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24-654: The current lake was formed from the flooding of three ponds, Rand, Little and Msssenger Ponds in 1865, by a dam across the Fall River, a tributary of the Farmington River created by the Farmington River Power Company. It was used for water storage, ensuring a steady supply of water power for mills along the Farmington River. In the early part of the twentieth century, the rise of the automobile led to

48-556: A 68-foot (21 m) dam with a hydroelectric generator and a fish ladder , dams the river at Windsor, a few miles before the river flows into the Connecticut River. A number of other dams have been built on the river since European settlement, usually to power mills and other industry. A few, such as in Collinsville, are still mostly intact. The Collinsville Renewable Energy Promotion Act (H.R. 316;113th Congress) would instruct

72-461: A local Native man, Manahanoose, burnt a large quantity of tar belonging to John Griffin. Manahanoose was arrested and fined 500 fathoms , or 914.4 meters, of wampum . The local Indians did not possess that vast quantity of wampum, so the coithe sachem , or political leader, of the native community deeded the land to Griffin to avoid the initial alternative penalty determined by the General Court of

96-440: A popular camping, boat launch, and swimming area occupies about a quarter of the shoreline. A private campground, Camp Overflow, is also located on the reservoir. A small marina , D&J Marina, also run a boat launch facility on the north side of the lake. The water level is seasonal, being lowered by about 10 feet (3.0 m) over the winter. The reservoir fills in the spring from snow melt and underground springs. The lake

120-612: 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 Westfield River directly to its north. The Farmington River's watershed covers 609 square miles (1,580 km ). Historically,

144-746: Is also popular with tubers, and the Crystal Rapids section in Collinsville and Unionville, Connecticut, which offers 4 miles (6.4 km) of Class 2 waters. The west branch of the river includes two hydroelectric dams in West Hartland and Colebrook , run by the Metropolitan District Commission of Connecticut . The largest dam on the east branch is the Saville Dam , which impounds the Barkhamsted Reservoir . The Rainbow Dam,

168-437: Is usually at full level by late spring, but in the occasional years of low snow melt and low rainfall, it may remain up to several feet below its typical level. Water is let out of the lake in the fall so that ice will not damage docks and other structures around the lake. This also leads to excellent water quality , as a significant portion of the water is replaced every year. Farmington River The Farmington River

192-699: The Federal Energy Regulatory Commission to issue licenses to the town of Canton, Connecticut , to restart two small power dams along the river. The bill passed the United States House of Representatives on February 12, 2013, but has not yet become law. Water released from or flowing over the Otis Reservoir dam enters the Farmington River just north of Reservoir Road in Otis, Massachusetts. Significant quantities of water are released during

216-506: The Tunxis , a Wappinger people . The Massaco were first encountered by Dutch settlers at the beginning of the 17th century, who referred to the river where they dwelt as the Massaco . Over time, the term Massaco came to refer to the indigenous peoples, the river, the village they occupied, and the land adjacent to the river. The area known as Massaco was transferred to European settlers, when

240-528: The Connecticut, lacking only the Yellow lampmussel , which is found only in the mainstem of the Connecticut from Turners Falls, MA downriver to Windsor, CT. Massaco Massaco was a native settlement near the present-day towns of Simsbury and Canton along the banks of the Farmington River . The small, local Algonquian -speaking Indians who lived there in the 17th and early 18th centuries belonged to

264-647: The Town of Farmington, Connecticut was named by the Connecticut General Assembly, and this was re-affirmed in 1650 by the execution of a deed by the General Assembly and the reservation of land for the "Tunxis Indians" near "Indian Neck" on the east bank of the Farmington River. A group of twenty wigwams existed in Farmington at the beginning of the eighteenth century, but only four or five families resided in

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288-789: The West Branch and main stem. It also hosts a robust population of wild, stream-born trout, which have been found to account for roughly 40% of the river's trout population. The West Branch, in particular, has developed a reputation as one of the best trout streams in the Northeastern United States, owing largely to being a bottom-release tailwater which remains cold, well-oxygenated and especially conducive to sustaining coldwater fish species year-round. The unique "Survivor Strain" brown trout, selectively bred at state hatcheries to be supremely adapted to Connecticut's waters, relies on annual collections of high-quality wild and holdover trout from

312-769: The West Branch. The river has several whitewater sections that are popular for tubing and kayaking. One of these, the colloquial "Upper Farmington" section of the West Branch in New Boston, Massachusetts , is about 7 miles (11 km) long. It is Class 2 through farm and woods scenery to an iron bridge, where kayak and canoe slalom races are held. A second whitewater section is found in Tariffville, Connecticut , consisting of 1.5 miles (2.4 km) of technical Class 2 and Class 3 water with heavy currents. Other whitewater areas include Satan's Kingdom in New Hartford, Connecticut, which

336-661: The base of the Metacomet Ridge , the flow of the Farmington River changes its direction to the northeast, where it eventually joins up with the Connecticut River in Windsor . When Europeans first arrived, the "Tunxis Sepus" territory consisted of a 165-mile square area bounded by Simsbury to the North, Wallingford to the South, to the northwest by Mohawk country, and on the east by the current towns of Windsor, Hartford and Wethersfield. In 1645,

360-581: The bridge crossing the Farmington River downstream at Route 187 , derived its name from the silver plating factory erected in 1840 on the north bank of the river. It was the first factory of its kind in the United States. Several bridges constructed in the 19th century and early 20th century still span the Farmington River to this day. Among these are: The Farmington River is among Connecticut's most heavily stocked trout streams, with over 50,000 brook, brown, rainbow and tiger trout planted in 2022 throughout

384-642: The development of many seasonal cottages along the lake shore. Building took place along most of the lake shore and on many inland lots. These cottages were fairly inexpensive, being purchased by middle-class people: bankers, barbers, tradesmen, construction contractors, and others. A trend that accelerated in the 1980s was for wealthy people to purchase cottages and upgrade or replace them with expensive second homes. This trend continues. Many people from Connecticut and New York use these as weekend or vacation homes. In addition, many have converted their cottages into year-round residences. Tolland State Forest ,

408-654: The fall in order to drop the reservoir water level for the winter. Much of the Farmington River has been designated as part of the United States National Wild & Scenic Rivers System . The first such designation on the river was bestowed in 1994 and included 14 miles of water, mostly along the Farmington River West Branch but also a section of the river's main stem, from Hartland to the New Hartford - Canton town line. In 2019, this designation

432-573: The first 11 miles of its course by the Saville Dam to create the Barkhamsted Reservoir and Lake McDonough, exiting the latter in New Hartford , Connecticut, and joining the West Branch one mile south of the lake. Upper reaches of the river generally flow southward, but the river turns northward in Farmington, Connecticut , and runs mostly north and east until it flows into the Connecticut River in Windsor, Connecticut . Sites built adjacent to

456-562: The lands of the Native American indigenous people called the Massaco , a sub-tribe of the Tunxis , who were affiliated with the Wappinger . The name Tunxis, a word in the Quiripi family of Eastern Algonquian languages , derives from the indigenous term Wuttunkshau for "the point where the river bends". Halfway through the course of the river, in a floodplain in the town of Farmington at

480-550: The river by nomadic peoples at the end of the last Ice Age , c. 12,400 years BP of the Younger Dryas indicate the presence of the earliest peoples to populate the region that would become known as southern New England . In the winter of 2019, the remains of the site were excavated in Avon , along with stone tools and artifacts constructed from materials in neighboring regions. The upper Connecticut and Farmington River valleys were

504-663: 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 headwaters of the Farmington River consist of the East and West Branches. The West Branch begins at the outlet of Hayden Pond in Otis, Massachusetts , while the East Branch begins in Hartland , Connecticut, at the confluence of Pond, Hubbard and Valley Brooks. The East Branch has been impounded along

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528-463: The river, the Connecticut Department of Energy and Environmental Protection , Metropolitan District Commission , National Park Service , Farmington River Watershed Association and Farmington River Anglers Association. The Farmington River and its tributaries are known to contain 11 species of freshwater mussels . The Farmington has the highest mussel species diversity of any tributary to

552-822: The settlement by 1761 The land of the Massaco was subsequently purchased by the Dutch. This and its settlement during the era of the Connecticut Colony are described in the early history of Simsbury . The Spoonville Dam, built on the Farmington River in 1899 below the Tariffville Gorge in East Granby , was breached in the Flood of 1955 and remained as a partial dam for several decades before being removed in July 2012. The dam, as well as

576-549: Was extended 1.1 miles further downstream to the confluence with the Nepaug River . Most of the Farmington River main stem and the Salmon Brook tributary system, totalling 61.7 miles of additional water, were also designated Wild & Scenic in 2019. The Farmington River Coordinating Committee oversees the implementation of management plans for the designated runs of the Farmington River and includes representatives from towns along

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