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- W83018072 abstract "Exposures of Carboniferous rocks are located along Interstate 24 on the east and west sides of Monteagle Mountain (three exposures in all). Here the Upper Mississippian Pennington formation accumulated in a high intertidal paleoenvironment. Lowermost Pennsylvanian marginal marine deposits form the Raccoon Mountain formation. In this area, the Mississippian-Pennsylvanian systemic boundary may be placed at different levels, depending on the bias of the observer, and therefore may be considered either as transitional or erosional. Five cycles of braided stream fining upward sequences are mapped as Warren Point Sandstone, Signal Point Shale, and Sewanee Sandstone. These cyclic Pennsylvanian deposits on Monteagle Mountain may be an eastern extension of the well-known, mid-continent Pennsylvanian cyclothems." @default.
- W83018072 created "2016-06-24" @default.
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- W83018072 date "1990-10-01" @default.
- W83018072 modified "2023-09-27" @default.
- W83018072 title "Lower Pennsylvanian-Upper Mississippian Deposystems, Monteagle Mountain, Tennessee" @default.
- W83018072 hasPublicationYear "1990" @default.
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