The topic of Comerford Reservoir is one that has captured the attention of many people in recent years. Since its emergence, Comerford Reservoir has generated a continuous debate in different sectors of society, whether in the academic, political, economic or cultural spheres. Opinions regarding Comerford Reservoir vary greatly, and its impact has become evident in various spheres. In this article, we will explore various perspectives on Comerford Reservoir and its influence today, as well as its historical relevance. Additionally, we will analyze the role that Comerford Reservoir plays in people's daily lives and in society as a whole.
Comerford Reservoir | |
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Location | Caledonia County, Vermont; Grafton County, New Hampshire |
Coordinates | 44°19′31″N 72°0′03″W / 44.32528°N 72.00083°W |
Type | Reservoir |
Primary inflows | Connecticut River |
Primary outflows | Connecticut River |
Basin countries | United States |
Max. length | 7.3 mi (11.7 km) |
Max. width | 1.1 mi (1.8 km) |
Surface area | 1,029 acres (4 km2) |
Surface elevation | 647 ft (197 m) |
Settlements | Monroe, NH Littleton, NH Barnet, VT Waterford, VT |
Comerford Reservoir is a 1,029-acre (4 km2) impoundment located on the Connecticut River on the boundary between Vermont and New Hampshire in the United States. The reservoir is formed by the Frank D. Comerford Dam in the towns of Monroe, New Hampshire, and Barnet, Vermont, and impounds water into the towns of Littleton, New Hampshire, and Waterford, Vermont, nearly to the Moore Reservoir upstream on the Connecticut.