Mineral Resources On-Line Spatial Data
Mineral Resources > Online Spatial Data > Geology > by state > Vermont
| State | Vermont |
|---|---|
| Name | Clarendon Springs, Ticonderoga, and Rock River Dolomites; Gorge Formation |
| Geologic age | Cambrian |
| Original map label | Ccs |
| Comments | Part of Champlain and Vermont Valleys Conodont biostratigraphy indicates that the Gorge Formation in VT is of Late Cambrian and Early Ordovician age (Landing, 1983) per VT015. |
| Primary rock type | dolostone (dolomite) |
| Secondary rock type | sandstone |
| Other rock types | chert; conglomerate |
| Lithologic constituents | Major
Sedimentary > Carbonate > Dolostonemassive, smooth weathered gray dolomite characterized by numerous geodes and knots of white quartz Incidental
Sedimentary > Clastic > ConglomerateThe Gorge is a partly conglomeratic facies on the west limb of the St. Albans synclinorium. Sedimentary > Chemical > Chertirregular masses of chert are near the top Sedimentary > Clastic > Sandstone |
| Map references | Nicholson, S.W., Dicken, C.L., Horton, J.D., Foose, M.P., Mueller, J.A.L., and Hon, Rudi, 2006, Preliminary integrated geologic map databases for the United States: Connecticut, Maine, Massachusetts, New Hampshire, New Jersey, Rhode Island, and Vermont: U.S. Geological Survey Open-File Report 2006-1272. |
| Unit references | Doll, C.G., Cady, W.M., Thompson, J.B., Jr., and Billings, M.P., 1961, Centennial Geologic Map of Vermont: Vermont Geological Survey, Miscellaneous Map MISCMAP-01, scale 1:250,000. Landing, Ed, 1983, Highgate Gorge; Upper Cambrian and Lower Ordovician continental slope deposition and biostratigraphy, northwestern Vermont: Journal of Paleontology, v. 57, no. 6, p. 1149-1187. |
| Geographic coverage | Addison - Bennington - Chittenden - Franklin - Rutland |
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