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1,591 to 1,600 of 2,055 Results
Mar 14, 2024 - WSGS
Carroll, C.J.; Ratigan, D.R.; Lynds, R.M.; Palkovic, M.J., 2024, "Preliminary geologic map of the Rawlins Peak SW quadrangle, Carbon County, Wyoming", https://doi.org/10.15786/13687261, Wyoming Data Repository, V1
The Rawlins Peak SW 1:24000-scale quadrangles is located in south-central Wyoming on the eastern margin of the Great Divide Basin, a sub-basin of the Greater Green River Basin. Upper Cretaceous through Eocene formations were studied and mapped in addition to the sedimentology, geochronology, and coal stratigraphy. Data from the map are reported in...
ZIP Archive - 19.4 MB - MD5: 08bf0a3b3b02bcc11a2c8a9a9419506d
Mar 14, 2024 - WSGS
Kehoe, K. S.; Gay, G. W.; Lichtner, D. T., 2024, "Preliminary Geologic Map of the Richards Gap Quadrangle, Sweetwater County, Wyoming, and Daggett County, Utah.", https://doi.org/10.15786/14771004, Wyoming Data Repository, V1
The main goal of mapping the bedrock geology of the Richards Gap 7.5' quadrangle is to further understanding of the mineral and energy resources in the Firehole Canyon area of southwestern Wyoming. The bedrock geologic units exposed in the quadrangle range in age from Upper Cretaceous to Oligocene, and record a transition from deposition at the mar...
Mar 14, 2024 - WSGS
Webber, P.M.; Lynds, R.M.; Stotter, S.V.; Krupnick, J.M., 2024, "Preliminary investigation of the critical mineral potential of the central Laramie Mountains, Wyoming", https://doi.org/10.15786/21222374, Wyoming Data Repository, V1
Preliminary investigation of the critical mineral potential of the central Laramie Mountains, Wyoming
Mar 14, 2024 - WSGS
Gregory, R. W.; Webber, P. M.; Stotter, S. V.; Jordan, Bear; Lynds, R. M.; Frost, B. R., 2024, "Preliminary geologic map of the Goat Mountain quadrangle, Albany and Laramie counties, Wyoming.", https://doi.org/10.15786/14779617, Wyoming Data Repository, V1
The Goat Mountain 7.5-minute quadrangle straddles the Albany-Laramie county line in southeastern Wyoming. Paleoproterozoic rocks are exposed in the western half of the quadrangle, while Phanerozoic rocks make up most of the eastern half. Laramide reverse faulting resulted in a tightly folded sequence of Paleozoic and Mesozoic rocks exposed in the I...
ZIP Archive - 18.8 MB - MD5: c200201454a9cb2bbab3b647781deb23
Mar 14, 2024 - WSGS
Lynds, R.M.; Lichtner, D.T., 2024, "Stratigraphy and hydrocarbon potential of the Fort Union and Lance Formations in the Great Divide and Washakie basins, south-central Wyoming", https://doi.org/10.15786/13696882, Wyoming Data Repository, V1
The Lance and Fort Union Formations of the Greater Green River Basin record the retreat of the Cretaceous Western Interior Seaway and the transition from marine deposition to continental, synorogenic sedimentation. Structural development of the eastern Greater Green River Basin began during the latest Cretaceous, with its main depocenter in the nor...
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