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Cathedral Peak (California)

From Biocrawler, the free encyclopedia.

Cathedral Peak
Cathedral Peak from Cathedral Lakes
Elevation:	10,911 ft (3,326 m)
Location:	California, USA
Range:	Cathedral Range, Sierra Nevada

<tr><td bgcolor=#e7dcc3 width=85>Coordinates: <td style="border-top:1px solid #e7dcc3" width=220>37° 50′ 52.5″ N 119° 24′ 19.8″ W (http://kvaleberg.com/extensions/mapsources/index.php?params=37_50_52.5_N_119_24_19.8_W_type:mountain_region:US) <tr><td bgcolor=#e7dcc3 width=85>Topo map: <td style="border-top:1px solid #e7dcc3" width=220>USGS Tenaya Lake <tr><td bgcolor=#e7dcc3 width=85>Type: <td style="border-top:1px solid #e7dcc3" width=220>Granite arete <tr><td bgcolor=#e7dcc3 width=85>Age of rock: <td style="border-top:1px solid #e7dcc3" width=220>Cretaceous <tr><td bgcolor=#e7dcc3 width=85>First ascent: <td style="border-top:1px solid #e7dcc3" width=220>1869 by John Muir <tr><td bgcolor=#e7dcc3 width=85>Easiest route: <td style="border-top:1px solid #e7dcc3" width=220>rock climb (class 4) </table> Cathedral Peak is the crowning peak of the Cathedral Range, a mountain range in the south-central portion of Yosemite National Park in Tuolumne County, California. The range is an offshoot of the Sierra Nevada. The peak, which lends its name to the range, derives its name from its cathedral-shaped peak, which was formed by glacial activity: the peak remained uneroded above the glaciers in the Pleistocene. The west peak of Cathedral Peak (shown foreshortened in the photograph) is called Eichorn Pinnacle, after Jules Eichorn, who first ascended a YDS 5.4 route in 1931. In 1869, John Muir wrote My first summer in the Sierra, where he described Cathedral Peak as

The body of the Cathedral is nearly square, and the roof slopes are wonderfully regular and symmetrical, the ridge trending northeast and southwest. This direction has apparently been determined by structure joints in the granite. The gable on the northeast end is magnificent in size and simplicity, and at its base there is a big snow-bank protected by the shadow of the building. The front is adorned with many pinnacles and a tall spire of curious workmanship. Here too the joints in the rock are seen to have played an important part in determining their forms and size and general arrangement. The Cathedral is said to be about eleven thousand feet above the sea, but the height of the building itself above the level of the ridge it stands on is about fifteen hundred feet. A mile or so to the westward there is a handsome lake, and the glacier-polished granite about it is shining so brightly it is not easy in some places to trace Front of Cathedral Peak the line between the rock and water, both shining alike.

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Reference

The High Sierra: Peaks, Passes, and Trails, 2nd edition, by R. J. Secor, ISBN 0898866251

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External links

Maps and aerial photos (http://kvaleberg.com/extensions/mapsources/index.php?params=37.84792_N_-119.4055_E_type:mountain_region:US)
- Topographic map from TopoZone (http://topozone.com/map.asp?lat=37.84792&lon=-119.4055&s=200&size=m&layer=DRG100)
- Aerial image from TerraServer-USA (http://terraserver-usa.com/map.aspx?t=1&s=14&lon=-119.4055&lat=37.84792&w=750&h=500)
- Surrounding area map from Google Maps (http://maps.google.com/maps?ll=37.84792,-119.4055&spn=0.4,0.6)
- Location in the United States from the Census Bureau (http://tiger.census.gov/cgi-bin/mapgen?lat=36.0000&lon=-97.0000&wid=50&ht=28&iwd=550&iht=260&mlat=37.84792&mlon=-119.4055&on=GRID&off=BACK&msym=smalldot)