그리그산
Griggs
성층화산 · United States · 2317m

- 화산 유형
- 성층화산
- 국가
- United States
- 지역
- 북아메리카 / Alaska Peninsula Volcanic Arc
- 해발
- 2317m
- 좌표
- 58.354, -155.092
- 마지막 분화
- -1790년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The summit of Mount Griggs towers above Knife Creek on the NE side of the Valley of Ten Thousand Smokes. The volcano is offset west of the NE-trending alignment of volcanoes in the Katmai area. The broad stratovolcano, formerly known as Knife Peak, consists of a late-Pleistocene edifice with glacial valleys on the north that was truncated on its SW side by an early Holocene collapse. A Holocene volcano was subsequently constructed within the 1.5-km-wide scarp left following a large SW-flank debris avalanche. Nested cones with three concentric craters mostly fill the scarp, and thick, blocky lava flows cover the SW flanks below the collapse scarp. In contrast to the more silicic centers of the Katmai area along the crest of the range, lava flows from Griggs are dominantly andesitic in composition, and dacitic lava flows are uncommon. No eruptions have been observed, but noisy fumarolic jets near the summit can be heard from the valley floor.
Wikipedia 요약
영어 요약Mount Griggs, formerly known as Knife Peak Volcano, is a stratovolcano, which lies 10 km behind the volcanic arc defined by other Katmai group volcanoes. Although no historic eruptions have been reported from Mount Griggs, vigorously active fumaroles persist in a summit crater and along the upper southwest flank. The fumaroles on the southwest flank are the hottest, and some of the flank fumaroles can roar so loudly that they can be heard from the valley floor. The slopes of Mount Griggs are heavily mantled by fallout from the 1912 eruption of Novarupta volcano. The summit consists of three concentric craters, the lowest and largest of which contains a recent summit cone topped by two craters. The volume of the volcanic edifice is estimated at 25 cubic kilometers (6.0 cu mi). Isotopic analysis indicates that the source of Griggs' magma is distinct from the other Katmai volcanoes.
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분화 이력
상세 타임라인
- 기원전 1790년 (±40년)VEI ?지질학적 추정BCE 1790 ~ 진행 중
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