Indian River | |
---|---|
Location | |
Country | United States |
State | Connecticut |
County | New Haven |
Physical characteristics | |
Source | Orange, Connecticut |
Mouth | Long Island Sound |
• location | Milford, Connecticut |
• coordinates | 41°13′36″N73°02′11″W / 41.2267639°N 73.0364944°W |
The Indian River is a stream in New Haven County in the U.S. state of Connecticut. [1] It rises in Orange and flows through Milford before discharging into Long Island Sound at Gulf Pond.
Bodies of water along the stream include Clark Pond and Roses Mill Pond in Milford and Indian Lake bordering Milford and Orange. Stubbly Plain Brook and Silver Brook are tributaries. Fish supported by the stream include the American eel and alewife. A fish ladder helps fish reach spawning grounds at Clark's Pond. [2]
Sherman is the northernmost and least populous town of Fairfield County, Connecticut, United States. The population was 3,527 at the 2020 census. The town is part of the Western Connecticut Planning Region. The town was formed in 1802 from the northern part of New Fairfield. It is named for Roger Sherman, the only person who signed all four founding documents of the United States of America. He also had a cobblers shop in the north end of town which has been reconstructed behind the Northrup House in the center of town.
Milford is a coastal city in New Haven County, Connecticut, United States, between New Haven and Bridgeport. The population was 50,558 at the 2020 United States Census. The city includes the village of Devon and the borough of Woodmont. Milford is part of the South Central Connecticut Planning Region and New York metropolitan area.
The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for 406 miles (653 km) through four states. It rises 300 yards south of the U.S. border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses 11,260 square miles (29,200 km2), covering parts of five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at 18,400 cubic feet (520 m3) per second.
The Housatonic River is a river, approximately 149 miles (240 km) long, in western Massachusetts and western Connecticut in the United States. It flows south to southeast, and drains about 1,950 square miles (5,100 km2) of southwestern Connecticut into Long Island Sound.
The Farmington River is a river, 46.7 miles (75.2 km) in length along its main stem, located in northwest Connecticut with major tributaries extending into southwest Massachusetts. The longest route of the river, from the origin of its West Branch, is 80.4 miles (129.4 km) long, making it the Connecticut River's longest tributary by 2.3 miles (3.7 km) over the major river directly to its north, the Westfield River. The Farmington River's watershed covers 609 square miles (1,580 km2). Historically, the river played an important role in small-scale manufacturing in towns along its course, but it is now mainly used for recreation and drinking water.
The Mascoma River is a 31.6-mile-long (50.9 km) river in western New Hampshire in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. The Mascoma comprises two sections which are split by Mascoma Lake in the communities of Enfield and Lebanon. Counting the lake would add 2.7 miles (4.3 km) to the river's length.
The Johns River, in northern New Hampshire, arises at Cherry Pond in Jefferson and runs approximately 14 miles (23 km), generally northwest, to the Connecticut River. It passes through Hazens Pond, near the Mount Washington Regional Airport, traverses the town of Whitefield, where it is crossed by U.S. Route 3, and then crosses the town of Dalton before joining the Connecticut. It is named for an early hunter and trapper of the area, John Glines, who established a fishing and hunting camp in the area in the 18th century. Another nearby river, the Israel River, is named for John's brother Israel.
Eastman Pond is a 320-acre (1.3 km2) water body located in Sullivan and Grafton counties in western New Hampshire, United States, in the towns of Grantham and Enfield. Water from Eastman Pond flows via Eastman Brook and Stocker Brook to the North Branch of the Sugar River, then the Sugar River, and finally the Connecticut River.
The Naugatuck River is a 40.2-mile-long (64.7 km) river in the U.S. state of Connecticut. Its waters carve out the Naugatuck River Valley in the western reaches of the state, flowing generally due south and eventually emptying into the Housatonic River at Derby, Connecticut and thence 11 miles (18 km) to Long Island Sound. The Plume and Atwood Dam in Thomaston, completed in 1960 following the Great Flood of 1955, creates a reservoir on the river and is the last barrier to salmon and trout migrating up from the sea.
The Oyster River is a 4.1-mile-long (6.6 km) stream located in the state of Connecticut in New Haven County. It flows south through Orange and forms the boundary of West Haven and Orange and flows through Yale University's West Campus. Further downstream, it forms the boundary of West Haven and Milford. It empties into Long Island Sound, just south of Route 162 at Oyster River Point. Swans, box turtles and many other animals call this area home.
The Moosup River is a river in the U.S. states of Rhode Island and Connecticut. It flows approximately 23.7 miles (38.1 km). The river is named after the Native American sachem Maussup.
The Mill River is a river in the U.S. states of Massachusetts and Rhode Island. It flows approximately 17.1 miles (27.5 km).
The Green Fall River is a river in the U.S. states of Connecticut and Rhode Island. It flows approximately 13 km (8 mi).
The Salmon River is formed at the confluence of the Blackledge and Jeremy rivers about one mile west of North Westchester, Connecticut. It drains 96,000 acres and courses for 10.4 miles (16.7 km) to Salmon Cove near Moodus where it flows into the Connecticut River. The Salmon River is probably the largest stream and watershed whose sources and mouth are entirely within the limits of Connecticut.
The Indian Head River rises on the southern boundary of Hanover, Massachusetts and northern boundary line of Hanson, Massachusetts at the intersection of tributaries from Drinkwater River in Hanover and Indian Head Brook in Hanson. The river then flows east along the Hanover-Pembroke border. The river, 3.7 miles (6.0 km) long, is a tributary of the North River, which flows into Massachusetts Bay. The Indian Head River was an important fishing and water pathway for the Massachuset Indian village of Mattakeeset which was located around the Pembroke Ponds.
Meredith Brook is a tributary of the Lackawanna River in Susquehanna County, Lackawanna County, and Wayne County, in Pennsylvania, in the United States. It is approximately 2.1 miles (3.4 km) long and flows through Forest City and Clifford Township in Susquehanna County, Vandling in Lackawanna County, and Clinton Township in Wayne County. In the early 1900s, the stream was clear in its lower reaches despite receiving water from a borehole and culm banks. There are two shallow lakes in the watershed: Lake Erie and Kennedy Pond. Various fish inhabit the lakes.
Nine Partners Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately 10 miles (16 km) long and flows through New Milford Township, Harford Township, and Lenox Township. The watershed of the creek has an area of 38.6 square miles (100 km2). The creek has two named tributaries: Butler Creek and Leslie Creek. The surficial geology in the vicinity of Nine Partners Creek includes Wisconsinan Till, alluvium, bedrock, alluvial fan, and wetlands. The creek's drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.
The Wepawaug River is a stream in New Haven County in the U.S. state of Connecticut. It rises in Woodbridge and flows through Orange and Milford before discharging into Milford Harbor on Long Island Sound. The river is dammed at more than ten places. In Orange, dams form the Wepawaug Reservoir, managed by the South Central Connecticut Regional Water Authority and Lake Wepawaug. In Milford, dams form the Upper and Lower Lagoons. Race Brook is a tributary.