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Tuolumne Meadows (/ t u ˈ ɒ l əm i /) is a gentle, dome-studded, sub-alpine meadow area along the Tuolumne River in the eastern section of Yosemite National Park in the United States. Its approximate location is 37°52.5′N 119°21′W / 37.8750°N 119.350°W / 37.8750; -119
Stately Pleasure Dome - Hermaphrodite Flake. In Tuolumne, rock climbing is popular, [40] [41] [42] and there are many granite domes, there and elsewhere in Yosemite. [43]In contrast to the big walls of Yosemite Valley, climbing at Tuolumne generally consists of short- to medium-length routes on eleven major domes and several minor ones; see Granite Domes of Yosemite National Park.
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 ...
Elizabeth Lake is a lake, in the area of Tuolumne Meadows, in Yosemite National Park, California. It was named for a geologist's niece, one Elizabeth Crow Simmons. [1] The lake is at the base of Unicorn Peak, and is also near Johnson Peak. [2] [3] The lake is in Tuolumne County, California. [4]
Ragged Peak is a mountain, in the Tuolumne Meadows area of Yosemite National Park. Of the ridge south of the Young Lakes region, Ragged Peak is the most prominent feature. It is 4 miles (6.4 km) north of Tioga Road and its summit has a great view of Mount Conness's southwest face. [2] Ragged Peak is an isolated summit, close to Young Lakes. [3]
Universities and colleges in Tuolumne County, California (2 P) Pages in category "Tourist attractions in Tuolumne County, California" The following 8 pages are in this category, out of 8 total.
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Johnson Peak is the highest mountain, in Tuolumne Meadows, Yosemite National Park. [2] Johnson Peak is made of eroded granite. At 85 Ma, the Johnson Granite Porphyry is the youngest granite rock in the Yosemite National Park, though the entire peak formed beneath the Earth's crust. It broached the surface much later, via subduction. [3]