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Geologic units in Chester county, Pennsylvania

Felsic to mafic gneiss (Precambrian) at surface, covers 2 % of this area
Felsic to mafic gneiss - Light, medium grained; predominantly quartz and feldspar of igneous origin.
Lithology: felsic gneiss; mafic gneiss; orthogneiss
Wissahickon Schist (Paleozoic) at surface, covers < 0.1 % of this area
Wissahickon Schist - Dense micaceous schist, gneiss and migmatite.
Lithology: mica schist; gneiss; migmatite
Conestoga Formation (Ordovician and Cambrian) at surface, covers 2 % of this area
Conestoga Formation - Light-gray, thin-bedded, impure, contorted limestone having shale partings; conglomeratic at base; in Chester Valley, includes micaceous limestone in upper part, phyllite in middle, and alternating dolomite and limestone in lower part.
Lithology: limestone; phyllite; conglomerate; dolostone (dolomite); shale
Felsic and intermediate gneiss (Precambrian) at surface, covers 6 % of this area
Felsic and intermediate gneiss - Light, medium grained; includes rocks of probable sedimentary origin.
Lithology: felsic gneiss; mafic gneiss; paragneiss
Felsic gneiss (Precambrian) at surface, covers 4 % of this area
Felsic gneiss - Light, medium grained; includes rocks of probable sedimentary origin.
Lithology: felsic gneiss; paragneiss
"Glenarm Wissahickon" formation (Probably lower Paleozoic) at surface, covers 24 % of this area
"Glenarm Wissahickon" formation - Lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Lithology: mica schist; mafic gneiss; amphibolite;
Bryn Mawr Formation (Tertiary) at surface, covers < 0.1 % of this area
Bryn Mawr Formation - High-level terrace deposits; reddish-brown gravelly sand and some silt. Age uncertain.
Lithology: gravel; sand; silt
Stockton Formation (Triassic) at surface, covers 3 % of this area
Stockton Formation - Light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone.
Lithology: arkose; siltstone; sandstone; mudstone
Pensauken and Bridgeton Formations, undifferentiated (Tertiary) at surface, covers < 0.1 % of this area
Pensauken and Bridgeton Formations, undifferentiated - Dark-reddish-brown, cross-stratified, feldspathic quartz sand and some thin beds of fine gravel and rare layers of clay or silt.
Lithology: sand; gravel; clay or mud; silt
Vintage Formation (Cambrian) at surface, covers 0.4 % of this area
Vintage Formation - Dark-gray, knotty, argillaceous dolomite; impure light-gray marble at base locally.
Lithology: dolostone (dolomite); marble
Hammer Creek Formation (Triassic) at surface, covers < 0.1 % of this area
Hammer Creek Formation - Gray and pale red, fine- to coarse-grained quartzose sandstone, siltstone, and mudstone.
Lithology: sandstone; siltstone; mudstone
Mafic gneiss (Probably lower Paleozoic) at surface, covers 0.8 % of this area
Mafic gneiss - Dark, medium grained; includes rocks of probable sedimentary origin; may be equivalent to pCAmgh in places.
Lithology: mafic gneiss; paragneiss
Metagabbro (Probably lower Paleozoic) at surface, covers < 0.1 % of this area
Metagabbro - Ranges from fine- to medium-grained, altered gabbro to hornblende gneiss.
Lithology: mafic gneiss; gabbro
Hammer Creek conglomerate (Triassic) at surface, covers 1 % of this area
Hammer Creek conglomerate - Cobble and pebble quartz conglomerate interbedded with red sandstone.
Lithology: conglomerate; sandstone
Mafic gneiss (Precambrian) at surface, covers 0.9 % of this area
Mafic gneiss - Dark, medium grained; includes rocks of probable sedimentary origin; may be equivalent to "PZmgp" in places.
Lithology: mafic gneiss; paragneiss
Diabase (Jurassic) at surface, covers 0.7 % of this area
Diabase - Medium- to coarse-grained, quartz-normative tholeiite; composed of labradorite and various pyroxenes; occurs as dikes, sheets, and a few small flows. Includes the dark-gray York Haven Diabase (high titanium oxide) and the slightly younger Rossville Diabase (low titanium oxide). In chilled margins, the Rossville is distinguished from the York Haven by its lighter gray color and distinctive, sparse, centimeter-sized calcic-plagioclase phenocrysts.
Lithology: diabase
Ultramafic rocks (Probably lower Paleozoic) at surface, covers 2 % of this area
Ultramafic rocks - Includes serpentine, steatite, and other products of alteration of peridotites and pyroxenites.
Lithology: serpentinite; pyroxenite; peridotite
Elbrook Formation (Cambrian) at surface, covers 1 % of this area
Elbrook Formation - Microcrystalline limestone and, in places, marble; includes subordinate dolomite containing abundant phyllitic layers; occurs in Chester and Montgomery Counties; relation to Elbrook of Cumberland Valley sequence is uncertain.
Lithology: limestone; dolostone (dolomite); phyllite; marble
Metabasalt (Precambrian) at surface, covers < 0.1 % of this area
Metabasalt - Dark-gray, fine-grained intrusives; locally, mineralogy is altered and unit has greenish color.
Lithology: meta-basalt
Felsic and intermediate gneiss (Precambrian) at surface, covers 8 % of this area
Felsic and intermediate gneiss - Medium grained, light pink to greenish gray; largely quartz, feldspar, and mica; commonly gneissic, containing alteration minerals; interfingers with gabbroic gneiss.
Lithology: felsic gneiss; gneiss
Banded mafic gneiss (Precambrian) at surface, covers 3 % of this area
Banded mafic gneiss - Dark, fine to medium grained; includes rocks of probable sedimentary origin; may be equivalent to "PZmgh."
Lithology: mafic gneiss; paragneiss
Ledger Formation (Cambrian) at surface, covers 2 % of this area
Ledger Formation - Light-gray, locally mottled, massive, pure, coarsely crystalline dolomite; siliceous in middle part.
Lithology: dolostone (dolomite)
Amphibolite (Paleozoic) at surface, covers < 0.1 % of this area
Amphibolite - amphibolite
Lithology: amphibolite
Cockeysville Marble (Probably lower Paleozoic) at surface, covers 1 % of this area
Cockeysville Marble - White to light bluish gray, finely to coarsely crystalline.
Lithology: marble
Brunswick Formation (Triassic) at surface, covers 4 % of this area
Brunswick Formation - Reddish-brown mudstone, siltstone, and shale, containing a few green and brown shale interbeds; red and dark-gray, interbedded argillites near base. Youngest beds in Brunswick may be Jurassic in age.
Lithology: mudstone; siltstone; shale; argillite
Metadiabase (Precambrian) at surface, covers 0.1 % of this area
Metadiabase - Dark-gray, fine-grained intrusives; locally, mineralogy is altered and unit has greenish color.
Lithology: mafic metavolcanic rock
Mafic gneiss (Precambrian) at surface, covers 0.1 % of this area
Mafic gneiss - Dark, medium grained; includes rocks of probable sedimentary origin; may be equivalent to "PZmgh" in places.
Lithology: mafic gneiss; paragneiss
Lockatong Formation (Triassic) at surface, covers 0.6 % of this area
Lockatong Formation - Dark-gray to black, thick-bedded argillite containing a few zones of thin-bedded black shale; locally has thin layers of impure limestone and calcareous shale.
Lithology: argillite; shale; limestone; black shale
Kinzers Formation (Cambrian) at surface, covers 0.1 % of this area
Kinzers Formation - Base--dark-brown shale; middle--gray and white spotted limestone and, locally, marble having irregular partings; top--sandy limestone which weathers to a fine-grained, friable, porous, sandy mass.
Lithology: limestone; marble; shale; sand
Pegmatite (Paleozoic) at surface, covers < 0.1 % of this area
Pegmatite - Pegmatite
Lithology: pegmatite
Pegmatite (Probably lower Paleozoic) at surface, covers 0.2 % of this area
Pegmatite - Coarse to medium grained, granitic; contacts range from sharp to narrowly gradational; some zoning in places.
Lithology: pegmatite
Antietam Formation (Cambrian) at surface, covers 0.2 % of this area
Antietam Formation - Gray, buff-weathering quartzite and quartz schist.
Lithology: quartzite; schist
Franklin Marble (Precambrian) at surface, covers < 0.1 % of this area
Franklin Marble - White, coarsely crystalline; disseminated graphite flakes.
Lithology: marble
Graphitic felsic gneiss (Precambrian) at surface, covers 5 % of this area
Graphitic felsic gneiss - Includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin.
Lithology: gneiss; marble; paragneiss
Antietam and Harpers Formations, undivided (Cambrian) at surface, covers 0.7 % of this area
Antietam and Harpers Formations, undivided - Includes, in descending order, the Antietam (CAa) and Harpers (CAh) Formations. Antietam Formation - gray, buff-weathering quartzite. Harpers Formation - Dark-greenish-gray phyllite and schist containing thin quartzite layers; includes Montalto Member (CAhm) - gray quartztite
Lithology: quartzite; schist; phyllite
Octoraro Formation (Probably lower Paleozoic) at surface, covers 6 % of this area
Octoraro Formation - Includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members.
Lithology: schist; phyllite; gneiss; granitoid
Setters Quartzite (Probably lower Paleozoic) at surface, covers 2 % of this area
Setters Quartzite - Includes white feldspathic quartzite, gray mica gneiss, and mica schist.
Lithology: quartzite; mica gneiss; mica schist
Peters Creek Schist (Probably lower Paleozoic) at surface, covers 9 % of this area
Peters Creek Schist - Chlorite-sericite schist containing interbedded quartzite.
Lithology: schist; quartzite
Graphitic felsic gneiss (Precambrian) at surface, covers 5 % of this area
Graphitic felsic gneiss - Medium grained, medium to dark gray; locally gneissic, predominantly feldspar and quartz, plus dark accessories and various alteration minerals.
Lithology: felsic gneiss; mafic gneiss
Harpers Formation (Cambrian) at surface, covers 0.2 % of this area
Harpers Formation - Dark-greenish-gray phyllite and schist containing thin quartzite layers.
Lithology: phyllite; schist; quartzite
Chickies Formation (Cambrian) at surface, covers 4 % of this area
Chickies Formation - Light-gray, hard, massive, Scolithus-bearing quartzite and quartz schist; thin, interbedded dark slate at top; conglomerate (Hellam Member) at base.
Lithology: quartzite; schist; slate; conglomerate
Anorthosite (Precambrian) at surface, covers 2 % of this area
Anorthosite - Medium to coarse grained, light to dark bluish gray, predominantly plagioclase; local alteration minerals.
Lithology: anorthosite

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