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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 ]
The Onondaga outcrops in a line that usually forms an escarpment (the steep face of a cuesta), because of its resistance to erosion. The outcrop can be traced from the Hudson River valley westward along the southern rim of the Mohawk River valley, passing just south of Syracuse , and along the northern heads of the major Finger Lakes to Buffalo ...
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 completed pipeline has a capacity of 2 million dekatherms (Dths) of natural gas per day (approximately 200 TWh per year), with gas produced from the Marcellus and Utica shale formations. The pipeline was met with opposition in the form of legal challenges, regulatory hurdles, direct action and destruction of property.
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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.