Sherman Marble of Hubbard (1924) redefined and restricted stratigraphically and geographically to include only rocks at type locality and adjacent Whitingham area as used by Skehan (1961). Other occurrences outside type locality shown as Sherman Marble by Skehan, interbedded with albitic schists, are probably Proterozoic Z or Early Cambrian in age and may be regarded as correlatives of part of Hoosac Formation. Sherman is interbedded with Wilmington Gneiss of Skehan (1961) and unconformably underlies Readsboro Formation of Skehan (1961). Age is Proterozoic Y [no explanation given for age].
Source: GNU records (USGS DDS-6; Reston GNULEX).
Used as Sherman Marble of Proterozoic Y age. Occurs at Sherman Reservoir at State line.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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