This article needs additional citations for
verification. (January 2021) |
Venus Temple | |
---|---|
Highest point | |
Elevation | 6,281 ft (1,914 m) [1] |
Prominence | 501 ft (153 m) [1] |
Parent peak | Jupiter Temple |
Isolation | 0.86 mi (1.38 km) [1] |
Coordinates | 36°07′25″N 111°53′01″W / 36.1234963°N 111.8834947°W [2] |
Geography | |
Location |
Grand Canyon National Park Coconino County, Arizona, US |
Parent range |
Kaibab Plateau (Walhalla Plateau) Colorado Plateau |
Topo map | USGS Cape Royal |
Geology | |
Age of rock | Pennsylvanian down to Neoproterozoic |
Mountain type | sedimentary rock: sandstone, siltstone, mudstone, limestone, shale volcanic rock: basalt |
Type of rock |
Supai Group, Redwall Limestone, Muav Limestone, Bright Angel Shale, Tapeats Sandstone, Grand Canyon Supergroup-(4 units), 2– Nankoweap Formation, 1– Unkar Group-members-(5) 5_ Cardenas Basalt, 4_ Dox Formation |
Venus Temple is a 6,281-foot-elevation summit located in the eastern
Grand Canyon, in
Coconino County of northern
Arizona,
US. The landform is attached to
Apollo Temple immediately south-southeast. Venus Temple is ~2.0 mi northwest of the southwest-flowing
Colorado River. Both Venus and Apollo Temples are 4.0 mi west of the south end of the
Grand Canyon’s East Rim. The east side of Venus Temple drains into Upper Basalt Canyon and Creek; the west side drains west-then-south into Lower Unkar Creek.
The prominence of Venus Temple is composed of lower members of the orange-red
Supai Group on the upper platform of the cliff-forming
Redwall Limestone, upon the Cambrian Tonto Group. Members of the
Grand Canyon Supergroup lie below.