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Barrett Pond (Carver, Massachusetts)
Barrett Pond is a , warm water pond in the Myles Standish State Forest in Carver, Massachusetts, located less than ½ mile north of the forest headquarters, west of East Head Reservoir, and southwest of College Pond in Plymouth Plymouth () is a port city and unitary authority in South West England. It is located on the south coast of Devon, approximately south-west of Exeter and south-west of London. It is bordered by Cornwall to the west and south-west. Plymouth .... The pond has an average depth of six feet and a maximum depth of . Most of the shoreline is undeveloped except for a campground area on the eastern shore. Access is possible off Lower College Pond Road and is suitable only for car top boats or canoes, electric motors only. External linksMassWildlife - Pond Maps Ponds of Plymouth County, Massachusetts Ponds of Massachusetts {{PlymouthCountyMA-geo-stub ...
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Carver, Massachusetts
Carver is a town in Plymouth County, Massachusetts, United States. The population was 11,645 at the 2020 census. It is named for John Carver, the first governor of the Plymouth Colony. The town features two popular tourist attractions: Edaville USA theme park and King Richard's Faire, the largest and longest-running renaissance fair in New England. History and overview Archaeological research revealed 9,000 years of settlement at the Annasnappet Pond Site in Carver, from 10,000 to 1,000 years ago. The site contained 100,000 stone flakes, 1600 stone tools and a human burial. Carver separated from Plympton, Massachusetts, and was incorporated in 1790 because many residents lived too far away to attend church in Plympton. The town was named for John Carver, the first Governor of the Plymouth Colony. Initially agricultural, Carver was known for the iron ore from its swamp lands used to make cooking tools by the 1730s. The first iron works was "Pope's Point Furnace", built in 173 ...
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Myles Standish State Forest
Myles Standish State Forest is a state forest located in the towns of Plymouth and Carver in southeastern Massachusetts, approximately 45 miles (70 km) south of Boston. It is the largest publicly owned recreation area in this part of Massachusetts and is managed by the Department of Conservation and Recreation (DCR). Description The forest is part of the Atlantic coastal pine barrens ecoregion and consists largely of pitch pine and scrub oak forests—at , one of the largest such forests north of Long Island. The forest surrounds 16 lakes and ponds, including several ecologically significant coastal kettle ponds. Ecology Species commonly found in Southeast Massachusetts pine barrens: Plants Trees * Pitch pine *Bear oak (scrub oak) * Dwarf chestnut oak (scrub oak) Fruit-bearing * Hillside and lowbush blueberry *Black huckleberry *Bearberry * Birds'-foot violet Animals Birds *Eastern towhee *Eastern bluebird *Pine warbler *Prairie warbler *Whip-poor-will Insects * ...
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East Head Reservoir
East Head Reservoir, also known as East Head Pond, is a pond in Carver and Plymouth, Massachusetts, within the Myles Standish State Forest, located northeast of the forest headquarters, east of Barrett Pond, southwest of New Long Pond and College Pond, and northwest of Fearing Pond. The reservoir is the headwaters to the Wankinco River The Wankinco River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 river in eastern Massachusetts, United States. It is a tributary of the Wareham River, which drains .... External linksEnvironmental Protection Agency Ponds of Plymouth, Massachusetts Ponds of Massachusetts {{PlymouthCountyMA-geo-stub ...
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College Pond
College Pond is a natural kettlehole pond in Plymouth, Massachusetts, located in the Myles Standish State Forest northeast of East Head Reservoir, Three Cornered Pond, New Long Pond and Barrett Pond, and north of Fearing Pond Fearing Pond, also erroneously named on some maps as Fearings Pond (pronounced to rhyme with ''bearing''), is a natural kettlehole pond in Plymouth, Massachusetts. The average depth is ten feet and the maximum depth is . It is located in the sout .... There is a swimming beach and picnic area along the north shore of the pond. College Pond may be named after a series, or collection, of nearby ponds. References External links *  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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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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