Re-uploaded again with its very interesting history by Karl E. Hayes

 

Otter 233 was delivered to the United States Army on 12 February 1958 with serial 57-6114 (tail number 76114). It was one of sixteen Army Otters flown from Downsview to Addison, Texas for work on them by Collins Radio Corporation, to equip them for service overseas. Its initial unit allocation is unknown but it did serve in Europe, and was noted undergoing overhaul at the SABCA plant at Gosseleis near Brussels (who performed maintenance on US Army aircraft) during September 1960. By January 1962 it had joined the Military Assistance Advisory Group (MAAG), Italy based at Rome’s Ciampino Airport. It flew alongside a USAF C-47 which was also serving with the MAAG Flight.

 

Kenneth Ketzler flew the Otter. Apart from trips to Brienne-le-Chateau, France for maintenance, all his flying was within Italy, often visiting Italian military bases where US supplied helicopters were being introduced and MAAG personnel were working with Italian Army aviation units on these helicopters. There were also VIP flights and personnel transportation, which took the Otter all over Italy, from the mountains in the north down to the Mediterranean. As he recalls: “Ice seemed to cause me more concern than anything else. I especially remember several times flying IFR between Florence and Bologna at the lowest altitude of 12,000 feet and seeing ice forming on the wings. Flying over large bodies of water on one engine is not exactly my cup of tea. Seemed like the engine always ran rough whenever there was a trip to the islands of Sicily or Sardinia”.

 

76114 continued in service with MAAG Italy until February 1966, when it headed south to a new posting with the United States Mapping Mission to Ethiopia, based at the “old airport” at Addis Ababa. For this tasking the Otter was re-painted from the standard olive drab it had flown in while in Italy to the white/red colour scheme used by Army aircraft on survey work. It joined some Beavers with the Mapping Mission (76143 and 82026), a Douglas C-47 (17203) and UH-1B Huey helicopters, all of which were engaged in a topographic survey of Ethiopia. The Ethiopian Army had received some Otters under a Military Air Program and they were also based at the same airfield, making it quite an important Otter base.

 

The Otter was noted there in June 1969, just prior to its long flight north to Coleman Barracks, Mannheim, Germany from where it was transported to the Sharpe Army Depot, Stockton, California where it arrived in August 1969. After overhaul at the Depot it was assigned in March 1970 to the Aviation Section at Fort Ord, California used as a maintenance support aircraft. It remained in service at Fort Ord until June 1975 when its Army career came to an end. The Otter was transferred to the Civil Air Patrol (CAP) on 30 June 1975, registered that day as N5325G, and flown from Fort Ord north to Boeing Field, Seattle where Foreign & Domestic Enterprises prepared the Otter for service with the CAP. This was the company of Lloyd Rekow, who specialised in Otters. That master Otter rebuilder Harold Hansen was also involved. The Otter was surveyed on arrival at Boeing Field and found to be in excellent condition. Little work was required and on 16 July 1975 it received its Certificate of Airworthiness, with total airframe time of 3,776 hours. It was painted into an unusual colour scheme of blue top with white and red undersides and was noted as such at Boeing Field during August 1975.

 

Its service with the CAP lasted little more than a year and by Bill of Sale 19 November 1976 it was sold to Eagle Aviation Inc., aircraft dealers of Jones-Riverside Airport, Tulsa, Oklahoma. It was sold on for $89,500 by Bill of Sale dated 2 January 1977 to Travelair Taxi Inc., doing business as Island Airlines of Port Clinton, Ohio. When it arrived at its new base at Port Clinton it was painted in a garish red, white and blue bi-centennial colour scheme, but was soon re-painted in the somewhat more attractive house colours of Island Airlines, which was white with a silver cowling, blue around the cockpit with a red flash behind the windows. It joined the other members of the Island Airlines fleet, Beaver N62352 and Ford Tri-Motor N7584. The Ford was used for sight-seeing flights but the Beaver and the Otter flew scheduled services from Port Clinton, located at the western end of Lake Erie, to islands in the Lake – Kelley’s Island, Put-in-Bay, Middle Bass and north Bass.

 

This unique operation styled itself “The Shortest Airline in the World”, with some justification. Departing from Carl Keller Field at Port Clinton, the Otter took all of seven minutes to complete its scheduled flight to Put-in-Bay, and a similar time for the return sector. As Edward J. Rusch, the company’s Chief Pilot, said: “The Otter works the rough sod and stone fields of the islands very efficiently”. By March 1981 the Otter had a total time of 4,833 hours on the airframe. On the scheduled services to the islands, the Otter (or Beaver, depending on the load) carried the resident population year round; tourist during the summer as well as migrant Mexican labourers for fruit picking; and fishermen during the winter for ice fishing. The Otter also carried mail and freight and performed medevac flights, averaging several each weekend during the summer as tourists injured themselves. The island’s policeman acted as a paramedic and accompanied the flight. During the winter months when the lake froze over and the ferry no longer operated, these Beaver and Otter flights were the only means of access to the islands.

 

After nearly 16 years of flying with the Otter, this unique operation came to an end. Island Airlines was taken over by Griffing Flying Service Inc of Port Clinton, to whom the Otter was transferred by Bill of Sale dated 23 September 1992, and to whom the Otter was registered the following month, still as N5325G. The scheduled services were terminated and the Otter put up for sale. The buyer, through brokers C&S Enterprises, was Delay River Outfitters Inc, trading as Air Schefferville to whom the Otter was registered C-FQND on 23 August 1993 and it set off for its new base of Schefferville in the remote bush country of northern Quebec.

 

In 1994 the Otter was sold to Aircraft Investments LLC., of Oshkosh, Wisconsin and leased by them to Waweig Lake outfitters Ltd of Thunder Bay, Ontario to whom it was registered on 18 April 1994. It went to Recon Air at Geraldton, Ontario who converted it to a Vazar turbine Otter with a PT6A-135 engine, and it was repainted orange overall with a white cheatline and tail band. It then entered service with Waweig Lake Outfitters.

 

For the next number of years the Otter would fly out of Waweig Lake during the summer months, carrying tourists, fishermen and hunters wishing to experience the delights of the Ontario bush country. This business was carried on by Waweig Lake Outfitters in association with Wilderness North Air of Milwaukee. By Bill of Sale 14 April 1997 Aircraft Investments LLC, owners of the Otter, transferred title to 3006298 Nova Scotia Company, but the lease to Waweig Lake Outfitters continued. The Otter continued to fly for Waweig Lake Outfitters and Wilderness North Air alongside turbine Otters C-GMLB (359) and C-FYCX (44). On 6 June 2001 Otter QND was registered to 1401380 Ontario Ltd., (Waweig Air) and continued its services in the Ontario bush country.

 

Early in 2002 the Otter undertook a unique “Flight of Friendship” tour of 35 US cities, sponsored by Wilderness North Air. As the company’s website explained: “We wanted to show our friends in the US that they are welcome here in Canada during a period of uncertainty due to the attacks on the World trade Center. This is why we felt compelled to fly one of our Canadian icons, a turbine Otter, on this Canadian Hospitality Tour. At each of the 35 stops, presentations will be made by the Wilderness North Chief Pilot Randy Melnick of items donated by Canadian fire departments to their US counterparts, as a sign of solidarity and friendship. North West Ontario is renowned for its pristine wilderness environment and excellent recreational sports activities, said Alan Cheeseman, President of Wilderness North, who operate one of Canada’s finest fly-in fishing and adventure sports facilities. Wilderness North flies its guests into 16 different lakes and outpost camps from its base in Armstrong, Ontario just north of Thunder Bay”.

 

Otter QND, on wheels, departed Thunder Bay on 8 January 2002 and returned at the end of March. Its routing on the tour was Thunder Bay-St.Charles, Illinois-Madison, Wisconsin-Chicago/Springfield-Indianapolis-Columbus-Cincinnati-Louisville-St.Louis-Springfield, Missouri-Memphis, Tennessee-Little Rock-Oklahoma City-Dallas (Love Field)-Houston-New Orleans-Tallahassee-Tampa-Orlando-Fort Lauderdale-West Palm Beach-Daytona Beach-Jacksonville-Savannah-Atlanta-Columbia-Charlotte-Richmond-Washington-Baltimore (Ocean City)-Philadelphia-New York (Teterboro)-Boston-Albany-Buffalo-Cleveland-Dayton-Detroit-Grand Rapids-Lansing-Kalamazoo-Cedar Rapids-Des Moines-Rochester-La Crosse-Minneapolis-Duluth-Thunder Bay. On completion of this extensive tour, QND resumed flying in the Ontario bush country, along with Otters C-GMLB and C-FYCX, for Waweig Air and Wilderness North Air, flying from Armstrong Lake and the nearby seaplane base at Waweig Lake. It is mentioned in a CADORS report for 8 September 2007. QND arrived at the Churchill, Manitoba water base but the pilot did not call down and clear after landing. The airport operator did a ground check to make sure the aircraft was down and safe. As the report shows, QND did not confine its operations to Ontario, also visiting such distant places as Churchill, Manitoba.

 

In September 2010 Otter QND was advertised for sale, as having 12,130 hours total time and with an asking price of US $1,300,000. It was again advertised for sale in February 2013, price reduced to $1,250,000. The advert stated: “This aircraft is currently being run through the shop” and there were photographs of QND in a hangar having work done to it. It flew again for Waweig Air/Wilderness North Air for summer 2013 but was sold at the end of the summer season, in September 2013, to Vancouver Island Air.

 

In early October 2013 the Otter set off for its long delivery flight westwards, in the course of which an incident was recorded on CADORS on 4 October at La Ronge, Saskatchewan. On that day, Transwest Air DHC-6 Twin Otter C-FVOG on a local VFR flight out of La Ronge, reported seeing a DHC-3 Otter turning into him on finals for the La Ronge water base. The FSS had no information on the conflicting traffic. After landing the crew of the Twin Otter were able to identify the other aircraft as Otter QND and passed the information to the FSS. A few hours later the pilot of QND contacted the FSS and advised he had had radio failure inbound to La Ronge. QND was on straight floats and after La Ronge continued “lake hopping” across the country, eventually arriving at Campbell River on Vancouver Island, its new base. Registration of the Otter to 1401380 Ontario Ltd .,(Waweig Air) was cancelled on 31 October 2013 and C-FQND was registered to Vancouver Island Air Ltd., on 9 December 2013.

 

The Otter retained its orange overall colour scheme with white cheatline and tail stripe but acquired Vancouver Island Air fuselage titles. It replaced Beech 18 C-FGNR, which was sold, and joined Otter C-GVIX (97), these two turbine Otters from then on constituting the Vancouver Island Air fleet. Both Otters were still in service during summer 2017, flying the company’s charters and schedules out of Campbell River.

Mertasari Beach, Sanur, Bali - Indonesia.

Nikon D7000

Tokina 11-16mm

Lee 0.9 Hard Graduated Filter

B+W ND110 filter

Image Averaging

Excerpt from youractionsmatter.ca/e-waste/:

 

E-Waste

 

• The production of new electronics consumes large amounts of energy, contributing to climate change, and requires the extraction and depletion of raw materials, leading to the degradation of ecosystems.

• With lifespans lasting only a couple of years for many of these devices, an inordinate amount of waste is produced.

• Canada generates a whopping 954 kilotonnes of e-waste annually, a figure that has almost quadrupled in just 20 years. This amounts to 25 kg for every Canadian, three times the global average.

• What’s worse, this is expected to rise to 1.2 megatonnes by 2030, or over 31 kg per person.

• Electronic products contain hundreds of toxic substances such as lead, mercury, and cadmium.

• Historically, 90% of this waste has ended up in landfills with only 10% being recycled or recovered.

• When dumped in landfills, this toxic waste can leak into the soil and groundwater, harming plants, animals, and even humans.

• Worse still, e-waste in landfills can contribute to air pollution, releasing these chemicals into the atmosphere.

• Greenhouse gas emissions from electronic devices and their associated waste increased by over 50 percent between 2014 and 2020.

• Exposure to these toxins can cause a range of health issues in humans, including neurological disorders, reproductive problems, and various forms of cancer.

• With 80% of Canadians having unwanted electronics at home ready to be recycled, properly recycling them would go a long way to solving the growing issue of e-waste.

• Just as important is the Right to Repair movement, which advocates for consumers to have the ability to repair their own devices. With widespread implementation, it would drastically help alleviate the growing e-waste problem.

 

Electronic waste has become a significant environmental issue in recent years. In 2021, human beings discarded an estimated 57.4 million tonnes of electronic waste, outweighing the Great Wall of China, the world's heaviest human construction. More concerning is the projection that global e-waste is set to reach 74 million tonnes by 2030, nearly doubling over a 16-year period.

 

With the rapid pace of technological advancements, consumers replace their cell phones approximately every two years, substantially contributing to the swelling problem of e-waste. The manufacture of electronic devices requires significant amounts of resources. For instance, the production of just one desktop computer needs at least 240 kg of fossil fuels, 22 kg of chemicals, and 1.5 tonnes of water. The substantial consumption of these resources underlines the importance of extending the lifespan of our current gadgets as a crucial step towards reducing our environmental footprint.

 

This environmental crisis also presents a valuable opportunity. E-waste harbors rich reserves of resources such as gold, silver, copper, and rare earth metals. In 2019 alone, the estimated worth of global e-waste was a staggering $57 billion, an amount surpassing the annual GDP of several countries. With worldwide smartphone sales surpassing a billion units every year, the proper disposal and recycling of these devices can both mitigate the e-waste issue and tap into an enormous repository of precious materials.

 

In this light it is important to highlight the Right to Repair. This refers to the principle that consumers should have the legal ability to repair and modify their own devices without facing barriers from manufacturers. It aims to counter restrictive practices by manufacturers that limit repairs to authorized service centers, thereby promoting longevity of products and reducing e-waste. Supporting this initiative would drastically reduce our e-waste for years to come.

I should have looked for a female Chrysomelid beetle with a very smug expression. Imagine the fun of laying eggs on this leaf!

 

I think they are probably Paropsisterna agricola

GIANT MORAY (Gymnothorax javanicus) - FILITHEYO ISLAND, MALDIVES -

These moray eels are on average 3m long and 30kg, however some exceed 3m and weigh up to 70kg.

 

Zoom to full screen: click on L, then on F11

Exit full screen: click on F11, then on L

 

Zoom plein écran: clic sur L, puis sur F11

Sortie du plein écran: clic sur F11, puis sur L

Goldfinch

(Carduelis carduelis)

 

The average goldfinch is 12–13 cm long with a wingspan of 21–25 cm and a weight of 14 to 19 grams. The sexes are broadly similar, with a red face, black and white head, warm brown upperparts, white underparts with buff flanks and breast patches, and black and yellow wings.

 

Thank you for taking the time to view or comment.

~Andy Rooney

Enzo in natural window light. I love the line of the blinds going across his back.

 

© All Rights Reserved.

en.wikipedia.org/wiki/Red_Sea

   

The Red Sea (alternatively Arabian Gulf[1] or Gulf of Arabia[2][3]) is a seawater inlet of the Indian Ocean, lying between Africa and Asia. The connection to the ocean is in the south through the Bab el Mandeb strait and the Gulf of Aden. In the north, there is the Sinai Peninsula, the Gulf of Aqaba, and the Gulf of Suez (leading to the Suez Canal). The Red Sea is a Global 200 ecoregion. The sea is underlain by the Red Sea Rift which is part of the Great Rift Valley.

The Red Sea has a surface area of roughly 438,000 km² (169,100 mi²).[4][5] It is about 2250 km (1398 mi) long and, at its widest point, 355 km (220.6 mi) wide. It has a maximum depth of 2211 m (7254 ft) in the central median trench, and an average depth of 490 m (1,608 ft). However, there are also extensive shallow shelves, noted for their marine life and corals. The sea is the habitat of over 1,000 invertebrate species, and 200 soft and hard corals. It is the world's northernmost tropical sea.

  

Extent

The International Hydrographic Organization defines the limits of the Red Sea as follows:[6]

On the North. The Southern limits of the Gulfs of Suez [A line running from Ràs Muhammed (27°43'N) to the South point of Shadwan Island (34°02'E) and thence Westward on a parallel (27°27'N) to the coast of Africa] and Aqaba [A line running from Ràs al Fasma Southwesterly to Requin Island (

27°57′N 34°36′E) through Tiran Island to the Southwest point thereof and thence Westward on a parallel (27°54'N) to the coast of the Sinaï Peninsula].

On the South. A line joining Husn Murad (

12°40′N 43°30′E) and Ras Siyan (

12°29′N 43°20′E).

   

Name

 

Red Sea is a direct translation of the Greek Erythra Thalassa (Ερυθρὰ Θάλασσα) and Latin Mare Rubrum (alternatively Sinus Arabicus, literally "Arabian Gulf"), Arabic Al-Baḥr Al-Aḥmar (البحر الأحمر) or Baḥr Al-Qalzam(بحر القلزم), Somali Badda Cas and Tigrinya Qeyyiḥ bāḥrī (ቀይሕ ባሕሪ). The name of the sea may signify the seasonal blooms of the red-coloured Trichodesmium erythraeum near the water's surface.[7] A theory favored by some modern scholars[who?] is that the name red is referring to the direction South, just as the Black Sea's name may refer to North. The basis of this theory is that some Asiatic languages used color words to refer to the cardinal directions.[8] Herodotus on one occasion uses Red Sea and Southern Sea interchangeably.[9]

The association of the Red Sea with the Biblical account of the Israelite Crossing the Red Sea is ancient, and was made explicit in the Septuagint translation of the Book of Exodus from Hebrew to Koine Greek in approximately the third century B.C. In that version, the Hebrew Yam Suph (ים סוף) is translated as Erythra Thalassa (Red Sea). (See also the more recent suggestion that the Yam Suph of the Exodus refers to a Sea of Reeds). The Red Sea is one of four seas named in English after common color terms — the others being the Black Sea, the White Sea and the Yellow Sea. The direct rendition of the Greek Erythra thalassa in Latin as Mare Erythraeum refers to the north-western part of the Indian Ocean, and also to a region on Mars.

  

History

 

The earliest known exploration of the Red Sea was conducted by Ancient Egyptians, as they attempted to establish commercial routes to Punt. One such expedition took place around 2500 BC, and another around 1500 BC ( by Hatshepsut ). Both involved long voyages down the Red Sea.[10] The Biblical Book of Exodus tells the story of the Israelites' miraculous crossing of a body of water, which the Hebrew text calls Yam Suph. Yam Suph is traditionally identified as the Red Sea. The account is part of the Israelites' escape from slavery in Egypt. Yam Suph can also been translated as Sea of Reeds.

In the 6th century BC, Darius the Great of Persia sent reconnaissance missions to the Red Sea, improving and extending navigation by locating many hazardous rocks and currents. A canal was built between the Nile and the northern end of the Red Sea at Suez. In the late 4th century BC, Alexander the Great sent Greek naval expeditions down the Red Sea to the Indian Ocean. Greek navigators continued to explore and compile data on the Red Sea. Agatharchides collected information about the sea in the 2nd century BC. The Periplus of the Erythraean Sea ("Periplus of the Red Sea"), a Greek periplus written by an unknown author around the 1st century AD, contain a detailed description of the Red Sea's ports and sea routes.[11] The Periplus also describes how Hippalus first discovered the direct route from the Red Sea to India.

 

The Red Sea was favored for Roman trade with India starting with the reign of Augustus, when the Roman Empire gained control over the Mediterranean, Egypt, and the northern Red Sea. The route had been used by previous states but grew in the volume of traffic under the Romans. From Indian ports goods from China were introduced to the Roman world. Contact between Rome and China depended on the Red Sea, but the route was broken by the Aksumite Empire around the 3rd century AD.[12]

During the Middle Ages, the Red Sea was an important part of the Spice trade route. In 1513, trying to secure that channel to Portugal, Afonso de Albuquerque laid siege to Aden.[13] but was forced to retreat. They cruised the Red Sea inside the Bab al-Mandab, as the first European fleet to have sailed this waters.

In 1798, France ordered General Bonaparte to invade Egypt and take control of the Red Sea. Although he failed in his mission, the engineer Jean-Baptiste Lepère, who took part in it, revitalised the plan for a canal which had been envisaged during the reign of the Pharaohs. Several canals were built in ancient times from the Nile to the Red Sea along or near the line of the present Sweet Water Canal, but none lasted for long. The Suez Canal was opened in November 1869. At the time, the British, French, and Italians shared the trading posts. The posts were gradually dismantled following the First World War. After the Second World War, the Americans and Soviets exerted their influence whilst the volume of oil tanker traffic intensified. However, the Six Day War culminated in the closure of the Suez Canal from 1967 to 1975. Today, in spite of patrols by the major maritime fleets in the waters of the Red Sea, the Suez Canal has never recovered its supremacy over the Cape route, which is believed to be less vulnerable.

   

Oceanography

 

The Red Sea lies between arid land, desert and semi-desert. The main reasons for the better development of reef systems along the Red Sea is because of its greater depths and an efficient water circulation pattern, The Red Sea water mass exchanges its water with the Arabian Sea, Indian Ocean via the Gulf of Aden. These physical factors reduce the effect of high salinity caused by evaporation water in the north and relatively hot water in the south.

The climate of the Red Sea is the result of two distinct monsoon seasons; a northeasterly monsoon and a southwesterly monsoon. Monsoon winds occur because of the differential heating between the land surface and sea. Very high surface temperatures coupled with high salinities makes this one of the hottest and saltiest bodies of seawater in the world. The average surface water temperature of the Red Sea during the summer is about 26 °C (79 °F) in the north and 30 °C (86 °F) in the south, with only about 2 °C (3.6 °F) variation during the winter months. The overall average water temperature is 22 °C (72 °F). Today surface water temperatures remain relatively constant at 21–25 °C (70–77 °F). Temperature and visibility remain good to around 200 m (656 ft). The sea is known for its strong winds and unpredictable local currents.

The rainfall over the Red Sea and its coasts is extremely low, averaging 0.06 m (2.36 in) per year. The rain is mostly in the form of showers of short spells, often associated with thunderstorms and occasionally with dust storms. The scarcity of rainfall and no major source of fresh water to the Red Sea result in the excess evaporation as high as 205 cm (81 in) per year and high salinity with minimal seasonal variation. A recent underwater expedition to the Red Sea offshore from Sudan and Eritrea[14] found surface water temperatures 28 °C in winter and up to 34 °C in the summer, but despite that extreme heat the coral was healthy with much fish life with very little sign of coral bleaching, and there were plans to use samples of these corals' apparently heat-adapted commensal algae to salvage bleached coral elsewhere.

 

Salinity

 

The Red Sea is one of the most saline bodies of water in the world, due to high evaporation. Salinity ranges from between ~36 ‰ in the southern part due to the effect of the Gulf of Aden water and reaches 41 ‰ in the northern part, due mainly to the Gulf of Suez water and the high evaporation. The average salinity is 40 ‰. (Average salinity for the world's seawater is ~35 ‰ on the Practical Salinity Scale, or PPS; that translates to 3.5 % actual dissolved salts.)

In terms of salinity, the Red Sea is greater than the world average, approximately 4 percent. This is due to several factors:

1.High rate of evaporation and very little precipitation.

2.Lack of significant rivers or streams draining into the sea.

3.Limited connection with the Indian Ocean, which has lower water salinity.

 

Tidal range

In general tide ranges between 0.6 m (2.0 ft) in the north, near the mouth of the Gulf of Suez and 0.9 m (3.0 ft) in the south near the Gulf of Aden but it fluctuates between 0.20 m (0.66 ft) and 0.30 m (0.98 ft) away from the nodal point. The central Red Sea (Jeddah area) is therefore almost tideless, and as such the annual water level changes are more significant. Because of the small tidal range the water during high tide inundates the coastal sabkhas as a thin sheet of water up to a few hundred metres rather than inundating the sabkhas through a network of channels. However, south of Jeddah in the Shoiaba area the water from the lagoon may cover the adjoining sabkhas as far as 3 km (2 mi) whereas, north of Jeddah in the Al-kharrar area the sabkhas are covered by a thin sheet of water as far as 2 km (1.2 mi). The prevailing north and northeastern winds influence the movement of water in the coastal inlets to the adjacent sabkhas, especially during storms. Winter mean sea level is 0.5 m (1.6 ft) higher than in summer. Tidal velocities passing through constrictions caused by reefs, sand bars and low islands commonly exceed 1–2 m/s (3–6.5 ft/s). Coral reefs in the Red Sea are near Egypt, Saudi Arabia, Israel and Sudan.

 

Current

In the Red Sea detailed current data is lacking, partially because they are weak and variable both spatially and temporally. Temporal and spatial currents variation is as low as 0.5 m (1.6 ft) and are governed all by wind. During the summer, NW winds drive surface water south for about four months at a velocity of 15–20 cm/s (6–8 in/s), whereas in winter the flow is reversed resulting in the inflow of water from the Gulf of Aden into the Red Sea. The net value of the latter predominates, resulting in an overall drift to the northern end of the Red Sea. Generally, the velocity of the tidal current is between 50–60 cm/s (20–23.6 in/s) with a maximum of 1 m/s (3.3 ft) at the mouth of the al-Kharrar Lagoon. However, the range of the north-northeast current along the Saudi coast is 8–29 cm/s (3–11.4 in/s).

 

Wind regime

With the exception of the northern part of the Red Sea, which is dominated by persistent north-west winds, with speeds ranging between 7 km/h (4.3 mph) and 12 km/h (7.5 mph), the rest of the Red Sea and the Gulf of Aden are subjected to the influence of regular and seasonally reversible winds. The wind regime is characterized by both seasonal and regional variations in speed and direction with average speed generally increasing northward.

Wind is the driving force in the Red Sea for transporting the material either as suspension or as bedload. Wind induced currents play an important role in the Red Sea in initiating the process of resuspension of bottom sediments and transfer of materials from sites of dumping to sites of burial in quiescent environment of deposition. Wind generated current measurement is therefore important in order to determine the sediment dispersal pattern and its role in the erosion and accretion of the coastal rock exposure and the submerged coral beds.

 

Geology

 

The Red Sea was formed by Arabia splitting from Africa due to movement of the Red Sea Rift. This split started in the Eocene and accelerated during the Oligocene. The sea is still widening and it is considered that the sea will become an ocean in time (as proposed in the model of John Tuzo Wilson). In 1949, a deep water survey reported anomalously hot brines in the central portion of the Red Sea. Later work in the 1960s confirmed the presence of hot, 60 °C (140 °F), saline brines and associated metalliferous muds. The hot solutions were emanating from an active subseafloor rift. The highly saline character of the waters was not hospitable to living organisms.[15]

Sometimes during the Tertiary period the Bab el Mandeb closed and the Red Sea evaporated to an empty hot dry salt-floored sink. Effects causing this would be:

•A "race" between the Red Sea widening and Perim Island erupting filling the Bab el Mandeb with lava.

•The lowering of world sea level during the Ice Ages due to much water being locked up in the ice caps.

A number of volcanic islands rise from the center of the sea. Most are dormant, but in 2007 Jabal al-Tair island, in the Bab el Mandeb strait, erupted violently. An eruption among the nearby Zubair islands followed in 2011.[16]

  

Mineral resources

In terms of mineral resources the major constituents of the Red Sea sediments are as follows:

•Biogenic constituents:

Nanofossils, foraminifera, pteropods, siliceous fossils

•Volcanogenic constituents:

Tuffites, volcanic ash, montmorillonite, cristobalite, zeolites

•Terrigenous constituents:

Quartz, feldspars, rock fragments, mica, heavy minerals, clay minerals

•Authigenic minerals:

Sulfide minerals, aragonite, Mg-calcite, protodolomite, dolomite, quartz, chalcedony.

•Evaporite minerals:

Magnesite, gypsum, anhydrite, halite, polyhalite

•Brine precipitate:

Fe-montmorillonite, goethite, hematite, siderite, rhodochrosite, pyrite, sphalerite, anhydrite.

 

Living resources

The Red Sea is a rich and diverse ecosystem. More than 1200 species of fish[17] have been recorded in the Red Sea, and around 10% of these are found nowhere else.[18] This also includes 42 species of deepwater fish.[17]

 

The rich diversity is in part due to the 2,000 km (1,240 mi) of coral reef extending along its coastline; these fringing reefs are 5000–7000 years old and are largely formed of stony acropora and porites corals. The reefs form platforms and sometimes lagoons along the coast and occasional other features such as cylinders (such as the Blue Hole (Red Sea) at Dahab). These coastal reefs are also visited by pelagic species of red sea fish, including some of the 44 species of shark.

The Red Sea also contains many offshore reefs including several true atolls. Many of the unusual offshore reef formations defy classic (i.e., Darwinian) coral reef classification schemes, and are generally attributed to the high levels of tectonic activity that characterize the area.

The special biodiversity of the area is recognized by the Egyptian government, who set up the Ras Mohammed National Park in 1983. The rules and regulations governing this area protect local marine life, which has become a major draw for diving enthusiasts.

Divers and snorkellers should be aware that although most Red Sea species are innocuous, a few are hazardous to humans: see Red Sea species hazardous to humans.[19]

Other marine habitats include sea grass beds, salt pans, mangroves and salt marshes.

 

Desalination plants

There is extensive demand of desalinated water to meet the requirement of the population and the industries along the Red Sea.

There are at least 18 desalination plants along the Red Sea coast of Saudi Arabia which discharge warm brine and treatment chemicals (chlorine and anti-scalants) that may cause bleaching and mortality of corals and diseases to the fish stocks. Although this is only a localized phenomenon, it may intensify with time and have a profound impact on the fishing industry.[20]

The water from the Red Sea is also utilized by oil refineries and cement factories for cooling purposes. Used water drained back into the coastal zones may cause harm to the nearshore environment of the Red Sea.

 

Security

The Red Sea is part of the sea roads between Europe, the Persian Gulf and East Asia, and as such has heavy shipping traffic. Piracy in Somalia occurs principally near the area of the Gulf of Aden south of the sea. Government-related bodies with responsibility to police the Red Sea area include the Port Said Port Authority, Suez Canal Authority and Red Sea Ports Authority of Egypt, Jordan Maritime Authority, Israel Port Authority, Saudi Ports Authority and Sea Ports Corporation of Sudan.

 

Facts and figures

•Length: ~2,250 km (1,398.1 mi) - 79% of the eastern Red Sea with numerous coastal inlets

•Maximum Width: ~ 306–355 km (190–220 mi)– Massawa (Eritrea)

•Minimum Width: ~ 26–29 km (16–18 mi)- Bab el Mandeb Strait (Yemen)

•Average Width: ~ 280 km (174.0 mi)

•Average Depth: ~ 490 m (1,607.6 ft)

•Maximum Depth: ~2,211 m (7,253.9 ft)

•Surface Area: 438-450 x 10² km² (16,900–17,400 sq mi)

•Volume: 215–251 x 10³ km³ (51,600–60,200 cu mi)

•Approximately 40% of the Red Sea is quite shallow (under 100 m/330 ft), and about 25% is under 50 m (164 ft) deep.

•About 15% of the Red Sea is over 1,000 m (3,300 ft) depth that forms the deep axial trough.

•Shelf breaks are marked by coral reefs

•Continental slope has an irregular profile (series of steps down to ~500 m/1,640 ft)

•Centre of Red Sea has a narrow trough (~ 1,000 m/3,281 ft; some deeps may exceed 2,500 m/8,202 ft)

 

Tourism

 

The sea is known for its spectacular recreational diving sites, such as Ras Mohammed, SS Thistlegorm (shipwreck), Elphinstone, The Brothers, Dolphin Reef and Rocky Island in Egypt and less known sites in Sudan such as Sanganeb, Abington, Angarosh and Shaab Rumi.

The Red Sea became known as a sought-after diving destination after the expeditions of Hans Hass in the 1950s, and later by Jacques-Yves Cousteau. Popular tourist resorts include El Gouna, Hurghada, Safaga, Marsa Alam, on the western shore of the Red Sea, and Sharm-El-Sheikh, Dahab, and Taba on the Egyptian side of Sinaï, as well as Aqaba in Jordan and Eilat in Israel in an area known as the Red Sea Riviera.

The popular tourist beach of Sharm el-Sheikh was closed to all swimming in December 2010 due to several serious shark attacks, including one fatal one. As of December 2010, scientists are investigating the attacks and have identified, but not verified, several possible causes including over fishing which causes large sharks to hunt closer to shore, tourist boat operators who chum the waters just offshore to present shark-photo opportunities, and reports of passing ships throwing dead livestock overboard. Furthermore the geography of some parts of the Red Sea is such that large sharks can sometimes wander close to shore. This is due to the sea's narrow width, significant depth, and sharp drop-offs, all of which combine to form a geography where large deep-water sharks can roam in hundreds of meters of water, yet be within a hundred meters of swimming areas.

 

Bordering countries

The Red Sea may be geographically divided into three sections: the Red Sea proper, and in the north, the Gulf of Aqaba and the Gulf of Suez. The six countries bordering the Red Sea proper are:

•Eastern shore:

o Saudi Arabia

o Yemen

•Western shore:

o Egypt

o Sudan

o Eritrea

o Djibouti

The Gulf of Suez is entirely bordered by Egypt. The Gulf of Aqaba borders Egypt, Israel, Jordan and Saudi Arabia.

In addition to the standard geographical definition of the six countries bordering the Red Sea cited above, areas such as Somalia and Ethiopia are sometimes also described as Red Sea territories. This is primarily due to their proximity to and geological similarities with the nations facing the Red Sea and/or political ties with said areas.[21][22]

 

Towns and cities

Towns and cities on the Red Sea coast (including the coasts of the Gulfs of Aqaba and Suez) include:

• Al Hudaydah (الحديدة)

• Al Lith (الليِّث)

• Al Qunfudhah (القنفذة)

• Al-Qusair (القصير)

• Al Wajh (الوجه)

• Aqaba (العقبة)

• Asseb (ዓሳብ)

• Dahab (دهب)

• Duba (ضباء)

• Eilat (אילת)

• El Gouna (الجونة)

• El Suweis (السويس)

• / Hala'ib (حلايب) (disputed)

• Haql (حقل)

• Hirgigo (ሕርጊጎ)

• Hurghada (الغردقة)

• Jeddah (جدة)

• Jazan (جازان)

• Marsa Alam (مرسى علم)

• Massawa (ምጽዋ)

• Nuweiba (نويبع)

• Port Safaga (ميناء سفاجا)

• Port Sudan (بورت سودان)

• Rabigh (رابغ)

• Sharm el Sheikh (شرم الشيخ)

• Soma Bay (سوما باي)

• Suakin (سواكن)

• Taba (طابا)

• Thuwal (ثول)

• Yanbu (ينبع)

   

Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.

 

The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.

 

Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.

 

As stated in the foundation document in U.S. National Park Service website:

 

The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.

 

The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.

 

The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.

 

As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.

 

Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.

 

Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.

 

Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.

 

The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.

 

The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.

 

A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.

 

In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.

 

In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.

 

In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".

 

Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.

 

Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.

 

Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.

 

Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.

 

Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.

 

American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.

 

An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.

 

A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.

 

Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.

 

Among the notable features of the park are the following:

Balanced Rock – a large balancing rock, the size of three school buses

Courthouse Towers – a collection of tall stone columns

Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail

Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park

Devils Garden – many arches and columns scattered along a ridge

Double Arch – two arches that share a common end

Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)

Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)

Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area

The Phallus – a rock spire that resembles a phallus

Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008

The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.

 

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.

Miltoniopsis phalaenopsis, variété intermédiaire de très bonne forme. Je n'aime pas d'utiliser le flash et ne le fais presque jamais, mais lá j'ai fait un essai pour voir... Trop de réverbération lumineuse á mon goût, dans ce cas montrant comme cette espèce brille, mais cela permet plus de netteté bien sur.

 

Miltoniopsis phalaenopsis, average variety with good shape. I don't like to use flash and almost never do, but I tried to see... Too much light reverberation for me, in this case showing how glistening can be this species, but that allows more sharpness of course.

 

Miltoniopsis phalaenopsis, variedad intermedia de muy buena forma. No me gusta usar flash y casi no lo hago, pero probé para ver... Demasiado reverberación de la luz para mi, mostrando en el caso de esta especie como brilla, pero permite más nitidez por supuesto.

The Great Tit , Parus major is the largest bird in the tit family. It is also the most widespread and common family member with birds found in Britain , mainland Europe , the Middle east , Asia and North Africa. This woodland bird tends to be resident in all but the extreme climates and normally does not migrate.

 

The Great tit , is a distinctive looking garden visitor with it’s white and black head. The largest of the tit family it has a wingspan of up to 26cm , with a body length of between 12-14cm and body weight up to 20g. It has a bright yellow breast with a broad black stripe and blue-green wings. the female has the same colouring as the male with slightly duller colours.

 

The Great Tit can be found in a wide range of habitats including all types of woodland , parks and urban gardens. The bird is generally not migratory and once established will normally stay in their territory all year round. Young birds will be chased away by their parents but will normally stay within 10 miles from their nest site.

 

In Britain the Great Tit breading season normally begins in March . Nests are formed in cavities in trees and walls, the birds are also willing occupants of bird nesting boxes. the nests are built by the female bird and made of hair, moss, feathers and grass/plant materials. The number of eggs in each clutch varies from as few as 5 up to 12 eggs.

 

Britain’s population of around 2 million pairs puts it in 8th place in Europe. Germany has the most: an estimated 8 million pairs.

 

The mating pair can have a second brood later in the year an these tend to be much smaller in numbers. The mother takes on all the incubation duties , the male’s main role being supply of food. the incubation period lasts up to 15 days and the chicks hatch blind and unfeathered. Both parents are evolved with feeding the chicks with food within the nest for the next 20 days . Survival rates for the young are low with an average of 40% making it to adulthood.

 

Read more at www.wildonline.blog

The Moon’s average distance from Earth is more than 238,800 miles, but today, it’ll be 7.26 percent closer than that. That means it'll look about 14 percent larger than your average full moon, and 30 percent brighter. And this year, the supermoon is extra close to Earth. Not only is it the closest supermoon we’ve had since January 1948, but it’s going to be closer than 99.7 percent of all full moons in the past 200 years.

 

So go. Stare at the Moon. Let it remind you of our beautiful, cosmic neighborhood that is so much bigger than ourselves.

Rather average pain jobs. I like them all without helmets better.

average,boring, complete

Average people have wishes and hopes. Confident people have goals and plans.

  

www.millionairemindset.net/average-people-have-wishes-and...

Its in average condition some of the paint has peeled but it still looks good on the rear all of the metal clips are missing which comes as no surprise for a clip on trim but the fixings are all good

Tuban Beach, Sanur, Bali - Indonesia.

Nikon D7000

Tokina 11-16mm

Lee 0.9 Hard Graduated ND filter

Image Averaging 21 x 5.8sec.

Total exposure 121.8sec.

Just your average beach scene really ;-)

 

View On Black

 

I was excited to see an advert on telly tonight for the

film I saw being made on Marloes sands in Pembrokeshire last year.

It's called Snow White and the huntsman.

I uploaded some shots last year and these can be seen in the set I've made for them.

www.flickr.com/photos/27955898@N07/sets/72157627722523575/

++++ from WIKIPEDIA ++++++

 

Abruzzo (UK: /æˈbrʊtsoʊ/,[5] US: /ɑːˈbruːtsoʊ, əˈ-/; Italian: [aˈbruttso]; Abbrùzze [abˈbruttsə], Abbrìzze [abˈbrittsə] or Abbrèzze [abˈbrɛttsə] in Neapolitan Abruzzese; Aquilano: Abbrùzzu) or Abruzzi is a region of Southern Italy with an area of 10,763 square km (4,156 sq mi) and a population of 1.3 million. It is divided into four provinces: L'Aquila, Teramo, Pescara, and Chieti. Its western border lies 80 km (50 mi) east of Rome. Abruzzo borders the region of Marche to the north, Lazio to the west and south-west, Molise to the south-east, and the Adriatic Sea to the east. Geographically, Abruzzo is divided into a mountainous area in the west, which includes the Gran Sasso d'Italia, and a coastal area in the east with beaches on the Adriatic Sea.

 

Abruzzo is considered a region of Southern Italy in terms of its culture, language, history and economy, although geographically it may also be considered central.[8] The Italian Statistical Authority (ISTAT) also deems it to be part of Southern Italy, partly because of Abruzzo's historic association with the Kingdom of the Two Sicilies.

 

Abruzzo is known as "the greenest region in Europe" as almost half of its territory, the largest in Europe,[9] is set aside as national parks and protected nature reserves. There are three national parks, one regional park, and 38 protected nature reserves. These ensure the survival of 75% of Europe's living species, including rare species such as the golden eagle, the Abruzzo (or Abruzzese) chamois, the Apennine wolf and the Marsican brown bear.[10] Abruzzo is also home to Calderone, Europe's southernmost glacier.

 

The visiting nineteenth-century Italian diplomat and journalist Primo Levi (1853–1917) said that the adjectives "forte e gentile" (strong and kind) best describe the beauty of the region and the character of its people. "Forte e gentile" has since become the motto of the region and its inhabitants.

 

Provinces and politics

Abruzzo provinces

Provinces

 

Abruzzo is divided into four administrative provinces:

Province Area (km2) Population Density (inh./km2)

Chieti 2,588 396,190 153.1

L'Aquila 5,034 308,876 61.3

Pescara 1,225 318,701 260.1

Teramo 1,948 308,769 158.5

Politics

 

History

Human settlements in Abruzzo have existed since at least the Neolithic times. A skeleton from Lama dei Peligni in the province of Chieti dates back to 6,540 BC under radiometric dating.[13] The name Abruzzo appears to be derivative of the Latin word "Aprutium". In Roman times, the region was known as Picenum, Sabina et Samnium, Flaminia et Picenum, and Campania et Samnium.[14] The region was known as Aprutium in the Middle Ages, arising from four possible sources: it is a combination of Praetutium, or rather of the name of the people Praetutii, applied to their chief city, Interamnia, the old Teramo.

 

Many cities in Abruzzo date back to ancient times. Corfinio was known as Corfinium when it was the chief city of the Paeligni, and later was renamed Pentima by the Romans. Chieti is built on the site of the ancient city of Teate, Atri was known as Adria. Teramo, known variously in ancient times as Interamnia and Teramne, has Roman ruins which attract tourists.

 

After the fall of the Roman Empire, a string of invasions and rulers dominated the region, including the Lombards, Byzantines, and Hungarians. Between the 9th and 12th centuries, the region was dominated by the popes. Subsequently, the Normans took over, and Abruzzo became part of the Kingdom of Sicily, later the Kingdom of Naples. Spain ruled the kingdom from the sixteenth to the eighteenth centuries. The French Bourbon dynasty took over in 1815, establishing the Kingdom of the Two Sicilies, and ruled until Italian unification (also known as the Risorgimento) in 1860.

 

Until 1963, Abruzzo was part of the combined Abruzzi e Molise region. The term Abruzzi (plural of Abruzzo) derives from the time when the region was part of the Kingdom of the Two Sicilies. The territory was administered as Abruzzo Citeriore (nearer Abruzzo) and Abruzzo Ulteriore I and II (farther Abruzzo I and II) from Naples, the capital of the kingdom.[14] Abruzzo Citeriore is now Chieti province. Teramo and Pescara provinces now comprise what was Abruzzo Ulteriore I. Abruzzo Ulteriore II is now the province of L'Aquila.

 

In the twentieth century, war had a great impact on the region. During the Second World War, Abruzzo was on the Gustav Line, part of the German's Winter Line. One of the most brutal battles was the Battle of Ortona. Abruzzo was the location of two prisoner of war camps, Campo 21 in Chieti,[18] and Campo 78 in Sulmona. The Sulmona camp also served as a POW camp in World War 1; much of the facility is still intact and attracts tourists interested in military history.

 

Geography

Geographically, Abruzzo is located in central Italy and southern Italy, stretching from the heart of the Apennines to the Adriatic Sea, and includes mainly mountainous and wild land. The mountainous land is occupied by a vast plateau, including Gran Sasso, at 2,912 metres (9,554 ft) the highest peak of the Apennines, and Mount Majella at 2,793 metres (9,163 ft). The Adriatic coastline is characterized by long sandy beaches to the North and pebbly beaches to the South. Abruzzo is well known for its landscapes and natural environment, parks and nature reserves, characteristic hillside areas rich in vineyards and olive groves, and one of the highest densities of Blue Flag beaches.

 

Climate

The Abruzzo region has two types of climate that are strongly influenced by the Apennine Mountains, dividing the climate of the coastal and sub-Apennine hills from the interior's high mountain ranges. Coastal areas have a Mediterranean climate with hot dry summers and mild winters and rainy hills with a sublittoral climate where temperatures decrease progressively with increasing altitude and precipitation with altitude. Precipitation is also strongly affected by the presence of the Apennines mountain ridges of the region; it increases with the proportion being more abundant in the field and on the slopes exposed to the west, instead of decreasing towards the east and east-facing slopes. Often the Adriatic coast are sidelined rainfall from the west to the barrier effect of the Apennines undergoing the action of gentle winds descending from it (or Libeccio).[21] The minimum annual rainfall, however, is found in some inland valleys, sheltered from much disturbance to the blocking action of mountain ridges, such as the Peligna Valley, or the valley of the river Tirino, which in some places (Ofena, Capestrano) showed barely 500 millimetres (19.7 inches), and not along the coast where it never falls below 600 millimetres (23.6 inches); for if Teramo is relatively little watered by rain (Teramo less than 800 millimetres (31.5 inches)), the metre is exceeded in Chieti, reaching maximum levels in the Adriatic, while between Ortona and Vasto in Costa dei Trabocchi decrease again.[21] The highest rainfall occurs in upland areas on the border with Lazio; they are especially vulnerable to Atlantic disturbances. Around 1,500 to 2,000 millimetres (59 to 79 inches) of precipitation is typical (Pescara in 2010 showed a value close to 2,800 millimetres (110.2 inches)).

 

Flora and fauna

As with many Mediterranean regions, Abruzzo's vegetation is characterized by different Mediterranean ecosystems. The coast and the surrounding areas are characterized by the presence of typical plants of Mediterranean shrubland, such as myrtle, heather and mastic, while in the hilly areas other species grow, including olive, pine, willow, oak, poplar, alder, arbutus, broom, acacia, capers, rosemary, hawthorn, licorice and almond trees, interspersed with oak trees. At elevations between 600 and 1,000 metres (2,000 and 3,300 ft) there is sub-montane vegetation, mainly characterized by mixed forests of oak and turkey oak, maple and hornbeam; shrubs include dog rose and red juniper. Elevations between 1,000 and 1,900 metres (3,300 and 6,200 ft) are dominated by beech trees. In the Apennine Mountains at elevations above 2,000 metres (6,600 ft) species include alpine orchid, mountain juniper, silver fir, black cranberry and the Abruzzo edelweiss.

 

The fauna of Abruzzo is highly varied, including the region's symbol, the Abruzzo chamois (Rupicapra pyrenaica ornata), which has recovered from near-extinction. Animals typical of this region include: marsican brown bear, along with Italian wolf, deer, lynx, roe deer, snow vole, fox, porcupine, wild cat, wild boar, badger, otter, and viper.

 

The natural parks of the region include the Abruzzo National Park, the Gran Sasso and Monti della Laga National Park,[24] the Maiella National Park and the Sirente-Velino Regional Park, as well as many other natural reserves and protected areas.

 

Economy

Until a few decades ago, Abruzzo was a region of poverty in Southern Italy; over the past decades, however, it has developed to such an extent that it has escaped from the spiral of underdevelopment to become the 'first' region of the 'Italian Mezzogiorno'. This confirms its pivotal role in the national economic system. Since the 1950s, Abruzzo has had steady economic growth. In 1951, Abruzzo per capita income or GDP was 53% of that of Northern Italy, the nation's richest region. By 1971, Abruzzo was at 65% and, by 1994, per capita income was at 76% of Northern Italy's per capita income, giving Abruzzo the highest per capita GDP of Southern Italy and surpassing the growth of every other region of Italy. The construction of autostrade (motorways) from Rome to Teramo (A24) and Rome to Pescara (A25) opened Abruzzo to easy access. State and private investment in the region increased, and Abruzzo attained higher per capita education levels and greater productivity growth than the rest of the South. As of 2003, Abruzzo's per capita GDP was €19,506 or 84% of the national average of €23,181 and well outpacing that of the South (€15,808). The region's average GDP per capita was approximately 20,100 EUR.

 

The 2009 L'Aquila earthquake led to a sharp economic slowdown. However, according to statistics at the end of 2010, it seems that the economy of Abruzzo is recovering, despite the negative on regarding employment.[28] In fact, at the end of 2010, Abruzzo's growth was 1.47%, which placed it fourth among the Italian regions with the highest annual growth rates after Lazio, Lombardy and Calabria.[30] In 2011 Abruzzo's economic growth was +2.3%, the highest percentage among the regions of Southern Italy.[31] The region is also the richest region of Southern Italy, with a GDP per capita of €25,700.[21]

Travel poster from the 1920s.

 

Abruzzo's industrial sector expanded rapidly, especially in mechanical engineering, transportation equipment and telecommunications. The structure of production in the region reflects the transformation of the economy from agriculture to industry and services. Although industry has developed strongly, it retains weak points due to the existence of only a few large businesses alongside a huge fabric of small and medium-sized businesses. Both pure and applied research are carried out in the region, where there are major institutes and factories involved in research in the fields of pharmaceutics, biomedicine, electronics, aerospace and nuclear physics. The industrial infrastructure is spread throughout the region in industrial zones. The most important of these are: Val Pescara, Val Sangro, Val Trigno, Val Vibrata and Conca del Fucino. A further activity worthy of note is seaside and mountain tourism, which is of considerable importance to the economy of the region.[33] Agriculture, involving small holdings, has succeeded in modernising and offering high-quality products. The mostly small, agricultural holdings produce: wine, cereals, sugar beet, potatoes, olives, vegetables, fruit and dairy products. Traditional products are saffron and liquorice. Most famous in the world is Abruzzo's wine Montepulciano d'Abruzzo; in the late 20th and early 21st century, Montepulciano d'Abruzzo earned a reputation as being one of the most widely exported DOC classed wine in Italy.[34]

 

In the past decade, tourism has increased, in particular by internal and European arrivals. Abruzzo is world-famous for its wildlife parks (Abruzzo National Park, Gran Sasso and Monti della Laga National Park, Maiella National Park) and regional park (Sirente Velino), and 38 protected areas between oasis, regional reserves, and state reserves. The inland mountainous region contains several ski resorts, and coastal tourism is also well-developed, in particular, the Trabocchi Coast. Abruzzo's castles and medieval towns, especially around the town of L'Aquila, have earned it in some quarters the nickname of "Abruzzoshire", by analogy with the "Chiantishire", nickname sometimes used to refer to the Chianti area of Tuscany, but Abruzzo is still off the beaten path for most visitors to Italy.[35]

 

Chieti

Although the population density of Abruzzo has increased over recent decades, it is still well below the Italian national average: in 2008, 123.4 inhabitants per km2, compared to 198.8. In the provinces, the density varies: as of 2008 Pescara is the most densely populated with 260.1 inhabitants per km2, whereas L'Aquila is the least densely populated with 61.3 inhabitants per km2, although it has the largest area. After decades of emigration from the region, the main feature of the 1980s is immigration from third world countries. The population increase is due to the positive net migration. Since 1991 more deaths than births were registered in Abruzzo (except for 1999, when their numbers were equal).[36] In 2008, the Italian national institute of statistics ISTAT estimated that 59,749 foreign-born immigrants live in Abruzzo, equal to 4.5% of the total regional population.

 

The most serious demographic imbalance is between the mountainous areas of the interior and the coastal strip. The largest province, L'Aquila, is situated entirely in the interior and has the lowest population density. The movement of the population of Abruzzo from the mountains to the sea has led to the almost complete urbanization of the entire coastal strip especially in the province of Teramo and Chieti. The effects on the interior have been impoverishment and demographic aging, reflected by an activity rate in the province of L'Aquila which is the lowest among the provinces in Abruzzo – accompanied by geological degradation as a result of the absence of conservation measures. In the coastal strip, however, there is such a jumble of accommodations and activities that the environment has been negatively affected. The policy of providing incentives for development has resulted in the setting-up of industrial zones, some of which (Vasto, Avezzano, Carsoli, Gissi, Val Vibrata, Val di Sangro) have made genuine progress, while others (Val Pescara, L'Aquila) have run into trouble after their initial success. The zones of Sulmona and Guardiagrele have turned out to be more or less failures. Outside these zones, the main activities are agriculture and tourism.

 

Main settlements

L'Aquila is both the capital city of the Abruzzo region and of the Province of L'Aquila and second largest city (pop. 73,000). L'Aquila was hit by an earthquake on 6 April 2009, which destroyed much of the city centre. The other provincial capitals are Pescara, which is Abruzzo's largest city and major port (pop. 123,000); Teramo (pop. 55,000) and Chieti (pop. 55,000). Other large municipalities in Abruzzo include the industrial and high tech center Avezzano (pop. 41,000), as well as three important industrial and touristic centers such as Vasto (pop. 40,636), Lanciano (pop. 36,000), and Sulmona (pop. 25,000).

 

Transport

Airports

 

Abruzzo International Airport is the only international airport in the region. Open to civilian traffic since 1996, the number of passengers has increased over the years because of low-cost air carriers' use of the facility. Today, the airport has a catchment area of over 500,000 passengers annually and connects the city of Pescara and the entire region with many Italian and Europe destinations.

L'Aquila-Preturo Airport is located in the nearby village of Courts and was recently renovated and modernized to accommodate presidential flights for G8 activities.

 

Ports

There are four main ports in Abruzzo: Pescara, Ortona, Vasto and Giulianova.

 

Over the years the Port of Pescara became one of the most important tourist ports of Italy and the Adriatic Sea. Heavily damaged in World War II, it underwent some sixty years of major restoration and was reborn as a modern marina with advanced moorings and shipbuilding facilities. It has been honored with the European Union's blue flag for the quality of services offered. The port of Pescara has lost passenger traffic because of its shallowness and silting, but its fishery and aquaculture activities are thriving.[38]

Railways

 

There is a significant disparity between the railways of the Abruzzo coast and the inland areas, which badly need modernization to improve the service, in particular, the Rome-Pescara line.

 

Existing railway lines:

Adriatic railway runs through the whole of Italy from north to south, along the Adriatic Sea.

Train Rome – Sulmona – Pescara

Sulmona – Carpinone

Sulmona–Terni railway

Avezzano railroad – Roccasecca

Giulianova – Teramo

Sangritana (Lanciano – Castel di Sangro)

 

Highways

There are three highways that serve the region:

 

Highway A24 Rome – L'Aquila – Teramo, was built in the 1970s and connects Rome with Lazio and more specifically to the Abruzzo Teramo via L'Aquila. It performs an important liaison function of the region, both Tyrrhenian to the Adriatic, due to the presence of several interchanges of connecting roads and highways. The Gran Sasso tunnel, the longest road tunnel entirely on Italian territory, was opened in 1984. It connects L'Aquila and Teramo on the A24 making the northern Abruzzo coast reachable within two hours from Rome.

 

Highway A25 Turin – Avezzano – Pescara makes the connection between Rome and Pescara. The road running out of Turin begins its journey where it branches off the A24, runs into the Conca del Fucino, crosses the Abruzzo Apennines, comes to the valley of Peligna, and ends at the exit for Pescara-Villanova to join the A14.

Motorway A14 Bologna – Taranto known as the A14 "Adriatica", includes 743 km (461.68 mi) of road, including lengths in the cities of Bologna and Taranto. Opened to traffic in 1965, it is now a major tourist road, running through the coastal towns of Emilia Romagna, Marche, Abruzzo, Molise, and Apulia.

 

Culture

Castel del Monte, one of Abruzzo's little-known hill towns

Gabriele d'Annunzio from Pescara

Abbazia di San Liberatore a Majella (Serramonacesca)

Ovid from Sulmona

Cathedral of San Giustino (Chieti)

Fishing trabucco of San Vito Chietino

 

The museum Museo Archeologico Nazionale d'Abruzzo in Chieti houses the famed warrior statue Warrior of Capestrano which was found in a necropolis from 6th century B.C. Of cultural importance are: Teramo Cathedral, its archeological museum and Roman theater, the Castello della Monica, the Collurania-Teramo Observatory, the famous L'Aquila Basilica of Santa Maria di Collemaggio (which holds the remains of Pope Celestine V), the Museo Nazionale d'Abruzzo, Santa Maria del Suffragio, the Forte Spagnolo, the Fountain of 99 Spouts, Gabriele D'Annunzio's house in Pescara, Campli's Scala Sancta and its church, the church of Santissima Annunziata in Sulmona, the cathedrals of Chieti, Lanciano, Guardiagrele, Atri and Pescara along with the castles of Ortona, Celano and Ortucchio.

 

Every 28–29 August, L'Aquila's Santa Maria di Collemaggio commemorates the Perdonanza Celestiniana, the indulgence issued by Pope Celestine V to any who, "truly repentant and confessed" would visit that Church from the Vespers of the vigil to the vespers of 29 August.[39] Sulmona's Holy Week is commemorated with traditional celebrations and rituals, such as 'La Madonna che Scappa in Piazza', where a large statue of the Madonna, carried by a group of Sulmonesi part of Confraternities, is taken through the square towards her resurrected Son.[40] Cocullo, in the province of L'Aquila, holds the annual 'Festa dei serpari' (festival of snake handlers) in which a statue of St. Dominic, covered with live snakes, is carried in a procession through the town; it attracts thousands of Italian and foreign visitors. In many Abruzzo villages, Anthony the Great's feast is celebrated in January with massive and scenic bonfires.[41] In the past, the region of Abruzzo was well known for the transumanza, the migratory movement of sheep principally south to the region of Puglia during the cold winter months.[42] The Feast of St. Biagio, protector of wool dealers, is the most widespread in Abruzzo. On the third of February in Taranta Peligna every year since the sixteenth century an evocative ritual is carried out, entailing the distribution of panicelle, which are small loaves made of flour and water, in the shape of a blessing hand, which are distributed to the faithful.

 

Historical figures include: the Roman orator Asinius Pollio; Latin poets Sallust and Ovid, who were born in L'Aquila and Sulmona respectively, Gaius Cassius Longinus, Roman senator and leading instigator of the plot to kill Julius Caesar; and Pontius Pilate, who was born in the province of Teramo and is best known for authorizing the crucifixion of Jesus. Abruzzo's religious personalities include Saint Berardo; John of Capistrano, who led a crusade against the Ottoman Empire; Thomas of Celano, author of three hagiographies about Saint Francis of Assisi; and Alessandro Valignano, who introduced Catholicism to the Far East and Japan. The Polish Pope John Paul II loved the mountains of Abruzzo, where he would retire often and pray in the church of San Pietro della Ienca. When he died, Cardinal Stanislaw Dziwisz, gave the local Abruzzo community some of the late pontiff's blood as a token of the love he had felt for the mountainous area.[43] The greatest Italian poet of the 20th century Gabriele D'Annunzio was from Pescara; other notable Abruzzo personalities in the field of humanities include: poet Ignazio Silone, director Ennio Flaiano who co-wrote La dolce vita, philosopher Benedetto Croce, composer Sir Paolo Tosti and the sculptor Venanzo Crocetti.

 

American artists and celebrities such as: Madonna, Dean Martin, Bradley Cooper, Perry Como, Henry Mancini, Nancy Pelosi, Rocky Marciano, Rocky Mattioli, Bruno Sammartino, Mario Batali, John and Dan Fante, Tommy Lasorda, Dan Marino, Mario Lanza, Garry Marshall, Penny Marshall, Al Martino, Ariana Grande and Canadian Michael Bublé have Abruzzo origins.

 

Some international movies shot in Abruzzo include The American, Jean-Jacques Annaud's The Name of the Rose, Fellini's La Strada and I Vitelloni, Schwarzenegger's Red Sonja, Ladyhawke, King David, Francesco, Keoma, The Barbarians, The Fox and the Child and Krull.

Medieval and Renaissance hill towns

The fortress of Civitella is the most visited monument in Abruzzo

 

For most of its history, a large number of the Abruzzese people have been hill people, often working as shepherds in mountainous areas, or establishing hill towns, especially in the parts of Abruzzo further from the Adriatic coast.[citation needed] Before the 2009 earthquake, Abruzzo was the region with the highest number of castles and hill towns in Italy, but it still holds many of Italy's best-preserved medieval and Renaissance hill towns, twenty-three of which are among The Most Beautiful Villages in Italy.[44] These awards are not only for aesthetic beauty but also for art and culture, historical importance and livability.

 

The abrupt decline of Abruzzo's agricultural economy in the early to mid-20th-century saved some of the region's historic hill towns from modern development. Many lie entirely within regional and national parks. Among the most well preserved are Castel del Monte and Santo Stefano di Sessanio, which lie in the Gran Sasso National Park on the edge of the high plain of Campo Imperatore and nestled beneath the Apennines' highest peaks. Both hill towns, which were ruled by the Medicis for over a century-and-a-half, have relatively little tourism. Between the two towns sits Rocca Calascio, the ruin of an ancient fortress popular with filmmakers. Both Monteferrante and Roccascalegna are two of the most representative Abruzzo villages in the province of Chieti. Within the Gran Sasso National Park is also found Castelli, an ancient pottery center whose artisans produced ceramics for most of the royal houses of Europe.

 

Civitella del Tronto played a crucial role in the history of the unification of Italy. The fortress of Civitella is the most visited monument in the Abruzzo region today.[45] Other medieval hill towns located fully within Abruzzo's park system are Pacentro in the Maiella National Park and Pescasseroli in the Abruzzo National Park. Pacentro, which features a 14th-century castle with two intact towers, has been little touched by modernisation. The Shrine of Gabriel of Our Lady of Sorrows, in the province of Teramo, which attracts some two million visitors per year, is one of the 15 most-visited sanctuaries in the world.[46] Capestrano, a small town in the province of L'Aquila, is the hometown of Saint John of Capistrano, Franciscan friar and Catholic priest, as well as the namesake of the Franciscan missions San Juan Capistrano in Southern California, the mission Mission San Juan Capistrano (Texas) and the city of San Juan Capistrano in Orange County. Giulianova is a notable example of a Renaissance "ideal city."

 

The proximity to Rome, the protected natural reserves and landscapes which make the region one of the greenest in Europe, the presence of some of the most beautiful Italian villages, its rich and heterogeneous gastronomy, along with a long history of deep-rooted local tradition and authentic Italian culture, make Abruzzo fifth among Italian regions for tourist visits after Calabria, Marche, Sardinia and Trentino. In 2010, visitors included 6,381,067 Italians and 925,884 foreign tourists.

 

In 2015, the American organization Live and Invest Overseas included Abruzzo on its list of World's Top 21 Overseas Retirement Havens. The study was based on such factors as climate, infrastructure, health care, safety, taxes, cost of living and more. In 2017 the Chamber of Commerce of Pescara presented Abruzzo region to the Annual conference of Live and Invest Overseas in Orlando (USA). One year later, in October 2018, Live and Invest Overseas held its first conference in Abruzzo.

 

Universities

There are three universities in the Abruzzo region:

University of L'Aquila

D'Annunzio University of Chieti–Pescara

University of Teramo

 

Harvard University bases an intensive summer Italian language and culture program in Vasto, a resort town on Abruzzo's southern coast.

 

Science

Between the province of Teramo and L'Aquila, under the Gran Sasso Tunnel, is the Laboratori Nazionali del Gran Sasso (LNGS) of the INFN, one of the three underground astroparticle laboratories in Europe.

 

The Istituto Zooprofilattico Sperimentale dell'Abruzzo e del Molise "Giuseppe Caporale", which conducts research in veterinary and environmental public health, is located in Teramo.

 

The Gran Sasso Science Institute, located in L'Aquila, is an advanced research institute which offers doctorates in astroparticle physics, computer science, and mathematics as well as urban studies and regional science, and which also conducts scientific research.

Sports

 

Interamnia World Cup, the largest international youth handball competition worldwide, takes place yearly in Teramo.[51]

 

There are several football clubs in Abruzzo. Delfino Pescara 1936 is a Serie B club; based in Pescara, its home stadium is Stadio Adriatico – Giovanni Cornacchia.

Dialects

 

The regional dialects of Abruzzo include Teramano, Abruzzese Orientale Adriatico and Abruzzese Occidentale. The first two form part of the dialect of southern Italy also known simply as "Neapolitan" since the region has been part of the Kingdom of Naples and the Kingdom of the Two Sicilies, while Aquilano is related to the Central Italian dialects including Romanesco. The dialects spoken in the Abruzzo region can be divided into three main groups:

Sabine dialect, in the province of L'Aquila (central Italian dialects)

Abruzzo Adriatic dialect, in the province of Teramo, Pescara and Chieti, that is virtually abandoned in the province of Ascoli Piceno (southern Italian dialects)

Abruzzo western dialect, in the province of L'Aquila (southern Italian dialects)

 

Cuisine

Renowned for its variety and richness due to the heterogeneity of its territory, Abruzzo's cuisine is among the best in Italy. In 2013 an Italian organization Confesercenti survey of foreign tourists showed that Abruzzo is the best Italian region to eat in. Both the agricultural and coastal aspects of Abruzzo have contributed to its cuisine. Due to the mountains, much of Abruzzo was isolated from international influence until the 20th century. As a result, the region's cuisine remained unique.

 

Popular dishes

One of the most popular regional dishes is spaghetti alla chitarra which is made by pressing or cutting pasta through a chitarra, an implement to form long thin noodles similar to spaghetti. The pasta is served with a tomato-based sauce, often flavored with peppers, pork, goose, or lamb. This dish is complemented by regional side dishes, such as the bean and noodle soup, sagne e fagioli. This soup is traditionally flavored with tomatoes, garlic, oil, and peperoncini. In terms of common ingredients, cuisine in Abruzzo often includes:

 

Lamb and mutton, primarily in the mountains.[54] Sheep's milk (or ricotta) is an important source of Abruzzese cheese, and lamb intestines are used as sausage casing or for stuffed meat rolls.[54][55] Mountain goat meat is also common in Abruzzo.

Truffles and mushrooms, particularly wild mushrooms from the forests and hills

Garlic, especially red garlic

Rosemary

Hot chili pepper or peperoncini, regionally known as diavolilli or diavoletti, is common in Abruzzese cuisine and often used to add spice to dishes. Abruzzo residents are well known for frequently adding peperoncini, or hot peppers, to their meals.

Vegetables such as lentils, grasspeas and other legumes, artichoke, eggplant, and cauliflower[54][55][56][57]

 

Other popular dishes include:

Gnocchi carrati, flavored with bacon, eggs and pecorino cheese

Scrippelle, a rustic French-style crêpe served either mbusse (a type of soup) or used to form a sort of soufflé with some ragù and stuffed with chicken liver, meatballs, hard-boiled eggs, and cheese

Pastuccia, a polenta stew with sausage, eggs, and cheese

 

Across the region, roast lamb is enjoyed in several variations. Some of these variations include:

 

Arrosticini, a skewered lamb dish

Pecora al cotturo, lamb stuffed with a variety of mountain herbs and cooked in a copper pot

Lamb cooked whole in a bread oven

Agnello cacio e ovo, a lamb-based fricassee

Mazzerella: lamb intestines stuffed with lamb, garlic, marjoram, lettuce, and spices

Le virtù: a soup from Teramo filled with legumes, vegetables and pork, usually eaten in the spring at celebrations

Timballo abruzzese: lasagna-like dish with pasta sheets (scrippelle) layered with meat, vegetables and rice; often served for Christmas and Easter[58]

Porchetta abruzzese: moist boneless-pork roast, slow-roasted with rosemary, garlic, and pepper[58]

 

Seafood is also popular, especially in coastal areas. The variety of fish available to the area has resulted in several fish-based Brodetti (broths), coming from such places as Vasto, Giulianova, and Pescara. These broths are often made by cooking fish, flavored with tomatoes, herbs, and peperoncino, in an earthenware pot. Rustic pizzas are also very common. Some of these are:

 

Easter Pizza, a rustic cake with cheese and pepper from the Teramo area

Fiadoni from Chieti, a dough of eggs and cheese well risen, cooked in the oven in a thin casing of pastry

A rustic tart pastry filled with everything imaginable: eggs, fresh cheeses, ricotta, vegetables, and all sorts of flavorings and spices.

 

Also from Teramo are the spreadable sausages flavored with nutmeg, and liver sausages tasting of garlic and spices. The ventricina from the Vasto area is made with large pieces of fat and lean pork, pressed and seasoned with powdered sweet peppers and fennel all encased in the dehydrated stomach of the pig itself. Atri and Rivisondoli are famous for cheeses. Mozzarella, either fresh or seasoned, is made from ewe's milk, although a great number of lesser known varieties of these cheeses can be found all over Abruzzo and Molise.

Sweets

 

The Abruzzo's sweets are world-famous and include:

 

Confetti, sugar-coated almonds, from Sulmona

Torrone Nurzia, a chocolate nougat from L'Aquila

Parrozzo , a cake-like treat made from a mixture of crushed almonds, and coated in chocolate.

Ferratelle (also known as Pizzelle). A wafer cookie, often flavored with anise

Croccante, a type of nougat made from almonds and caramelized suger, often flavored with lemon[59]

 

A Montepulciano d'Abruzzo wine labelled as being made from old vines.

Olive oil

 

The extra-virgin olive oil produced in Colline Teramane (Teramo hills) is marked by the DOP.[60]

 

The region has several cultivars that includes Carboncella, Dritta (Dritta Francavillese and Dritta di Moscufo), Gentile del Chieti, Nostrana (Nostrana di Brisighella), and Sargano olive cultivars.[61]

Wines and liquors

 

Renowned wines like Montepulciano DOCG and Trebbiano d'Abruzzo DOC are judged to be amongst the world's finest.[62] In 2012, a bottle of Trebbiano d'Abruzzo ranked No. 1 in the top 50 Italian wine awards.[63] In recent decades these wines have been joined, particularly, by wines from lesser known (heritage) white grapes, such as, Pecorino, Cococciola, Passerina, Montonico Bianco and Fiano.[64]

 

The region is also well known for the production of liquors such as Centerbe, Limoncello, Ratafia and Genziana.

at Bryn Oh's Gathering

 

maps.secondlife.com/secondlife/Immersiva/12/108/23

The average achievement in NSW hospitals is 79.6%.

 

[Enhanced phone camera image]

 

Westmead Hospital, Sydney, Australia (Thursday 7 September 2017)

The much-loved mallard is our most familiar duck, found across town and country. If your feeding the ducks please don't feed them bread - it's not good for them! Instead, they love eating sweetcorn, lettuce, oats and seeds.

 

Statistics

Length: 55-62cm

Wingspan: 90cm

Weight: 970g-1.2kg

Average lifespan: 3 years

Conservation status

Classified in the UK as Amber under the Birds of Conservation Concern 4: the Red List for Birds (2021). Protected in the UK under the Wildlife and Countryside Act, 1981.

 

When to see

January to December

Cuenca es un municipio español perteneciente a la comunidad autónoma de Castilla-La Mancha y una ciudad, capital de la provincia homónima. Está situada algo al norte del centro geográfico de la provincia, a una altitud media de 946 msnm y su extenso término municipal, de 911.06 km² es uno de los mayores de España. El municipio contaba con una población empadronada de 56.703 habitantes en 2011.

 

Cuenca is a Spanish municipality located in the autonomous community of Castilla-La Mancha and a city, capital of the homonymous province. It is situated some north of the geographic center of the province, at an average altitude of 946 m and its extensive municipal, of 911.06 km ² is one of the largest in Spain. The municipality had a registered population of 56,703 inhabitants in 2011.

Preset Style = ナチュラル

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Paint = Natural

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Current estimates of average nodule abundance in four major locations.

 

For any form of publication, please include the link to this page:

www.grida.no/resources/7366

 

This photo has been graciously provided to be used in the GRID-Arendal resources library by: GRID-Arendal

On average / there is 20 years / between moving from house / to house or / as an alternative / between renovation / of the bathroom / and the kitchen.

Künstler Sir Tony Cragg, Standort Bonn

Average seeing, great experience :)

 

Skywatcher 10" dobson

Zwo ASI224MC colour camera

TeleVue 2.5x powermate

Baader IR-Pass filter

Circa 1973. I remember this young woman as taller than average. She wasn't abnormally tall, mind you, simply taller than most of the other female students. She may have been tall as I was at the time.

 

In any case, I remember her as a sweet and lovely young woman. A resident of College Park West, I first met her as the friend of another friend, who also lived in College Park West.

 

College Park West sits between the San Diego Freeway (I-405) and the Los Angeles-Orange County Line. In order to access College Park West (Seal Beach in Orange County), one necessarily has to exit Orange County into Los Angeles County first. It sounds somewhat odd, but it is true.

 

Taken with my father's Contax IIa 35mm rangefinder camera with 5cm f/1.5 Carl Zeiss Sonnar lens.

The Saguaro cactus in the picture is about 75 years old. That is the average age they get their first arms. The one in left background at around 6 feet tall is about 35 years old.

The one thing that unites all human beings, regardless of age, gender, religion or ethnic background, is that we all believe we are above-average drivers. ~ Dave Barry

(yup, he's right.... except with me, it's true! ;-)

And I know it's super late to enter for Me Again Monday, but I'm throwin' it in there! Theme: Quotes

After transitioning off the Jacob's Ladder Trestle, Mt. Washington Cog Railway trains tackle this stretch of track, known as "Long Trestle", with an average grade of 25%....which is damn steep! The trestle is not named for someone named Long, but is so-named purely because of its length. This structure affords the passengers an awesome view of the 1900 ft. deep Burt Ravine on the left side of the train. Folks who are squeamish about heights might want to avoid sitting on the left side here, as it's a pretty steep drop-off. A quick look to the right reveals that we're pretty much reaching the tree line here. This is the last of the Krummholtz. From here on up, this mountain is nothing but grass and granite. There is a reason it is called "The Rockpile."

 

In this image, you can see the results of the recent re-railing effort undertaken by the railway. For over 100 years, the rails used here were 25 lb. light rail, spiked to support timbers (called "side pieces"), which sat on top of the ties. The side pieces were necessary to build the rail up to the height of the cog rack, which also sits on similar support timbers (called "center pieces.") Needless to say, the additional lumber supporting the rails was a constant maintenance headache. The light rail also made for a rougher ride and was never designed to handle the heavy diesel hydraulic locomotives in use now, or the increased train traffic. To improve the situation, the railway has replaced all of the 25 lb. rail with 100 lb. rail, which is tall enough to no longer require the side pieces. The track is now more robust and the ride is smoother. The cog rack still sits on support timbers, but unlike the rails, it has to be replaced periodically, as it does wear out, so the wood is replaced when this happens. Why was the cog rack elevated to begin with? Mainly because the gearing for the cog wheels on the steam locomotives hangs below the level of the wheels which ride on the rails, so both the rails and the cog rack needed to be tall enough to allow the gears to clear the cross-ties. Got all of that?

Craters of the Moon National Monument and Preserve is a U.S. national monument and national preserve in the Snake River Plain in central Idaho. It is along US 20 (concurrent with US 93 and US 26), between the small towns of Arco and Carey, at an average elevation of 5,900 feet (1,800 m) above sea level.

 

The Monument was established on May 2, 1924. In November 2000, a presidential proclamation by President Clinton greatly expanded the Monument area. The 410,000-acre National Park Service portions of the expanded Monument were designated as Craters of the Moon National Preserve in August 2002. It spreads across Blaine, Butte, Lincoln, Minidoka, and Power counties. The area is managed cooperatively by the National Park Service and the Bureau of Land Management (BLM).

 

The Monument and Preserve encompass three major lava fields and about 400 square miles (1,000 km2) of sagebrush steppe grasslands to cover a total area of 1,117 square miles (2,893 km2). The Monument alone covers 343,000 acres (139,000 ha). All three lava fields lie along the Great Rift of Idaho, with some of the best examples of open rift cracks in the world, including the deepest known on Earth at 800 feet (240 m). There are excellent examples of almost every variety of basaltic lava, as well as tree molds (cavities left by lava-incinerated trees), lava tubes (a type of cave), and many other volcanic features.

 

Craters of the Moon is in south-central Idaho, midway between Boise and Yellowstone National Park. The lava field reaches southeastward from the Pioneer Mountains. Combined U.S. Highway 20–26–93 cuts through the northwestern part of the monument and provides access to it. However, the rugged landscape of the monument itself remains remote and undeveloped, with only one paved road across the northern end.

 

The Craters of the Moon Lava Field spreads across 618 square miles (1,601 km2) and is the largest mostly Holocene-aged basaltic lava field in the contiguous United States. The Monument and Preserve contain more than 25 volcanic cones, including outstanding examples of spatter cones. The 60 distinct solidified lava flows that form the Craters of the Moon Lava Field range in age from 15,000 to just 2,000 years. The Kings Bowl and Wapi lava fields, both about 2,200 years old, are part of the National Preserve.

 

This lava field is the largest of several large beds of lava that erupted from the 53-mile (85 km) south-east to north-west trending Great Rift volcanic zone, a line of weakness in the Earth's crust. Together with fields from other fissures they make up the Lava Beds of Idaho, which in turn are in the much larger Snake River Plain volcanic province. The Great Rift extends across almost the entire Snake River Plain.

 

Elevation at the visitor center is 5,900 feet (1,800 m) above sea level.

 

Total average precipitation in the Craters of the Moon area is between 15–20 inches (380–510 mm) per year. Most of this is lost in cracks in the basalt, only to emerge later in springs and seeps in the walls of the Snake River Canyon. Older lava fields on the plain have been invaded by drought-resistant plants such as sagebrush, while younger fields, such as Craters of the Moon, only have a seasonal and very sparse cover of vegetation. From a distance this cover disappears almost entirely, giving an impression of utter black desolation. Repeated lava flows over the last 15,000 years have raised the land surface enough to expose it to the prevailing southwesterly winds, which help to keep the area dry. Together these conditions make life on the lava field difficult.

 

Paleo-Indians visited the area about 12,000 years ago but did not leave much archaeological evidence. Northern Shoshone created trails through the Craters of the Moon Lava Field during their summer migrations from the Snake River to the camas prairie, west of the lava field. Stone windbreaks at Indian Tunnel were used to protect campsites from the dry summer wind. No evidence exists for permanent habitation by any Native American group. A hunting and gathering culture, the Northern Shoshone pursued elk, bears, American bison, cougars, and bighorn sheep — all large game who no longer range the area. The most recent volcanic eruptions ended about 2,100 years ago and were likely witnessed by the Shoshone people. Ella E. Clark has recorded a Shoshone legend which speaks of a serpent on a mountain who, angered by lightning, coiled around and squeezed the mountain until liquid rock flowed, fire shot from cracks, and the mountain exploded.

 

In 1879, two Arco cattlemen named Arthur Ferris and J.W. Powell became the first known European-Americans to explore the lava fields. They were investigating its possible use for grazing and watering cattle but found the area to be unsuitable and left.

 

U.S. Army Captain and western explorer B.L.E. Bonneville visited the lava fields and other places in the West in the 19th century and wrote about his experiences in his diaries. Washington Irving later used Bonneville's diaries to write the Adventures of Captain Bonneville, saying this unnamed lava field is a place "where nothing meets the eye but a desolate and awful waste, where no grass grows nor water runs, and where nothing is to be seen but lava."

 

In 1901 and 1903, Israel Russell became the first geologist to study this area while surveying it for the United States Geological Survey (USGS). In 1910, Samuel Paisley continued Russell's work and later became the monument's first custodian. Others followed and in time much of the mystery surrounding this and the other Lava Beds of Idaho was lifted.

 

The few European settlers who visited the area in the 19th century created local legends that it looked like the surface of the Moon. Geologist Harold T. Stearns coined the name "Craters of the Moon" in 1923 while trying to convince the National Park Service to recommend protection of the area in a national monument.

 

The Snake River Plain is a volcanic province that was created by a series of cataclysmic caldera-forming eruptions which started about 15 million years ago. A migrating hotspot thought to now exist under Yellowstone Caldera in Yellowstone National Park has been implicated. This hot spot was under the Craters of the Moon area some 10 to 11 million years ago but 'moved' as the North American Plate migrated northwestward. Pressure from the hot spot heaves the land surface up, creating fault-block mountains. After the hot spot passes the pressure is released and the land subsides.

 

Leftover heat from this hot spot was later liberated by Basin and Range-associated rifting and created the many overlapping lava flows that make up the Lava Beds of Idaho. The largest rift zone is the Great Rift; it is from this 'Great Rift fissure system' that Craters of the Moon, Kings Bowl, and Wapi lava fields were created. The Great Rift is a National Natural Landmark.

 

In spite of their fresh appearance, the oldest flows in the Craters of the Moon Lava Field are 15,000 years old and the youngest erupted about 2000 years ago, according to Mel Kuntz and other USGS geologists. Nevertheless, the volcanic fissures at Craters of the Moon are considered to be dormant, not extinct, and are expected to erupt again in less than a thousand years. There are eight major eruptive periods recognized in the Craters of the Moon Lava Field. Each period lasted about 1000 years or less and were separated by relatively quiet periods that lasted between 500 and as long as 3000 years. Individual lava flows were up to 30 miles (50 km) long with the Blue Dragon Flow being the longest.

 

Kings Bowl Lava Field erupted during a single fissure eruption on the southern part of the Great Rift about 2,250 years ago. This eruption probably lasted only a few hours to a few days. The field preserves explosion pits, lava lakes, squeeze-ups, basalt mounds, and an ash blanket. The Wapi Lava Field probably formed from a fissure eruption at the same time as the Kings Bowl eruption. More prolonged activity over a period of months to a few years led to the formation of low shield volcanoes in the Wapi field. The Bear Trap lava tube, between the Craters of the Moon and the Wapi lava fields, is a cave system more than 15 miles (24 km) long. The lava tube is remarkable for its length and for the number of well-preserved lava cave features, such as lava stalactites and curbs, the latter marking high stands of the flowing lava frozen on the lava tube walls. The lava tubes and pit craters of the monument are known for their unusual preservation of winter ice and snow into the hot summer months, due to shielding from the sun and the insulating properties of basalt.

 

A typical eruption along the Great Rift and similar basaltic rift systems starts with a curtain of very fluid lava shooting up to 1,000 feet (300 m) high along a segment of the rift up to 1 mile (1.6 km) long. As the eruption continues, pressure and heat decrease and the chemistry of the lava becomes slightly more silica rich. The curtain of lava responds by breaking apart into separate vents. Various types of volcanoes may form at these vents: gas-rich pulverized lava creates cinder cones (such as Inferno Cone – stop 4), and pasty lava blobs form spatter cones (such as Spatter Cones – stop 5). Later stages of an eruption push lava streams out through the side or base of cinder cones, which usually ends the life of the cinder cone (North Crater, Watchmen, and Sheep Trail Butte are notable exceptions). This will sometimes breach part of the cone and carry it away as large and craggy blocks of cinder (as seen at North Crater Flow – stop 2 – and Devils Orchard – stop 3). Solid crust forms over lava streams, and lava tubes (a type of cave) are created when lava vacates its course (examples can be seen at the Cave Area – stop 7).

 

Geologists feared that a large earthquake that shook Borah Peak, Idaho's tallest mountain, in 1983 would restart volcanic activity at Craters of the Moon, though this proved not to be the case. Geologists predict that the area will experience its next eruption some time in the next 900 years with the most likely period in the next 100 years.

 

All plants and animals that live in and around Craters of the Moon are under great environmental stress due to constant dry winds and heat-absorbing black lavas that tend to quickly sap water from living things. Summer soil temperatures often exceed 150 °F (66 °C) and plant cover is generally less than 5% on cinder cones and about 15% over the entire monument. Adaptation is therefore necessary for survival in this semi-arid harsh climate.

 

Water is usually only found deep inside holes at the bottom of blow-out craters. Animals therefore get the moisture they need directly from their food. The black soil on and around cinder cones does not hold moisture for long, making it difficult for plants to establish themselves. Soil particles first develop from direct rock decomposition by lichens and typically collect in crevices in lava flows. Successively more complex plants then colonize the microhabitat created by the increasingly productive soil.

 

The shaded north slopes of cinder cones provide more protection from direct sunlight and prevailing southwesterly winds and have a more persistent snow cover (an important water source in early spring). These parts of cinder cones are therefore colonized by plants first.

 

Gaps between lava flows were sometimes cut off from surrounding vegetation. These literal islands of habitat are called kīpukas, a Hawaiian name used for older land surrounded by younger lava. Carey Kīpuka is one such area in the southernmost part of the monument and is used as a benchmark to measure how plant cover has changed in less pristine parts of southern Idaho.

 

Idaho is a landlocked state in the Mountain West subregion of the United States. It shares a small portion of the Canada–United States border to the north, with the province of British Columbia. It borders Montana and Wyoming to the east, Nevada and Utah to the south, and Washington and Oregon to the west. The state's capital and largest city is Boise. With an area of 83,570 square miles (216,400 km2), Idaho is the 14th largest state by land area. With a population of approximately 1.8 million, it ranks as the 13th least populous and the 6th least densely populated of the 50 U.S. states.

 

For thousands of years, and prior to European colonization, Idaho has been inhabited by native peoples. In the early 19th century, Idaho was considered part of the Oregon Country, an area of dispute between the U.S. and the British Empire. It officially became a U.S. territory with the signing of the Oregon Treaty of 1846, but a separate Idaho Territory was not organized until 1863, instead being included for periods in Oregon Territory and Washington Territory. Idaho was eventually admitted to the Union on July 3, 1890, becoming the 43rd state.

 

Forming part of the Pacific Northwest (and the associated Cascadia bioregion), Idaho is divided into several distinct geographic and climatic regions. The state's north, the relatively isolated Idaho Panhandle, is closely linked with Eastern Washington, with which it shares the Pacific Time Zone—the rest of the state uses the Mountain Time Zone. The state's south includes the Snake River Plain (which has most of the population and agricultural land), and the southeast incorporates part of the Great Basin. Idaho is quite mountainous and contains several stretches of the Rocky Mountains. The United States Forest Service holds about 38% of Idaho's land, the highest proportion of any state.

 

Industries significant for the state economy include manufacturing, agriculture, mining, forestry, and tourism. Several science and technology firms are either headquartered in Idaho or have factories there, and the state also contains the Idaho National Laboratory, which is the country's largest Department of Energy facility. Idaho's agricultural sector supplies many products, but the state is best known for its potato crop, which comprises around one-third of the nationwide yield. The official state nickname is the "Gem State."

 

The history of Idaho is an examination of the human history and social activity within the state of Idaho, one of the United States of America located in the Pacific Northwest area near the west coast of the United States and Canada. Other associated areas include southern Alaska, all of British Columbia, Washington, Oregon, western Montana and northern California and Nevada.

 

Humans may have been present in Idaho for 16,600 years. Recent findings in Cooper's Ferry along the Salmon River in western Idaho near the town of Cottonwood have unearthed stone tools and animal bone fragments in what may be the oldest evidence of humans in North America. Earlier excavations in 1959 at Wilson Butte Cave near Twin Falls revealed evidence of human activity, including arrowheads, that rank among the oldest dated artifacts in North America. Native American tribes predominant in the area in historic times included the Nez Perce and the Coeur d'Alene in the north; and the Northern and Western Shoshone and Bannock peoples in the south.

 

Idaho was one of the last areas in the lower 48 states of the US to be explored by people of European descent. The Lewis and Clark expedition entered present-day Idaho on August 12, 1805, at Lemhi Pass. It is believed that the first "European descent" expedition to enter southern Idaho was by a group led in 1811 and 1812 by Wilson Price Hunt, which navigated the Snake River while attempting to blaze an all-water trail westward from St. Louis, Missouri, to Astoria, Oregon. At that time, approximately 8,000 Native Americans lived in the region.

 

Fur trading led to the first significant incursion of Europeans in the region. Andrew Henry of the Missouri Fur Company first entered the Snake River plateau in 1810. He built Fort Henry on Henry's Fork on the upper Snake River, near modern St. Anthony, Idaho. However, this first American fur post west of the Rocky Mountains was abandoned the following spring.

 

The British-owned Hudson's Bay Company next entered Idaho and controlled the trade in the Snake River area by the 1820s. The North West Company's interior department of the Columbia was created in June 1816, and Donald Mackenzie was assigned as its head. Mackenzie had previously been employed by Hudson's Bay and had been a partner in the Pacific Fur Company, financed principally by John Jacob Astor. During these early years, he traveled west with a Pacific Fur Company's party and was involved in the initial exploration of the Salmon River and Clearwater River. The company proceeded down the lower Snake River and Columbia River by canoe, and were the first of the Overland Astorians to reach Fort Astoria, on January 18, 1812.

 

Under Mackenzie, the North West Company was a dominant force in the fur trade in the Snake River country. Out of Fort George in Astoria, Mackenzie led fur brigades up the Snake River in 1816-1817 and up the lower Snake in 1817-1818. Fort Nez Perce, established in July, 1818, became the staging point for Mackenzies' Snake brigades. The expedition of 1818-1819 explored the Blue Mountains, and traveled down the Snake River to the Bear River and approached the headwaters of the Snake. Mackenzie sought to establish a navigable route up the Snake River from Fort Nez Perce to the Boise area in 1819. While he did succeed in traveling by boat from the Columbia River through the Grand Canyon of the Snake past Hells Canyon, he concluded that water transport was generally impractical. Mackenzie held the first rendezvous in the region on the Boise River in 1819.

 

Despite their best efforts, early American fur companies in this region had difficulty maintaining the long-distance supply lines from the Missouri River system into the Intermountain West. However, Americans William H. Ashley and Jedediah Smith expanded the Saint Louis fur trade into Idaho in 1824. The 1832 trapper's rendezvous at Pierre's Hole, held at the foot of the Three Tetons in modern Teton County, was followed by an intense battle between the Gros Ventre and a large party of American trappers aided by their Nez Perce and Flathead allies.

 

The prospect of missionary work among the Native Americans also attracted early settlers to the region. In 1809, Kullyspell House, the first white-owned establishment and first trading post in Idaho, was constructed. In 1836, the Reverend Henry H. Spalding established a Protestant mission near Lapwai, where he printed the Northwest's first book, established Idaho's first school, developed its first irrigation system, and grew the state's first potatoes. Narcissa Whitman and Eliza Hart Spalding were the first non-native women to enter present-day Idaho.

 

Cataldo Mission, the oldest standing building in Idaho, was constructed at Cataldo by the Coeur d'Alene and Catholic missionaries. In 1842, Father Pierre-Jean De Smet, with Fr. Nicholas Point and Br. Charles Duet, selected a mission location along the St. Joe River. The mission was moved a short distance away in 1846, as the original location was subject to flooding. In 1850, Antonio Ravalli designed a new mission building and Indians affiliated with the church effort built the mission, without nails, using the wattle and daub method. In time, the Cataldo mission became an important stop for traders, settlers, and miners. It served as a place for rest from the trail, offered needed supplies, and was a working port for boats heading up the Coeur d'Alene River.

 

During this time, the region which became Idaho was part of an unorganized territory known as Oregon Country, claimed by both the United States and Great Britain. The United States gained undisputed jurisdiction over the region in the Oregon Treaty of 1846, although the area was under the de facto jurisdiction of the Provisional Government of Oregon from 1843 to 1849. The original boundaries of Oregon Territory in 1848 included all three of the present-day Pacific Northwest states and extended eastward to the Continental Divide. In 1853, areas north of the 46th Parallel became Washington Territory, splitting what is now Idaho in two. The future state was reunited in 1859 after Oregon became a state and the boundaries of Washington Territory were redrawn.

 

While thousands passed through Idaho on the Oregon Trail or during the California gold rush of 1849, few people settled there. In 1860, the first of several gold rushes in Idaho began at Pierce in present-day Clearwater County. By 1862, settlements in both the north and south had formed around the mining boom.

 

The Church of Jesus Christ of Latter-Day Saints missionaries founded Fort Lemhi in 1855, but the settlement did not last. The first organized town in Idaho was Franklin, settled in April 1860 by Mormon pioneers who believed they were in Utah Territory; although a later survey determined they had crossed the border. Mormon pioneers reached areas near the current-day Grand Teton National Park in Wyoming and established most of the historic and modern communities in Southeastern Idaho. These settlements include Ammon, Blackfoot, Chubbuck, Firth, Idaho Falls, Iona, Pocatello, Rexburg, Rigby, Shelley, and Ucon.

 

Large numbers of English immigrants settled in what is now the state of Idaho in the late 19th and early 20th century, many before statehood. The English found they had more property rights and paid less taxes than they did back in England. They were considered some of the most desirable immigrants at the time. Many came from humble beginnings and would rise to prominence in Idaho. Frank R. Gooding was raised in a rural working-class background in England, but was eventually elected as the seventh governor of the state. Today people of English descent make up one fifth of the entire state of Idaho and form a plurality in the southern portion of the state.

 

Many German farmers also settled in what is now Idaho. German settlers were primarily Lutheran across all of the midwest and west, including Idaho, however there were small numbers of Catholics amongst them as well. In parts of Northern Idaho, German remained the dominant language until World War I, when German-Americans were pressured to convert entirely to English. Today, Idahoans of German ancestry make up nearly one fifth of all Idahoans and make up the second largest ethnic group after Idahoans of English descent with people of German ancestry being 18.1% of the state and people of English ancestry being 20.1% of the state.

 

Irish Catholics worked in railroad centers such as Boise. Today, 10% of Idahoans self-identify as having Irish ancestry.

 

York, a slave owned by William Clark but considered a full member of Corps of Discovery during expedition to the Pacific, was the first recorded African American in Idaho. There is a significant African American population made up of those who came west after the abolition of slavery. Many settled near Pocatello and were ranchers, entertainers, and farmers. Although free, many blacks suffered discrimination in the early-to-mid-late 20th century. The black population of the state continues to grow as many come to the state because of educational opportunities, to serve in the military, and for other employment opportunities. There is a Black History Museum in Boise, Idaho, with an exhibit known as the "Invisible Idahoan", which chronicles the first African-Americans in the state. Blacks are the fourth largest ethnic group in Idaho according to the 2000 census. Mountain Home, Boise, and Garden City have significant African-American populations.

 

The Basque people from the Iberian peninsula in Spain and southern France were traditionally shepherds in Europe. They came to Idaho, offering hard work and perseverance in exchange for opportunity. One of the largest Basque communities in the US is in Boise, with a Basque museum and festival held annually in the city.

 

Chinese in the mid-19th century came to America through San Francisco to work on the railroad and open businesses. By 1870, there were over 4000 Chinese and they comprised almost 30% of the population. They suffered discrimination due to the Anti-Chinese League in the 19th century which sought to limit the rights and opportunities of Chinese emigrants. Today Asians are third in population demographically after Whites and Hispanics at less than 2%.

 

Main articles: Oregon boundary dispute, Provisional Government of Oregon, Oregon Treaty, Oregon Territory, Washington Territory, Dakota Territory, Organic act § List of organic acts, and Idaho Territory

 

On March 4, 1863, President Abraham Lincoln signed an act creating Idaho Territory from portions of Washington Territory and Dakota Territory with its capital at Lewiston. The original Idaho Territory included most of the areas that later became the states of Idaho, Montana and Wyoming, and had a population of under 17,000. Idaho Territory assumed the boundaries of the modern state in 1868 and was admitted as a state in 1890.

 

After Idaho became a territory, legislation was held in Lewiston, the capital of Idaho Territory at the time. There were many territories acts put into place, and then taken away during these early sessions, one act being the move of the capital city from Lewiston to Boise City. Boise was becoming a growing area after gold was found, so on December 24, 1864, Boise City was made the final destination of the capital for the Territory of Idaho.

 

However, moving the capital to Boise City created a lot of issues between the territory. This was especially true between the north and south areas in the territory, due to how far south Boise City was. Problems with communicating between the north and south contributed to some land in Idaho Territory being transferred to other territories and areas at the time. Idaho’s early boundary changes helped create the current boundaries of Washington, Wyoming, and Montana States as currently exist.

 

In a bid for statehood, Governor Edward A. Stevenson called for a constitutional convention in 1889. The convention approved a constitution on August 6, 1889, and voters approved the constitution on November 5, 1889.

 

When President Benjamin Harrison signed the law admitting Idaho as a U.S. state on July 3, 1890, the population was 88,548. George L. Shoup became the state's first governor, but resigned after only a few weeks in office to take a seat in the United States Senate. Willis Sweet, a Republican, was the first congressman, 1890 to 1895, representing the state at-large. He vigorously demanded "Free Silver" or the unrestricted coinage of silver into legal tender, in order to pour money into the large silver mining industry in the Mountain West, but he was defeated by supporters of the gold standard. In 1896 he, like many Republicans from silver mining districts, supported the Silver Republican Party instead of the regular Republican nominee William McKinley.

 

During its first years of statehood, Idaho was plagued by labor unrest in the mining district of Coeur d'Alene. In 1892, miners called a strike which developed into a shooting war between union miners and company guards. Each side accused the other of starting the fight. The first shots were exchanged at the Frisco mine in Frisco, in the Burke-Canyon north and east of Wallace. The Frisco mine was blown up, and company guards were taken prisoner. The violence soon spilled over into the nearby community of Gem, where union miners attempted to locate a Pinkerton spy who had infiltrated their union and was passing information to the mine operators. But agent Charlie Siringo escaped by cutting a hole in the floor of his room. Strikers forced the Gem mine to close, then traveled west to the Bunker Hill mining complex near Wardner, and closed down that facility as well. Several had been killed in the Burke-Canyon fighting. The Idaho National Guard and federal troops were dispatched to the area, and union miners and sympathizers were thrown into bullpens.

 

Hostilities would again erupt at the Bunker Hill facility in 1899, when seventeen union miners were fired for having joined the union. Other union miners were likewise ordered to draw their pay and leave. Angry members of the union converged on the area and blew up the Bunker Hill Mill, killing two company men.

 

In both disputes, the union's complaints included pay, hours of work, the right of miners to belong to the union, and the mine owners' use of informants and undercover agents. The violence committed by union miners was answered with a brutal response in 1892 and in 1899.

 

Through the Western Federation of Miners (WFM) union, the battles in the mining district became closely tied to a major miners' strike in Colorado. The struggle culminated in the December 1905 assassination of former Governor Frank Steunenberg by Harry Orchard (also known as Albert Horsley), a member of the WFM. Orchard was allegedly incensed by Steunenberg's efforts as governor to put down the 1899 miner uprising after being elected on a pro-labor platform.

 

Pinkerton detective James McParland conducted the investigation into the assassination. In 1907, WFM Secretary Treasurer "Big Bill" Haywood and two other WFM leaders were tried on a charge of conspiracy to murder Steunenberg, with Orchard testifying against them as part of a deal made with McParland. The nationally publicized trial featured Senator William E. Borah as prosecuting attorney and Clarence Darrow representing the defendants. The defense team presented evidence that Orchard had been a Pinkerton agent and had acted as a paid informant for the Cripple Creek Mine Owners' Association. Darrow argued that Orchard's real motive in the assassination had been revenge for a declaration of martial law by Steunenberg, which prompted Orchard to gamble away a share in the Hercules silver mine that would otherwise have made him wealthy.

 

Two of the WFM leaders were acquitted in two separate trials, and the third was released. Orchard was convicted and sentenced to death. His sentence was commuted, and he spent the rest of his life in an Idaho prison.

 

Mining in Idaho was a major commercial venture, bringing a great deal of attention to the state. From 1860-1866 Idaho produced 19% of all gold in the United States, or 2.5 million ounces.

 

Most of Idaho's mining production, 1860–1969, has come from metals equating to $2.88 billion out of $3.42 billion, according to the best estimates. Of the metallic mining areas of Idaho, the Coeur d'Alene region has produced the most by far, and accounts for about 80% of the total Idaho yield.

 

Several others—Boise Basin, Wood River Valley, Stibnite, Blackbirg, and Owyhee—range considerably above the other big producers. Atlanta, Bear Valley, Bay Horse, Florence, Gilmore, Mackay, Patterson, and Yankee Fork all ran on the order of ten to twenty million dollars, and Elk City, Leesburg, Pierce, Rocky Bar, and Warren's make up the rest of the major Idaho mining areas that stand out in the sixty or so regions of production worthy of mention.

 

A number of small operations do not appear in this list of Idaho metallic mining areas: a small amount of gold was recovered from Goose Creek on Salmon Meadows; a mine near Cleveland was prospected in 1922 and produced a little manganese in 1926; a few tons of copper came from Fort Hall, and a few more tons of copper came from a mine near Montpelier. Similarly, a few tons of lead came from a property near Bear Lake, and lead-silver is known on Cassia Creek near Elba. Some gold quartz and lead-silver workings are on Ruby Creek west of Elk River, and there is a slightly developed copper operation on Deer Creek near Winchester. Molybdenum is known on Roaring River and on the east fork of the Salmon. Some scattered mining enterprises have been undertaken around Soldier Mountain and on Chief Eagle Eye Creek north of Montour.

 

Idaho proved to be one of the more receptive states to the progressive agenda of the late 19th century and early 20th century. The state embraced progressive policies such as women's suffrage (1896) and prohibition (1916) before they became federal law. Idahoans were also strongly supportive of Free Silver. The pro-bimetallism Populist and Silver Republican parties of the late 1890s were particularly successful in the state.

 

Eugenics was also a major part of the Progressive movement. In 1919, the Idaho legislature passed an Act legalizing the forced sterilization of some persons institutionalized in the state. The act was vetoed by governor D.W. Davis, who doubted its scientific merits and believed it likely violated the Equal Protection clause of the US Constitution. In 1925, the Idaho legislature passed a revised eugenics act, now tailored to avoid Davis's earlier objections. The new law created a state board of eugenics, charged with: the sterilization of all feebleminded, insane, epileptics, habitual criminals, moral degenerates and sexual perverts who are a menace to society, and providing the means for ascertaining who are such persons.

The Eugenics board was eventually folded into the state's health commission; between 1932 and 1964, a total of 30 women and eight men in Idaho were sterilized under this law. The sterilization law was formally repealed in 1972.

 

After statehood, Idaho's economy began a gradual shift away from mining toward agriculture, particularly in the south. Older mining communities such as Silver City and Rocky Bar gave way to agricultural communities incorporated after statehood, such as Nampa and Twin Falls. Milner Dam on the Snake River, completed in 1905, allowed for the formation of many agricultural communities in the Magic Valley region which had previously been nearly unpopulated.

 

Meanwhile, some of the mining towns were able to reinvent themselves as resort communities, most notably in Blaine County, where the Sun Valley ski resort opened in 1936. Others, such as Silver City and Rocky Bar, became ghost towns.

 

In the north, mining continued to be an important industry for several more decades. The closure of the Bunker Hill Mine complex in Shoshone County in the early 1980s sent the region's economy into a tailspin. Since that time, a substantial increase in tourism in north Idaho has helped the region to recover. Coeur d'Alene, a lake-side resort town, is a destination for visitors in the area.

 

Beginning in the 1980s, there was a rise in North Idaho of a few right-wing extremist and "survivalist" political groups, most notably one holding Neo-Nazi views, the Aryan Nations. These groups were most heavily concentrated in the Panhandle region of the state, particularly in the vicinity of Coeur d'Alene.

 

In 1992 a stand-off occurred between U.S. Marshals, the F.B.I., and white separatist Randy Weaver and his family at their compound at Ruby Ridge, located near the small, northern Idaho town of Naples. The ensuing fire-fight and deaths of a U.S. Marshal, and Weaver's son and wife gained national attention, and raised a considerable amount of controversy regarding the nature of acceptable force by the federal government in such situations.

 

In 2001, the Aryan Nations compound, which had been located in Hayden Lake, Idaho, was confiscated as a result of a court case, and the organization moved out of state. About the same time Boise installed an impressive stone Human Rights Memorial featuring a bronze statue of Anne Frank and quotations from her and many other writers extolling human freedom and equality.

 

The demographics of the state have changed. Due to this growth in different groups, especially in Boise, the economic expansion surged wrong-economic growth followed the high standard of living and resulted in the "growth of different groups". The population of Idaho in the 21st Century has been described as sharply divided along geographic and cultural lines due to the center of the state being dominated by sparsely-populated national forests, mountain ranges and recreation sites: "unless you're willing to navigate a treacherous mountain pass, you can't even drive from the north to the south without leaving the state." The northern population gravitates towards Spokane, Washington, the heavily Mormon south-east population towards Utah, with an isolated Boise "[being] the closest thing to a city-state that you'll find in America."

 

On March 13, 2020, officials from the Idaho Department of Health and Welfare announced the first confirmed case of the novel coronavirus COVID-19 within the state of Idaho. A woman over the age of 50 from the southwestern part of the state was confirmed to have the coronavirus infection. She contracted the infection while attending a conference in New York City. Conference coordinators notified attendees that three individuals previously tested positive for the coronavirus. The Idahoan did not require hospitalization and was recovering from mild symptoms from her home. At the time of the announcement, there were 1,629 total cases and 41 deaths in the United States. Five days beforehand, on March 8, a man of age 54 had died of an unknown respiratory illness which his doctor had believed to be pneumonia. The disease was later suspected to be – but never confirmed as – COVID-19.

 

On March 14, state officials announced the second confirmed case within the state. The South Central Public Health District, announced that a woman over the age of 50 that resides in Blaine County had contracted the infection.[44] Like the first case, she did not require hospitalization and she was recovering from mild symptoms from home. Later on in the day, three additional confirmed cases of COVID-19 were reported in the state by three of the seven health districts in the state, which brought the confirmed total cases of coronavirus to five in Idaho. Officials from Central District Health announced their second confirmed case, which was a male from Ada County in his 50s. He was not hospitalized and was recovering at home. South Central Public Health reported their second confirmed case in a female that is over the age of 70 who was hospitalized. Eastern Idaho Public Health reported a confirmed positive case in a woman under the age of 60 in Teton County. She had contracted the coronavirus from contact with a confirmed case in a neighboring state; she was not hospitalized. The South Central Public Health District announced that a woman over the age of 50 that resides in Blaine County had contracted the infection. Like the first case, she did not require hospitalization and she was recovering from mild symptoms from home.

 

On March 17, two more confirmed cases of the infection were reported, bringing the total to seven. The first case on this date was by officials from Central District Health reported that a female under the age of 50 in Ada County was recovering at home and was not hospitalized. The second confirmed case was a female over the age of 50 as reported by South Central Public Health officials.

 

On March 18, two additional confirmed cases were announced by South Central Public Health District officials. One is a male from Blaine County in his 40s and the other a male in his 80s from Twin Falls County. These cases were the first known community spread transmission of the coronavirus in South Central Idaho.

Tried something a bit different today. Got up at 5am to go downtown Houston to shoot some early morning shots. Came back with this that I was surprisingly happy with.

 

****I see now this is a bit confusing as to what you all are actually looking at.

 

This is a building, and I am looking almost VERTICAL up the wall and into the sky. A very mind melting perspective.

Me, sporting covid hair, wearing mask by Joe Average.

 

WIKI - "Joe Average (born October 10, 1957) is a Canadian artist who resides in Vancouver, British Columbia. Diagnosed HIV+ at age 27, Average made the decision to commit the rest of his life to art."

 

Joe is a beloved national icon, philanthropist and humanitarian. joeaverageart.com/

In the 1930's, Heber Springs was the largest town in Cleburne County, with a population of 1,400 residents. A nearby Post Oak school was a two-room school with two teachers. The average school year might be six months since children were often needed on the farm. In these days, receiving an 8th grade education was considered educated by Cleburne County standards.

 

This cotton gin was built in the 1930's by Dick Hunt. Dick lost his father when he was 11 years old, which soon left him to take responsibility to help his mother with six children. Some say this pushed him to become a great leader, one who would eventually be one of the most successful businessmen in Cleburne County. He married in the early 1920's and eventually had five sons and three daughters. He and his wife farmed through the late 1920's, then as the depression continued, he pursued other venues. He tried a "rolling store" (horse-drawn wagon), then later a truck. He was also known for carrying mail by horseback and operated several passenger buses. He built three cotton gins and other various drilling businesses.

 

Dick bought this cotton gin in Texas and had it shipped/moved to Heber Springs. He and his sons worked the Gin. Horse-drawn wagons carried cotton to the Gin. Dick Hunt had the only cotton gin in the northeast section of Cleburne County. Sometimes wagons were lined up the length of a football field waiting for their cotton to be ginned. Dick Hunt also had the largest mercantile store in Cleburne County. While some farmers waited for their cotton, they would buy a 'soda pop' and candy from Mr. Hunt's store. You could buy a hamburger and coke for thirty cents.

 

In 1949, the Arkansas State Legislature passed a law to consolidate the small one and two-room schools. In the fall of 1949, students from Post Oak were transferred to West Side Public School. This was the first time these students had an opportunity to ride a school bus. In the early 1960's, the Greers Ferry Dam and Lake was completed, covering the land which cotton had thrived, consequently slowing cotton production to a halt.

 

Heber Springs, Arkansas.

Photo # KS1_8585-8618hbws. February, 2012.

(c) Kelly Shipp Photography.

What you see is an average day, of a Targeted Individual, in the United States.

 

I was in Goodyear, Arizona. I drove by an Autozone store and decided to pull in and get a few parts. They were common parts, for routine maintenance on the motorhome. I had searched a few of the parts, the night before, on my cell phone. I had just left a laundromat, where the local police made an intentional presence. The Autozone was on the way home. I missed my turn, so I took the next road, and came in from the back. As I approached the back of the store; I was cut off by two guys in a large black truck. Yep, another one of those damn; Billy Bob Trucks. They pulled around to the front, and went in quickly.

I parked in front of the store. Then took Koda over to an area, where he could take a pee. As I walked towards the entrance; I saw a young guy standing beside a vintage Honda motorcycle. I’ve had a few in my younger years, so I stopped and had a pleasant conversation with him. I noticed his plates had expired in 2021. I didn’t mention it, and went inside. I thought the guy with the motorcycle was leaving, but he later came back into the store.

As Koda and I walked into the store, the two men in the black truck rushed out quickly, without a purchase. I walked over to an area, to grab a part I needed; but it wasn’t there. I went up to the counter and asked an older man, about the part. He walked over to the display I was looking at, and they didn’t have it. He reached down, and put his hand in Koda’s face. I said politely, “sir, he’s a service dog, please leave him alone”. Koda was wearing his large red, service dog, collar.

We went to the counter, so he could look up another part I needed. He spent a long time on the computer, went to the back, came back to the front and said “we don’t have it”. He was fidgeting with a few items I placed on the counter. As he did, he stood there staring directly into Koda’s eyes. As, you can see, in the screenshot above. He continued to stare at Koda’s eyes, after I repeatedly asked him not to. He finally told the man to stop, dogs take it as an act of aggression. Koda’s still laying at my left side. We were at the counter for a while, so Koda laid down, after setting. Which I’ve trained him to do.

The guy told me they didn’t have the part, left it at that, instead of seeing if another store had one. Again, a very common automotive part. I asked if he could locate one for me. As he took his time, with a pissy attitude, the guy in the top screenshot came from behind the counter. He leaned over, sat his backpack on the floor, right beside Koda. Once he stood up, something in the backpack startled the hell out of Koda. He jumped up, and was pulling away from the backpack. This is extremely uncommon for him. There was something in the backpack, that was frightened him. He wanted to get the both of us, away from it. The young guy, just stood there smiling. He was the same guy, I was talking with, about his motorcycle. Police will follow me from store to store, but won’t bother him, and his expired plates.

I wonder why????

Koda, has acted similar, when I took him to a couple doggy, day care facilities, on a second visit. One place in Gilbert, Arizona, he won’t even get out of the car. He just sat there trembling. It almost brought me to tears. Wondering what they had done to him, on a previous visit. I’ve had this happen at three facilities, I’ve taken him too. When I have MRIs, or X-rays, the VA, won’t allow him there. Unless someone can watch him in the waiting area. That’s just the VA. The last two weeks, I’ve had MRI’s and X-rays, at two different facilities, they allowed him, and loved him. He would lay on the floor, by a chair; after giving him the command to Wait. The last place, he sat up quickly, when the pain in my neck, produced pheromones. I explained to the technicians, they were amazed. He really is Magnificat.

So, the guy finally said there was another store close, they had the part I wanted. He said I could pay for the part there, and pick it up at the other store. I had a $10.00 coupon, with a barcode on my phone. I paid for the parts, and was headed out the door. Just ahead of me, was a woman with pink and purple hair. There was a guy, standing directly in front of my car. I hit the keyphob, didn’t hear the doors unlock. I pulled on the handle, it was unlocked. I locked it when we got out, but now, it’s unlocked. The guy standing in front of my car; looks at me and smiles. Once, in the car; I looked over my receipt, the $10, wasn’t deducted. I had to go back in. The guy argued with me, kept saying “you saw me scan it”. After some more bullshit, I got the $10.

Koda and I headed to the other store, to get the part I had paid for. As we walked in, an employee was leaving. I see at the counter, the woman with the pink and purple hair, from the other store we were just at. She, and the woman behind the counter, were talking away, stalling as much as they could. There was another guy, at a different register. I told him I had a paid part, to pick up. He pointed at the two women, said, she can help you. The women continued their conversation, while Koda and I stood there waiting. Koda, has amazing facial expressions, he knew I was getting a bit frustrated, and gives me his WTF, look. I patiently waited. Once at the counter, the woman was pleasant, and gave me my part. There was still another part I needed, so we were off to a different parts store. It wasn’t an Autozone, They didn’t have the part. The guy at the counter, gave me the name of another store, so Koda and I went out to the car to call them. I was on the phone forever, the person on the other end, stalling. It was a transmission pan, plug kit. Something that most auto parts stores carry. It was a part, I was looking at on Amazon, the night before. As Koda, and I set in the car, I’m still on the phone; a man pulls up beside us. He gets out, puts on a black backpack. He slowly walks across the front of our car, takes both hand, pushes up the bottom of the backpack, as he looks at us and smiles. Again, Koda tilts his head, gives me the WTF, look. Just after, the guy walks pass, here come another, Goodyear, AZ, police car. Driving slowing, across the front of our car. I finally gave up on the person, on the phone. We pull out of the parking lot, to the first intersection. We caught a red light. While setting there; here comes a perp, riding a bicycle on the sidewalk. He had a bright orange helmet, a basket on the back of his bicycle, filled with America Flags. I’ve caught trucks and vans before, dropping this kind of trash off, along my routs. It’s just another kick in the nuts. They love to throw the American flag, in my face, after the bullshit we just went through. Yep, folks, these people are proud as hell, for harassing a total stranger, and his service dog. By Golly, this is the United States of Merica. I’m sure you have seen, the Village Idiot, driving around in his big truck. Brandishing a huge American flag, in the truck bed. Doing this with pride, totally ignorant, of our own Constitution.

After I got home, I decided to check the 1st Autozone store, I went to. I wanted to see if they did have the part I needed. Yes, they did. I put in the Autozone store #2784, at 435 N Litchfield, Goodyear, Arizona. I searched the part number, and they had it in stock, the whole time. I took a screenshot, just to cover myself.

 

Any given week; tens of thousands, of Americans, are treated like this. This is what many Americans, are teaching their children. The many involved in Gangstalking, and Workplace Mobbing. This is why, the American workplace, has become so toxic. This is what pushes many Americans, over their limits. This is one of the many reasons, we have trouble keeping quality Law Enforcement.

 

Thanks for visiting my photostream. All content in my photostream; is free to download, copy, share and print. Please, leave my logos on them. Violence is not the answer, exposure is.

My client (I really made her stretch that neck!) and I. notice that only I stand "on" the furniture.

More about the room we are standing in here

 

First of the year for me. Taken at Sandy while I was looking for the hawfinch. It was worth getting cold and muddy knees for.

Average shot but it was blingin 👍

The San Francisco Seals were a minor league baseball team in San Francisco, California, that played in the Pacific Coast League from 1903 until 1957 before transferring to Phoenix, Arizona. They were named for the abundant California sea lion and harbor seal populations in the Bay Area. The 1909, 1922, 1925, and 1928 Seals were recognized as being among the 100 greatest minor league teams of all time.

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Harry Richard "Rube" Suter (b. September 15, 1887 in Independence, Missouri – d. July 24, 1971 at age 83 in Topeka, Kansas) was a professional baseball pitcher from 1906 to 1912. He played one season in Major League Baseball for the Chicago White Sox. Suter was 5 feet 10 inches (1.78 m) tall and weighed 190 pounds (86 kg). He started his baseball career in 1906 with the South Texas League's Austin Senators and had a win–loss record of 15–9. The following season, he was 23–13. Suter then joined the San Francisco Seals of the Pacific Coast League and became one of the top pitchers in the circuit. In 1908, pitching a league-leading 415 innings, he went 27–20 with a 2.00 earned run average. Suter's contract was purchased by the Chicago White Sox in August 1908. He was on the White Sox roster throughout 1909, and he made seven starts, relieved in 11 other games, and went 2–3 with a 2.47 ERA. His contract was then sold back to San Francisco after the season, and he never played in the majors again. Returning to his old club in 1910, Suter picked up where he left off, going 16–14 with a 1.95 ERA. The following season, his ERA rose to 2.67, but he struck out 339 batters to set a Seals team record. He also threw a no-hitter on April 25 to beat Oakland, 1–0. In 1912, Suter joined the Portland Beavers. He set a Pacific Coast League record on October 12, when he struck out 16 batters in a game against San Francisco. Suter pitched in 20 games that year and won only 5. His playing career ended after the season. In 1938, Suter was the manager of the Western Association's Salina Millers.

 

(Clipped from - The Topeka State Journal newspaper - Topeka, Kansas - 8 Jun 1905) - Sedalia has a new pitcher by the name of Harry Suter, son of George Suter of Fulton. He is a home-guard, but promises In great shape. He formerly pitched for the Westminster College team.

 

(Clipped from - The Topeka State Journal newspaper - Topeka, Kansas - 17 Jun 1905) - Sedalia - Harry Suter, the home guard kid phenom, who showed up so well in the box, refused to go along on the present trip. He only wants to play at home. In July he pitched for the Nevada Elks baseball team.

 

(Clipped from - The Sedalia Democrat newspaper - Sedalia, Missouri - 23 Feb 1906) - Sedalian Signed As Pitcher - Harry Suter, the young man who pitched such phenomenal ball for the Nevada Elks last summer, has signed with the Austin, Tex., ball team, says the Nevada Mall. Suter will make good in the Texas league, and If no accidents happen to him he will be In professional company before the passing of many seasons. He is a real “box-artist" of the strikeout order.

 

(Clipped from - The Sedalia Democrat newspaper - Sedalia, Missouri - 5 Nov 1906) - SEDALIA BALL PLAYER - Austin, He Will Likely Be Sold by Austin, Texas to St. Paul. Harry Suter, the plumber and baseball pitcher, who played last season with the Austin, Texas, baseball team in the Southern Texas league, is in receipt of a letter from W. P. Allen, secretary of the league, in which he states that Suter will very likely be sold to the St. Paul, Minn. American association club the coming season. (he ended up staying one more year with the Austin baseball team).

 

(Clipped from - The Morning Union newspaper - Grass Valley, California - 18 February 1908) - LONG SIGNS GOOD MAN FROM TEXAS - SAN FRANCISCO, Feb 17. - Danny Long announced today that he had all but signed Harry Suter, who helped to pitch Austin into the championship in the Texas League last year. Suter was drafted by Washington. When Long sold Street to Cantillon the understanding was that the latter should send him a player in addition to the money that was passed. Now if Washington can secure waivers on Suter he will be turned over to the Seals. "Suter is a left-handed pitcher", said Long, "and was one of the best men in the Texas League last year. His side-kicker, Bailey, was tried out by the St. Louis American Club last fail and made good, and from all accounts Suter is as good a man. I am told that he has a lot of speed and for a left-hander and is remarkably steady. We need a good southpaw and I look for Suter to fill the bill."

 

(Clipped from - The Sedalia Democrat newspaper - Sedalia, Missouri - 2 April 1908) - A SEDALIA BALL PLAYER WHO HAS MADE GOOD WITH THE SAN FRANCISCO TEAM IN COAST LEAGUE. HARRY SUTER IS A FIXTURE THERE - Washington Drafted Him From Texas, but Turned Him Adrift Without a Trial and Is Sure to Regret It. Harry Suter, son of George Suter, the plumber of this city, has made good with the San Francisco club of the Pacific Coast Baseball League. Suter has something up his sleeve that no other pitcher is working on. Suter’s new junk is the “knuckle ball.” it is a combination of the slow ball and the spitter. In making the delivery, Suter grasps the ball firmly of course, against the knuckles of the pitching hand. It is delivered with the same motion that sends the swift ball across the plate. And that is where the deception lies. While the swing is that of a fast ball the knuckle sphere is in reality a slow ball, it comes to the batter looming up as large as a balloon and then suddenly drops, just like the “saliva special.’

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T212 Obaks were to the West Coast what T206’s were to the rest of the country. While little of the players are known, their images endure...trade cards from the "Obak Baseball Players" series (T212), distributed by the California branch of the American Tobacco Company to promote their Obak Mouthpiece Cigarettes brand. The set was released in three separate subsets, one per year from 1909 through 1911.

 

While the players may not be well known to fans today—and most probably weren't to fans in the eastern half of the country even in 1910—the cards are appreciated for their stunning good looks. The artwork on these is sensational, transporting you back in time to a period when the game was beginning to grow up in California, Oregon and Washington, where these players toiled in hopes of getting noticed by a big league club in the east.

 

Link to - Obak Cards Were West Coast’s Version of T206 - www.sportscollectorsdaily.com/obak-cards-were-west-coasts...

 

All three Obak sets feature the same front design. The design has a brightly-colored lithograph of a player, surrounded by a white border. At the bottom are the player's last name and team city, and the specific league is added for the 1910 and '11 sets. Collectors can identify which year the card was issued by its back design. 1909 cards feature an Obak advertisement in Old English script. 1910 had the Obak wording in block type, along with a mention of either 150 or 175 subjects. There are a total of 35 different slogans available on the 1910 card backs. Finally, the 1911 cards are printed in red ink, with a biography of the player and a few lines of statistics. There are 426 total cards in the three sets.

 

Many 1909 Obaks were obviously hand-cut at the factory and were issued exactly in this manner; these cards are encapsulated as "Authentic" due to their very slight irregular cut but are definitely not trimmed. There were 10 horizontal cards issued in the 1909 set (Boyce, Brackenridge, Brown, Dillion, W. Hogan, Martinke, Mohler, Nelson, Reidy and Wiggs).

 

1911 Obak - The final year of production for the original Obak baseball card brand. The 1911 Obak Baseball set featured players from the six PCL teams and the four NWL teams. These teams included professional clubs from Spokane, Tacoma, Vancouver, Los Angeles, Oakland, Portland, Sacramento, San Francisco, Vernon, and Seattle. This year is noticeably different from the previous two years as the backs are printed in red ink and contain a bio and statistics. The stats are a first for minor league cards.

 

Link to - Finding 5 Gems In The T212 Obak Minor League Set - www.sportscollectorsdaily.com/t212-obak-set/

 

The OBAK (T212) cards were printed in San Francisco at the Schmidt Lithography Co. Judging from the 76-card

uncut sheet shown in Post #8, Schmidt Lithography used a 30-inch wide press track to print 19 cards across the

sheet.

 

Links to 1911 T212-3 Obak Cigarettes (179 cards) complete sheet (printed by the Schmidt lithography company in San Francisco, sold for $16,000) - www.mercurynews.com/wp-content/uploads/2016/11/cct-worth-...

 

sep10.hugginsandscott.com/cgi-bin/showitem.pl?itemid=25005

 

- link to the full write-up - sep10.hugginsandscott.com/cgi-bin/showitem.pl?itemid=25005

318 your average household gods are gleaming alluringly and twisting capriciously in this innocuous little white-roofed house p 40x50

 

Red-headed Cardinal Beetle. Taken at Wilstone Res, Tring.

Savage and Average in SL opt out 30/60 - Group Cover

 

Thank you so much for this honour! I am thrilled you saw my work as cover worthy for your group!

 

See it here: www.flickr.com/groups/14769191@N23/

 

++++++FROM WIKIPEDIA ++++

 

Puri (About this soundlisten (help·info)) is a city and a Municipality in the state of Odisha in eastern India. It is the district headquarters of Puri district and is situated on the Bay of Bengal, 60 kilometres (37 mi) south of the state capital of Bhubaneswar. It is also known as Sri Jagannatha Dhama after the 12th-century Jagannatha Temple located in the city. It is one of the original Char Dham pilgrimage sites for Hindus.

Puri

 

ପୁରୀ

 

Puri is known by several names since the ancient times, and was locally known as "Sri Kshetra" and Lord Jagannatha temple is known as "Badadeula". Puri and the Jagannatha Temple were invaded 18 times by Hindu and Muslim rulers, from the 4th century AD till the early 19th century with the objective of looting the treasures of the temple. Odisha, including Puri and its temple, were part of British India from 1803 till India attained independence in August 1947. Even though princely states do not exist in India today, the heirs of the Gajapati Dynasty of Khurda still perform the ritual duties of the temple. The temple town has many Hindu religious mathas or monasteries.

 

The economy of Puri is dependent on the religious importance of the Jagannatha Temple to the extent of nearly 80 percent. The 24 festivals, including 13 major ones, held every year in the temple complex contribute to the economy; Ratha Yatra and its related festivals are the most important which are attended by millions of people every year. Sand art and applique art are some of the important crafts of the city.

 

Puri has been chosen as one of the heritage cities for Heritage City Development and Augmentation Yojana (HRIDAY) scheme of Government of India.

Geography and climateEdit

GeographyEdit

The Atharanala Bridge dating back to the 16th century at the entrance of Puri

 

Puri, located on the east coast of India on the Bay of Bengal, is in the centre of the Puri district. It is delimited by the Bay of Bengal on the southeast, the Mauza Sipaurubilla on the west, Mauza Gopinathpur in the north and Mauza Balukhand in the east. It is within the 67 kilometres (42 mi) coastal stretch of sandy beaches that extends between Chilika Lake and the south of Puri city. However, the administrative jurisdiction of the Puri Municipality extends over an area of 16.3268 square kilometres (6.3038 sq mi) spread over 30 wards, which includes a shore line of 5 kilometres (3.1 mi).[1]

 

Puri is in the coastal delta of the Mahanadi River on the shores of the Bay of Bengal. In the ancient days it was near to Sisupalgarh (also known as "Ashokan Tosali"). Then the land was drained by a tributary of the Bhargavi River, a branch of the Mahanadi River. This branch underwent a meandering course creating many arteries altering the estuary, and formed many sand hills. These sand hills could be cut through by the streams. Because of the sand hills, the Bhargavi River, flowing to the south of Puri, moved away towards the Chilika Lake. This shift also resulted in the creation of two lagoons, known as Sar and Samang, on the eastern and northern parts of Puri respectively. Sar lagoon has a length of 5 miles (8.0 km) in an east-west direction and a width of 2 miles (3.2 km) in north-south direction. The estuary of the Bhargavi River has a shallow depth of just 5 feet (1.5 m) and the process of siltation continues. According to a 15th-century Odia writer Saraladasa, the bed of the unnamed stream that flowed at the base of the Blue Mountain or Neelachal was filled up. Katakarajavamsa, a 16th-century chronicle (c.1600), attributes filling up of the bed of the river which flowed through the present Grand Road, as done during the reign of King Narasimha II (1278–1308) of Eastern Ganga dynasty.[2]

ClimateEdit

 

According to the Köppen–Geiger climate classification system the climate of Puri is classified as Aw (Tropical savanna climate). The city has moderate and tropical climate. Humidity is fairly high throughout the year. The temperature during summer touches a maximum of 36 °C (97 °F) and during winter it is 17 °C (63 °F). The average annual rainfall is 1,337 millimetres (52.6 in) and the average annual temperature is 26.9 °C (80.4 °F). The weather data is given in the following table.[3][4]

 

HistoryEdit

Main article: Timeline of Puri

Names in historyEdit

 

Puri, the holy land of Lord Jagannatha, also known by the popular vernacular name Shrikhetra, has many ancient names in the Hindu scriptures such as the Rigveda, Matsya purana, Brahma Purana, Narada Purana, Padma Purana, Skanda Purana, Kapila Purana and Niladrimahodaya. In the Rigveda, in particular, it is mentioned as a place called Purushamandama-grama meaning the place where the Creator deity of the world – Supreme Divinity deified on an altar or mandapa was venerated near the coast and prayers offered with Vedic hymns. Over time the name got changed to Purushottama Puri and further shortened to Puri, and the Purusha came to be known as Jagannatha. Sages like Bhrigu, Atri and Markandeya had their hermitage close to this place.[5] Its name is mentioned, conforming to the deity worshipped, as Srikshetra, Purusottama Dhāma, Purusottama Kshetra, Purusottama Puri and Jagannath Puri. Puri, however, is the popular usage. It is also known by the geographical features of its location as Shankhakshetra (the layout of the town is in the form of a conch shell),[6] Neelāchala ("Blue mountain" a terminology used to name a very large sand lagoon over which the temple was built but this name is not in vogue), Neelāchalakshetra, Neelādri.[7] In Sanskrit, the word "Puri" means town or city,[8] and is cognate with polis in Greek.[9]

 

Another ancient name is Charita as identified by General Alexander Cunningham of the Archaeological Survey of India, which was later spelled as Che-li-ta-lo by Chinese traveller Hiuen Tsang. When the present temple was built by the Eastern Ganga king Anantavarman Chodaganga in the 11th and 12th centuries AD, it was called Purushottamkshetra. However, the Moghuls, the Marathas and early British rulers called it Purushottama-chhatar or just Chhatar. In Moghul ruler Akbar's Ain-i-Akbari and subsequent Muslim historical records it was known as Purushottama. In the Sanskrit drama Anargha Raghava Nataka as well, authored by Murari Mishra, a playwright, in the 8th century AD, it is referred to as Purushottama.[6] It was only after the 12th century AD that Puri came to be known by the shortened form of Jagannatha Puri, named after the deity or in a short form as Puri.[7] It is the only shrine in India, where Radha, along with Lakshmi, Saraswati, Durga, Bhudevi, Sati, Parvati, and Shakti, abodes with Krishna, who is also known by the name Jagannatha.[10]

Ancient periodEdit

king Indradyumna of Ujjayani credited with building the original temple in 318 AD

 

According to the chronicle Madala Panji, in 318 AD, the priests and servitors of the temple spirited away the idols to escape the wrath of the Rashtrakuta king Rakatavahu.[11] In the temple's historical records it finds mention in the Brahma Purana and Skanda Purana stating that the temple was built by the king Indradyumna, Ujjayani.[12]

 

S. N. Sadasivan, a historian, in his book A Social History of India quotes William Joseph Wilkins, author of the book Hindu Mythology, Vedic and Purānic as stating that in Puri, Buddhism was once a well established practice but later Buddhists were persecuted and Brahmanism became the order of the religious practice in the town; the Buddha deity is now worshipped by the Hindus as Jagannatha. It is also said by Wilkinson that some relics of Buddha were placed inside the idol of Jagannatha which the Brahmins claimed were the bones of Lord Krishna. Even during Maurya king Ashoka's reign in 240 BC, Kalinga was a Buddhist center and that a tribe known as Lohabahu (barbarians from outside Odisha) converted to Buddhism and built a temple with an idol of Buddha which is now worshipped as Jagannatha. Wilkinson also says that the Lohabahu deposited some Buddha relics in the precincts of the temple.[13]

 

Construction of the Jagannatha Temple started in 1136 AD and completed towards the latter part of the 12th century. The Eastern Ganga king Anangabhima III dedicated his kingdom to Lord Jagannatha, then known as the Purushottama-Jagannatha, and resolved that from then on he and his descendants would rule under "divine order as Jagannatha's sons and vassals". Even though princely states do not exist in India today, the heirs of the Gajapati dynasty of Khurda still perform the ritual duties of the temple; the king formally sweeps the road in front of the chariots before the start of the Ratha Yatra.[14]

Medieval and early modern periodsEdit

 

The history of Puri is on the same lines as that of the Jagannatha Temple, which was invaded 18 times during its history to plunder the treasures of the temple, rather than for religious reasons. The first invasion occurred in the 8th century AD by Rastrakuta king Govinda-III (798–814 AD), and the last took place in 1881 AD by the monotheistic followers of Alekh (Mahima Dharma) who did not recognise the worship of Jagannatha.[15] From 1205 AD onward [14] there were many invasions of the city and its temple by Muslims of Afghan and Moghul descent, known as Yavanas or foreigners. In most of these invasions the idols were taken to safe places by the priests and the servitors of the temple. Destruction of the temple was prevented by timely resistance or surrender by the kings of the region. However, the treasures of the temple were repeatedly looted.[16] The table lists all the 18 invasions along with the status of the three images of the temple, the triad of Jagannatha, Balabhadra and Subhadra following each invasion.[15]

Invasion number Invader (s), year (s) AD Local rulers Status of the three images of the Jagannatha temple

1 Raktabahu or Govinda III (798–814) of the Rashtrakuta Empire King Subhanadeva of Bhaumakara dynasty Idols shifted to Gopali near Sonepur. Was brought back to Puri by Yayati I after 146 years and re-consecrated after performing Nabakalebara.[17]

2 Illias Shah, Sultan of Bengal, 1340 Narasinghadeva III Images shifted to a secret location.[18]

3 Feroz Shah Tughlaq, 1360 Ganga King Bhanudeva III Images not found, though rumored that they were thrown into the Bay Of Bengal.[18]

4 Ismail Ghazi commander of Alauddin Hussain Shah of Bengal, 1509 King Prataprudradeva Images shifted to Chandhei Guha Pahada near Chilika Lake.[18]

5 Kalapahara, army assistant general of Sulaiman Karrani of the Afghan Sultan of Bengal, 1568 Mukundadeva Harichandan Images initially hidden in an island in Chilika Lake. However, the invader took the idols from here to the banks of the Ganges River and burnt them. Bisher Mohanty, a Vaishnavite saint, who had followed the invading army, retrieved the Brahmas and hid it in a drum at Khurdagada in 1575 AD and finally re-installed it in the deities. Deities were brought back to Puri and consecrated in the Jagannatha Temple.[19]

6 Suleman, the son of Kuthu Khan and Osman, the son of Isha (ruler of Orissa), 1592 Ramachandradeva, the Bhoi dynasty ruler of Khurda Revolt was by local Muslim rulers who desecrated the images.[20]

7 Mirza Khurum, the commander of Islam Khan I, the Nawab of Bengal, 1601 Purushottamadeva of Bhoi Dynasty Image moved to Kapileswarpur village by boat through the river Bhargavi and kept in the Panchamukhi Gosani temple. Thereafter, the deities were kept in Dobandha—Pentha.[20]

8 Hasim Khan, the Subedar of Orissa, 1608 Purushottam Deva, the King of Khurda Images shifted to the Gopal temple at Khurda and brought back in 1608.[20]

9 Hindu Rajput Jagirdar Kesodasmaru, 1610 Purusottamdeva, the king of Khurda Images kept at the Gundicha Temple and brought back to Puri after eight months.[20]

10 Kalyan Malla, 1611 Purushottamadeva, the King of Khurda Images moved to 'Mahisanasi' also known as'Brahmapura' or 'Chakanasi' in the Chilika Lake where they remained for one year.[21]

11 Kalyan Malla, 1612 Paiks of Purushottamadeva, the King of Khurda Images placed on a fleet of boats at Gurubai Gada and hidden under the 'Lotani Baragachha' or Banyan tree) and then at 'Dadhibaman Temple'.[22]

12 Mukarram Khan, 1617 Purushottama Deva, the King of Khurda Images moved to the Bankanidhi temple, Gobapadar and brought back to Puri in 1620.[22]

13 Mirza Ahmad Beg, 1621 Narasingha Deva Images shifted to 'Andharigada' in the mouth of the river Shalia across the Chilika Lake. Moved back to Puri in 1624.[23]

14 Amir Mutaquad Khan alias Mirza Makki, 1645 Narasingha Deva and Gangadhar Not known.[24]

15 Amir Fateh Khan, 1647 Not known Not known[24]

16 Ekram Khan and Mastram Khan on behalf of Mughal Emperor Aurangzeb, 1692 Divyasingha Deva, the king of Khurda Images moved to 'Maa Bhagabati Temple' and then to Bada Hantuada in Banpur across the Chilika Lake, and finally brought back to Puri in 1699.[24]

17 Muhammad Taqi Khan, 1731 and 1733 Birakishore Deva and Birakishore Deva of Athagada Images moved to Hariswar in Banpur, Chikili in Khalikote, Rumagarh in Kodala, Athagada in Ganjam and lastly to Marda in Kodala. Shifted back to Puri after 2.5 years.[24]

18 Followers of Mahima Dharma, 1881 Birakishore Deva and Birakishore Deva of Athagada Images burnt in the streets. [25]

 

Puri is the site of the Govardhana Matha, one of the four cardinal institutions established by Adi Shankaracharya, when he visited Puri in 810 AD, and since then it has become an important dham (divine centre) for the Hindus; the others being those at Sringeri, Dwarka and Jyotirmath. The Matha (monastery of various Hindu sects) is headed by Jagatguru Shankarachrya. It is a local belief about these dhams that Lord Vishnu takes his dinner at Puri, has his bath at Rameshwaram, spends the night at Dwarka and does penance at Badrinath.[12][26]

 

In the 16th century, Chaitanya Mahaprabhu of Bengal established the Bhakti movements of India, now known by the name the Hare Krishna movement. He spent many years as a devotee of Jagannatha at Puri; he is said to have merged with the deity.[27] There is also a matha of Chaitanya Mahaprabhu here known as Radhakanta Math.[12]

 

In the 17th century, for the sailors sailing on the east coast of India, the temple served as a landmark, being located in a plaza in the centre of the city, which they called the "White Pagoda" while the Konark Sun Temple, 60 kilometres (37 mi) away to the east of Puri, was known as the "Black Pagoda".[27]

 

The iconic representation of the images in the Jagannatha temple is believed to be the forms derived from the worship made by the tribal groups of Sabaras belonging to northern Odisha. These images are replaced at regular intervals as the wood deteriorates. This replacement is a special event carried out ritualistically by special group of carpenters.[27]

Govardhana matha main gate

 

The city has many other Mathas as well. The Emar Matha was founded by the Tamil Vaishnava saint Ramanujacharya in the 12th century AD. This Matha, which is now located in front of Simhadvara across the eastern corner of the Jagannatha Temple, is reported to have been built in the 16th century during the reign of kings of Suryavamsi Gajapatis. The Matha was in the news on 25 February 2011 for the large cache of 522 silver slabs unearthed from a closed chamber.[28][29]

 

The British conquered Orissa in 1803, and, recognising the importance of the Jagannatha Temple in the life of the people of the state, they initially appointed an official to look after the temple's affairs and later declared the temple as part of a district.[14]

Modern historyEdit

H.H Jagadguru Swami Nischalananda Saraswati, The Shankaracharya of Puri

 

In 1906, Sri Yukteswar, an exponent of Kriya Yoga and a resident of Puri, established an ashram, a spiritual training center, named "Kararashram" in Puri. He died on 9 March 1936 and his body is buried in the garden of the ashram.[30][31]

 

The city is the site of the former summer residence of British Raj, the Raj Bhavan, built in 1913–14 during the era of governors.[32]

 

For the people of Puri, Lord Jagannatha, visualized as Lord Krishna, is synonymous with their city. They believe that Lord Jagannatha looks after the welfare of the state. However, after the partial collapse of the Jagannatha Temple (in the Amalaka part of the temple) on 14 June 1990, people became apprehensive and considered it a bad omen for Odisha. The replacement of the fallen stone by another of the same size and weight (7 tonnes (7.7 tons)), that could be done only in the early morning hours after the temple gates were opened, was done on 28 February 1991.[27]

 

Puri has been chosen as one of the heritage cities for the Heritage City Development and Augmentation Yojana scheme of the Indian Government. It is chosen as one of the 12 heritage cities with "focus on holistic development" to be implemented within 27 months by the end of March 2017.[33]

 

Non-Hindus are not permitted to enter the shrines but are allowed to view the temple and the proceedings from the roof of the Raghunandan library, located within the precincts of the temple, for a small donation.[34]

DemographicsEdit

See also: List of cities in Odisha

 

According to the 2011 Census of India, Puri is an urban agglomeration governed by the Municipal Corporation in Odisha state, with a population of 201,026[35] This rose to 200,564 in 2011 – comprising 104,086 males, 96,478 females, and 18,471 children (under six years of age). The sex ratio is 927. The average literacy rate in the city is 88.03 percent (91.38 percent for males and 84.43 percent for females).

EconomyEdit

 

The economy of Puri is dependent on tourism to the extent of about 80 percent. The temple is the focal point of the city and provides employment to the people of the town. Agricultural production of rice, ghee, vegetables and so forth of the region meet the large requirements of the temple. Many settlements around the town exclusively cater to the other religious requirements of the temple.[36] The temple administration employs 6,000 men to perform the rituals. The temple also provides economic sustenance to 20,000 people.[34] According to Colleen Taylor Sen an author on food and travel, writing on the food culture of India, the temple kitchen has 400 cooks serving food to as many as 100,000 people,.[37] According to J Mohapatra, Director, Ind Barath Power Infra Ltd (IBPIL), the kitchen is known as "a largest and biggest kitchen of the world."[38]

City management and governanceEdit

Samudra arati or worship of the sea at Swargadwar by disciples of the Govardhana matha

 

The Puri Municipality, Puri Konark Development Authority, Public Health Engineering Organisation and Orissa Water Supply Sewerage Board are some of the principal organisations that are devolved with the responsibility of providing for civic amenities such as water supply, sewerage, waste management, street lighting and infrastructure of roads. The major activity, which puts maximum pressure on these organisations, is the annual event of the Ratha Yatra held during June- July. According to the Puri Municipality more than a million people attend this event. Hence, development activities such as infrastructure and amenities to the pilgrims, apart from security, gets priority attention.[39]

 

The civic administration of Puri is the responsibility of the Puri Municipality. The municipality came into existence in 1864 in the name of the Puri Improvement Trust, which was converted into Puri Municipality in 1881. After India's independence in 1947, the Orissa Municipal Act (1950) was promulgated entrusting the administration of the city to the Puri Municipality. This body is represented by elected representatives with a Chairperson and councilors representing the 30 wards within the municipal limits.[40]

LandmarksEdit

Jagannatha temple

Jagannatha Temple at PuriEdit

Main article: Jagannath Temple (Puri)

Left: Jagannath Temple at Puri Right: View of the temple at night

 

The Jagannatha Temple at Puri is one of the major Hindu temples built in the Kalinga style of architecture.[41] The temple tower, with a spire, rises to a height of 58 metres (190 ft), and a flag is unfurled above it, fixed over a wheel (chakra).[34][42]

Left:Ritual chakra and flags at the top shikhara of Puri temple of Jagannatha also related to Sudarsana chakra. The red flag (12 hand or 14 feet (4.3 m) denotes that Jagannath is within the temple.

Right: Statue of Aruna the charioteer of the Sun God on top of the Aruna Stambha in front of the Singhadwara

 

The temple is built on an elevated platform (of about 420,000 square feet (39,000 m2) area),[43] 20 feet (6.1 m) above the adjacent area. The temple rises to a height of 214 feet (65 m) above the road level. The temple complex covers an area of 10.7 acres (4.3 ha).[39] There are four entry gates in four cardinal directions of the temple, each gate located at the central part of the walls. These gates are: the eastern gate called the Singhadwara (Lions Gate), the southern gate known as Ashwa Dwara (Horse Gate), the western gate called the Vyaghra Dwara (Tigers Gate) or the Khanja Gate, and the northern gate called the Hathi Dwara or (elephant gate). These four gates symbolize the four fundamental principles of Dharma (right conduct), Jnana (knowledge), Vairagya (renunciation) and Aishwarya (prosperity). The gates are crowned with pyramid shaped structures. There is a stone pillar in front of the Singhadwara, called the Aruna Stambha {Solar Pillar}, 11 metres (36 ft) in height with 16 faces, made of chlorite stone; at the top of the stamba an elegant statue of Aruṇa (Sun) in a prayer mode is mounted. This pillar was shifted from the Konarak Sun Temple.[44] The four gates are decorated with guardian statues in the form of lion, horse mounted men, tigers, and elephants in the name and order of the gates.[34] A pillar made of fossilized wood is used for placing lamps as offering. The Lion Gate (Singhadwara) is the main gate to the temple, which is guarded by two guardian deities Jaya and Vijaya.[43][44][45] The main gate is ascended through 22 steps known as Baisi Pahaca, which are revered, as it is believed to possess "spiritual animation". Children are made to roll down these steps, from top to bottom, to bring them spiritual happiness. After entering the temple, on the left side, there is a large kitchen where food is prepared in hygienic conditions in huge quantities; the kitchen is called as "the biggest hotel of the world".[43]

The main entrance of the Jagannatha Temple

 

According to a legend King Indradyumma was directed by Lord Jagannatha in a dream to build a temple for him which he did as directed. However, according to historical records the temple was started some time during the 12th century by King Chodaganga of the Eastern Ganga dynasty. It was completed by his descendant, Anangabhima Deva, in the 12th century. The wooden images of Jagannatha, Balabhadra and Subhadra were then deified here. The temple was under the control of the Hindu rulers up to 1558. Then, when Orissa was occupied by the Afghan Nawab of Bengal, it was brought under the control of the Afghan General Kalapahad. Following the defeat of the Afghan king by Raja Mansingh, the General of Mughal emperor Akbar, the temple became part of the Mughal empire till 1751. Subsequently, it was under the control of the Marathas till 1803. During the British Raj, the Puri Raja was entrusted with its management until 1947.[42]

 

The triad of images in the temple are of Jagannatha, personifying Lord Krishna, Balabhadra, His older brother, and Subhadra, His younger sister. The images are made of neem wood in an unfinished form. The stumps of wood which form the images of the brothers have human arms, while that of Subhadra does not have any arms. The heads are large, painted and non-carved. The faces are marked with distinctive large circular eyes.[27]

The Pancha Tirtha of PuriEdit

Main article: Pancha Tirtha of Puri

Markandeshwar Tank

 

Hindus consider it essential to bathe in the Pancha Tirtha or the five sacred bathing spots of Puri, to complete a pilgrimage to Puri. The five sacred water bodies are the Indradyumana Tank, the Rohini Kunda, the Markandeya Tank, the Swetaganga Tank, and the Bay of Bengal also called the Mahodadhi, in Sanskrit 'Mahodadhi' means a "great ocean";[46] all are considered sacred bathing spots in the Swargadwar area.[47][48][49] These tanks have perennial sources of supply from rainfall and ground water.[50]

Gundicha TempleEdit

Main article: Gundicha Temple

The Main Gate of the Gundicha Temple

 

The Gundicha Temple, known as the Garden House of Jagannatha, stands in the centre of a beautiful garden, bounded by compound walls on all sides. It lies at a distance of about 3 kilometres (1.9 mi) to the northeast of the Jagannatha Temple. The two temples are located at the two ends of the Bada Danda (Grand Avenue), which is the pathway for the Ratha Yatra. According to a legend, Gundicha was the wife of King Indradyumna who originally built the Jagannatha temple.[51]

 

The temple is built using light-grey sandstone, and, architecturally, it exemplifies typical Kalinga temple architecture in the Deula style. The complex comprises four components: vimana (tower structure containing the sanctum), jagamohana (assembly hall), nata-mandapa (festival hall) and bhoga-mandapa (hall of offerings). There is also a kitchen connected by a small passage. The temple is set within a garden, and is known as "God's Summer Garden Retreat" or garden house of Jagannatha. The entire complex, including the garden, is surrounded by a wall which measures 430 by 320 feet (131 m × 98 m) with height of 20 feet (6.1 m).[52]

 

Except for the 9-day Ratha Yatra, when the triad images are worshipped in the Gundicha Temple, otherwise it remains unoccupied for the rest of the year. Tourists can visit the temple after paying an entry fee. Foreigners (generally prohibited entry in the main temple) are allowed inside this temple during this period.[53] The temple is under the Jagannatha Temple Administration, Puri, the governing body of the main temple. A small band of servitors maintain the temple.[52]

SwargadwarEdit

The Sea at Swargadwar of Puri

 

Swargadwar is the name given to the cremation ground or burning ghat which is located on the shores of the sea. Here thousands of dead bodies of Hindus brought from faraway places are cremated. It is a belief that the Chitanya Mahaparabhu disappeared from this Swargadwar about 500 years back.[54]

BeachEdit

Puri sea sunrise

Puri Sea Beach viewed from the light house

 

The beach at Puri, known as the "Ballighai beach, at the mouth of Nunai River, is 8 kilometres (5.0 mi) away from the town and is fringed by casurina trees.[12] It has golden yellow sand. Sunrise and sunset are pleasant scenic attractions here.[55] Waves break in at the beach which is long and wide.[27]

District museumEdit

 

The Puri district museum is located on the station road where the exhibits in display are the different types of garments worn by Lord Jagannatha, local sculptures, patachitra (traditional, cloth-based scroll painting), ancient Palm-leaf manuscripts, and local craft work.[56]

Raghunandana libraryEdit

 

Raghunandana Library is located in the Emara Matha complex (opposite Simhadwara or lion gate, the main entrance gate). The Jagannatha Aitihasika Gavesana Samiti (Jagannatha Historical Centre) is also located here. The library houses ancient palm leaf manuscripts on Jagannatha, His cult and the history of the city.[56]

Festivals of PuriEdit

Main article: List of festivals observed at Jagannatha Temple, Puri

The Grand Road near the Jagannatha Temple

 

Puri witnesses 24 festivals every year, of which 13 are major. The most important of these is the Ratha Yatra, or the car festival, held in the June–July, which is attended by more than 1 million people.[57]

Ratha Yatra at PuriEdit

Main article: Ratha-Yatra (Puri)

The Ratha Yatra in Puri in modern times showing the three chariots of the deities with the Temple in the background

 

The Jagannatha Temple triad are normally worshipped in the sanctum of the temple at Puri, but once during the month of Asadha (rainy season of Orissa, usually in June or July), they are brought out on the Bada Danda (main street of Puri) and taken over a distance of (3 kilometres (1.9 mi)) to the Shri Gundicha Temple[58] in huge chariots (ratha), allowing the public to have darśana (holy view). This festival is known as the Ratha Yatra, meaning the journey (yatra) of the chariots.[59] The yatra starts every year according to the Hindu calendar on the Asadha Sukla Dwitiya day, the second day of bright fortnight of Asadha (June–July).[60]

 

Historically, the ruling Ganga dynasty instituted the Ratha Yatra on the completion of the Jagannatha Temple around 1150 AD. This festival was one of those Hindu festivals that was reported to the Western world very early.[61] Friar Odoric, in his account of 1321, reported how the people put the "idols" on chariots, and the King, the Queen and all the people drew them from the "church" with song and music.[62][63]

 

The Rathas are huge wooden structures provided with large wheels, which are built anew every year and are pulled by the devotees. The chariot for Lord Jagannatha is about 45 feet (14 m) high and 35 square feet (3.3 m2) and takes about 2 months for its construction.[64] The chariot is mounted with 16 wheels, each of 7 feet (2.1 m) diameter. The carving in the front face of the chariot has four wooden horses drawn by Maruti. On its other three faces, the wooden carvings are of Rama, Surya and Vishnu. The chariot is known as Nandi Ghosha. The roof of the chariot is covered with yellow and red coloured cloth. The next chariot is of Balabhadra which is 44 feet (13 m) in height fitted with 14 wheels. The chariot is carved with Satyaki as the charioteer, roof covered in red and green coloured cloth, and the chariot is known as Taladhwaja. The carvings on this chariot include images of Narasimha and Rudra as Jagannatha's companions. The next chariot in the order is of Subhadra, which is 43 feet (13 m) in height supported on 12 wheels, roof covered in black and red colour cloth, and the chariot is known as Darpa Dalaan and the charioteer carved is Arjuna. Other images carved on the chariot are of Vana Durga, Tara Devi and Chandi Devi.[60][65] The artists and painters of Puri decorate the cars and paint flower petals and other designs on the wheels, the wood-carved charioteer and horses, and the inverted lotuses on the wall behind the throne.[59] The chariots of Jagannatha pulled during Ratha Yatra is the etymological origin of the English word Juggernaut.[66] The Ratha Yatra is also termed as the Shri Gundicha yatra and Ghosha yatra[60]

Pahandi bije during Ratha Yatra at Puri

Chhera PaharaEdit

 

The Chhera Pahara (sweeping with water) is a significant ritual associated with the Ratha Yatra. During this ritual, the Gajapati King wears the outfit of a sweeper and sweeps all around the deities and chariots. The king cleans the road in front of the chariots with a gold-handled broom and sprinkles sandalwood water and powder. As per the custom, although the Gajapati King has been considered the most exalted person in the Kalingan kingdom, he still renders the menial service to Jagannatha. This ritual signifies that under the lordship of Jagannatha, there is no distinction between the powerful sovereign and the humblest devotee.[67]

Chandan YatraEdit

The Narendra Tirtha tank where ceremonies of Chandan Yatra are performed

Main article: Chandan Yatra

 

The Chandan Yatra festival held every year on Akshaya Tritiya day marks the commencement of the construction of the chariots of the Ratha Yatra. It also marks the celebration of the Hindu new year.[12]

Snana YatraEdit

Main article: Snana Yatra

 

Every year, on the Purnima day in the Hindu calendar month of Jyestha (June), the triad images of the Jagannatha Temple are ceremonially bathed and decorated on the occasion of Snana Yatra. Water for the bath is taken in 108 pots from the Suna kuan (meaning: "golden well") located near the northern gate of the temple. Water is drawn from this well only once in a year for the sole purpose of the religious bath of the deities. After the bath the triad images are dressed in the fashion of the elephant god, Ganesha. Later, during the night, the original triad images are taken out in a procession back to the main temple but kept at a place known as Anasara pindi.[60] After this the Jhulana Yatra is performed when proxy images of the deities are taken out in a grand procession for 21 days, cruised over boats in the Narendra Tirtha tank.[12]

Anavasara or AnasaraEdit

Images during the Snana Yatra.

 

Anasara, a derivative of the Sanskrit word "Anabasara",[68] literally means vacation. Every year after the holy Snana Yatra, the triad images, without the Sudarshana Chakra, are taken to a secret altar named Anavasara Ghar (also known as Anasara pindi, 'pindi' is Oriya term meaning "platform" [68]) where they remain for the next fortnight of (Krishna paksha); devotees are not allowed to view these images. Instead, devotees go to the nearby Brahmagiri to see the Lord in the four-handed form of Alarnath, a depiction of Vishnu.[60][69] Devotees then get the first glimpse of the Lord only on the day before Ratha Yatra, which is called Navayouvana. It is a local belief that the gods suffer from fever after taking an elaborate ritual bath, and they are treated by the special servants, the Daitapatis, for 15 days. Daitapatis perform special nitis (rites) known as Netrotchhaba (a rite of painting the eyes of the triad). During this period cooked food is not offered to the deities.[70]

Naba KalebaraEdit

Main articles: Nabakalevara and Nabakalebara 2015

 

Naba Kalebara is one of the most grand events associated with the Lord Jagannatha that takes place when one lunar month of Ashadha is followed by another of Ashadha called Adhika Masa (extra month). This can take place at an interval of 8, 12 or even 18 years. Literally meaning the "New Body" (Nava = New, Kalevar = Body) in Odia, the festival is witnessed by millions of people and the budget for this event generally exceeds $500,000. The event involves installation of new images in the temple and burial of the old ones in the temple premises at Koili Vaikuntha. During the Nabakalebara ceremony held during July 2015 the idols that were installed in the temple in 1996 were replaced by specially carved new images made of neem wood.[71][72] More than 3 million people are reported to have attended this festival.[73]

Suna BeshaEdit

Main article: Suna Besha

Suna Besha or Golden Attire of Lord Jagannatha

 

Suna Besha, ('Suna besh'in English translates to "gold dressing”[74]) also known as Raja or Rajadhiraja Bhesha [75] or Raja Bhesha, is an event when the triad images of the Jagannatha Temple are adorned with gold jewelry. This event is observed five times in a year. It is commonly observed on Magha Purnima (January), Bahuda Ekadashi also known as Asadha Ekadashi (July), Dashahara (Bijayadashami) (October), Karthik Purnima (November), and Pousa Purnima (December).[76][77] One such Suna Bhesha event is observed on Bahuda Ekadashi during the Ratha Yatra on the chariots placed at the Simhadwar. The other four Beshas are observed inside the temple on the Ratna Singhasana (gem studded altar). On this occasion gold plates are decorated over the hands and feet of Jagannatha and Balabhadra; Jagannatha is also adorned with a Chakra (disc) made of gold on the right hand while a silver conch adorns the left hand. Balabhadra is decorated with a plough made of gold on the left hand while a golden mace adorns his right hand.[76]

Niladri BijeEdit

 

Niladri Bije, celebrated in the Hindu calendar month Asadha (June–July) on Trayodashi (13th day),[78] marks the end of the Ratha Yatra. The large wooden images of the triad of gods are taken out from the chariots and then carried to the sanctum sanctorum, swaying rhythmically; a ritual which is known as pahandi.[72]

Sahi yatraEdit

A scene from a play being enacted during the Sahi Yatra

 

The Sahi Yatra, considered the world's biggest open-air theatre,[79] is an annual event lasting 11 days; a traditional cultural theatre festival or folk drama which begins on Ram Navami and ends on Rama avishke (Sanskrit meaning : anointing). The festival includes plays depicting various scenes from the Ramayana. The residents of various localities, or Sahis, are entrusted the task of performing the drama at the street corners.[80]

Samudra AratiEdit

Samudra arati of worship of the sea by disciples of the Matha at Puri

 

The Samudra arati is a daily tradition started by the present Shankaracharya 9 years ago.[81] The daily practise includes prayer and fire offering to the sea at Swargadwar in Puri by disciples of the Govardhan Matha. On Paush Purnima of every year the Shankaracharya himself comes out to offer prayers to the sea.

TransportEdit

 

Earlier, when roads did not exist, people used to walk or travel by animal-drawn vehicles or carriages along beaten tracks to reach Puri. Travel was by riverine craft along the Ganges up to Calcutta, and then on foot or by carriages. It was only during the Maratha rule that the popular Jagannath Sadak (Road) was built around 1790. The East India Company laid the rail track from Calcutta to Puri, which became operational in 1898.[82] Puri is now well-connected by rail, road and air services. A broad gauge railway line of the South Eastern Railways which connects Puri with Calcutta, and Khurda is an important railway junction on this route. The rail distance is about 499 kilometres (310 mi) from Calcutta[83] and 468 kilometres (291 mi) from Vishakhapatnam. Road network includes NH 203 that links the city with Bhubaneswar, the state capital, situated about 60 kilometres (37 mi) away. NH 203 B connects the city with Satapada via Brahmagiri. Marine drive, which is part of NH 203 A, connects Puri with Konark. The nearest airport is the Biju Patnaik International Airport at Bhubaneswar.[57] Puri railway station is among the top hundred booking stations of the Indian Railways.[84]

Arts and craftsEdit

Sand artEdit

Sand art of a Baby Elephant

 

Sand art is a special art form that is created on the beaches of Puri. The art form is attributed to Balaram Das, a poet who lived in the 14th century. Sculptures of various gods and famous people are now created in sand by amateur artists. These are temporary in nature as they get washed away by waves. This art form has gained international fame in recent years. One of the famed sand artists of Odisha is Sudarshan Patnaik. He established the Golden Sand Art Institute in 1995, in the open air on the shores of Bay of Bengal, to provide training to students interested in this art form.[85][80]

Appliqué artEdit

An applique art work

 

Appliqué art, which is a stitching-based craft unlike embroidery, was pioneered by Hatta Maharana of Pipili. It is widely used in Puri, both for decoration of the deities and for sale. Maharana's family members are employed as darjis or tailors or sebaks by the Maharaja of Puri. They prepare articles for decorating the deities in the temple for various festivals and religious ceremonies. The appliqué works are brightly coloured and patterned fabric in the form of canopies, umbrellas, drapery, carry bags, flags, coverings of dummy horses and cows, and other household textiles; these are marketed in Puri. The cloth used is made in dark colours of red, black, yellow, green, blue and turquoise blue.[86]

CultureEdit

Odissi dancer

 

Cultural activities, including the annual religious festivals, in Puri are: The Puri Beach Festival held from 5 to 9 November every year, and the Shreekshetra Utsav held from 20 December to 2 January every year. The cultural programmes include unique sand art, display of local and traditional handicrafts and food festival.[87] In addition, cultural programmes are held for two hours on every second Saturday of the month at the district Collector's Conference Hall near Sea Beach Police Station. Odissi dance, Odissi music and folk dances are part of this event.[87] Odissi dance is the cultural heritage of Puri. This dance form originated in Puri from the dances performed by Devadasis (Maharis) attached to the Jagannatha Temple who performed dances in the Nata mandapa of the temple to please the deities. Though the devadasi practice has been discontinued, the dance form has become modern and classical and is widely popular; many of the Odissi virtuoso artists and gurus (teachers) are from Puri.[88] Some of the famous Odissi dancers are Kelucharan Mohapatra, Mayadhar Raut, Sonal Mansingh, Sanjukta Panigrahi and many more

EducationEdit

Samanta Chandra Sekhar College, Puri

 

Some of the educational institutions in Puri are:

 

Ghanashyama Hemalata Institute of Technology and Management

Gangadhar Mohapatra Law College, established in 1981[89]

Extension Unit of Regional Research Institute of Homoeopathy, Puri, under Central Council for Research in Homoeopathy (CCRH), New Delhi; established in March 2006 [90]

Shri Jagannath Sanskrit University, established in July 1981[91]

Gopabandhu Ayurveda Mahavidyalaya, a college and hospital where treatment and training is based on Ayurveda school of medicine [92]

The Industrial Training Institute, a premier technical institution to provide education to skilled, committed & talented technicians was established in 1966 by the Government of India[93]

Blessed Sacrament High School established in 1952 is otherwise known as Puri convent. It is one of the best schools in the city. The school features classes 1 to 10. It is located in VIP Road, Puri.

 

Puri peopleEdit

 

Jayee Rajguru - Freedom fighter

Chakhi Khuntia (Chandan Hajuri) – Freedom fighter [94]

Utkalmani Pandit Gopabandhu Das – Social worker

Pandit Nilakantha Das – Social activist

Bhaktakabi Madhusudan Rao – Odia Poet

Padma Vibhushan Kelucharan Mohapatra – Odissi dancer

Padma Shri Pankaj Charan Das – Odissi dancer

Padma Shri Pandit Sadashiv Rathasharma – Scholar and Preacher of Shri Jagannatha Culture

Padma Vibhushan Raghunath Mohapatra – Architect and sculptor

Padma Shri Sudarshan Pattnaik – Sand Artist

Baisali Mohanty - ALC Global Fellow at University of Oxford, United Kingdom

Rituraj Mohanty – Singer