From Wikipedia, the free encyclopedia
Bald Knoll is the youngest of a group of cinder cones on the SW part of the Paunsaugunt Plateau in southern Utah.
|Elevation||7,003 ft (2,135 m)|
- "Bald Knoll". Global Volcanism Program. Smithsonian Institution.
- "Bald Knoll". Volcano Global Risk Identification and Analysis Project (VOGRIPA). February 5, 2012. Retrieved February 15, 2014.
|This article about a location in Utah is a stub. You can help Wikipedia by expanding it.|