The East Temple

The East Temple is a prominent 7,709 feet (2,350 m) summit composed of Navajo Sandstone in Zion National Park, in Washington County of southwest Utah, United States.[3] It is one of the notable landmarks in the park. The nearest neighbor is Twin Brothers, one-half mile to the north, and the nearest higher peak is The West Temple, 3.85 miles (6.20 km) to the west-southwest.[1] The mountain is situated 1.8 miles northeast of the park headquarters, at the confluence of Pine Creek and the North Fork Virgin River. This feature's name was applied by John Wesley Powell during his explorations in 1872, and was officially adopted in 1934 by the U.S. Board on Geographic Names.[3] The first ascent was made in 1937 by Glen Dawson, Dick Jones, Homer Fuller, Wayland Gilbert, and Jo Momyer.[4]

The East Temple
The East Temple, west aspect
Highest point
Elevation7,709 ft (2,350 m)[1]
Prominence1,709 ft (521 m)[1]
Parent peakThe West Temple (7,810 ft)[2]
Isolation3.9 mi (6.3 km)[2]
Coordinates37°13′14″N 112°57′03″W[1]
Geography
The East Temple
Location in Utah
The East Temple
The East Temple (the United States)
LocationZion National Park
Washington County, Utah
United States
Parent rangeColorado Plateau
Topo mapUSGS Springdale East
Geology
Age of rockJurassic
Type of rockNavajo sandstone
Climbing
First ascent1937
Easiest routeclass 5.4 climbing[2]

Climbing Routes

Climbing Routes on The East Temple[5]

Climate

Spring and fall are the most favorable seasons to visit The East Temple. 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.[6]

See also

References

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