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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. The confluence of the west and east branches of the Sippican River The Sippican River ("long river") is a short river in Massachusetts, United States. The Sippican River is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 arising fro ... 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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Rochester, Massachusetts
Rochester is a town in Plymouth County, Massachusetts, United States. The population was 5,717 at the 2020 census. 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, Marion and parts of 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, England, from which early settlers to the town came. The town originally thrived with the early shipbuilding and whaling trade in Mattapoisett Harbor. However, in 1852 and 1857 the towns of Marion and Mattapoisett, respectively, were separated and incorporated as separate towns, thus landlocking Rochester. Since that time, the town has become mostly rural-residential, with some farms located in town. Rochester is a " Right to Farm" community. Geography Accordin ...
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Sippican River
The Sippican River ("long river") is a short river in Massachusetts, United States. The Sippican River is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 arising from east and west branches in the towns of Mattapoisett, Marion (once known as Sippican), and Rochester, Massachusetts. Each branch flows through a complex system of cranberry bogs and reservoirs, and empties a short distance away through Wareham into Buzzards Bay near the Weweantic River mouth In animal anatomy, the mouth, also known as the oral cavity, or in Latin cavum oris, is the opening through which many animals take in food and issue vocal sounds. It is also the cavity lying at the upper end of the alimentary canal, bounded on t .... As of 2006, efforts are underway to restore the native alewife population to the river. References Marion, Massachusetts Rochester, Massachusetts Wareham, Massachusetts Rivers of Pl ...
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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, United States. The population was 5,717 at the 2020 census. History Rochester was settled in 1679 on the lands called "Sippican" by the local Wampanoags, along the coast of Buzzards Bay. .... 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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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 m ...
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