A body of water or waterbody (often spelled water body) is any significant accumulation of water, generally on a planet's surface. The term most often refers to oceans, seas, and lakes, but it includes smaller pools of water such as ponds, wetlands, or more rarely, puddles. A body of water does not have to be still or contained; rivers, streams, canals, and other geographical features where water moves from one place to another are also considered bodies of water.
Most are naturally occurring geographical features, but some are artificial. There are types that can be either. For example, most reservoirs are created by engineering dams, but some natural lakes are used as reservoirs. Similarly, most harbors are naturally occurring bays, but some harbors have been created through construction.
British...especially an inlet...(whereas) NZ, North American, Australian...stream or minor tributary.
North American, Australian, NZ...A stream, brook, or minor tributary of a river.
U.S., Canada , and Australia…a stream smaller than a river.
US, Canadian, Australian and New Zealand a small stream or tributary
a narrow stream
British...especially an inlet
Chiefly Atlantic States and British...a recess or inlet in the shore of the sea.
BRITISH a long narrow area of ocean stretching into the land
Chiefly British a narrow inlet or bay
A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a type of smaller bay with a circular inlet and narrow entrance. A fjord is a particularly steep bay shaped by glacial activity.
A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in northeastern Canada. Some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology.
The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have beaches, which "are usually characterized by a steep upper foreshore with a broad, flat fronting terrace". Bays were significant in the history of human settlement because they provided safe places for fishing. Later they were important in the development of sea trade as the safe anchorage they provide encouraged their selection as ports.Budgewoi Lake
The Budgewoi Lake, a lagoon that is part of the Tuggerah Lakes, is located within the Central Coast Council local government area in the Central Coast region of New South Wales, Australia. The lake is located near the settlement of Budgewoi and is situated about 100 kilometres (62 mi) north of Sydney.Bukkehåmmårtjørna
Bukkehåmmårtjørna is a small lake in eastern Jotunheimen. This is the highest lake that
has been investigated as a climate archive in southern Norway, being situated 1594 m above sea level.
A small glacier, Bukkehåmmårbreen, is draining meltwater into the lake at present. This glacier reformed just short of 6,000 years ago following the Holocene climate optimum and has existed continuously since. After growing gradually towards 4,000 years before present (BP) the glacier has been of near present size over the last 4,000 years, growing slightly larger over the last 2-2,500 years.
Prior to the climate optimum and following the deglaciation the glacier melted some 10,000 years before present.
The flat valley-shoulder that the lake is eroded into is locally known as a "fly". This particular level at about 1600 m a.s.l. and is believed to have been formed between 100 and 85 million years ago during the Cretaceous period. Standing on the shore-line of Bukkehåmmårtjørna thus means that you are standing on the remnants of a landscape that the Dinosaurs ruled.
The small lake existed prior to the Last Glacial Maximum since it contains organic material older than 30,000 years old. Currently being reassessed, growing evidence now indicates that much of the landscape that can be seen from this site is practically unchanged since the age of the Mammoth who lived on the wide plateaus more than 40,000 years ago.
The view from the lake, or higher up on the mountain-peak Høgdebrotet therefore includes a view into the landscapes of the distant past, including the landscape of the dinosaurs, the pre-ice age landscape, the landscape of the Mammoth during the last glacial period. By squinting your eyes and imagining the present forest-limit below, located some 300 m higher than at present and by imagining the glaciers of Leirungsalpene being absent you can also see the landscape as it was 7,000 years ago.Channel (geography)
In physical geography, a channel is a type of landform consisting of the outline of a path of relatively shallow and narrow body of fluid, most commonly the confine of a river, river delta or strait. The word is cognate to canal, and sometimes shows in this form, e.g. the Hood Canal.Clifton Court Forebay
Clifton Court Forebay is a reservoir in the San Joaquin River Delta region of eastern Contra Costa County, California, 17 mi (27 km) southwest of Stockton. The estuary region the forebay is located in is only 1m to 3m above mean sea level.Endeavour Strait
The Endeavour Strait is a strait running between the Australian mainland Cape York Peninsula and Prince of Wales Island in the extreme south of the Torres Strait, in northern Queensland, Australia. It was named in 1770 by explorer James Cook, after his own vessel, HMS Endeavour, and he used the strait as passage out to the Indian Ocean on his voyage.Fish River (Maine)
The Fish River is a 69.9-mile-long (112.5 km) river in northern Maine in the United States. It is a tributary of the Saint John River, which flows to the Bay of Fundy (an arm of the Atlantic Ocean) in New Brunswick, Canada.
From its start at the confluence of Fox Brook and Carr Pond Stream (46°46′37″N 68°46′52″W), in Maine Township 13, Range 8, WELS, the river runs north to Fish River Lake, then east to Portage Lake. It then runs northwards through St. Froid Lake and Eagle Lake to the Saint John River at Fort Kent. The latter section is roughly parallel to Maine State Route 11.Inflow (hydrology)
In hydrology, the inflow of a body of water is the source of the water in the body of water. It can also refer to the average volume of incoming water in unit time. It is contrasted with outflow.Lagoon
A lagoon is a shallow body of water separated from a larger body of water by barrier islands or reefs. Lagoons are commonly divided into coastal lagoons and atoll lagoons. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world.Little Androscoggin River
The Little Androscoggin River is a 51.4-mile-long (82.7 km) river in Maine. It flows from Bryant Pond in Woodstock (44°21′53″N 70°38′18″W) to its confluence with the Androscoggin River in Auburn. The Androscoggin flows into Merrymeeting Bay in the Kennebec River estuary.
The Little Androscoggin flows through the towns of Woodstock, Greenwood, West Paris, Paris (including the village of South Paris), Norway, Oxford, Mechanic Falls, Minot, and Poland, and the city of Auburn.Lost Lake (Groton)
Lost Lake also known as Knop/p/s Pond is a reservoir in Groton, Massachusetts, United States. It was formed from three lakes by the headwaters of Salmon Brook. The southern part of the lake is known as Knops Pond where it is near 30 feet deep. It is stocked with rainbow, brown and brook trout every spring and fall and is home to several species of warm water fish. There is also a boat launch located on the northeastern side of the lake.Magalloway River
The Magalloway River is a river in northwestern Maine and northern New Hampshire in the United States. It is a tributary of the Androscoggin River, which flows to the Kennebec River at Merrymeeting Bay in Maine, near the Atlantic Ocean. The total length of the river is 30 miles (48 km), or 48 miles (77 km) if the distances across intervening lakes are included.
The Magalloway River rises near the extreme northwestern corner of Maine, at the juncture of the West Branch and the Second East Branch of the Magalloway. The river flows south through logging country to 2.5-mile (4.0 km)-long Parmachenee Lake, then descends for another 2.6 miles (4.2 km) to the 15-mile (24 km)-long Aziscohos Lake. Below the lake dam, the Magalloway turns west and descends 250 feet (76 m) in 2 miles (3.2 km) to the village of Wilsons Mills, Maine, before once again turning south, now along the New Hampshire-Maine border. The river ends where it joins the outlet of Umbagog Lake, forming the Androscoggin River.
Tributaries of the Magalloway include the West Branch, the Second East Branch, the First East Branch, the Little Magalloway River, and the Dead Diamond River. The Magalloway passes through the townships of Parmachenee, Lynchtown, Parkertown, Lincoln, and Magalloway Plantation in Maine, and the townships of Second College Grant and Wentworth's Location in New Hampshire.
Its name is from some Native American language, meaning "large tail".Moxie Falls
Moxie Falls is a waterfall in Somerset County, Maine. At a vertical drop of over 90 feet (30 m) into a pool about 17 feet (5 m) deep, Moxie Falls is one of the highest falls in New England. The falls are part of Moxie Stream which flows from Moxie Pond into the Kennebec River approximately 1 kilometer (0.62 mi) downstream the falls. Moxie Stream drains Moxie Pond approximately 5 miles (8.0 km) upstream of the falls.
The hiking trail to Moxie Falls is approximately 0.5 miles with a boardwalk for viewing the falls at the end. There are several pools for swimming upstream of the falls.Peninsula
A peninsula (Latin: paeninsula from paene "almost” and insula "island") is a landform surrounded by water on the majority of its border while being connected to a mainland from which it extends. The surrounding water is usually understood to be continuous, though not necessarily named as a single body of water. Peninsulas are not always named as such; one can also be a headland, cape, island promontory, bill, point, fork, or spit. A point is generally considered a tapering piece of land projecting into a body of water that is less prominent than a cape. A river which courses through a very tight meander is also sometimes said to form a "peninsula" within the (almost closed) loop of water. In English, the plural versions of peninsula are peninsulas and, less commonly, peninsulae.Salt lake
A salt lake or saline lake is a landlocked body of water that has a concentration of salts (typically sodium chloride) and other dissolved minerals significantly higher than most lakes (often defined as at least three grams of salt per litre). In some cases, salt lakes have a higher concentration of salt than sea water; such lakes can also be termed hypersaline lakes. An alkalic salt lake that has a high content of carbonate is sometimes termed a soda lake.
Saline lake classification:
subsaline 0.5–3 ‰
hyposaline 3–20 ‰
mesosaline 20–50 ‰
hypersaline greater than 50 ‰Sebec River
The Sebec River is a tributary of the Piscataquis River in Piscataquis County, Maine. From the outflow of Sebec Lake (45°16′13″N 69°06′54″W) in Sebec, the river runs 10.0 miles (16.1 km) east and southeast to its confluence with the Piscataquis in Milo.Shoal
In oceanography, geomorphology, and earth sciences, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water to near the surface. Often it refers to those submerged ridges, banks, or bars that rise near enough to the surface of a body of water as to constitute a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.The term shoal is also used in a number of ways that can be either similar or quite different from how it is used in the geologic, geomorphic, and oceanographic literature. Sometimes, this terms refers to either any relatively shallow place in a stream, lake, sea, or other body of water; a rocky area on the sea floor within an area mapped for navigation purposes; a growth of vegetation on the bottom of a deep lake that occurs at any depth; and as a verb for the process of proceeding from a greater to a lesser depth of water.Shore
A shore or a shoreline is the fringe of land at the edge of a large body of water, such as an ocean, sea, or lake. In physical oceanography, a shore is the wider fringe that is geologically modified by the action of the body of water past and present, while the beach is at the edge of the shore, representing the intertidal zone where there is one. In contrast to a coast, a shore can border any body of water, while the coast must border an ocean; in that sense a coast is a type of shore; however, coast often refers to an area far wider than the shore, often stretching miles into the interior.
Shores are influenced by the topography of the surrounding landscape, as well as by water induced erosion, such as waves. The geological composition of rock and soil dictates the type of shore which is created.Sound (geography)
In geography, a sound is a large sea or ocean inlet, deeper than a bight and wider than a fjord; or a narrow sea or ocean channel between two bodies of land (see also strait).There is little consistency in the use of "sound" in English-language place names.