Teton Range
| Teton Range | |
|---|---|
Teton Range, from the Snake River overlook, by Ansel Adams
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| Highest point | |
| Peak | Grand Teton |
| Elevation | 13,775 ft (4,199 m) NAVD 88 |
| Coordinates | 43°44′28″N 110°48′06″W / 43.74111°N 110.80167°W |
| Geography | |
| Country | United States |
| State | Wyoming |
| Range coordinates | 43°45′N 110°50′W / 43.750°N 110.833°WCoordinates: 43°45′N 110°50′W / 43.750°N 110.833°W |
| Parent range | Rocky Mountains |
The Teton Range is a mountain range of the Rocky Mountains in North America.
A north-south range, it is mostly on Wyoming's eastern side of the Idaho state line. It is south of Yellowstone National Park. Most of the east slope of the range is in Grand Teton National Park.
Early French Voyageurs used the name les trois tétons (the three nipples). It is likely that the Shoshone people once called the whole range Teewinot, meaning "many pinnacles".
The principal summits of the central massif, sometimes referred to as the Cathedral Group, are Grand Teton 13,775 feet (4,199 m), Mount Owen 12,928 feet (3,940 m), Teewinot 12,325 feet (3,757 m), Middle Teton 12,804 feet (3,903 m) and South Teton 12,514 feet (3,814 m). Other peaks in the range include Mount Moran 12,605 feet (3,842 m), Mount Wister 11,490 feet (3,500 m), Buck Mountain 11,938 feet (3,639 m) and Static Peak 11,303 feet (3,445 m).
Between six and nine million years ago, stretching and thinning of the Earth's crust caused movement along the Teton fault. The west block along the fault line rose to form the Teton Range, creating the youngest range of the Rocky Mountains. The fault's east block fell to form the valley called Jackson Hole. The geological processes that led to the current composition of the oldest rocks in the Teton range began about 2.5 billion years ago. At that time, sand and volcanic debris settled into an ancient ocean. Additional sediment was deposited for millions of years and eventually heat and pressure metamorphosed the sediment into gneiss. Subsequently, magma was forced up through the cracks in the gneiss to form granite, anywhere from inches to hundreds of feet thick. Other intrusive igneous rocks are noticeable as the black dikes of diabase, visible on the southwest face of Mount Moran and on the Grand Teton. Starting during the Cambrian period, deep deposits of sedimentary rock were deposited in shallow seas over the metamorphic basement rocks. Erosion and uplift have exposed the metamorphic and intrusive igneous rocks now visible on the east slope of the range and in the Cathedral Group and the paleozoic and cenozoic sedimentary rocks on the west slope. 2.1 million years ago the Huckleberry Ridge Tuff was deposited along the west slope of the north part of the range.
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Wikipedia