Marcellus Formation | |
---|---|
Stratigraphic range: Middle Devonian | |
Type | Geological formation |
Unit of | Hamilton Group |
Sub-units | See: Named members |
Underlies | Mahantango Formation and Skaneatales Formation/Stafford Lime Mbr |
Overlies | Huntersville Chert, Needmore Shale, and Onondaga Formation |
Thickness | up to 900 feet (270 m)[1] |
Lithology | |
Primary | Shale |
Other | Slate, limestone, sandstone, tuff |
Location | |
Region | Appalachian Basin of eastern North America |
Extent | 600 miles (970 km)[2] |
Type section | |
Named for | Marcellus, New York |
Named by | James Hall, 1839 |
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.[4][5][6]
The unit name usage by the U.S. Geological Survey (USGS) includes Marcellus Shale and Marcellus Formation.[7] The term "Marcellus Shale" is the preferred name throughout most of the Appalachian region, although the term "Marcellus Formation" is also acceptable within the State of Pennsylvania.[7] The unit was first described and named as the "Marcellus shales" by J. Hall in 1839.[8]
White
was invoked but never defined (see the help page).MGS1918
was invoked but never defined (see the help page).