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Bascom Formation, and undifferentiated Luke Hill, Naylor Ledge and Hastings Creek Limestones

Bascom Formation, and undifferentiated Luke Hill, Naylor Ledge and Hastings Creek Limestones - Interbedded dolomite, limestone or marble, calcareous sandstone, quartzite and limestone breccia; irregular dolomitic layers, thin sandy laminae, and slaty or phyllitic partings characterize limestone and marble of lower, middle, and upper parts of the Bascom, respectively; south of West Rutland it includes some of the Chipman formation. The combined Luke Hill, Naylor Ledge, and Hastings Creek, east of Philipsburg thrust, are stratigraphically equivalent to the Bascom.
StateVermont
NameBascom Formation, and undifferentiated Luke Hill, Naylor Ledge and Hastings Creek Limestones
Geologic ageOrdovician
Original map labelOb
CommentsPart of Champlain and Vermont Valleys, Beekmantown Group Secondary unit desription per VT012: Bascom Subgroup is defined as the entire carbonate clastic succession of the Beekmantown, representing the core of the group. This sequence was referred to as "Calciferous sand-rock" by Eaton (1824). Bascom name is appropriate since Bascom Ledges consist of various portions of this sequence. Included within this Subgroup are (ascending) Cutting Hill Formation (Cutting Formation redefined and renamed), Lemon Fair Formation (named), and Fort Cassin Formation. Unit overlies Whitehall Dolostone and underlies Providence Island Formation, both of Beekmantown Group. Age is Early Ordovician. [Rank of subgroup is not recognized in the NACSN.] (Washington and Chisick, 1988).
Primary rock typedolostone (dolomite)
Secondary rock typelimestone
Other rock typesmarble; sandstone; quartzite; sedimentary breccia
Lithologic constituents
Minor
Metamorphic > Metasedimentary > Metaclastic > Quartzite
Sedimentary > Clastic > Sandstone (Calcareous)
Metamorphic > Metasedimentary > Metacarbonate > Marble (Bed)irregular dolomitic layers, thin sandy laminae, and slaty or phyllitic partings characterize limestone and marble of lower, middle, and upper parts of the Bascom, respectively
Sedimentary > Carbonate > Limestone (Bed)irregular dolomitic layers, thin sandy laminae, and slaty or phyllitic partings characterize limestone and marble of lower, middle, and upper parts of the Bascom, respectively
Sedimentary > Carbonate > Dolostone (Bed)irregular dolomitic layers, thin sandy laminae, and slaty or phyllitic partings characterize limestone and marble of lower, middle, and upper parts of the Bascom, respectively
Incidental
Sedimentary > Clastic > Sedimentary-breccia (Bed)limestone breccia
Map references
Nicholson, S.W., Dicken, C.L., Horton, J.D., Foose, M.P., Mueller, J.A.L., and Hon, Rudi, 2006, Preliminary integrated geologic map databases for the United States: Connecticut, Maine, Massachusetts, New Hampshire, New Jersey, Rhode Island, and Vermont: U.S. Geological Survey Open-File Report 2006-1272.
Unit references
Doll, C.G., Cady, W.M., Thompson, J.B., Jr., and Billings, M.P., 1961, Centennial Geologic Map of Vermont: Vermont Geological Survey, Miscellaneous Map MISCMAP-01, scale 1:250,000.
Ratcliffe, N.M., 1994, Changes in stratigraphic nomenclature in the eastern cover sequence in the Green Mountain massif from Ludlow to West Bridgewater, Vermont, IN Stratigraphic notes, 1992: U.S. Geological Survey Bulletin, 2060, p. 1-10.
Geographic coverageAddison - Bennington - Chittenden - Franklin - Grand Isle - Rutland

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