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The Gros Ventre Formation is a geologic formation in Wyoming, USA. It preserves fossils dating back to the Cambrian period . The Gros Ventre consists of three main members; the Wolsey Shale , the Death Canyon Limestone, and the Park Shale .
The Gros Ventre Range (/ ˌ ɡ r oʊ ˈ v ɑː n t / groh-VAHNT) is part of the Central Rocky Mountains and is located west of the Continental Divide in U.S. state of Wyoming. The name "Gros Ventre" is French for "big belly." The highest summit in the range is Doubletop Peak at 11,720 feet (3,570 m). [1]
Latest Cretaceous time saw the formation of a low broad northwest-trending arch along the approximate area of the present Teton Range and Gros Ventre Mountains. Part of the evidence for the first Laramide mountain building west of the Teton region is the several hundred cubic miles of quartzite boulders derived from the Targhee uplift , which ...
Hodges Peak is located on the crest of the Gros Ventre Range which is a subrange of the Rocky Mountains.Hodges Peak ranks as the ninth-highest peak in the range and is 2.27 miles (3.65 km) south-southeast of Doubletop Peak, the highest peak in the range. [2]
Sheep Mountain is in the Gros Ventre Wilderness of Bridger–Teton National Forest. At the northern end of Sheep Mountain is the location of the Gros Ventre landslide . In 1996, a U.S. Air Force C-130 cargo plane carrying an automobile and equipment outbound from Jackson Hole crashed into Sheep Mountain, killing a U.S. Secret Service agent and ...
The Gros Ventre Wilderness (/ ˌ ɡ r oʊ ˈ v ɑː n t / groh-VAHNT) is located in Bridger-Teton National Forest in the U.S. state of Wyoming. Most of the Gros Ventre Range is located within the wilderness. U.S. Wilderness Areas do not allow motorized or mechanized vehicles, including bicycles.
White Eagle, "the last major Chief of the Gros Ventre people", died "at the mouth of the Judith River" on February 9, 1881. [11] Gros Ventre moving camp on horses rigged with travois. In 1884, gold was discovered in the Little Rocky Mountains. Pressure from miners and mining companies forced the tribes to cede sections of the mountains in 1885.
The landslide created a large dam over 200 feet (61 m) high and 400 yards (370 m) wide across the Gros Ventre River, backing up the water and forming Lower Slide Lake. On May 18, 1927, part of the landslide dam failed, resulting in a massive flood that was six feet (1.8 m) deep for at least 25 miles (40 km) downstream.