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The Fenton River runs through Mansfield, Storrs, and Willington, as well as small parts of Windham, all but the latter in Tolland County, Connecticut spanning 18.895 miles (about 30.408 kilometers). It feeds into Mansfield Hollow reservoir at its end, making it a tributary to the Mount Hope , Natchaug , and Willimantic rivers.
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The Airline Trail South crosses the Willimantic River to enter Willimantic on a 2016 built path that ends at Bridge St. [76] [77] The Airline Trail North starts on Jackson St. across the street from Jillson Park, the trail then goes through the northeastern part of Willimantic before crossing the Natchuag River to leave the CDP and heading on ...
Location: Mansfield & Windham, Connecticut: Coordinates: 1]: Type: Reservoir: Primary inflows: Natchaug River, Fenton River, Mount Hope River: Primary outflows: Natchaug River: Catchment area: 163 sq mi (420 km 2) [2]: Basin countries: United States: Max. length: 2.2 miles (3.5 km): Max. width: 2,400 feet (730 m): Surface area: 440 acres (180 ha): Normal pool [2]: Max. depth: 23 ft (7.0 m) [2 ...
The Prospect Hill Historic District encompasses a large residential area in the Willimantic section of Windham, Connecticut. Located north of the Main Street commercial district, it was developed between about 1865 and 1930, and is one of the state's largest historic districts, with more than 800 contributing buildings. It is roughly bounded by ...
Copper River Grill, a South Carolina-based regional chain serving American cuisine, closed permanently amid the COVID-19 pandemic in 2020. ... The lunch menu is available from 11 a.m.- 3 p.m ...
Gurleyville is located what is now a rural setting of north-central Mansfield, Connecticut.The historic district is bounded on the west mostly by the Fenton River, historically the source of power for the village's mills, and the south by the junction of Stone Mill and Grist Mill Roads.
The Shetucket River is a tributary of the Thames River, 20.4 miles (32.8 km) long, [2] in eastern Connecticut in the United States. It is formed at Willimantic by the junction of the Willimantic and Natchaug rivers.