Belkofski 23 mi (37 km) SW King Cove 30 mi (48 km) SW Cold Bay 36 mi (58 km) SW Nelson Lagoon 49 mi (78 km) NE Anchorage 590 mi (950 km) NE
DESCRIPTION
From Miller and others (1998) [1]: "Pavlof Volcano is a largely snow-covered, cone-shaped mountain with a high ridge extending to the southwest towards the rim of Emmons Lake Caldera. The volcano is approximately 7 km in diameter and has active vents on the north and east sides close to the summit [2]. It is situated high on the northeastern flank of Emmons Lake Caldera along a northeast-trending alignment of vents that includes Pavlof Sister, and several intracaldera cones [3]. The stratovolcano is relatively undissected and is mostly Holocene in age. Pavlof lies within the Shumagin seismic gap [4]." The name Pavlof comes from Russian, translating to "Paul" or "Saint Paul". This volcano name was first published as "Pavlovskoi Volcan" by Captain Lutke in 1836.
Geology of Pavlof Volcano and vicinity, Alaska, 1955 Kennedy, G. C., and Waldron, H. H., 1955, Geology of Pavlof Volcano and vicinity, Alaska: in Investigations of Alaskan volcanoes, U.S. Geological Survey Bulletin 1028-A, 19 p., 1 sheet, scale 1:100,000. full-text PDF : 744 KB plate 3 PDF : 9.1 MB
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Miller, T. P., McGimsey, R. G., Richter, D. H., Riehle, J. R., Nye, C. J., Yount, M. E., and Dumoulin, J. A., 1998, Catalog of the historically active volcanoes of Alaska: U.S. Geological Survey Open-File Report 98-0582, 104 p.
McNutt, S. R., Miller, T. P., and Taber, J. J., 1991, Geological and seismological evidence of increased explosivity during the 1986 eruptions of Pavlof Volcano, Alaska: Bulletin of Volcanology, v. 53, n. 2, p. 86-98.
Kennedy, G. C., and Waldron, H. H., 1955, Geology of Pavlof Volcano and vicinity, Alaska: in Investigations of Alaskan volcanoes, U.S. Geological Survey Bulletin 1028-A, 19 p., 1 sheet, scale 1:100,000.
