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Geologic units in Putnam county, New York

Pyroxene-hornblende-quartz-plagioclase gneiss (Middle Proterozoic) at surface, covers 2 % of this area
Pyroxene-hornblende-quartz-plagioclase gneiss.
Lithology: mafic gneiss
Gabbro or norite to hornblende diorite (Upper Ordovician) at surface, covers 0.4 % of this area
Gabbro or norite to hornblende diorite - rock complex with minor pyroxenite; Croton Falls and Peach Lake complexes in New York, and Mt. Prospect Complex in Connecticut.
Lithology: gabbro; norite; diorite; pyroxenite
Rusty and gray biotite-quartz-feldspar gneiss (Middle Proterozoic) at surface, covers 0.1 % of this area
Rusty and gray biotite-quartz-feldspar gneiss - rusty facies contains variable amounts of garnet, sillimanite, cordierite, graphite, sulfides; minor marble and calcsilicate rock.
Lithology: gneiss; marble; calc-silicate rock
Hartland Formation (Ordovician?) at surface, covers 0.2 % of this area
Hartland Formation - basal amphibolite overlain by pelitic schists.
Lithology: amphibolite; pelitic schist
Diorite with hornblende and/or biotite (Upper Ordovician) at surface, covers < 0.1 % of this area
Diorite with hornblende and/or biotite.
Lithology: diorite
Garnet-biotite-quartz-feldspar gneiss (Middle Proterozoic) at surface, covers 1 % of this area
Garnet-biotite-quartz-feldspar gneiss - quartzite, quartz-feldspar gneiss, calcsilicate rock.
Lithology: gneiss; quartzite; calc-silicate rock
Inwood Marble (Early Cambrian - Lower Ordovician) at surface, covers 0.7 % of this area
Inwood Marble - dolomite marble, calc-schist, granulite, and quartzite, overlain by calcite marble; grades into underlying patchy Lowerre Quartzite of Early Cambrian age.
Lithology: marble; schist; granulite; quartzite
Calcitic and dolomitic marble (Middle Proterozoic) at surface, covers 0.4 % of this area
Calcitic and dolomitic marble - predominantly; variably siliceous; in part with calcsilicate rock and amphibolite.
Lithology: marble; calc-silicate rock; amphibolite
Amphibolite (Middle Proterozoic) at surface, covers 20 % of this area
Amphibolite - commonly biotitic; garnetiferous, pyroxenic, in and adjacent to Adirondack Highlands.
Lithology: amphibolite
Biotite-quartz-plagioclase gneiss (Middle Proterozoic) at surface, covers 26 % of this area
Biotite-quartz-plagioclase gneiss - with subordinate biotite granitic gneiss, amphibolite, calcsilicate rock.
Lithology: gneiss; granitic gneiss; amphibolite; calc-silicate rock
Poughquag Quartzite (Cambrian) at surface, covers 0.2 % of this area
Poughquag Quartzite - (includes local Dalton Formation at base)-locally conglomeratic.
Lithology: quartzite; conglomerate
Hornblende granite and granite gneiss (Middle Proterozoic) at surface, covers 1 % of this area
Hornblende granite and granite gneiss - with subordinate leucogranite.
Lithology: granite; granitic gneiss
Walloomsac Formation (Middle Ordovician) at surface, covers 2 % of this area
Walloomsac Formation - slate, phyllite, schist, metagraywacke.
Lithology: slate; phyllite; schist; metasedimentary rock
Garnet-bearing gneiss and interlayered quartzite (Middle Proterozoic) at surface, covers 12 % of this area
Garnet-bearing gneiss and interlayered quartzite - contains varying amounts of biotite, garnet, sillimanite; minor marble, amphibolite, rusty paragneiss.
Lithology: gneiss; quartzite; marble; amphibolite; paragneiss
Stockbridge Formation (Cambrian - Lower Ordovician) at surface, covers 3 % of this area
Stockbridge Formation - calcitic and dolomitic marble.
Lithology: marble
Manhattan Formation (A Member) (Middle Ordovician) at surface, covers 0.2 % of this area
Manhattan Formation (A member) - sillimanite-garnet-muscovite-biotite-quartz- plagioclase schists; calcite marble and calcsilicate rock at base.
Lithology: schist; marble; calc-silicate rock
Biotite granite gneiss (Middle Proterozoic) at surface, covers 23 % of this area
Biotite granite gneiss - overprint signifies inequigranular texture.
Lithology: granitic gneiss
Cambrian thru Middle Ordovician carbonate rock (Cambrian - Middle Ordovician) at surface, covers < 0.1 % of this area
Cambrian thru Middle Ordovician (Barneveld) carbonate rock - occuring as slivers caught along thrusts of later allochthones, or carbonate blocks in Taconic Melange.
Lithology: carbonate; melange
Manhattan Formation, undivided (Ordovician?) at surface, covers 6 % of this area
Manhattan Formation, undivided - pelitic schists, amphibolite; Units ?Omb, ?Omc, and ?Omd may be Cambrian eugeosynclinal rocks thrust upon Oma; ?Omd - sillimanite-garnet-muscovite-biotite-plagioclase-quartz gneiss; ?Omc - sillimanite-garnet-muscovite-biotite-quartz-plagioclase schistose gneiss, sillimanite nodules, local quartz-rich layers; ?Omb - discontinous unit of amphibolite and ?Omc-type schist.
Lithology: pelitic schist; gneiss; amphibolite

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