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Wapi Lava Field

Gunung api perisai · United States · 1597 m

The dramatic Kings Bowl rift cutting diagonally across the top of the photo produced a small 6-sq-km lava field about 2250 years ago immediately north of the much larger Wapi lava field.  Kings Bowl itself is the small elongated crater on the right-center side of the rift in this photo; it formed during a phreatic explosion that deposited lighter-colored tephra to the east (upper right).  The massive Wapi lava field, located out of view south (right) of Kings Bowl, covers an area of about 325 km2 and originated from Pillar Butte, a small shield volcano.
The dramatic Kings Bowl rift cutting diagonally across the top of the photo produced a small 6-sq-km lava field about 2250 years ago immediately north of the much larger Wapi lava field. Kings Bowl itself is the small elongated crater on the right-center side of the rift in this photo; it formed during a phreatic explosion that deposited lighter-colored tephra to the east (upper right). The massive Wapi lava field, located out of view south (right) of Kings Bowl, covers an area of about 325 km2 and originated from Pillar Butte, a small shield volcano. · Foto: Photo by Susan Sakimoto (NASA, courtesy of Scott Hughes, Idaho State University). · Wikimedia Commons
Tipe
Gunung api perisai
Negara
United States
Wilayah
North America Volcanic Regions / Yellowstone-Snake River Hotspot Volcano Group
Ketinggian
1597 m
Koordinat
42.886, -113.217
Letusan terakhir
-300
Kondisi tektonik
Rift zone / Continental crust (> 25 km)
Bentuk lahan
Shield
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

The Wapi Lava Field, SE of the Craters of the Moon, covers about 325 km2, and consists of a low shield volcano formed during an eruption around 300 BCE that produced ~6 km3 of pahoehoe lava flows. The mass of layered lava flows and agglutinates forming the high point of the lava shield is named Pillar Butte. The vent area lies along the Great Rift of the Craters of the Moon and consists of five major and six minor vents covering an area of 0.5 km2. The largest of the vents contains several pit craters truncating lava lakes that filled the crater. The small King's Bowl rift immediately to the north formed at about the same time along a central eruptive fissure flanked by two parallel non-eruptive fissures. This eruption also produced a phreatic explosion that created Kings Bowl, an 80-m-long, 30-m-deep explosion crater. Split Butte maar to the west is partially overlapped by Wapi flows.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
300 BCE~300 BCE · 1 letusan · VEI maks. 2300 BCE300 BCE299 BCE299 BCE299 BCE

Garis waktu rinci

  1. 300 SMVEI 2Perkiraan geologi
    BCE 300 – Berlangsung
    Kings Bowl Rift, Wapi Lava Field

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.