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Mount Spurr information


Mount Spurr
Mount Spurr from the south
Highest point
Elevation11,070 ft (3,370 m)[1][2]
Prominence585 m (1,919 ft)[3]
Parent peakMount Torbert[3]
ListingMountains of Alaska
Coordinates61°17′59″N 152°15′05″W / 61.29972°N 152.25139°W / 61.29972; -152.25139[4]
Naming
Native nameK'idazq'eni (Tanaina)
Geography
Mount Spurr is located in Alaska
Mount Spurr
Mount Spurr
Kenai Peninsula Borough, Alaska, United States
Parent rangeTordrillo Mountains, Alaska Range
Topo mapUSGS Tyonek B-7
Geology
Age of rock< 10,000 years
Mountain typeStratovolcano
Volcanic arc/beltAleutian Arc
Last eruptionJune to September 1992[1]
Climbing
First ascent1960[3]

Mount Spurr (Dena'ina: K'idazq'eni) is a stratovolcano in the Aleutian Arc of Alaska, named after United States Geological Survey geologist and explorer Josiah Edward Spurr, who led an expedition to the area in 1898. The Alaska Volcano Observatory (AVO) currently rates Mount Spurr as Level of Concern Color Code Green.[1] The mountain is known aboriginally by the Dena'ina Athabascan name K'idazq'eni, literally 'that which is burning inside'.[5]

Mount Spurr, the highest volcano of the Aleutian Arc, is a large lava dome constructed at the center of a roughly 5 km-wide horseshoe-shaped caldera that is open to the south. The volcano lies 80.87 miles west of Anchorage and NE of Chakachamna Lake. The caldera was formed by a late-Pleistocene or early Holocene debris avalanche and associated pyroclastic flows that destroyed an ancestral Spurr volcano. The debris avalanche traveled more than 15.5 miles to the SE, and the resulting deposit contains blocks as large as 100m in diameter. Several ice-carved post-caldera domes lie in the caldera. Present Mt. Spurr is the highest of the post-caldera. This regrown summit peak of Spurr experienced a heating event in 2004 which created a small crater lake. By 2008, the summit crater had cooled enough to have begun to have accumulated significant amounts of snow again. The youngest post-caldera dome, Crater Peak (2309m, 7575 ft), formed at the breached southern end of the caldera about 3.2 km south of Spurr, has been the source of about 40 identified Holocene tephra layers. Spurr's two historical eruptions, from Crater Peak in 1953 and 1992, deposited ash on the city of Anchorage. Crater Peak has a summit crater that is itself slightly breached along the south rim; the north wall of the crater exposes the truncated remains of an older dome or lava lake. Before the 1992 eruption, a small crater lake occupied the bottom of Crater Peak's crater.

As with other Alaskan volcanoes, the proximity of Spurr to major trans-Pacific aviation routes means that an eruption of this volcano can significantly disrupt air travel. Volcanic ash can cause jet engines to fail.[6]

  1. ^ a b c Cite error: The named reference avo was invoked but never defined (see the help page).
  2. ^ "Topographic map of Mount Spurr". opentopomap.org. Retrieved 2023-05-22.
  3. ^ a b c "Mount Spurr". Bivouac.com. Retrieved 2008-09-20.
  4. ^ "Mount Spurr". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-03-06.
  5. ^ Kari, James (2007). "Dena'ina Topical Dictionary". International Journal of American Linguistics. 75 (1). Fairbanks: Alaska Native Language Center. doi:10.1086/598210.
  6. ^ Boeing Company. "Volcanic Ash Avoidance". Retrieved 2013-06-13.

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