Belknap Crater
Belknap
순상화산 · United States · 2094m

- 화산 유형
- 순상화산
- 국가
- United States
- 지역
- North America Volcanic Regions / High Cascades Volcanic Arc
- 해발
- 2094m
- 좌표
- 44.285, -121.842
- 마지막 분화
- 475년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Shield
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The Belknap Crater area near McKenzie Pass in Oregon, north of the Three Sisters volcanoes, was the source of one of the largest concentrations of youthful volcanism in the Cascade Range. The basaltic to basaltic andesite Belknap shield volcano, topped by the Belknap Crater pyroclastic cone and the Little Belknap shield volcano immediately to the east, have produced widespread late Holocene lava flows on all sides, much of which took place between about 3,000 and 1,500 years ago. Eruptions from the NE base of Belknap crater produced lava flows that traveled 15 km W into the McKenzie River valley.
Wikipedia 요약
영어 요약Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness. Belknap is not forested and most of its lava flows are not vegetated, though there is some wildlife in the area around the volcano, as well as a number of tree molds formed by its eruptive activity.
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분화 이력
상세 타임라인
- 475년 (±215년)VEI 2지질학적 추정475 ~ 진행 중Belknap Crater
- 기원전 685년 (±50년)VEI 2지질학적 추정BCE 685 ~ 진행 중South Belknap and Twin Craters
- 기원전 1071년 (±241년)VEI 0지질학적 추정BCE 1071 ~ 진행 중Little Belknap
- 기원전 5050년VEI ?지질학적 추정BCE 5050 ~ 진행 중
외부 링크
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