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Capping Strata, Pleasant Hill Mound


Figure 15. Green shale and dolomite beds draping carbonate mound (white).

Glauconitic green shales and interbedded mudstones cap the Pleasant Hill mound (Fig. 15). The capping units are exposed even at high water levels. From the lake, capping layers on both margins of the mound overly large listric glide planes dipping off of both mound flanks (Figs. 2, 16). Thin dolomitic interbeds contain quartz geodes and abundant crinoids.


Figure 16. Slumped green shales and siltstones along the western margin of the underlying carbonate mound, showing slight rotation off of the mound.

 

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