Mount Doody, Mountain summit in Glacier National Park, Montana, US
Mount Doody is a mountain summit in the Lewis Range within Glacier National Park, reaching an elevation that places it among the park's higher peaks. The peak sits along the same ridgeline as the Cloudcroft Peaks, making it part of a distinctive chain of summits in this region.
The peak received its name from Dan Doody, one of the first six rangers who patrolled Glacier National Park's Middle Fork drainages in its early years. Its rock layers formed approximately 170 million years ago through the Lewis Overthrust, a major geological event that shaped this mountain range.
The mountain forms part of the Lewis Range ecosystem, contributing to the geographical and natural heritage of Glacier National Park's protected landscape.
Reaching this summit requires mountain climbing experience with steep slopes and exposed rock sections, so proper equipment and fitness are necessary. Conditions change rapidly at elevation, especially in exposed areas where wind and cold become significantly stronger.
The mountain's rock formation consists of sedimentary layers that were thrust over older rocks through a major geological event, making it a striking example of this rare process. This thrust created layers in unexpected positions, revealing the earth's powerful reshaping forces to anyone paying attention.
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