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Zion National Park is an American national park located in southwestern Utah near the town of Springdale. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River.

 

Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Ancestral Puebloans (who used to be called Anasazi by early non-indigenous archeologists)(c. 300 CE). Subsequently, what has been called the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s.

 

In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park's name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." On November 19, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. Congress designated 85% of the park a wilderness area in 2009.

 

The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago.

 

As stated in the foundation document:

 

The purpose of Zion National Park is to preserve the dramatic geology including Zion Canyon and a labyrinth of deep and brilliantly colored Navajo sandstone canyons formed by extraordinary processes of erosion at the margin of the Colorado Plateau; to safeguard the park's wilderness character and its wild and scenic river values; to protect evidence of human history; and to provide for scientific research and the enjoyment and enlightenment of the public.

 

The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40.

 

The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m).

 

Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America.

 

The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round.

 

The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at US 89 at Mount Carmel Junction. Park features on the east side of the park include Checkerboard Mesa and The East Temple.

 

The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features Tucupit Point and one of the world's longest natural arches, Kolob Arch.

 

Other notable geographic features of Zion Canyon include Angels Landing, The Great White Throne, the Court of the Patriarchs, The Sentinel, The West Temple, Towers of the Virgin, the Altar of Sacrifice, The Watchman, Weeping Rock, and the Emerald Pools.

 

Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March.

 

Archaeologists have divided the long span of Zion's human history into three cultural periods: the Archaic, Protohistoric and Historic periods. Each period is characterized by distinctive technological and social adaptations.

 

Archaic period

The first human presence in the region dates to 8,000 years ago when family groups camped where they could hunt or collect plants and seeds. About 2,000 years ago, some groups began growing corn and other crops, leading to an increasingly sedentary lifestyle. Later groups in this period built permanent villages called pueblos. Archaeologists call this the Archaic period and it lasted until c. 500. Baskets, cordage nets, and yucca fiber sandals have been found and dated to this period. The Archaic toolkits included flaked stone knives, drills, and stemmed dart points. The dart points were attached to wooden shafts and propelled by throwing devices called atlatls.

 

By c. 300, some of the archaic groups developed into an early branch of seminomadic Anasazi, the Basketmakers. Basketmaker sites have grass- or stone-lined storage cists and shallow, partially underground dwellings called pithouses. They were hunters and gatherers who supplemented their diet with limited agriculture. Locally collected pine nuts were important for food and trade.

 

Both the Virgin Anasazi and the Parowan Fremont disappeared from the archaeological record of southwestern Utah by c. 1300. Extended droughts in the 11th and 12th centuries, interspersed with catastrophic flooding, may have made horticulture impossible in this arid region.

 

Tradition and archaeological evidence hold that their replacements were Numic-speaking cousins of the Virgin Anasazi, such as the Southern Paiute and Ute. The newcomers migrated on a seasonal basis up and down valleys in search of wild seeds and game animals. Some, particularly the Southern Paiute, also planted fields of corn, sunflowers, and squash to supplement their diet. These more sedentary groups made brownware vessels that were used for storage and cooking.

 

The Historic period begins in the late 18th century with the exploration of southern Utah by padre Silvestre Vélez de Escalante and padre Francisco Atanasio Domínguez. The padres passed near what is now the Kolob Canyons Visitor Center on October 13, 1776, becoming the first people of European descent known to visit the area. In 1825, trapper and trader Jedediah Smith explored some of the downstream areas while under contract with the American Fur Company.

 

In 1847, Mormon farmers from the Salt Lake area became the first people of European descent to settle the Virgin River region. In 1851, the Parowan and Cedar City areas were settled by Mormons who used the Kolob Canyons area for timber, and for grazing cattle, sheep, and horses. They prospected for mineral deposits, and diverted Kolob water to irrigate crops in the valley below. Mormon settlers named the area Kolob which in Mormon scripture is the heavenly place nearest the residence of God.

 

Settlements had expanded 30 miles (48 km) south to the lower Virgin River by 1858. That year, a Southern Paiute guide led young Mormon missionary and interpreter Nephi Johnson into the upper Virgin River area and Zion Canyon.[28] Johnson wrote a favorable report about the agricultural potential of the upper Virgin River basin, and returned later that year to found the town of Virgin. In 1861 or 1862, Joseph Black made the arduous journey to Zion Canyon and was very impressed by its beauty.

 

The floor of Zion Canyon was settled in 1863 by Isaac Behunin, who farmed corn, tobacco, and fruit trees. The Behunin family lived in Zion Canyon near the site of today's Zion Lodge during the summer, and wintered in Springdale. Behunin is credited with naming Zion, a reference to the place of peace mentioned in the Bible. Two more families settled Zion Canyon in the next couple of years, bringing with them cattle and other domesticated animals. The canyon floor was farmed until Zion became a Monument in 1909.

 

The Powell Geographic Expedition of 1869 entered the area after their first trip through the Grand Canyon. John Wesley Powell visited Zion Canyon in 1872 and named it Mukuntuweap, under the impression that that was the Paiute name. Powell Survey photographers John K. Hillers and James Fennemore first visited the Zion Canyon and Kolob Plateau region in the spring of 1872. Hillers returned in April 1873 to add more photographs to the "Virgin River Series" of photographs and stereographs. Hillers described wading the canyon for four days and nearly freezing to death to take his photographs.

 

Paintings of the canyon by Frederick S. Dellenbaugh were exhibited at the Saint Louis World's Fair in 1904, followed by a favorable article in Scribner's Magazine the next year. The article and paintings, along with previously created photographs, paintings, and reports, led to President William Howard Taft's proclamation on July 31, 1909, that created Mukuntuweap National Monument. In 1917, the acting director of the newly created National Park Service visited the canyon and proposed changing its name from the locally unpopular Mukuntuweap to Zion, a name used by the local Mormon community. The United States Congress added more land and established Zion National Park on November 19, 1919. A separate Zion National Monument, the Kolob Canyons area, was proclaimed on January 22, 1937, and was incorporated into the park on July 11, 1956.

 

Travel to the area before it was a national park was rare due to its remote location, lack of accommodations, and the absence of real roads in southern Utah. Old wagon roads were upgraded to the first automobile roads starting about 1910, and the road into Zion Canyon was built in 1917 leading to the Grotto, short of the present road that now ends at the Temple of Sinawava.

 

Touring cars could reach Zion Canyon by the summer of 1917. The first visitor lodging in Zion Canyon, called Wylie Camp, was established that same year as a tent camp. The Utah Parks Company, a subsidiary of the Union Pacific Railroad, acquired Wylie Camp in 1923, and offered ten-day rail/bus tours to Zion, nearby Bryce Canyon, the Kaibab Plateau, and the North Rim of the Grand Canyon. The Zion Lodge complex was built in 1925 at the site of the Wylie tent camp. Architect Gilbert Stanley Underwood designed the Zion Lodge in a rustic architectural style, while the Utah Parks Company funded the construction.

 

Work on the Zion Mount Carmel Highway started in 1927 to enable reliable access between Springdale and the east side of the park. The road opened in 1930 and park visit and travel in the area greatly increased. The most famous feature of the Zion – Mount Carmel Highway is its 1.1-mile (1.8 km) tunnel, which has six large windows cut through the massive sandstone cliff.

 

In 1896, local rancher John Winder improved the Native American footpath up Echo Canyon, which later became the East Rim Trail. Entrepreneur David Flanigan used this trail in 1900 to build cableworks that lowered lumber into Zion Canyon from Cable Mountain. More than 200,000 board feet (470 m3) of lumber were lowered by 1906. The auto road was extended to the Temple of Sinawava, and a trail built from there 1 mile (1.6 km) to the start of the Narrows. Angel's Landing Trail was constructed in 1926 and two suspension bridges were built over the Virgin River. Other trails were constructed by the Civilian Conservation Corps during the 1930s.

 

Zion National Park has been featured in numerous films, including The Deadwood Coach (1924), Arizona Bound (1927), Nevada (1927), Ramrod (1947) and Butch Cassidy and the Sundance Kid (1969).

 

Zion Canyon Scenic Drive provides access to Zion Canyon. Traffic congestion in the narrow canyon was recognized as a major problem in the 1990s and a public transportation system using propane-powered shuttle buses was instituted in the year 2000. As part of its shuttle fleet, Zion has two electric trams each holding up to 36 passengers. Usually from early April through late October, the scenic drive in Zion Canyon is closed to private vehicles and visitors ride the shuttle buses. The National Park Service has contracted the management of the shuttle bus system to transit operator RATP Dev.

 

On April 12, 1995, heavy rains triggered a landslide that blocked the Virgin River in Zion Canyon. Over a period of two hours, the river carved away part of the only exit road from the canyon, trapping 450 guests and employees at the Zion Lodge. A one-lane, temporary road was constructed within 24 hours to allow evacuation of the Lodge. A more stable albeit temporary road was completed on May 25, 1995, to allow summer visitors to access the canyon. This road was replaced with a permanent road during the first half of 1996.

 

The Zion–Mount Carmel Highway can be travelled year-round. Access for oversized vehicles requires a special permit, and is limited to daytime hours, as traffic through the tunnel must be one way to accommodate large vehicles. The 5-mile (8.0 km)-long Kolob Canyons Road was built to provide access to the Kolob Canyons section of the park. This road often closes in the winter.

 

In March 2009, President Barack Obama signed into law the Omnibus Public Land Management Act of 2009, which designated and further protected 124,406 acres (50,345 ha) of park land, about 85% of the park, as the Zion Wilderness.

 

In September 2015, flooding trapped a party of seven in Keyhole Canyon, a slot canyon in the park. The flash flood killed all seven members of the group, whose remains were located after a search lasting several days.

 

In 2017, some scenes from the TV series Extinct were shot in the park.

 

The nine known exposed geologic formations in Zion National Park are part of a super-sequence of rock units called the Grand Staircase. Together, these formations represent about 150 million years of mostly Mesozoic-aged sedimentation in that part of North America. The formations exposed in the Zion area were deposited as sediment in very different environments:

 

The warm, shallow (sometimes advancing or retreating) sea of the Kaibab and Moenkopi formations

Streams, ponds, and lakes of the Chinle, Moenave, and Kayenta formations

The vast desert of the Navajo and Temple Cap formations

The dry near-shore environment of the Carmel Formation

 

Uplift affected the entire region, known as the Colorado Plateaus, by slowly raising these formations more than 10,000 feet (3,000 m) higher than where they were deposited. This steepened the stream gradient of the ancestral Virgin and other rivers on the plateau.

 

The faster-moving streams took advantage of uplift-created joints in the rocks. Eventually, all Cenozoic-aged formations were removed and gorges were cut into the plateaus. Zion Canyon was cut by the North Fork of the Virgin River in this way. During the later part of this process, lava flows and cinder cones covered parts of the area.

 

High water volume in wet seasons does most of the downcutting in the main canyon. These flood events are responsible for transporting most of the 3 million short tons (2.7 million metric tons) of rock and sediment that the Virgin River transports yearly. The Virgin cuts away its canyon faster than its tributaries can cut away their own streambeds, so tributaries end in waterfalls from hanging valleys where they meet the Virgin. The valley between the peaks of the Twin Brothers is a notable example of a hanging valley in the canyon.

 

The Great Basin, Mojave Desert, and Colorado Plateau converge at Zion and the Kolob canyons. This, along with the varied topography of canyon–mesa country, differing soil types, and uneven water availability, provides diverse habitat for the equally diverse mix of plants and animals that live in the area. The park is home to 289 bird, 79 mammals, 28 reptiles, 7 fish, and 6 amphibian species. These organisms make their homes in one or more of four life zones found in the park: desert, riparian, woodland, and coniferous forest.

 

Desert conditions persist on canyon bottoms and rocky ledges away from perennial streams. Sagebrush, prickly pear cactus, and rabbitbrush, along with sacred datura and Indian paintbrush, are common. Utah penstemon and golden aster can also be found. Milkvetch and prince's plume are found in pockets of selenium-rich soils.

 

Common daytime animals include mule deer, rock squirrels, pinyon jays, and whiptail and collared lizards. Desert cottontails, jackrabbits, and Merriam's kangaroo rats come out at night. Cougars, bobcats, coyotes, badgers, gray foxes, and ring-tail cats are the top predators.

 

Cooler conditions persist at mid-elevation slopes, from 3,900 to 5,500 feet (1,200 to 1,700 m). Stunted forests of pinyon pine and juniper coexist here with manzanita shrubs, cliffrose, serviceberry, scrub oak, and yucca. Stands of ponderosa pine, Gambel oak, manzanita and aspen populate the mesas and cliffs above 6,000 feet (1,800 m).

 

Golden eagles, red-tailed hawks, peregrine falcons, and white-throated swifts can be seen in the area. Desert bighorn sheep were reintroduced in the park in 1973. California condors were reintroduced in the Arizona Strip and in 2014 the first successful breeding of condors in the park was confirmed. Nineteen species of bat also live in the area.

 

Boxelder, Fremont cottonwood, maple, and willow dominate riparian plant communities. Animals such as bank beavers, flannel-mouth suckers, gnatcatchers, dippers, canyon wrens, the virgin spinedace, and water striders all make their homes in the riparian zones.

 

Activities

Rangers at the visitor centers in Zion Canyon and Kolob Canyons can help visitors plan their stay. Guided horseback riding trips, nature walks, and evening programs are available from late March to early November. The Junior Ranger Program for children ages 4 and up is active year-round at the Nature Center, Human History Museum, and the visitor centers.[65] A bookstore attached to the Zion Canyon visitor center offers books, maps, and souvenirs. The Grotto in Zion Canyon, the visitor center, and the viewpoint at the end of Kolob Canyons Road have the only designated picnic sites.

 

Seven trails with round-trip times of half an hour (Weeping Rock) to 4 hours (Angels Landing) are found in Zion Canyon. Two popular trails, Taylor Creek (4 hours round trip) and Kolob Arch (8 hours round trip), are in the Kolob Canyons section of the park, near Cedar City. Hiking up into The Narrows from the Temple of Sinawava is popular in summer, but hiking beyond Big Springs requires a permit. The entire Narrows from Chamberlain's Ranch is a 16-mile one way trip that typically takes 12 hours of strenuous hiking. A shorter alternative is to enter the Narrows via Orderville Canyon. Both Orderville and the full Narrows require a back country permit. Entrance to the Parunuweap Canyon section of the park downstream of Labyrinth Falls is prohibited. Other often-used backcountry trails include the West Rim and LaVerkin Creek. The more primitive sections of Zion include the Kolob Terrace and the Kolob Canyons. A network of trails totaling 50 miles in distance connect Zion's northwest corner of the park (Lee Pass Trailhead) to its southeast section (East Rim Trailhead). Popularly known as the Zion Traverse, the route offers backpackers a diverse experience of the park.

 

Zion is a center for rock climbing, with short walls like Spaceshot, Moonlight Buttress, Prodigal Son, Ashtar Command, and Touchstone being the most popular, highly rated routes.

 

Lodging in the park is available at Zion Lodge, located halfway through Zion Canyon. Just outside the park more lodging is available in Springdale.

 

Zion has three campgrounds: South and Watchman at the far southern side of the park, and a primitive site at Lava Point in the middle of the park off Kolob Terrace Road. Overnight camping in the backcountry requires permits.

 

Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.

 

Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.

 

People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.

 

Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.

 

The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.

 

Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.

 

The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:

 

use of the bow and arrow while hunting,

building pithouse shelters,

growing maize and probably beans and squash,

building above ground granaries of adobe or stone,

creating and decorating low-fired pottery ware,

producing art, including jewelry and rock art such as petroglyphs and pictographs.

 

The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.

 

These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.

 

In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.

 

In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.

 

Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.

 

At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.

 

The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.

 

A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.

 

Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.

 

Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.

 

Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.

 

Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.

 

Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.

 

The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.

 

Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.

 

Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.

 

In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.

 

The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.

 

Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.

 

After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.

 

As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.

 

Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.

 

Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.

 

Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.

 

Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.

 

On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.

 

Main article: Latter Day Saint polygamy in the late-19th century

During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.

 

The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.

 

Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:

 

William Torrington in Carson City (then a part of Utah territory), 1859

Thomas Coleman (Black man) in Salt Lake City, 1866

3 unidentified men at Wahsatch, winter of 1868

A Black man in Uintah, 1869

Charles A. Benson in Logan, 1873

Ah Sing (Chinese man) in Corinne, 1874

Thomas Forrest in St. George, 1880

William Harvey (Black man) in Salt Lake City, 1883

John Murphy in Park City, 1883

George Segal (Japanese man) in Ogden, 1884

Joseph Fisher in Eureka, 1886

Robert Marshall (Black man) in Castle Gate, 1925

Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).

 

Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.

 

Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.

 

During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.

 

In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.

 

Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.

 

Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.

 

As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.

 

One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.

 

It is estimated that 1,450 soldiers from Utah were killed in the war.

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Pelargonium is a genus of flowering plants that includes about 280 species of perennials, succulents, and shrubs, commonly called geraniums, pelargoniums, or storksbills. Geranium is also the botanical name and common name of a separate genus of related plants, also known as cranesbills. Both genera belong to the family Geraniaceae. Carl Linnaeus originally included all the species in one genus, Geranium, and they were later separated into two genera by Charles Louis L'Héritier de Brutelle in 1789.

 

While Geranium species are mostly temperate herbaceous plants, dying down in winter, Pelargonium species are evergreen perennials indigenous to warm temperate and tropical regions of the world, with many species in southern Africa. They are drought and heat tolerant but can tolerate only minor frosts. Some species are extremely popular garden plants, grown as houseplants and bedding plants in temperate regions. They have a long flowering period, with flowers mostly in red, orange, or white, but intensive breeding has produced a huge array of cultivars with great variety in size, flower colour, leaf form and aromatic foliage.

 

Etymology

 

One of hundreds of garden and houseplant cultivars

The name Pelargonium is derived from the Greek πελαργός, pelargós (stork), because the seed head looks like a stork's beak. Dillenius originally suggested the name 'stork', because Geranium was named after a crane — "a πελαργός, ciconia, sicuti vocamus Gerania, γερανός, grus" (from pelargos, stork, as we call the Gerania, geranos, crane).

 

Description

Pelargonium occurs in a large number of growth forms, including herbaceous annuals, shrubs, subshrubs, stem succulents and geophytes. The erect stems bear five-petaled flowers in umbel-like clusters, which are occasionally branched. Because not all flowers appear simultaneously, but open from the centre outwards, this is a form of inflorescence is referred to as pseudoumbels.

 

The flower has a single symmetry plane (zygomorphic), which distinguishes it from the Geranium flower, which has radial symmetry (actinomorphic). Thus the lower three (anterior) petals are differentiated from the upper two (posterior) petals. The posterior sepal is fused with the pedicel to form a hypanthium (nectary tube). The nectary tube varies from only a few millimeters, up to several centimeters, and is an important floral characteristic in morphological classification. Stamens vary from 2 to 7, and their number, position relative to staminodes, and curvature are used to identify individual species. There are five stigmata in the style. For the considerable diversity in flower morphology, see figure 1 of Röschenbleck et al. (2014).

 

Leaves are usually alternate, and palmately lobed or pinnate, often on long stalks, and sometimes with light or dark patterns. The leaves of Pelargonium peltatum (Ivy-leaved Geranium), have a thick cuticle better adapting them for drought tolerance.

 

Taxonomy

 

Dillenius' introduction of the term 'Pelargonium' in Hortus Elthamensis 1732

 

Pelargonium inquinans, (Geranium Afric. arborescens), Hortus Elthamensis

Pelargonium is the second largest genus (after Geranium) within the family Geraniaceae, within which it is sister to the remaining genera of the family in its strict sense, Erodium, Geranium, and Monsonia including Sarcocaulon. The Geraniaceae have a number of genetic features unique amongst angiosperms, including highly rearranged plastid genomes differing in gene content, order and expansion of the inverted repeat.

 

Genus history

The name Pelargonium was first proposed by Dillenius in 1732, who described and illustrated seven species of geraniums from South Africa that are now classified as Pelargonium. Dillenius, who referred to these seven species with apparent unique characteristics as Geranium Africanum (African Geranium) suggested "Possent ergo ii, quibus novi generis cupido est, ea, quorum flores inaequales vel et irrregulares sunt, Pelargonia vocare" (Those who wish a new genus can therefore call those, whose flowers are unequal or irregular, ‘Pelargonia’). The name was then formally introduced by Johannes Burman in 1738. However Carl Linnaeus who first formally described these plants in 1753 did not recognise Pelargonium and grouped together in the same genus (Geranium) the three similar genera Erodium, Geranium, and Pelargonium. Linnaeus' reputation prevented further differentiation for forty years. The eventual distinction between them was made by Charles L’Héritier based on the number of stamens or anthers, seven in the case of Pelargonium. In 1774, P. cordatum, P. crispum, P. quercifolium and P. radula were introduced, followed by P. capitatum in 1790.

 

Circumscription

Pelargonium is distinguished from the other genera in the family Geraniaceae by the presence of a hypanthium, which consists of an adnate nectar spur with one nectary, as well as a generally zygomorphic floral symmetry.

 

Subdivision

De Candolle first proposed dividing the genus into 12 sections in 1824, based on the diversity of growth forms. Traditionally the large number of Pelargonium species have been treated as sixteen sections, based on the classification of Knuth (1912) who described 15 sections, as modified by van der Walt et al. (1977-1997) who added Chorisma, Reniformia and Subsucculentia.

 

These are as follows;

 

section Campylia (Lindley ex Sweet) de Candolle

section Chorisma (Lindley ex Sweet) de Candolle

section Ciconium (Sweet) Harvey

section Cortusina (DC.) Harvey

section Glaucophyllum Harvey

section Hoarea (Sweet) de Candolle

section Isopetalum (Sweet) de Candolle

section Jenkinsonia (Sweet) de Candolle

section Ligularia (Sweet) Harvey

section Myrrhidium de Candolle

section Otidia (Lindley ex Sweet) de Candolle

section Pelargonium (Sweet) Harvey

section Peristera de Candolle

section Polyactium de Candolle

section Reniformia (Knuth) Dreyer

section Subsucculentia J.J.A. van der Walt

Phylogenetic analyses

All subdivision classifications had depended primarily on morphological differences till the era of phylogenetic analyses (Price and Palmer 1993). However phylogenetic analysis shows only three distinct clades, labelled A, B and C. In this analysis not all sections were monophyletic, although some were strongly supported including Chorisma, Myrrhidium and Jenkinsonia, while other sections were more paraphyletic. This in turn has led to a proposal, informal at this stage, of a reformulation of the infrageneric subdivision of Pelargonium.

 

In the proposed scheme of Weng et al. there would be two subgenera, based on clades A+B, and C respectively and seven sections based on subclades. Subsequent analysis with an expanded taxa set confirmed this infrageneric subdivision into two groups which also correspond to chromosome length (<1.5 μ, 1.5-3.0μ), but also two subclades within each major clade, suggesting the presence of four subgenera, these correspond to clades A, B, C1 and C2 of the earlier analysis, A being by far the largest clade with 141 taxa. As before the internal structure of the clades supported monophyly of some sections (Myrrhidium, Chorisma, Reniformia, Pelargonium, Ligularia and Hoarea) but paraphyly in others (Jenkinsonia, Ciconium, Peristera). A distinct clade could be identified within the paraphyletic Polyactium, designated section Magnistipulacea. As a result, Polyactium has been split up to provide this new section, which in itself contains two subsections, Magnistipulacea and Schizopetala, following Knuth's original treatment of Polyactium as having four subsections.

 

Subgenus Pelargonium section Otidia: P. crithmifolium

Thus Röschenbleck et al. (2014) provide a complete revision of the subgeneric classification of Pelargonium based on four subgenera corresponding to their major clades (A, B, C1, C2);

 

subgenus Magnipetala Roeschenbl. & F. Albers Type: Pelargonium praemorsum (Andrews) F Dietrich

subgenus Parvulipetala Roeschenbl. & F. Albers Type: Pelargonium hypoleucum Turczaninow

subgenus Paucisignata Roeschenbl. & F. Albers Type: Pelargonium zonale (L.) L'Hér. in Aiton

subgenus Pelargonium L'Hér. Type: Pelargonium cucullatum (L.) Aiton

Sixteen sections were then assigned to the new subgenera as follows, although many species remained only assigned to subgenera at this stage

 

subgenus Magnipetala 3 sections

section Chorisma (Lindley ex Sweet) de Candolle - 4 species

section Jenkinsonia (Sweet) de Candolle - 11 species

section Myrrhidium de Candolle - 8 species

subgenus Parvulipetala 3 sections

section Isopetalum (Sweet) de Candolle - 1 species (Pelargonium cotyledonis (L.) L'Hér.)

section Peristera de Candolle - 30 species

section Reniformia (Knuth) Dreyer - 8 species

subgenus Paucisignata 2 sections

section Ciconium (Sweet) Harvey - 16 species

section Subsucculentia J.J.A. van der Walt - 3 species

subgenus Pelargonium 8 sections

section Campylia (Lindley ex Sweet) de Candolle - 9 species

section Cortusina (DC.) Harvey - 7 species

section Hoarea (Sweet) de Candolle - 72 species

section Ligularia (Sweet) Harvey - 10 species

section Magnistipulacea Roeschenbl. & F. Albers Type: Pelargonium schlecteri Knuth - 2 subsections

subsection Magnistipulacea Roeschenbl. & F. Albers Type: Pelargonium schlecteri Knuth - 2 species (P. schlecteri & P. luridum)

subsection Schizopetala (Knuth) Roeschenbl. & F. Albers Type: Pelargonium caffrum (Eckl. & Zeyh.) Steudel - 3 species (P. caffrum, P. bowkeri, P. schizopetalum)

section Otidia (Lindley ex Sweet) de Candolle - 14 species

section Pelargonium L'Hér. - 34 species

section Polyactium de Candolle - 2 subsections

subsection Caulescentia Knuth - 1 species (Pelargonium gibbosum)

subsection Polyactium de Candolle - 7 species

Subgenera

Subgenus Magnipetala: Corresponds to clade C1, with 24 species. Perennial to short lived, spreading subshrubs, rarely herbaceous annuals. Petals five, but may be four, colour mainly white. Mainly winter rainfall region of South Africa, spreading into summer rainfall region. One species in northern Namibia and Botswana. Two species in East Africa and Ethiopia. Chromosomes x=11 and 9.

 

Subgenus Parvulipetala: Corresponds to clade B, with 39-42 species. Perennials, partly annuals. Petals five and equal, colour white or pink to deep purplish red. Mainly South Africa, but also other southern hemisphere except South America. a few species in East Africa and Ethiopia. Chromosomes x=7-19.

 

Subgenus Paucisignata: Corresponds to clade C2, with 25-27 species. Erect sometimes trailing shrubs or subshrubs, rarely geophytes or semi-geophytes. Petals five and equal, colour pink to red sometimes white. Summer rainfall region of South Africa, spreading into winter rainfall region and northern Namibia, with a few species in tropical Africa, Ethiopia, Somalia, Madagascar, the Arabian Peninsula and Asia Minor. Chromosomes x=mainly 9 or 10, but from 4-18.

 

Subgenus Pelargonium: Corresponds to clade A, with 167 species. Frequently xerophytic deciduous perennials with many geophytes and succulent subshrubs, less frequently woody evergreen shrubs or annual herbs. Petals five, colour shades of pink to purple or yellow. Winter rainfall region of South Africa and adjacent Namibia, spreading to summer rainfall area, and two species in tropical Africa. Chromosomes x=11, may be 8-10.

 

Species

Main article: List of Pelargonium species

Pelargonium has around 280 species. Röschenbleck et al lists 281 taxa. There is considerable confusion as to which Pelargonium are true species, and which are cultivars or hybrids. The nomenclature has changed considerably since the first plants were introduced to Europe in the 17th century.

 

Distribution

Pelargonium is a large genus within the family Geraniaceae, which has a worldwide distribution in temperate to subtropical zones with some 800 mostly herbaceous species. Pelargonium itself is native to southern Africa (including Namibia) and Australia. Southern Africa contains 90% of the genus, with only about 30 species found elsewhere, predominantly the East African rift valley (about 20 species) and southern Australia, including Tasmania. The remaining few species are found in southern Madagascar, Yemen, Iraq, Asia Minor, the north of New Zealand and isolated islands in the south Atlantic Ocean (Saint Helena and Tristan da Cunha) and Socotra in the Indian Ocean. The centre of diversity is in southwestern South Africa where rainfall is confined to the winter, unlike the rest of the country where rainfall is predominantly in the summer months. Most of the Pelargonium plants cultivated in Europe and North America have their origins in South Africa.

 

Ecology

Pelargonium species are eaten by the caterpillars of some Lepidoptera species, including the noctuid moth angle shades, Phlogophora meticulosa. The diurnal butterflies Cacyreus marshalli and C. tespis (Lycaenidae), native to southern Africa, also feed on Geranium and Pelargonium. C. marshallii has been introduced to Europe and can develop into a pest on cultivated Pelargoniums. It has naturalised along the Mediterranean, but does not survive the winter in Westen Europe.

 

The Japanese beetle, an important agricultural insect pest, becomes rapidly paralyzed after consuming flower petals of the garden hybrids known as "zonal geraniums" (P. × hortorum). The phenomenon was first described in 1920, and subsequently confirmed. Research conducted by Dr. Christopher Ranger with the USDA Agricultural Research Service and other collaborating scientists have demonstrated the excitatory amino acid called quisqualic acid present within the flower petals is responsible for causing paralysis of the Japanese beetle. Quisqualic acid is thought to mimic L-glutamic acid, which is a neurotransmitter in the insect neuromuscular junction and mammalian central nervous system.

 

A study by the Laboratory of Apiculture & Social Insects group at the University of Sussex on the attractiveness of common garden plants to pollinators found that a cultivar of Pelargonium × hortorum was unattractive to pollinators in comparison to other selected garden plants such as Lavandula (lavender) and Origanum.

 

Pests and diseases

Main articles: List of geranium diseases, Pelargonium flower break virus, and Pelargonium line pattern virus

The geranium bronze butterfly is a pest of Pelargonium species. The larvae of the geranium bronze bore into the stem of the host plant, causing the stem to typically turn black and die soon after. Geranium bronze are currently listed as an A2 quarantine pest by the European and Mediterranean Plant Protection Organization and can cause significant damage to Pelargonium species.

 

Cultivation

 

Pelargonium triste, the first species of its genus to be cultivated, here shown in its native habitat in Cape Town

Various types of Pelargonium are regular participants in flower shows and competitive events, with numerous societies devoted exclusively to their cultivation. They are easy to propagate vegetatively from cuttings. It is recommended that cuttings should have at least two nodes. Zonal geraniums grow in U.S. Department of Agriculture hardiness zones 9 through 12. Zonal geraniums are basically tropical perennials. Although they are often grown as annuals, they may overwinter in zones as cool as zone 7.

 

Cultivation history

The first species of Pelargonium known to be cultivated was P. triste, a native of South Africa. It was probably brought to the Botanical Garden in Leiden before 1600 on ships which had stopped at the Cape of Good Hope. In 1631, the English gardener John Tradescant the elder bought seeds from Rene Morin in Paris and introduced the plant to England. By 1724, P. inquinans, P. odoratissimum, P. peltatum, P. vitifolium, and P. zonale had been introduced to Europe.

 

Cultivars

 

Zonal pelargonium

There was little attempt at any rational grouping of Pelargonium cultivars, the growing of which was revived in the mid-twentieth century, and the origins of many if not most were lost in obscurity. In 1916 the American botanist Liberty Hyde Bailey (1858–1954) introduced two new terms for zonal and regal pelargoniums. Those pelargoniums which were largely derived from P. zonale he referred to as P. × hortorum (i.e. from the garden), while those from P. cucullatum he named P. × domesticum (i.e. from the home) In the late 1950s a list (the Spalding List) was produced in the United States, based on nursery listings and the 1897 list of Henri Dauthenay. It described seven groups, listing each cultivar with the list of its originator, and in most cases a date. These were Species, Zonals, Variegated-Leaved, Domesticum (Regals), Ivy-Leaved, Scented-Leaved and Old. In the 1970s the British Pelargonium and Geranium Society produced a checklist and the Australian Geranium Society started to produce a register but it was not completed till its author, Jean Llewellyn's death in 1999. None of these were published. The most complete list in its time was the 2001 compilation by The Geraniaceae Group, which included all cultivars up to 1959.

 

Registration of cultivars is the responsibility of the Pelargonium & Geranium Society (PAGS: formed in 2009 from the British Pelargonium and Geranium Society and the British and European Geranium Society) which administers the International Register of Pelargonium Cultivars. PAGS is the International Cultivar Registration Authority (ICRA) of the International Society for Horticultural Science for pelargoniums.

  

Contrasting leaves: Ivy-leaved Group (Left) Zonal Group (Right)

Cultivated pelargoniums are commonly divided into six groups in addition to species pelargoniums and primary hybrids. The following list is ordered by position in the PAGS classification. Abbreviations indicate Royal Horticultural Society usage.

 

A. Zonal (Z)

B. Ivy-leaved (I)

C. Regal (R)

D. Angel (A)

E. Unique (U)

F. Scented-leaved (Sc)

G. Species

H. Primary hybrids

Of these, A, U and Sc groups are sometimes lumped together as Species Derived (Sppd). This term implies that they are closely related to a species from which they were derived, and do not fit into the R, I or Z groups.

 

In addition to the primary groups, additional descriptors are used. The Royal Horticultural Society has created description codes. These include;

 

Cactus (Ca)

Coloured foliage (C)

Decorative (Dec)

Double (d)

Dwarf (Dw)

Dwarf Ivy-leaved (Dwl)

Frutetorum (Fr)

Miniature (Min)

Miniature Ivy-leaved (MinI)

Stellar (St)

Tulip (T)

Variegated (v)

These may then be combined to form the code, e.g. Pelargonium 'Chelsea Gem' (Z/d/v), indicating Zonal Double with variegated foliage. Crosses between groups are indicated with an ×, e.g. Pelargonium 'Hindoo' (R × U), indicating a Regal × Unique cross.

 

A. Zonal pelargoniums (Pelargonium × hortorum Bailey)

 

Pelargonium × hortorum (Zonal)

These are known as zonal geraniums because many have zones or patterns in the center of the leaves,[36] this is the contribution of the Pelargonium zonale parent. Common names include storksbill, fish or horseshoe geraniums.[50] They are also referred to as Pelargonium × hortorum Bailey. Zonal pelargoniums are tetraploid, mostly derived from P. inquinans and P. zonale, together with P. scandens and P. frutetorum.

 

Zonal pelargoniums are mostly bush-type plants with succulent stems grown for the beauty of their flowers, traditionally red, salmon, violet, white or pink. The scarlet colouring is attributed to the contribution of P. inquinans. Flowers may be double or single. They are the pelargoniums most often confused with genus Geranium, particularly in summer bedding arrangements. This incorrect nomenclature is widely used in horticulture, particularly in North America.

 

Zonals include a variety of plant types along with genetic hybrids such as hybrid ivy-leaved varieties that display little or no ivy leaf characteristics (the Deacons varieties), or the Stellar varieties. Hybrid zonals are crosses between zonals and either a species or species-derived pelargonium. There are hundreds of zonal cultivars available for sale, and like other cultivars are sold in series such as 'Rocky Mountain', each of which is named after its predominant colour, e.g. 'Rocky Mountain Orange', 'White', 'Dark Red', etc.

  

'Rocky Mountain Orange' (Zonal)

(i) Basic plants – Mature plants with foliage normally exceeding 180 mm (7 in) in height above the rim of the pot. For exhibition these should be grown in a pot exceeding 120 mm (4+3⁄4 in) in diameter but not normally exceeding 165 mm (6+1⁄2 in).

(ii) Dwarf plants – Smaller than basic. Mature plants with foliage more than 125 mm (5 in) above the rim of the pot, but not normally more than 180 mm (7 in). For exhibition should be grown in a pot exceeding 90 mm (3+1⁄2 in) but not exceeding 120 mm (4+3⁄4 in). They should not exceed 200 mm in height, grown in an 11 cm pot.

(iii) Miniature plants – Slowly growing pelargoniums. Mature plants with foliage normally less than 125 mm (5 in) above the rim of the pot. For exhibition should be grown in a pot not exceeding 90 mm (3+1⁄2 in). They should not exceed 125 mm in height, grown in a 9 cm pot.

(iv) Micro-miniature plants – Smaller and more slowly growing than miniature pelargoniums. Mature plants with foliage normally less than 100 mm (4 in) above the rim of the pot. They should not exceed 75 mm in height, grown in a 6 cm pot. Usually no separate classes for these in exhibition and will therefore normally be shown as Miniature Zonals.

(v) Deacon varieties –Genetic hybrid similar to a large Dwarf. For exhibition (when shown in a separate class), usually grown in a pot not exceeding 125 mm (5 in), otherwise as for Dwarf Zonals.

(vi) Stellar varieties – A relatively modern genetic hybrid originating from the work done by the Australian hybridiser Ted Both in the late 1950s and 1960s from crosses between Australian species and Zonal types. Easily identifiable by their distinctive half-star-shaped leaves and slim-petalled blooms which create an impression of being star shaped (or five fingered). Single varieties tend to have larger elongated triangular petals whereas doubles tend to have thin feathered petals that are tightly packed together. For exhibition purposes there is a separate class for 'Stellar' varieties, but being Zonals could be shown in an open class for Basic, Dwarf or Miniature Zonals (unless otherwise stated). Also known as "The Five-fingered Geraniums", "Staphysagroides", "Both’s Staphs", "Both’s Hybrid Staphs", "Fingered Flowers" and "Bodey’s Formosum Hybrids".

Fancy-leaf zonal pelargoniums – besides having green leaves with or without zoning, this group also have variable coloured foliage[50] that is sometimes used in classifying for exhibition purposes, e.g. ‘Bicolour’, ‘Tricolour’, ‘Bronze’ or ‘Gold’. Other foliage types are: ‘Black’ or ‘Butterfly’. There are an increasing number of these plants with showy blooms;

 

(a) Bicolour – includes those with white or cream veined leaves or those with two distinct colours with clearly defined edges, other than the basic zone.

(b) Tricolour – (May be Silver Tricolour (usually called a Silver Leaf) or a Gold Tricolour).

(i) Gold Tricolour – Leaves of many colours including red and gold, but usually with clearly defined edges of golden yellow and having a leaf zone, usually red or bronze, that overlays two or more of the other distinct leaf colours, so that the zone itself appears as two or more distinct colours.

(ii) Silver Tricolour or Silver Leaf – These tend to resemble a normal bi-colour leaf plant with two distinct colours usually of green and pale cream or white; the third colour is usually made up of bronze zoning. When this zoning overlays the green part of the leaf it is deemed to represent a silver colour.

(c) Bronze Leaved – Leaves of Green or Golden/Green with a heavy bronze or chestnut coloured centre zone which is known as a medallion. For exhibition purposes, when exhibited in specific ‘Bronze’ Leaf class – Must have over 50% of leaf surface bronze coloured. The dwarf plant ‘Overchurch’ which has a heavy bronze medallion.

(d) Gold Leaved – Leaves coloured golden/yellow or green/yellow but not showing a tendency to green. For exhibition purposes, when exhibited in specific ‘Gold’ Leaf class – Must have over 50% of leaf surface gold coloured.

(e) Black Leaved – Leaves coloured black, purple-black or with distinct large dark zones or centre markings on green.

(f) Butterfly Leaved – Leaves with a butterfly marking of distinct tone or hue in centre of leaf. This can be encompassed in many of the coloured leaf varieties.

Zonal pelargoniums have many flower types, as follows:

 

(a) Single flowered (S) – each flower pip normally having no more than five petals. This is the standard flower set for all Pelargoniums.

(b) Semi-double flowered (SD) – each flower pip normally having between six and nine petals.

(c) Double flowered (D)– each flower pip composed of more than nine petals (i.e. double the standard flower set) but not ‘hearted’ like the bud of a rose, e.g. the dwarf ‘Dovepoint’ which has full double blooms.

(d) Rosebud (or noisette) flowered – each bloom fully double and ‘hearted’. The middle petals are so numerous that they remain unopened like the bud of a rose.

(e) Tulip flowered – having semi-double blooms that never fully open. The large cup shaped petals open just sufficiently to resemble a miniature tulip.

(f) Bird's-egg group – having blooms with petals that have spots in a darker shade than the base colour, like many birds eggs.

(g) Speckled flowered group – having petals that are marked with splashes and flecks of another colour, e.g. ‘Vectis Embers’.

(h) Quilled (or cactus-flowered group, or poinsettia in USA) – having petals twisted and furled like a quill.

“Zonquil” pelargoniums result from a cross between Zonal pelargonium cultivars and P. quinquelobatum.

 

B. Ivy-leaved pelargoniums (derived from Pelargonium peltatum)

 

Pelargonium peltatum (Ivy-leaved)

Also known as "ivy geraniums". Usually of lax growth (trailing), mainly due to the long thin stems, with thick, waxy ivy-shaped stiff fleshy evergreen leaves developed by the species P. peltatum to retain moisture during periods of drought. Much used for hanging pots, tubs and basket cultivation. In the UK the bulbous double-headed types are preferred whilst on the European continent the balcon single types for large-scale hanging floral displays are favoured. Ivy-leaved pelargoniums embrace all such growth size types including small-leaved varieties and genetic hybrid crosses, which display little or no zonal characteristics. May have bicolour leaves and may have flowers that are single, double or rosette. Ivy pelargoniums are often sold as series such as 'Great Balls of Fire', in a variety of colours such as 'Great Balls of Fire Burgundy'.

 

Additional descriptive terms include;

 

Hybrid Ivy — the result of ivy × zonal crosses, but still more closely resemble ivy-leaved pelargoniums.

Fancy leaf — leaves with marked color variation, together with or other than green.

Miniature — miniature leaves and flowers, stems with short nodes, and compact growth. e.g. 'Sugar Baby' listed as Dwarf Ivy (DwI) by RHS.

C. Regal pelargoniums (Pelargonium × domesticum Bailey)

 

'Karl Offenstein' (Regal)

These are large bush-type floriferous evergreen pelargoniums. In addition to "Regals" they are also known as “Show Pelargoniums”. In the United States they are often known as the "Martha Washington" or ‘"Lady Washington" pelargoniums. They are grown primarily for the beauty and richness of their flower heads, which are large. Most of those cultivars grown currently are the result of hybridization over the last 50 years. They are very short-jointed and compact, which results in their requiring very little work in order to create a floriforous and well-rounded plant. Flowers are single, rarely double, in mauve, pink, purple or white. They have rounded, sometimes lobed or partially toothed (serrated) leaves, unlike the Zonal groups, without any type of zoning.

 

Additional descriptive terms include;

Decorative pelargoniums (Decoratives) – Descendants of older, less compact, smaller-flowered varieties that are more suited to outdoor conditions. These have smaller flowers than Regal, but are otherwise similar. e.g. ‘Royal Ascot’

Miniature – Flowers and leaves similar to Regal, but miniature in form, with compact growth. Other terms include “Pansy Geraniums” or “Pansy Pelargoniums”. e.g. ‘Lara Susan’

Oriental pelargoniums – The result of crosses between Regals and members of the Angel group (see below). Some have bicolour foliage.

D. Angel pelargoniums (derived from Pelargonium crispum)

 

'Angeleyes Randy' (Angel)

Angel pelargoniums are similar to Regal pelargoniums but more closely resemble P. crispum in leaf shape and growth habit. The majority of Angel cultivars originate from a cross between P. crispum and a Regal variety in the early part of the 20th century. Angels have grown in popularity in the last 30 years or so due mainly to an explosion of new varieties being released by specialist nurseries resulting from the work done by dedicated amateur hybridisers. These hybrisers have managed to obtain many new flower colour breaks and tighter growth habits resulting in plants suitable for all sorts of situations. Angels basically have the appearance of a small Regal with small serrated leaves and much smaller flowers and are more compact and bushy. The group extends to include similar small-leaved and -flowered types but usually with P. crispum in their parentage. They are mostly upright bush-type plants but there are some lax varieties that can be used for basket or hanging pot cultivation. Often called "pansy-faced" in the US. Some varieties have bicolour foliage. Other terms include ‘Langley-Smith Hybrids’.

 

E. Unique pelargoniums (derived from Pelargonium fulgidum)

 

Unique in sense of not fitting into any of the above categories. The parentage of Unique pelargoniums is confused and obscure. One theory being a derivation from P. fulgidum, but a derivation from an older cultivar 'Old Unique’, also known as or ‘Rollinson’s Crimson’, in the mid-19th century is also claimed. Unique pelargoniums resemble upright Scented Leaf pelargoniums in being shrubby and woody evergreens. They have distinctly scented leaves, and small flowers with blotched and feathered petals. They may have bicolour foliage. Some types, popularly known in the hobby as hybrid Uniques, have been crossed with Regal pelargoniums and, as a result of this cross, are much more floriferous.

 

Cultivar

Pelargonium graveolens (Scented leaf)

Shrubby evergreen perennials grown chiefly for their fragrance, may be species or cultivars but all must have a clear and distinct scented foliage. Scent is emitted when the leaves are touched or bruised with some scents aromatic, others pungent and in a few cases, quite unpleasant. Several of the scented leaved pelargoniums are grown for the oil geraniol, which is extracted from the leaves and is an essential oil much used commercially in perfumery. The scent of some species growing in their natural habitat, acts as a deterrent to grazing animals who appear to dislike the emitted scent. Conversely, it also attracts other insect life to visit the bloom and pollinate the plant. The scented leaves can be used for potpourri and they also have a use as flavourings in cooking. Occasionally scented types can be found in some of the other groups mentioned; for example, the Angels, having P. crispum in their genetic makeup, can often have a strong citrus scent. Leaves are lobed, toothed, incised or variegated. Growth habit is very variable, but the flowers are less prominent than other groups, and most closely resemble the species they originated from.

 

These include:

Pelargonium ionidiflorum (Scented leaf)

Almond - Pelargonium quercifolium

Apple - Pelargonium odoratissimum

Apple - Pelargonium cordifolium

Apple/Mint - Pelargonium album

Apricot/Lemon - Pelargonium scabrum

Balsam - Pelargonium panduriforme

Camphor - Pelargonium betulinum

Celery - Pelargonium ionidiflorum

Cinnamon - Pelargonium 'Ardwyck Cinnamon'

Coconut - Pelargonium grossalarioides (Pelargonium parriflorum)

Eau de Cologne - Pelargonium 'Brilliantine'

Eucalyptus - Pelargonium 'Secret Love'

Grapefruit - Pelargonium 'Poquita'

Ginger - Pelargonium 'Torrento' or 'Cola Bottles' which is a variety of Pelargonium x nervosum

Hazelnut - Pelargonium 'Odorata Hazelnut

Lavender - Pelargonium 'Lavender Lindy'

Lemon - Pelargonium crispum

Lemon - Pelargonium citronellum (Synonym - Pelargonium 'Mabel Grey')

Lemon Balm - Pelargonium x melissinum

Lime - Pelargonium x nervosum

Myrrh - Pelargonium myrrhifolium

Nutmeg - Pelargonium x fragrans

Old Spice - Variety of Pelargonium x fragrans

Orange - Pelargonium x citriodorum (Synonym - Pelargonium 'Prince of Orange')

Peach - Pelargonium 'Peaches and Cream'

Peppermint - Pelargonium tomentosum

Pine - Pelargonium denticulatum

Pineapple - Pelargonium 'Brilliant'

Raspberry - Pelargonium 'Red Raspberry'

Rose - Pelargonium graveolens (Synonym - Pelargonium roseum)

Rose - Pelargonium capitatum

Rose - Pelargonium radens

Southernwood - Pelargonium abrotanifolium

Spicy - Pelargonium exstipulatum

Strawberry - Pelargonium x scarboroviae

Cultivars

'Attar of Roses' - a cultivar of P. capitatum

'Crowfoot Rose' - a cultivar of P. radens

'Dr. Livingston' - a cultivar of P. radens

'Grey Lady Plymouth' - a cultivar of P. graveolens

'Prince Rupert' - a cultivar of P. crispum

G. Species pelargoniums

The species are the forefathers of all the cultivar groups listed above. In general, the definition of a species is that it breeds true, and is to be found doing this in the "wild". Species pelargoniums have a large diversity of characteristics in habit, shape, size and colour, which probably accounts for them having retained their popularity for more than 300 years.

 

H. Primary hybrids

A primary hybrid is recognised as being the resultant plant from a first-time cross between two different known species. Examples are P. × ardens – from P. lobatum × P. fulgidum (1810). P. × glauciifolium – from P. gibbosum × P. lobatum (1822). Usually, but not always, primary hybrids are sterile.

 

The following is a selection of pelargoniums which have gained the Royal Horticultural Society's Award of Garden Merit:

 

'Attar of Roses' (rose scented leaves, pink flowers)

'Citriodorum' (lemon scented leaves, rose pink flowers

'Dolly Varden' (variegated leaves, scarlet flowers)

'Frank Headley' (cream vareigated leaves, salmon pink flowers)

'Fringed Aztec' (white & purple fringed flowers)

'Gemstone' (scented leaves, pink flowers)

'Grace Thomas' (lemon scented leaves, pale pink flowers)

'Joy' (pink & white frilled flowers)

'Lady Plymouth' (P. graveolens variegata - small mauve flowers)

'Lara Candy Dancer' (scented leaves, pale mauve flowers)

'Lara Starshine' (aromatic leaves, lilac flowers.

'L'Élégante' (ivy-leaved, trailing, white and purple flowers)

'Mabel Grey' (lemon-scented leaves, mauve flowers)

'Mrs Quilter' (bronze leaves, salmon pink flowers)

'Radula' (lemon & rose scented leaves, pink & purple flowers)

'Royal Oak' (balsam scented leaves, mauve flowers)

'Spanish Angel' (lilac & magenta flowers)

'Sweet Mimosa' (balsam-scented leaves, pale pink flowers)

'Tip Top Duet' (pink & wine-red flowers)

'Voodoo' (crimson & black flowers)

P. tomentosum (peppermint-scented leaves, small white flowers)

Usage

Ornamental plants

Pelargoniums rank as one of the highest number of potted flowering plants sold and also in terms of wholesale value.

 

Scented leaf pelargoniums

Other than being grown for their beauty, species such as P. graveolens are important in the perfume industry and are cultivated and distilled for their scents. Although scented pelargoniums exist which have smells of citrus, mint, pine, spices or various fruits, the varieties with rose scents are most commercially important. Pelargonium distillates and absolutes, commonly known as "scented geranium oil" are sometimes used to supplement or adulterate expensive rose oils. The oils of the scented pelargoniums contain citronellol, geraniol, eugenol, alpha-pinene and many other compounds. The edible leaves and flowers are also used as a flavouring in desserts, cakes, jellies and teas. Scented-leafed pelargoniums can be used to flavor jellies, cakes, butters, ice cream, iced tea and other dishes, The rose-, lemon- and peppermint-scents are most commonly used. Also used are those with hints of peach, cinnamon and orange. Commonly used lemon-scented culinary species include P. crispum and P. citronellum. Rose-scenteds include P. graveolens and members of the P. graveolens cultivar group. Other species and cultivars with culinary use include the lime-scented P. ‘Lime’, the lemon balm-scented P. ‘Lemon Balm’, the strawberry-lemon-scented P. ‘Lady Scarborough’ and the peppermint-scented P. tomentosum.[81] Scented leaf pelargoniums have also been historically used as toilet paper by fishermen in remote places, such as the Minquiers.

 

Herbal medicine

In herbal medicine, Pelargonium has been used for intestinal problems, wounds and respiratory ailments, but Pelargonium species have also been used for fevers, kidney complaints and other conditions. Geranium (Pelargonium) oil is considered a relaxant in aromatherapy, and in recent years, respiratory/cold remedies made from P. sidoides and P. reniforme have been sold in Europe and the United States. P. sidoides along with Echinacea is used for bronchitis. P. odoratissimum is used for its astringent, tonic and antiseptic effects. It is used internally for debility, gastroenteritis, and hemorrhage and externally for skin complaints, injuries, and neuralgia and throat infections. The essential oil is used in aromatherapy.

 

Pets

According to the ASPCA, these plants are toxic to cats, dogs, and horses.

 

Chemistry

Pelargonin (pelargonidin 3,5-O-diglucoside) is a petal pigment of the scarlet pelargonium.

 

Culture

The chemist, John Dalton, realized that he was color blind in 1794 when he heard others describe the color of the flowers of the pink Pelargonium zonale as pink or red, when to him it looked either pink or blue, having no relationship to red at all.

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

 

An Austin Healey 3000 heads out of the paddock during the 76th Members' Meeting, Goodwood

This image has been re worked to include in an on-line gallery recently created to display and sell my most popular art....view it here:

 

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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

 

Please include credit line if you want to copy this to pinterest/tumblr etc :)

Herbstzeitlose,

Colchicum autumnale

 

"Wenn man die Natur wahrhaft liebt, findet man es überall schön."

 

"If you truly love nature, you will find it beautiful everywhere."

Vincent van Gogh

 

I love the time between summer and fall, when the sun is lower and the air is cooler and that includes the simple beauty of this flower.

 

Ich liebe die Zeit zwischen Sommer und Herbst, wenn die Sonne tiefer steht und die Luft kühler wird und dazu gehört die einfache Schönheit der Herbstzeitlosen.

Castle , Kasteel de Haar near the suburb of Vleuten that includes village of Haarzuilen rebuild by architect Pierre Cuyper Project was finished in around 1912 took 20 years to be finished , Martin’s photograph , Utrecht , the Netherlands , June 5. 2019

  

Beautiful staircase

Beautiful staircase in castle , Kasteel de Haar

Staircase

Stairway critters sculptures in Castle

Stairway sculptures

Spiral stairway

Central Station in Amsterdam , build by architect Pierre Cuyper

de Rijks Museum in Amsterdam build by architect Pierre Cuyper

de Rijks Museum in Amsterdam

Central Station in Amsterdam

Amsterdam

Lavet bad tub

Lavet bad tub and washing machine

main door

Beautiful staircase

Kasteel de Haar near the suburb of Vleuten that includes village of Haarzuilen

architect Pierre Cuyper

Martin’s photograph

Utrecht

the Netherlands

Nederland

June 2019

Favourites

IPhone 6

Village of Haarzuilen

Kasteel de Haar

Castle the Haar

Kasteel de Haar was rebuild by architect Pierre Cuyper Project was finished in around 1912 took 20 years to be finished

city of Utrecht in the province Utrecht

Beautiful staircase in Kasteel de Haar

Door knocker

Beautiful window and seating

architect Pierre Cuyper

Includes 3 colors with LeLutka/Catwa/Genus appliers. Also includes standard eyes layers (BOM compatible)

 

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Wisdom includes being in one's garden when the town is oveeflowing with Memorial Weekend extravaganza outdoors exploitations, with the sounds of blaring horns of cars whose owners haven't figured out how to stop them yet, and rock climbers, beer drinkers, kitsch buyers etc. etc. so the advice I was given is: make your yard your refuge. design it so in summer you can't see your neighbor's houses, avoid straight line, grow bird friendly bushes, lots of berries, and a cherry tree to drool over everey year...i't really hard to leave this Garden of Eden, as there's always something to pick , to plant, to trim, to separate, and with all, I play the creator, the decider...no time for Memorial Day Parties.

A circular scenic route in the Picos de Europa including the "Desfiladero de los Beyos" and this viewpoint in the "Valle de Valdeon"

Includes a spring-loaded Ustokal ballista

Includes a functional, easy to load rubber-band powered floating arm trebuchet with extra shots

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.

Drawing is a form of visual art in which a person uses various drawing instruments to mark paper or another two-dimensional medium. Instruments include graphite pencils, pen and ink, inked brushes, wax color pencils, crayons, charcoal, chalk, pastels, various kinds of erasers, markers, styluses, various metals (such as silverpoint) and electronic drawing.

 

A drawing instrument releases small amount of material onto a surface, leaving a visible mark. The most common support for drawing is paper, although other materials, such as cardboard, plastic, leather, canvas, and board, may be used. Temporary drawings may be made on a blackboard or whiteboard or indeed almost anything. The medium has been a popular and fundamental means of public expression throughout human history. It is one of the simplest and most efficient means of communicating visual ideas.[1] The wide availability of drawing instruments makes drawing one of the most common artistic activities.

In addition to its more artistic forms, drawing is frequently used in commercial illustration, animation, architecture, engineering and technical drawing. A quick, freehand drawing, usually not intended as a finished work, is sometimes called a sketch. An artist who practices or works in technical drawing may be called a drafter, draftsman or a draughtsman.[2]

Drawing is one of the major forms of expression within the visual arts. It is generally concerned with the marking of lines and areas of tone onto paper/other material, where the accurate representation of the visual world is expressed upon a plane surface.[3] Traditional drawings were monochrome, or at least had little colour,[4] while modern colored-pencil drawings may approach or cross a boundary between drawing and painting. In Western terminology, drawing is distinct from painting, even though similar media often are employed in both tasks. Dry media, normally associated with drawing, such as chalk, may be used in pastel paintings. Drawing may be done with a liquid medium, applied with brushes or pens. Similar supports likewise can serve both: painting generally involves the application of liquid paint onto prepared canvas or panels, but sometimes an underdrawing is drawn first on that same support.

  

Madame Palmyre with Her Dog, 1897. Henri de Toulouse-Lautrec

 

Galileo Galilei. Phases of the Moon. 1616.

Drawing is often exploratory, with considerable emphasis on observation, problem-solving and composition. Drawing is also regularly used in preparation for a painting, further obfuscating their distinction. Drawings created for these purposes are called studies.

 

There are several categories of drawing, including figure drawing, cartooning, doodling, free hand and shading. There are also many drawing methods, such as line drawing, stippling, shading, the surrealist method of entopic graphomania (in which dots are made at the sites of impurities in a blank sheet of paper, and lines are then made between the dots), and tracing (drawing on a translucent paper, such as tracing paper, around the outline of preexisting shapes that show through the paper).

 

A quick, unrefined drawing may be called a sketch.

 

In fields outside art, technical drawings or plans of buildings, machinery, circuitry and other things are often called "drawings" even when they have been transferred to another medium by printing.

 

History[edit]

Drawing as a Form of Communication Drawing is one of the oldest forms of human expression, with evidence for its existence preceding that of written communication.[5] It is believed that drawing was used as a specialised form of communication before the invent of the written language,[5][6] demonstrated by the production of cave and rock paintings created by Homo sapiens sapiens around 30,000 years ago.[7] These drawings, known as pictograms, depicted objects and abstract concepts.[8] The sketches and paintings produced in prehistoric times were eventually stylised and simplified, leading to the development of the written language as we know it today.

 

Drawing in the Arts Drawing is used to express one's creativity, and therefore has been prominent in the world of art. Throughout much of history, drawing was regarded as the foundation for artistic practise.[9] Initially, artists used and reused wooden tablets for the production of their drawings.[10] Following the widespread availability of paper in the 14th century, the use of drawing in the arts increased. At this point, drawing was commonly used as a tool for thought and investigation, acting as a study medium whilst artists were preparing for their final pieces of work.[11][12] In a period of artistic flourish, the Renaissance brought about drawings exhibiting realistic representational qualities,[13] where there was a lot of influence from geometry and philosophy.[14]

 

The invention of the first widely available form of photography led to a shift in the use of drawing in the arts.[15] Photography took over from drawing as a more superior method for accurately representing visual phenomena, and artists began to abandon traditional drawing practises.[16] Modernism in the arts encouraged "imaginative originality"[17] and artists' approach to drawing became more abstract.

 

Drawing Outside the Arts Although the use of drawing is extensive in the arts, its practice is not confined purely to this field. Before the widespread availability of paper, 12th century monks in European monasteries used intricate drawings to prepare illustrated, illuminated manuscripts on vellum and parchment. Drawing has also been used extensively in the field of science, as a method of discovery, understanding and explanation. In 1616, astronomer Galileo Galilei explained the changing phases of the moon through his observational telescopic drawings.[16] Additionally, in 1924, geophysicist Alfred Wegener used illustrations to visually demonstrate the origin of the continents.The medium is the means by which ink, pigment or color are delivered onto the drawing surface. Most drawing media are either dry (e.g. graphite, charcoal, pastels, Conté, silverpoint), or use a fluid solvent or carrier (marker, pen and ink). Watercolor pencils can be used dry like ordinary pencils, then moistened with a wet brush to get various painterly effects. Very rarely, artists have drawn with (usually decoded) invisible ink. Metalpoint drawing usually employs either of two metals: silver or lead.[20] More rarely used are gold, platinum, copper, brass, bronze, and tinpoint.

 

Paper comes in a variety of different sizes and qualities, ranging from newspaper grade up to high quality and relatively expensive paper sold as individual sheets.[21] Papers can vary in texture, hue, acidity, and strength when wet. Smooth paper is good for rendering fine detail, but a more "toothy" paper holds the drawing material better. Thus a coarser material is useful for producing deeper contrast.

 

Newsprint and typing paper may be useful for practice and rough sketches. Tracing paper is used to experiment over a half-finished drawing, and to transfer a design from one sheet to another. Cartridge paper is the basic type of drawing paper sold in pads. Bristol board and even heavier acid-free boards, frequently with smooth finishes, are used for drawing fine detail and do not distort when wet media (ink, washes) are applied. Vellum is extremely smooth and suitable for very fine detail. Coldpressed watercolor paper may be favored for ink drawing due to its texture.

 

Acid-free, archival quality paper keeps its color and texture far longer than wood pulp based paper such as newsprint, which turns yellow and become brittle much sooner.

 

The basic tools are a drawing board or table, pencil sharpener and eraser, and for ink drawing, blotting paper. Other tools used are circle compass, ruler, and set square. Fixative is used to prevent pencil and crayon marks from smudging. Drafting tape is used to secure paper to drawing surface, and also to mask an area to keep it free of accidental marks sprayed or spattered materials and washes. An easel or slanted table is used to keep the drawing surface in a suitable position, which is generally more horizontal than the position used in painting.

 

Technique[edit]

 

Raphael, study for what became the Alba Madonna, with other sketches

Almost all draftsmen use their hands and fingers to apply the media, with the exception of some handicapped individuals who draw with their mouth or feet.[22]

 

Prior to working on an image, the artist typically explores how various media work. They may try different drawing implements on practice sheets to determine value and texture, and how to apply the implement to produce various effects.

 

The artist's choice of drawing strokes affects the appearance of the image. Pen and ink drawings often use hatching—groups of parallel lines.[23] Cross-hatching uses hatching in two or more different directions to create a darker tone. Broken hatching, or lines with intermittent breaks, form lighter tones—and controlling the density of the breaks achieves a gradation of tone. Stippling, uses dots to produce tone, texture or shade. Different textures can be achieved depending on the method used to build tone.[24]

 

Drawings in dry media often use similar techniques, though pencils and drawing sticks can achieve continuous variations in tone. Typically a drawing is filled in based on which hand the artist favors. A right-handed artist draws from left to right to avoid smearing the image. Erasers can remove unwanted lines, lighten tones, and clean up stray marks. In a sketch or outline drawing, lines drawn often follow the contour of the subject, creating depth by looking like shadows cast from a light in the artist's position.

 

Sometimes the artist leaves a section of the image untouched while filling in the remainder. The shape of the area to preserve can be painted with masking fluid or cut out of a frisket and applied to the drawing surface, protecting the surface from stray marks until the mask is removed.

 

Another method to preserve a section of the image is to apply a spray-on fixative to the surface. This holds loose material more firmly to the sheet and prevents it from smearing. However the fixative spray typically uses chemicals that can harm the respiratory system, so it should be employed in a well-ventilated area such as outdoors.

 

Another technique is subtractive drawing in which the drawing surface is covered with graphite or charcoal and then erased to make the image.[25]

 

Tone[edit]

 

Line drawing in sanguine by Leonardo da Vinci

Shading is the technique of varying the tonal values on the paper to represent the shade of the material as well as the placement of the shadows. Careful attention to reflected light, shadows and highlights can result in a very realistic rendition of the image.

 

Blending uses an implement to soften or spread the original drawing strokes. Blending is most easily done with a medium that does not immediately fix itself, such as graphite, chalk, or charcoal, although freshly applied ink can be smudged, wet or dry, for some effects. For shading and blending, the artist can use a blending stump, tissue, a kneaded eraser, a fingertip, or any combination of them. A piece of chamois is useful for creating smooth textures, and for removing material to lighten the tone. Continuous tone can be achieved with graphite on a smooth surface without blending, but the technique is laborious, involving small circular or oval strokes with a somewhat blunt point.

 

Shading techniques that also introduce texture to the drawing include hatching and stippling. A number of other methods produce texture. In addition to the choice of paper, drawing material and technique affect texture. Texture can be made to appear more realistic when it is drawn next to a contrasting texture; a coarse texture is more obvious when placed next to a smoothly blended area. A similar effect can be achieved by drawing different tones close together. A light edge next to a dark background stands out to the eye, and almost appears to float above the surface.

 

Form and proportion[edit]

 

Pencil portrait by Ingres

Measuring the dimensions of a subject while blocking in the drawing is an important step in producing a realistic rendition of the subject. Tools such as a compass can be used to measure the angles of different sides. These angles can be reproduced on the drawing surface and then rechecked to make sure they are accurate. Another form of measurement is to compare the relative sizes of different parts of the subject with each other. A finger placed at a point along the drawing implement can be used to compare that dimension with other parts of the image. A ruler can be used both as a straightedge and a device to compute proportions.

 

When attempting to draw a complicated shape such as a human figure, it is helpful at first to represent the form with a set of primitive volumes. Almost any form can be represented by some combination of the cube, sphere, cylinder, and cone. Once these basic volumes have been assembled into a likeness, then the drawing can be refined into a more accurate and polished form. The lines of the primitive volumes are removed and replaced by the final likeness. Drawing the underlying construction is a fundamental skill for representational art, and is taught in many books and schools. Its correct application resolves most uncertainties about smaller details, and makes the final image look consistent.[26]

 

A more refined art of figure drawing relies upon the artist possessing a deep understanding of anatomy and the human proportions. A trained artist is familiar with the skeleton structure, joint location, muscle placement, tendon movement, and how the different parts work together during movement. This allows the artist to render more natural poses that do not appear artificially stiff. The artist is also familiar with how the proportions vary depending on the age of the subject, particularly when drawing a portrait.

 

Perspective[edit]

Linear perspective is a method of portraying objects on a flat surface so that the dimensions shrink with distance. Each set of parallel, straight edges of any object, whether a building or a table, follows lines that eventually converge at a vanishing point. Typically this convergence point is somewhere along the horizon, as buildings are built level with the flat surface. When multiple structures are aligned with each other, such as buildings along a street, the horizontal tops and bottoms of the structures typically converge at a vanishing point.

  

Two-point perspective drawing

When both the fronts and sides of a building are drawn, then the parallel lines forming a side converge at a second point along the horizon (which may be off the drawing paper.) This is a two-point perspective.[27] Converging the vertical lines to a third point above or below the horizon then produces a three-point perspective.

 

Depth can also be portrayed by several techniques in addition to the perspective approach above. Objects of similar size should appear ever smaller the further they are from the viewer. Thus the back wheel of a cart appears slightly smaller than the front wheel. Depth can be portrayed through the use of texture. As the texture of an object gets further away it becomes more compressed and busy, taking on an entirely different character than if it was close. Depth can also be portrayed by reducing the contrast in more distant objects, and by making their colors less saturated. This reproduces the effect of atmospheric haze, and cause the eye to focus primarily on objects drawn in the foreground.

 

Artistry[edit]

 

Chiaroscuro study drawing by William-Adolphe Bouguereau

The composition of the image is an important element in producing an interesting work of artistic merit. The artist plans element placement in the art to communicate ideas and feelings with the viewer. The composition can determine the focus of the art, and result in a harmonious whole that is aesthetically appealing and stimulating.

 

The illumination of the subject is also a key element in creating an artistic piece, and the interplay of light and shadow is a valuable method in the artist's toolbox. The placement of the light sources can make a considerable difference in the type of message that is being presented. Multiple light sources can wash out any wrinkles in a person's face, for instance, and give a more youthful appearance. In contrast, a single light source, such as harsh daylight, can serve to highlight any texture or interesting features.

 

When drawing an object or figure, the skilled artist pays attention to both the area within the silhouette and what lies outside. The exterior is termed the negative space, and can be as important in the representation as the figure. Objects placed in the background of the figure should appear properly placed wherever they can be viewed.

  

Drawing process in the Academic Study of a Male Torso by Jean-Auguste-Dominique Ingres (1801, National Museum, Warsaw)

A study is a draft drawing that is made in preparation for a planned final image. Studies can be used to determine the appearances of specific parts of the completed image, or for experimenting with the best approach for accomplishing the end goal. However a well-crafted study can be a piece of art in its own right, and many hours of careful work can go into completing a study.

 

Process[edit]

Individuals display differences in their ability to produce visually accurate drawings.[28] A visually accurate drawing is described as being "recognized as a particular object at a particular time and in a particular space, rendered with little addition of visual detail that can not be seen in the object represented or with little deletion of visual detail”.[29]

 

Investigative studies have aimed to explain the reasons why some individuals draw better than others. One study posited four key abilities in the drawing process: perception of objects being drawn, ability to make good representational decisions, motor skills required for mark-making and the drawer's own perception of their drawing.[29] Following this hypothesis, several studies have sought to conclude which of these processes are most significant in affecting the accuracy of drawings.

 

Motor function Motor function is an important physical component in the 'Production Phase' of the drawing process.[30] It has been suggested that motor function plays a role in drawing ability, though its effects are not significant.[29]

 

Perception It has been suggested that an individual's ability to perceive an object they are drawing is the most important stage in the drawing process.[29] This suggestion is supported by the discovery of a robust relationship between perception and drawing ability.[31]

 

This evidence acted as the basis of Betty Edwards' how-to drawing book, Drawing on the Right Side of the Brain.[32] Edwards aimed to teach her readers how to draw, based on the development of the reader's perceptual abilities.

 

Furthermore, the influential artist and art critic John Ruskin emphasised the importance of perception in the drawing process in his book The Elements of Drawing.[33] He stated that "For I am nearly convinced, that once we see keenly enough, there is very little difficult in drawing what we see".

 

Visual memory has also been shown to influence one's ability to create visually accurate drawings. Short-term memory plays an important part in drawing as one’s gaze shifts between the object they are drawing and the drawing itself.[34]

include something (red) in the photograph .... It was pioneered by National Geographic photographers, who had subjects wear, or chose subjects who wore overly colorful clothes, (not necessarily red) though red was preferred as it rendered best on Kodachrome film.

  

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The Laing Art Gallery in Newcastle upon Tyne, England, is located on New Bridge Street West. The gallery was designed in the Baroque style with Art Nouveau elements by architects Cackett & Burns Dick and is now a Grade II listed building. It was opened in 1904 and is now managed by Tyne & Wear Archives & Museums and sponsored by the Department for Culture, Media and Sport. In front of the gallery is the Blue Carpet. The building, which was financed by a gift from a local wine merchant, Alexander Laing, is Grade II listed.

 

The gallery collection contains paintings, watercolours and decorative historical objects, including Newcastle silver. In the early 1880s, Newcastle was a major glass producer in the world and enamelled glasses by William Beilby are on view along with ceramics (including Maling pottery), and diverse contemporary works by emerging UK artists. It has a programme of regularly rotating exhibitions and has free entry.

 

The gallery's collection of paintings includes John Martin's dramatic The Destruction of Sodom and Gomorrah, as well as works by Sir Joshua Reynolds, Edward Burne-Jones (Laus Veneris), Isabella and the Pot of Basil from 1868 by William Holman Hunt, and Ben Nicholson. Local paintings include pictures by Ralph Hedley. There is also a collection of 18th- and 19th-century watercolours and drawings, including work by J. M. W. Turner and John Sell Cotman.[

 

Newcastle upon Tyne, or simply Newcastle is a cathedral city and metropolitan borough in Tyne and Wear, England. It is located on the River Tyne's northern bank, opposite Gateshead to the south. It is the most populous settlement in the Tyneside conurbation and North East England.

 

Newcastle developed around a Roman settlement called Pons Aelius, the settlement became known as Monkchester before taking on the name of a castle built in 1080 by William the Conqueror's eldest son, Robert Curthose. It was one of the world's largest ship building and repair centres during the industrial revolution. Newcastle was part of the county of Northumberland until 1400, when it separated and formed a county of itself. In 1974, Newcastle became part of Tyne and Wear. Since 2018, the city council has been part of the North of Tyne Combined Authority.

 

The history of Newcastle upon Tyne dates back almost 2,000 years, during which it has been controlled by the Romans, the Angles and the Norsemen amongst others. Newcastle upon Tyne was originally known by its Roman name Pons Aelius. The name "Newcastle" has been used since the Norman conquest of England. Due to its prime location on the River Tyne, the town developed greatly during the Middle Ages and it was to play a major role in the Industrial Revolution, being granted city status in 1882. Today, the city is a major retail, commercial and cultural centre.

 

Roman settlement

The history of Newcastle dates from AD 122, when the Romans built the first bridge to cross the River Tyne at that point. The bridge was called Pons Aelius or 'Bridge of Aelius', Aelius being the family name of Roman Emperor Hadrian, who was responsible for the Roman wall built across northern England along the Tyne–Solway gap. Hadrian's Wall ran through present-day Newcastle, with stretches of wall and turrets visible along the West Road, and at a temple in Benwell. Traces of a milecastle were found on Westgate Road, midway between Clayton Street and Grainger Street, and it is likely that the course of the wall corresponded to present-day Westgate Road. The course of the wall can be traced eastwards to the Segedunum Roman fort at Wallsend, with the fort of Arbeia down-river at the mouth of the Tyne, on the south bank in what is now South Shields. The Tyne was then a wider, shallower river at this point and it is thought that the bridge was probably about 700 feet (210 m) long, made of wood and supported on stone piers. It is probable that it was sited near the current Swing Bridge, due to the fact that Roman artefacts were found there during the building of the latter bridge. Hadrian himself probably visited the site in 122. A shrine was set up on the completed bridge in 123 by the 6th Legion, with two altars to Neptune and Oceanus respectively. The two altars were subsequently found in the river and are on display in the Great North Museum in Newcastle.

 

The Romans built a stone-walled fort in 150 to protect the river crossing which was at the foot of the Tyne Gorge, and this took the name of the bridge so that the whole settlement was known as Pons Aelius. The fort was situated on a rocky outcrop overlooking the new bridge, on the site of the present Castle Keep. Pons Aelius is last mentioned in 400, in a Roman document listing all of the Roman military outposts. It is likely that nestling in the shadow of the fort would have been a small vicus, or village. Unfortunately, no buildings have been detected; only a few pieces of flagging. It is clear that there was a Roman cemetery near Clavering Place, behind the Central station, as a number of Roman coffins and sarcophagi have been unearthed there.

 

Despite the presence of the bridge, the settlement of Pons Aelius was not particularly important among the northern Roman settlements. The most important stations were those on the highway of Dere Street running from Eboracum (York) through Corstopitum (Corbridge) and to the lands north of the Wall. Corstopitum, being a major arsenal and supply centre, was much larger and more populous than Pons Aelius.

 

Anglo-Saxon development

The Angles arrived in the North-East of England in about 500 and may have landed on the Tyne. There is no evidence of an Anglo-Saxon settlement on or near the site of Pons Aelius during the Anglo-Saxon age. The bridge probably survived and there may well have been a small village at the northern end, but no evidence survives. At that time the region was dominated by two kingdoms, Bernicia, north of the Tees and ruled from Bamburgh, and Deira, south of the Tees and ruled from York. Bernicia and Deira combined to form the kingdom of Northanhymbra (Northumbria) early in the 7th century. There were three local kings who held the title of Bretwalda – 'Lord of Britain', Edwin of Deira (627–632), Oswald of Bernicia (633–641) and Oswy of Northumbria (641–658). The 7th century became known as the 'Golden Age of Northumbria', when the area was a beacon of culture and learning in Europe. The greatness of this period was based on its generally Christian culture and resulted in the Lindisfarne Gospels amongst other treasures. The Tyne valley was dotted with monasteries, with those at Monkwearmouth, Hexham and Jarrow being the most famous. Bede, who was based at Jarrow, wrote of a royal estate, known as Ad Murum, 'at the Wall', 12 miles (19 km) from the sea. It is thought that this estate may have been in what is now Newcastle. At some unknown time, the site of Newcastle came to be known as Monkchester. The reason for this title is unknown, as we are unaware of any specific monasteries at the site, and Bede made no reference to it. In 875 Halfdan Ragnarsson, the Danish Viking conqueror of York, led an army that attacked and pillaged various monasteries in the area, and it is thought that Monkchester was also pillaged at this time. Little more was heard of it until the coming of the Normans.

 

Norman period

After the arrival of William the Conqueror in England in 1066, the whole of England was quickly subjected to Norman rule. However, in Northumbria there was great resistance to the Normans, and in 1069 the newly appointed Norman Earl of Northumbria, Robert de Comines and 700 of his men were killed by the local population at Durham. The Northumbrians then marched on York, but William was able to suppress the uprising. That same year, a second uprising occurred when a Danish fleet landed in the Humber. The Northumbrians again attacked York and destroyed the garrison there. William was again able to suppress the uprising, but this time he took revenge. He laid waste to the whole of the Midlands and the land from York to the Tees. In 1080, William Walcher, the Norman bishop of Durham and his followers were brutally murdered at Gateshead. This time Odo, bishop of Bayeux, William's half brother, devastated the land between the Tees and the Tweed. This was known as the 'Harrying of the North'. This devastation is reflected in the Domesday Book. The destruction had such an effect that the North remained poor and backward at least until Tudor times and perhaps until the Industrial Revolution. Newcastle suffered in this respect with the rest of the North.

 

In 1080 William sent his eldest son, Robert Curthose, north to defend the kingdom against the Scots. After his campaign, he moved to Monkchester and began the building of a 'New Castle'. This was of the "motte-and-bailey" type of construction, a wooden tower on top of an earthen mound (motte), surrounded by a moat and wooden stockade (bailey). It was this castle that gave Newcastle its name. In 1095 the Earl of Northumbria, Robert de Mowbray, rose up against the king, William Rufus, and Rufus sent an army north to recapture the castle. From then on the castle became crown property and was an important base from which the king could control the northern barons. The Northumbrian earldom was abolished and a Sheriff of Northumberland was appointed to administer the region. In 1091 the parish church of St Nicholas was consecrated on the site of the present Anglican cathedral, close by the bailey of the new castle. The church is believed to have been a wooden building on stone footings.

 

Not a trace of the tower or mound of the motte and bailey castle remains now. Henry II replaced it with a rectangular stone keep, which was built between 1172 and 1177 at a cost of £1,444. A stone bailey, in the form of a triangle, replaced the previous wooden one. The great outer gateway to the castle, called 'the Black Gate', was built later, between 1247 and 1250, in the reign of Henry III. There were at that time no town walls and when attacked by the Scots, the townspeople had to crowd into the bailey for safety. It is probable that the new castle acted as a magnet for local merchants because of the safety it provided. This in turn would help to expand trade in the town. At this time wool, skins and lead were being exported, whilst alum, pepper and ginger were being imported from France and Flanders.

 

Middle Ages

Throughout the Middle Ages, Newcastle was England's northern fortress, the centre for assembled armies. The Border war against Scotland lasted intermittently for several centuries – possibly the longest border war ever waged. During the civil war between Stephen and Matilda, David 1st of Scotland and his son were granted Cumbria and Northumberland respectively, so that for a period from 1139 to 1157, Newcastle was effectively in Scottish hands. It is believed that during this period, King David may have built the church of St Andrew and the Benedictine nunnery in Newcastle. However, King Stephen's successor, Henry II was strong enough to take back the Earldom of Northumbria from Malcolm IV.

 

The Scots king William the Lion was imprisoned in Newcastle, in 1174, after being captured at the Battle of Alnwick. Edward I brought the Stone of Scone and William Wallace south through the town and Newcastle was successfully defended against the Scots three times during the 14th century.

 

Around 1200, stone-faced, clay-filled jetties were starting to project into the river, an indication that trade was increasing in Newcastle. As the Roman roads continued to deteriorate, sea travel was gaining in importance. By 1275 Newcastle was the sixth largest wool exporting port in England. The principal exports at this time were wool, timber, coal, millstones, dairy produce, fish, salt and hides. Much of the developing trade was with the Baltic countries and Germany. Most of the Newcastle merchants were situated near the river, below the Castle. The earliest known charter was dated 1175 in the reign of Henry II, giving the townspeople some control over their town. In 1216 King John granted Newcastle a mayor[8] and also allowed the formation of guilds (known as Mysteries). These were cartels formed within different trades, which restricted trade to guild members. There were initially twelve guilds. Coal was being exported from Newcastle by 1250, and by 1350 the burgesses received a royal licence to export coal. This licence to export coal was jealously guarded by the Newcastle burgesses, and they tried to prevent any one else on the Tyne from exporting coal except through Newcastle. The burgesses similarly tried to prevent fish from being sold anywhere else on the Tyne except Newcastle. This led to conflicts with Gateshead and South Shields.

 

In 1265, the town was granted permission to impose a 'Wall Tax' or Murage, to pay for the construction of a fortified wall to enclose the town and protect it from Scottish invaders. The town walls were not completed until early in the 14th century. They were two miles (3 km) long, 9 feet (2.7 m) thick and 25 feet (7.6 m) high. They had six main gates, as well as some smaller gates, and had 17 towers. The land within the walls was divided almost equally by the Lort Burn, which flowed southwards and joined the Tyne to the east of the Castle. The town began to expand north of the Castle and west of the Lort Burn with various markets being set up within the walls.

 

In 1400 Henry IV granted a new charter, creating a County corporate which separated the town, but not the Castle, from the county of Northumberland and recognised it as a "county of itself" with a right to have a sheriff of its own. The burgesses were now allowed to choose six aldermen who, with the mayor would be justices of the peace. The mayor and sheriff were allowed to hold borough courts in the Guildhall.

 

Religious houses

During the Middle Ages a number of religious houses were established within the walls: the first of these was the Benedictine nunnery of St Bartholomew founded in 1086 near the present-day Nun Street. Both David I of Scotland and Henry I of England were benefactors of the religious house. Nothing of the nunnery remains now.

 

The friary of Blackfriars, Newcastle (Dominican) was established in 1239. These were also known as the Preaching Friars or Shod Friars, because they wore sandals, as opposed to other orders. The friary was situated in the present-day Friars Street. In 1280 the order was granted royal permission to make a postern in the town walls to communicate with their gardens outside the walls. On 19 June 1334, Edward Balliol, claimant to be King of Scotland, did homage to King Edward III, on behalf of the kingdom of Scotland, in the church of the friary. Much of the original buildings of the friary still exist, mainly because, after the Dissolution of the Monasteries the friary of Blackfriars was rented out by the corporation to nine of the local trade guilds.

 

The friary of Whitefriars (Carmelite) was established in 1262. The order was originally housed on the Wall Knoll in Pandon, but in 1307 it took over the buildings of another order, which went out of existence, the Friars of the Sac. The land, which had originally been given by Robert the Bruce, was situated in the present-day Hanover Square, behind the Central station. Nothing of the friary remains now.

 

The friary of Austinfriars (Augustinian) was established in 1290. The friary was on the site where the Holy Jesus Hospital was built in 1682. The friary was traditionally the lodging place of English kings whenever they visited or passed through Newcastle. In 1503 Princess Margaret, eldest daughter of Henry VII of England, stayed two days at the friary on her way to join her new husband James IV of Scotland.

 

The friary of Greyfriars (Franciscans) was established in 1274. The friary was in the present-day area between Pilgrim Street, Grey Street, Market Street and High Chare. Nothing of the original buildings remains.

 

The friary of the Order of the Holy Trinity, also known as the Trinitarians, was established in 1360. The order devoted a third of its income to buying back captives of the Saracens, during the Crusades. Their house was on the Wall Knoll, in Pandon, to the east of the city, but within the walls. Wall Knoll had previously been occupied by the White Friars until they moved to new premises in 1307.

 

All of the above religious houses were closed in about 1540, when Henry VIII dissolved the monasteries.

 

An important street running through Newcastle at the time was Pilgrim Street, running northwards inside the walls and leading to the Pilgrim Gate on the north wall. The street still exists today as arguably Newcastle's main shopping street.

 

Tudor period

The Scottish border wars continued for much of the 16th century, so that during that time, Newcastle was often threatened with invasion by the Scots, but also remained important as a border stronghold against them.

 

During the Reformation begun by Henry VIII in 1536, the five Newcastle friaries and the single nunnery were dissolved and the land was sold to the Corporation and to rich merchants. At this time there were fewer than 60 inmates of the religious houses in Newcastle. The convent of Blackfriars was leased to nine craft guilds to be used as their headquarters. This probably explains why it is the only one of the religious houses whose building survives to the present day. The priories at Tynemouth and Durham were also dissolved, thus ending the long-running rivalry between Newcastle and the church for control of trade on the Tyne. A little later, the property of the nunnery of St Bartholomew and of Grey Friars were bought by Robert Anderson, who had the buildings demolished to build his grand Newe House (also known as Anderson Place).

 

With the gradual decline of the Scottish border wars the town walls were allowed to decline as well as the castle. By 1547, about 10,000 people were living in Newcastle. At the beginning of the 16th century exports of wool from Newcastle were more than twice the value of exports of coal, but during the century coal exports continued to increase.

 

Under Edward VI, John Dudley, Duke of Northumberland, sponsored an act allowing Newcastle to annexe Gateshead as its suburb. The main reason for this was to allow the Newcastle Hostmen, who controlled the export of Tyne coal, to get their hands on the Gateshead coal mines, previously controlled by the Bishop of Durham. However, when Mary I came to power, Dudley met his downfall and the decision was reversed. The Reformation allowed private access to coal mines previously owned by Tynemouth and Durham priories and as a result coal exports increase dramatically, from 15,000 tons in 1500 to 35,000 tons in 1565, and to 400,000 tons in 1625.

 

The plague visited Newcastle four times during the 16th century, in 1579 when 2,000 people died, in 1589 when 1700 died, in 1595 and finally in 1597.

 

In 1600 Elizabeth I granted Newcastle a charter for an exclusive body of electors, the right to elect the mayor and burgesses. The charter also gave the Hostmen exclusive rights to load coal at any point on the Tyne. The Hostmen developed as an exclusive group within the Merchant Adventurers who had been incorporated by a charter in 1547.

 

Stuart period

In 1636 there was a serious outbreak of bubonic plague in Newcastle. There had been several previous outbreaks of the disease over the years, but this was the most serious. It is thought to have arrived from the Netherlands via ships that were trading between the Tyne and that country. It first appeared in the lower part of the town near the docks but gradually spread to all parts of the town. As the disease gained hold the authorities took measures to control it by boarding up any properties that contained infected persons, meaning that whole families were locked up together with the infected family members. Other infected persons were put in huts outside the town walls and left to die. Plague pits were dug next to the town's four churches and outside the town walls to receive the bodies in mass burials. Over the course of the outbreak 5,631 deaths were recorded out of an estimated population of 12,000, a death rate of 47%.

 

In 1637 Charles I tried to raise money by doubling the 'voluntary' tax on coal in return for allowing the Newcastle Hostmen to regulate production and fix prices. This caused outrage amongst the London importers and the East Anglian shippers. Both groups decided to boycott Tyne coal and as a result forced Charles to reverse his decision in 1638.

 

In 1640 during the Second Bishops' War, the Scots successfully invaded Newcastle. The occupying army demanded £850 per day from the Corporation to billet the Scottish troops. Trade from the Tyne ground to a halt during the occupation. The Scots left in 1641 after receiving a Parliamentary pardon and a £4,000,000 loan from the town.

 

In 1642 the English Civil War began. King Charles realised the value of the Tyne coal trade and therefore garrisoned Newcastle. A Royalist was appointed as governor. At that time, Newcastle and King's Lynn were the only important seaports to support the crown. In 1644 Parliament blockaded the Tyne to prevent the king from receiving revenue from the Tyne coal trade. Coal exports fell from 450,000 to 3,000 tons and London suffered a hard winter without fuel. Parliament encouraged the coal trade from the Wear to try to replace that lost from Newcastle but that was not enough to make up for the lost Tyneside tonnage.

 

In 1644 the Scots crossed the border. Newcastle strengthened its defences in preparation. The Scottish army, with 40,000 troops, besieged Newcastle for three months until the garrison of 1,500 surrendered. During the siege, the Scots bombarded the walls with their artillery, situated in Gateshead and Castle Leazes. The Scottish commander threatened to destroy the steeple of St Nicholas's Church by gunfire if the mayor, Sir John Marley, did not surrender the town. The mayor responded by placing Scottish prisoners that they had captured in the steeple, so saving it from destruction. The town walls were finally breached by a combination of artillery and sapping. In gratitude for this defence, Charles gave Newcastle the motto 'Fortiter Defendit Triumphans' to be added to its coat of arms. The Scottish army occupied Northumberland and Durham for two years. The coal taxes had to pay for the Scottish occupation. In 1645 Charles surrendered to the Scots and was imprisoned in Newcastle for nine months. After the Civil War the coal trade on the Tyne soon picked up and exceeded its pre-war levels.

 

A new Guildhall was completed on the Sandhill next to the river in 1655, replacing an earlier facility damaged by fire in 1639, and became the meeting place of Newcastle Town Council. In 1681 the Hospital of the Holy Jesus was built partly on the site of the Austin Friars. The Guildhall and Holy Jesus Hospital still exist.

 

Charles II tried to impose a charter on Newcastle to give the king the right to appoint the mayor, sheriff, recorder and town clerk. Charles died before the charter came into effect. In 1685, James II tried to replace Corporation members with named Catholics. However, James' mandate was suspended in 1689 after the Glorious Revolution welcoming William of Orange. In 1689, after the fall of James II, the people of Newcastle tore down his bronze equestrian statue in Sandhill and tossed it into the Tyne. The bronze was later used to make bells for All Saints Church.

 

In 1689 the Lort Burn was covered over. At this time it was an open sewer. The channel followed by the Lort Burn became the present day Dean Street. At that time, the centre of Newcastle was still the Sandhill area, with many merchants living along the Close or on the Side. The path of the main road through Newcastle ran from the single Tyne bridge, through Sandhill to the Side, a narrow street which climbed steeply on the north-east side of the castle hill until it reached the higher ground alongside St Nicholas' Church. As Newcastle developed, the Side became lined with buildings with projecting upper stories, so that the main street through Newcastle was a narrow, congested, steep thoroughfare.

 

In 1701 the Keelmen's Hospital was built in the Sandgate area of the city, using funds provided by the keelmen. The building still stands today.

 

Eighteenth century

In the 18th century, Newcastle was the country's largest print centre after London, Oxford and Cambridge, and the Literary and Philosophical Society of 1793, with its erudite debates and large stock of books in several languages predated the London Library by half a century.

 

In 1715, during the Jacobite rising in favour of the Old Pretender, an army of Jacobite supporters marched on Newcastle. Many of the Northumbrian gentry joined the rebels. The citizens prepared for its arrival by arresting Jacobite supporters and accepting 700 extra recruits into the local militia. The gates of the city were closed against the rebels. This proved enough to delay an attack until reinforcements arrived forcing the rebel army to move across to the west coast. The rebels finally surrendered at Preston.

 

In 1745, during a second Jacobite rising in favour of the Young Pretender, a Scottish army crossed the border led by Bonnie Prince Charlie. Once again Newcastle prepared by arresting Jacobite supporters and inducting 800 volunteers into the local militia. The town walls were strengthened, most of the gates were blocked up and some 200 cannon were deployed. 20,000 regulars were billeted on the Town Moor. These preparations were enough to force the rebel army to travel south via the west coast. They were eventually defeated at Culloden in 1746.

 

Newcastle's actions during the 1715 rising in resisting the rebels and declaring for George I, in contrast to the rest of the region, is the most likely source of the nickname 'Geordie', applied to people from Tyneside, or more accurately Newcastle. Another theory, however, is that the name 'Geordie' came from the inventor of the Geordie lamp, George Stephenson. It was a type of safety lamp used in mining, but was not invented until 1815. Apparently the term 'German Geordie' was in common use during the 18th century.

 

The city's first hospital, Newcastle Infirmary opened in 1753; it was funded by public subscription. A lying-in hospital was established in Newcastle in 1760. The city's first public hospital for mentally ill patients, Wardens Close Lunatic Hospital was opened in October 1767.

 

In 1771 a flood swept away much of the bridge at Newcastle. The bridge had been built in 1250 and repaired after a flood in 1339. The bridge supported various houses and three towers and an old chapel. A blue stone was placed in the middle of the bridge to mark the boundary between Newcastle and the Palatinate of Durham. A temporary wooden bridge had to be built, and this remained in use until 1781, when a new stone bridge was completed. The new bridge consisted of nine arches. In 1801, because of the pressure of traffic, the bridge had to be widened.

 

A permanent military presence was established in the city with the completion of Fenham Barracks in 1806. The facilities at the Castle for holding assizes, which had been condemned for their inconvenience and unhealthiness, were replaced when the Moot Hall opened in August 1812.

 

Victorian period

Present-day Newcastle owes much of its architecture to the work of the builder Richard Grainger, aided by architects John Dobson, Thomas Oliver, John and Benjamin Green and others. In 1834 Grainger won a competition to produce a new plan for central Newcastle. He put this plan into effect using the above architects as well as architects employed in his own office. Grainger and Oliver had already built Leazes Terrace, Leazes Crescent and Leazes Place between 1829 and 1834. Grainger and Dobson had also built the Royal Arcade at the foot of Pilgrim Street between 1830 and 1832. The most ambitious project covered 12 acres 12 acres (49,000 m2) in central Newcastle, on the site of Newe House (also called Anderson Place). Grainger built three new thoroughfares, Grey Street, Grainger Street and Clayton Street with many connecting streets, as well as the Central Exchange and the Grainger Market. John Wardle and George Walker, working in Grainger's office, designed Clayton Street, Grainger Street and most of Grey Street. Dobson designed the Grainger Market and much of the east side of Grey Street. John and Benjamin Green designed the Theatre Royal at the top of Grey Street, where Grainger placed the column of Grey's Monument as a focus for the whole scheme. Grey Street is considered to be one of the finest streets in the country, with its elegant curve. Unfortunately most of old Eldon Square was demolished in the 1960s in the name of progress. The Royal Arcade met a similar fate.

 

In 1849 a new bridge was built across the river at Newcastle. This was the High Level Bridge, designed by Robert Stephenson, and slightly up river from the existing bridge. The bridge was designed to carry road and rail traffic across the Tyne Gorge on two decks with rail traffic on the upper deck and road traffic on the lower. The new bridge meant that traffic could pass through Newcastle without having to negotiate the steep, narrow Side, as had been necessary for centuries. The bridge was opened by Queen Victoria, who one year later opened the new Central Station, designed by John Dobson. Trains were now able to cross the river, directly into the centre of Newcastle and carry on up to Scotland. The Army Riding School was also completed in 1849.

 

In 1854 a large fire started on the Gateshead quayside and an explosion caused it to spread across the river to the Newcastle quayside. A huge conflagration amongst the narrow alleys, or 'chares', destroyed the homes of 800 families as well as many business premises. The narrow alleys that had been destroyed were replaced by streets containing blocks of modern offices.

 

In 1863 the Town Hall in St Nicholas Square replaced the Guildhall as the meeting place of Newcastle Town Council.

 

In 1876 the low level bridge was replaced by a new bridge known as the Swing Bridge, so called because the bridge was able to swing horizontally on a central axis and allow ships to pass on either side. This meant that for the first time sizeable ships could pass up-river beyond Newcastle. The bridge was built and paid for by William Armstrong, a local arms manufacturer, who needed to have warships access his Elswick arms factory to fit armaments to them. The Swing Bridge's rotating mechanism is adapted from the cannon mounts developed in Armstrong's arms works. In 1882 the Elswick works began to build ships as well as to arm them. The Barrack Road drill hall was completed in 1890.

 

Industrialisation

In the 19th century, shipbuilding and heavy engineering were central to the city's prosperity; and the city was a powerhouse of the Industrial Revolution. Newcastle's development as a major city owed most to its central role in the production and export of coal. The phrase "taking coals to Newcastle" was first recorded in 1538; it proverbially denotes bringing a particular commodity to a place that has more than enough of it already.

 

Innovation in Newcastle and surrounding areas included the following:

 

George Stephenson developed a miner's safety lamp at the same time that Humphry Davy developed a rival design. The lamp made possible the opening up of ever deeper mines to provide the coal that powered the industrial revolution.

George and his son Robert Stephenson were hugely influential figures in the development of the early railways. George developed Blücher, a locomotive working at Killingworth colliery in 1814, whilst Robert was instrumental in the design of Rocket, a revolutionary design that was the forerunner of modern locomotives. Both men were involved in planning and building railway lines, all over this country and abroad.

 

Joseph Swan demonstrated a working electric light bulb about a year before Thomas Edison did the same in the USA. This led to a dispute as to who had actually invented the light bulb. Eventually the two rivals agreed to form a mutual company between them, the Edison and Swan Electric Light Company, known as Ediswan.

 

Charles Algernon Parsons invented the steam turbine, for marine use and for power generation. He used Turbinia, a small, turbine-powered ship, to demonstrate the speed that a steam turbine could generate. Turbinia literally ran rings around the British Fleet at a review at Spithead in 1897.

 

William Armstrong invented a hydraulic crane that was installed in dockyards up and down the country. He then began to design light, accurate field guns for the British army. These were a vast improvement on the existing guns that were then in use.

 

The following major industries developed in Newcastle or its surrounding area:

 

Glassmaking

A small glass industry existed in Newcastle from the mid-15th century. In 1615 restrictions were put on the use of wood for manufacturing glass. It was found that glass could be manufactured using the local coal, and so a glassmaking industry grew up on Tyneside. Huguenot glassmakers came over from France as refugees from persecution and set up glasshouses in the Skinnerburn area of Newcastle. Eventually, glass production moved to the Ouseburn area of Newcastle. In 1684 the Dagnia family, Sephardic Jewish emigrants from Altare, arrived in Newcastle from Stourbridge and established glasshouses along the Close, to manufacture high quality flint glass. The glass manufacturers used sand ballast from the boats arriving in the river as the main raw material. The glassware was then exported in collier brigs. The period from 1730 to 1785 was the highpoint of Newcastle glass manufacture, when the local glassmakers produced the 'Newcastle Light Baluster'. The glassmaking industry still exists in the west end of the city with local Artist and Glassmaker Jane Charles carrying on over four hundred years of hot glass blowing in Newcastle upon Tyne.

 

Locomotive manufacture

In 1823 George Stephenson and his son Robert established the world's first locomotive factory near Forth Street in Newcastle. Here they built locomotives for the Stockton and Darlington Railway and the Liverpool and Manchester Railway, as well as many others. It was here that the famous locomotive Rocket was designed and manufactured in preparation for the Rainhill Trials. Apart from building locomotives for the British market, the Newcastle works also produced locomotives for Europe and America. The Forth Street works continued to build locomotives until 1960.

 

Shipbuilding

In 1296 a wooden, 135 ft (41 m) long galley was constructed at the mouth of the Lort Burn in Newcastle, as part of a twenty-ship order from the king. The ship cost £205, and is the earliest record of shipbuilding in Newcastle. However the rise of the Tyne as a shipbuilding area was due to the need for collier brigs for the coal export trade. These wooden sailing ships were usually built locally, establishing local expertise in building ships. As ships changed from wood to steel, and from sail to steam, the local shipbuilding industry changed to build the new ships. Although shipbuilding was carried out up and down both sides of the river, the two main areas for building ships in Newcastle were Elswick, to the west, and Walker, to the east. By 1800 Tyneside was the third largest producer of ships in Britain. Unfortunately, after the Second World War, lack of modernisation and competition from abroad gradually caused the local industry to decline and die.

 

Armaments

In 1847 William Armstrong established a huge factory in Elswick, west of Newcastle. This was initially used to produce hydraulic cranes but subsequently began also to produce guns for both the army and the navy. After the Swing Bridge was built in 1876 allowing ships to pass up river, warships could have their armaments fitted alongside the Elswick works. Armstrong's company took over its industrial rival, Joseph Whitworth of Manchester in 1897.

 

Steam turbines

Charles Algernon Parsons invented the steam turbine and, in 1889, founded his own company C. A. Parsons and Company in Heaton, Newcastle to make steam turbines. Shortly after this, he realised that steam turbines could be used to propel ships and, in 1897, he founded a second company, Parsons Marine Steam Turbine Company in Wallsend. It is there that he designed and manufactured Turbinia. Parsons turbines were initially used in warships but soon came to be used in merchant and passenger vessels, including the liner Mauretania which held the blue riband for the Atlantic crossing until 1929. Parsons' company in Heaton began to make turbo-generators for power stations and supplied power stations all over the world. The Heaton works, reduced in size, remains as part of the Siemens AG industrial giant.

 

Pottery

In 1762 the Maling pottery was founded in Sunderland by French Huguenots, but transferred to Newcastle in 1817. A factory was built in the Ouseburn area of the city. The factory was rebuilt twice, finally occupying a 14-acre (57,000 m2) site that was claimed to be the biggest pottery in the world and which had its own railway station. The pottery pioneered use of machines in making potteries as opposed to hand production. In the 1890s the company went up-market and employed in-house designers. The period up to the Second World War was the most profitable with a constant stream of new designs being introduced. However, after the war, production gradually declined and the company closed in 1963.

 

Expansion of the city

Newcastle was one of the boroughs reformed by the Municipal Corporations Act 1835: the reformed municipal borough included the parishes of Byker, Elswick, Heaton, Jesmond, Newcastle All Saints, Newcastle St Andrew, Newcastle St John, Newcastle St Nicholas, and Westgate. The urban districts of Benwell and Fenham and Walker were added in 1904. In 1935, Newcastle gained Kenton and parts of the parishes of West Brunton, East Denton, Fawdon, Longbenton. The most recent expansion in Newcastle's boundaries took place under the Local Government Act 1972 on 1 April 1974, when Newcastle became a metropolitan borough, also including the urban districts of Gosforth and Newburn, and the parishes of Brunswick, Dinnington, Hazlerigg, North Gosforth and Woolsington from the Castle Ward Rural District, and the village of Westerhope.

 

Meanwhile Northumberland County Council was formed under the Local Government Act 1888 and benefited from a dedicated meeting place when County Hall was completed in the Castle Garth area of Newcastle in 1910. Following the Local Government Act 1972 County Hall relocated to Morpeth in April 1981.

 

Twentieth century

In 1925 work began on a new high-level road bridge to span the Tyne Gorge between Newcastle and Gateshead. The capacity of the existing High-Level Bridge and Swing Bridge were being strained to the limit, and an additional bridge had been discussed for a long time. The contract was awarded to the Dorman Long Company and the bridge was finally opened by King George V in 1928. The road deck was 84 feet (26 m) above the river and was supported by a 531 feet (162 m) steel arch. The new Tyne Bridge quickly became a symbol for Newcastle and Tyneside, and remains so today.

 

During the Second World War, Newcastle was largely spared the horrors inflicted upon other British cities bombed during the Blitz. Although the armaments factories and shipyards along the River Tyne were targeted by the Luftwaffe, they largely escaped unscathed. Manors goods yard and railway terminal, to the east of the city centre, and the suburbs of Jesmond and Heaton suffered bombing during 1941. There were 141 deaths and 587 injuries, a relatively small figure compared to the casualties in other industrial centres of Britain.

 

In 1963 the city gained its own university, the University of Newcastle upon Tyne, by act of parliament. A School of Medicine and Surgery had been established in Newcastle in 1834. This eventually developed into a college of medicine attached to Durham University. A college of physical science was also founded and became Armstrong College in 1904. In 1934 the two colleges merged to become King's College, Durham. This remained as part of Durham University until the new university was created in 1963. In 1992 the city gained its second university when Newcastle Polytechnic was granted university status as Northumbria University.

 

Newcastle City Council moved to the new Newcastle Civic Centre in 1968.

 

As heavy industries declined in the second half of the 20th century, large sections of the city centre were demolished along with many areas of slum housing. The leading political figure in the city during the 1960s was T. Dan Smith who oversaw a massive building programme of highrise housing estates and authorised the demolition of a quarter of the Georgian Grainger Town to make way for Eldon Square Shopping Centre. Smith's control in Newcastle collapsed when it was exposed that he had used public contracts to advantage himself and his business associates and for a time Newcastle became a byword for civic corruption as depicted in the films Get Carter and Stormy Monday and in the television series Our Friends in the North. However, much of the historic Grainger Town area survived and was, for the most part, fully restored in the late 1990s. Northumberland Street, initially the A1, was gradually closed to traffic from the 1970s and completely pedestrianised by 1998.

 

In 1978 a new rapid transport system, the Metro, was built, linking the Tyneside area. The system opened in August 1980. A new bridge was built to carry the Metro across the river between Gateshead and Newcastle. This was the Queen Elizabeth II Bridge, commonly known as the Metro Bridge. Eventually the Metro system was extended to reach Newcastle Airport in 1991, and in 2002 the Metro system was extended to the nearby city of Sunderland.

 

As the 20th century progressed, trade on the Newcastle and Gateshead quaysides gradually declined, until by the 1980s both sides of the river were looking rather derelict. Shipping company offices had closed along with offices of firms related to shipping. There were also derelict warehouses lining the riverbank. Local government produced a master plan to re-develop the Newcastle quayside and this was begun in the 1990s. New offices, restaurants, bars and residential accommodation were built and the area has changed in the space of a few years into a vibrant area, partially returning the focus of Newcastle to the riverside, where it was in medieval times.

 

The Gateshead Millennium Bridge, a foot and cycle bridge, 26 feet (7.9 m) wide and 413 feet (126 m) long, was completed in 2001. The road deck is in the form of a curve and is supported by a steel arch. To allow ships to pass, the whole structure, both arch and road-deck, rotates on huge bearings at either end so that the road deck is lifted. The bridge can be said to open and shut like a human eye. It is an important addition to the re-developed quayside area, providing a vital link between the Newcastle and Gateshead quaysides.

 

Recent developments

Today the city is a vibrant centre for office and retail employment, but just a short distance away there are impoverished inner-city housing estates, in areas originally built to provide affordable housing for employees of the shipyards and other heavy industries that lined the River Tyne. In the 2010s Newcastle City Council began implementing plans to regenerate these depressed areas, such as those along the Ouseburn Valley.

The picturesque coastal village of Glandore, County Cork.

Includes Legacy Mesh Body appliers and BOM layers for Maitreya, Legacy and Reborn!

 

Full coverage panties in 8 cute colors ♥

 

www.facebook.com/AetronResident/

 

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Includes: Pumpkin Bench, 2 wooden carved pumpkins with candles (glows a warm orange glow), piles of leaves for the floor with individual sculpted leaves, harvest box, 2 different types of hanging maple garland, leaf and acorn mirror and maple and acorn wreath (not shown). Available until Sunday SLT midnight. Garlands and leaves are copyable.

 

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Aerial BMX action from the GAS Arena at the Goodwood Festival. They all landed safely from even the most extreme positions

Includes teams from Mitchell, Harrisburg, Watertown, Aberdeen 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

 

Friday at the Goodwood Revival. A bright, low 'bow after a brief shower.

The Wartturm feature at Bastei, Saxony. A large part of the feature broke off 15 years ago sending 800 tonnes of rock crashing down en.wikipedia.org/wiki/Wartturm_%28crag%29

 

Worn or weathered #56 in 115 pictures

Vogue Nippon (Japan) Editorial

 

"Follow That Woman" (a.k.a. "Chase The Lady")

 

Mikael Jansson - Photographer

 

Charles Devoe - Male Model

Edita Vilkeviciute - Model

Nil Hoppenot - Male Model

 

Flocked by a handsome pair of semi-nude super-hunks, recently married young top model Edita has a new found air of sexual maturity about her in this classic Vogue Nippon editorial.

“Follow That Woman” captures Edita spends her luxurious honeymoon in multiple locations on the Côte d'Azur, which include a super-luxe Riva "Aquarama" Runabout boat, beach and penthouse setting, all paid for by her newly-wed husband. But whether it’s for her hubby's money or her charming irresistible allure, one thing’s for sure, those sexy alpha males are really "following that woman", like bees to honey!

 

(please download to fully appreciate the image)

More rally car action from Firle Beacon

Passing the Vasco da Gama Bridge after leaving Lisbon airport

"The Woodstock Village Historic District was listed on the National Register of Historic Places in 1973. It includes the village center and additional properties along the Ottauquechee River. The district covers an area of 275 acres (111 ha) encompassing 95 buildings, sites, and structures that contribute to the historical significance of the area. The center of the district is an elliptical village green located at the junction of U.S. Route 4 and Vermont Route 106. Around the green and along the main road following the river are a number of residential, commercial, and public buildings showcasing architectural development from the late 18th to late 19th centuries. One of these buildings is The Norman Williams Public Library, built by Norman's son, Dr. Edward H. Williams, on the site where their home had stood previously. The district also includes the Billings Farm and Museum, and the George Perkins Marsh Boyhood Home, the architectural centerpiece of Marsh-Billings-Rockefeller National Historical Park, and F. H. Gillingham & Sons, the oldest, same-family operated general store in Vermont.

 

Woodstock is the shire town (county seat) of Windsor County, Vermont, United States. As of the 2020 census, the town population was 3,005. It includes the villages of Woodstock, South Woodstock, Taftsville, and West Woodstock.

 

Chartered by New Hampshire Governor Benning Wentworth on July 10, 1761, the town was a New Hampshire grant to David Page and 61 others. It was named after Woodstock in Oxfordshire, England, as a homage to both Blenheim Palace and its owner, George Spencer, 4th Duke of Marlborough. The town was first settled in 1768 by James Sanderson and his family. In 1776, Joab Hoisington built a gristmill, followed by a sawmill, on the south branch of the Ottauquechee River. The town was incorporated in 1837.

 

Although the Revolution slowed settlement, Woodstock developed rapidly once the war ended in 1783. The Vermont General Assembly met here in 1807 before moving the next year to the new capital at Montpelier. Waterfalls in the Ottauquechee River provided water power to operate mills. Factories made scythes and axes, carding machines, and woolens. There was a machine shop and gunsmith shop. Manufacturers also produced furniture, wooden wares, window sashes and blinds. Carriages, horse harnesses, saddles, luggage trunks and leather goods were also manufactured. By 1859, the population was 3,041. The Woodstock Railroad opened to White River Junction on September 29, 1875, carrying freight and tourists. The Woodstock Inn opened in 1892.

 

The Industrial Revolution helped the town grow prosperous. The economy is now largely driven by tourism. Woodstock has the 20th highest per-capita income of Vermont towns as reported by the United States Census, and a high percentage of homes owned by non-residents. The town's central square, called the Green, is bordered by restored late Georgian, Federal Style, and Greek Revival houses. The cost of real estate in the district adjoining the Green is among the highest in the state. The seasonal presence of wealthy second-home owners from cities such as Boston and New York has contributed to the town's economic vitality and livelihood, while at the same time diminished its accessibility to native Vermonters.

 

The town maintains a free (paid for through taxation) community wi-fi internet service that covers most of the village of Woodstock, dubbed "Wireless Woodstock"." - info from Wikipedia.

 

The fall of 2022 I did my 3rd major cycling tour. I began my adventure in Montreal, Canada and finished in Savannah, GA. This tour took me through the oldest parts of Quebec and the 13 original US states. During this adventure I cycled 7,126 km over the course of 2.5 months and took more than 68,000 photos. As with my previous tours, a major focus was to photograph historic architecture.

 

Now on Instagram.

 

Become a patron to my photography on Patreon or donate.

"The Masonic Temple is a historic Masonic building in Philadelphia. Located at 1 North Broad Street, directly across from Philadelphia City Hall, it serves as the headquarters of the Grand Lodge of Pennsylvania, Free and Accepted Masons. The Temple features the Masonic Library and Museum of Pennsylvania, and receives thousands of visitors every year to view the ornate structure, which includes seven lodge rooms, where today a number of Philadelphia lodges and the Grand Lodge conduct their meetings.

 

The Temple was designed in the medieval Norman style by James H. Windrim, who was 27 years old at the time he won the design competition. The massive granite cornerstone, weighing ten tons, was leveled on St. John the Baptist's Day, June 24, 1868. The ceremonial gavel used on that day by Grand Master Richard Vaux was the same gavel used by President George Washington in leveling the cornerstone of the nation's Capitol building in 1793.

 

The construction was completed five years later, in 1873. The interior, designed by George Herzog, was begun in 1887 and took another fifteen years to finish.

 

The bold and elaborate elevations on Broad and Filbert Streets, especially the beautiful portico of Quincy granite, make it one of the great architectural wonders of Philadelphia. The exterior stone of the building on Broad and Filbert Streets is Cape Ann Syenite from Syne in Upper Egypt.

 

On May 27, 1971, the Temple was listed on the National Register of Historic Places. It was designated a National Historic Landmark in 1985. It was cited in its landmark designation as one of the nation's most elaborate examples of Masonic architecture.

 

Philadelphia, often called Philly, is the largest city in the Commonwealth of Pennsylvania, the sixth-largest city in the U.S., the second-largest city in both the Northeast megalopolis and Mid-Atlantic regions after New York City, and the 68th-largest city in the world. Since 1854, the city has been coextensive with Philadelphia County, the most populous county in Pennsylvania and the urban core of the Delaware Valley, the nation's seventh-largest and world's 68th-largest metropolitan region, with 6.245 million residents as of 2020. The city's population as of the 2020 census was 1,603,797, and over 56 million people live within 250 mi (400 km) of Philadelphia.

 

Philadelphia was founded in 1682 by William Penn, an English Quaker. The city served as capital of the Pennsylvania Colony during the British colonial era and went on to play a historic and vital role as the central meeting place for the nation's founding fathers whose plans and actions in Philadelphia ultimately inspired the American Revolution and the nation's independence. Philadelphia hosted the First Continental Congress in 1774 following the Boston Tea Party, preserved the Liberty Bell, and hosted the Second Continental Congress during which the founders signed the Declaration of Independence, which historian Joseph Ellis has described as "the most potent and consequential words in American history". Once the Revolutionary War commenced, both the Battle of Germantown and the Siege of Fort Mifflin were fought within Philadelphia's city limits. The U.S. Constitution was later ratified in Philadelphia at the Philadelphia Convention of 1787. Philadelphia remained the nation's largest city until 1790, when it was surpassed by New York City, and served as the nation's first capital from May 10, 1775, until December 12, 1776, and on four subsequent occasions during and following the American Revolution, including from 1790 to 1800 while the new national capital of Washington, D.C. was under construction.

 

During the 19th and 20th centuries, Philadelphia emerged as a major national industrial center and railroad hub. The city’s blossoming industrial sector attracted European immigrants, predominantly from Germany and Ireland, the two largest reported ancestry groups in the city as of 2015. In the 20th century, immigrant waves from Italy and elsewhere in Southern Europe arrived. Following the end of the Civil War in 1865, Philadelphia became a leading destination for African Americans in the Great Migration. In the 20th century, Puerto Rican Americans moved to the city in large numbers. Between 1890 and 1950, Philadelphia's population doubled to 2.07 million. Philadelphia has since attracted immigrants from East and South Asia, Eastern Europe, and Latin America.

 

With 18 four-year universities and colleges, Philadelphia is one of the nation's leading centers for higher education and academic research. As of 2021, the Philadelphia metropolitan area was the nation's ninth-largest metropolitan economy with a gross metropolitan product (GMP) of US$479 billion. Philadelphia is the largest center of economic activity in Pennsylvania and the broader multi-state Delaware Valley region; the city is home to five Fortune 500 corporate headquarters as of 2022. The Philadelphia skyline, which includes several globally renowned commercial skyscrapers, is expanding, primarily with new residential high-rise condominiums. The city and the Delaware Valley are a biotechnology and venture capital hub; and the Philadelphia Stock Exchange, owned by NASDAQ, is the nation's oldest stock exchange and a global leader in options trading. 30th Street Station, the city's primary rail station, is the third-busiest Amtrak hub in the nation, and the city's multimodal transport and logistics infrastructure, including Philadelphia International Airport, the PhilaPort seaport, freight rail infrastructure, roadway traffic capacity, and warehouse storage space, are all expanding.

 

Philadelphia is a national cultural hub, hosting more outdoor sculptures and murals than any other American city. Fairmount Park, when combined with adjacent Wissahickon Valley Park in the same watershed, is 2,052 acres (830 ha), representing one of the nation's largest contiguous urban parks and the 45th largest urban park in the world. The city is known for its arts, culture, cuisine, and colonial and Revolution-era history; in 2016, it attracted 42 million domestic tourists who spent $6.8 billion, representing $11 billion in total economic impact to the city and surrounding Pennsylvania counties.

 

With five professional sports teams and a hugely loyal fan base, the city is often ranked as the nation's best city for professional sports fans. The city has a culturally and philanthropically active LGBTQ+ community. Philadelphia also has played an immensely influential historic and ongoing role in the development and evolution of American music, especially R&B, soul, and rock.

 

Philadelphia is a city of many firsts, including the nation's first library (1731), hospital (1751), medical school (1765), national capital (1774), university (by some accounts) (1779), stock exchange (1790), zoo (1874), and business school (1881). Philadelphia contains 67 National Historic Landmarks, including Independence Hall. From the city's 17th century founding through the present, Philadelphia has been the birthplace or home to an extensive number of prominent and influential Americans. In 2021, Time magazine named Philadelphia one of the world's greatest 100 places." - info from Wikipedia.

 

The fall of 2022 I did my 3rd major cycling tour. I began my adventure in Montreal, Canada and finished in Savannah, GA. This tour took me through the oldest parts of Quebec and the 13 original US states. During this adventure I cycled 7,126 km over the course of 2.5 months and took more than 68,000 photos. As with my previous tours, a major focus was to photograph historic architecture.

 

Now on Instagram.

 

Become a patron to my photography on Patreon or donate.

08/10/17. #1742. Warm and sunny for a display of classic cars at Stanmer House, Brighton. This tiny Fiat clearly has BIG ideas.

 

‏‏‎ ‏‏‎

· ▸ Kitchen Cleaning Supplies includes:

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ㅤㅤ• 3 Wearable Pairs · R + L Hands

ㅤㅤ• 14 Decor items

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· ▸ Land Impacts · 1 - 2 Each

‏‏‎ ‏‏‎

· ▸ Materials Enabled

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· ▸ Copy

· ▸ Modify

· ▸ No Transfer

‏‏‎ ‏‏‎

ㅤㅤｓｈｏｐ ｔｈｉｓ ａｔ ｅｑｕａｌ１０ 苛 尉 ズ ょ ド

ㅤㅤ

▸ Ｊｏｉｎ　ｕｓ　ｏｎ　Ｐｒｉｍｆｅｅｄ

ㅤㅤ

▸ Ｊｏｉｎ　ｕｓ　ｏｎ　Ｆａｃｅｂｏｏｋ

ㅤㅤ

▸ Ｊｏｉｎ　ｕｓ　ｏｎ　Ｉｎｓｔａｇｒａｍ

ㅤㅤ

▸ Ｊｏｉｎ　ｕｓ　ｏｎ　Ｙｏｕｔｕｂｅ

ㅤㅤ

▸ Main Sim

ㅤㅤ

▸ Cam sim 1

ㅤㅤ

▸ Cam sim 2

Includes Farmers Market in Marion Square, Charleston, South Carolina, and Pride Parade 2016

Includes teams from Estelline/Hendricks, Chamberlain, Milbank Area, Wall/Kadoka Area/Philip and Sisseton. 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 7 minifigures with assorted weapons and accessories: King Ulysses, 2 Ardun soldiers, Rothut, 2 Ustokal warriors, and an Ustokal archer

♥ Includes Exclusive Textures ♥

Winter Release of Farrah Winter Leather & Faux Fur with Tank Duo

 

Marketplace Here: marketplace.secondlife.com/p/GH-Farrah-Leather-Fur-Scarf-...

Inworld Here: maps.secondlife.com/secondlife/Cevedale/99/18/315

 

 

TD:: Lace Jeans Outfit [Mesh] DEMO + Lara X

★★★ MESH OUTFIT★★★

════════════════════════════════════════════════════

➣ Includes:

 

• Mesh Shirt

• Mesh Jeans

 

• Texture HUD Driven

 

════════════════════════════════════════════════════

➣ Compatible with:

 

➠ LARA X, Petite

➠ MAITREYA, Petite

➠ LEGACY, Perky

➠ REBORN, Waifus

➠ GENX, Curvy

➠ KUPRA

➠ ERIKA

 

════════════════════════════════════════════════════

★ Before buying, please try the free demo.

 

★ Thank you for shopping at ::TIFFANY DESIGNS:: !

 

☎ In world assistance if you need additional help - please contact LucyHope.

 

See item in Second Life

  

TRUTH Tempted

 

LaraX

 

Lyrium Hali Static 2 [m]

gabbyjaws.blogspot.com/2024/12/still-crazy-for-christmas....

Tiffany Designs Eve Christmas Gown [Mesh] DEMO + Lara X

★★★ MESH XMAS GOWN ★★★

 

════════════════════════════════════════════════════

➣ Includes:

 

• Mesh Bra Bow

• Mesh Dress

• Mesh Gloves

• Mesh Fur

• Mesh Headbox

• Mesh Spine Decorations/lights

• Mesh Jewelry

• Glitter Emitter (white stars)

 

════════════════════════════════════════════════════

➣ Compatible with:

 

➠ LARA X

➠ MAITREYA

➠ LEGACY, Perky

➠ REBORN

➠ GENX, Curvy

➠ KUPRA

➠ ERIKA

 

════════════════════════════════════════════════════

★ Before buying, please try the free demo.

 

★ Thank you for shopping at ::TIFFANY DESIGNS:: !

 

☎ In world assistance if you need additional help - please contact LucyHope.

 

Tiffany Designs

 

LM: maps.secondlife.com/secondlife/Hilton%20Villas/232/207/22

 

MP: marketplace.secondlife.com/stores/139726?

 

NOVA Gigi group gift

 

LaraX

Includes teams from Mitchell, Harrisburg, Watertown, Aberdeen 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 Bento ears and tail.

2 FATPACK EXCLUSIVE colors

Female/femboi omega

HappyPaw Foxcat Head Appliers

marketplace.secondlife.com/p/SS-Chibi-Floof-Fatpack-Omega...

Spring was in the air at Sompting this afternoon.

The new REBIRTH RoX head series include features never seen before in other heads.

 

In addition to common features like HD layers, RoX heads innovate with features like :

- Brand new FX layers to play with amazing effects or create your owns with the devkit inworld.

 

- Moods that include original and customizable sound FX with your own sounds (devkit available in the store).

 

- Animations synchronized with the smile FX for an even more realistic effects.

 

- Revolutionary "2kBOM" skins with realistic FULL 2048 px rendering and easy to design with an evoX compatibility (devkit available in the store and on rebirth-sl.com/).

 

- Themed heads with cross-compatibility content for all other RoX heads to create an original collection and mix styles.

 

- 2 neck versions of the head to fit most bodies, male or female. RoX head are easy to shape and very versatile, so you can build a female or male avatar with each head.

 

- RoX packs contain an unprecedented quantity of items to spend hours in customization.

 

Locations:

French Touch event

 

maps.secondlife.com/secondlife/Scheveningen/232/226/23

 

Rebirth Heads Store

 

maps.secondlife.com/secondlife/REBIRTH%20Forever/47/79/21

 

Info about hair, earrings and dress on my Blog:

tillyopaline3.wixsite.com/tilly-opaline/post/rebirth-rox-...

ok, trying to compensate for the lamentable absence of PaD last two days (shame on me!) I thought I would try to give the viewer real value for money and include a free original story to go with the pic, pro bono as they come, but being lazy I engaged an AI dude, ChatGPT to be specific, to write it for me and here it goes, I accept no responsibility for the product, not a single word changed from AI's effort

  

"In a city where the traffic lights were permanently stuck on yellow, and everyone walked a little sideways just because it felt right, there stood a statue of a lion with a leaf clasped gently in his mouth. The statue's name was Sir Reginald P. Lionhart III, but everyone just called him Reggie. No one knew why a lion would hold a leaf, and frankly, no one questioned the oddities in this town—like the crosswalks that led nowhere or the park benches facing brick walls.

 

Reggie's leaf wasn't just any leaf; it was a meticulously chosen leaf from the only tree in the city that grew upside down. The roots reached for the sky, and the branches plunged into the earth, defying all botanical logic. One day, the leaf decided it had enough of subterranean life and embarked on an adventure upward, eventually landing squarely into Reggie's open mouth.

 

Reggie, being a lifelike statue with a keen sense of irony, decided to keep the leaf right there. It was his silent protest against the mundane expectations placed upon stone lions. Holding a leaf was his way of saying, "I contain multitudes."

 

People started to notice. The local philosopher, who held office hours on the corner between the invisible bookstore and the café that only served imaginary tea, proclaimed that the leaf symbolized the absurdity of existence. "It's a manifestation of our intrinsic desire to find meaning in the meaningless!" he shouted to a crowd of none.

 

Children began to leave offerings at Reggie's feet: mismatched socks, left-handed gloves, and drawings of three-headed dragons playing saxophones. They felt a kinship with this lion who dared to be different in a world that was already quite different.

 

One night, a mime—who wasn't actually trapped in an invisible box but liked to pretend he was—approached Reggie. "Why the leaf?" the mime didn't say. Reggie didn't reply, because statues and mimes share an unspoken bond that transcends words.

 

Meanwhile, the mayor issued a decree that all statues must adhere to the "Statue Code of Conduct," which explicitly forbade the unauthorized holding of foliage. Reggie remained unmoved—literally and metaphorically. The townspeople loved him for it. They started a movement called "Leaf It Be," campaigning for the rights of statues to express themselves.

 

Amidst all this, the leaf began to sprout tiny wings. Turns out, it wasn't a leaf at all but a caterpillar in disguise, yearning to become a butterfly but accidentally becoming a leaf instead. Reggie didn't mind. He admired the caterpillar’s commitment to its absurd identity crisis.

 

Eventually, the caterpillar-leaf took flight, leaving Reggie's mouth and soaring into the nonsensical sky, where clouds sometimes floated underground and rain fell upwards. Reggie felt a pang of something that might have been emotion if statues could feel.

 

In the end, Reggie decided to hold a spoon in his mouth next, just to keep things interesting. The townspeople applauded his new choice, reading all sorts of culinary and existential meanings into it. The philosopher began writing a book titled "The Spoonful of Existence," which no one would read because the pages were all blank.

 

By the way, did you ever consider that maybe the lion isn't holding the leaf—the leaf is holding the lion? In a world that absurd, anything is possible. Perhaps the real question isn't why the lion has a leaf in his mouth, but why we think a leaf doesn't belong there in the first place."

   

On an errand to Fittleworth, so I chose to pause for a photo at the old bridge at Stopham.

 

Stopham Bridge is said to be the finest medieval bridge in Sussex. It was built in 1423 to replace an earlier (1309) wooden bridge across the River Arun. The central arch was raised in 1822 to allow masted ships access to the Wey and Arun canal further upriver. A replacement road bridge was built in the 1980s to take away heavy traffic.

www.nationaltransporttrust.org.uk/heritage-sites/heritage...