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Dunkard Group
Red and green shale, siltstone, and sandstone, with thin lenticular beds of argillaceous limestone and thin beds of impure coal; thick-bedded, white conglomeratic sandstone at base; thickness greater than 200 feet; occurs only on hilltops in center of Georges Creek Basin. |
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Monongahela Formation
Interbedded claystone, argillaceous limestone, shale, sandstone, and coal beds; Waynesburg coal at top; Pittsburgh coal at base; thickness 240 feet in west, increases to 375 feet in east. |
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Conemaugh Formation
Includes the rocks between the base of the Pittsburgh coal and the top of the Upper Freeport coal; consists of two unnamed members which are separated by the Barton coal; both members are gray and brown claystone, shale, siltstone, and sandstone, with several coal beds; lower member also contains redbeds and fossiliferous marine shales; thickness 825 to 925 feet. |
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Allegheny Formation
Interbedded sandstone, siltstone, claystone, shale, and coal beds; Upper Freeport coal at top; where present, Brookville coal defines base; thickness 275 feet in northeast, increases to 325 feet in south and west.
Pottsville Formation
Interbedded sandstone, siltstone, claystone, shale, and coal beds; conglomeratic orthoquartzite and protoquartzite at base; thickness 60 feet in northeast, increases to 440 feet in southwest.
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Mauch Chunk Formation
Red and green shale, reddish-purple mudstone, and red, green, brown, and gray thin-bedded and cross-bedded sandstone; thickness 500 feet in west, increases to about 800 feet in east. |
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Greenbrier Formation
Upper part red calcareous shale and sandstone interbedded with greenish-gray and reddish gray argillaceous limestone; Loyalhanna Limestone Member; Gray to red, cross-bedded, arenaceous calcarenite; total thickness 200 to 300 feet. |
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Pocono Group
Gray, white, tan, and brown, thin- to thick-bedded, cross-bedded sandstone, locally conglomeratic; interbedded gray and reddish-brown shale, mudstone, and siltstone; fragmentary plant fossils. Undifferentiated in Garrett and western Allegany Counties.
Purslane Sandstone
White, thick-bedded, coarse-grained sandstone and conglomerate with thin coal beds and red shales. Eastern Allegany and Washington Counties.
Rockwell Formation
Coarse-grained arkosic sandstone, fine-grained conglomerate, and buff shale; dark shale with thin coal beds near base. Eastern Allegany and Washington Counties.
Total thickness of Group 250 feet in west, increase to 1,700 feet in east. |
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Hampshire Formation
Interbedded red shale, red mudstone, and red to brown cross-bedded siltstone and sandstone; some thin green shale; greenish-gray sandstone and shale toward top; fragmentary plant fossils; thickness 1,400 to 2,000 feet in west, increases to 3,800 in east. |
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"Chemung" Formation
Predominantly marine beds characterized by gray to olive-green graywacke, siltstone, and shale; thickness ranges from 2,000 to 3,000 feet.
Parkhead Sandstone
Gray to olive-green sandy shale, conglomeratic sandstone, and graywacke; present in Washington County, identification uncertain in west; thickness averages 400 feet.
Brallier Formation
(Woodmont Shale of earlier reports). Medium to dark gray, laminated shale and siltstone; weathers to light olive-gray; grain size coarsens upward; thickness about 2,000 feet in west, about 1,700 feet in east.
Harrell Shale
Dark gray laminated shale; absent in east and where Brallier lies directly on Mahantango, Tully Limestone lies near base in west, in subsurface of Garrett County; total thickness in west 140 to 300 feet. |
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Hamilton Group
Mahantango Formation
dark gray, laminated shale, siltstone, and very fine-grained sandstone; thickness 600 feet in west, increases to 1,200 feet in east.
Marcellus Shale
Gray-black, thinly laminated, pyritic, carbonaceous shale; thickness 250 feet in east, increasing to 500 feet in west.
Tioga Metabentonite Bed
Brownish-gray, thinly laminated shale containing sand-sized mica flakes; thickness less than one foot.
Needmore Shale
Olive-gray to black shale and dark, thin-bedded, fossiliferous, argillaceous limestone; thickness ranges from 70 to 145 feet.
Note: Hamilton Group, Tioga Metabentonite Bed, and Needmore Shale formerly were designated Romney Formation. |
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Ridgeley Sandstone
White, medium- to coarse-grained, fossiliferous, calcareous orthoquartzite; thickness 160 feet in west. Medium to dark gray cherty, arenaceous limestone in east; thickness 50 feet.
Shriver Chert
Dark gray, brown and black silty shales, cherty shales, and nodular and bedded black chert; fossiliferous; thickness 170 feet in west, upper boundary gradational with Ridgeley. Thickness 14 feet in east where the lower Shriver intertongues with the Licking Creek Limestone Member of the Helderburg Formation. |
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Helderburg Formation
Licking Creek Member: (Becraft Limestone of earlier reports.) Present only in east. Medium gray, medium-grained limestone near top; bedded black chert and thin-bedded limestone in middle; silty argillaceous limestone and shale near base; contains tongues of Shriver and Mandata; thickness 110 feet.
Mandata Shale Member: Dark brown to black, thin-bedded shale; fossiliferous; thickness 20 to 30 feet in west, intertongues with Licking Creek Limestone Member in east. Corriganville Limestone Member (Head): (New Scotland Limestone of earlier reports.) Medium gray, medium-grained, medium-bedded limestone, interbedded with chert; fossiliferous; thickness 15 to 30 feet. New Creek Limestone Member: (Coeymans Limestone of earlier reports.) Medium gray, thick-bedded, coarse-grained limestone; fossiliferous; thickness 9 to 10 feet. Limestone changes facies eastward into sandstone, the Elbow Ridge Sandstone Member: Medium-bedded, medium- to coarse-grained, calcareous sandstone; thickness 10 to 18 feet.
Keyser Limestone
Dark gray, thin- to thick-bedded, fine- to coarse-grained calcarenite; contains nodular limestone, dolomitic limestone, and calcareous shale; cherty near top; fossiliferous; thickness 200 to 300 feet. |
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Tonoloway Formation
Gray, thin-bedded limestone, dolomitic limestone, and calcareous shale; thin sandstone member in east 20 feet above base; fossiliferous; thickness 400 feet in east, increases to 600 feet in west. |
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Wills Creek Shale
Olive to yellowish-gray, thin-bedded sandstone, calcareous shale, argillaceous limestone, and sandstone; thickness 450 feet in west, increases to 600 feet in east.
Bloomsburg Formation
Bright red, hematitic, thin- to thick-bedded sandstone and shale; some dark sandstone and green shale; Cedar Creek Member: Dark gray, fine- to medium-grained argillaceous limestone, occurs in middle part of formation; total thickness 20 feet in west, increases to 200 feet in east. |
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McKenzie Formation
Gray, thin-bedded shale and argillaceous limestone; interbedded red sandstone and shale in east; thickness 160 in western Washington County, increases to 300 feet in east and 380 feet in west. |
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Rochester Shale
Gray, thin-bedded calcareous shale and dark gray, thin- to medium-bedded lenticular limestone; thickness 25 to 40 feet.
Keefer Sandstone
White to yellowish-gray, thick-bedded protoquartzite and orthoquartzite, calcareous to west; thickness 1o feet in west, increase to 35 feet in east.
Rose Hill Formation
Olive-gray to drab, thin-bedded sandstone; Cresaptown Iron Sandstone |
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Tuscarora Sandstone
White to light gray, thin- to thick-bedded cross-stratified subgraywacke and orthoquartzite; thickness 60 feet in east, increasing to 400 feet in west. |
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Juniata Formation
Red to greenish-gray, thin- to thick-bedded siltstone, shale, subgraywacke, and protoquartzite; interbedded conglomerate; thickness 180 feet in east, increases to 500 feet in west. |
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Martinsburg Formation
Upper part rhythmically interbedded graywackes, siltstones, and dark shales; lower part dark brown, dark gray, and black, thin-bedded fissile shale; thickness 2,000 to 2,500 feet. |
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Chambersburg Limestone
Dark gray, fine- to medium grained, thin-bedded argillaceous limestone; nodular and fossiliferous; thickness 225 to 250 feet.
St. Paul Group
New Market Limestone
Upper part gray, thick-bedded calcilutite; fossiliferous. Lower part light gray, thin-bedded, laminated argillaceous calcilutite; thickness 285 feet in south, increases to 700 feet in north.
Row Park Limestone
Light gray, fine-grained, medium- to thick-bedded calcerenite, calcilutite, and dolomitic limestone; interbedded dark gray, cherty, granular limestone; thickness 100 feet in south, increases to 680 feet in north.
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Pinesburg Station Dolomite
Light gray, laminated and mottled cherty dolomite; nonfossiliferous; thickness 375 to 500 feet. |
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Rockdale Run Formation
Upper one-third gray, mottled cherty dolomite and dolomitic limestone; lower two-thirds gray, cherty argillaceous calcarenite and algal limestone with interbedded dolomite and oolitic limestone; thickness at least 1,700 feet east of Conococheague Creek, increases to about 2,500 feet in west. |
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Stonehenge Limestone
Upper part gray, thin-bedded, coarse-grained to conglomeratic, oolitic calcarenite; some dolomite; lower part gray, thick-bedded, fine-grained algal limestone; thickness s500 to 800 feet. |
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Conococheague Limestone
Dark blue, laminated, oolitic, argillaceous and siliceous limestone, algal limestone, and flat-pebble conglomerate; siliceous shale partings; some sandstone and dolomite; thickness 1,6000 to 1,900 feet. |
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Elbrook Limestone
Light blue, laminated, argillaceous limestone and calcareous shale; some dolomite; thickness 1,400 to possibly 3,000 feet |
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Waynesboro Formation
Upper part red, gray, and yellowish-brown, thin-bedded siltstone, shale, and ripple-marked, cross-bedded sandstone; lower part interbedded dark gray to red shale and thin-bedded dolomite; thickness approximately 600 feet. |
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