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The Carrizozo volcanic field is a monogenetic volcanic field located in New Mexico, US. The volcanic field consists of two lava flows, the Broken Back flow and the Carrizozo lava flow (Carrizozo Malpais), the second youngest in New Mexico. [5] Both lava flows originated from groups of cinder cones. The Broken Back flow is approximately 16 ...
Zuni-Bandera volcanic field (also known as Bandera lava field, Grants Malpais and Malpais volcanic field) is a volcanic field located in the state of New Mexico, United States. [1] The volcanic field has been considered for geothermal exploitation. [2] It is on the Trails of the Ancients Byway, one of the designated New Mexico Scenic Byways. [3]
The field is part of the Jemez Lineament, a zone of young volcanic fields stretching from central Arizona to northeastern New Mexico. Ar-Ar dating of rock from the Red Hill volcanic field reveals that it was erupted in two pulses, from 7.9-5.2 million years ago and from 2.5 to 0.071 Mya. The older activity was along a narrow zone roughly ...
El Malpais has many lava tubes; two are open to explore (unguided) with a free caving permit, available at NPS-staffed facilities. The two caves currently accessible by permit are Giant Ice in the Big Tubes area, and Lava Bomb in the Hoya de Cibola area. The Junction Bridge lava tube ia also accessible as part of the El Calderon trail. [7]
The Valles Caldera (or Jemez Caldera) is a 13.7-mile (22.0 km) wide volcanic caldera in the Jemez Mountains of northern New Mexico. [1] Hot springs, streams, fumaroles, natural gas seeps, and volcanic domes dot the caldera landscape. [4]
Bandera Volcano Ice Cave, also known as Zuni Ice Cave, is a lava tube cave in New Mexico with an internal temperature significantly less than above-ground summertime ambient temperature; it contains perennial ice. [1] The inside temperatures can fluctuate between −1 and 10 °C (31 and 50 °F). Some areas of the ice cave never reach above ...
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