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The Global Volcanism Program has no activity reports for Takawangha.
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Takawangha is a 1449-m-high, youthful volcano with an ice-filled caldera on northern Tanaga Island, near the western end of the Andreanof Islands. Takawangha lies across a saddle from historically active Tanaga volcano to the west; older, deeply eroded volcanoes lie adjacent to Takawangha on the east. The summit of the dominantly basaltic to basaltic-andesite volcano is largely ice covered, with the exception of five Holocene craters that during the last few thousand years produced explosive eruptions and lava flows that reached the lower flanks of the volcano. No historical eruptions are known from Takawangha, although radiocarbon dating indicates explosive eruptions have occurred within the past several hundred years.
Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|1550 (?)||Unknown||Confirmed||Radiocarbon (uncorrected)|
The Global Volcanism Program has no synonyms or subfeatures listed for Takawangha.
|Broad Takawangha volcano (left), seen here from the east, is a 1449-m-high, youthful stratovolcano on northern Tanaga island with an ice-filled caldera. Numerous small post-caldera tephra cones are located within the caldera, as well as on its rim and flanks. The youngest cones are some of those in the caldera. No historical eruptions are known from Takawangha, in contrast to sharp-peaked Tanaga volcano (right), which occupies the NW tip of Tanaga Island.
Photo by Tom Edgarton, 1986 (U.S. Fish and Wildlife Service).
|The broad Takawangha volcano is seen looking east from the summit of East Tanaga. The 1449-m-high, youthful volcano lies across a saddle from historically active Tanaga volcano to the west. The summit of the dominantly basaltic to basaltic-andesite volcano is largely ice covered, with the exception of five Holocene craters that during the last few thousand years produced explosive eruptions and lava flows that reached the lower flanks of the volcano.
Photo by Michelle Coombs, 2003 (Alaska Volcano Observatory, U.S. Geological Survey).
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. 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.
Coombs M L, McGimsey R G, Browne B L, 2007a. Preliminary volcano-hazard assessment for the Tanaga volcanic cluster, Tanaga Island, Alaska. U S Geol Surv, Sci Invest Rpt, 2007-5094: 1-35.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Motyka R J, Liss S A, Nye C J, Moorman M A, 1993. Geothermal resources of the Aleutian arc. Alaska Div Geol Geophys Surv, Prof Rpt, no 114, 17 p and 4 map sheets.
Smith R L, Shaw H R, Luedke R G, Russell S L, 1978. Comprehensive tables giving physical data and thermal energy estimates for young igneous systems of the United States. U S Geol Surv Open-File Rpt, 78-925: 1-25.
Wood C A, Kienle J (eds), 1990. Volcanoes of North America. Cambridge, England: Cambridge Univ Press, 354 p.