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| Snake Range | |
|---|---|
 Wheeler Peak, highest mountain in the Snake Range | |
| Highest point | |
| Peak | Wheeler Peak |
| Elevation | 13,063 ft (3,982 m) |
| Coordinates | 38°59′09″N114°18′50″W / 38.98583°N 114.31389°W /38.98583; -114.31389 |
| Dimensions | |
| Length | 60 mi (97 km) North-South |
| Geography | |
 Location of the Snake Range within Nevada | |
| Country | United States |
| State | Nevada |
| Borders on | Schell Creek Range and Confusion Range |
TheSnake Range is amountain range inWhite Pine County,Nevada,United States.[1] The south-central portion of the range is included withinGreat Basin National Park, with most of the remainder included within theHumboldt-Toiyabe National Forest. The range reaches a maximum elevation of 13,065 feet (3,982 m) at the summit ofWheeler Peak, the tallest independent mountain within Nevada and the second highest point within the state (the highest point beingBoundary Peak).[2] The range also contains four of the five highest mountain peaks in Nevada, including all peaks greater than 12,000 feet (3,658 m) except for Boundary Peak.[3]
Typical of other ranges in theBasin and Range Province, the Snake Range runs in a north–south direction, for approximately 60 miles (97 km).
To the west are Spring Valley and theSchell Creek Range, and to the east across theUtah border areSnake Valley and theConfusion Range. Sacramento Pass (7,154 feet [2,181 m]) is whereU.S. Route 6-50, the "Loneliest Highway in America", crosses the range. It is the principal means of eastbound access to this part of eastern Nevada.
Great Basin National Park is located in the southern section of the Snake Range. Established in 1986, it protects the unique geologic and habitat features of the mountain range andGreat Basin Desert, and their representations of theCentral Basin and Range ecoregion. The southern section also includes the natural rockLexington Arch (83 feet (25 m) span), and theLehman Caves, both formed from the range'slimestone.
Several large groves of ancientGreat Basin Bristlecone Pine (Pinus longaeva) trees thrive in theGreat Basin montane forests of the range's higher elevations.
The higher elevations of the Snake Range in the northern section are protected by theMount Moriah Wilderness Area, and in the southern section by theHighland Ridge Wilderness.
The Snake Range includes two groups of peaks. The southern section rises quickly from a point near the border withLincoln County, reaching the summit of Granite Peak (11,218 feet [3,419 m]) just 10 miles (16 km) to the north.
From there northwards the range continues to rise, passingLincoln Peak (11,597 feet [3,535 m]), Mt. Washington (11,658 feet [3,553 m]),Pyramid Peak (11,926 feet [3,635 m]),Baker Peak (12,298 feet [3,748 m]), andDoso Doyabi (12,775 feet [3,894 m][4]).
It finally reaches its apex atWheeler Peak (13,063 feet [3,982 m]).
North of Wheeler Peak the range begins to drop, reaching 7,154 feet (2,181 m) at Sacramento Pass, just 11 miles (18 km) to the north. Sacramento Pass is where the more remote northern section of the range begins.
In just 12 miles (19 km) the North Snake Range rises past Silver Creek Canyon and Hendrys Creek Canyon to the summit of photogenicMt. Moriah (12,067 feet [3,678 m]). To the north of this peak is an unusual formation, a flatplateau of sub-alpine tundra called "The Table", covering about 2 square miles (5.2 km2) at an elevation of 11,000 feet (3,400 m). A grove of ancient Great Basin Bristlecone Pines grows on this plateau near the peak.
North of "The Table" is another unusual geologic feature. Deadman Creek and Smith Creek, draining eastward into Snake Valley, combine to carve a deep canyon into the range. The mouth of this canyon lies below 3,000-foot (910 m) cliffs, 6,000 feet (1,800 m) below and 6 miles (9.7 km) away from the summit of Mt. Moriah.
TheNorth Snake Range is an important geologic feature, containing some of the world's best examples of metamorphic rock and extensional deformation. The range has been designated as only the first 100 geoheritage sites by theInternational Union of Geological Sciences (IUGS).[5] Instead of normal faulting creating basins and ranges, like is seen throughout most of the Great Basin, the North Snake Range metamorphic core complex has undergone ductile deformation so that the metamorphic rocks have been stretched resulting in rocks that are 10% of their original thickness, stretching like taffy.[6]
