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The East Temple
The East Temple from west.jpg
The East Temple, west aspect
Highest point
Elevation 7,709 ft (2,350 m)
Prominence 1,709 ft (521 m)
Isolation 3.9 mi (6.3 km)
Parent peak The West Temple (7,810 ft)
Geography
The East Temple is located in Utah
The East Temple
The East Temple
Location in Utah
The East Temple is located in the United States
The East Temple
The East Temple
Location in the United States
Location Zion National Park
Washington County, Utah
United States
Parent range Colorado Plateau
Topo map USGS Springdale East
Geology
Age of rock Jurassic
Type of rock Navajo sandstone
Climbing
First ascent 1937
Easiest route class 5.4 climbing

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. 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. 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. The first ascent was made in 1937 by Glen Dawson, Dick Jones, Homer Fuller, Wayland Gilbert, and Jo Momyer.

Climbing Routes

Climbing Routes on The East Temple

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.

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