Bald Knoll

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Bald Knoll is the youngest of a group of cinder cones on the SW part of the Paunsaugunt Plateau in southern Utah.

Bald Knoll is a cinder cone in Utah, in the Southwestern United States.

It is the youngest volcano at the southwest portion of the Paunsaugunt Plateau and it consists of basaltic lava with a well-preserved volcanic crater at its summit.[1]

[edit] References

  1. ^ "Bald Knoll". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1207-03-.

Coordinates: 37°19′38″N 112°24′32″W / 37.32722°N 112.40889°W / 37.32722; -112.40889

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