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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.
- 1,565 to 1,730 m (5,135 to 5,676 ft)
- volcanic field
- 3250 BCE ± 500 years
The 75-km- (50-mi-) long Carrizozo lava flow is located in south-central New Mexico in the Tularose Basin. Eruption began approximately 5,000 years ago, and after two to three decades at a relatively low effusion rate, 4.3 km 3 (1 mi 3 ) of basalt lava covered 330 km 2 (130 mi 2 ) of land.
Geological Summary. The massive Carrizozo lava flow, which traveled 75 km down the Tularosa Basin of south-central New Mexico, is one of Earth's longest known Holocene lava flows. The youthful-looking flow originated from a broad low basaltic shield on the floor of the Tularosa Basin, east of the Rio Grande Rift, topped by Little Black Peak, a ...
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Carrizozo lava flow field. Location: 33° 20' N to 33° 53' N, 106° W, Lincoln County. Type: Basaltic lava flow. Age: Holocene, ~5,000 years. Significance: One of the largest volume young (morphologically preserved) lava flows on Earth. Composition: Between alkalic and tholeiitic basalt. Geological Overview.
Carrizozo Lava Flow Wilderness Study Area. The Carrizozo Lava Flow WSA is located in central New Mexico. This lava flow is believed to be one of the most recent lava flows in the continental United States, dating back 1,500 years. This is a flat plain but a rugged landscape nonetheless.
The Carrizozo Malpais are a lava flow that formed by magma (molten rock) pouring out of a small crack in the earth's surface in a "Hawaiian-style" volcanic eruption. In Hawaii today, this type of eruption is very passive and is typically characterized by lava pouring from a small vent, and then travelling either across the earth's surface or ...
Mar 22, 2024 · Carrizozo Volcano. Updated: Mar 22, 2024 19:53 GMT - 52 seconds ago. The massive Carrizozo lava flow is one of Earth's longest known lava flows that were erupted in the past 10,000 years. The basalt flow is 50 m thick, 75 km long, 1-5 km wide and was mainly fed by lava tubes.
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