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Extra info for The Eastern Countries: Trail Map Tm2, No 9404 (Dungeons and Dragons Official Game Accessory)

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15 0:: co :E 40 I0:: o ,MARL, medium gray, weathers to tan clay, massive bedded, s i 1ty, sandy, foss i 1i ferous. E. cance11ata Stephenson. - 0- w.. w.. =>' Section projected across bottom about 500 feet to southwest. -J co 20 :E w.. V) 5 -J o o 0- :E CHALK, medium gray, weathers light gray, massivebedded, indistinct bedding, "spa ll s " into slabby plates, silty, fossi1ifferous, bioturbated. Reeflike accumulations of Pycnodonta mutabi1is, Agerostrea fa1cata, Exogyra cance11ata, and others. 13.

Payne Chert and the gravels of the ~~Tennessee lithofacies" of the McShan is absent. The Tombigbee Sand Member is Early Campanian age in Mississippi. The glauconitic, pale red to yellowish-orange sands of the Eutaw Formation are irregular to lenticular in bedding and cross-bedded. Small discoidal, rip-up clasts of clay lie along bedding planes. Ophiomorphs are common. The upper sands tend to be more massively bedded and these grade upward into micaceous, silty, clayey, glauconitic, massive-bedded sands of the upper Tombigbee Sand Member, which contains carbonized and lignified plant materials and mollusc imprints.

Thin discontinuous lag bed of oyster hash. 11. 2. Fossiliferous marls in the top of the Mooreville Formation and the base of the Demopolis Formation. The contact is marked by the uppermost nodular limestone layer in the Arcola Limestone Member of the Mooreville Formation. 3. 5-minute quadrangle, sec. 5, T. , R. 15 E. More than 20 m of impure chalk with thin interbeds of marl in the top of the upper chalk member of the Demopolis Chalk (see fig. 1) is exposed along a county road (fig. 12). The chalks are gray, weathering to chalky white, massive-bedded with numerous burrows and some feeding traces and thin lenses of foraminiferal and shell ~~hash," probably the result of winnowing.

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