Catskill Formation

Catskill Formation Stratigraphic range: Devonian
Outcrop of the Irish Valley Member of the Catskill Formation along the Horseshoe Curve, Blair County, Pennsylvania
Type	sedimentary
Underlies	Rockwell Formation, Huntley Mountain Formation, Spechty Kopf Formation
Overlies	Lock Haven Formation, Foreknobs Formation
Lithology
Primary	sandstone
Other	siltstone, shale
Location
Region	Appalachian Mountains
Country	United States
Extent	Pennsylvania, New York
Type section
Named for	Catskill Mountains, New York

The Devonian Catskill Formation or the Catskill clastic wedge is a unit of mostly terrestrial sedimentary rock found in Pennsylvania and New York. Minor marine layers exist in this thick rock unit (up to 10,000 feet). It is equivalent to the Hampshire Formation of Maryland, West Virginia, and Virginia.

The Catskill is the largest bedrock unit of the Upper Devonian in northeast Pennsylvania and the Catskill region of New York, from which its name is derived. The Pocono Mountains of Pennsylvania are largely underlain by this unit as well. The rocks of the Catskill are predominantly red sandstone indicating a large scale terrestrial deposition during the Acadian orogeny. Many beds are cyclical in nature, preserving the record of a dynamic environment during its approximately 20 million years of deposition.

Depositional Environment

Cut slab of the Catskill Formation from the Coleman Quarry of the Endless Mountain Stone Company, Susquehanna County, Pennsylvania, showing mud clasts within sandstone

Point bar deposits in the Catskill Formation (Devonian) near North Bend, PA.

During the Devonian period, the Catskill Delta was formed by a series of river deltas and otherwise marshy terrain. This terrain was sandwiched between the epicontinental Kaskaskia Sea in central North America and the now-vanished Acadian Mountains. Erosion brought sediment from the mountain westwards into the sea, forming the deltas.

Eventually the Delta formation was buried and transformed into sandstone, which was then revealed in places when the Catskill and Appalachian Mountains were formed at a later date. This transformation and uncovering is the primary reason why the Catskill Delta is notable in the present; western Pennsylvania's petroleum was formed as a consequence. This was the first major oil region to be developed.

The Catskill was once considered to be related to the Old Red Sandstone, but in actuality the two are only coincidentally similar. Both formed at approximately the same time, and under similar conditions: to the north of the Acadian Mountains were the Caledonian Mountains, and a similar region of marsh and river delta formed there.

Members

Eastern Pennsylvania

Towamensing, Walcksville, Beaverdam Run, Long Run, Packerton, Poplar Gap, Sawmill Run, Berry Run, Clarks Ferry, Duncannon

Central Pennsylvania

Irish Valley, Sherman Creek, Buddys Run, Clarks Ferry, Duncannon

Geologic cross section of upper to middle Devonian strata from Cherry Valley, New York south-southwest across the Allegheny Plateau and then along the Ridge-and-Valley Appalachians to Tennessee. The Catskill Formation is at the top.^[1]

References

External links

• Depositional Environments In the Catskill Clastic Wedge