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The 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.
The Marcellus natural gas trend is a large geographic area of prolific shale gas extraction from the Marcellus Shale or Marcellus Formation, of Devonian age, in the eastern United States. [2] The shale play encompasses 104,000 square miles and stretches across Pennsylvania and West Virginia, and into eastern Ohio and western New York. [ 3 ]
They are directly overlain by a prominent ash bed, the Tioga Bentonite. The Bobs Ridge Sandstone and Tioga Bentonite indicate uplift and volcanic activity in the region, respectively. [3] The Tioga Bentonite, sometimes called the Tioga Ash Bed or Metabentonite, lies at the base of the Marcellus Shale. [2]
The Marcellus shale, a vast hydrocarbon-bearing formation that spans several states in the Northeast, is widely regarded as the most economical shale gas play in the country. According to Bentek ...
The Hamilton Group is a Devonian-age geological group which is located in the Appalachian region of the United States.It is present in New York, Pennsylvania, Maryland, Ohio, West Virginia, northwestern Virginia and Ontario, Canada, [1] [2] and is mainly composed of marine shale with some sandstone.
The Marcellus Formation, a shale rich in natural gas, lies thousands of feet below Worlds End State Park and much of Pennsylvania. As of June 30, 2012, there were 127 active gas wells in Sullivan County, with 14 of those in Forks or Shrewsbury Townships. [50]