Publications in Williamson
Title | Publication Year | Abstract | Author | Series | Publisher | |
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Geologic map of the Weir quadrangle, Texas | 1997 | Collins, E.W. | Open-File Map | Bureau of Economic Geology | |
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Geologic map of the Coupland quadrangle, Texas | 2000 | Collins, E.W. | Open-File Map | Bureau of Economic Geology | |
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Geologic map of the Nameless Quadrangle, Texas | 1999 | Collins, E.W. | Open-File Map | Bureau of Economic Geology | |
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Geologic map of the Beaukiss quadrangle, Texas | 2001 | Collins, E.W. | Open-File Map | Bureau of Economic Geology | |
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Geologic map of the Travis Peak quadrangle | 2014 | Woodruff, C.M., Jr. | Open-File Map | Bureau of Economic Geology | |
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Geologic map of Mansfield Dam, Jollyville, Austin West, and Bee Cave quadrangles, Central Texas (Lower Lake Travis and Lake Austin vicinity) | 2018 | Woodruff, C.M., Jr., Collins, E.W. | Open-File Map | Bureau of Economic Geology | |
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Geologic map of the Taylor quadrangle | 2020 | Woodruff, C.M., Jr., Costard, L. | Open-File Map | Bureau of Economic Geology | |
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Stratigraphy of the Fredericksburg Division, south-central Texas | 1964 | Sediments of the Fredericksburg Division in south-central Texas were deposited on the slowly subsiding west flank of the Tyler basin. In this region there are three stratigraphically distinct areas. The southern area has a thick Edwards Limestone unit overlying a thin Walnut Formation. |
Moore, C.H. | Report of Investigations | Bureau of Economic Geology |
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Nomenclature revision of basal Cretaceous rocks between the Colorado and Red Rivers, Texas | 1966 | Based on need for convenient, small-scale cartographic units, the basal Cretaceous rocks in Texas from Red River to Burnet County and on the Callahan Divide are herein divided into three distinctive lithologic sequences. |
Fisher, W.L., Rodda, P.U. | Report of Investigations | Bureau of Economic Geology |
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Stratigraphy of Lower Cretaceous Trinity deposits of central Texas | 1971 | The stratigraphic record of the Lower Cretaceous Trinity Division in Central Texas, as revealed by extensive outcrop investigation, is that of a shallow sea transgressing the southern flank of the ancient Llano Uplift. |
Stricklin, F.L., Smith, C.I., Lozo, F.E. | Report of Investigations | Bureau of Economic Geology |