Round Pond (Duxbury, Massachusetts)
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Round Pond (Duxbury, Massachusetts)
Round Pond is an reservoir in Duxbury, Massachusetts. The reservoir is located northeast of Pine Lake, northwest of Island Creek Pond, and southwest of North Hill Marsh Pond. An inlet provides the inflow for this reservoir from Pine Lake. The reservoir is associated hydro logically with an adjacent cranberry bog operation. It is a kettle hole 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 gla ... formed by melting glaciers over ten thousand years ago. The north-west segment is bounded by a retaining berm that separates the pond from a cranberry bog. A pump house sits at the western edge with an intake pipe extending into the pond. External linksEnvironmental Protection Agency
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Duxbury, Massachusetts
Duxbury (alternative older spelling: "Duxborough") is a historic seaside town in Plymouth County, Massachusetts, Plymouth County, Massachusetts, United States. A suburb located on the South Shore (Massachusetts), South Shore approximately to the southeast of Boston, the population was 16,090 at the 2020 census. Geographic and demographic information on the specific parts of the town of Duxbury is available in the articles Duxbury (CDP), Massachusetts, Duxbury (CDP), Green Harbor, Massachusetts, Green Harbor, and South Duxbury, Massachusetts, South Duxbury. History The area now known as Duxbury was inhabited by people as early as 12,000 to 9,000 BCE. By the time European settlers arrived here, the region was inhabited by the Wampanoag (tribe), Wampanoags, who called this place Mattakeesett, meaning "place of many fish."
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Pine Lake (Duxbury, Massachusetts)
Pine Lake is a lake in Duxbury, Massachusetts in the village of Tinkertown. The lake is located southwest of Round Pond, northwest of Island Creek Pond Island Creek Pond is a pond in Duxbury, Massachusetts in the village of Tinkertown. The pond is located north of Mill Pond A mill pond (or millpond) is a body of water used as a reservoir for a water-powered mill. Description Mill ponds we ..., and east of Route 3 near the East Street underpass. The outflow is a small stream that flows into Round Pond. A small subdivision lies along the southern shore of the lake. References External linksEnvironmental Protection AgencySouth Shore Coastal Watersheds - Lake Assessments

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Island Creek Pond
Island Creek Pond is a pond in Duxbury, Massachusetts in the village of Tinkertown. The pond is located north of Mill Pond, south of North Hill Marsh Pond North Hill Marsh Pond is a pond in Duxbury, Massachusetts, USA. The pond is the headwaters to the Back River. The pond is located northeast of Round Pond and north of Island Creek Pond Island Creek Pond is a pond in Duxbury, Massachusetts in ..., and southwest of Pine Lake and Round Pond. The pond is the headwaters to Island Creek. The water quality is impaired due to non-native aquatic plants and non-native fish in the pond. Crocker Park, an open space area owned by the Town of Duxbury, is situated along the southern shore of the pond. External linksIsland Creek Pond, Mill Pond, Island Creek InformationEnvironmental Protection Agency
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North Hill Marsh Pond
North Hill Marsh Pond is a pond in Duxbury, Massachusetts, USA. The pond is the headwaters to the Back River. The pond is located northeast of Round Pond and north of Island Creek Pond Island Creek Pond is a pond in Duxbury, Massachusetts in the village of Tinkertown. The pond is located north of Mill Pond, south of North Hill Marsh Pond North Hill Marsh Pond is a pond in Duxbury, Massachusetts, USA. The pond is the headwate .... A wildlife sanctuary borders this pond to the south, and the North Hill Country Club, accessible via Merry Avenue, off Route 14, borders this pond to the northeast. The water quality is impaired due to non-native aquatic plants in the pond. These series of ponds are all part of the Island Creek Fish Ladder restoration project of 2006. The Massachusetts Audubon Society's sanctuary on Mayflower Street includes a forest, bike trails, and a pond. References External linksEnvironmental Protection Agency
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Kettle Hole
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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Lakes Of Plymouth County, Massachusetts
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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