| Vesta Temple | |
| Label: | Vesta Temple |
| Label Position: | bottom |
| Elevation Ft: | 6299 |
| Elevation Ref: | [1] |
| Prominence Ft: | 889 |
| Isolation Mi: | 1.27 |
| Isolation Ref: | [2] |
| Parent Peak: | Diana Temple (6,683 ft) |
| Country: | United States |
| State: | Arizona |
| Region: | Coconino |
| Region Type: | County |
| Part Type: | Protected area |
| Part: | Grand Canyon National Park |
| Range: | Coconino Plateau Colorado Plateau |
| Map: | Arizona#USA |
| Map Size: | 230 |
| Coordinates: | 36.0935°N -112.269°W |
| Coordinates Ref: | [3] |
| Topo: | USGS Piute Point |
| Rock: | limestone, sandstone, mudstone |
| First Ascent: | Alan Doty |
Vesta Temple is a 6299feet summit located in the Grand Canyon, in Coconino County of northern Arizona, US.[3] It is situated eight miles west-northwest of Grand Canyon Village, and immediately northeast of Mimbreno Point. Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north. Topographic relief is significant as Vesta Temple rises 3900abbr=offNaNabbr=off above the Colorado River in 2.5 miles. Vesta Temple is named for Vesta, the goddess of the hearth, home, and family according to Roman mythology.[4] Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities.[5] This geographical feature's toponym was officially adopted in 1908 by the U.S. Board on Geographic Names.[3] According to the Köppen climate classification system, Vesta Temple is located in a Cold semi-arid climate zone.[6]
The summit of Vesta Temple is composed of Permian Kaibab Limestone and Toroweap Formation overlaying cream-colored, cliff-forming, Permian Coconino Sandstone.[7] The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes. Below the Coconino Sandstone is reddish, slope-forming, Permian Hermit Formation, which in turn overlays the Pennsylvanian-Permian Supai Group.[8] Further down are strata of the conspicuous cliff-forming Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally granite of the Paleoproterozoic Vishnu Basement Rocks at river level in Granite Gorge. Precipitation runoff from Vesta Temple drains northeast to the Colorado River via Topaz Canyon and Boucher Creek.