Rhode Island
Jerimoth Hill |
Metamorphic (metamorphosed igneous) |
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Bedrock: Esmond Igneous Suite |
Late Proterozoic |
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Bedrock is not exposed at the highest point, but the granitic gneiss boulder there, as well as blocks along Rt.101, provide a close look at the rock. Formerly mapped as the Ponaganset gneiss, the rock is light to dark gray, fine to coarse porphyritic and porphyroblastic gneiss, commonly foliated, with oval biotite lineation splotches. The main minerals are microcline, plagioclase, quartz, biotite, plus or minus hornblende and muscovite. The Esmond Suite is part of the Avalon Terrane, which was accreted to North America in the Late Paleozoic. The highpoint lies about two miles east of a right-lateral strike-slip fault that separates the Esmond-Dedham subterrane from the Hope Valley subterranes to the west, all part of Avalon. Surficial Geology: Thin glacial till overlying bedrock. Soil Series: Gloucester stony fine sand loam: Light grayish-brown to yellowish-brown in the subsoil, well drained, acidic, formed on granitic glacial till. |
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