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Gilman-Hayden House

East Hartford, ConnecticutGeorgian architecture in ConnecticutHouses completed in 1784Houses in Hartford County, ConnecticutHouses on the National Register of Historic Places in Connecticut
National Register of Historic Places in Hartford County, Connecticut
GilmanHaydenHouseEastHartfordCT
GilmanHaydenHouseEastHartfordCT

The Gilman-Hayden House is a historic house at 1871 Main Street in East Hartford, Connecticut. Built in 1784, it is a good local example of Georgian architecture, and is also notable as the home of Edward Hayden, a diarist of the American Civil War. It was listed on the National Register of Historic Places in 1984.

Excerpt from the Wikipedia article Gilman-Hayden House (License: CC BY-SA 3.0, Authors, Images).

Gilman-Hayden House
Main Street,

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Latitude Longitude
N 41.791666666667 ° E -72.633611111111 °
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Main Street 1873
06108
United States
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GilmanHaydenHouseEastHartfordCT
GilmanHaydenHouseEastHartfordCT
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Lake Hitchcock
Lake Hitchcock

Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, creating the long, narrow lake. The lake existed for approximately 3,000 years, after which a combination of erosion and continuing geological changes likely caused it to drain. At its longest, Lake Hitchcock stretched from the moraine dam at present-day Rocky Hill, Connecticut, to St. Johnsbury, Vermont (about 320 kilometres (200 mi)). Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook. Lake Hitchcock is an important part of the geology of Connecticut. It experienced annual layering of sediments, or varves: silt and sand in the summertime (due to glacial meltwater) and clay in the wintertime (as the lake froze). Analysis of varves along Canoe Brook in Vermont was conducted by John Ridge and Frederick Larsen, including radiocarbon dating of organic materials. Their research indicates that the lake formed sometime prior to around 15,600 years ago. Later, abrupt changes in sediment composition around 12,400 years ago appear to mark the initial breaching of the lake's dam. These varved lake deposits were later used by European settlers for brick-making. The lake was named after Edward Hitchcock (1793–1864), a geology professor from Amherst College who had studied it.