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Black Butte Crater Lava Field

순상화산 · United States · 1478m

One of a series of interlocking craters forming the complex summit of Black Butte, the vent of the Shoshone lava field, is seen here from the summit of the butte.  The broad, low Shoshone shield volcano fed voluminous lava flows that traveled a small distance north towards the Mount Bennett Hills in the background, but the bulk of the flows traveled initially south and then west for a total distance of 60 km.  The Shoshone lava field, erupted about 10,000 years ago, is the westernmost of the young volcanic fields of the Snake River Plain.
One of a series of interlocking craters forming the complex summit of Black Butte, the vent of the Shoshone lava field, is seen here from the summit of the butte. The broad, low Shoshone shield volcano fed voluminous lava flows that traveled a small distance north towards the Mount Bennett Hills in the background, but the bulk of the flows traveled initially south and then west for a total distance of 60 km. The Shoshone lava field, erupted about 10,000 years ago, is the westernmost of the young volcanic fields of the Snake River Plain. · 사진: Photo by Lee Siebert, 2002 (Smithsonian Institution).
화산 유형
순상화산
국가
United States
지역
North America Volcanic Regions / Yellowstone-Snake River Hotspot Volcano Group
해발
1478m
좌표
43.185, -114.354
마지막 분화
-8180년
판구조 환경
Rift zone / Continental crust (> 25 km)
화산 지형
Shield
주요 암석
Basalt / Picro-Basalt
지질학적 요약

The Black Butte Crater lava field is the westernmost of the young lava fields of the Eastern Snake River Plain. It lies north of Twin Falls, Idaho, and created an L-shaped lava flow 2-5 km wide that extends 60 km S and then west. A single radiocarbon age of 10,130 +/- 350 years BP was obtained for lava flows here (Kuntz et al., 1986). Black Butte Crater caps a lava shield at the NE end of the flow field. The vent area contains a complex lava lake that forms a six-part flower-petal like depression with steep walls up to 30 m high that covers an area of 2 km2. A lava tube and channel system extending 5 km SE of the crater displays both roofed and collapsed portions. The Big Wood and Little Wood rivers follow the northern and southern margins of the distal part of the lava flow, respectively. The voluminous flow diverted the river channels so that they now join 40 km W of their former confluence.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
8180 BCE~8180 BCE · 1건 · 최고 VEI 08180 BCE8180 BCE8179 BCE8179 BCE8179 BCE

상세 타임라인

  1. 기원전 8180년 (±350년)VEI 0지질학적 추정
    BCE 8180 ~ 진행 중
    Black Butte Crater

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