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Lout Pond
Lout Pond is an kettlehole pond in Plymouth, Massachusetts, east of Billington Sea, southeast of Morton Park, and northwest of Cooks Pond Cook or The Cook may refer to: Food preparation * Cooking, the preparation of food * Cook (domestic worker), a household staff member who prepares food * Cook (professional), an individual who prepares food for consumption in the food industry * .... The pond has an average depth of and a maximum depth of . The northern and southern shores have been developed extensively. Cranberry bogs are along the western shore, and Billington Street runs along the eastern shore. Parking is available along the side of the road; however, due to the steep bank only canoes and car top boats can be launched, electric motors only. "Lout" is a name derived from the Latin ''lout'', meaning "clay" or "mud". References External linksMassWildlife - Pond Map and Info Ponds of Plymouth, Massachusetts Ponds of Massachusetts {{PlymouthCountyMA-geo-stub ...
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Plymouth, Massachusetts
Plymouth (; historically known as Plimouth and Plimoth) is a town in Plymouth County, Massachusetts, United States. Located in Greater Boston, the town holds a place of great prominence in American history, folklore, and culture, and is known as "America's Hometown". Plymouth was the site of the colony founded in 1620 by the ''Mayflower'' Pilgrims, where New England was first established. It is the oldest municipality in New England and one of the oldest in the United States. The town has served as the location of several prominent events, one of the more notable being the First Thanksgiving feast. Plymouth served as the capital of Plymouth Colony from its founding in 1620 until the colony's merger with the Massachusetts Bay Colony in 1691. The English explorer John Smith named the area Plymouth (after the city in South West England) and the region 'New England' during his voyage of 1614 (the accompanying map was published in 1616). It was a later coincidence that, after an ab ...
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Kettle (geology)
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluviog ...
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Billington Sea
Billington Sea (also Billington's Sea) is a warm water pond located in Plymouth, Massachusetts. Morton Park lies on the pond's northern shore. The pond is fed by groundwater and cranberry bog outlets. The average depth is seven feet and the maximum depth is . The pond provides the headwaters to Town Brook. Seymour Island is located in the center of the pond. Billington Sea was named after its discoverer, Francis Billington, one of the passengers on the ''Mayflower''. Description Billington Sea is located southwest of the center of Plymouth, Massachusetts, west of Massachusetts Route 3 and south of U.S. Route 44. It is 269 acres in surface area with depth averaging 7 feet, with an 11-foot maximum depth. It is a warmwater eutrophic pond with extensive aquatic vegetation and a mostly mud bottom, though with sandy shorelines. Apart from a town park on the northern shore, most of the shoreline is occupied by private residential property. History Billington's Sea was discovered in Jan ...
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Morton Park (Massachusetts)
Morton Park is a park in Plymouth, Massachusetts Plymouth (; historically known as Plimouth and Plimoth) is a town in Plymouth County, Massachusetts, United States. Located in Greater Boston, the town holds a place of great prominence in American history, folklore, and culture, and is known as ..., located west of Route 3 and northwest of Lout Pond with its main entrance off Summer Street and its rear entrance off Billington Street. It is Plymouth's largest park area consisting of of forest, the shoreline of Little Pond, the northern shoreline of Billington Sea, the headwaters to Town Brook, and over two miles (3 km) of footpaths. Morton Park was established in 1889, with funding from citizens of Plymouth as well as several landowners, including Dr. LeBaron Russell. The effort was led by Nathaniel Morton, for whom the park is named. External linksTown of Plymouth Parks, Playgrounds and Beaches
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Cooks Pond (Plymouth, Massachusetts)
Cooks Pond is a reservoir in Plymouth, Massachusetts. The pond is within the Eel River watershed, located north of South Pond village, near '' The Shops at 5'' and the main Post Office, and southeast of Lout Pond Lout Pond is an kettlehole pond in Plymouth, Massachusetts, east of Billington Sea, southeast of Morton Park, and northwest of Cooks Pond Cook or The Cook may refer to: Food preparation * Cooking, the preparation of food * Cook (domestic work .... The pond suffers from trash along the northern shore as well as erosion at the access point on the north side of the pond, each of which was noted in a 2002 field inspection. The pond was named after Jacob Cook, the original owner of the site. References External linksEnvironmental Protection Agency Ponds of Plymouth, Massachusetts Ponds of Massachusetts {{PlymouthCountyMA-geo-stub ...
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Ponds Of Plymouth, 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 f ...
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