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Generalized geologic map of the Yosemite area. (Based on a USGS image) The exposed geology of the Yosemite area includes primarily granitic rocks with some older metamorphic rock. The first rocks were laid down in Precambrian times, when the area around Yosemite National Park was on the edge of a very young North American continent.
Yosemite Falls is the highest waterfall in Yosemite National Park, dropping a total of 2,425 feet (739 m) from the top of the upper fall to the base of the lower fall. [2] Located in the Sierra Nevada of California , it is a major attraction in the park, especially in late spring when the water flow is at its peak.
Yosemite National Park (/ j oʊ ˈ s ɛ m ɪ t i / yoh-SEM-ih-tee [5]) is a national park of the United States in California. [ 6 ] [ 7 ] It is bordered on the southeast by Sierra National Forest and on the northwest by Stanislaus National Forest .
Annual park visitation exceeds 3.5 million, with most visitor use concentrated in the seven-square-mile (18 km 2) area of Yosemite Valley. [1] The geography of the Yosemite area can be visualized with the clickable map, below: Painting of Yosemite by Heinrich C. Berann. Aerial view of the entire park from the west, looking east.
Yosemite Falls is the highest waterfall in North America and is a big attraction, especially in the spring, when the water flow is at its peak. The valley is renowned for its natural environment and is regarded as the centerpiece of Yosemite National Park.
Now we know the valley and surrounding area as Yosemite National Park – one of America’s most popular national parks, with 3,897,070 million visitors in 2023 – designated in 1890. You have ...
Geological Ramblings in Yosemite. Heyday. ISBN 978-1-59714-072-0. Jones, Ray (2010). It Happened in Yosemite National Park: Remarkable Events That Shaped History. Globe Pequot. ISBN 978-0-7627-6231-6. Matthes, François (1930). Geologic history of the Yosemite valley. United States Government Printing Office. Righter, Robert W. (2005).
The glaciers that carved Yosemite Valley left many hanging valleys that spawned the waterfalls that pour into the valley. Most of the waterways that fed these falls carved the hanging valleys into steep cascades, but Bridalveil Creek still leaps into the valley from the edge of the precipice, although that edge has moved back into an alcove from the original edge of the valley.
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