Logo link to homepage

Global Volcanism Program | Image GVP-10088

The lava flow descended the SW flank of Pico de Orizaba is about 110 m thick and up to 1.3 km wide at its terminus 5.5 km from the summit, and.  has at least eight individual flow lobes. A portion of the flow that was diverted by topography to the west can be seen half-way up the flank. The smaller peak on the lower SW flank to the left of the lava flow is Cerro Colorado, a less than 90,000-year-old lava dome. Photo by Gerardo Carrasco-Núñez, 2002 (Universidad Nacional Autónoma de México).

The lava flow descended the SW flank of Pico de Orizaba is about 110 m thick and up to 1.3 km wide at its terminus 5.5 km from the summit, and. has at least eight individual flow lobes. A portion of the flow that was diverted by topography to the west can be seen half-way up the flank. The smaller peak on the lower SW flank to the left of the lava flow is Cerro Colorado, a less than 90,000-year-old lava dome.

Photo by Gerardo Carrasco-Núñez, 2002 (Universidad Nacional Autónoma de México).

Creative Commons Icon This image is made available under the Creative Commons BY-NC 4.0 license terms.

Keywords: stratovolcano | lava flow


Pico de Orizaba