The North Branch of the Millers River is a river in southwestern New Hampshire and northern Massachusetts in the United States. It is a tributary of the Millers River, which flows west to the Connecticut River, which in turn flows south to Long Island Sound, an arm of the Atlantic Ocean.
The North Branch rises in Rindge, New Hampshire, at the outlet of Island Pond. It flows west past East Rindge and Converseville to Lake Monomonac. From the lake's outlet in Massachusetts, the North Branch flows south parallel to U.S. Route 202, joining the Millers River at Whitney Pond in Winchendon.
The North Branch is 6.0 miles (9.7 km) long, 4.0 miles (6.4 km) of which are in New Hampshire, with 2.0 miles (3.2 km) in Massachusetts. If the channel length of 2.9 miles (4.7 km) through Lake Monomonac were included, the total length would be 8.9 miles (14.3 km).
Dublin Pond or Dublin Lake is a 236-acre (0.96 km2) water body located in Cheshire County in southwestern New Hampshire, United States, in the town of Dublin. The pond lies at an elevation of 1,480 feet (451 m) above sea level, near the height of land between the Connecticut River/Long Island Sound watershed to the west and the Merrimack River/Gulf of Maine watershed to the east.Lake Monomonac
Lake Monomonac is an artificial lake that straddles the border between Rindge, New Hampshire, and Winchendon, Massachusetts, in the United States. It was created from a small pond in New Hampshire by the construction of dams on the North Branch of the Millers River, a part of the Connecticut River watershed.
Lake Monomonac is 594 acres (240 ha) in size, with 411 acres (166 ha) in New Hampshire and the remaining 183 acres (74 ha) in Massachusetts. The lake has a maximum recorded depth of 22 feet (6.7 m) and an average depth of 10 feet (3.0 m).The lake is classified as a warmwater fishery, with observed species including smallmouth and largemouth bass, black crappie, chain pickerel, white perch, pumpkinseed, bluegill, horned pout, and green sunfish.List of rivers of Massachusetts
List of rivers in Massachusetts (U.S. state).
All Massachusetts rivers flow to the Atlantic Ocean. The list is arranged by drainage basin from north to south, with respective tributaries indented under each larger stream's name, arranged travelling upstream along the larger stream.List of rivers of New Hampshire
This is a list of rivers and significant streams in the U.S. state of New Hampshire.
All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to the New Hampshire Comprehensive Shoreland Protection Act or are more than 10 miles (16 km) long. New Hampshire rivers and streams qualify for state shoreland protection (and are listed here in bold) if they are fourth-order or larger water bodies, based on the Strahler method of stream order classification.Saville Dam
Saville Dam is an earthen embankment dam with masonry work on the eastern branch of the Farmington River in southwestern Barkhamsted, Connecticut. The dam is 135 ft. (41 m) tall and 1,950 ft. (590 m) long and has an uncontrolled spillway on its western portion. It creates the Barkhamsted Reservoir which has a volume of 36.8 billion US gallons (139,000,000 m3) and is the primary water source for Hartford, Connecticut.
In 1927, the Metropolitan District Commission began to purchase land in the present-day footprint of the dam and reservoir. Construction of the dam commenced in 1936 while land to the north was being stripped of lumber and buildings.
Before the Metropolitan District Commission named the Saville Dam in 1940 in honor of its chief engineer, Caleb Mills Saville, it was referred to as the Bill's Brook Dam after the brook that ran near the site at the time.
The foundations for "Bill's Brook Dam" and the diversion tunnel for the East Branch of the Farmington River were completed in August 1934. Subsequently, the East Branch was diverted into the concrete conduit at the bottom of the Bill's Brook Dam site. The dam was completed in May 1940, at a total cost for dam and reservoir of $10M.Although the Saville Dam was completed in 1940, it was not until 1948 that the Barkhamsted Reservoir finally filled to capacity. The Farmington River East Branch is impounded for nearly 8 miles (13 km) behind the dam, with the northernmost open waters of Barkhamsted Reservoir terminating in Hartland, Connecticut just south of the Massachusetts border.The reservoir flooded many buildings and farms of Barkhamsted, including the village of Barkhamsted Hollow. The village of Barkhamsted Center, partially flooded, lies just to the west of the reservoir. Its remaining buildings are part of the Barkhamsted Center Historic District, listed on the National Register of Historic Places.
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