Today, North Arapaho Peak is a topic that generates great interest and debate in society. For a long time, North Arapaho Peak has been the subject of study and analysis, but over time it has acquired even greater relevance. This topic has captured the attention of experts and professionals from various areas, who have dedicated themselves to researching and delving into its different aspects. Whether due to its impact on daily life, politics, culture or technology, North Arapaho Peak has become an unavoidable reference point today. In this article, we will thoroughly explore the different facets of North Arapaho Peak and its influence on our society.
North Arapaho Peak | |
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Highest point | |
Elevation | 13,508 ft (4,117 m)[1][2] |
Prominence | 1,665 ft (507 m)[2] |
Isolation | 15.38 mi (24.75 km)[2] |
Listing | |
Coordinates | 40°01′35″N 105°39′01″W / 40.026524°N 105.65035°W[3] |
Geography | |
Location | Continental Divide between Boulder and Grand counties, Colorado, United States[4] |
Parent range | Front Range, Highest summit of the Indian Peaks[2] |
Topo map | USGS 7.5' topographic map Monarch Lake, Colorado[3] |
North Arapaho Peak is the highest summit of the Indian Peaks in the northern Front Range of the Rocky Mountains of North America. The 13,508-foot (4,117 m) thirteener is located in the Indian Peaks Wilderness, 7.8 miles (12.6 km) west-southwest (bearing 245°) of the Town of Ward, Colorado, United States, on the Continental Divide separating Roosevelt National Forest and Boulder County from Arapaho National Forest and Grand County.[1][2][4][3]
Between North Arapaho Peak and neighboring South Arapaho Peak sits Arapaho Glacier, which is owned by the City of Boulder as part of its water supply. North and South Arapahoe Peaks are connected by a 0.8 mile, Class 4 connecting ridge. West of these peaks is Arapaho Pass.
According to the Köppen climate classification system, the mountain is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers.[5] 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. Climbers can expect afternoon rain, hail, and lightning from the seasonal monsoon in late July and August. This climate supports the Arapaho Glacier on the peak's east slope.