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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 (3,000 m)). It is equivalent to the Hampshire Formation of Maryland, West Virginia, and Virginia.
Stratigraphic range: Devonian
|Underlies||Rockwell Formation, Huntley Mountain Formation, Pocono Formation, Spechty Kopf Formation|
|Overlies||Foreknobs Formation, Lock Haven Formation, Trimmers Rock Formation|
|Thickness||Up to 10,000 ft (3,000 m)|
|Extent||Pennsylvania, New York (state)|
|Named for||Catskill Mountains, New York|
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.
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.
Though both mountain ranges were formed during the Acadian orogeny, the Catskill Mountains, unlike the Appalachian Mountains underwent glacial erosion. Much of what formed the Catskills as they stand today is a result of the Wisconsin glaciation which ended only about 12,000 years ago.
Signs of GlaciationEdit
These markers include:
Towamensing, Walcksville, Beaverdam Run, Long Run, Packerton, Poplar Gap, Sawmill Run, Berry Run, Clarks Ferry, and Duncannon.
Irish Valley, Sherman Creek, Buddys Run, Clarks Ferry, and Duncannon.
- Rich, John Lyon (1906). "Local Glaciation in the Catskill Mountains". The Journal of Geology. 14 (2): 113–121. doi:10.1086/621285. JSTOR 30055593.
- Titus, Robert (1996). The Catskills in the Ice Age. Flieschmanns, New York: Purple Mountain Press. pp. 14–29. ISBN 978-0-935796-77-3.
- Boughton, Carol J.; McCoy, Kurt J. (2006). "Hydrogeology, Aquifer Geochemistry, and Ground-Water Quality in Morgan County, West Virginia". U.S. Geological Survey. Scientific Investigations Report 2006-5198. Cite journal requires