(J.B. Hadley, 1938, Geologic map and structure sections of the New Hampshire portion of the Mt. Cube quadrangle).
Baker Pond gneiss in Oliverian magma series. Fine-grained gray gneiss, locally containing microcline phenocrysts. Largely quartz monzonite with some granodiorite. Border phase is dark-greenish-gray quartz diorite gneiss. Included in Oliverian magma series whose age is younger than Lower Devonian and is probably Upper Devonian. [Age of Oliverian Plutonic Suite has since been changed to Middle Ordovician.]
Mapped in the area around Upper Baker Pond, which is located on the border of the Mount Cube and Rumney quadrangles, west-central NH.
Source: US geologic names lexicon (USGS Bull. 1200, p. 196); supplemental information from GNU records (USGS DDS-6; Reston GNULEX).
Shown on accompanying geologic map northeast of Mt. Cube and east of Indian Pond pluton (Bethlehem Gneiss). Age is Ordovician. Consists of foliated granite.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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