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Bookmark or Share- Marcellus Shale: Results Continue to Amaze GeologistsThe Marcellus Shale, also referred to as the Marcellus Formation, is a Middle Devonian-age, black, low-density, carbonaceous (organic-rich) shale that occurs in the subsurface beneath much of Ohio, West Virginia, Pennsylvania and New York.
- The Marcellus Shale: The Science Beneath the SurfaceWhat is the Marcellus Shale? The Marcellus Shale is an organic-rich layer of rock extending deep underground from Ohio and West Virginia northeast into Pennsylvania and southern New York.
- Updated geologic maps provide greater detail for Marcellus formationThe Marcellus Middle Devonian-age shale extends from New York in the north to Kentucky and Tennessee in the south and is the most prolific natural gas-producing formation in the Appalachian basin. The formation's and play's footprints cover about 95,000 square miles and 72,000 square miles, respectively.
- Marcellus Shale CoalitionThe Marcellus Shale Coalition® (MSC) works with exploration and production, midstream, and supply chain partners in the Appalachian Basin and across the country to address issues regarding the production of clean, job-creating, American natural gas from the Marcellus and Utica Shale plays.
- Marcellus Formation - WikipediaThe Marcellus Formation or the Marcellus Shale is a Middle Devonian age unit of sedimentary rock found in eastern North America. Named for a distinctive outcrop near the village of Marcellus, New York, in the United States, [3] it extends throughout much of the Appalachian Basin. [4][5][6]
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