Regal Mountain
Appearance
Regal Mountain | |
---|---|
Wrangell-St. Elias National Park and Preserve, Alaska, U.S. | |
Parent range | Wrangell Mountains |
Topo map | USGS McCarthy C-5 |
Geology | |
Mountain type | Eroded stratovolcano or shield volcano |
Climbing | |
First ascent | August 3, 1964 by Yasuichi Kitamura, Ryoichi Hasegawa, Masao Tanaka, and Shinichi Naito[2] |
Easiest route | Glacier climb |
Regal Mountain is an eroded
glaciers
, no geological studies have been done, but published references state and the geological map shows that the mountain is an old eroded volcanic edifice.
Several major glaciers flow from the steep and heavily eroded flanks of Regal Mountain. The Rohn Glacier and Regal Glacier head east and southeast to join the Nizina Glacier, while the Root Glacier flows south 15 miles (24 km) to join the Kennicott Glacier just above the town of McCarthy. Each of those large glaciers exceeds 1 mile (1.6 km) in width, but largest of all on Regal Mountain is a massive unnamed glacier, over 3 miles (5 km) across, which flows northwest just over 10 mi (16 km) to join the mighty Nabesna.
See also
![](http://upload.wikimedia.org/wikipedia/commons/thumb/8/81/Regal_Mountain_summit.jpg/380px-Regal_Mountain_summit.jpg)
References
- Richter, Donald H.; Danny S. Rosenkrans; Margaret J. Steigerwald (1995). Guide to the Volcanoes of the Western Wrangell Mountains, Alaska. USGSBulletin 2072.
- Winkler, Gary R. (2000). A Geologic Guide to Wrangell—Saint Elias National Park and Preserve, Alaska: A Tectonic Collage of Northbound Terranes. ISBN 0-607-92676-7.
- Richter, Donald H.; Cindi C. Preller; Keith A. Labay; Nora B. Shew (2006). Geologic Map of the Wrangell-Saint Elias National Park and Preserve, Alaska. USGSScientific Investigations Map 2877.
- ^ a b "Alaska 13,000-foot Peaks". Peakbagger.com. Retrieved 2007-03-10.
- ^ "Alaska's Summits 13,000 feet and above". Archived from the original on June 30, 2006. Retrieved 2007-03-10.