Mount Dutton: Difference between revisions
imported>Volcanoguy removed Category:Mountains of Alaska; added Category:One-thousanders of the United States using HotCat |
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| coordinates = {{coord|55.168|N|162.272|W|format=dms|type:mountain_region:US|display=inline,title}} | | coordinates = {{coord|55.168|N|162.272|W|format=dms|type:mountain_region:US|display=inline,title}} | ||
| topo = <!-- [[United States Geological Survey|USGS]] McCarthy B-2 --> | | topo = <!-- [[United States Geological Survey|USGS]] McCarthy B-2 --> | ||
| formed_by = [[Aleutian subduction zone|Subduction zone]] [[volcanism]] | |||
| age = | |||
| type = [[Stratovolcano]] | | type = [[Stratovolcano]] | ||
| volcanic_arc = [[Aleutian Arc]] | | volcanic_arc = [[Aleutian Arc]] | ||
| last_eruption = Unknown | | last_eruption = Unknown | ||
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==Sources== | ==Sources== | ||
* [ | * [https://geopubs.wr.usgs.gov/dds/dds-40/ Volcanoes of the Alaska Peninsula and Aleutian Islands-Selected Photographs] | ||
* [http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Dutton Alaska Volcano Observatory] | * [http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Dutton Alaska Volcano Observatory] | ||
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[[Category:Mountains of Aleutians East Borough, Alaska]] | [[Category:Mountains of Aleutians East Borough, Alaska]] | ||
[[Category:Holocene stratovolcanoes]] | [[Category:Holocene stratovolcanoes]] | ||
[[Category:Quaternary Alaska]] | |||
{{AleutiansEastAK-geo-stub}} | {{AleutiansEastAK-geo-stub}} | ||
Latest revision as of 16:55, 15 November 2025
Template:Short description Template:Infobox mountain
Mount Dutton is a stratovolcano in the Aleutian Range of the U.S. state of Alaska, on the Alaska Peninsula. It is also the crash site of a World Airways DC-8.
Geography
Dutton lies just short of Script error: No such module "convert". from King Cove, a fishing headquarters for the locality.[1]
Geologic activity
Dutton is a highly glaciated volcano. Its summit is composed of a series of lava domes which form a complex stratovolcano. The mountain's recent history is marked by at least avalanche which removed andesitic lava flows and several lava domes from the flank of its body and swiftly cascaded westward and southward towards Belkofski Bay.[1]
Between 1984 and 1985, a series of earthquake swarms took place in the volcano's vicinity. Another swarm took place in the summer of 1988.[1]
See also
References
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- ↑ a b c Template:Cite gvp
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