Geology of Connecticut

Geology at a Glance

The State has three major geologic regions—the eastern and western highlands, each composed of older, metamorphic rock, and a central valley, largely composed of basalt overlain by sandstone.

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History

    • 1842 James Gates Percival – Report on the Geology of Connecticut
      • In 8 months surveyed the state East to West at 4 mile intervals. The resurveyed again East to West at intervals between the former to bring him in contact with each of the 4600 square miles of the state.
      • He collected estimated 8000 specimens, as well as noted dips, bearings, and formations making it likely the most accurate survey ever conducted of the state
      • However, despite two years of survey and he was “rushed” by the state legislature and wrote a “hasty outline” of over 500 pages
    • 1906 Manual of the Geology of Connecticut and Preliminary Geological Map by William North Rice and Herbert Ernest Gregory
    • 1924 H. H. Robinson – State Geological and Natural History Survey
    • 1977 The Connecticut Assembly names Garnet the state mineral
    • 1985 John Rodgers (compiler) Bedrock Geological Map of Connecticut

Geologic Reports of Parks

State Parks

Other Parks”]

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