Global Volcanism Program | Image GVP-02997
The western slopes of Mount Jefferson rise above forested hills composed of older Pleistocene volcanic rocks. Scoria cones younger than the eroded main edifice, which ceased activity during the late Pleistocene, are located to the south.
Photo by Lee Siebert, 1982 (Smithsonian Institution).
This image is made available under the Public Domain Dedication CC0 license, but proper attribution is appreciated.