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Mary's Pond
Mary's Pond, also known as Marys Pond, is an kettle pond in Rochester, Massachusetts Rochester is a town in Plymouth County, Massachusetts, Plymouth County, Massachusetts, United States. The population was 5,717 at the 2020 census. Rochester is a part of the South Coast (Massachusetts), South Coast region of Massachusetts which ..., United States. The pond is located east of Leonards Pond. The average depth is , and the maximum depth is . Rochester's town beach is located on the northwestern shore of the pond along Mary's Pond Road. In 2011, amid plans to create a recreation area on the popular beach, a title search revealed that the beach was privately owned. Although the town of Rochester maintains Mary's Pond Road through an easement, and although the State of Massachusetts maintains the pond itself, the beach is now closed to the public. References External linksMassWildlife - Pond Map and info
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Rochester, Massachusetts
Rochester is a town in Plymouth County, Massachusetts, Plymouth County, Massachusetts, United States. The population was 5,717 at the 2020 census. Rochester is a part of the South Coast (Massachusetts), South Coast region of Massachusetts which encompasses the cities and towns that surround Buzzards Bay (excluding the Elizabeth Islands, Bourne, Massachusetts, Bourne and Falmouth, Massachusetts, Falmouth), Mount Hope Bay and the Sakonnet River. History Rochester was settled in 1679 on the lands called "Sippican" by the local Wampanoags, along the coast of Buzzards Bay. (''Sippican'' was the name of the local tribe.) It originally included the lands of Mattapoisett, Massachusetts, Mattapoisett, Marion, Massachusetts, Marion and parts of Wareham, Massachusetts, Wareham (which was lost when Wareham was founded in 1739). The town was officially incorporated on June 4, 1686, as Rochester, and was named for Rochester, Kent, Rochester, England, from which early settlers to the town c ...
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Kettle Pond
A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or 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 and 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 acidic conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are ...
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Leonards Pond (Rochester, Massachusetts)
Leonards Pond, also known as Leonard's Pond, is a pond in Rochester, Massachusetts. The pond is located west of Mary's Pond Mary's Pond, also known as Marys Pond, is an kettle pond in Rochester, Massachusetts Rochester is a town in Plymouth County, Massachusetts, Plymouth County, Massachusetts, United States. The population was 5,717 at the 2020 census. Rocheste .... The confluence of the west and east branches of the Sippican River is at this pond, and the Sippican River continues as the outflow. External linksEnvironmental Protection Agency Ponds of Plymouth County, Massachusetts Rochester, Massachusetts Ponds of Massachusetts {{PlymouthCountyMA-geo-stub ...
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Ponds Of Plymouth County, Massachusetts
A pond is a small, still, land-based body of water formed by pooling inside a depression, either naturally or artificially. A pond is smaller than a lake and there are no official criteria distinguishing the two, although defining a pond to be less than in area, less than in depth and with less than 30% of its area covered by emergent vegetation helps in distinguishing the ecology of ponds from those 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). 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, botto ...
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