(J.B. Hadley, 1938, Geologic map and structure sections of the New Hampshire portion of the Mt. Cube quadrangle).
Piermont member of Albee formation. Consists of dark-gray quartz-mica schist, mica schist, staurolite schist and local beds of fine conglomerate, of volcanic origin in part, interbedded with the schists and quartzites of the Albee formation. Age is Late Ordovician(?).
Source: US geologic names lexicon (USGS Bull. 1200, p. 3012-3013).
Pg. 117, 119 (fig. 2), 126-127. Piermont member of Albee formation. Maximum thickness estimated 1,000 feet. Occurs about 1,000 feet above base of Albee formation. Type locality cited.
Type locality: Mt. Cube area, in and near village of Piermont, [Mt. Cube 15-min quadrangle], Grafton Co., western NH.
Source: US geologic names lexicon (USGS Bull. 1200, p. 3012-3013).
Map; M.P. Billings, 1956, Geol. New Hampshire, Pt. 2 Bedrock geol., p. 16. Piermont member of Albee formation. Gray to dark-gray mica schists with porphyoblasts of biotite, garnet, and/or staurolite. Confined to area around Piermont, [Grafton County, New Hampshire]. Lies in staurolite metamorphic zone. Age is Ordovician(?).
Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 3012-3013).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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