Report on Veniaminof (United States) — August 1995
Bulletin of the Global Volcanism Network, vol. 20, no. 8 (August 1995)
Managing Editor: Richard Wunderman.
Veniaminof (United States) Small steam plumes and hot spots on satellite images
Please cite this report as:
Global Volcanism Program, 1995. Report on Veniaminof (United States). In: Wunderman, R (ed.), Bulletin of the Global Volcanism Network, 20:8. Smithsonian Institution. https://dx.doi.org/10.5479/si.GVP.BGVN199508-312070.
56.17°N, 159.38°W; summit elev. 2507 m
All times are local (unless otherwise noted)
Clouds frequently obscured the volcano in July and August, preventing ground and satellite observations. Observers in Perryville (~30 km S of Veniaminof) got good views on 13 and 27 July, and reported light steaming on both days. On 28 July a weak hot spot centered on Veniaminof was noted on an AVHRR image. Perryville residents reported clear skies but no evidence of activity on the morning of 4 August, and AVHRR satellite images on 4 and 5 August showed no hot spot. Perryville residents saw a small steam plume on 9 August, a small steam plume and "smoke" during the week of 12-18 August, and a small steam plume again during 19-25 August. AVHRR satellite images on 14 and 21 August showed no hot spots. Another AVHRR image from late on 31 August showed a possible steam plume ~50 km long blowing NW of Veniaminof. The hot spot was ~15°C warmer than the surrounding features (probably ice and snow near the summit).
Geologic Background. Massive Veniaminof volcano, one of the highest and largest volcanoes on the Alaska Peninsula, is truncated by a steep-walled, 8 x 11 km, glacier-filled caldera that formed around 3700 years ago. The caldera rim is up to 520 m high on the north, is deeply notched on the west by Cone Glacier, and is covered by an ice sheet on the south. Post-caldera vents are located along a NW-SE zone bisecting the caldera that extends 55 km from near the Bering Sea coast, across the caldera, and down the Pacific flank. Historical eruptions probably all originated from the westernmost and most prominent of two intra-caldera cones, which rises about 300 m above the surrounding icefield. The other cone is larger, and has a summit crater or caldera that may reach 2.5 km in diameter, but is more subdued and barely rises above the glacier surface.
Information Contacts: Alaska Volcano Observatory (AVO), a cooperative program of a) U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667 USA, 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.