Connecticut Valley Synclinorium (CT Geology)

Connecticut Valley Synclinorium (CT Geology)

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Connecticut's geological landscape is shaped by several tectonic terranes, one of which plays a significant role. A clear boundary between these terranes can be determined using the Connecticut GIS Bedrock Geology Map provided by the CT DEEP. To obtain accurate elevation data, researchers rely on the 1/3 arcsec digital elevation model available from the USGS National Map. This model does, however, exhibit gaps in certain areas: notably, the Waterbury Dome and a narrow strip of the Newark Basin, both of which belong to distinct geological periods - an older Proto-North America terrane and younger rifting respectively.

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