Piscataquog River
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Piscataquog River
The Piscataquog River is a river located in southern New Hampshire in the United States. It is a tributary of the Merrimack River, which flows to the Gulf of Maine. The Piscataquog River begins at the outlet of Deering Reservoir, a lake in Deering, New Hampshire. The river takes a winding course north, then east, then south, then east again through Hillsborough County to reach the Merrimack River in Manchester. On its way, it passes through the town of Weare, where it is impounded in two reservoirs — Weare Reservoir (or "Lake Horace") and Everett Lake. Everett Lake is part of the watershed-spanning Hopkinton-Everett flood control reservoir — a canal crossing the drainage divide connects Everett Lake to Hopkinton Reservoir, which impounds the Contoocook River. The Piscataquog proceeds south from the Everett Dam along the eastern side of Weare, entering Goffstown shortly before the river's junction with the South Branch, the Piscataquog's largest tributary. From Goffs ...
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Weare, NH
Weare is a town in Hillsborough County, New Hampshire, United States. The population was 9,092 at the 2020 census. It is close to two important New Hampshire cities, Manchester and Concord. History It was granted to veterans of the Canadian wars in 1735 by Governor Jonathan Belcher, who named it "Beverly-Canada" after their hometown, Beverly, Massachusetts. But the charter was ruled invalid because of a prior claim by the Masonian proprietors, who granted as "Hale's Town" to Ichabod Robie in 1749. It was also known as "Robie's Town" or "Weare's Town" before being incorporated by Governor Benning Wentworth in 1764 as Weare, after Meshech Weare, who served as the town's first clerk and later went on to become New Hampshire's first governor. In 1834, Moses Cartland founded Clinton Grove Academy, the first Quaker seminary in the state. A cousin of John Greenleaf Whittier, Cartland named the village where the school was located "Clinton Grove", in honor of DeWitt Clinton, chief ...
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Tributary
A tributary, or an ''affluent'', is a stream or river that flows into a larger stream (''main stem'' or ''"parent"''), river, or a lake. A tributary does not flow directly into a sea or ocean. Tributaries, and the main stem river into which they flow, drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean, another river, or into an endorheic basin. The Irtysh is a chief tributary of the Ob (river), Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream.
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Rivers Of New Hampshire
This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to thNew Hampshire Comprehensive Shoreland Protection Actor are more than long. New Hampshire rivers and streams qualify for state shoreland protection (and are listed here in bold) if they are ''fourth-order'' or larger water bodies, based on the Strahler method of stream order classification. Strahler, A. N. (1952). "Dynamic basis of geomorphology". ''Geological Society of America Bulletin'', 63, 923–938. By drainage basin All New Hampshire rivers ultimately flow to the Atlantic Ocean. The list is sorted by major drainage basin, running from north to south along the Atlantic coast, with respective tributaries arranged based on their entry into the main stream from mouth to source. Where several tributaries enter a single lake, they are listed running clockwise from the lak ...
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Tributaries Of The Merrimack River
A tributary, or an ''affluent'', is a stream or river that flows into a larger stream (''main stem'' or ''"parent"''), river, or a lake. A tributary does not flow directly into a sea or ocean. Tributaries, and the main stem river into which they flow, drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean, another river, or into an endorheic basin. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream.
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List Of Rivers Of New Hampshire
This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to thNew Hampshire Comprehensive Shoreland Protection Actor are more than long. New Hampshire rivers and streams qualify for state shoreland protection (and are listed here in bold) if they are ''fourth-order'' or larger water bodies, based on the Strahler method of stream order classification. Strahler, A. N. (1952). "Dynamic basis of geomorphology". ''Geological Society of America Bulletin'', 63, 923–938. By drainage basin All New Hampshire rivers ultimately flow to the Atlantic Ocean. The list is sorted by major drainage basin, running from north to south along the Atlantic coast, with respective tributaries arranged based on their entry into the main stream from mouth to source. Where several tributaries enter a single lake, they are listed running clockwise from the la ...
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Contoocook River
The Contoocook River () is a river in New Hampshire. It flows from Contoocook Lake on the Jaffrey/ Rindge border to Penacook (just north of Concord), where it empties into the Merrimack River. It is one of only a few rivers in New Hampshire that flow in a predominantly northward direction. Four covered bridges span the river, one in the town of Henniker, one on the Hancock- Greenfield line, and two in the town of Hopkinton, New Hampshire with one being in the village of Contoocook, and the other in the populated place of West Hopkinton. Residents and tourists have made the Contoocook popular for fishing and whitewater boating. The name ''Contoocook'' came from the Pennacook tribe of Native Americans and perhaps means "place of the river near pines". Other variations of the name include the Abenaki meaning "nut trees river" or Natick language meaning "small plantation at the river." The river gives its name to Contoocook, New Hampshire, a census-designated place (CDP) with ...
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Flood Control
Flood management or flood control are methods used to reduce or prevent the detrimental effects of flood waters. Flooding can be caused by a mix of both natural processes, such as extreme weather upstream, and human changes to waterbodies and runoff. Flood management methods can be either of the ''structural'' type (i.e. flood control) and of the ''non-structural'' type. Structural methods hold back floodwaters physically, while non-structural methods do not. Building hard infrastructure to prevent flooding, such as flood walls, is effective at managing flooding. However, it is best practice within landscape engineering to rely more on soft infrastructure and Nature-based solutions, natural systems, such as marshes and Floodplain, flood plains, for handling the increase in water. Flood management can include ''flood risk management,'' which focuses on measures to reduce risk, vulnerability and exposure to flood disasters and providing risk analysis through, for example, flood ris ...
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Drainage Basin
A drainage basin is an area of land in which all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the drainage divide, made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, " watershed" is used only in its original sense, that of the drainage divide line. A drainage basin's boundaries are determined by watershed delineation, a common task in environmental engineering and science. In a closed drainage basin, or endorheic basin, rather than flowing to the ocean, water converges toward the ...
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Weare Reservoir
Weare Reservoir is a impoundment on the Piscataquog River in Hillsborough County in southern New Hampshire, United States, in the town of Weare. The reservoir is also known as Lake Horace. It is classified as a warmwater fishery, with observed species including rainbow trout, brown trout, smallmouth and largemouth bass, chain pickerel, horned pout, and black crappie. See also *List of lakes in New Hampshire This is a list of lakes and ponds in the U.S. state of New Hampshire. The New Hampshire Department of Environmental Services lists 944 lakes and impoundments in their ''Official List of Public Waters''. The water bodies that are listed include na ... References Lakes of Hillsborough County, New Hampshire Reservoirs in New Hampshire Weare, New Hampshire {{NewHampshire-geo-stub ...
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Reservoir (water)
A reservoir (; ) is an enlarged lake behind a dam, usually built to store fresh water, often doubling for hydroelectric power generation. Reservoirs are created by controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an Bay, embayment within it, excavating, or building any number of retaining walls or levees to enclose any area to store water. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley and rely on the natural topography to provide most of the basin of the reservoir. These reservoirs can either be ''on-stream reservoirs'', which are located on the original streambed of the downstream river and are filled by stream, creeks, rivers or rainwater that surface runoff, runs off the surrounding forested catchments, or ''off-stream reservoirs'', which receive water diversion, diverted water from a nearby stream or aqueduct (water supply), aqueduct or pi ...
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Gulf Of Maine
The Gulf of Maine is a large gulf of the Atlantic Ocean on the east coast of North America. It is bounded by Cape Cod at the eastern tip of Massachusetts in the southwest and by Cape Sable Island at the southern tip of Nova Scotia in the northeast. The gulf includes the entire coastlines of the U.S. states of New Hampshire and Maine, as well as Massachusetts north of Cape Cod, and the southern and western coastlines of the Canadian provinces of New Brunswick and Nova Scotia, respectively. The gulf was named for the adjoining English colonial Province of Maine, which was in turn likely named by early explorers after the province of Maine in France. Massachusetts Bay, Penobscot Bay, Passamaquoddy Bay, and the Bay of Fundy are all arms of the Gulf of Maine. Geography and hydrography The Gulf of Maine is a roughly rectangular depression with a surface area of around , enclosed to the west and north by the North American mainland and communicating with the Atlantic Ocean to the so ...
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River
A river is a natural stream of fresh water that flows on land or inside Subterranean river, caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the Runoff (hydrology), runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their Bank (geography), banks and flood the surrounding area, spreading nutrients to the surrounding area. Sedime ...
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