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Yosemite National Park
Rock Formations in Yosemite Valley
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Over eons, rivers and glaciers somehow carved 3,000 feet into solid granite to create Yosemite Valley. The nuances of the Valley form spectacular rock formations, for which Yosemite Valley is famous.
Visitors all year can gaze up from the Valley floor to appreciate the enormity of it all. During summer (or for those willing to do an overnight ski trip in winter), the view from Glacier Point provides a perspective from above.
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Half Dome is perhaps the most recognized symbol of Yosemite. Rising nearly 5,000 feet above the Valley floor, it is one of the most sought-after landmarks in Yosemite. Some people even hike or rock climb to the top! Half Dome can be seen throughout eastern Yosemite Valley and from Glacier Point.
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El Capitan is a favorite for experienced rock climbers. Rising more than 3,000 feet above the Valley floor, it is the largest monolith of granite in the world. El Capitan is opposite Bridalveil Fall and is best seen at the far west end of Yosemite Valley at Bridalveil and El Capitan Meadows.
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Cathedral Rocks and Spires form the eastern side of the canyon through which Bridalveil Creek flows. Some people think these rocks, just opposite of El Capitan, are even more impressive than El Capitan!
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The Three Brothers are located just east of El Capitan. It is made up of Eagle Peak (the uppermost "brother"), and Middle and Lower Brothers. It is best viewed from Southside Drive or the Merced River just east of El Capitan Picnic Area.
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Sentinel Rock, like a sentry, overlooks Yosemite Valley, along the opposite side of the Valley From Yosemite Falls.
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Glacier Point is most famous for the view you can see from it, but the Glacier Point cliff itself is quite impressive, as seen from near The Ahwahnee (left) or, more spectacularly, from Curry Village.
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Did You Know?
Unrestricted camping is no longer allowed in Yosemite Valley because of damage it causes. The placement of campgrounds and campsites has changed over the past 75 years in response to a growing understanding of river dynamics, geologic hazards, and the park's natural and cultural resources.
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Last Updated: March 09, 2007 at 21:40 EST |
