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Welcome to Capulin Volcano National Monument!

Park History

Capulin Volcano is a cinder cone volcano that erupted into existence around 60,000 years ago. After its eruption ended, Capulin Volcano became extinct, although it was hardly the only volcano to erupt in this area. Capulin is part of the Raton-Clayton Volcanic Field (RCVF), which is an 8,000 square mile area of volcanic activity containing over 100 volcanoes and volcanic vents. Though there has been no volcanic activity in the RCVF for around 30,000 years, the field itself is considered dormant and could become active again, though it is unlikely to happen anytime soon.

The first volcanic eruptions in the Raton-Clayton Volcanic Field happened around 9 million years ago in the western portion of the volcanic field during what is known as the Raton phase of eruptions. The Raton phase lasted from around 9 million years ago to around 3.5 million years ago and consisted mainly of basaltic lava flows that formed the mesas near Raton, NM and the Red Mountain Rhyodacite that formed highly eroded volcanic domes. Some examples of volcanoes and lava flows that erupted during the Raton phase include Johnson Mesa, Fishers Peak Mesa, Mesa de Maya or Black Mesa, Red Mountain, the Pine Buttes, Palo Blanco Mountain, and Laughlin Peak.

After the Raton phase of eruptions, the volcanic field was dormant for around half a million years until volcanoes started erupting in the eastern portion of the RCVF during what is known as the Clayton phase of eruptions. The Clayton phase lasted from around 3 million years ago to around 2.25 million years ago and eruptions that happened during this period consisted of the highest volume of magma erupted during the different phases of volcanic activity in this area. Most of the eruptions consisted of basaltic cinder cones and lava flows and Basanite cinder cones, such as Rabbit Ear Mountain, Mount Dora, Mount Clayton, Jose Butte, and Robinson Peak. However, the eruption of Sierra Grande also happened during the Clayton phase. An unusual volcano, Sierra Grande consists of andesite lava flows and is the only volcano that erupted andesite in this area.

After the Clayton phase of eruptions in the Raton-Clayton Volcanic Field, there was another dormant period of around half a million years. After this dormant period, the most recent phase of eruptions in the volcanic field, known as the Capulin phase, began and lasted from around 1.7 million years ago to around 30,000 years ago. This phase included the eruption of Capulin Volcano and other basaltic cinder cones, basanites, and small fissure eruptions near the center of the volcanic field. Some examples of other volcanoes that erupted during the Capulin phase include Mud Hill, Horseshoe Crater, Carr Mountain, Emery Peak, Eagle Tail Mesa, Twin Mountain, Baby Capulin, and Purvine Mesa. Though Capulin was one of the more recent eruptions in the Raton-Clayton Volcanic Field at around 60,000 years ago, Twin Mountain, Baby Capulin, and Purvine Mesa all had more recent volcanic eruptions than Capulin.

Despite the fact that the volcanic activity here has been paused for around 30,000 years, other geologic activity is still ongoing in the area. The slow weathering and erosion of the volcanoes in northeastern New Mexico is constant and can be seen in the furrows or 'wrinkles' extending down the sides of the volcanoes here. Capulin Volcano itself is estimated to have lost around 100 feet of elevation in the 60,000 years since the eruption built the cinder cone. -- Source Google



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