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Regal Mountain

Regal Mountain is an eroded stratovolcano or shield volcano in the Wrangell Mountains of eastern Alaska. It is located in Wrangell-Saint Elias National Park about 19 mi (31 km) east of Mount Blackburn, the second highest volcano in the United States, and southeast of the massive Nabesna Glacier. Regal Mountain is the third highest thirteener (a peak between 13,000 and 13,999 feet in elevation) in Alaska, ranking just behind its neighbor, Atna Peaks.[1] Because the mountain is almost entirely covered in 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.

Regal Mountain
Regal Mountain rises above the Regal Glacier
Highest point
Elevation13,845 ft (4,220 m)
Prominence4,345 ft (1,324 m)[1]
Isolation12 mi (19 km)
Listing
Coordinates61°44′39″N 142°51′55″W / 61.74417°N 142.86528°W / 61.74417; -142.86528
Geography
LocationWrangell-St. Elias National Park and Preserve, Alaska, U.S.
Parent rangeWrangell Mountains
Topo mapUSGS McCarthy C-5
Geology
Mountain typeEroded stratovolcano or shield volcano
Climbing
First ascentAugust 3, 1964 by Yasuichi Kitamura, Ryoichi Hasegawa, Masao Tanaka, and Shinichi Naito[2]
Easiest routeGlacier climb

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 edit

References edit

  • Richter, Donald H.; Danny S. Rosenkrans; Margaret J. Steigerwald (1995). Guide to the Volcanoes of the Western Wrangell Mountains, Alaska. USGS Bulletin 2072.
  • Winkler, Gary R. (2000). A Geologic Guide to Wrangell—Saint Elias National Park and Preserve, Alaska: A Tectonic Collage of Northbound Terranes. USGS Professional Paper 1616. 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. USGS Scientific Investigations Map 2877.
  1. ^ a b "Alaska 13,000-foot Peaks". Peakbagger.com. Retrieved 2007-03-10.
  2. ^ . Archived from the original on June 30, 2006. Retrieved 2007-03-10.

External links edit

regal, mountain, confused, with, mount, royal, disambiguation, eroded, stratovolcano, shield, volcano, wrangell, mountains, eastern, alaska, located, wrangell, saint, elias, national, park, about, east, mount, blackburn, second, highest, volcano, united, state. Not to be confused with Mount Royal disambiguation Regal Mountain is an eroded stratovolcano or shield volcano in the Wrangell Mountains of eastern Alaska It is located in Wrangell Saint Elias National Park about 19 mi 31 km east of Mount Blackburn the second highest volcano in the United States and southeast of the massive Nabesna Glacier Regal Mountain is the third highest thirteener a peak between 13 000 and 13 999 feet in elevation in Alaska ranking just behind its neighbor Atna Peaks 1 Because the mountain is almost entirely covered in 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 Regal MountainRegal Mountain rises above the Regal GlacierHighest pointElevation13 845 ft 4 220 m Prominence4 345 ft 1 324 m 1 Isolation12 mi 19 km ListingNorth America highest peaks 70thUS highest major peaks 52ndAlaska highest major peaks 16thCoordinates61 44 39 N 142 51 55 W 61 74417 N 142 86528 W 61 74417 142 86528GeographyLocationWrangell St Elias National Park and Preserve Alaska U S Parent rangeWrangell MountainsTopo mapUSGS McCarthy C 5GeologyMountain typeEroded stratovolcano or shield volcanoClimbingFirst ascentAugust 3 1964 by Yasuichi Kitamura Ryoichi Hasegawa Masao Tanaka and Shinichi Naito 2 Easiest routeGlacier climbSeveral 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 Contents 1 See also 2 References 3 External linksSee also edit nbsp North America portal nbsp United States portal nbsp Alaska portal nbsp Mountains portal nbsp Volcanoes portalList of mountain peaks of North America List of mountain peaks of the United States List of mountain peaks of Alaska List of volcanoes in the United StatesReferences editRichter Donald H Danny S Rosenkrans Margaret J Steigerwald 1995 Guide to the Volcanoes of the Western Wrangell Mountains Alaska USGS Bulletin 2072 Winkler Gary R 2000 A Geologic Guide to Wrangell Saint Elias National Park and Preserve Alaska A Tectonic Collage of Northbound Terranes USGS Professional Paper 1616 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 USGS Scientific 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 External links editRegal Mountain at Wikipedia s sister projects nbsp Definitions from Wiktionary nbsp Media from Commons nbsp News from Wikinews nbsp Quotations from Wikiquote nbsp Texts from Wikisource nbsp Textbooks from Wikibooks nbsp Resources from Wikiversity Retrieved from https en wikipedia org w index php title Regal Mountain amp oldid 1094892447, wikipedia, wiki, book, books, library,

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