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There are no activity reports for Behm Canal-Rudyerd Bay.
Available Weekly Reports
There are no Weekly Reports available for Behm Canal-Rudyerd Bay.
There are no Holocene eruptions known for Behm Canal-Rudyerd Bay. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.
Berg H C, Elliott R L, Koch R D, 1988. Geologic map of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska. U S Geol Surv Map, I-1807, 1:250,000 scale and 27 p text.
Buddington A F, Chapin T, 1929. Geology and mineral deposits of southeastern Alaska.. U S Geol Surv Bull, 800: 278-279.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Wanek A A, Callahan J E, 1971. Geologic reconnaissance of a proposed powersite at Lake Grace, Revillagigedo Island southeastern Alaska. U S Geol Surv Bull, 1211-E: 1-24.
Wood C A, Kienle J (eds), 1990. Volcanoes of North America. Cambridge, England: Cambridge Univ Press, 354 p.
Numerous basaltic cinder cones and lava flows occur in the panhandle of SE Alaska on both sides of Behm Canal, which divides Revillagigedo Island from the mainland. The lava flows, which are locally columnar-jointed, overlie glacial-fluvial sediments and granitic gneisses of the Coast Mountains and are located on the east and SE sides of Revillagigedo Island and at Rudyerd Bay across Behm Canal to the east. Most exposures are on SE Revillagigedo Island, but outcrops also occur on the mainland east of Behm Canal at the southern end of Punchbowl Cove at Rudyerd Bay. Undisturbed cinder cones and lava-flow surfaces at Painted Peak on SE Revillagigedo Island and elsewhere indicated that most of the activity was postglacial (Brew, in Wood and Kienle 1990). Pumice, lapilli, and ash deposits locally cover parts of glaciated ridge tops. Lava flows at the outlet of Lake Grace near Behm Canal on the eastern side of Revillagigedo Island were considered to be of late-Pleistocene or Holocene age (Wanek and Callahan 1971). Minor andesitic and trachyandesitic flows are also present.