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Gallows Pond
Gallows Pond is a kettlehole pond in Plymouth, Massachusetts. The pond is west of and adjacent to Long Pond, south of Little Long Pond, and northeast of Halfway Pond Halfway Pond a warm water pond located in Plymouth, Massachusetts between Myles Standish State Forest and Long Pond, west of Round Pond, southwest of Gallows Pond, and north of Fawn Pond and White Island Pond. The average depth is nine feet a .... Camp Wind-in-the-Pines Girl Scout Center is located along the shore of this pond. References External linksEnvironmental Protection Agency Ponds of Plymouth, Massachusetts [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Long Pond (Plymouth, Massachusetts)
Long Pond is a cold water pond in Plymouth, Massachusetts, east of Myles Standish State Forest, Halfway Pond and Round Pond, west of Route 3 at Exit 3 and The Pinehills, northwest of Bloody Pond, and north of West Wind Shores. The pond has an average depth of and a maximum depth of . It is fed by groundwater and an inlet from Little Long Pond, and drains through the pond bottom. A paved boat ramp provided by the Public Access Board with ample parking spaces is easily accessible from Route 3. The Pond has a 50 hp limitation on boating. Long Pond village The village of the same name to the southwest of the pond includes Faunce Church . See also *Neighborhoods in Plymouth, Massachusetts *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 ... References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Long Pond (Plymouth, Massachusetts)
Little Long Pond is a pond in Plymouth, Massachusetts, north of Long Pond and Gallows Pond. The outflow of this pond is a stream that feeds into Long Pond. There is another Little Long Pond partially within Plymouth's borders located east of the southeasternmost point of 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 Massac .... References External links Mass Division of Fisheries and Wildlife Pond map/info Ponds of Plymouth, Massachusetts [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halfway Pond (Massachusetts)
Halfway Pond a warm water pond located in Plymouth, Massachusetts between Myles Standish State Forest and Long Pond, west of Round Pond, southwest of Gallows Pond, and north of Fawn Pond and White Island Pond. The average depth is nine feet and the maximum depth is . The pond is fed by groundwater springs and drains into the Agawam River. Halfway Pond Island lies in the middle of the pond and is managed as a research natural area by The Nature Conservancy in Massachusetts. There are almost three miles (5 km) of shoreline. Access here is informal and can be located off of Mast Road, a portion of which abuts the western shoreline of the pond. Parking is limited to just two or three cars and boaters will have to stick with canoes and other car top craft. Substantial amounts of shoreline are open to fishing. Halfway Pond village Halfway Pond, a small village of Plymouth, is located on the southwestern shore of Halfway Pond . See also *Neighborhoods in Plymouth, Massachusett ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
