Geologic evolution of the lower Connecticut River valley: Influence of bedrock geology, glacial deposits, and sea level
This fieldtrip illustrates the character of the lower Connecticut River bedrock valley, in particular its depth, and the lithology and structure of bedrock units it crosses. It examines the character and distribution of the glaciodeltaic terraces that partially fill the valley and discusses the depth of postglacial incision into them.
Connecticut↗