Vulcan's Throne
Vulcan's Throne[1] | |
---|---|
Highest point | |
Elevation | 1,555 m (5,102 ft) |
Coordinates | 36°13′08″N 113°04′39″W / 36.21889°N 113.07750°W |
Geography | |
Location | Grand Canyon National Park, Mohave County, Arizona, United States |
Topo map | USGS Vulcans Throne |
Geology | |
Age of rock | 73,000 years[2] |
Mountain type | cinder cone |
Vulcan's Throne is a cinder cone volcano and a prominent landmark on the North Rim of the Grand Canyon in Arizona, US. Vulcan's Throne, about a mile (1.7 km) west of Toroweap overlook, is part of the Uinkaret volcanic field.[2] The journals of traveler George Corning Fraser record a trip to the summit of Vulcan's Throne in 1914. At the time, the surrounding area was used for sheep grazing, and a small reservoir had been constructed at the base of the volcano.[3] Fraser wrote that
Vulcan's Throne is a pure cinder cone covered with scoriae, cinders, clinkers and peperino lying loose on the surface, with a slope, as near as I could measure, from 28° to 31°. A little sage, many cacti and perhaps some other similar low plants grow on it, but otherwise nothing. Climbing it was like ascending a sand-dune. Every step forward involved slipping half way back and boots were soon filled with painful bits of stone.
— George Corning Fraser, 17 July 1914, Journeys in the Canyon Lands of Utah and Arizona, 1914 - 1916, pp 25-26
The cinder cone was formed during the Quaternary Period, and is cut by recent movement on the Toroweap Fault.[4]
See also
References
- ^ Wood, Charles A.; Jűrgen Kienle (1993). Volcanoes of North America. Cambridge University Press. pp. 277–278. ISBN 0-521-43811-X.
- ^ a b "Uinkaret Field". Global Volcanism Program. Smithsonian Institution. Retrieved 2007-05-23.
- ^ Fraser, George Corning (2005). Frederick H. Swanson (ed.). Journeys in the Canyon Lands of Utah and Arizona, 1914 - 1916. University of Arizona Press. p. 25. Retrieved 20 May 2013.
- ^ "America's Volcanic Past: Arizona". U.S. Geological Survey. Retrieved 20 May 2013.
Vulcan's Throne, a Quaternary cinder cone on the rim of the Canyon is cut by recent fault movement on the Toroweap fault.