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National Geologic Map Database
Geologic Unit: Stissing
Map showing publication footprint
  • Usage in publication:
    • Stissing dolomite
  • Modifications:
    • Named
  • Dominant lithology:
    • Dolomite
  • AAPG geologic province:
    • New England province
Publication:

Knopf, E.B., 1946, Stratigraphy of the Lower Paleozoic rocks surrounding Stissing Mountain, Dutchess County, New York [abs.]: Geological Society of America Bulletin, Chicago, December 26-28, 1946, v. 57, no. 12, pt. 2, p. 1211-1212.


Summary:

The Stissing dolomite is light-colored dolomites carrying HYOLITHELLUS MICANS Billings in four localities. Upper part is dark dolomites carrying PATERINA STISSINGENSIS Dwight and PROZACANTHOIDES STISSINGENSIS Dwight in two localities. These species indicate the unit is of late Early Cambrian age. The Stissing is 500 feet thick. It underlies the Pine Plains formation and overlies the Poughquag quartzite.

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


Map showing publication footprint
  • Usage in publication:
    • Stissing Dolomite*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • New England province
Publication:

Ratcliffe, N.M., and Burton, W.C., 1990, Bedrock geologic map of the Poughquag quadrangle, New York: U.S. Geological Survey Geologic Quadrangle Map, GQ-1662, 1 sheet, scale 1:24,000 [http://ngmdb.usgs.gov/Prodesc/proddesc_440.htm]


Summary:

The Stissing Dolomite is here assigned to the Wappinger Group. Overlies Poughquag Quartzite; underlies Pine Plains Formation of the Wappinger Group.

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


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).