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During Ice Ages, glacial activity shaped much of New England’s landscape, eroding mountains, leaving glacial till scattered everywhere, and forming glacial lakes. At its greatest extent, one of these glaciers left behind a moraine which became today's Long Island.
They represent the geological and ecological history of Connecticut, including glacial features such as bogs, old growth forests and swamps. There are also well preserved dinosaur tracks, There are also well preserved dinosaur tracks,
It was first identified in 1985 as a single geologic feature consisting of trap rock by the State Geological and Natural History Survey of Connecticut. [4] A 2004 report conducted for the National Park Service extends that definition to include the entire traprock ridge from Long Island Sound to the Pocumtuck Range in Greenfield, Massachusetts. [1]
For-profit genealogy company. Databases include Find a Grave, RootsWeb, a free genealogy community, and Newspapers.com. Archives.gov: US National Archives and Records Administration. Free online repository with a section dedicated to genealogical research [1] BALSAC: Population database of Quebec, Canada Cyndi's List
The hill is composed mostly of high-purity milky quartz and it occupies the inactive Lantern Hill Fault, which runs south into the Atlantic Ocean. Analysis of the quartz reveals that it is 238 million years old—the mid-Triassic Period of the Mesozoic Era in geologic time, according to current theories. The formation of the fault and the ...
A Committee to locate a mill at the first falls on the Quinnipiac River between Wallingford and Meriden was held in September 1686. In 1704 the mill was sold to William Tyler, and the community became known as Tyler's Mills.
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