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Origin of Yosemite Valley, Chapter 4, Glaciers of California, by Bill Guyton; Geology of the National Parks: Yosemite National Park's Geology (USGS online exhibit) The Geologic Story of Yosemite National Park by Dr. N. King Huber (USGS, 1987) USGS Bulletin 1595. Complete text online; The Geologic Story of Yosemite National Park (1987) by N ...
The natural and cultural history of Yosemite Valley is presented at the Yosemite Valley Visitor Center, the adjoining Yosemite Museum, and the Nature Center at Happy Isles. The parks' two National Historic Landmarks are the Sierra Club 's LeConte Memorial Lodge (Yosemite's first public visitor center), and the Ahwahnee Hotel.
McCauley purchased the land in 1883 and began to live full-time at the ranch in 1897. McCauley's son Fred inherited the ranch after James' death in an wagon accident in 1911. Fred dispersed the property, which became known as "Foresta" and was unoccupied after 1955. The National Park Service acquired the ranch in 1974. The barn is a wood ...
The Mono Basin is an endorheic drainage basin located east of Yosemite National Park in California and Nevada. [3] [4] It is bordered to the west by the Sierra Nevada, to the east by the Cowtrack Mountains, to the north by the Bodie Hills, and to the south by the north ridge of the Long Valley Caldera.
Half Dome is a quartz monzonite batholith at the eastern end of Yosemite Valley in Yosemite National Park, California. It is a well-known rock formation in the park, named for its distinct shape. One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half.
Map of the trails joining six of the High Sierra Camps in Yosemite National Park. The High Sierra Camps are nine rustic lodging facilities located in two national parks and a national monument in California's Sierra Nevada mountain range. Open most years from June or July to September, they are staffed camps with tent cabins and food service ...
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