Shawangunk Formation

Shawangunk Formation Stratigraphic range: Lower Silurian PreЄ Є O S D C P T J K Pg N
Exposure of the Shawangunk at Lehigh Gap, PA
Type	Geological formation
Underlies	Bloomsburg Formation
Overlies	Martinsburg Formation
Thickness	approx. 1400 ft
Lithology
Primary	quartzarenite (sandstone), conglomerate
Location
Region	Appalachian Mountains
Extent	Pennsylvania, New Jersey, New York
Type section
Named for	Shawangunk Ridge
Named by	W. W. Mather, 1840

The Silurian Shawangunk Formation is a mapped bedrock unit in eastern Pennsylvania, New Jersey, and New York. It is named for the Shawangunk Ridge for which it is the dominant rock type. The division of the Shawangunk between the Tuscarora Formation and Clinton Group has not been conclusively determined. The shift of nomenclature currently has the divide between Hawk Mountain and Lehigh Gap.

The Shawangunk is defined as a light to dark-gray, fine to very coarsed grained sandstone and conglomerate, containing a few shale interbeds. There are also four members of this formation: Tammany, Lizard Creek, Minsi, and Weiders.

The Lizard Creek member is described at Lehigh Gap as having conglomerates, sandstone, calcareous sandstone, siltstone, and shale with a few minor red beds. The Minsi Member is described as a congloeritic quartzite and the Weiders is described as both a conglomerate and quartzite. The Tammany and Lizard Creek members are equivalent to the Clinton Formation and the Minsi and Weiders members are equivalent to the Tuscarora Formation in the central and western part of Pennsylvania. The Tammany Member was not described at Lehigh Gap.

The depositional environment of the Shawangunk has always been intrepreted as mostly terrestrial to a shallow marine deposit resulting in a molasse sequence produced by the Taconic orogeny. The numerous coarse-grained beds, especially in the lower part, suggest a relatively close orogenic source with very high to high energy fluvial systems depositing the sediments. Shale interbeds may indicate a slowing or shifting of these ancient river systems.

Very few fossils exist in the Shawangunk; however, Eurypterids can be found in the middle portions of the formation roughly 420–750 feet from the base in some locations in New York State. Linguloid brachiopods were identified in the Lizard Creek Member.