand.

Queen Anne’s Lace.

 

The Wild Carrot, Daucus carota, whose common names include wild carrot, bird's nest, bishop's lace, and Queen Anne's lace (North America), is a white, flowering plant in the family Apiaceae, native to temperate regions of Europe and southwest Asia, and naturalized to North America and Australia. Domesticated carrots are cultivars of a subspecies, Daucus carota subsp. sativus.

 

The plant is a herbaceous, somewhat variable biennial plant that grows between 30 and 60 cm (1 and 2 ft) tall, and is roughly hairy, with a stiff, solid stem. The leaves are tripinnate, finely divided and lacy, and overall triangular in shape. The leaves are bristly and alternate in a pinnate pattern that separates into thin segments. The flowers are small and dull white, clustered in flat, dense umbels. The main identifier is the hairy stem of the wild carrot.

 

Scientific name: Daucus carota subsp. L.

 

Taxonomy -

 

Class: Equisetopsida Subclass: Magnoliidae Superorder: Asteranae

 

Order: Apiales Family:Apiaceae Genus: Daucus

 

Common name( s): wild carrot, carrot, Queen Anne’s lace, bird’s nest, devil’s plague

 

Synonym (s): Carota sylvestr is (Mill.) Rupr., Caucalis carnosa Roth more here

 

Conservation status: Widespread and not considered to be threatened.

 

Habitat: Rough grassland, coastal cliffs and dunes.

 

Key uses: Food and drink.

 

Known hazards: Wild carrot has some medical properties and is similar in appearance to poisonous species such as poison hemlock (Conium maculatum), water hemlock (Cicuta maculata) and fool's parsley (Aethusa cynapium).

 

Taxonomy Class: Equisetopsida

 

Subclass: Magnoliidae Super or der : Asteranae

 

Order : Apiales Family: Apiaceae

 

Genus: Daucus (source for the above - Royal Botanical Gardens, Kew, London UK - more information - www.kew.org/plants-fungi/Daucus-carota.htm) picture - Deutschlands Flora in Abbildungen, Jacob Sturm und Johann Georg Sturm (1796) Original Description Echte Möhre, Daucus carota.

 

The Wild Carrot (Daucus Carota) (a.k.a.Queen Anne's Lace) is thought to have originated on the Iranian Plateau (an area which now includes Afghanistan, Pakistan and Iran). It is abundant in temperate regions across the globe, particularly Western Asia and Europe, and is widely distributed across much of the United States whereCarrot Now and then - wild and domestic it is often found along roadsides, abandoned fields, and pastures.

 

Cultivated plant species and their sexually-compatible wild relatives often overlap in terms of geographic proximity and phenology. This overlap provides the opportunity for gene flow between crops and their wild relatives. Farmers and breeders are often concerned with the potential for wild allelic contamination into agricultural fields, which can hinder production efficiency.

 

In many carrot producing regions throughout the world, wild carrot populations can be found growing in close proximity to cultivated carrot fields.

 

Wild carrot is the progenitor of the cultivated carrot, D. carota subsp. sativus, and the two subspecies are sexually compatible. The cultivated carrot was likely domesticated in Central Asia roughly 1,100 yr ago and is grown worldwide from both open pollinated and hybrid seed.

 

Wild Carrot mainly occurs in free-draining and slightly acidic soils on rough grassland, coastal cliffs and dunes. It frequently naturalises in fields and gardens.

 

It is one of many umbelliferous plants to be found growing around the world. Wild carrot appears in many temperate regions of the world, far beyond its Mediterranean and Asian centres of origin where this plant displays great diversity. It is quite possible that ancient cultures in those regions used wild carrot as a herb, and it is also quite likely that the seeds were used medicinally in the Mediterranean region since antiquity (Banga 1958).

 

Almost certainly the wild and early forms of the domesticated carrot were first used as a medicine before they were used as a root vegetable in the conventional sense of that term today. There is good genetic evidence that wild carrot is the direct progenitor of the cultivated carrot (Simon 2000). Selection for a swollen rooted type suitable for domestic consumption undoubtedly took many centuries.

 

Both the wild and the cultivated carrots belong to the species Daucus carota. Wild carrot is distinguished by the name Daucus carota, Carota, whereas domesticated carrot belongs to Daucus carota, sativus. As a member of the carrot family it has a long taproot and lacy leaves. Dig up and crush a Wild Carrot root and you will find that it smells just like a carrot.

 

It is yellowish or ivory in colour, spindle-shaped, slender, firm and woody; a pernicious weed in some areas. It is edible when young but the root (especially the centre) soon gets tough and woody due to the high content of xylem tissue. The domestic carrot is a relative that lacks most of this tissue. The wild carrot has finely divided leaves like that of the domesticated carrot. The leaves, petioles and flower stems may be densely hairy or have no hair. The leaves on the stem are arranged alternately. Flowering wild carrot may grow four feet tall. At the end of the stem is a primary umbel (seed head) made up of numerous individual white flowers and possibly a purple flower in the center together with drooping, narrow bracts on the underside . Plants also may have many secondary umbels produced at any node on the stem below the primary umbel.

 

Each flower on the umbel produces two seeds. After seed set, the umbel closes upward. Once the seeds have turned brown, they are mature. The roots of wild carrot are typically white. The characteristic odour of carrot is present when any part of the plant is crushed. Spent umbels curl inwards forming a depressed cup. The fruits are covered in hooked spines, which aid dispersal by clinging to the fur of passing animals. Flowering period (in England) is from June to August and the native biennial can reach a height of 90 centimetres.

 

Wild Carrot is also known as Queen Anne's Lace, Birds Nest Weed, Bees Nest, Devils Plague, garden carrot, Bird's Nest Root, Fools Parsley, Lace Flower, Rantipole, Herbe a dinde and Yarkuki. Herbe a dinde derives from its use as a feed for young turkeys-dinde.

 

"Daucus" comes from daukos, name given by the Greeks to some members of the Umbelliferae family and it seems to derive from "daîo" : I overheat . Carota means carrot in Latin.

 

Can you eat carrot flowers? - Yes at your won risk! - Your best bet is to read up on survival or self sufficiency foods, a good source from people who have tried and lived to tell the tale!

 

As I recall from reading such a survival book, wild carrot flowers (and many others ) are edible. The big caveat is, and I cannot emphasise this too much - be absolutely sure it is Wild Carrot as it is very similar to poison hemlock (which killed Socrates!).

 

Deep fried carrot flower is supposed to be a delicacy - www.altnature.com/gallery/Wild_Carrot.htm

So on that basis domestic carrot flowers should be edible too.

 

My friend from What's Cooking America has a useful guide for you - whatscookingamerica.net/EdibleFlowers/EdibleFlowersMain.htm

And another guide for you - www.herbsarespecial.com.au/self-sufficiency/edible-flower...

 

The Mystery of the Purple Floret

 

Queen Anne’s Lace is common in North America, Europe and Asia. In the summer it produces beautiful compound flowers that form a carpet of hundreds of tiny white florets. Strangely, quite often you will find a single darkly coloured floret just off center, standing tall above the rest. No one knows why.

 

Botanists have debated the mystery of the coloured floret in Daucas carota (also known as “Queen Anne’s Lace,” “Wild Carrot,” “Bishop’s Lace,” and “Bird’s Nest”) for at least the last 150 years. Back then some of the most learned botanists believed that the floret was a genetic oddity that provided no service to the plant. Many modern botanists disagree. Some suspect that the coloured floret tricks flying insects into thinking that a bug is already sitting on the flower.

 

Perhaps this attracts predatory wasps to land hoping to snatch a quick meal. Perhaps the presence of one insect is a signal to others that there is something on this flower worth having. If so, then the floret might entice flying insects to land and thereby help pollinate the plant.

 

The research that’s been done so far on this question has produced contradictory results. Some naturalists argue that they have found evidence that favours the idea that the dark floret is an insect mimic. Others have presented data that suggests that the floret does nothing to help the plant increase the number of viable seeds it produces, and therefore does nothing to help it propagate its species.

 

By solving the great debate of its function, new knowledge about the central dark spot and its possible role as an insect attractant could lead to future developments in cultivation as well as in methods for improving agricultural processes in cultivated carrots.

 

The wild carrot is an aromatic herb that acts as a diuretic, soothes the digestive tract and stimulates the uterus. A wonderfully cleansing medicine, it supports the liver, stimulates the flow of urine and the removal of waste by the kidneys. An infusion is used in the treatment of various complaints including digestive disorders, kidney and bladder diseases and in the treatment of dropsy.

 

An infusion of the leaves has been used to counter cystitis and kidney stone formation, and to diminish stones that have already formed. Carrot leaves contain significant amounts of porphyrins, which stimulate the pituitary gland and lead to the release of increased levels of sex hormones.

 

The plant is harvested in July and dried for later use. A warm water infusion of the flowers has been used in the treatment of diabetes. The grated raw root, especially of the cultivated forms, is used as a remedy for threadworms. The root is also used to encourage delayed menstruation.

 

The root of the wild plant can induce uterine contractions and so should not be used by pregnant women. A tea made from the roots is diuretic and has been used in the treatment of urinary stones.

 

An infusion is used in the treatment of oedema, flatulent indigestion and menstrual problems. The seed is a traditional 'morning after' contraceptive and there is some evidence to uphold this belief. It requires further investigation. Carrot seeds can be abortifacient and so should not be used by pregnant women.

 

Ancient folk lore said that to cure epileptic seizures you should eat the dark coloured middle flower of Queen Annes Lace. The flower is also used in ancient rituals an spells, for women to increase fertility and for men to increase potency and sexual desire!

 

A warm water infusion of the flowers has been used in the treatment of diabetes. The grated raw root, especially of the cultivated forms, is used as a remedy for threadworms.

 

The root is also used to encourage delayed menstruation. The root of the wild plant can induce uterine contractions and so should not be used by pregnant women.

 

A tea made from the roots is diuretic and has been used in the treatment of urinary stones. The seeds are diuretic, carminative, emmenagogue and anthelmintic.

 

An infusion is used in the treatment of oedema, flatulent indigestion and menstrual problems. The seed is a traditional ‘morning after’ contraceptive and there is some evidence to uphold this belief. It requires further investigation. Carrot seeds can be abortifacient and so should not be used by pregnant women.

 

Queen Annes Lace is the wild progenitor of the domesticated carrot. Although native to the Old World, these white lacy umbels are a familiar sight in the United States and Canada. The medicinal properties of Queen Annes Lace are many. More detail is given below. Its seeds may be collected, dried and used for tea. It is interesting to note that this plant is the closest living relative (on the basis of family and medicinal activity) to Silphion, which was picked and used by the Romans as a culinary spice and contraceptive until it became extinct in the first century AD. Apparently it was extremely effective. Supposedly Nero was given the last remaining root.

 

In the late 1980s scientists began studying Queen Annes Lace and found that (in mice at least) it blocked the production of progesterone and inhibited fetal and ovarian growth. Check out thecontraception page of the Museum.

 

Queen Anne's Lace is quite an aggressive plant. It is a biennial, so lives only 2 years, thus never forms a big root mass like daisies or other perennial wildflowers. However, it is such a prolific seeder, it does spread rapidly, and is almost impossible to eradicate. It is an alien, but one of the ones that's been in the US since colonial times. It came across the ocean in sacks of grain, probably with the Pilgrims. It's now established in every State. It's beautiful in the wildflower meadow I am not so sure in the garden.

 

If you want to plant it, easiest way is to gather a handful of the seeds from a plant dying down in the fall. They seem to be everywhere. But there is also another option. Try an annual named Ammi majus. It's the flower common in the cut flower trade as "Queen Anne's Lace", and is also sometimes called "Bishop's Flower." The two look very similar, but the latter doesn't last in your soil forever as Daucus does.

 

Today, in some parts of rural United States, this herb is used as a sort of morning-after contraceptive by women who drink a teaspoonful of the seeds with a glass of water immediately after sex. The seeds are also used for the prevention and washing out of gravel and urinary stones. As they are high in volatile oil, some find them soothing to the digestive system, useful for colic and flatulence. Be very, very sure that if you do decide to harvest any part of Queen Annes Lace for consumption that you have the correct plant. It is similar to Hemlock (Conium maculatum), a herb which was used medicinally but is now seldom used because of its high toxicity.

 

The Wild Carrot is still very much prevalent, particularly in the US where it was introduced from Europe and is the genetic source of edible carrots. Wild Carrot is found in sandy or gravelly soils and in wets areas. It is abundant west of the Cascades in Oregon and Washington where it is classed as a Class C noxious weed. Wild Carrot causes problems in pastures, hay fields, Christmas tree farms, grass seed fields and most other open areas that are not tilled annually. It is an especially serious threat in areas where carrot seed is produced because it hybridizes with the crop and ruins the seed.

 

Washington state has gone so far as to quarantine the plants to prevent any further escapes into its wildlands and agricultural regions. It is illegal to transport, buy, sell or distribute seed there. The penalty is a $5,000 fine.

 

Wild Cwild carrot and rosettearrot is easy to grow, it prefers a sunny position and a well-drained neutral to alkaline soil. Considered an obnoxious weed by some, it can spread very quickly. Its root is small and spindle shaped, whitish, slender and hard, (tender when young), but soon gets tough, with a strong aromatic smell. Harvest entire plant in July or when flowers bloom, and dry for later herb use. Collect edible roots and shoots in spring when tender. Gather seed in autumn (the fall).

 

There is no record of wild carrot toxicity in the US but in Europe wild carrot has been known to be mildly toxic to horses and cattle. A high concentration of wild carrot in hay is potentially a problem because livestock eat hay less selectively than green forage. Sheep appear to graze wild carrot without any harmful effect. Find out about some of the myths as to why Queen Annes Lace is so called click here.

 

wild carrot plantThis plant is a biennial which grows, in its second year, from a taproot (the carrot) to a height of two to four feet. The stems are erect and branched; both stems and leaves are covered with short coarse hairs.

 

The leaves are very finely divided; the botanical term is tri-pinnate. When a leaf is composed of a number of lateral leaflets, it is said to be pinnate or feather-like; and when these lateral divisions are themselves pinnated, it is said to be bi-pinnate, or twice-feathered. The leaves of this plant are like that but some of the lower leaves are still more divided and become tri-pinnate. The lower leaves are considerably larger than the upper ones, and their arrangement on the main stem is alternate. All of these leaves embrace the stem with a sheathing base.

wild carrot flowerThe attractive two to four inch "flower" is actually a compound inflorescence made up of many small flowers. The umbels of the flowers are terminal and composed of many rays. The flowers themselves are very small, but from their whiteness and number, present a very conspicuous appearance. The central flower of each umbel is often purple.

 

During the flowering period the head is nearly flat or slightly convex, but as the seeds ripen the form becomes very cup-like; hence one of the popular names for this plant is "bird's nest." The seeds are covered with numerous little bristles arranged in five rows. For more photos click here.

 

Like their domestic cousins, wild carrot roots can be eaten. However, they are only edible when very young. After that, they are too tough and woody. The flowers are also edible. Flower clusters can be french fried for a carrot-flavoured, quite attractive dish.

  

Shoreditch London City Road Closed Silicon Roundabout Major Road Works. This cycle lane change is a three-year project. The road is the inner ring road for London. They have blocked one of the tube entrances which includes the underpass. Ironically, cyclist do not even use this route since they blocked off the backstreets to traffic. They are trying to sabotage London. The situation is disgusting.

Includes 16 color recipes, several jewelry projects and 3 mini-tutorials

Includes teams from O'Gorman, Yankton, Pierre T.F. Riggs, Huron. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.

©2021 SDPB

 

I set off on a road trip that would include driving Shafer Trail and Potash Road through Canyonlands National Park. When I made it back to pavement I raced over to the southern entrance to take in the Needles District and go to the end of the road, with a quick stop at Newspaper Rock.

 

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Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab. The park preserves a colorful landscape eroded into numerous canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964.

 

The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the combined rivers—the Green and Colorado—which carved two large canyons into the Colorado Plateau. While these areas share a primitive desert atmosphere, each retains its own character. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."

 

Source: Wikipedia

en.wikipedia.org/wiki/Canyonlands_National_Park

 

Dylan Marlais Thomas (27 October 1914 – 9 November 1953) was a Welsh poet and writer whose works include the poems "Do not go gentle into that good night" and "And death shall have no dominion"; the 'play for voices' Under Milk Wood; and stories and radio broadcasts such as A Child's Christmas in Wales and Portrait of the Artist as a Young Dog. He became widely popular in his lifetime and remained so after his premature death at the age of 39 in New York City. By then, he had acquired a reputation, which he had encouraged, as a "roistering, drunken and doomed poet".[3]

 

Thomas was born in Swansea, Wales, in 1914. An undistinguished pupil, he left school at 16 and became a journalist for a short time. Many of his works appeared in print while he was still a teenager; however, it was the publication of "Light breaks where no sun shines," in 1934, that caught the attention of the literary world. While living in London, Thomas met Caitlin Macnamara, whom he married in 1937. Their relationship was defined by alcoholism and was mutually destructive.[3] In the early part of their marriage, Thomas and his family lived hand-to-mouth, settling in the Welsh fishing village of Laugharne.

 

Thomas came to be appreciated as a popular poet during his lifetime, and he found earning a living as a writer difficult. He began augmenting his income with reading tours and radio broadcasts. His radio recordings for the BBC during the late 1940s brought him to the public's attention, and he was frequently used by the BBC as a populist voice of the literary scene.

 

Thomas first traveled to the United States in the 1950s. This is where his readings brought him a level of fame while his erratic behaviour and drinking worsened. His time in America cemented Thomas's legend, however, and he went on to record to vinyl such works as A Child's Christmas in Wales. During his fourth trip to New York in 1953, Thomas became gravely ill and fell into a coma, from which he never recovered. He died on 9 November 1953. His body was returned to Wales where he was interred at the village churchyard in Laugharne on 25 November 1953.

 

Though Thomas wrote exclusively in the English language, he has been acknowledged as one of the most important Welsh poets of the 20th century. He is noted for his original, rhythmic and ingenious use of words and imagery. Thomas's position as one of the great modern poets has been much discussed, and he remains popular with the public.

 

en.wikipedia.org/wiki/Dylan_Thomas

 

This blue plaque is affixed to 54 Delancey Street, Camden

Bali is an island and province of Indonesia. The province includes the island of Bali and a few smaller neighbouring islands, notably Nusa Penida, Nusa Lembongan, and Nusa Ceningan. It is located at the westernmost end of the Lesser Sunda Islands, between Java to the west and Lombok to the east. Its capital of Denpasar is located at the southern part of the island.

 

With a population of 3,890,757 in the 2010 census, and 4,225,000 as of January 2014, the island is home to most of Indonesia's Hindu minority. According to the 2010 Census, 83.5% of Bali's population adhered to Balinese Hinduism, followed by 13.4% Muslim, Christianity at 2.5%, and Buddhism 0.5%.

 

Bali is a popular tourist destination, which has seen a significant rise in numbers since the 1980s. It is renowned for its highly developed arts, including traditional and modern dance, sculpture, painting, leather, metalworking, and music. The Indonesian International Film Festival is held every year in Bali.

 

Bali is part of the Coral Triangle, the area with the highest biodiversity of marine species. In this area alone over 500 reef building coral species can be found. For comparison, this is about 7 times as many as in the entire Caribbean. There is a wide range of dive sites with high quality reefs, all with their own specific attractions. Many sites can have strong currents and swell, so diving without a knowledgeable guide is inadvisable. Most recently, Bali was the host of the 2011 ASEAN Summit, 2013 APEC and Miss World 2013.

 

HISTORY

ANCIENT

Bali was inhabited around 2000 BC by Austronesian people who migrated originally from Southeast Asia and Oceania through Maritime Southeast Asia. Culturally and linguistically, the Balinese are closely related to the people of the Indonesian archipelago, Malaysia, the Philippines, and Oceania. Stone tools dating from this time have been found near the village of Cekik in the island's west.

 

In ancient Bali, nine Hindu sects existed, namely Pasupata, Bhairawa, Siwa Shidanta, Waisnawa, Bodha, Brahma, Resi, Sora and Ganapatya. Each sect revered a specific deity as its personal Godhead.

 

Inscriptions from 896 and 911 don't mention a king, until 914, when Sri Kesarivarma is mentioned. They also reveal an independent Bali, with a distinct dialect, where Buddhism and Sivaism were practiced simultaneously. Mpu Sindok's great granddaughter, Mahendradatta (Gunapriyadharmapatni), married the Bali king Udayana Warmadewa (Dharmodayanavarmadeva) around 989, giving birth to Airlangga around 1001. This marriage also brought more Hinduism and Javanese culture to Bali. Princess Sakalendukirana appeared in 1098. Suradhipa reigned from 1115 to 1119, and Jayasakti from 1146 until 1150. Jayapangus appears on inscriptions between 1178 and 1181, while Adikuntiketana and his son Paramesvara in 1204.

 

Balinese culture was strongly influenced by Indian, Chinese, and particularly Hindu culture, beginning around the 1st century AD. The name Bali dwipa ("Bali island") has been discovered from various inscriptions, including the Blanjong pillar inscription written by Sri Kesari Warmadewa in 914 AD and mentioning "Walidwipa". It was during this time that the people developed their complex irrigation system subak to grow rice in wet-field cultivation. Some religious and cultural traditions still practised today can be traced to this period.

 

The Hindu Majapahit Empire (1293–1520 AD) on eastern Java founded a Balinese colony in 1343. The uncle of Hayam Wuruk is mentioned in the charters of 1384-86. A mass Javanese emigration occurred in the next century.

 

PORTUGUESE CONTACTS

The first known European contact with Bali is thought to have been made in 1512, when a Portuguese expedition led by Antonio Abreu and Francisco Serrão sighted its northern shores. It was the first expedition of a series of bi-annual fleets to the Moluccas, that throughout the 16th century usually traveled along the coasts of the Sunda Islands. Bali was also mapped in 1512, in the chart of Francisco Rodrigues, aboard the expedition. In 1585, a ship foundered off the Bukit Peninsula and left a few Portuguese in the service of Dewa Agung.

 

DUTCH EAST INDIA

In 1597 the Dutch explorer Cornelis de Houtman arrived at Bali, and the Dutch East India Company was established in 1602. The Dutch government expanded its control across the Indonesian archipelago during the second half of the 19th century (see Dutch East Indies). Dutch political and economic control over Bali began in the 1840s on the island's north coast, when the Dutch pitted various competing Balinese realms against each other. In the late 1890s, struggles between Balinese kingdoms in the island's south were exploited by the Dutch to increase their control.

 

In June 1860 the famous Welsh naturalist, Alfred Russel Wallace, travelled to Bali from Singapore, landing at Buleleng on the northcoast of the island. Wallace's trip to Bali was instrumental in helping him devise his Wallace Line theory. The Wallace Line is a faunal boundary that runs through the strait between Bali and Lombok. It has been found to be a boundary between species of Asiatic origin in the east and a mixture of Australian and Asian species to the west. In his travel memoir The Malay Archipelago, Wallace wrote of his experience in Bali:

 

I was both astonished and delighted; for as my visit to Java was some years later, I had never beheld so beautiful and well-cultivated a district out of Europe. A slightly undulating plain extends from the seacoast about ten or twelve miles inland, where it is bounded by a fine range of wooded and cultivated hills. Houses and villages, marked out by dense clumps of coconut palms, tamarind and other fruit trees, are dotted about in every direction; while between them extend luxurious rice-grounds, watered by an elaborate system of irrigation that would be the pride of the best cultivated parts of Europe.

 

The Dutch mounted large naval and ground assaults at the Sanur region in 1906 and were met by the thousands of members of the royal family and their followers who fought against the superior Dutch force in a suicidal puputan defensive assault rather than face the humiliation of surrender. Despite Dutch demands for surrender, an estimated 200 Balinese marched to their death against the invaders. In the Dutch intervention in Bali, a similar massacre occurred in the face of a Dutch assault in Klungkung.

 

AFTERWARD THE DUTCH GOVERNORS

exercised administrative control over the island, but local control over religion and culture generally remained intact. Dutch rule over Bali came later and was never as well established as in other parts of Indonesia such as Java and Maluku.

 

n the 1930s, anthropologists Margaret Mead and Gregory Bateson, artists Miguel Covarrubias and Walter Spies, and musicologist Colin McPhee all spent time here. Their accounts of the island and its peoples created a western image of Bali as "an enchanted land of aesthetes at peace with themselves and nature." Western tourists began to visit the island.

 

Imperial Japan occupied Bali during World War II. It was not originally a target in their Netherlands East Indies Campaign, but as the airfields on Borneo were inoperative due to heavy rains, the Imperial Japanese Army decided to occupy Bali, which did not suffer from comparable weather. The island had no regular Royal Netherlands East Indies Army (KNIL) troops. There was only a Native Auxiliary Corps Prajoda (Korps Prajoda) consisting of about 600 native soldiers and several Dutch KNIL officers under command of KNIL Lieutenant Colonel W.P. Roodenburg. On 19 February 1942 the Japanese forces landed near the town of Senoer [Senur]. The island was quickly captured.

 

During the Japanese occupation, a Balinese military officer, Gusti Ngurah Rai, formed a Balinese 'freedom army'. The harshness of war requisitions made Japanese rule more resented than Dutch rule. Following Japan's Pacific surrender in August 1945, the Dutch returned to Indonesia, including Bali, to reinstate their pre-war colonial administration. This was resisted by the Balinese rebels, who now used recovered Japanese weapons. On 20 November 1946, the Battle of Marga was fought in Tabanan in central Bali. Colonel I Gusti Ngurah Rai, by then 29 years old, finally rallied his forces in east Bali at Marga Rana, where they made a suicide attack on the heavily armed Dutch. The Balinese battalion was entirely wiped out, breaking the last thread of Balinese military resistance.

 

INDIPENDENCE FROM THE DUTCH

In 1946, the Dutch constituted Bali as one of the 13 administrative districts of the newly proclaimed State of East Indonesia, a rival state to the Republic of Indonesia, which was proclaimed and headed by Sukarno and Hatta. Bali was included in the "Republic of the United States of Indonesia" when the Netherlands recognised Indonesian independence on 29 December 1949.

 

CONTEMPORARY

The 1963 eruption of Mount Agung killed thousands, created economic havoc and forced many displaced Balinese to be transmigrated to other parts of Indonesia. Mirroring the widening of social divisions across Indonesia in the 1950s and early 1960s, Bali saw conflict between supporters of the traditional caste system, and those rejecting this system. Politically, the opposition was represented by supporters of the Indonesian Communist Party (PKI) and the Indonesian Nationalist Party (PNI), with tensions and ill-feeling further increased by the PKI's land reform programs. An attempted coup in Jakarta was put down by forces led by General Suharto.

 

The army became the dominant power as it instigated a violent anti-communist purge, in which the army blamed the PKI for the coup. Most estimates suggest that at least 500,000 people were killed across Indonesia, with an estimated 80,000 killed in Bali, equivalent to 5% of the island's population. With no Islamic forces involved as in Java and Sumatra, upper-caste PNI landlords led the extermination of PKI members.

 

As a result of the 1965/66 upheavals, Suharto was able to manoeuvre Sukarno out of the presidency. His "New Order" government reestablished relations with western countries. The pre-War Bali as "paradise" was revived in a modern form. The resulting large growth in tourism has led to a dramatic increase in Balinese standards of living and significant foreign exchange earned for the country. A bombing in 2002 by militant Islamists in the tourist area of Kuta killed 202 people, mostly foreigners. This attack, and another in 2005, severely reduced tourism, producing much economic hardship to the island.

 

GEOGRAPHY

The island of Bali lies 3.2 km east of Java, and is approximately 8 degrees south of the equator. Bali and Java are separated by the Bali Strait. East to west, the island is approximately 153 km wide and spans approximately 112 km north to south; administratively it covers 5,780 km2, or 5,577 km2 without Nusa Penida District, its population density is roughly 750 people/km2.

 

Bali's central mountains include several peaks over 3,000 metres in elevation. The highest is Mount Agung (3,031 m), known as the "mother mountain" which is an active volcano rated as one of the world's most likely sites for a massive eruption within the next 100 years. Mountains range from centre to the eastern side, with Mount Agung the easternmost peak. Bali's volcanic nature has contributed to its exceptional fertility and its tall mountain ranges provide the high rainfall that supports the highly productive agriculture sector. South of the mountains is a broad, steadily descending area where most of Bali's large rice crop is grown. The northern side of the mountains slopes more steeply to the sea and is the main coffee producing area of the island, along with rice, vegetables and cattle. The longest river, Ayung River, flows approximately 75 km.

 

The island is surrounded by coral reefs. Beaches in the south tend to have white sand while those in the north and west have black sand. Bali has no major waterways, although the Ho River is navigable by small sampan boats. Black sand beaches between Pasut and Klatingdukuh are being developed for tourism, but apart from the seaside temple of Tanah Lot, they are not yet used for significant tourism.

 

The largest city is the provincial capital, Denpasar, near the southern coast. Its population is around 491,500 (2002). Bali's second-largest city is the old colonial capital, Singaraja, which is located on the north coast and is home to around 100,000 people. Other important cities include the beach resort, Kuta, which is practically part of Denpasar's urban area, and Ubud, situated at the north of Denpasar, is the island's cultural centre.

 

Three small islands lie to the immediate south east and all are administratively part of the Klungkung regency of Bali: Nusa Penida, Nusa Lembongan and Nusa Ceningan. These islands are separated from Bali by the Badung Strait.

 

To the east, the Lombok Strait separates Bali from Lombok and marks the biogeographical division between the fauna of the Indomalayan ecozone and the distinctly different fauna of Australasia. The transition is known as the Wallace Line, named after Alfred Russel Wallace, who first proposed a transition zone between these two major biomes. When sea levels dropped during the Pleistocene ice age, Bali was connected to Java and Sumatra and to the mainland of Asia and shared the Asian fauna, but the deep water of the Lombok Strait continued to keep Lombok Island and the Lesser Sunda archipelago isolated.

 

CLIMATE

Being just 8 degrees south of the equator, Bali has a fairly even climate year round.

 

Day time temperatures at low elevations vary between 20-33⁰ C although it can be much cooler than that in the mountains. The west monsoon is in place from approximately October to April and this can bring significant rain, particularly from December to March. Outside of the monsoon period, humidity is relatively low and any rain unlikely in lowland areas.

 

ECOLOGY

Bali lies just to the west of the Wallace Line, and thus has a fauna that is Asian in character, with very little Australasian influence, and has more in common with Java than with Lombok. An exception is the yellow-crested cockatoo, a member of a primarily Australasian family. There are around 280 species of birds, including the critically endangered Bali myna, which is endemic. Others Include barn swallow, black-naped oriole, black racket-tailed treepie, crested serpent-eagle, crested treeswift, dollarbird, Java sparrow, lesser adjutant, long-tailed shrike, milky stork, Pacific swallow, red-rumped swallow, sacred kingfisher, sea eagle, woodswallow, savanna nightjar, stork-billed kingfisher, yellow-vented bulbul and great egret.

 

Until the early 20th century, Bali was home to several large mammals: the wild banteng, leopard and the endemic Bali tiger. The banteng still occurs in its domestic form, whereas leopards are found only in neighbouring Java, and the Bali tiger is extinct. The last definite record of a tiger on Bali dates from 1937, when one was shot, though the subspecies may have survived until the 1940s or 1950s. The relatively small size of the island, conflict with humans, poaching and habitat reduction drove the Bali tiger to extinction. This was the smallest and rarest of all tiger subspecies and was never caught on film or displayed in zoos, whereas few skins or bones remain in museums around the world. Today, the largest mammals are the Javan rusa deer and the wild boar. A second, smaller species of deer, the Indian muntjac, also occurs. Saltwater crocodiles were once present on the island, but became locally extinct sometime during the last century.

 

Squirrels are quite commonly encountered, less often is the Asian palm civet, which is also kept in coffee farms to produce Kopi Luwak. Bats are well represented, perhaps the most famous place to encounter them remaining the Goa Lawah (Temple of the Bats) where they are worshipped by the locals and also constitute a tourist attraction. They also occur in other cave temples, for instance at Gangga Beach. Two species of monkey occur. The crab-eating macaque, known locally as "kera", is quite common around human settlements and temples, where it becomes accustomed to being fed by humans, particularly in any of the three "monkey forest" temples, such as the popular one in the Ubud area. They are also quite often kept as pets by locals. The second monkey, endemic to Java and some surrounding islands such as Bali, is far rarer and more elusive is the Javan langur, locally known as "lutung". They occur in few places apart from the Bali Barat National Park. They are born an orange colour, though by their first year they would have already changed to a more blackish colouration. In Java however, there is more of a tendency for this species to retain its juvenile orange colour into adulthood, and so you can see a mixture of black and orange monkeys together as a family. Other rarer mammals include the leopard cat, Sunda pangolin and black giant squirrel.

 

Snakes include the king cobra and reticulated python. The water monitor can grow to at least 1.5 m in length and 50 kg and can move quickly.

 

The rich coral reefs around the coast, particularly around popular diving spots such as Tulamben, Amed, Menjangan or neighbouring Nusa Penida, host a wide range of marine life, for instance hawksbill turtle, giant sunfish, giant manta ray, giant moray eel, bumphead parrotfish, hammerhead shark, reef shark, barracuda, and sea snakes. Dolphins are commonly encountered on the north coast near Singaraja and Lovina.

 

A team of scientists conducted a survey from 29 April 2011 to 11 May 2011 at 33 sea sites around Bali. They discovered 952 species of reef fish of which 8 were new discoveries at Pemuteran, Gilimanuk, Nusa Dua, Tulamben and Candidasa, and 393 coral species, including two new ones at Padangbai and between Padangbai and Amed. The average coverage level of healthy coral was 36% (better than in Raja Ampat and Halmahera by 29% or in Fakfak and Kaimana by 25%) with the highest coverage found in Gili Selang and Gili Mimpang in Candidasa, Karangasem regency.

 

Many plants have been introduced by humans within the last centuries, particularly since the 20th century, making it sometimes hard to distinguish what plants are really native.[citation needed] Among the larger trees the most common are: banyan trees, jackfruit, coconuts, bamboo species, acacia trees and also endless rows of coconuts and banana species. Numerous flowers can be seen: hibiscus, frangipani, bougainvillea, poinsettia, oleander, jasmine, water lily, lotus, roses, begonias, orchids and hydrangeas exist. On higher grounds that receive more moisture, for instance around Kintamani, certain species of fern trees, mushrooms and even pine trees thrive well. Rice comes in many varieties. Other plants with agricultural value include: salak, mangosteen, corn, kintamani orange, coffee and water spinach.

 

ENVIRONMENT

Some of the worst erosion has occurred in Lebih Beach, where up to 7 metres of land is lost every year. Decades ago, this beach was used for holy pilgrimages with more than 10,000 people, but they have now moved to Masceti Beach.

 

From ranked third in previous review, in 2010 Bali got score 99.65 of Indonesia's environmental quality index and the highest of all the 33 provinces. The score measured 3 water quality parameters: the level of total suspended solids (TSS), dissolved oxygen (DO) and chemical oxygen demand (COD).

 

Because of over-exploitation by the tourist industry which covers a massive land area, 200 out of 400 rivers on the island have dried up and based on research, the southern part of Bali would face a water shortage up to 2,500 litres of clean water per second by 2015. To ease the shortage, the central government plans to build a water catchment and processing facility at Petanu River in Gianyar. The 300 litres capacity of water per second will be channelled to Denpasar, Badung and Gianyar in 2013.

 

ECONOMY

Three decades ago, the Balinese economy was largely agriculture-based in terms of both output and employment. Tourism is now the largest single industry in terms of income, and as a result, Bali is one of Indonesia's wealthiest regions. In 2003, around 80% of Bali's economy was tourism related. By end of June 2011, non-performing loan of all banks in Bali were 2.23%, lower than the average of Indonesian banking industry non-performing loan (about 5%). The economy, however, suffered significantly as a result of the terrorist bombings 2002 and 2005. The tourism industry has since recovered from these events.

 

AGRICULTURE

Although tourism produces the GDP's largest output, agriculture is still the island's biggest employer; most notably rice cultivation. Crops grown in smaller amounts include fruit, vegetables, Coffea arabica and other cash and subsistence crops. Fishing also provides a significant number of jobs. Bali is also famous for its artisans who produce a vast array of handicrafts, including batik and ikat cloth and clothing, wooden carvings, stone carvings, painted art and silverware. Notably, individual villages typically adopt a single product, such as wind chimes or wooden furniture.

 

The Arabica coffee production region is the highland region of Kintamani near Mount Batur. Generally, Balinese coffee is processed using the wet method. This results in a sweet, soft coffee with good consistency. Typical flavours include lemon and other citrus notes. Many coffee farmers in Kintamani are members of a traditional farming system called Subak Abian, which is based on the Hindu philosophy of "Tri Hita Karana". According to this philosophy, the three causes of happiness are good relations with God, other people and the environment. The Subak Abian system is ideally suited to the production of fair trade and organic coffee production. Arabica coffee from Kintamani is the first product in Indonesia to request a Geographical Indication.

 

TOURISM

The tourism industry is primarily focused in the south, while significant in the other parts of the island as well. The main tourist locations are the town of Kuta (with its beach), and its outer suburbs of Legian and Seminyak (which were once independent townships), the east coast town of Sanur (once the only tourist hub), in the center of the island Ubud, to the south of the Ngurah Rai International Airport, Jimbaran, and the newer development of Nusa Dua and Pecatu.

 

The American government lifted its travel warnings in 2008. The Australian government issued an advice on Friday, 4 May 2012. The overall level of the advice was lowered to 'Exercise a high degree of caution'. The Swedish government issued a new warning on Sunday, 10 June 2012 because of one more tourist who was killed by methanol poisoning. Australia last issued an advice on Monday, 5 January 2015 due to new terrorist threats.

 

An offshoot of tourism is the growing real estate industry. Bali real estate has been rapidly developing in the main tourist areas of Kuta, Legian, Seminyak and Oberoi. Most recently, high-end 5 star projects are under development on the Bukit peninsula, on the south side of the island. Million dollar villas are being developed along the cliff sides of south Bali, commanding panoramic ocean views. Foreign and domestic (many Jakarta individuals and companies are fairly active) investment into other areas of the island also continues to grow. Land prices, despite the worldwide economic crisis, have remained stable.

 

In the last half of 2008, Indonesia's currency had dropped approximately 30% against the US dollar, providing many overseas visitors value for their currencies. Visitor arrivals for 2009 were forecast to drop 8% (which would be higher than 2007 levels), due to the worldwide economic crisis which has also affected the global tourist industry, but not due to any travel warnings.

 

Bali's tourism economy survived the terrorist bombings of 2002 and 2005, and the tourism industry has in fact slowly recovered and surpassed its pre-terrorist bombing levels; the longterm trend has been a steady increase of visitor arrivals. In 2010, Bali received 2.57 million foreign tourists, which surpassed the target of 2.0–2.3 million tourists. The average occupancy of starred hotels achieved 65%, so the island is still able to accommodate tourists for some years without any addition of new rooms/hotels, although at the peak season some of them are fully booked.

 

Bali received the Best Island award from Travel and Leisure in 2010. The island of Bali won because of its attractive surroundings (both mountain and coastal areas), diverse tourist attractions, excellent international and local restaurants, and the friendliness of the local people. According to BBC Travel released in 2011, Bali is one of the World's Best Islands, ranking second after Santorini, Greece.

 

In August 2010, the film Eat Pray Love was released in theatres. The movie was based on Elizabeth Gilbert's best-selling memoir Eat, Pray, Love. It took place at Ubud and Padang-Padang Beach at Bali. The 2006 book, which spent 57 weeks at the No. 1 spot on the New York Times paperback nonfiction best-seller list, had already fuelled a boom in Eat, Pray, Love-related tourism in Ubud, the hill town and cultural and tourist center that was the focus of Gilbert's quest for balance through traditional spirituality and healing that leads to love.

 

In January 2016, after music icon David Bowie died, it was revealed that in his will, Bowie asked for his ashes to be scattered in Bali, conforming to Buddhist rituals. He had visited and performed in a number of Southest Asian cities early in his career, including Bangkok and Singapore.

 

Since 2011, China has displaced Japan as the second-largest supplier of tourists to Bali, while Australia still tops the list. Chinese tourists increased by 17% from last year due to the impact of ACFTA and new direct flights to Bali. In January 2012, Chinese tourists year on year (yoy) increased by 222.18% compared to January 2011, while Japanese tourists declined by 23.54% yoy.

 

Bali reported that it has 2.88 million foreign tourists and 5 million domestic tourists in 2012, marginally surpassing the expectations of 2.8 million foreign tourists. Forecasts for 2013 are at 3.1 million.

 

Based on Bank Indonesia survey in May 2013, 34.39 percent of tourists are upper-middle class with spending between $1,286 to $5,592 and dominated by Australia, France, China, Germany and the US with some China tourists move from low spending before to higher spending currently. While 30.26 percent are middle class with spending between $662 to $1,285.

 

SEX TOURISM

In the twentieth century the incidence of tourism specifically for sex was regularly observed in the era of mass tourism in Indonesia In Bali, prostitution is conducted by both men and women. Bali in particular is notorious for its 'Kuta Cowboys', local gigolos targeting foreign female tourists.

 

Tens of thousands of single women throng the beaches of Bali in Indonesia every year. For decades, young Balinese men have taken advantage of the louche and laid-back atmosphere to find love and lucre from female tourists—Japanese, European and Australian for the most part—who by all accounts seem perfectly happy with the arrangement.

 

By 2013, Indonesia was reportedly the number one destination for Australian child sex tourists, mostly starting in Bali but also travelling to other parts of the country. The problem in Bali was highlighted by Luh Ketut Suryani, head of Psychiatry at Udayana University, as early as 2003. Surayani warned that a low level of awareness of paedophilia in Bali had made it the target of international paedophile organisations. On 19 February 2013, government officials announced measures to combat paedophilia in Bali.

 

TRANSPORTATION

The Ngurah Rai International Airport is located near Jimbaran, on the isthmus at the southernmost part of the island. Lt.Col. Wisnu Airfield is found in north-west Bali.

 

A coastal road circles the island, and three major two-lane arteries cross the central mountains at passes reaching to 1,750m in height (at Penelokan). The Ngurah Rai Bypass is a four-lane expressway that partly encircles Denpasar. Bali has no railway lines.

 

In December 2010 the Government of Indonesia invited investors to build a new Tanah Ampo Cruise Terminal at Karangasem, Bali with a projected worth of $30 million. On 17 July 2011 the first cruise ship (Sun Princess) anchored about 400 meters away from the wharf of Tanah Ampo harbour. The current pier is only 154 meters but will eventually be extended to 300–350 meters to accommodate international cruise ships. The harbour here is safer than the existing facility at Benoa and has a scenic backdrop of east Bali mountains and green rice fields. The tender for improvement was subject to delays, and as of July 2013 the situation remained unclear with cruise line operators complaining and even refusing to use the existing facility at Tanah Ampo.

 

A Memorandum of Understanding has been signed by two ministers, Bali's Governor and Indonesian Train Company to build 565 kilometres of railway along the coast around the island. As of July 2015, no details of this proposed railways have been released.

 

On 16 March 2011 (Tanjung) Benoa port received the "Best Port Welcome 2010" award from London's "Dream World Cruise Destination" magazine. Government plans to expand the role of Benoa port as export-import port to boost Bali's trade and industry sector. The Tourism and Creative Economy Ministry has confirmed that 306 cruise liners are heading for Indonesia in 2013 – an increase of 43 percent compared to the previous year.

 

In May 2011, an integrated Areal Traffic Control System (ATCS) was implemented to reduce traffic jams at four crossing points: Ngurah Rai statue, Dewa Ruci Kuta crossing, Jimbaran crossing and Sanur crossing. ATCS is an integrated system connecting all traffic lights, CCTVs and other traffic signals with a monitoring office at the police headquarters. It has successfully been implemented in other ASEAN countries and will be implemented at other crossings in Bali.

 

On 21 December 2011 construction started on the Nusa Dua-Benoa-Ngurah Rai International Airport toll road which will also provide a special lane for motorcycles. This has been done by seven state-owned enterprises led by PT Jasa Marga with 60% of shares. PT Jasa Marga Bali Tol will construct the 9.91 kilometres toll road (totally 12.7 kilometres with access road). The construction is estimated to cost Rp.2.49 trillion ($273.9 million). The project goes through 2 kilometres of mangrove forest and through 2.3 kilometres of beach, both within 5.4 hectares area. The elevated toll road is built over the mangrove forest on 18,000 concrete pillars which occupied 2 hectares of mangroves forest. It compensated by new planting of 300,000 mangrove trees along the road. On 21 December 2011 the Dewa Ruci 450 meters underpass has also started on the busy Dewa Ruci junction near Bali Kuta Galeria with an estimated cost of Rp136 billion ($14.9 million) from the state budget. On 23 September 2013, the Bali Mandara Toll Road is opened and the Dewa Ruci Junction (Simpang Siur) underpass is opened before. Both are ease the heavy traffic congestion.

 

To solve chronic traffic problems, the province will also build a toll road connecting Serangan with Tohpati, a toll road connecting Kuta, Denpasar and Tohpati and a flyover connecting Kuta and Ngurah Rai Airport.

 

DEMOGRAPHICS

The population of Bali was 3,890,757 as of the 2010 Census; the latest estimate (for January 2014) is 4,225,384. There are an estimated 30,000 expatriates living in Bali.

 

ETHNIC ORIGINS

A DNA study in 2005 by Karafet et al. found that 12% of Balinese Y-chromosomes are of likely Indian origin, while 84% are of likely Austronesian origin, and 2% of likely Melanesian origin. The study does not correlate the DNA samples to the Balinese caste system.

 

CASTE SYSTEM

Bali has a caste system based on the Indian Hindu model, with four castes:

 

- Sudra (Shudra) – peasants constituting close to 93% of Bali's population.

- Wesia (Vaishyas) – the caste of merchants and administrative officials

- Ksatrias (Kshatriyas) – the kingly and warrior caste

- Brahmana (Bramhin) – holy men and priests

 

RELIGION

Unlike most of Muslim-majority Indonesia, about 83.5% of Bali's population adheres to Balinese Hinduism, formed as a combination of existing local beliefs and Hindu influences from mainland Southeast Asia and South Asia. Minority religions include Islam (13.3%), Christianity (1.7%), and Buddhism (0.5%). These figures do not include immigrants from other parts of Indonesia.

 

Balinese Hinduism is an amalgam in which gods and demigods are worshipped together with Buddhist heroes, the spirits of ancestors, indigenous agricultural deities and sacred places. Religion as it is practised in Bali is a composite belief system that embraces not only theology, philosophy, and mythology, but ancestor worship, animism and magic. It pervades nearly every aspect of traditional life. Caste is observed, though less strictly than in India. With an estimated 20,000 puras (temples) and shrines, Bali is known as the "Island of a Thousand Puras", or "Island of the Gods". This is refer to Mahabarata story that behind Bali became island of god or "pulau dewata" in Indonesian language.

 

Balinese Hinduism has roots in Indian Hinduism and Buddhism, and adopted the animistic traditions of the indigenous people. This influence strengthened the belief that the gods and goddesses are present in all things. Every element of nature, therefore, possesses its own power, which reflects the power of the gods. A rock, tree, dagger, or woven cloth is a potential home for spirits whose energy can be directed for good or evil. Balinese Hinduism is deeply interwoven with art and ritual. Ritualizing states of self-control are a notable feature of religious expression among the people, who for this reason have become famous for their graceful and decorous behaviour.

 

Apart from the majority of Balinese Hindus, there also exist Chinese immigrants whose traditions have melded with that of the locals. As a result, these Sino-Balinese not only embrace their original religion, which is a mixture of Buddhism, Christianity, Taoism and Confucianism, but also find a way to harmonise it with the local traditions. Hence, it is not uncommon to find local Sino-Balinese during the local temple's odalan. Moreover, Balinese Hindu priests are invited to perform rites alongside a Chinese priest in the event of the death of a Sino-Balinese. Nevertheless, the Sino-Balinese claim to embrace Buddhism for administrative purposes, such as their Identity Cards.

 

LANGUAGE

Balinese and Indonesian are the most widely spoken languages in Bali, and the vast majority of Balinese people are bilingual or trilingual. The most common spoken language around the tourist areas is Indonesian, as many people in the tourist sector are not solely Balinese, but migrants from Java, Lombok, Sumatra, and other parts of Indonesia. There are several indigenous Balinese languages, but most Balinese can also use the most widely spoken option: modern common Balinese. The usage of different Balinese languages was traditionally determined by the Balinese caste system and by clan membership, but this tradition is diminishing. Kawi and Sanskrit are also commonly used by some Hindu priests in Bali, for Hinduism literature was mostly written in Sanskrit.

 

English and Chinese are the next most common languages (and the primary foreign languages) of many Balinese, owing to the requirements of the tourism industry, as well as the English-speaking community and huge Chinese-Indonesian population. Other foreign languages, such as Japanese, Korean, French, Russian or German are often used in multilingual signs for foreign tourists.

 

CULTURE

Bali is renowned for its diverse and sophisticated art forms, such as painting, sculpture, woodcarving, handcrafts, and performing arts. Balinese cuisine is also distinctive. Balinese percussion orchestra music, known as gamelan, is highly developed and varied. Balinese performing arts often portray stories from Hindu epics such as the Ramayana but with heavy Balinese influence. Famous Balinese dances include pendet, legong, baris, topeng, barong, gong keybar, and kecak (the monkey dance). Bali boasts one of the most diverse and innovative performing arts cultures in the world, with paid performances at thousands of temple festivals, private ceremonies, or public shows.

 

The Hindu New Year, Nyepi, is celebrated in the spring by a day of silence. On this day everyone stays at home and tourists are encouraged to remain in their hotels. On the day before New Year, large and colourful sculptures of ogoh-ogoh monsters are paraded and finally burned in the evening to drive away evil spirits. Other festivals throughout the year are specified by the Balinese pawukon calendrical system.

 

Celebrations are held for many occasions such as a tooth-filing (coming-of-age ritual), cremation or odalan (temple festival). One of the most important concepts that Balinese ceremonies have in common is that of désa kala patra, which refers to how ritual performances must be appropriate in both the specific and general social context. Many of the ceremonial art forms such as wayang kulit and topeng are highly improvisatory, providing flexibility for the performer to adapt the performance to the current situation. Many celebrations call for a loud, boisterous atmosphere with lots of activity and the resulting aesthetic, ramé, is distinctively Balinese. Often two or more gamelan ensembles will be performing well within earshot, and sometimes compete with each other to be heard. Likewise, the audience members talk amongst themselves, get up and walk around, or even cheer on the performance, which adds to the many layers of activity and the liveliness typical of ramé.

 

Kaja and kelod are the Balinese equivalents of North and South, which refer to ones orientation between the island's largest mountain Gunung Agung (kaja), and the sea (kelod). In addition to spatial orientation, kaja and kelod have the connotation of good and evil; gods and ancestors are believed to live on the mountain whereas demons live in the sea. Buildings such as temples and residential homes are spatially oriented by having the most sacred spaces closest to the mountain and the unclean places nearest to the sea.

 

Most temples have an inner courtyard and an outer courtyard which are arranged with the inner courtyard furthest kaja. These spaces serve as performance venues since most Balinese rituals are accompanied by any combination of music, dance and drama. The performances that take place in the inner courtyard are classified as wali, the most sacred rituals which are offerings exclusively for the gods, while the outer courtyard is where bebali ceremonies are held, which are intended for gods and people. Lastly, performances meant solely for the entertainment of humans take place outside the walls of the temple and are called bali-balihan. This three-tiered system of classification was standardised in 1971 by a committee of Balinese officials and artists to better protect the sanctity of the oldest and most sacred Balinese rituals from being performed for a paying audience.

 

Tourism, Bali's chief industry, has provided the island with a foreign audience that is eager to pay for entertainment, thus creating new performance opportunities and more demand for performers. The impact of tourism is controversial since before it became integrated into the economy, the Balinese performing arts did not exist as a capitalist venture, and were not performed for entertainment outside of their respective ritual context. Since the 1930s sacred rituals such as the barong dance have been performed both in their original contexts, as well as exclusively for paying tourists. This has led to new versions of many of these performances which have developed according to the preferences of foreign audiences; some villages have a barong mask specifically for non-ritual performances as well as an older mask which is only used for sacred performances.

 

Balinese society continues to revolve around each family's ancestral village, to which the cycle of life and religion is closely tied. Coercive aspects of traditional society, such as customary law sanctions imposed by traditional authorities such as village councils (including "kasepekang", or shunning) have risen in importance as a consequence of the democratisation and decentralisation of Indonesia since 1998.

 

WIKIPEDIA

Includes three working doors (Rear, both back side), working lightbar, opening hatch, opening gunports and more.

 

At Pevensey Castle

 

Pevensey Castle: a Saxon Shore fort, Norman defences, a medieval enclosure castle, and later associated remains

The monument includes Anderita Saxon Shore fort, traces of later, Norman defences, an enclosure castle, a 16th century gun emplacement and World War II defences situated on a low spur of sand and clay which now lies around 2km north west of the present East Sussex coastline at Pevensey. During the Roman and medieval periods the spur formed a peninsula projecting into a tidal lagoon and marshland, but coastal deposition and land reclamation have gradually built up the ground around it so that it is now completely land-locked. The roughly oval, north east-south west aligned Roman fort is the earliest of the structures which make up the monument and has been dated to the first half of the fourth century AD. Covering almost 4ha, the fort survives in the form of substantial ruins and buried remains. It is enclosed by a massive defensive wall with a flint and sandstone rubble core faced by coursed greensand and ironstone blocks, interspersed with red tile bonding courses. The whole is up to 3.7m thick and survives to a height of up to 8.1m. The wall was originally topped by a wall walk and parapet. Part excavation in 1906-8 showed that the wall was constructed on footings of rammed chalk and flints underpinned by oak piles and held together by a framework of wooden beams. Investigation of the internal face indicated that this was stepped upwards from a wide base so as to provide extra strength and support. Despite these precautions, a landslip on the south eastern side of the fort has resulted in the destruction of a c.180m length of the perimeter walls and, although fragments of the fallen masonry do survive, most have been removed over the years. Smaller sections of wall have also collapsed along the north western and eastern stretches. The defensive strength provided by the perimeter wall was enhanced by irregularly-spaced, externally projecting semicircular bastions with diameters of around 5m. There were originally at least 15 of these, of which 10 survive today. The fort was entered from its south western, landward approach by way of the main gateway. In front of this a protective ditch 5.5m wide was dug, and, although this became infilled over the years, a 40m stretch located towards its south eastern end has been recut and exposed. The ditch would have been spanned originally by a wooden bridge, although this no longer survives. The main gateway takes the form of a rectangular gatehouse set back between two solid semicircular bastions 8m apart. The 2.7m wide, originally arched entrance is flanked by two oblong guardrooms and the whole gateway structure projects beyond the inner face of the perimeter wall into the fort and is thought to have been originally two or even three storeys high. On the eastern side of the fort is a more simply designed subsidiary gateway, originally a 3m wide archway entrance, giving access to part of the adjacent Roman harbour, now overlain by Pevensey village. The extant archway is a modern reconstruction of the Norman rebuilding of the original entrance. Traces of a wooden causeway which led from it into the fort have been found during partial excavation. Midway along the north western stretch of perimeter wall is a now ruined postern c.2m wide, approached by a curved passage set within the wall. Part excavation between 1906-1908 indicated that the internal buildings which housed the garrison of up to 1,000 men, along with their livestock and supplies, were constructed of timber infilled with wattle and daub. A c.1m sq timber-lined Roman well was found in the south western sector of the fort, at the bottom of which were the remains of the wooden bucket with rope still attached. The well was found to have been filled with rubbish in Roman times and the presence of the bones of cattle, sheep, red deer, wild boar, wild birds, domestic dogs and cats, along with sea shells, gives some indication of the diet and lifestyle of the fort's original inhabitants. Anderita is thought to have been abandoned by its garrison by the latter half of the 4th century AD, and although little is known of its subsequent history until the 11th century, the Anglo-Saxon Chronicle records a massacre of Britons by the invading Saxons at the fort in AD 491. The Bayeux Tapestry states that William the Conquerer landed at Pevensey in 1066, and the Norman army are believed to have made use of the Roman fort as one of their first armed camps. The defences at Pevensey and the surrounding land were granted to King William's half-brother Robert, Count of Mortain. The medieval defences then went through at least 300 years of development, culminating in the construction of a stone built enclosure castle within the largely intact walls of the earlier Roman fort. It is thought that the first Norman defences took the form of a wooden palisade surrounded by a bank and ditch, and a c.40m length of partially infilled ditch up to 9m wide which survives across the north eastern sector of the earlier fort may indicate their original extent. Limited excavations in 1993-94 showed that the ground surface in the south eastern sector of the fort, in the vicinity of the later stone-built keep, was artificially raised some time before 1200, suggesting that a motte may also have been constructed. The original Roman gateways were rebuilt and a new ditch dug in front of the south western gate. Most of the Norman defences and interior wooden buildings will now survive in buried form beneath the later medieval castle, although herringbone-pattern repairs to the Roman masonry, by then serving as the outer bailey of the medieval defences, also date from this time. Around 1100 the defences were strengthened and the accommodation improved by the addition of a masonry keep in the south eastern sector of the earlier fort. The subject of a complex history of alteration, collapse and repair, the keep utilises part of the earlier, Roman perimeter wall and bastions. It takes the form of a rectangular block measuring c.16.8m by c.9m internally, reinforced by apsidal projections on all sides. Now surviving in ruined form up to first floor level, the keep originally took the form of a tall tower with an entrance on the first floor. A rectangular building measuring 7.6m by 6m was later constructed in the south eastern angle between the keep and the Roman wall. At around 1200 work began on the construction of a smaller, stone-built inner bailey in the south eastern sector of the earlier fort. An L-shaped ditch around 20m wide was dug to define the new enclosure, and this retains water in its northern arm. The material excavated from the ditch and from the destruction of the earlier bank was spread over much of the outer bailey to a depth of up to 1.5m. The ditch was recut during extensive renovations carried out during the early 20th century. The first structure to be built in this phase was the gatehouse to the south west which has an arched entrance between twin, semicircular external towers, now ruined. The basement chambers beneath each tower have ashlar-faced walls and barrel-vaulted ceilings, the southern chamber being entered by way of a newel staircase, the northern by a trapdoor. Both were used to house prisoners. Many subsequent alterations included the replacement, during the 15th century, of the wooden bridge over the outer ditch by a stone causeway. The originally embattled curtain wall enclosing the inner bailey was built within the ditch and inner berm around 1250. This survives almost to its full original height and is faced with coursed Greensand ashlar. Three semicircular external towers provided flanking cover from the narrow embrasures which pierce their walls. Each has a narrow staircase to a basement, a branch staircase off it into the ditch and a room and garderobe, or latrine, at ground floor level. Upper rooms were entered by way of the wall walk and were heated by fireplaces. The basement of the northernmost tower has two rib-vaulted bays, the keeled ribs resting on stiff-leaf corbels. The interior castle buildings continued to be built mainly of wood and these will survive in buried form, although the stone foundations of a chapel were exposed during partial excavation of the northern sector of the inner bailey. Around 20m south east of the chapel is a large stone-lined well at least 15.5m deep, and near this is a pile of medieval stone missile-balls, a selection of those recovered from the ditch. These were thrown from trebuchets during the four sieges of the castle. William, Count of Mortain forfeited Pevensey after an unsuccessful rebellion against Henry I in 1101 and the castle, which remained in the royal gift until the later Middle Ages, passed into the hands of the de Aquila family. The most famous siege took place in 1264-65 when the supporters of Henry III, fleeing from their defeat by the Barons at Lewes, took refuge in the castle. In 1372 the castle was given to John of Gaunt, and during his period of office was used to imprison James I, King of Scotland, who had been seized in 1406, and Joan, Queen of Navarre, accused of witchcraft by her stepson, Henry V. By 1300, the sea had gradually begun to recede from around the castle and its military importance declined as a result. Contemporary records show that the castle walls were constantly in need of expensive repair and by the end of the 14th century were not being properly maintained, although the roof leads were kept intact until the middle of the 15th century. By 1500 the castle had ceased to be inhabited and fell rapidly into decay. The threat of the Spanish Armada led to some renewed interest in the defensive value of the site, and a survey of 1587 records that the castle housed two demi-culverins, or heavy guns. These were sited on the contemporary, south east orientated, M-shaped earthen gun emplacement situated in the outer bailey around 90m north east of the main Roman gateway. This takes the form of a raised level platform c.20m long bounded on the seaward side by a slight bank c.0.4m high and around 3m wide. One of the cast iron guns, manufactured in the East Sussex Weald, is now housed within the inner bailey on a modern replica carriage. From the 17th century the castle passed through the hands of various private owners. Valued as a picturesque ruin during the 18th and 19th centuries, it features in many contemporary engravings and illustrations. In 1925 the Duke of Devonshire presented the monument to the state, and extensive repairs began with a view to opening the monument to the public. These were interrupted by the outbreak of World War II, when the castle resumed its original military purpose of protecting the south coast. The castle was refortified in May 1940 as an observation and command post. It was continuously occupied by regular troops, including Canadian forces and the United States Army Air Corps, who used it as a radio direction centre, and by the Home Guard until 1944. The World War II defences include two pillboxes and three machine gun posts of concrete faced with rubble and flints, carefully concealed and camouflaged within the earlier Roman and medieval fabric. An internal tower was built just to the south of the Roman east gateway and a blockhouse housing anti-tank weapons was built in front of the main Roman gateway. The blockhouse no longer survives. Modifications carried out to the medieval mural towers included lining the interiors with brick and inserting wooden floors. In 1945 the monument was returned to peaceful use and is now in the guardianship of the Secretary of State and open to the public.

[Historic England]

The Lake District, also known as the Lakes or Lakeland, is a mountainous region and national park in Cumbria, North West England. It is primarily famous for the Cumbrian Mountains, its lake and coastal scenery, and for its literary associations with William Wordsworth and other Lake Poets, Beatrix Potter, and John Ruskin.

 

The Cumbrian mountains, or fells, include England's tallest mountains: Scafell Pike (978 m (3,209 ft)), Helvellyn (950 m (3,120 ft)), Skiddaw (931 m (3,054 ft)), and Cross Fell (893 m (2,930 ft)), which all have a topographical prominence of more than 600m. The region contains sixteen major lakes. They include Windermere, which with a length of 18 km (11 miles) and an area of 14.73 km2 (5.69 square miles) is both the longest and largest lake in England, and Wast Water, which at 79 metres (259 ft) is the deepest lake in England.

 

The Lake District National Park was established in 1951, and covers an area of 2,362 km2 (912 square miles), the bulk of the region. It was designated a UNESCO World Heritage Site in 2017.

 

National Park

The Lake District National Park includes all of the central Lake District, though the town of Kendal, some coastal areas, and the Lakeland Peninsulas are outside the park boundary. The area was designated a national park on 9 May 1951, a month after the Peak District, the first UK national park. It retained its original boundaries until 2016 when it was extended by 3% in the direction of the Yorkshire Dales National Park to incorporate areas land of high landscape value around the Lune Valley.

 

The national park received 18.14 million tourist visitors in 2022. This equates to 29.15 million tourist days, counting visits of greater than three hours. It is the largest of the thirteen national parks in England and Wales and the second largest in the UK after the Cairngorms National Park. Its aim is to protect the landscape by restricting unwelcome change by industry or commerce. The area of the national park, with the exception of the 2016 extension, was designated a World Heritage Site in 2017 as a cultural landscape. This was the fourth attempt to list the park, after two attempts in the 1980s and one in 2012 failed.

 

The park is governed by the National Park Authority, which is based at offices in Kendal. It runs a visitor centre on Windermere at a former country house called Brockhole, Coniston Boating Centre, and Information Centres. The Park Authority has 20 members: six appointed by Westmorland and Furness Council, four by Cumberland Council, and ten by the Secretary of State for Environment, Food, and Rural Affairs.

 

Human geography

The precise extent of the Lake District was not defined traditionally, but is slightly larger than that of the National Park[citation needed], the total area of which is about 2,362 square kilometres (912 sq mi). The park extends just over 51 kilometres (32 mi) from east to west and nearly 64 kilometres (40 mi) from north to south, with areas such as the Lake District Peninsulas to the south lying outside the National Park.

 

Settlement

There are only a few major settlements within this mountainous area: the towns of Keswick, Windermere, Ambleside, and Bowness-on-Windermere are the four largest. Significant settlements close to the boundary of the national park include Carlisle, Barrow-in-Furness, Kendal, Ulverston, Dalton-in-Furness, Whitehaven, Workington, Cockermouth, Penrith, Millom and Grange-over-Sands; each of these has important economic links with the area. Other villages are Coniston, Threlkeld, Glenridding, Pooley Bridge, Broughton-in-Furness, Grasmere, Newby Bridge, Staveley, Lindale, Gosforth and Hawkshead. The economies of almost all are intimately linked with tourism. Beyond these are a scattering of hamlets and many isolated farmsteads, some of which are still tied to agriculture;[citation needed] others now function as part of the tourist economy.

 

Communications

Roads

The Lake District is very nearly contained within a box of trunk routes and major A roads. It is flanked to the east by the A6 road, which runs from Kendal to Penrith (though the National Park extension approved in 2015 is east of the A6); across its southern fringes by the A590, which connects the M6 to Barrow-in-Furness, and the A5092, and across its northern edge by the A66 trunk road between Penrith and Workington. The A595 (linking the A66 with the A5092) forms the park boundary from Calder Bridge to Holmrook, then crosses the coastal plain of the park until turning inland at the Whicham Valley, forming much of the park boundary again until joining the A5092 at Grizebeck.

 

Besides these, a few A roads penetrate the area itself, notably the A591 which runs north-westwards from Kendal to Windermere and then on to Keswick. It continues up the east side of Bassenthwaite Lake. "The A591, Grasmere, Lake District" was short-listed in the 2011 Google Street View awards in the Most Romantic Street category. The A593 and A5084 link the Ambleside and Coniston areas with the A590 to the south whilst the A592 and A5074 similarly link Windermere with the A590. The A592 also continues northwards from Windermere to Ullswater and Penrith by way of the Kirkstone Pass.

 

Some valleys which are not penetrated by A roads are served by B roads. The B5289 serves Lorton Vale and Buttermere and links via the Honister Pass with Borrowdale. The B5292 ascends the Whinlatter Pass from Lorton Vale before dropping down to Braithwaite near Keswick. The B5322 serves the valley of St John's in the Vale whilst Great Langdale is served by the B5343. Other valleys such as Little Langdale, Eskdale and Dunnerdale are served by minor roads. The last of these is connected with the first two by the Wrynose and Hardknott passes respectively; both of these passes are known for their steep gradients and are together one of the most popular climbs in the United Kingdom for cycling enthusiasts. A minor road through the Newlands Valley connects via Newlands Hause with the B5289 at Buttermere. Wasdale is served by a cul-de-sac minor road,[a] as is Longsleddale and the valleys at Haweswater and Kentmere. There are networks of minor roads in the lower-lying southern part of the area, connecting numerous communities between Kendal, Windermere, and Coniston.

 

Railways and ferries

The West Coast Main Line skirts the eastern edge of the Lake District and the Cumbrian Coast Line passes through the southern and western fringes of the area. A single railway line, the Windermere Branch Line, penetrates from Kendal to Windermere via Staveley. Railways once served Broughton-in-Furness and Coniston (closed to passengers in 1958) and another ran from Penrith to Cockermouth via Keswick (closed west of Keswick in 1966 and completely in 1972). Part of the track of the latter is used by the improved A66 trunk road.

 

The Cumbrian Coast line has three stations within the boundaries of the national park (and additionally Drigg, about a third of a mile from the park boundary). The line gives railway enthusiasts and others a flavour of a pre-Beeching railway line, with features like manually operated level crossing gates, as well as giving a good connection to the steam railway into Eskdale and providing access for cyclists and serious walkers to the Western Fells.

 

The narrow gauge Ravenglass and Eskdale Railway runs from Ravenglass on the west coast up Eskdale as far as Dalegarth Station near the hamlet of Boot, catering for tourists. Another heritage railway, the Lakeside and Haverthwaite Railway, runs between Lake Windermere and Haverthwaite, and tourists can connect at Lakeside with the boats up the lake to Bowness.

 

A vehicle-carrying cable ferry, the Windermere Ferry, runs frequent services across Windermere. There are also seasonal passenger boats on Coniston Water, Derwent Water, and Ullswater.

 

Footpaths and bridleways

There are many paths over which the public has a right of way, all of which are signposted at their origin on public roads and at some other points. Within the area of the National Park in 2012 there were 2,159 km (1,342 mi) of public footpaths, 875 km (544 mi) of public bridleways, 15 km (9 mi) of restricted byways and 30 km (19 mi) of byways open to all traffic. There is also a general "right to roam" in open country, which includes approximately 50% of the national park.

 

Many of these tracks arose centuries ago and were used either as ridge highways (such as along High Street) or as passes for travelling across the ridges between settlements in the valleys. Historically these paths were not planned for reaching summits, but more recently they are used by fell walkers for that purpose. The Coast to Coast Walk, which crosses the north of England from the Irish Sea to the North Sea, traverses the national park from west to east.

 

Bridleways are intended for horse riding and walkers, with cyclists also permitted to use them. Cyclists must give way to all other bridleway users. Motor vehicles are only allowed on "byways open to all traffic" (green lanes) but in practice Traffic Regulation Orders have been brought in on several prohibiting motor traffic, although a system of permits operates on Gatesgarth Pass.

 

Land ownership

Most of the land within the national park is in private ownership, with about 55% registered as agricultural land. Landowners include:

 

Individual farmers and other private landowners, with more than half of the agricultural land farmed by the owners.

The National Trust owns around 25% of the total area (including some lakes and land of significant landscape value).

The Forestry Commission and other investors in forests and woodland.

United Utilities (owns 8%)

Lake District National Park Authority (owns 3.9%)

 

Physical geography

The Lake District is a roughly circular upland massif, deeply dissected by a broadly radial pattern of major valleys which are largely the result of repeated glaciations over the last 2 million years. The apparent radial pattern is not from a central dome, but from an axial watershed extending from St Bees Head in the west to Shap in the east. Most of these valleys display the U-shaped cross-section characteristic of glacial origin and often contain long narrow lakes in bedrock hollows, with tracts of relatively flat ground at their infilled heads, or where they are divided by lateral tributaries (Buttermere-Crummock Water; Derwent Water-Bassenthwaite Lake).[b] Smaller lakes known as tarns occupy glacial cirques at higher elevations. It is the abundance of both which has led to the area becoming known as the Lake District.

 

Many of the higher fells are rocky, while moorland predominates lower down. Vegetation cover in better-drained areas includes bracken and heather, although much of the land is boggy, due to the high rainfall. Deciduous native woodland occurs on many of the steeper slopes below the tree line, but with native oak supplemented by extensive conifer plantations in many areas, particularly Grizedale Forest in the generally lower southern part of the area. The Lake District extends to the sea to the west and south.

 

The highest mountain in England, Scafell Pike (978m/3210'), has a far-reaching view on a clear day, ranging from the Galloway Hills of Scotland, the Mourne Mountains in Northern Ireland, the Isle of Man, and Snowdonia in Wales.

 

Cumbrian Mountains

Lake District is located in the Lake DistrictScafell PikeScafell PikeScafellScafellScafellScafellHelvellynHelvellynSkiddawSkiddawHigh StreetHigh StreetGrasmoorGrasmoorConiston Old ManConiston Old ManGreat GableGreat GableKendalKendalPenrithPenrithKeswickKeswickAmblesideAmblesideCockermouthCockermouthWindermereWindermereGrasmereGrasmere

 

Major fells and towns shown within the National Park

Lake District

The mountains (or 'fells') of the Lake District are known as the "Cumbrian Mountains", "Cumbrian Fells" or "Lakeland Fells". The four highest fells exceed 3,000 feet (914 m). These are:

 

Scafell Pike, 978 m (3,209 ft)

Scafell, 965 m (3,166 ft)

Helvellyn, 951 m (3,120 ft)

Skiddaw, 931 m (3,054 ft)

 

Northern Fells

The Northern Fells are a clearly defined range of hills contained within a 13 km (8 mi) diameter circle between Keswick in the southwest and Caldbeck in the northeast. They culminate in the 931 m (3,054 ft) peak of Skiddaw. Other notable peaks are Blencathra (also known as Saddleback) (868 m (2,848 ft)) and Carrock Fell. Bassenthwaite Lake occupies the valley between this massif and the North Western Fells.

 

North Western Fells

The North Western Fells lie between Borrowdale and Bassenthwaite Lake to the east and Buttermere and Lorton Vale to the west. Their southernmost point is at Honister Pass. This area includes the Derwent Fells above the Newlands Valley and hills to the north amongst which are Dale Head, Robinson. To the north stand Grasmoor, highest in the range at 852 m (2,795 ft), Grisedale Pike and the hills around the valley of Coledale, and in the far northwest is Thornthwaite Forest and Lord's Seat. The fells in this area are rounded Skiddaw slate, with few tarns and relatively few rock faces.

 

Western Fells

The Western Fells lie between Buttermere and Wasdale, with Sty Head forming the apex of a large triangle. Ennerdale bisects the area, which consists of the High Stile ridge north of Ennerdale, the Loweswater Fells in the far northwest, the Pillar group in the southwest, and Great Gable (899 m (2,949 ft)) near Sty Head. Other tops include Seatallan, Haystacks and Kirk Fell. This area is craggy and steep, with the impressive pinnacle of Pillar Rock its showpiece. Wastwater, located in this part, is England's deepest lake.

 

Central Fells

The Central Fells are lower in elevation than surrounding areas of fell, peaking at 762 m (2,500 ft) at High Raise. They take the form of a ridge running between Derwent Water in the west and Thirlmere in the east, from Keswick in the north to Langdale Pikes in the south. A spur extends southeast to Loughrigg Fell above Ambleside. The central ridge running north over High Seat is exceptionally boggy.

 

Eastern Fells

The Eastern Fells consist of a long north-to-south ridge, the Helvellyn range, running from Clough Head to Seat Sandal with the 950 m (3,118 ft) Helvellyn at its highest point. The western slopes of these summits tend to be grassy, with rocky corries and crags on the eastern side. The Fairfield group lies to the south of the range and forms a similar pattern with towering rock faces and hidden valleys spilling into the Patterdale valley. It culminates in the height of Red Screes overlooking the Kirkstone Pass.

 

Far Eastern Fells

The Far Eastern Fells refers to all of the Lakeland fells to the east of Ullswater and the A592 road running south to Windermere. At 828 m (2,717 ft), the peak known as High Street is the highest point on a complex ridge that runs broadly north-south and overlooks the hidden valley of Haweswater to its east. In the north of this region are the lower fells of Martindale Common and Bampton Common whilst in the south are the fells overlooking the Kentmere valley. Further to the east, beyond Mardale and Longsleddale is Shap Fell, an extensive area consisting of high moorland, more rolling and Pennine in nature than the mountains to the west.

 

Southern Fells

The Southern Fells occupy the southwestern quarter of the Lake District. They can be regarded as comprising a northern grouping between Wasdale, Eskdale, and the two Langdale valleys, a southeastern group east of Dunnerdale and south of Little Langdale, and a southwestern group bounded by Eskdale to the north and Dunnerdale to the east.

 

The first group includes England's highest mountains: Scafell Pike in the centre, at 978 m (3,209 ft) and Scafell one mile (1.6 km) to the southwest. Though it is slightly lower, Scafell has a 700 ft (210 m) rockface, Scafell Crag, on its northern side. This group also includes the Wastwater Screes overlooking Wasdale, the Glaramara ridge overlooking Borrowdale, the three tops of Crinkle Crags, Bowfell and Esk Pike. The core of the area is drained by the infant River Esk. Collectively these are some of the Lake District's most rugged hillsides.

 

The second group, otherwise known as the Furness Fells or Coniston Fells, have as their northern boundary the steep and narrow Hardknott and Wrynose passes. The highest are Old Man of Coniston and Swirl How which slightly exceed 800 m (2,600 ft).

 

The third group to the west of the Duddon includes Harter Fell and the long ridge leading over Whitfell to Black Combe and the sea. The south of this region consists of lower forests and knolls, with Kirkby Moor on the southern boundary. The southwestern Lake District ends near the Furness peninsula and Barrow-in-Furness, a town which many Lake District residents rely on for basic amenities.

 

Southeastern area

The southeastern area is the territory between Coniston Water and Windermere and east of Windermere towards Kendal and south to Lindale. There are no high summits in this area which are mainly low hills, knolls and limestone cuestas such as Gummer's How and Whitbarrow. Indeed, it rises only as high as 333 m (1,093 ft) at Top o' Selside east of Coniston Water; the wide expanse of Grizedale Forest stands between the two lakes. Kendal and Morecambe Bay stand at the eastern and southern edges of the area.

 

Valleys

The main radial valleys are (clockwise from the south) Dunnerdale, Eskdale, Wasdale, Ennerdale, the Vale of Lorton, and Buttermere valley, the Derwent Valley and Borrowdale, the Ullswater valley, Haweswater valley, Longsleddale, the Kentmere valley, those converging on the head of Windermere - Grasmere, Great Langdale and Little Langdale, and the Coniston Water valley. The valleys break the mountains up into blocks, which have been described by various authors in different ways. The most frequently encountered approach is that made popular by Alfred Wainwright who published seven separate area guides to the Lakeland Fells.

 

Only one of the lakes in the Lake District is called by that name, Bassenthwaite Lake. All the others such as Windermere, Coniston Water, Ullswater and Buttermere are meres, tarns and waters, with mere being the least common and water being the most common. The major lakes and reservoirs in the National Park are given below.

 

Bassenthwaite Lake

Brotherswater

Buttermere

Coniston Water

Crummock Water

Derwent Water

Devoke Water

Elter Water

Ennerdale Water

Esthwaite Water

Grasmere

Haweswater Reservoir

Hayeswater

Loweswater

Rydal Water

Thirlmere

Ullswater

Wast Water

Windermere

 

Woodlands

Below the tree line are wooded areas, including British and European native oak woodlands and introduced softwood plantations. The woodlands provide habitats for native English wildlife. The native red squirrel is found in the Lake District and a few other parts of England. In parts of the Lake District, the rainfall is higher than in any other part of England. This gives Atlantic mosses, ferns, lichen, and liverworts the chance to grow. There is some ancient woodland in the National Park. Management of the woodlands varies: some are coppiced, some pollarded, some left to grow naturally, and some provide grazing and shelter.

 

Coast

The Lake District extends to the coast of the Irish Sea from Drigg in the north to Silecroft in the south, encompassing the estuaries of the Esk and its tributaries, the Irt and the Mite. The intertidal zone of the combined estuaries includes sand, shingle and mudflats, and saltmarsh. The dune systems on either side of the estuary are protected as nature reserves; Drigg Dunes and Gullery to the north and Eskmeals Dunes[31] to the south. South of the estuary, the coast is formed in low cliffs of glacial till, sands, and gravels.

 

The district also extends to the tidal waters of Morecambe Bay and several of its estuaries alongside the Furness and Cartmel Peninsulas, designated on M6 motorway signposts as the "Lake District Peninsulas", and the southern portions of which lie outside the park. These are the Duddon Estuary, the Leven Estuary, and the western banks and tidal flats of the Kent Estuary. These areas are each characterised by sand and mudflats of scenic and wildlife interest. The coast is backed by extensive flats of raised marine deposits left when the relative sea level was higher.

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

 

The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater. Due to the Yellowstone Plateau's high elevation the average boiling temperature at Yellowstone's geyser basins is 199 °F (93 °C). When properly confined and close to the surface it can periodically release some of the built-up pressure in eruptions of hot water and steam that can reach up to 390 feet (120 m) into the air (see Steamboat Geyser, the world's tallest geyser). Water erupting from Yellowstone's geysers is superheated above that boiling point to an average of 204 °F (95.5 °C) as it leaves the vent. The water cools significantly while airborne and is no longer scalding hot by the time it strikes the ground, nearby boardwalks, or even spectators. Because of the high temperatures of the water in the features it is important that spectators remain on the boardwalks and designated trails. Several deaths have occurred in the park as a result of falls into hot springs.

 

Prehistoric Native American artifacts have been found at Mammoth Hot Springs and other geothermal areas in Yellowstone. Some accounts state that the early people used hot water from the geothermal features for bathing and cooking. In the 19th century Father Pierre-Jean De Smet reported that natives he interviewed thought that geyser eruptions were "the result of combat between the infernal spirits". The Lewis and Clark Expedition traveled north of the Yellowstone area in 1806. Local natives that they came upon seldom dared to enter what we now know is the caldera because of frequent loud noises that sounded like thunder and the belief that the spirits that possessed the area did not like human intrusion into their realm. The first white man known to travel into the caldera and see the geothermal features was John Colter, who had left the Lewis and Clark Expedition. He described what he saw as "hot spring brimstone". Beaver trapper Joseph Meek recounted in 1830 that the steam rising from the various geyser basins reminded him of smoke coming from industrial smokestacks on a cold winter morning in Pittsburgh, Pennsylvania. In the 1850s famed trapper Jim Bridger called it "the place where Hell bubbled up".

 

The heat that drives geothermal activity in the Yellowstone area comes from brine (salty water) that is 1.5–3 miles (7,900–15,800 ft; 2,400–4,800 m) below the surface. This is actually below the solid volcanic rock and sediment that extends to a depth of 3,000 to 6,000 feet (900 to 1,800 m) and is inside the hot but mostly solid part of the pluton that contains Yellowstone's magma chamber. At that depth the brine is superheated to temperatures that exceed 400 °F (204 °C) but is able to remain a liquid because it is under great pressure (like a huge pressure cooker).

 

Convection of the churning brine and conduction from surrounding rock transfers heat to an overlaying layer of fresh groundwater. Movement of the two liquids is facilitated by the highly fractured and porous nature of the rocks under the Yellowstone Plateau. Some silica is dissolved from the fractured rhyolite into the hot water as it travels through the fractured rock. Part of this hard mineral is later redeposited on the walls of the cracks and fissures to make a nearly pressure-tight system. Silica precipitates at the surface to form either geyserite or sinter, creating the massive geyser cones, the scalloped edges of hot springs, and the seemingly barren landscape of geyser basins.

 

There are at least five types of geothermal features found at Yellowstone:

 

Fumaroles: Fumaroles, or steam vents, are the hottest hydrothermal features in the park. They have so little water that it all flashes into steam before reaching the surface. At places like Roaring Mountain, the result is loud hissing of steam and gases.

Geysers: Geysers such as Old Faithful are a type of geothermal feature that periodically erupt scalding hot water. Increased pressure exerted by the enormous weight of the overlying rock and water prevents deeper water from boiling. As the hot water rises it is under less pressure and steam bubbles form. They, in turn, expand on their ascent until the bubbles are too big and numerous to pass freely through constrictions. At a critical point the confined bubbles actually lift the water above, causing the geyser to splash or overflow. This decreases the pressure of the system and violent boiling results. Large quantities of water flash into tremendous amounts of steam that force a jet of water out of the vent: an eruption begins. Water (and heat) is expelled faster than the geyser's recharge rate, gradually decreasing the system's pressure and eventually ending the eruption.

Hot springs: Hot springs such as Grand Prismatic Spring are the most common hydrothermal features in the park. Their plumbing has no constrictions. Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below. This circulation, called convection, prevents water from reaching the temperature needed to set off an eruption. Many hot springs give rise to streams of heated water.

Mudpots: Mudpots such as Fountain Paint Pots are acidic hot springs with a limited water supply. Some microorganisms use hydrogen sulfide (rotten egg smell), which rises from deep within the earth, as an energy source. They convert the gas into sulfuric acid, which breaks down rock into clay.

Travertine terraces: Travertine terraces, found at Mammoth Hot Springs, are formed from limestone (a rock type made of calcium carbonate). Thermal waters rise through the limestone, carrying high amounts of dissolved carbonate. Carbon dioxide is released at the surface and calcium carbonate deposited as travertine, the chalky white rock of the terraces. These features constantly and quickly change due to the rapid rate of deposition.

Geyser basins

 

The Norris Geyser Basin 44°43′43″N 110°42′16″W is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago.

 

The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters.

 

The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

 

Algae on left bacteria on right at the intersection of flows from the Constant & Whirlgig Geysers at Norris Geyser Basin

The tallest active geyser in the world, Steamboat Geyser,[11] is located in Norris Basin. Unlike the slightly smaller but much more famous Old Faithful Geyser located in Upper Geyser Basin, Steamboat has an erratic and lengthy timetable between major eruptions. During major eruptions, which may be separated by intervals of more than a year (the longest recorded span between major eruptions was 50 years), Steamboat erupts over 300 feet (90 m) into the air. Steamboat does not lie dormant between eruptions, instead displaying minor eruptions of approximately 40 feet (12 m).

 

Norris Geyser Basin periodically undergoes a large-scale, basin-wide thermal disturbance lasting a few weeks. Water levels fluctuate, and temperatures, pH, colors, and eruptive patterns change throughout the basin. During a disturbance in 1985, Porkchop Geyser continually jetted steam and water; in 1989, the same geyser apparently clogged with silica and blew up, throwing rocks more than 200 feet (61 m). In 2003 a park ranger observed it bubbling heavily, the first such activity seen since 1991. Activity increased dramatically in mid-2003. Because of high ground temperatures and new features beside the trail much of Back Basin was closed until October. In 2004 the boardwalk was routed around the dangerous area and now leads behind Porkchop Geyser.

 

North of Norris, Roaring Mountain is a large, acidic hydrothermal area (solfatara) with many fumaroles. In the late 19th and early 20th centuries, the number, size, and power of the fumaroles were much greater than today. The fumaroles are most easily seen in the cooler, low-light conditions of morning and evening.

 

The Gibbon Geyser Basin 44°41′58″N 110°44′34″W includes several thermal areas in the vicinity of the Gibbon River between Gibbon Falls and Norris. The most accessible feature in the basin is Beryl Spring, with a small boardwalk right along the Grand Loop Road. Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots.

 

The Monument Geyser Basin 44°41′03″N 110°45′14″W has no active geysers, but its 'monuments' are siliceous sinter deposits similar to the siliceous spires discovered on the floor of Yellowstone Lake. Scientists hypothesize that this basin's structures formed from a hot water system in a glacially dammed lake during the waning stages of the Pinedale Glaciation. The basin is on a ridge reached by a very steep one-mile (1.6 km) trail south of Artists' Paint Pots. Other areas of thermal activity in Gibbon Geyser Basin lie off-trail.

 

South of Norris along the rim of the caldera is the Upper Geyser Basin 44°27′52″N 110°49′45″W, which has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet (430 m) northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin.

 

The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

 

Evidence of glacial activity is common, and it is one of the keys that allows geysers to exist. Glacier till deposits underlie the geyser basins providing storage areas for the water used in eruptions. Many landforms, such as Porcupine Hills north of Fountain Flats, are made up of glacial gravel and are reminders that 70,000 to 14,000 years ago, this area was buried under ice.

 

Signs of the forces of erosion can be seen everywhere, from runoff channels carved across the sinter in the geyser basins to the drainage created by the Firehole River. Mountain building is evident on the drive south of Old Faithful, toward Craig Pass. Here the Rocky Mountains reach a height of 8,262 feet (2,518 m), dividing the country into two distinct watersheds.

 

Midway Geyser Basin 44°31′04″N 110°49′56″W is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot-wide (60 by 90 m) Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot-wide (110 m) and 121-foot-deep (37 m) Grand Prismatic Spring is found here. Also in the basin is Turquoise Pool and Opal Pool.

 

Lower Geyser Basin

Blue spring with steam rising from it; irregular blotches of red and orange residue are on the banks, along with dead tree trunks.

Silex Spring at Fountain Paint Pot

 

Farther north is the Lower Geyser Basin 44°32′58″N 110°50′09″W, which is the largest geyser basin in area, covering approximately 11 square miles. Due to its large size, it has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also there is Firehole Spring, Celestine Pool, Leather Pool, Red Spouter, Jelly spring, and a number of fumaroles.

 

Geysers in Lower Geyser Basin include Great Fountain Geyser, whose eruptions reach 100 to 200 feet (30–61 m) in the air, while waves of water cascade down its sinter terraces., the Fountain group of Geysers (Clepsydra Geyser which erupts nearly continuously to heights of 45 feet (14 m), Fountain Geyser, Jelly Geyser, Jet Geyser, Morning Geyser, and Spasm Geyser), the Pink Cone group of geysers (Dilemma Geyser, Labial Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser), the White Dome group of geysers (Crack Geyser, Gemini Geyser, Pebble Geyser, Rejuvenated Geyser, and White Dome Geyser), as well as Sizzler Geyser.

 

Clepsydra Geyser erupting. July 2019

Fountain Paint Pots

White Dome Geyser

West Thumb Geyser Basin

Several pools of blue water in ashen rock basin.

West Thumb Geyser Basin

Blackened basin with orange streaks; steam is rising from it with fir trees in the background.

Overflow areas of Silex springs

 

The West Thumb Geyser Basin 44°25′07″N 110°34′23″W, including Potts Basin to the north, is the largest geyser basin on the shores of Yellowstone Lake. The heat source of the thermal features in this location is thought to be relatively close to the surface, only 10,000 feet (3,000 m) down. West Thumb is about the same size as another famous volcanic caldera, Crater Lake in Oregon, but much smaller than the great Yellowstone Caldera which last erupted about 640,000 years ago. West Thumb is a caldera within a caldera.

 

West Thumb was created approximately 162,000 years ago when a magma chamber bulged up under the surface of the earth and subsequently cracked it along ring fracture zones. This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today.

 

The thermal features at West Thumb are not only found on the lake shore, but extend under the surface of the lake as well. Several underwater hydrothermal features were discovered in the early 1990s and can be seen as slick spots or slight bulges in the summer. During the winter, the underwater thermal features are visible as melt holes in the icy surface of the lake. The surrounding ice can reach three feet (one yard) in thickness.

 

Perhaps the most famous hydrothermal feature at West Thumb is a geyser on the lake shore known as Fishing Cone. Walter Trumbull of the 1870 Washburn-Langford-Doane Expedition described a unique event while a man was fishing adjacent to the cone: "...in swinging a trout ashore, it accidentally got off the hook and fell into the spring. For a moment it darted about with wonderful rapidity, as if seeking an outlet. Then it came to the top, dead, and literally boiled." Fishing Cone erupted frequently to the height of 40 feet (12 m) in 1919 and to lesser heights in 1939. One fisherman was badly burned in Fishing Cone in 1921. Fishing at the geyser is now prohibited.

 

Early visitors would arrive at West Thumb via stagecoach from the Old Faithful area. They had a choice of continuing on the stagecoach or boarding the steamship Zillah to continue the journey by water to Lake Hotel. The boat dock was located near the south end of the geyser basin near Lakeside Spring.

 

Backcountry Geyser Basins

The Heart Lake 44°18′00″N 110°30′56″W, Lone Star 44°24′50″N 110°49′04″W, and Shoshone Geyser Basins 44°21′16″N 110°47′57″W are located away from the road and require at least several miles of hiking to reach. These areas lack the boardwalks and other safety features of the developed areas. As falling into geothermal features can be fatal, it is usually advisable to visit these areas with an experienced guide or at the very least, travelers need to ensure they remain on well-marked trails.

 

The Heart Lake Geyser Basin contains several groups of geysers and deep blue hot springs near Heart Lake in the south-central portion of Yellowstone, southeast of most of the main geyser basins. Lying in the Snake River watershed east of Lewis Lake and south of Yellowstone Lake, Heart Lake was named sometime before 1871 for Hart Hunney, a hunter. Other explorers in the region incorrectly assumed that the lake's name was spelled 'heart' because of its shape. The Heart Lake Geyser Basin begins a couple miles from the lake and descends along Witch Creek to the lakeshore. Five groups of hydrothermal features comprise the basin, and all of them contain geysers, although some are dormant.

 

Between Shoshone Lake and Old Faithful is the Lone Star Geyser Basin, of which the primary feature is Lone Star Geyser, named for its isolation from the nearby geysers of the Upper Geyser Basin. The basin is reachable on foot or bicycle via a 3 mile road that is closed to vehicles.

 

The Shoshone Geyser Basin, reached by hiking or by boat, contains one of the highest concentrations of geysers in the world – more than 80 in an area 1,600 by 800 feet (490 by 240 m). Hot springs and mudpots dot the landscape between the geyser basin and Shoshone Lake.

 

Hot Spring Basin is located 15 miles (24 km) north-northeast of Fishing Bridge and has one of Yellowstone's largest collections of hot springs and fumaroles. The geothermal features there release large amounts of sulfur. This makes water from the springs so acidic that it has dissolved holes in the pants of people who sit on wet ground and causes mounds of sulfur three feet (1 m) high to develop around fumaroles. The very hot acidic water and steam have also created voids in the ground that are only covered by a thin crust.

 

Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.

 

The thermal features at Mud Volcano and Sulphur Caldron are primarily mud pots and fumaroles because the area is situated on a perched water system with little water available. Fumaroles or "steam vents" occur when the ground water boils away faster than it can be recharged. Also, the vapors are rich in sulfuric acid that leaches the rock, breaking it down into clay. Because no water washes away the acid or leached rock, it remains as sticky clay to form a mud pot. Hydrogen sulfide gas is present deep in the earth at Mud Volcano and is oxidized to sulfuric acid by microbial activity, which dissolves the surface soils to create pools and cones of clay and mud. Along with hydrogen sulfide, steam, carbon dioxide, and other gases explode through the layers of mud.

 

A series of shallow earthquakes associated with the volcanic activity in Yellowstone struck this area in 1978. Soil temperatures increased to nearly 200 °F (93 °C). The slope between Sizzling Basin and Mud Geyser, once covered with green grass and trees, became a barren landscape of fallen trees known as "the cooking hillside".

 

Yellowstone National Park is a national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion.

 

While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park originally fell under the jurisdiction of the U.S. Department of the Interior, the first Secretary of the Interior to supervise the park being Columbus Delano. However, the U.S. Army was eventually commissioned to oversee the management of Yellowstone for 30 years between 1886 and 1916. In 1917, the administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than a thousand archaeological sites.

 

Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km2), comprising lakes, canyons, rivers, and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent. The caldera is considered a dormant volcano. It has erupted with tremendous force several times in the last two million years. Well over half of the world's geysers and hydrothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly intact ecosystem in the Earth's northern temperate zone. In 1978, Yellowstone was named a UNESCO World Heritage Site.

 

Hundreds of species of mammals, birds, fish, reptiles, and amphibians have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the contiguous United States. Grizzly bears, cougars, wolves, and free-ranging herds of bison and elk live in this park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one-third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing, and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

 

Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY-ID Micropolitan Statistical Area.

 

Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake).

 

Wyoming is a state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.

 

Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.

 

Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.

 

Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.

 

Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights". It is among the least religious states in the country, and is known for having a political culture that leans towards libertarian conservatism. The Republican presidential nominee has carried the state in every election since 1968.

Nice light up on the South Downs above Steyning this evening

Includes inflatable ego and breasts.

Also includes SLNCR trains and the 2 services (1 passenger, 1 goods) each way on the line to Claremorris and Limerick

From the paddock at the 76th Members' Meeting, Goodwood.

This artisan fairy house is handpainted and the exterior includes pebbles, pine cone bits, acorns, real crushed roses and lavender, handmade clay flowers, and many layers of moss. Many!

 

Scale is 1" = 1' on house and all furnishings and accessories. The house footprint is approximately 17" x 17" and height is approximately 20". The house includes a lazy susan base for easy rotating and play.

 

The fairy house includes real operable windows and doors and a fish pond with 3 goldfish residing. The exterior lighting is all LED and constructed and hand painted to look like candles. LED lights are used for longevity and safety and the exterior lights all run off of one switch that uses a watch battery.

 

The rooftop garden includes clay flowers and vegetables, a garden hose and tools, real acorns, crushed flowers, moss, aspen bark and a couple of little mouse visitors.

 

Exterior furnishings include everything you see in the photos: garden accessories, bird bath with "water", handmade chairs and bench, rabbit hutch, mailbox, bunnies and snoozing kitty.

 

The interior furniture is all custom made by me and includes: desk and chair set, dining table and chairs set, fireplace, bed, toilet plus all accessories you see in the photos. Each furniture set has its own LED lighting and switch for ease when you want to reorganize your fairy house.

 

The desk and chair feature two candle lights, plus a handmade acorn "banker's" lamp that really works. The desk displays an assortment of books, newspaper, pencils and a notepad.

 

The dining table and chair has two candle lights and two dining chairs.

 

The fireplace includes a handmade acorn oil lamp that really works, plus two candle lights and a fire light. The fireplace displays many fairy treasures including some peppermint sticks, a gerbil home with two gerbils, copper pots, a wine and cheese board, bottle of wine, copper utensils, brass fireplace tools and a stack of logs.

 

The bed was lovingly created using willow and aspen sticks, burlap, real moss, crushed flowers, acorns and gingham fabric. The bed features 2 candle lights plus a handmade acorn reading lamp that really works. The bookshelf above the bed includes lots of reading material, a postcard and some canned goods :).

 

The fairy toilet has real "water" inside and features two candle lights, books and toilet paper (with an xtra roll).

 

This fairy house and furnishings are intended for an older child or adult collector due to lots of small parts.

 

Thanks for looking!

 

Tori

Includes teams from O'Gorman, Yankton, Pierre T.F. Riggs, Huron. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.

©2021 SDPB

 

INCLUDES 4 COLOURS

200 LINDEN <3

 

13/02/16 #1139. Cold and very grey down at Shoreham Beach this afternoon, but at least the morning's heavy rain had cleared through. A long exposure "big stopper" shot

From a quick look at the RNLI Selsey Lifeboat Station, after meeting up with some of the 365 gang at North Mundham. A bit more cloud motion would have given this "big stopper" shot a boost

Frosty this morning with a touch of mist around the steaming waters of the River Adur. The wooden decking of the Old Tollbridge gets incredibly slippery in such conditions.

The head office of this agency is articulated through modular elements, glass partitions and integrated furniture. The facilities include offices, classrooms, workshops and a multipurpose hall.

    

Read more:

www.aqso.net/projects/1211lsb

    

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Las oficinas de esta agencia se articulan a través de elementos modulares, particiones de vidrio y mobiliario integrado. Las instalaciones albergan despachos, aulas, espacio para talleres de trabajo y una sala polivalente.

    

Leer más:

www.aqso.es/proyectos/1211lsb

Includes Wakefields new Enviro200s and Leeds Park & Ride

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