File:Bald Knoll.jpg

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Description
English: Bald Knoll is the youngest of a group of cinder cones on the SW part of the Paunsaugunt Plateau in southern Utah. It is seen here from the SW with the escarpment forming the Pink Cliffs of the renowned Grand Staircase of Paleozoic sedimentary rocks in the background. The proximal part of a voluminous blocky lava flow that traveled to the south from a vent at the base of the youthful-looking cinder cone forms the shaded area in the foreground.
Date
Source http://www.volcano.si.edu/world/volcano.cfm?vnum=1207-03-&volpage=photos&photo=102067
Author Lee Siebert (Smithsonian Institution)
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Public domain
This image or file is a work of a Smithsonian Institution employee, taken or made as part of that person's official duties. As a work of the U.S. federal government, the image is in the public domain in the United States.

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current19:30, 26 May 2010Thumbnail for version as of 19:30, 26 May 2010640 × 463 (37 KB)Michael Metzger{{Information |Description={{en|1=Bald Knoll is the youngest of a group of cinder cones on the SW part of the Paunsaugunt Plateau in southern Utah. It is seen here from the SW with the escarpment forming the Pink Cliffs of the renowned Grand Staircase of
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