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Black Rock Desert volcanic field

Black Rock Desert

Campo volcánico · United States · 1800 m

The Black Rock Desert volcanic field consists of a cluster of closely spaced small volcanic fields of Pleistocene-to-Holocene age in the Black Rock and Sevier deserts.  This view shows Utah's youngest known lava flow, the 660-year-old Ice Springs flow, which originated from a series of nested cinder and spatter cones.  The rim of Crescent Crater is at the right, with the symmetrical Pocket Crater at the left and Pavant Butte in the distance.  This tuff cone erupted through the waters of Pleistocene Lake Bonneville about 16,000 years ago.
The Black Rock Desert volcanic field consists of a cluster of closely spaced small volcanic fields of Pleistocene-to-Holocene age in the Black Rock and Sevier deserts. This view shows Utah's youngest known lava flow, the 660-year-old Ice Springs flow, which originated from a series of nested cinder and spatter cones. The rim of Crescent Crater is at the right, with the symmetrical Pocket Crater at the left and Pavant Butte in the distance. This tuff cone erupted through the waters of Pleistocene Lake Bonneville about 16,000 years ago. · Foto: Photo by Lee Siebert, 1996 (Smithsonian Institution). · Wikimedia Commons
Tipo
Campo volcánico
País
United States
Región
North America Volcanic Regions / Basin and Range Volcanic Province
Altitud
1800 m
Coordenadas
38.970, -112.500
Última erupción
1290
Contexto tectónico
Rift zone / Continental crust (> 25 km)
Forma volcánica
Cluster
Roca principal
Basalt / Picro-Basalt
Resumen geológico

The Black Rock Desert volcanic field consists of a group of closely spaced small Pleistocene-to-Holocene volcanic fields in the Black Rock and Sevier deserts of south-central Utah, at the eastern margin of the Great Basin. The Black Rock Desert field contains both Utah's youngest known rhyolite dome (400,000 years old) and its youngest eruptive vent, which produced the roughly 660-year-old Ice Springs lava flows. The broader volcanic field includes the smaller Deseret, Pavant, Kanosh, Tabernacle, Ice Spring, and northern Black Rock Desert fields. The Pavant Butte and Tabernacle Hill tuff cones were erupted about 16,000 and 14,000 years ago through the waters of glacial Lake Bonneville. Lava flows from the Ice Springs crater complex traveled about 4 km west and north, overlapping late-Pleistocene flows from Pavant Butte.

Resumen de Wikipedia

Resumen en inglés

The Black Rock Desert volcanic field in Millard County, Utah, is a cluster of several volcanic features of the Great Basin including Pahvant Butte, The Cinders, and Tabernacle Hill. The field's Ice Springs event was an explosive eruption followed by lava flows that were Utah's most recent volcanic activity. which overlapped the older flows of Pavant Butte.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1290~1290 · 1 erupciones · VEI máx. ?12901290129112911291

Línea de tiempo detallada

  1. 1290 (±150 años)VEI ?Estimación geológica
    1290 – En curso
    Ice Springs Craters

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.