Item talk:Q59777
From geokb
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"name": "Postglacial eruptive history, geochemistry, and recent seismicity of Aniakchak volcano, Alaska Peninsula",
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"abstract": "Aniakchak is a Pleistocene to Holocene composite volcano of the Alaska\u2013Aleutian arc that suffered at least one caldera-forming eruption in postglacial time and last erupted in 1931. The oldest recognized postglacial eruption, Aniakchak\u00a0I, produced andesite ignimbrite ca. 9,500\u20137,500\u00a014C yr B.P. Subsequently, a vent northeast of the summit issued dacite\u2013rhyodacite magma ca. 7,000 14C yr B.P. mainly as the Black Nose Pumice falls. The ca.\u00a03,430 14C yr B.P. Aniakchak\u00a0II eruption produced rhyodacite plinian fall followed by rhyodacite and andesite ignimbrite extending \u226550\u00a0km to the Bering Sea and Pacific coasts and resulted in collapse of the 10-km-diameter caldera.\n\u00a0\nPostcaldera vents are mainly on the caldera ring-fracture system. The earliest extruded small dacite domes into a deep caldera lake and a lava flow on the northwest flank. Three basaltic andesite\u2013andesite tuff cones were constructed on the eastern caldera floor after catastrophic draining of the lake by ~200\u00a0m. Dacite\u2013andesite magmas issued from Vent Mountain and Half Cone starting as early as ~1,000 years ago. Plinian eruption at Half Cone ~400\u00a014C yr B.P. yielded widespread dacite Pink and overlying andesite Brown Pumice fall deposits. Strombolian eruption of basaltic andesite built Blocky Cone after Half Cone and most Vent Mountain activity. The most recent eruption, in 1931, yielded dacite\u2013rhyodacite tephra followed by relatively voluminous andesite tephra and ended with minor basaltic andesite.\n\u00a0\nCurrent indications of an active magmatic system include high 3He/4He of CO2-rich gas at intracaldera Surprise Lake, InSAR pattern of caldera floor subsidence, and episodic seismicity. The majority of earthquakes are long-period (LP) events. Epicenters for 135 (2009\u20132012; ML \u22642.1) define a bow-tie pattern elongated parallel to plate convergence. Hypocenters identify events14\u201328\u00a0km below sea level (bsl), few events 7\u201314\u00a0km bsl beneath the caldera, and events <10\u00a0km bsl concentrated under Vent Mountain. Recent seismicity is consistent with long-lived mush in the quiet zone, from which magma escapes to be stored ephemerally to within ~2.5\u00a0km bsl.\n\u00a0\nFuture volcanic activity of Aniakchak could include hydromagmatic explosions, possibly followed by effusion or strombolian eruption of basaltic andesite to Plinian eruption of dacite. Another voluminous eruption, such as Aniakchak II, is considered unlikely in the near future.",
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