Crown Point limestone. Adopted the subdivisions of the Chazy proposed by E. Brainerd and H.M. Seely in 1888 (Amer. Geol., v. 2, p. 323-330), as explained under Chazy group, and proposed Crown Point limestone for group B or middle Chazy, probably from exposures at or near Crown Point, Essex County, Champlain Valley, eastern New York. Age is Early Ordovician.
Source: US geologic names lexicon (USGS Bull. 896, p. 549).
Geographically extended the Crown Point limestone to west-central VT. Unit is part of Chazyan succession (Chazy group) and is lowest formation in the group. Overlies the Bridport dolomite of the upper part of the Beekmantown and underlies the Beldens limestone. Thickness is 0 to 150 feet. The Crown Point is of Middle Ordovician age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Revised the Crown Point to the Crown Point member of the Chazy limestone in VT. Consists of massive limestone with characteristic MACLURITES MAGNUS fossils. Overlies the Day Point member and underlies the Valcour member, both of the Chazy limestone. The Crown Point is of Middle Ordovician age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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