HR: 1330h
AN: V42B-0342    [PDF]
TI: Black Peak Caldera, Alaska: Preliminary Investigations of the $\sim$4600 BP Caldera-forming Eruption and Subsequent Post-caldera Activity
AU: * McGimsey, R G
EM: mcgimsey@usgs.gov
AF: U.S. Geological Survey, Alaska Volcano Observatory 4200 University Drive, Anchorage, AK 99508
AU: Neal, C A
EM: tneal@usgs.gov
AF: U.S. Geological Survey, Alaska Volcano Observatory 4200 University Drive, Anchorage, AK 99508
AU: Adleman, J A
EM: ftjna@uaf.edu
AF: Department of Geology and Geophysics, University of Alaska Fairbanks, Fairbanks, AK 99775
AU: Larsen, J F
EM: faust@gi.alaska.edu
AF: Department of Geology and Geophysics, University of Alaska Fairbanks, Fairbanks, AK 99775
AU: Ramsey, M
EM: ramsey@ivis.eps.pitt.edu
AF: Department of Geology and Planetary Science, University of Pittsburgh, Pittsburgh, PA 15260
AB: Black Peak Caldera is a 4-km-diameter, circular crater located on the Alaska Peninsula midway between Aniakchak and Veniaminof Volcanoes, approximately 45 km south-southwest of the community of Port Heiden and 730 km southwest of Anchorage. The caldera truncates a highly altered volcanic edifice that consists largely of lava domes, minor lava flows, and volcaniclastics. New radiocarbon dating of soils beneath the ash-flow deposit confirm earlier dating and place the age of the caldera-forming event at approximately 4600 14C yrs BP. Climactic fall deposits from this eruption form a prominent, crystal-rich, regional tephra horizon informally referred to as the 'salt and pepper ash.' Coeval pyroclastic flow deposits fill the two major drainages around the caldera to a depth of up to 100 m, and extend at least 10 km from the caldera rim. Deposits consist of a lower, highly pumiceous, crystal-rich dacite flow unit capped by a conspicuously oxidized, lithic-rich unit that is less aerially extensive. We estimate the bulk volume of the eruption to be less than 10-20 km3. Post-caldera eruptions at Black Peak have largely consisted of viscous, crystal-rich, hornblende-bearing dacite lavas forming a coalescing field of steep-sided, blocky domes and at least one coulee that fill much of the caldera. No coarse tephra fall deposits related to these eruptions have been found. Fine-grained, highly altered ash fall deposits, possibly related to dome emplacement, form a thick, monotonous sequence on the caldera rim and immediately overlying the ash flow in exposures near the caldera. This suggests that the dome eruptions closely followed caldera formation. Several domes collapsed over the eastern rim of the caldera to form coarse block and ash avalanche fans that extend ~1.5 km down Red Bluff Creek. Radiocarbon dating of an overlying soil indicates an age of $>$500 14C yrs BP for these avalanches. There are no reports of eruptive activity at Black Peak in historic time (approximately 1750-present). A USGS report from 1926 noted both carbon dioxide and hydrogen sulfide springs within the caldera. With the exception of a few areas of diffuse bubbling, we were unable to relocate significant sites of degassing. An area of pervasive sulfur deposition against the west inner caldera wall is not thermally active at present. Radiometer measurements of Purple Lake showed rapid fluctuations due to possible overturning. Terraces, dry channels, and lake-clay exposures indicate that at least two of the several small lakes presently inside the caldera once formed a larger body of water.
DE: 1749 Volcanology, geochemistry, and petrology
SC: Volcanology, Geochemistry, Petrology [V]
MN: 2003 Fall Meeting