"Drakes Formation (0d).-The Drakes Formation consists of four members: Rowland, Preachersville, Bardstown, and Saluda Dolomite Members. The Rowland and Preachersville occur in the eastern part of the Outer Bluegrass region, and the Rowland, Bardstown, and Saluda occur on the west side. The Drakes Formation is composed of dolomite, limestone, mudstone, and shale. Dolomite, dolomitic limestone, and mudstone are most abundant and are commonly composed of silt-sized grains, are sparsely fossiliferous or unfossiliferous, partly laminated, and locally mud cracked and ripple marked. The Bardstown Member, which makes up only a small part of the total Drakes, is composed of fossiliferous limestone in irregular or nodular beds thinly interbedded with fossiliferous or sparsely fossiliferous shale. The Drakes Formation generally ranges in thickness from 20 to 150 ft. In south-central Kentucky, it is locally cut out by the unconformity at the base of the Devonian rocks."
1 comment:
Interesting stuff. I will have to discuss this with you more the next time I see you, since there is now way I can see doing any sort of informative discussion via comments on blogs.
Thanks for the cool posts and pictures.
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