Tuolumne Peak | |
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Southeast aspect centered at top | |
Highest point | |
Elevation | 10,845 ft (3,306 m) NAVD 88[1] |
Prominence | 685 ft (209 m) [1] |
Coordinates | [ ⚑ ] : 37°52′31″N 119°29′5″W / 37.87528°N 119.48472°W [1] |
Geography | |
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Location | Yosemite National Park Tuolumne County, California , United States |
Parent range | Sierra Nevada |
Topo map | USGS Falls Ridge |
Geology | |
Age of rock | Cretaceous |
Type of rock | Granodiorite |
Climbing | |
First ascent | Richard M. Leonard and Sierra Club party on July 9, 1932 |
Tuolumne Peak is a mountain, in Yosemite National Park, in the area of Tuolumne Meadows. It is a fractured granite, twin summited peak, and is close to geographic center of the park. Tuolumne Peak is located approximately 2.5 miles (4.0 km) northeast of Mount Hoffmann via a granite ridge-line. It is climbed less often than Hoffman, probably due to a more difficult approach.[2]
There is rock climbing, on Tuolumne Peak.[3]
Tenaya Glacier had effects, at least near Tuolumne Peak, during the Wisconsin Glacial Stage, over-topping the ridge that connects Tuolumne Peak to Mount Hoffman, isolating both tops.[4]
Tuolumne Peak is located in an alpine climate zone.[5] Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the range. Script error: No such module "weather box".
Original source: https://en.wikipedia.org/wiki/Tuolumne Peak.
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