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  2. Geology of Alabama - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Alabama

    The first scientific reports of Alabama's geology were made during field studies by R. T. Brumby in the late 1830s and Sir Charles Lyell in the early 1840s. Michael Tuomey , appointed state geologist in 1847, completed a Geological Map of Alabama and in 1849 and published the first of two comprehensive reports on the state's resources a year later.

  3. Odenville Formation - Wikipedia

    en.wikipedia.org/wiki/Odenville_Formation

    The Odenville Limestone is a geologic formation in Alabama.It preserves fossils dating from the early Ordovician Period.. As first described by geologist Charles Butts in a 1926 report on Alabama’s geology, the Odenville consisted of “impure argillaceous and siliceous dark fine-grained cherty limestone,” about fifty feet in thickness.

  4. Category:Geologic maps - Wikipedia

    en.wikipedia.org/wiki/Category:Geologic_maps

    Download as PDF; Printable version; In other projects ... Pages in category "Geologic maps" ... out of 13 total.

  5. Category:Alabama maps - Wikipedia

    en.wikipedia.org/wiki/Category:Alabama_maps

    Download as PDF; Printable version; In other projects ... Pages in category "Alabama maps" ... out of 3 total.

  6. Category:Geologic formations of Alabama - Wikipedia

    en.wikipedia.org/wiki/Category:Geologic...

    Download as PDF; Printable version; In other projects ... Pages in category "Geologic formations of Alabama" ... out of 13 total.

  7. Chattanooga Shale - Wikipedia

    en.wikipedia.org/wiki/Chattanooga_Shale

    The Chattanooga Shale is a geological formation in Alabama, Arkansas, Georgia, Kentucky, Missouri and Tennessee. It preserves conodont fossils dating to the Devonian period. [ 1 ] It occurs mostly as a subsurface geologic formation composed of layers of shale .

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  9. Mooreville Chalk - Wikipedia

    en.wikipedia.org/wiki/Mooreville_Chalk

    The Mooreville Chalk is a geological formation in North America, within the U.S. states of Alabama and Mississippi, which were part of the subcontinent of Appalachia.The strata date back to the early Santonian to the early Campanian stage of the Late Cretaceous. [1]