Publisher's Synopsis
Excerpt from Drainage Modifications and Glaciation in the Danbury Region, Connecticut
The region discussed in this bulletin is situated in western Connecticut and is approximately 8 miles wide and 18 miles long in a north-south direction, as shown on fig. Throughout, the rocks are crystalline and include gneiss, schist, and marble the metamorphosed equivalents Of a large variety Of ancient sedimentary and igneous rocks.
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