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Wampatuck Pond
Wampatuck Pond is a pond in Hanson, Massachusetts. Indian Head Brook both flows in and out of the pond. Along the northern shore of the pond are the Routes 14 and 58 concurrency, Hanson's Town Hall, and a small park. Access to the pond includes a concrete ramp managed by the Town of Hanson suitable for three trailers and six cars. The water quality is impaired due to noxious aquatic plants. External linksEnvironment Protection AgencySouth Shore Coastal Watersheds - Lake Assessments
Ponds of Plymouth County, Massachusetts Ponds of Massachusetts {{PlymouthCountyMA- ...
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Hanson, Massachusetts
Hanson is a town in Plymouth County, Massachusetts, United States. Part of Greater Boston, Hanson is located 20 miles (32 km) south of Boston and is one of the inland towns of the South Shore. The population was 10,639 at the 2020 census. History Hanson was first settled in 1632 as the western parish of Pembroke. The town was officially incorporated in 1820, and was named for Maryland publisher of the ''Federal Republican'' newspaper and U.S. Senator Alexander Contee Hanson. Hanson was a champion of free speech and freedom of the press, and he was severely beaten and his newspaper offices were attacked and destroyed by an angry mob after he published an article that was critical of the administration shortly after the outbreak of the War of 1812. The town's early industry revolved around farming, as well as bog iron and quarrying. Mills also popped up along the rivers during the nineteenth century. Today the town is mostly residential, with some farming and cranberry farm ...
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Massachusetts Route 14
Route 14 is a state highway in southeastern Massachusetts. It runs from Route 27 in Brockton east to Route 3A in Duxbury, near the coastline. Massachusetts Route 3, Route 3 (Pilgrims Highway) has an interchange with Route 14, at Exit 22 (formerly exit 11) in Duxbury. __NOTOC__ Route description From its western terminus at Route 27 in Brockton, Route 14 goes through Whitman, Massachusetts, Whitman south of the center of the town before going the northeastern corner of East Bridgewater, Massachusetts, East Bridgewater, crossing Route 27 once more. In Hanson, Massachusetts, Hanson, the road is concurrent with Massachusetts Route 58, Route 58 through the center of town, past Wampatuck Pond. It passes into Pembroke, Massachusetts, Pembroke between Oldham Pond (Massachusetts), Oldham Pond and Furnace Pond (Pembroke, Massachusetts), Furnace Pond before passing through the center of town. After another concurrency with Massachusetts Route 53, Route 53, the road passes into Duxb ...
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Massachusetts Route 58
Route 58 is a south–north state highway in southeastern Massachusetts. For all but its final , the route lies within Plymouth County. Its southern terminus is at Route 28 at the Rochester– Wareham town line and its northern terminus is at Route 18 in Weymouth. Along the way it intersect several major highways including Interstate 495 (I-495) in Wareham and U.S. Route 44 (US 44) in Carver. Route description Route 58 begins at Route 28 on the Rochester– Wareham town line. The route follows the town line for approximately a tenth of a mile before being wholly in Wareham. It then crosses I-495 before clipping the corner of Middleborough and re-entering Wareham for a short while before finally entering Carver. For the first of this route, none of the town line changes are signed. The route turns northward through the town of Carver, passing Edaville Railroad and the King Richard's Faire grounds as well as the center of town. In North Carver the town intersects U. ...
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Ponds Of Plymouth County, Massachusetts
A pond is an area filled with water, either natural or artificial, that is smaller than a lake. Defining them to be less than in area, less than deep, and with less than 30% emergent vegetation helps in distinguishing their ecology from that of lakes and wetlands.Clegg, J. (1986). Observer's Book of Pond Life. Frederick Warne, London Ponds can be created by a wide variety of natural processes (e.g. on floodplains as cutoff river channels, by glacial processes, by peatland formation, in coastal dune systems, by beavers), or they can simply be isolated depressions (such as a kettle hole, vernal pool, prairie pothole, or simply natural undulations in undrained land) filled by runoff, groundwater, or precipitation, or all three of these. They can be further divided into four zones: vegetation zone, open water, bottom mud and surface film. The size and depth of ponds often varies greatly with the time of year; many ponds are produced by spring flooding from rivers. Ponds may be ...
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