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National Geologic Map Database
Geologic Unit: Prospect
Map showing publication footprint
  • Usage in publication:
    • Prospect porphyritic gneiss*
  • Modifications:
    • Named
  • Dominant lithology:
    • Gneiss
    • Granite
  • AAPG geologic province:
    • New England province
Publication:

Gregory, H.E., 1906, The crystalline rocks, Chapter II, IN Rice, W.N., and Gregory, H.E., Manual of the geology of Connecticut: Connecticut Geological and Natural History Survey Bulletin, no. 6, p. 39-155.


Summary:

Unit described as a light-gray porphyritic gneiss, including small areas of porphyritic granite with inconspicuous gneissoid development and narrow bands of mica schist distributed unevenly. At its extreme northern limit, it is prevailingly less porphyritic and more quartzose and contains areas of intrusive basic rocks. Is believed to have been originally a mass of porphyritic granite intruded into Hartland (Hoosac) schist. Covers eastern part of Prospect Township. Age given as Ordovician(?).

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Prospect porphyritic gneiss
  • Modifications:
    • Revised
  • AAPG geologic province:
    • New England province
Publication:

Carr, M.H., 1960, The bedrock geology of the Naugatuck quadrangle, with map: Connecticut Geological and Natural History Survey Quadrangle Report, no. 9, 25 p.


Summary:

Unit is restricted to the dark-gray biotite augen gneiss. The interbanded schists are considered part of undifferentiated Hartland formation. Prospect gneiss is always found at same stratigraphic position--between The Straits schist member and the quartzitic member of Hartland formation.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Prospect Gneiss*
  • Modifications:
    • Revised
    • Age modified
  • AAPG geologic province:
    • New England province
Publication:

Fritts, C.E., 1962, Age and sequence of metasedimentary and metavolcanic formations northwest of New Haven, Connecticut; Article 128, IN Geological Survey Research 1962; short papers in geology, hydrology, and topography; Articles 120-179: U.S. Geological Survey Professional Paper, 450-D, p. D32-D36.


Summary:

Name changed from Prospect porphyritic gneiss to Prospect Gneiss. Intrudes the Straits Schist (redefined) and the Southington Mountain Schist (new). Age stated as Ordovician or Devonian.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Prospect Gneiss*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • New England province

Map showing publication footprint
  • Usage in publication:
    • Prospect Formation
  • Modifications:
    • Revised
    • Age modified
  • AAPG geologic province:
    • New England province
Publication:

Crowley, W.P., 1968, The bedrock geology of the Long Hill and Bridgeport quadrangles, Connecticut: Connecticut Geological and Natural History Survey Quadrangle Report, no. 24, 81 p.


Summary:

Prospect Formation assigned to Hartland Group. Subdivided into newly named Golden Hill Schist Member, Beardsley Gneiss Member, and Pumpkin Ground Member. Age shown as Middle and Late Ordovician(?).

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Prospect Gneiss*
  • Modifications:
    • Geochronologic dating
  • AAPG geologic province:
    • New England province
Publication:

Marvin, R.F., and Dobson, S.W., 1979, U.S. Geological Survey radiometric ages; Compilation "B": Isochron/West, no. 26, p. 3-32.


Summary:

Pg. 15, geologic time scale (inside front cover). Prospect Gneiss. Two samples from gneiss in hydrothermally altered zone, and granodiorite gneiss, in Southington quadrangle, New Haven County, Connecticut, yielded Pb-alpha age of 450 +/-50 Ma (zircon); reconnaissance age, zircons may be detrital. Age published by Fritts (1962); recalculated using decay constants of Steiger and Jager, 1977 (Earth Planet. Sci. Letters, v. 36, p. 359-362).

Source: Publication.


Map showing publication footprint
  • Usage in publication:
    • Prospect Gneiss*
  • Modifications:
    • Revised
    • Age modified
  • AAPG geologic province:
    • New England province
Publication:

Rodgers, John, 1985, Bedrock geological map of Connecticut: Connecticut Geological and Natural History Survey, scale 1:125,000


Summary:

Prospect Gneiss is mapped in the Connecticut Valley synclinorium in CT and includes the Beardsley and Pumpkin Ground Members, elsewhere assigned to the Harrison Gneiss. Golden Hill Schist Member is removed from the Prospect and raised to formation rank as the Golden Hill Schist. Indicated age of the Prospect is Middle(?) Ordovician.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Mt. Prospect [Prospect] Formation
  • Modifications:
    • Overview
  • AAPG geologic province:
    • New England province
Publication:

Panish, P.T., 1992, The Mt. Prospect region of western Connecticut; mafic plutonism in Iapetus-sequence strata and thrust emplacement onto the North American margin, IN Robinson, Peter, and Brady, J.B., eds., Guidebook for field trips in the Connecticut Valley region of Massachusetts and adjacent states; Volume 2: University of Massachusetts, Department of Geosciences Contribution, New England Intercollegiate Geological Conference, 84th annual meeting, Amherst, MA, October, 9-11, 1992, no. 66, p. 398-423.


Summary:

[It is the opinion of the reviewer that what the author refers to as the Mt. Prospect Formation of the Hartland Group, is actually the Prospect Formation, as the age, location, and lithologies appear similar. The Mount Prospect Complex occurs in the same area and is discussed at length in this article.] Author describes the unit as consisting of gray to brown, commonly rusty-weathering, thinly layered or laminated, sillimanite-garnet-muscovite-plagioclase-quartz-biotite schistose gneiss with subordinate, commonly laminated siliceous granulite, gray quartzite, biotite schist, local coticule, and garnet-cordierite-gedrite granulite. Also contains a mappable amphibolite unit, which is a dark-green, slabby, well foliated, quartz-labradorite-hornblende gneiss. The Hartland Group also includes the Mt. Rat Schist and the Bee Brook Formation in the Cameron's Line thrust sheet and the Litchfield Schist and the Mt. Tom Amphibolite in the Bantam Lake thrust sheet. Map symbol indicates a Cambrian(?) and Ordovician age.

Source: GNU records (USGS DDS-6; Reston GNULEX).


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