Report on Korovin (United States) — June 1998
Bulletin of the Global Volcanism Network, vol. 23, no. 6 (June 1998)
Managing Editor: Richard Wunderman.
Korovin (United States) Low eruption plume seen in June, dusting of ash in Atka
Please cite this report as:
Global Volcanism Program, 1998. Report on Korovin (United States). In: Wunderman, R. (ed.), Bulletin of the Global Volcanism Network, 23:6. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199806-311161.
52.381°N, 174.166°W; summit elev. 1518 m
All times are local (unless otherwise noted)
At about 1000 on 30 June, the Alaska Volcano Observatory (AVO) received a report of an eruption at Korovin from an observer in the village of Atka, near the volcano. The crew of a Coast Guard C-130 airplane confirmed that a low-level eruption plume had risen to almost 5 km above sea level by 1030, and late in the afternoon a pilot reported the plume at 9 km. The low-level ash-and-steam plume was not visible on satellite imagery due to meteorological clouds. Local winds at the time were light and to the SSW. A dusting of ash was reported in Atka. Poor weather on 1 July prohibited both direct and satellite observations.
Korovin volcano is located on the north end of Atka Island in the central Aleutians (figure 1), 538 km W of Dutch Harbor. It is 21 km N of the village of Atka, which has a population of about 100. The last reported eruption was in March 1987. AVO does not maintain seismic monitoring equipment on Atka Island.
Geologic Background. Korovin, the most frequently active volcano of the large volcanic complex at the NE tip of Atka Island, contains a 1533-m-high double summit with two craters located along a NW-SE line. The NW summit has a small crater, but the 1-km-wide crater of the SE cone has an unusual, open cylindrical vent of widely variable depth that sometimes contains a crater lake or a high magma column. A fresh-looking cinder cone lies on the flank of partially dissected Konia volcano, located on the SE flank. The volcano is dominantly basaltic in composition, although some late-stage dacitic lava flows are present on both Korovin and Konia.
Information Contacts: Alaska Volcano Observatory (AVO), a cooperative program of a) U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667, USA (URL: http://www.avo.alaska.edu/), b) Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775-7320, USA, and c) Alaska Division of Geological & Geophysical Surveys, 794 University Ave., Suite 200, Fairbanks, AK 99709, USA.