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Black Butte Crater Lava Field

Vulcano a scudo · United States · 1478 m

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. · Foto: Photo by Lee Siebert, 2002 (Smithsonian Institution).
Tipo
Vulcano a scudo
Paese
United States
Regione
North America Volcanic Regions / Yellowstone-Snake River Hotspot Volcano Group
Altitudine
1478 m
Coordinate
43.185, -114.354
Ultima eruzione
-8180
Contesto tettonico
Rift zone / Continental crust (> 25 km)
Forma vulcanica
Shield
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

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.

Storia delle eruzioni

Riepilogo (VEI nel tempo)
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8180 BCE~8180 BCE · 1 eruzioni · VEI max. 08180 BCE8180 BCE8179 BCE8179 BCE8179 BCE

Cronologia dettagliata

  1. 8180 a.C. (±350 anni)VEI 0Stima geologica
    BCE 8180 – In corso
    Black Butte Crater

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