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Global Volcanism Program | Image GVP-06750

A freight train passes Pisgah Crater and its associated lava field.  The 100-m-high cone is the most prominent feature of a lava field that covers 100 km2.  The irregular shape of the cone results from the mining of aggregate.  The composite lava flows extend up to 8 km to the SE and in a narrow lobe 18 km to the NW.  Most of the flows are pahoehoe, but some of the eastern flows are aa.  Other cones and lava flows of the Lavic Lake volcanic field are located nearby. Photo by Lee Siebert, 1997 (Smithsonian Institution).

A freight train passes Pisgah Crater and its associated lava field. The 100-m-high cone is the most prominent feature of a lava field that covers 100 km2. The irregular shape of the cone results from the mining of aggregate. The composite lava flows extend up to 8 km to the SE and in a narrow lobe 18 km to the NW. Most of the flows are pahoehoe, but some of the eastern flows are aa. Other cones and lava flows of the Lavic Lake volcanic field are located nearby.

Photo by Lee Siebert, 1997 (Smithsonian Institution).

Creative Commons Icon This image is made available under the Public Domain Dedication CC0 license, but proper attribution is appreciated.


Lavic Lake