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National Geologic Map Database
Geologic Unit: Ten Rod
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Map showing publication footprint
  • Usage in publication:
    • Ten Rod Granite Gneiss
  • Modifications:
    • Revised
    • Overview
    • Areal extent
  • Dominant lithology:
    • Gneiss
    • Granite
  • AAPG geologic province:
    • New England province
Publication:

Skehan, J.W., and Rast, Nicholas, 1990, Pre-Mesozoic evolution of Avalon terranes of southern New England, IN Socci, A.D., Skehan, J.W., and Smith, G.W., eds., Geology of the composite Avalon terrane of southern New England: Geological Society of America Special Paper, 245, p. 13-53.


Summary:

Sterling Plutonic Suite is here restricted to the Hope Valley terrane. (The Hope Valley together with the Esmond-Dedham terrane make up the Avalon superterrane of this report.) The Ponaganset Gneiss and the Ten Rod Granite Gneiss lie within the Esmond-Dedham terrane and are therefore removed from the Sterling. The Ten Rod is pinkish gray to medium gray, medium grained to fine-grained. Consists of a porphyritic and a nonporphyritic phase. Large crystals of pink to tan microcline are distinctive characteristic. Albite-oligoclase, quartz, and biotite also abundant in porphyritic rocks. Generally well-foliated; some lineation. Probable age of emplacement is 601+/-5 Ma (Hermes and Zartman, 1985).

Source: GNU records (USGS DDS-6; Reston GNULEX).


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