Mosquito Range
Geology
The mountains are faulted anticlines formed as part of the Sawatch Uplift during the Laramide orogeny around 65 million years ago (Mya). The mountains were originally contiguous with the higher Sawatch Range to the west, but were separated during the formation of the rift valley at the headwaters of the Arkansas River about 35 Mya. The range is primarily of granite. The eastern flank of the range along the rim of South Park is overlain by Paleozoic and Mesozoic sedimentary rocks. The northern end of the range was glaciated during Pleistocene time, forming U-shaped valleys in the canyons.
The high ridge of the range forms a relatively difficult barrier between South Park and the Arkansas headwaters. Several of the high peaks of the range are prominently visible from the southern side of Fremont Pass along State Highway 91 between Climax and Leadville. The range is not traversed by any major highway, but only in two places by backroads over high passes: Mosquito Pass and Weston Pass. Much of the range is located within the Pike National Forest.
Highest peaks
Rank | Peak | Elevation |
---|---|---|
1 | Mount Lincoln | 14,293 ft = 4356.5 m |
2 | Quandary Peak | 14,265 ft = 4348.0 m |
3 | Mount Democrat | 14,148 ft = 4312.3 m |
4 | Mount Sherman | 14,036 ft = 4278.2 m |
5 | Fletcher Mountain | 13,951 ft = 4252.3 m |
5 | Gemini Peak | 13,951 ft = 4252.3 m |
7 | Pacific Peak | 13,950 ft = 4252.0 m |
8 | Horseshoe Mountain | 13,898 ft = 4236.1 m |
See also
References
- ^ This table includes only mountain peaks with a minimum of 100 m (328 ft) of topographic prominence. Using this rule, Mount Bross is barely excluded.
- ^ Lipsher, Steve (2002-07-07). "No tall tale: State higher than thought". Denver Post. Retrieved 2007-06-21.
External links
- Media related to Mosquito Range at Wikimedia Commons
- Mosquito Range at Peakbagger.com