| The West Temple | |
|---|---|
.jpg) East aspect of The West Temple | |
| Highest point | |
| Elevation | 7,810 ft (2,380 m) |
| Prominence | 1,680 ft (510 m) |
| Isolation | 10.66 mi (17.16 km) |
| Coordinates | 37°12′39″N 113°01′15″W / 37.210869°N 113.02071°W / 37.210869; -113.02071 |
| Geography | |
  The West TempleLocation in UtahShow map of Utah The West TempleThe West Temple (the United States)Show map of the United States
| |
| Country | United States |
| State | Utah |
| County | Washington |
| Protected area | Zion National Park |
| Parent range | Colorado Plateau |
| Topo map | USGS Springdale West |
| Geology | |
| Rock age | Jurassic |
| Rock type | Navajo Sandstone |
| Climbing | |
| First ascent | 1933 |
| Easiest route | class 5.6 climbing |
The West Temple is a prominent 7,810-foot (2,380 m) mountain summit composed of Navajo Sandstone in Zion National Park in Washington County of Utah, United States. The West Temple, the highest feature in Zion Canyon, was originally called "Temp-o-i-tin-car-ur" meaning "Mountain without a trail" by the Paiute people. It was called Steamboat Mountain by local Mormon settlers before 1934, when the USGS officially changed it to its present name, which was applied by John Wesley Powell during his explorations in 1872. West Temple is situated two miles northwest of Springdale, Utah, one mile northeast of Mount Kinesava, and two miles west of the park headquarters. It is one of the notable landmarks in the park. The nearest higher peak is Windy Peak, 10.46 miles (16.83 km) to the north. Precipitation runoff from the mountain drains into tributaries of the Virgin River.
Climbing Routes
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Climbing Routes on The West Temple
- Southwest Ridge - class 5.6 - 10 pitches
- Back Where It All Begins - class 5.11a - 16 pitches
- Big Lebowski- class 5.11a/b - 21 pitches
- Lovelace - class 5.10 - 9 pitches
- Big Lie - class 5.10+ - 2 pitches
Geology
The upper white cliffs are composed of Navajo Sandstone, which in some places exhibit reddish staining caused by hematite (iron oxide), the source of which is the Temple Cap Formation caprock at the summit. Lower slopes and ledges are composed of Kayenta Formation, Moenave Formation, Chinle Formation, and Moenkopi Formation.
Climate
Spring and fall are the most favorable seasons to visit this feature. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.
See also
- Geology of the Zion and Kolob canyons area
- Mount Kinesava
- The Sundial
- The Witch Head
- Three Marys
- Altar of Sacrifice
References
- ^ "The West Temple, Utah". Peakbagger.com.
- ^ "West Temple, The - 7,810' UT". listsofjohn.com. Retrieved 2020-08-31.
- A Brief History of Climbing in Zion. bigwalls.net
- National Park Service nps.gov/zion
- U.S. Geological Survey Geographic Names Information System: The West Temple
- The West Temple Mountain Project
- "The Geology of Zion National Park", Utahgeology.com
- "Zion National Park, Utah, USA - Monthly weather forecast and Climate data". Weather Atlas. Archived from the original on January 27, 2019. Retrieved 31 August 2020.
External links
- Zion National Park National Park Service
- The West Temple: weather forecast
- Web cam