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Yosemite National Park has documented the presence of more than 130 non-native plant species within park boundaries. They were introduced into Yosemite following the migration of early Euro-American settlers in the late 1850s.
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.
Map of Yosemite National Park based on a map by the USGS image from here. Original notes that the data was "generalized from geological map of Yosemite National Park and vicinity (Huber and others, in press)" and that "an intrusive suite is a grouping of genetically related plutonic rocks". Date: 23 May 2012, 20:52 (UTC) Source
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.
Mammoth Peak and Kuna Crest, taken near Gaylor Lakes Mount Maclure, Yosemite's fifth-highest mountain. Many mountains in Yosemite National Park are higher than 12,000 feet (3,700 m); three are higher than 13,000 feet (4,000 m). [1] [2] The peaks of Yosemite are among some of the highest mountains in California.
This is intended to be a complete list of the properties and districts on the National Register of Historic Places in Yosemite National Park, California, United States. The locations of National Register properties and districts for which the latitude and longitude coordinates are included below, may be seen in a Google map.
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