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- W157499250 abstract "133 Introduction This study examines aspects of the subsurface geology of an area along the Clear Fork of Brazos River (Clear Fork) in parts of Throckmorton, Haskell, Shackelford, and Jones Counties, Texas (Figure 1). The study area extends from the town of Lueders in the southwest to Paint Creek in the northeast. It includes the originally proposed Cedar Ridge Reservoir damsite (CR) and the newly proposed damsite (site A), located about 8 km farther upstream (to the southwest). The study focuses on the distribution, thickness, and structure of a series of gypsum beds present in the Permian-age Jagger Bend/Valera Formation, which dips gently to the west at a rate of about 7 m/km. Abstract Cedar Ridge Dam and Reservoir will be built to supply water for the city of Abilene, Texas. The original damsite (CR) was to be located on Clear Fork of Brazos River in Throckmorton County, but initial coring of the damsite encountered unsuspected gypsum beds in the Permianage Jagger Bend/Valera Formation. Gypsum is a highly soluble rock that typically contains karst features, and its presence in a dam foundation or impoundment area could allow water to escape from the reservoir. A decision was made to look at potential sites farther upstream (to the southwest), where west-dipping gypsum beds would be deeper underground and karst problems would be minimized or eliminated." @default.
- W157499250 created "2016-06-24" @default.
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- W157499250 date "2013-01-01" @default.
- W157499250 modified "2023-10-14" @default.
- W157499250 title "Gypsum Karst Causes Relocation of Proposed Cedar Ridge Dam, Throckmorton County, Texas" @default.
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- W157499250 doi "https://doi.org/10.5038/9780979542275.1121" @default.
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