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51-621: Horseshoe Canyon , formerly known as Barrier Canyon , is in a remote area west of the Green River and north of the Canyonlands National Park Maze District in Utah , United States. It is known for its collection of Barrier Canyon Style (BCS) rock art, including both pictographs and petroglyphs , which was first recognized as a unique style here. A portion of Horseshoe Canyon containing The Great Gallery

102-595: A larger deposit of oil shale in the Green River formation. The Equity Oil Company currently has 17 wells in declining production of oil near Ashley Field and is looking to inject carbon dioxide into the Weber reservoir to increase the rate of oil flow through their pipelines. At the time of its discovery (2005), the Green River Formation was said to have the world's largest fossil fuel deposits in

153-576: A nomadic group of hunter-gatherers predating the Fremont and Ancestral Puebloans. The panel itself measures about 200 feet (61 m) long and 15 feet (4.6 m) high. The panel contains about 20 life-sized anthropomorphic images, the largest of which measures over 7 feet (2.1 m) tall. A Works Projects Administration produced reproduction of the paintings is located at the Natural History Museum of Utah . The Holy Ghost panel of

204-613: A panic caused by the Meeker Massacre in Colorado. Most of the land in the valley of the river today is owned and controlled by the federal government. Private holdings are largely limited to bottoms. Until the 1940s, the valley's economy was based largely on ranching. Tourism has emerged as the dominant industry in the region in the last several decades. A proposed nuclear power plant, the Blue Castle Project ,

255-625: A tributary of the Colorado River came about mainly for political reasons. In earlier nomenclature, the Colorado River began at its confluence with the Green River. Above the confluence, Colorado was called the Grand River. In 1921, U.S. Representative Edward T. Taylor of Colorado petitioned the Congressional Committee on Interstate and Foreign Commerce to rename the Grand River as the Colorado River. On July 25, 1921,

306-460: A wintering ground for American trappers in the next decades, with trading posts established at the mouth of the White near Whiterocks, Utah , and Browns Park . The Upper Green River Rendezvous Site near Pinedale, Wyoming was a popular location for annual mountain man rendezvous during the 1820s and 1830s, with as many as 450 to 500 trappers attending during its heyday in the 1830s. The region

357-579: Is actually 1 km wider than the Grand Canyon, making it the widest canyon in the world. Some canyons have notable cultural significance. Evidence of archaic humans has been discovered in Africa's Olduvai Gorge . In the southwestern United States, canyons are important archeologically because of the many cliff-dwellings built in such areas, largely by the ancient Pueblo people who were their first inhabitants. The following list contains only

408-650: Is joined by the Duchesne River , and three miles (5 km) farther downstream by the White River . Ten miles farther downstream, it is joined by the Willow River . South of the plateau, it is joined by Nine Mile Creek , then enters the Roan Cliffs where it flows south through the back-to-back Desolation and Gray canyons, with a combined length of 120 mi (192 km). In Gray Canyon, it

459-585: Is joined by the Price River . South of the canyon, it passes the town of Green River, Utah and is joined by the San Rafael River in southern Emery County . In eastern Wayne County it meanders through Canyonlands National Park , where it joins Colorado. The Flaming Gorge Dam in Utah is a significant regional source of water for irrigation and mining, as well as for hydroelectric power. Begun in

510-1095: Is less expensive for the production of soda ash in the United States than the synthetic Solvay process , which predominates in the rest of the world. The area has been mined for uranium . Canyon A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains , the Alps , the Himalayas or the Andes . Usually, a river or stream carves out such splits between mountains. Examples of mountain-type canyons are Provo Canyon in Utah or Yosemite Valley in California's Sierra Nevada . Canyons within mountains, or gorges that have an opening on only one side, are called box canyons. Slot canyons are very narrow canyons that often have smooth walls. Steep-sided valleys in

561-557: Is navigable by small craft throughout its course and by large motorboats upstream to Flaming Gorge Dam. Near the areas where the Oregon Trail crosses the river, it is 400 to 500 feet (120 to 150 m) wide and averages about 20 feet (6.1 m) deep at normal flow. Archaeological evidence indicates that the tributary canyons and sheltered areas in the river valley were home to the Fremont Culture , which flourished from

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612-767: Is now known as Sevier Lake . Later cartographers extended the error, representing the Buenaventura River as flowing into the Pacific Ocean . At least one charted the Buenaventura as draining the Great Salt Lake . Later, Spanish and Mexican explorers adopted the name Rio Verde, meaning "Green River" in Spanish . Exactly when the Spanish started using this name and why is unknown. Explanations of

663-676: Is occasionally used in the United Kingdom . In South Africa, kloof (in Krantzkloof Nature Reserve ) is used along with canyon (as in Blyde River Canyon ) and gorge (in Oribi Gorge ). Most canyons were formed by a process of long-time erosion from a plateau or table-land level. The cliffs form because harder rock strata that are resistant to erosion and weathering remain exposed on

714-474: Is part of a detached unit of Canyonlands National Park . The Horseshoe Canyon Unit was added to the park in 1971 in an attempt to preserve and protect the rock art found along much of its length. Human presence in Horseshoe Canyon has been dated as far back as 9000-7000 B.C., when Paleo-Indians hunted large mammals such as mastodons and mammoths across the southwest. Later inhabitants included

765-497: Is set to begin construction near Green River in 2023. The plant will use 53,500 acre-feet (66,000,000 m ) of water annually from the Green River once both reactors are commissioned. The La Barge oil field was discovered in 1924. Oil was produced from Tertiary sandstones ( Wasatch Formation and Green River Formation ), within an anticline 600 to 1200 feet deep. The Big Piney -La Barge complex has produced gas since 1956 and oil since 1960. Cumulative production by 1976

816-599: Is similarly imprecise, especially if one includes mountain canyons, as well as canyons cut through relatively flat plateaus (which have a somewhat well-defined rim elevation). The Yarlung Tsangpo Grand Canyon (or Tsangpo Canyon), along the Yarlung Tsangpo River in Tibet , is regarded by some as the deepest canyon on Earth at 5,500 metres (18,000 ft). It is slightly longer than the Grand Canyon in

867-598: Is soluble to a certain extent, cave systems form in the rock. When a cave system collapses, a canyon is left, as in the Mendip Hills in Somerset and Yorkshire Dales in Yorkshire , England. A box canyon is a small canyon that is generally shorter and narrower than a river canyon, with steep walls on three sides, allowing access and egress only through the mouth of the canyon. Box canyons were frequently used in

918-644: Is the Fish River Canyon in Namibia . In August 2013, the discovery of Greenland 's Grand Canyon was reported, based on the analysis of data from Operation IceBridge . It is located under an ice sheet. At 750 kilometres (470 mi) long, it is believed to be the longest canyon in the world. Despite not being quite as deep or long as the Grand Canyon, the Capertee Valley in Australia

969-688: Is the subject of the song "Green River" by C.W. McCall . The headwaters of the Green River is in western Wyoming, in northern Sublette County , on the western side of the Continental Divide in the Wind River Range and the Bridger–Teton National Forest . It flows south through Sublette County and western Wyoming in an area known as the Upper Green River Valley, then southwest and is joined by

1020-618: The Big Sandy River in western Sweetwater County . At the town of La Barge, it flows into Fontenelle Reservoir , formed by Fontenelle Dam. Below the dam, it flows through open sage-covered rolling prairie where it is crossed by the Oregon , California and Mormon emigration trails, and then further south past the town of Green River, Wyoming and into the Flaming Gorge Reservoir in southwestern Wyoming, formed by

1071-941: The Canyon of the Lodore (otherwise known as the Gates of Lodore) and is joined by the Yampa River at Steamboat Rock . It turns westward back into Utah along the southern edge of the Uintas in Whirlpool Canyon . In Utah, it meanders southwest across the Yampa Plateau and through the Uintah and Ouray Indian Reservation and the Ouray National Wildlife Refuge . Two miles south of Ouray, Utah , it

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1122-722: The Flaming Gorge Dam in northeastern Utah. Before the reservoir's creation, the Blacks Fork joined the Green River south of the town of Green River, but today the mouth of Blacks Fork is submerged by the reservoir. South of the dam, it is forced to turn sharply eastward by the uplift of the Uinta Mountains , looping around the eastern tip of the range as it travels from Utah into northwestern Colorado and through Browns Park before turning west and then south into Dinosaur National Monument , where it passes through

1173-477: The Oregon , California , and Mormon emigration trails. Nearly all primary emigration routes had to cross the Green River. The main trail crossed near where the Big Sandy River joins the Green River in Wyoming. The river is too big and much too deep to ford at any time of the year and is the largest, most dangerous river crossed by the Oregon Trail. For that reason, ferries were commonly run on this stretch of

1224-461: The United States , place names generally use canyon in the southwest (due to their proximity to Spanish-speaking Mexico ) and gorge in the northeast (which is closer to French Canada ), with the rest of the country graduating between these two according to geography. In Canada , a gorge is usually narrow while a ravine is more open and often wooded. The military-derived word defile

1275-642: The seabed of the continental slope are referred to as submarine canyons . Unlike canyons on land, submarine canyons are thought to be formed by turbidity currents and landslides . The word canyon is Spanish in origin ( cañón , pronounced [kaˈɲon] ), with the same meaning. The word canyon is generally used in North America , while the words gorge and ravine (French in origin) are used in Europe and Oceania , though gorge and ravine are also used in some parts of North America. In

1326-460: The western United States as convenient corrals, with their entrances fenced. The definition of "largest canyon" is imprecise, because a canyon can be large by its depth, its length, or the total area of the canyon system. Also, the inaccessibility of the major canyons in the Himalaya contributes to their not being regarded as candidates for the biggest canyon. The definition of "deepest canyon"

1377-618: The 1950s and finished in 1963, it was highly controversial and opposed by conservationists. Originally, a dam was to be built in Whirlpool Canyon, but the conservationist movement traded the Flaming Gorge Dam for halting that proposal. The Green is a large, deep, powerful river. It ranges from 100 to 300 feet (30 to 100 m) wide in the upper course and from 300 to 1,500 feet (91 to 457 m) wide in its lower course, and from 3 to 50 feet (0.91 to 15.24 m) in depth. It

1428-524: The 7th century to the 13th century. The Fremont were semi-nomadic people who lived in pithouses and are best known for the rock art on canyon walls and in sheltered overhangs. In later centuries, the river basin was home to the Shoshone and Ute peoples, both nomadic hunters. The Shoshone inhabited the river valley north of the Uinta Mountains , whereas the Utes lived to the south. The current reservation of

1479-585: The Desert Archaic culture, the Fremont culture , and Ancestral Puebloans . Occupation by the Fremont and Ancestral Puebloans was relatively brief; it is believed that the canyon was abandoned by Native American peoples by 1300 A.D. The Great Gallery is one of the largest and best preserved collections of Barrier Canyon Style rock art. The gallery was a product of the Desert Archaic culture,

1530-589: The Great Gallery has been dated to between 400 A.D. and 1100 A.D. by dating two rockfall events of which one exposed the rock face the panel on which it was made and the second damaging part of the panel. The Horseshoe Canyon trailhead is located on the west rim of the canyon. It can be accessed from State Route 24 via 30 miles (48 km) of graded dirt road, or from Green River via 47 miles (76 km) of dirt road. Both routes include segments of road that may become impassable when wet. Visitors may camp at

1581-531: The Great Gallery is roughly 6.5 miles (10.5 km) round trip, and requires 3 to 6 hours to complete. The trail is fairly well marked, but reaching the Great Gallery requires a certain amount of stamina and endurance, particularly in the heat. Three other significant panels of rock art are passed en route to the Great Gallery. 38°27′15″N 110°12′32″W  /  38.45417°N 110.20889°W  / 38.45417; -110.20889 Green River (Colorado River tributary) The Green River , located in

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1632-574: The Native Americans). A map of 1847 redirects the course of the Rafael to the north and labels it as Green River. It would be some time before the true confluence of the Green and Colorado Rivers would be known. The Old Spanish Trail from New Mexico to California crossed the river just above the present-day town of Green River, Utah. In the early 19th century, the upper river in Wyoming

1683-533: The United States, with an average depth of 1,600 metres (5,200 ft) and a volume of 4.17 trillion cubic metres (147 trillion cubic feet), is one of the world's largest canyons. It was among the 28 finalists of the New 7 Wonders of Nature worldwide poll. (Some referred to it as one of the seven natural wonders of the world .) The largest canyon in Europe is Tara River Canyon . The largest canyon in Africa

1734-627: The United States. Others consider the Kali Gandaki Gorge in midwest Nepal to be the deepest canyon, with a 6,400-metre (21,000 ft) difference between the level of the river and the peaks surrounding it. Vying for the deepest canyon in the Americas is the Cotahuasi Canyon and Colca Canyon , in southern Peru. Both have been measured at over 3,500 metres (11,500 ft) deep. The Grand Canyon of northern Arizona in

1785-670: The Utes is in the Uintah Basin . The Shoshone called the river the Seeds-kee-dee-Agie , meaning "Prairie Hen River." In 1776, the Spanish friars Silvestre Vélez de Escalante and Francisco Atanasio Domínguez crossed the river near present-day Jensen, naming it the Rio de San Buenaventura . The map-maker of the expedition, Captain Bernardo Miera y Pacheco , erroneously indicated that the river flowed southwest to what

1836-746: The canyon walls, in a process known as frost wedging. Canyon walls are often formed of resistant sandstones or granite . Sometimes large rivers run through canyons as the result of gradual geological uplift. These are called entrenched rivers , because they are unable to easily alter their course. In the United States, the Colorado River in the Southwest and the Snake River in the Northwest are two examples of tectonic uplift . Canyons often form in areas of limestone rock. As limestone

1887-462: The canyons, geographic features, and rapids along the river. For example, "we sweep around another great bend to the left, making a circuit of nine miles, and come back to a point within 600 feet of the beginning of the bend. In the two circuits, we describe almost in figure 8. The men call it a `bowknot' of a river; so we name it Bowknot Bend ." (Powell, 1869) From the 1840s through the 1860s, hundreds of thousands of emigrants made their way west along

1938-543: The form of a solid rock resource called oil shale . There is estimated to be between 500 billion and 1.1 trillion barrels (80 and 175 km ) of potentially recoverable oil in the basin, however; this estimated amount of recoverable oil in the form of kerogen is challenged, and in doubt, as currently there is no economically feasible technology to convert rock into a permeable oil. Kerogen is an uncooked form of hydrocarbon that nature did not convert into actual oil. The cost of converting Green River oil shale into actual oil at

1989-446: The moment would be higher than what it could be sold for. The EROI for oil shale is very low while having a very high destructive environmental impact. The Green River Basin contains the world's largest known deposit of trona ore near Green River, Wyoming. Soda ash mining from trona veins 900 and 1600 feet (300 and 500 m) deep is a major industrial activity in the area, employing over 2000 persons at four mines. The mining operation

2040-426: The name "Green" include ideas about the color of the water (though it is usually just as red as that of the Colorado), the color of soapstone along its banks, the color of the vegetation, and the name of a trapper. No explanation can be verified. Wilson Hunt of John Jacob Astor 's Pacific Fur Company called it The Spanish River in 1811. By that time it was clear to the trappers that Miera's map (if they had seen it)

2091-400: The name change was made official in House Joint Resolution 460 of the 66th Congress , over the objections of representatives from Wyoming and Utah and the United States Geological Survey , which noted that the drainage basin of the Green River was more extensive than that of the Grand River, although the Grand carried a higher volume of water at its confluence with the Green. The Green River

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2142-441: The river. Some popular ferries included the Lombard and Robinson ferries at the main crossing and the Mormon, Mountain Man, and Names Hill ferries where the popular Sublette-Greenwood cutoff crossed the river further upstream. In 1878 the first permanent settlement in the river valley was founded at Vernal by a party of Mormons led by Jeremiah Hatch . The settlement survived a diphtheria epidemic its first winter, as well as

2193-402: The route traverses the arid Colorado Plateau , where the river has carved some of the most spectacular canyons in the United States. The Green is slightly smaller than Colorado when the two rivers merge but typically carries a larger load of silt . The average yearly mean flow of the river at Green River, Utah is 6,121 cubic feet (173.3 m ) per second. The status of the Green River as

2244-426: The trappers and American explorers. While it was known that the Green River drained to Colorado, the exact course was not known. Miera's map showed the Colorado River branching into two major streams – the Nabajoo (San Juan) and the Zaguananas. It also showed the Zaguananas branching into four heads, including the Dolores and the Rafael (the latter of which Escalante's journal equates with Colorado per information from

2295-456: The valley walls. Canyons are much more common in arid areas than in wet areas because physical weathering has a more localized effect in arid zones. The wind and water from the river combine to erode and cut away less resistant materials such as shales . The freezing and expansion of water also serves to help form canyons. Water seeps into cracks between the rocks and freezes, pushing the rocks apart and eventually causing large chunks to break off

2346-413: The west rim trailhead, on public land managed by the Bureau of Land Management , or BLM. A vault toilet is provided but there is no water available. Overnight camping is not permitted in Horseshoe Canyon inside the Park boundaries. To see the rock art, visitors must descend 750 vertical feet (228 m) to the canyon bottom and hike approximately 3 miles (4.8 km). The hike from the West Rim trailhead to

2397-454: The western United States, is the chief tributary of the Colorado River . The watershed of the river, known as the Green River Basin , covers parts of the U.S. states of Wyoming , Utah , and Colorado . The Green River is 730 miles (1,170 km) long, beginning in the Wind River Mountains of Wyoming and flowing through Wyoming and Utah for most of its course, except for a short segment of 40 miles (64 km) in western Colorado. Much of

2448-400: Was 65 million bbl of oil and over 1.2 Tcf (trillion cubic feet ) of gas. Production includes the Cretaceous Mesaverde Formation and Frontier Formation . The discovery of petroleum at the Ashley Field after World War II has led to the exploitation of oil and natural gas in the region. The oil at Ashley Field is trapped in Aeolin deposits of "coversands and loess," while there is

2499-415: Was explored by John C. Fremont on several of his expeditions in the 1840s. Fremont corrected the cartographic error of Miera, establishing firmly that the river did not drain the Great Salt Lake. In 1869, the river was surveyed and mapped by John Wesley Powell as part of the first of his two expeditions to the region. During his two voyages in 1869 and 1871, he and his men gave most of the current names of

2550-405: Was part of the disputed Oregon Country . It was explored by trappers from the North West Company and Hudson's Bay Company , such as Donald Mackenzie who pioneered the area from 1819. In 1825, the American William Ashley and a party of American explorers floated down the river from north of the Uintah Mountains to the mouth of the White River . The valley of the river became increasingly used as

2601-461: Was wrong, for they had learned from the Native Americans that the Green River drained to the Colorado River and the Gulf of California . When Jedediah Smith reached the lower Colorado in 1826, he first called it the Seedskeedee, as the Green/Colorado River was commonly known among the trappers. By the time of Bonneville's expedition in 1832, the names "Seeds-kee-dee", "Spanish River", "Green River", and even "Colorado River" were used interchangeably by

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