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BASEMAPS
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WEATHER
Manhattan Schist
Geologic Formation
in
NJ
,
NY
,
CT
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Lithology
Gneiss
Amphibolite
Amphibolite
Other
(9 mi²)
Geologic Age
Cambrian (542 Ma – 487.3 Ma ago)
(125 mi²)
Neoproterozoic – Early Cambrian (1000 Ma – 521 Ma ago)
(9 mi²)
Geologic Unit Label
CAm
(101 mi²)
CAma
(24 mi²)
CAZm0
(9 mi²)
Dark-gray to silvery, rusty-weathering, generally coarse grained, foliated but poorly layered to massive gneiss or schistose gneiss, composed of quartz, oligoclase, microcline, biotite, and muscovite, and generally sillimanite and garnet. Amphibolite layers locally, especially near base where in places separately mapped as unit CAma. Cambrian Manhattan Schist in this report includes four informal members: Warren member, garnetiferous biotite schist member, Shepaug member, and schistose granulite member. The Warren member occurs only in the Above All thrust sheet, the Shepaug member only in the Rabbit Hill thrust sheet. The schist member occurs in both. The granulite member occurs in the Rabbit Hill thrust sheet and the Lake Waramaug thrust sheet. The Warren includes mainly interbedded, dark-gray, muscovite-garnet-chlorite-plagioclase-biotite-quartz schist, amphibolite lenses, siliceous granulite, and finely-layered schistose gneiss. The Shepaug consists of interbedded orthoclase-garnet-plagioclase-biotite-quartz schistose gneiss, rusty-weathering, schistose gneisses and schists with sillimanite rods, and subordinate granulite beds with sillimanite nodules similar to those in the schistose granulite member (Panish, 1992).
—
USGS
Taxonomy
Classified As
Geologic Formation
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