Pagoda Mountain | |
---|---|
Highest point | |
Elevation | 13,497 ft (4,114 m) [1] [2] |
Prominence | 410 ft (125 m) [3] |
Parent peak | Longs Peak (14,259 ft) [3] [4] |
Isolation | 0.71 mi (1.14 km) [3] |
Coordinates | 40°14′57″N105°37′35″W / 40.2493047°N 105.6262588°W [5] |
Geography | |
Country | United States |
State | Colorado |
County | Boulder County |
Protected area | Rocky Mountain National Park |
Parent range | Rocky Mountains Front Range |
Topo map | USGS Isolation Peak |
Geology | |
Rock age | Precambrian [6] |
Rock type | Granite of Longs Peak batholith [7] Biotite schist and gneiss [7] |
Climbing | |
Easiest route | class 3 scrambling [3] |
Pagoda Mountain is a 13,497-foot-elevation (4,114-meter) mountain summit in Boulder County, Colorado, United States.
Pagoda Mountain is located one mile east of the Continental Divide in the Front Range of the Rocky Mountains. [4] The mountain is situated within Rocky Mountain National Park and is the fifth-highest peak in Boulder County. [8] Precipitation runoff from the mountain's south slope drains to North St. Vrain Creek via Hunters Creek and the north slope drains to Glacier Creek which is a tributary of the Big Thompson River. Topographic relief is significant as the summit rises 1,940 feet (590 meters) above Green Lake in one-half mile. The mountain's toponym was officially adopted in 1911 by the United States Board on Geographic Names and is so named because the mountain's shape resembles a pagoda. [5]
According to the Köppen climate classification system, Pagoda Mountain is located in an alpine subarctic climate zone with cold, snowy winters and cool to warm summers. [9] Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring.
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