List of Great Basin Divide border landforms of Nevada

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A List of Great Basin Divide border landforms of Nevada .

Contents

Two sections cover Nevada, the north-northeast section with Oregon, Idaho, and Utah, and the southeast Nevada section, with Utah and California.

North-northeast Nevada list

From west to east

Southern Nevada list

Major watershed perimeters of Nevada Central Nevada Desert Basins.JPG
Major watershed perimeters of Nevada

Alphabetic

See also

Related Research Articles

Humboldt–Toiyabe National Forest National forest in Nevada and California, United States

The Humboldt–Toiyabe National Forest (HTNF) is the principal U.S. National Forest in the U.S. state of Nevada, and has a smaller portion in Eastern California. With an area of 6,289,821 acres (25,454.00 km2), it is the largest U.S. National Forest outside of Alaska.

Great Basin Large depression in western North America

The Great Basin is the largest area of contiguous endorheic watersheds – those with no outlets – in North America. It spans nearly all of Nevada, much of Utah, and portions of California, Idaho, Oregon, Wyoming, and Baja California, Mexico. 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 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.

Bruneau River River in Idaho and Nevada, United States

The Bruneau River is a 153-mile-long (246 km) tributary of the Snake River, in the U.S. states of Idaho and Nevada. It runs through a narrow canyon cut into ancient lava flows in southwestern Idaho. The Bruneau Canyon, which is up to 1,200 feet (370 m) deep and 40 miles (64 km) long, features rapids and hot springs, making it a popular whitewater trip.

Meadow Valley Wash Southern Nevada stream

The Meadow Valley Wash is a southern Nevada stream draining the Meadow Watershed that is bordered on three sides by the Great Basin Divide. The wash's Lincoln County headpoint is in the Wilson Creek Range, and the wash includes two upper confluences. Panaca is along the upper wash, and downstream of Caliente is the wash's confluence with its east fork. Just prior to the junction with the Muddy River, the wash flows from Lincoln County into northeastern Clark County. It flows into the Muddy in the Moapa Valley just west of Glendale adjacent to Interstate 15 approximately 40 miles (64 km) northwest of Las Vegas.

Sheep Range

The Sheep Range is located north of Las Vegas, Nevada in the United States. It is found in both Clark and Lincoln Counties in the Desert National Wildlife Refuge. The mountains reach a peak at Hayford Peak, 9,912 feet (3,021 m) above sea level between the Las Vegas Range to the east and the Desert Range to the west. The Sheep Range lies in a generally north-south direction.

Piute Range Landform in the Mojave Desert, California

The Piute Range is located in the Mojave Desert, primarily in northeast San Bernardino County, California, United States, with a north portion in Nevada. Most of the range is the eastern border of the Mojave National Preserve, a National Park Service natural area and park.

The Delamar Mountains are a mountain range in Lincoln County, Nevada, named after Captain Joseph Raphael De Lamar. The range extends for approximately 50 miles (80 km) in a NNE–SSW orientation with a width of about 11 miles (18 km). Surrounding ranges include the Burnt Springs Range and the Chief Range to the north, the Clover Mountains and Meadow Valley Mountains to the east and the Sheep Range and South Pahroc Range on the west. The Delamar Valley lies to the west, the Kane Springs Valley to the east and the Coyote Springs Valley lies to the south of the range.

Northern Basin and Range ecoregion

The Northern Basin and Range ecoregion is a Level III ecoregion designated by the United States Environmental Protection Agency (EPA) in the U.S. states of Oregon, Idaho, Nevada, Utah, and California. It contains dissected lava plains, rolling hills, alluvial fans, valleys, and scattered mountain ranges in the northern part of the Great Basin. Although arid, the ecoregion is higher and cooler than the Snake River Plain to the north and has more available moisture and a cooler climate than the Central Basin and Range to the south. Its southern boundary is determined by the highest shoreline of Pleistocene Lake Bonneville, which once inundated the Central Basin and Range. The western part of the region is internally drained; its eastern stream network drains to the Snake River system.

The Clover Mountains are a mountain range in Lincoln County, Nevada.

Seaman Range

The Seaman Range is a 30-mile (48 km) long mountain range in Lincoln and Nye counties, Nevada, in the western United States.

Snake Valley (Great Basin)

Snake Valley is a north-south trending valley that straddles the Nevada–Utah border in the central Great Basin. It is bound by the Snake Range and the Deep Creek Mountains to the west and the Confusion Range to the east. The valley is the gateway to Great Basin National Park and Lehman Caves, which is located in the western part of the valley and on the southern Snake Range.

Butler Valley is a valley of the Maria fold and thrust belt in western Arizona, USA. It lies east of the Colorado River, and is south of the west-flowing Bill Williams River.

Eldorado Valley

Eldorado Valley, or El Dorado Valley, is a Great Basin valley in the Mojave Desert southeast of Las Vegas and southwest of Boulder City, Nevada. The valley is endorheic, containing the Eldorado Dry Lake. The Great Basin Divide, transects ridgelines and saddles, on the north, northeast, east, and south around the valley, as the valley sits on the east of the McCullough Range, a Great Basin massif, on the Great Basin Divide at its north terminus and its south terminus.

Piute Valley

The Piute Valley is a 45-mile-long (72 km) north–south valley southeast of Las Vegas, Nevada, and northwest of Needles. The north of the valley is at Searchlight, with some of the valley extending northwest from Searchlight. At the center-north lies Cal-Nev-Ari, Nevada.

Sevier Desert Desert located in the southeast of the Great Basin

The Sevier Desert is a large arid section of central-west Utah, United States, and is located in the southeast of the Great Basin. It is bordered by deserts north, west, and south; its east border is along the mountain range and valley sequences at the perimeter of the Great Basin, with the large north–south Wasatch Range and its associated mountainous landforms. Its eastern border is specifically, the East Tintic, Gilson, and Canyon Mountains; also the massive Pahvant Range.

The Bull Valley Mountains are a 30-mi (48 km) long, mountain range in southwest Utah, located in northwest Washington County. The range is adjacent the Utah border and attached to the Clover Mountains of southeast Nevada. The Great Basin Divide transects the summits of both ranges, with the Escalante Desert north and northeast of the Bull Valley Mountains, and south of the mountains the Colorado River watershed, and specifically the Santa Clara River which drains southeasterly from an escarpment along the mountain range's southeast flank.


Indian Springs Pass, is a mountain pass 40-mi (64 km) northwest of Las Vegas in northwest Clark County, Nevada.

Jean Pass (north) is one of two passes on the west and northwest of the Jean Dry Lake basin, an endorheic basin bordering Jean, Nevada.

Toroweap Fault Geologic feature in the Grand Canyon, Arizona

The Toroweap Fault of northwest Arizona and southwest Utah is part of a fault system of the west Grand Canyon region, Arizona, US; also the west perimeter regions of the Coconino and Colorado Plateaus. The Hurricane Fault originates at the Toroweap Fault, in the region of the Colorado River, and strikes as the westerly depression of the Toroweap Fault. The Toroweap strikes northerly from the Colorado at the east of Toroweap Valley, and enters south Utah; from the Colorado River, the Hurricane Fault strikes north-northwest along the west flank of the small, regional Uinkaret Mountains, the west border of Toroweap Valley. The Hurricane Fault, and the Hurricane Cliffs strike into southwest Utah as part of the west, and southwest perimeter of the Colorado Plateau. The Hurricane Cliffs are made of Kaibab Limestone, an erosion resistant, cliff-forming rock unit.

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