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Aden Crater is a small shield volcano located in Doña Ana County, about 25 miles (40 km) southwest of Las Cruces, New Mexico. [3] It is located in the northwest part of the Aden-Afton basalt field, which is part of the central area of the Potrillo volcanic field.
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]
Capulin Volcano National Monument is a U.S. National Monument located in northeastern New Mexico that protects and interprets an extinct cinder cone volcano and is part of the Raton-Clayton volcanic field. A paved road spirals gradually around the volcano and visitors can drive up to a parking lot at the rim of the extinct volcano.
Vulcan is a spatter cone volcano, formed primarily by lava fountains that were active in the central vent and in smaller vents on flanks of the cone. These flank vents formed the arches and caves seen today. It is believed to have last erupted around 150,000 years ago.
Mount Taylor, seen from the South Map of Mount Taylor Volcanic Field in central New Mexico (modified from Crumpler, 1980).. Mount Taylor (Navajo: Tsoodził, Navajo pronunciation: [tsʰòːtsɪ̀ɬ] means "The Great Mountain" [3]) is a dormant stratovolcano in northwest New Mexico, northeast of the town of Grants. [4]
On Sunday, officials raised the volcano threat level to "Yellow Phase 3," which calls for those who live nearest to the volcano — including the 2,000 residents of Santiago Xalitzintla — to ...
Cabezon Peak is the solidified core of a volcano that erupted 2.658 ± 0.032 million years ago, based on argon-argon dating. The eruption at this volcano likely began with lava fountains from the vent, which built up a scoria cone. Lava later ponded in the interior of the cone, solidifying into a massive plug.
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 ...