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Global Volcanism Program | Image GVP-03375

Firepit Knoll cinder cone is the largest of a cluster of cones at the northern end of the Kolob volcanic field on the upper Kolob Plateau.  The northern cinder cones, of Pleistocene age, produced lava flows that traveled 10-15 km to the south.  The cones were erupted through rocks of the Navajo Sandstone, forming the red-colored pinnacle to the right. Photo by Lee Siebert, 1987 (Smithsonian Institution).

Firepit Knoll cinder cone is the largest of a cluster of cones at the northern end of the Kolob volcanic field on the upper Kolob Plateau. The northern cinder cones, of Pleistocene age, produced lava flows that traveled 10-15 km to the south. The cones were erupted through rocks of the Navajo Sandstone, forming the red-colored pinnacle to the right.

Photo by Lee Siebert, 1987 (Smithsonian Institution).

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


Kolob