Temple Butte | |
---|---|
Highest point | |
Elevation | 5,308 ft (1,618 m)[1] |
Prominence | 859 ft (262 m)[1] |
Parent peak | Chuar Butte (6,500 ft)[1] |
Isolation | 1.77 mi (2.85 km)[1] |
Coordinates | 36°09′45″N 111°49′26″W / 36.16250°N 111.82389°W[2] |
Geography | |
Location in Arizona (confluence of the Little Colorado and Colorado rivers) | |
Location | Palisades of the Desert,[3] East Rim, Grand Canyon |
Settlement | Grand Canyon Village, Arizona |
Parent range | East Rim, 2-mi[4] south of Little Colorado River with Colorado |
Topo map | USGS Cape Solitude |
Geology | |
Mountain type | sedimentary rock: sandstone, siltstone, mudstone, limestone, shale, sandstone |
Type of rock | Supai Group-(unit 4, eroded-prominence), Esplanade Sandstone), Supai Group, Redwall Limestone, (Tonto Group-(3 units)), 3_Muav Limestone, 2_Bright Angel Shale, 1_Tapeats Sandstone |
Climbing | |
Easiest route | class 4 climbing[1] |
Temple Butte, in the Grand Canyon, Arizona, US is a prominence below the East Rim. The butte lies on the west bank of the south-flowing Colorado River. The outfall from the Little Colorado River, draining from the Painted Desert to the east and southeast, is about two miles upstream.
Temple Butte is 5,308 feet (1,618 m) in elevation. It is the historical site of some wreckage of the 1956 Grand Canyon mid-air collision. It was first thought that smoke from Temple Butte, was due to a lightning strike fire, but later was found to be the result of the mid-air collision.
A closer view of Chuar and Temple Buttes.