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Location map of Cleveland volcano, Alaska (image: Janet Schaefer, Alaska Volcano Observatory / Alaska Division of Geological & Geophysical Surveys)
Location map of Cleveland volcano, Alaska (image: Janet Schaefer, Alaska Volcano Observatory / Alaska Division of Geological & Geophysical Surveys)
Latest news:
Tuesday, May 08, 2012
Based on analyses of satellite images, AVO reported on 4 May that the small lava dome recently emplaced in Cleveland's summit crater had been destroye... [more]
Thursday, May 03, 2012
Elevated surface temperatures were detected over Cleveland in satellite imagery during 25-29 April and possibly on 30 April.
Observations showe... [more]


Cleveland volcano

stratovolcano 1730 m (5,676 ft)
Alaska, 52.83°N / -169.94°W
Current status: minor activity or eruption warning (3 out of 5)
Cleveland webcams / live data
last update: 8 May 2012 (small explosions, destruction and re-growth of small lava dome)
Typical eruption style: Explosive
Cleveland volcano eruptions: 1893, 1897, 1929(?), 1932, 1938, 1944, 1951(?), 1953(?), 1975(?), 1984, 1985(?), 1986, 1987, 1989(?), 1994, 2001, 2006, 2008, 2010, 2011
The beautifully symmetrical Mount Cleveland stratovolcano forms the western half of the uninhabited Chuginadak Island in the eastern Aleutians, connected to the eastern half of the island by a narrow isthmus. It is one of the regions most active volcanoes, but at present has no seismic network. Monitoring of its activity is largely based on satellite observation.

Background:

The 1730-m-high Mount Cleveland has the native name of Chuginadak, referring to the Aleut goddess of fire, who was thought to reside on the volcano. Numerous large lava flows descend the steep-sided flanks of the volcano.

It is possible that some 18th to 19th century eruptions attributed to Carlisle should be ascribed to Cleveland (Miller et al., 1998). In 1944 Cleveland produced the only known fatality from an Aleutian eruption. Recent eruptions from Mount Cleveland have been characterized by short-lived explosive ash emissions, at times accompanied by lava fountaining and lava flows down the flanks. In February, 2001, Cleveland had 3 explosive events that produced ash clouds as high as 12 km (39,000 ft) above sea level. That eruption also produced a rubbly lava flow and hot avalanche that reached the sea.
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Sources: AVO/USGS, Smithsonian Institution



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