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| | Summary of Citation |
 | | Is a detrital facies of the early acid breccia in the south fork of Shoshone River, Park Co., Bighorn Basin, WY. thought to be slightly younger than Cathedral Cliffs Formation (new name) of the Clarks Fork area. |
 | | Publication: Bown, T.M., 1982, Geology, paleontology, and correlation of Eocene volcaniclastic rocks, southeast Absaroka Range, Hot Springs County, Wyoming, IN Geology of the Absaroka Range, northwest Wyoming: U.S. Geological Survey Professional Paper, 1201-A, p. |
 | | Publication: Eaton, J.G., 1982, Paleontology and correlation of Eocene volcanic rocks in the Carter Mountain area, Park County, southeastern Absaroka Range, Wyoming: University of Wyoming Contributions to Geology, v. |
| ngmdb.usgs.gov /Geolex/Refsmry/sumry_9824.html (576 words) |
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