Figure 3. Generalized bedrock geologic map of The Forks quadrangle which includes the boundary, interpreted as an angular unconformity, between older rocks of Cambrian and Ordovician age, and younger rocks of Silurian and Devonian age. The primary unit exposed at Moxie Falls is The Forks Formation of Silurian age shown in light green.

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Last updated on January 6, 2006.

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