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50-398: The western area of Malheur Lake consists of ponds separated by small islands and peninsulas. The lake's central and eastern sections are more open. The generally shallow water is suitable habitat for migratory birds, waterfowl, and aquatic plants. As is typical of Great Basin lakes, Malheur Lake's surface area changes dramatically with the local weather, climate, and season because the lake

100-528: A couple inches deep. This is the greatest evaporation potential in the United States, meaning that a 12 ft (3.8 m) lake could dry up in a single year. When the basin is flooded, some of the salt is dissolved; it is redeposited as clean crystals when the water evaporates. A popular site for tourists is the sign marking "sea level" on the cliff above the Badwater Basin. Similar to Owens Lake , it

150-678: A language in the Numic language group. To close a 1951 Indian Claims Commission case, the Western Shoshone Claims Distribution Act of 2004 established the United States payment of $ 117 million to the Great Basin tribe for the acquisition of 39,000 square miles (100,000 km ). European exploration of the Great Basin occurred during the 18th century Spanish colonization of the Americas . The first immigrant American to cross

200-516: Is a geographic division of the Basin and Range Province defined by Nevin Fenneman in 1931. The United States Geological Survey adapted Fenneman's scheme in their Physiographic division of the United States . The "section" is somewhat larger than the hydrographic definition. The Great Basin culture area , or indigenous peoples of the Great Basin , is a cultural classification of indigenous peoples of

250-458: Is characterized by a deep bed of unconsolidated valley fill from which the salt crust emerges. The current best understanding of the area's geological history is that the entire region between the Colorado River in the east and Baja California in the southwest (and bordered by various uplifts and mountains around the west-northwest-northern perimeters) has seen numerous cycles since at least

300-464: Is in a very flat basin. A large influence on the water volume is local snow melt, especially from Steens Mountain , south of the lake. For example, large snowpacks in the mid-1980s caused the lake to expand from approximately 67 to 160 square miles (170 to 410 km) within three years, flooding usually dry areas and damaging a branch of the Oregon Eastern Railway . Soon afterward, drought in

350-536: Is nicknamed "The Loneliest Road in America", and Nevada State Route 375 is designated the "Extraterrestrial Highway". The Great Basin is traversed by several rail lines including the Union Pacific Railroad 's Overland Route (Union Pacific Railroad) through Reno and Ogden , Feather River Route , Central Corridor and Los Angeles and Salt Lake Railroad . There has been a succession of indigenous peoples of

400-488: Is not the lowest point of the basin: the lowest point (which is only slightly lower) is several miles to the west and varies in position, depending on rainfall and evaporation patterns. The salt flats are hazardous to traverse (in many cases being only a thin white crust over mud), and so the sign marking the low point is at the pool instead. The basin was considered the lowest elevation in the Western Hemisphere until

450-464: Is part of the Great Basin's central Lahontan subregion. The hydrographic Great Basin contains multiple deserts and ecoregions , each with its own distinctive set of flora and fauna. The ecological boundaries and divisions in the Great Basin are unclear. The Great Basin overlaps four different deserts: portions of the hot Mojave and Colorado (a region within the Sonoran Desert ) Deserts to

500-697: Is present in Malheur Lake and has caused extreme habitat damage. Harney Lake has been inhospitable to redband trout for many years due to high alkalinities. Today, redband trout in the Malheur Lake basin are widely distributed in small- and medium-size streams. The redband trout is a unique subspecies adapted to the Malheur Lake basin ecosystem. In these closed, high-desert basins, redband trout have evolved to survive in environments with vast extremes of both water flow and temperature. They are one of only eight desert-basin populations of interior native redband trout. The Malheur Lake redband comprises 10 population groups in

550-574: Is slightly misleading; the region comprises many small basins. The Great Salt Lake , Pyramid Lake , and the Humboldt Sink are a few of the "drains" in the Great Basin. The Salton Sink is another closed basin within the Great Basin. The Great Basin Divide separates the Great Basin from the watersheds draining to the Pacific Ocean. The southernmost portion of the Great Basin is the watershed area of

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600-573: Is the largest area of contiguous endorheic watersheds , those with no outlets to the ocean, in North America . It spans nearly all of Nevada , much of Utah , and portions of California , Idaho , Oregon , Wyoming , and Baja California . It is noted for both its arid climate and the basin and range topography that varies from the North American low point at Badwater Basin in Death Valley to

650-518: Is the result of extension and thinning of the lithosphere , which is composed of crust and upper mantle . Extensional environments like the Basin and Range are characterized by listric normal faulting , or faults that level out with depth. Opposing normal faults link at depth producing a horst and graben geometry, where horst refers to the upthrown fault block and graben to the down dropped fault block. Sediment build-up over thousands of years filled

700-583: The Cui-ui sucker fish (endangered 1967) and the Lahontan cutthroat trout (threatened 1970). Large invertebrates include tarantulas (genus Aphonopelma ) and Mormon crickets . Exotic species, including chukar , grey partridge , and Himalayan snowcock , have been successfully introduced to the Great Basin, although the latter has only thrived in the Ruby Mountains . Cheatgrass , an invasive species which

750-690: The Great Basin fence lizard , longnose leopard lizard and horned lizard are common, especially in lower elevations. Rattlesnakes and gopher snakes are also present. The Inyo Mountains salamander is endangered. Shorebirds such as phalaropes and curlews can be found in wet areas. American white pelicans are common at Pyramid Lake . Golden eagles are also very common in the Great Basin. Mourning dove , western meadowlark , black-billed magpie , and common raven are other common bird species. Two endangered species of fish are found in Pyramid Lake:

800-711: The Gulf of Mexico or the Pacific Ocean . The region is bounded by the Wasatch Mountains to the east, the Sierra Nevada and Cascade Ranges to the west, and the Snake River Basin to the north. The south rim is less distinct. The Great Basin includes most of Nevada , half of Utah , substantial portions of Oregon and California , and small areas of Idaho , Wyoming , and Baja California, Mexico . The term "Great Basin"

850-678: The Laguna Salada . The Great Basin's longest and largest river is the Bear River of 350 mi (560 km), and the largest single watershed is the Humboldt River drainage of roughly 17,000 sq mi (44,000 km ). Most Great Basin precipitation is snow, and the precipitation that neither evaporates nor is extracted for human use will sink into groundwater aquifers , while evaporation of collected water occurs from geographic sinks . Lake Tahoe , North America's largest alpine lake ,

900-792: The National Park Service , its boundaries approximate the hydrographic Great Basin but exclude the southern " panhandle ". The Great Basin Province was defined by botanist Armen Takhtajan to extend well beyond the boundaries of the hydrographically defined Great Basin: it includes the Snake River Plain , the Colorado Plateau , the Uinta Basin , and parts of Arizona north of the Mogollon Rim . The Great Basin physiographic section

950-578: The Salton Sea . These alternate with periodic water body breakthroughs and rearrangements due to erosion and the proximity of the San Andreas Fault . This process has resulted in a high number of evaporating and reforming endorheic lakes throughout the Quaternary Period in the area, with an intertwined history of various larger bodies of water subsuming smaller ones during water table maxima and

1000-647: The Americas and a cultural region located between the Rocky Mountains and the Sierra Nevada. The culture area covers approximately 400,000 sq mi (1,000,000 km ), or just less than twice the area of the hydrographic Great Basin. The hydrographic Great Basin is a 209,162-square-mile (541,730 km ) area that once drained internally. All precipitation in the region evaporated, sank underground or flowed into lakes (mostly saline). As observed by Fremont, creeks, streams, or rivers find no outlet to either

1050-468: The Basin and Range Province contains the Great Basin, but extends into eastern Oregon , southern Idaho , and the Colorado River watershed and the northwest corner of Arizona ). The Basin and Range region is the product of geological forces stretching the Earth's crust, creating many north–south trending mountain ranges. These ranges are separated by flat valleys or basins. These hundreds of ranges make Nevada

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1100-551: The Fremont built small villages and grew crops like corn and squash. Seven hundred years ago, the Shoshone inhabited the area after the Fremont. They were hunter-gathers and lived in temporary homes to be able to follow animal herds and collect plants. Now, Shoshone descendants live in nearby areas. Other tribes in the area included the Ute , Mono , and Northern Paiute . All of the tribes speak

1150-466: The Great Basin . Paleo-Indian habitation by the Great Basin tribes began as early as 10,000 B.C. . Archaeological evidence of habitation sites along the shore of Lake Lahontan date from the end of the ice age when its shoreline was approximately 500 feet (150 m) higher along the sides of the surrounding mountains. The Paleo-Indians were mainly hunters and hunted bison, the extinct mammoth, and extinct ground sloth. For housing, since they followed

1200-625: The Great Basin from the Sierra Nevada was Jedediah Strong Smith in 1827. Peter Skene Ogden of the British Hudson's Bay Company explored the Great Salt Lake and Humboldt River regions in the late 1820s, following the eastern side of the Sierra Nevada to the Gulf of California. Benjamin Bonneville explored the northeast portion during an 1832 expedition . The United States had acquired claims to

1250-725: The Great Basin into three ecoregions roughly according to latitude: the Northern Basin and Range ecoregion , the Central Basin and Range ecoregion , and the Mojave Basin and Range ecoregion . Great Basin wildlife includes pronghorn , mule deer , mountain lion , and lagomorphs such as black-tailed jackrabbit and desert cottontail and the coyotes that prey on them. Packrats , kangaroo rats and other small rodents are also common, and are predominantly nocturnal. Elk and bighorn sheep are present but uncommon. Small lizards such as

1300-592: The animals they were hunting, they had no permanent villages. The next group to live in the area was the Great Basin Desert Archaic, from approximately 9,000 to 1,500 years ago. They hunted animals like mule deer and antelope and gathered onions, wild rye, and pinyon pine nuts. Then, from 1,500 to 700 years ago, the Fremont lived in the area. Unlike the Paleo-Indians, who moved around to follow bison herds,

1350-605: The basin experiences a semi-arid or arid climate with warm summers and cold winters. However, some of the mountainous areas in the basin are high enough in elevation to experience an alpine climate . Due to the region's altitude and aridity, most areas in the Great Basin experience a substantial diurnal temperature variation . Badwater Basin Badwater Basin is an endorheic basin in Death Valley National Park , Death Valley , Inyo County, California , noted as

1400-707: The closed interior basin of Harney and Malheur lakes. Historically, all streams were interconnected, and these fish moved through all the lakes and streams. While not an officially designated threatened or endangered species, the redband trout is recognized as important resource, and the Steens Mountain Cooperative Management and Protection Act of 2000 (Public Law 106-399) sets aside land in Oregon for protection and research of redband trout. Great Basin The Great Basin ( Spanish : Gran Cuenca )

1450-526: The discovery of Laguna del Carbón in Argentina at −344 ft (−105 m). At Badwater Basin, significant rainstorms flood the valley bottom periodically, covering the salt pan with a thin sheet of standing water, forming a temporary lake known as Lake Manly . Newly formed lakes do not last long though, because the 1.9 in (48 mm) of average rainfall is overwhelmed by a 150 in (3,800 mm) annual evaporation rate and usually lakes are only

1500-672: The down-faulted basins between ranges and created relatively flat lacustrine plains from Pleistocene lake beds of the Great Basin. For example, after forming about 32,000 years ago , Lake Bonneville overflowed about 14,500 years ago in the Bonneville Flood through Red Rock Pass and lowered to the "Provo Lake" level (the Great Salt Lake , Utah Lake , Sevier Lake , Rush Lake , and Little Salt Lake remain). Lake Lahontan , Lake Manly , and Lake Mojave were similar Pleistocene lakes. The Great Basin physiographic section of

1550-551: The early 1990s reduced the lake size to just 200 acres (0.31 sq mi), exposing large mudflats and dusty playas. Malheur Lake is a remnant of a much larger Pleistocene lake that drained east to the Malheur River , a tributary of the Snake River . The size of this ancient lake, which existed during a wetter climate, has been estimated at 900 square miles (2,300 km), with a maximum depth of 35 feet (11 m). Its outlet

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1600-704: The eastern regions of the 1848 California Gold Rush , with its immigrants crossing the Great Basin on the California Trail along Nevada's Humboldt River to Carson Pass in the Sierras. The Oregon Territory was established in 1848 and the Utah Territory in 1850. In 1869 the First transcontinental railroad was completed at Promontory Summit in the Great Basin. Around 1902, the San Pedro, Los Angeles and Salt Lake Railroad

1650-402: The elevation increases, the temperature decreases and precipitation increases. Because of this, forests can occur at higher elevations. Utah juniper / single-leaf pinyon (southern regions) and mountain mahogany (northern regions) form open pinyon-juniper woodland on the slopes of most ranges. Stands of limber pine and Great Basin bristlecone pine ( Pinus longaeva ) can be found in some of

1700-508: The higher ranges. In riparian areas with dependable water cottonwoods ( Populus fremontii ) and quaking aspen ( Populus tremuloides ) groves exist. Because the forest ecosystem is distinct from a typical desert, some authorities, such as the World Wildlife Fund , separate the mountains of the Great Basin desert into their own ecoregion: the Great Basin montane forests . Many rare and endemic species occur in this ecoregion, because

1750-526: The highest point of the contiguous United States , less than 100 miles (160 km) away at the summit of Mount Whitney . The region spans several physiographic divisions, biomes , ecoregions , and deserts . The term "Great Basin" is applied to hydrographic , biological , floristic , physiographic, topographic , and ethnographic geographic areas. The name was originally coined by John C. Frémont , who, based on information gleaned from Joseph R. Walker as well as his own travels, recognized

1800-476: The hydrographic nature of the landform as "having no connection to the ocean". The hydrographic definition is the most commonly used, and is the only one with a definitive border. The other definitions yield not only different geographical boundaries of "Great Basin" regions but regional borders that vary from source to source. The Great Basin Desert is defined by plant and animal communities, and, according to

1850-584: The individual mountain ranges are isolated from each other. During the Last Glacial Period , the Great Basin was wetter. As it dried during the Holocene epoch, some species retreated to the higher isolated mountains and have high genetic diversity. Other authorities divide the Great Basin into different ecoregions, depending on their own criteria. Armen Takhtajan defined the "Great Basin floristic province". The U.S. Environmental Protection Agency divides

1900-486: The lowest point in North America and the United States , with a depth of 282 ft (86 m) below sea level . Mount Whitney , the highest point in the contiguous United States , is only 84.6 miles (136 km) to the northwest. The site itself consists of a small spring -fed pool of "bad water" next to the road in a sink ; the accumulated salts of the surrounding basin make it undrinkable, thus giving it

1950-523: The most mountainous state in the country. The Great Basin's two most populous metropolitan areas are the Reno-Sparks metropolitan area to the west and the Wasatch Front to the east (with the latter being significantly more populous than the former). The region between these two areas is sparsely populated, but includes the smaller cities of Elko , Ely , Wendover , West Wendover , and Winnemucca . To

2000-473: The name. The pool does have animal and plant life , including pickleweed , aquatic insects , and the Badwater snail . Badwater Crater , the lowest place on the planet Mars , is named after the basin due to their similarities. Adjacent to the pool, where water is not always present at the surface, repeated freeze–thaw and evaporation cycles gradually push the thin salt crust into hexagonal shapes. The pool

2050-874: The north are; in California Susanville , in Oregon Burns and Hines , in Idaho Malad and in Wyoming Evanston . To the south are Cedar City , Tonopah , and Bishop and the very southern area of the basin has the communities of Pahrump , Palmdale , Victorville , and Palm Springs . Interstate Highways traversing the Great Basin are Interstate 80 (I-80) and I-15 , and I-70 and I-84 have their respective endpoints within its boundaries. Other major roadways are U.S. Route 6 (US 6), US 50 , US 93 , US 95 and US 395 . The section of US 50 between Delta, Utah , and Fallon, Nevada ,

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2100-477: The south, and the cold Great Basin and Oregon High Deserts in the north. The deserts can be distinguished by their plants: the Joshua tree and creosote bush occur in the hot deserts, while the cold deserts have neither. The cold deserts are generally higher than the hot and have more even spread of precipitation throughout the year. The climate and flora of the Great Basin are strongly dependent on elevation; as

2150-517: The start of the Pleistocene (and perhaps up to 3  Ma ). In these cycles, pluvial lakes of varying size have come and gone in a complex cycle, mainly tied to changing climate patterns (particularly, glaciation during the numerous recent Ice Age cycles ), but also influenced by the progressive depositing of alluvial plains and deltas by the Colorado River, as can also be seen in the case of

2200-523: The state of Connecticut . Malheur Lake contains many aquatic plants and grasses and is an important nesting and feeding area for waterfowl, migratory birds, and many other bird species. Wildlife includes ducks , geese , swans , herons , egrets , gulls , terns , and grebes . The Great Basin redband trout ( Oncorhynchus mykiss newberri ) has reduced access to Malheur and Harney lakes due to irrigation diversions, channelization, draining of marshlands, and high alkalinities . An exotic carp population

2250-525: The subsequent splitting and disappearance thereof during the evaporative part of the cycles. Although these local cycles are now somewhat modified by human presence, their legacy persists; despite appearances much to the contrary, Death Valley actually sits atop one of the largest aquifers in the world. Throughout the Quaternary's wetter spans, streams running from nearby mountains filled Death Valley, creating Lake Manly , which during its greatest extents

2300-601: The territory north of the 42nd parallel via the 1819 Adams–Onís Treaty with Spain and 1846 Oregon Treaty with Britain. The US gained claims to most of the rest of the Great Basin via the 1848 Mexican Cession . The first non-indigenous settlement was in 1847 in the Great Salt Lake Valley, leading to the first American religious settlement effort of the Mormon provisional State of Deseret in 1849 in present-day Utah and northern Nevada. Later settlements were connected with

2350-478: Was approximately 80 mi (130 km) long and up to 600 ft (180 m) deep. Numerous evaporation cycles and a lack of outflow caused an increasing hypersalinity , typical for endorheic bodies of water. Over time, this hypersalinization, combined with sporadic rainfall and occasional aquifer intrusion, has resulted in periods of "briny soup", or salty pools, on the lowest parts of Death Valley's floor. Salts (95% table salt – NaCl ) began to crystallize, coating

2400-402: Was constructed in the lower basin and Mojave Desert for California-Nevada rail service to Las Vegas, Nevada. The climate varies throughout the Great Basin by elevation, latitude, and other factors. Higher elevations tend to be cooler and receive more precipitation. The western areas of the basin tend to be drier than the eastern areas because of the rain shadow of the Sierra Nevada . Most of

2450-480: Was originally a channel near New Princeton , but lava flows diverted the water to a gap near Crane . Much of the original lake bottom has since turned into desert or become meadows periodically watered by lake overflows. Mud Lake and Harney Lake are also remnants of the original pluvial lake. The lakes as well as nearby marshes and playas are part of Harney Basin. The basin, a closed depression , covers 5,300 square miles (14,000 km), which makes it larger than

2500-422: Was unintentionally introduced, forms a critical portion of their diets. Feral horses ( mustangs ) and feral burros are highly reproductive, and ecosystem-controversial, alien species. Most of the Great Basin is open range and domestic cattle and sheep are widespread. The Great Basin includes valleys, basins, lakes and mountain ranges of the Basin and Range Province . The basin and range topography

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