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68-502: Goguac Lake is a 352-acre (1.42 km) lake in the city of Battle Creek , located in Calhoun County in the southwest portion of the U.S. state of Michigan . With a maximum depth of 66 feet (20 m), the lake is home to many fish species, including Crappie, Bluegill, Pike, Largemouth Bass, Yellow Perch, Rock Bass and Walleye. While the perimeter of the lake consists primarily of private residences and expansive estates;

136-544: A Native American term referring to the "undulating" prairie surrounding the lake. This was an area that was home for the Potawatomi tribe and Goguac Lake was said to be a gathering place for them from time to time. Since being settled by the English in the early nineteenth century, Goguac Lake has provided irrigation for crops, a ready supply of water and a focal point for community recreation. Like many lakes throughout

204-409: A body of water from 2 hectares (5 acres) to 8 hectares (20 acres). Pioneering animal ecologist Charles Elton regarded lakes as waterbodies of 40 hectares (99 acres) or more. The term lake is also used to describe a feature such as Lake Eyre , which is a dry basin most of the time but may become filled under seasonal conditions of heavy rainfall. In common usage, many lakes bear names ending with

272-500: A comprehensive analysis of the origin of lakes and proposed what is a widely accepted classification of lakes according to their origin. This classification recognizes 11 major lake types that are divided into 76 subtypes. The 11 major lake types are: Tectonic lakes are lakes formed by the deformation and resulting lateral and vertical movements of the Earth's crust. These movements include faulting, tilting, folding, and warping. Some of

340-402: A form of organic lake. They form where a buildup of partly decomposed plant material in a wet environment leaves the vegetated surface below the water table for a sustained period of time. They are often low in nutrients and mildly acidic, with bottom waters low in dissolved oxygen. Artificial lakes or anthropogenic lakes are large waterbodies created by human activity . They can be formed by

408-538: A higher perimeter to area ratio than other lake types. These form where sediment from a tributary blocks the main river. These form where sediment from the main river blocks a tributary, usually in the form of a levee . Lakes formed by other processes responsible for floodplain basin creation. During high floods they are flushed with river water. There are four types: 1. Confluent floodplain lake, 2. Contrafluent-confluent floodplain lake, 3. Contrafluent floodplain lake, 4. Profundal floodplain lake. A solution lake

476-510: A hypolimnion; accordingly, very shallow lakes are excluded from this classification system. Based upon their thermal stratification, lakes are classified as either holomictic , with a uniform temperature and density from top to bottom at a given time of year, or meromictic , with layers of water of different temperature and density that do not intermix. The deepest layer of water in a meromictic lake does not contain any dissolved oxygen so there are no living aerobic organisms . Consequently,

544-465: A journal which sired the dime novel and our modern mystery magazines, published a story whose setting was an island in Goguac Lake. The story was retold and republished several times and has been called "The Soul of Stephen Strand." The author is unknown. Its main character was a two personality man. He didn't have two personalities to begin with, like the later Dr. Jekyll and Mr. Hyde, but had stolen

612-428: A lake consists of a large area of standing water that occupies an extensive closed depression in limestone, it is also called a karst lake . Smaller solution lakes that consist of a body of standing water in a closed depression within a karst region are known as karst ponds. Limestone caves often contain pools of standing water, which are known as underground lakes . Classic examples of solution lakes are abundant in

680-470: A large number of studies agree that small ponds are much more abundant than large lakes. For example, one widely cited study estimated that Earth has 304 million lakes and ponds, and that 91% of these are 1 hectare (2.5 acres) or less in area. Despite the overwhelming abundance of ponds, almost all of Earth's lake water is found in fewer than 100 large lakes; this is because lake volume scales superlinearly with lake area. Extraterrestrial lakes exist on

748-489: A natural outflow and lose water solely by evaporation or underground seepage, or both. These are termed endorheic lakes. Many lakes are artificial and are constructed for hydroelectric power generation, aesthetic purposes, recreational purposes, industrial use, agricultural use, or domestic water supply . The number of lakes on Earth is undetermined because most lakes and ponds are very small and do not appear on maps or satellite imagery . Despite this uncertainty,

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816-403: A result of meandering. The slow-moving river forms a sinuous shape as the outer side of bends are eroded away more rapidly than the inner side. Eventually a horseshoe bend is formed and the river cuts through the narrow neck. This new passage then forms the main passage for the river and the ends of the bend become silted up, thus forming a bow-shaped lake. Their crescent shape gives oxbow lakes

884-535: A result of the 1959 Hebgen Lake earthquake . Most landslide lakes disappear in the first few months after formation, but a landslide dam can burst suddenly at a later stage and threaten the population downstream when the lake water drains out. In 1911, an earthquake triggered a landslide that blocked a deep valley in the Pamir Mountains region of Tajikistan , forming the Sarez Lake . The Usoi Dam at

952-422: A variation in density because of thermal gradients. Stratification can also result from a density variation caused by gradients in salinity. In this case, the hypolimnion and epilimnion are separated not by a thermocline but by a halocline , which is sometimes referred to as a chemocline . Lakes are informally classified and named according to the seasonal variation in their lake level and volume. Some of

1020-443: Is sag ponds . Volcanic lakes are lakes that occupy either local depressions, e.g. craters and maars , or larger basins, e.g. calderas , created by volcanism . Crater lakes are formed in volcanic craters and calderas, which fill up with precipitation more rapidly than they empty via either evaporation, groundwater discharge, or a combination of both. Sometimes the latter are called caldera lakes, although often no distinction

1088-403: Is a lake occupying a basin formed by surface dissolution of bedrock. In areas underlain by soluble bedrock, its solution by precipitation and percolating water commonly produce cavities. These cavities frequently collapse to form sinkholes that form part of the local karst topography . Where groundwater lies near the grounds surface, a sinkhole will be filled water as a solution lake. If such

1156-468: Is dammed behind an ice shelf that is attached to the coastline. They are mostly found in Antarctica. Fluvial (or riverine) lakes are lakes produced by running water. These lakes include plunge pool lakes , fluviatile dams and meander lakes. The most common type of fluvial lake is a crescent-shaped lake called an oxbow lake due to the distinctive curved shape. They can form in river valleys as

1224-452: Is made. An example is Crater Lake in Oregon , in the caldera of Mount Mazama . The caldera was created in a massive volcanic eruption that led to the subsidence of Mount Mazama around 4860 BCE. Other volcanic lakes are created when either rivers or streams are dammed by lava flows or volcanic lahars . The basin which is now Malheur Lake , Oregon was created when a lava flow dammed

1292-429: Is unknown but is estimated to be at least 2 million. Finland has 168,000 lakes of 500 square metres (5,400 sq ft) in area, or larger, of which 57,000 are large (10,000 square metres (110,000 sq ft) or larger). Most lakes have at least one natural outflow in the form of a river or stream , which maintain a lake's average level by allowing the drainage of excess water. Some lakes do not have

1360-614: The Kalamazoo River , a priceless 'first person' story was written for a local paper. Suspected as author of the story, and perhaps of the rumor, is William Pease who was owner, editor and possibly sole writer for The Jeffersonian , a short-lived newspaper in Battle Creek. The autobiographical bit told that the author was a visitor, living at the Battle Creek House, and that he was swimming in Goguac Lake when he

1428-759: The Malheur River . Among all lake types, volcanic crater lakes most closely approximate a circular shape. Glacial lakes are lakes created by the direct action of glaciers and continental ice sheets. A wide variety of glacial processes create enclosed basins. As a result, there are a wide variety of different types of glacial lakes and it is often difficult to define clear-cut distinctions between different types of glacial lakes and lakes influenced by other activities. The general types of glacial lakes that have been recognized are lakes in direct contact with ice, glacially carved rock basins and depressions, morainic and outwash lakes, and glacial drift basins. Glacial lakes are

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1496-499: The Proto-Indo-European root * leǵ- ('to leak, drain'). Cognates include Dutch laak ('lake, pond, ditch'), Middle Low German lāke ('water pooled in a riverbed, puddle') as in: de:Wolfslake , de:Butterlake , German Lache ('pool, puddle'), and Icelandic lækur ('slow flowing stream'). Also related are the English words leak and leach . There is considerable uncertainty about defining

1564-399: The density of water varies with temperature, with a maximum at +4 degrees Celsius, thermal stratification is an important physical characteristic of a lake that controls the fauna and flora , sedimentation, chemistry, and other aspects of individual lakes. First, the colder, denser water typically forms a layer near the bottom, which is called the hypolimnion . Second, normally overlying

1632-411: The 'soul' and appearance of a man dying here and placed them in his own sturdy body. The story included plenty of suspense and a spooky cat. Goguac Lake has no known natural outlets and its level changes according to season, going down during dry spells, coming up when there is much rain. An artificial inlet from Minges Brook controls this somewhat. Following a rumor that the lake has a hidden outlet into

1700-539: The Battle Creek Country Club and Willard Beach public park can be found on the lake. A fictional version of the lake was featured in the television show Battle Creek There are three islands on Goguac Lake. Picnic Island, farthest south, became Chamberlain's, then Elk's and finally Vince's Island. Dr. Vince, the English-born dentist, built a causeway from the shore so that he could drive to

1768-461: The Civil War and into the 20th century, various industries, from cereal production to pharmaceuticals to automobile parts, flourished. Several communities became sites for paper production, which used the river for water intake and waste discharge. Deinking practices no longer in use led to PCB contamination of the river. Sewage effluent, other industrial discharges, and trash also contributed to

1836-597: The Earth by extraterrestrial objects (either meteorites or asteroids ). Examples of meteorite lakes are Lonar Lake in India, Lake El'gygytgyn in northeast Siberia, and the Pingualuit crater lake in Quebec, Canada. As in the cases of El'gygytgyn and Pingualuit, meteorite lakes can contain unique and scientifically valuable sedimentary deposits associated with long records of paleoclimatic changes. In addition to

1904-404: The Earth's surface. It is localized in a basin or interconnected basins surrounded by dry land . Lakes lie completely on land and are separate from the ocean , although they may be connected with the ocean by rivers . Lakes, as with other bodies of water , are part of the water cycle , the processes by which water moves around the Earth. Most lakes are freshwater and account for almost all

1972-534: The Kalamazoo River basin continuously for more than 11,000 years. At the time of European contact, the Kalamazoo River area was inhabited primarily by members of Potawatomi tribes. The Jesuit priest Father Jacques Marquette and his companions were probably the first Europeans to glimpse the mouth of the Kalamazoo in 1675 as they returned from Illinois . It wasn't until the late eighteenth century that

2040-555: The Kalamazoo flows mostly westward through Marshall , Battle Creek , Augusta , Galesburg , Comstock , and Kalamazoo . From Kalamazoo, the river flows mostly north until just before it reaches Plainwell and then flows northwest through Otsego , Allegan , Saugatuck and then into Lake Michigan . Some of the larger tributaries of the Kalamazoo are Rice Creek, Wilder Creek , Wabascon Creek, Battle Creek River , Augusta Creek, Portage Creek, Gun River , Swan Creek, and Rabbit River . Archeological evidence indicates humans have used

2108-523: The Kalamazoo, initially causing two homes to be evacuated, and prohibitions against fishing and swimming to be posted. The US Environmental Protection Agency (EPA) later estimated the spill to be in excess of 1 million gallons. On 29 July 2010, the Calhoun County Health Department asked 30 to 50 households to evacuate, and twice as many were advised not to drink their water. The National Transportation Safety Board stated

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2176-571: The Lusatian Lake District, Germany. In India, Sudarshana Lake is a historical artificial lake located in the semi-arid region of Girnar, Gujarat, originally constructed during the reign of Chandragupta Maurya. See: List of notable artificial lakes in the United States Meteorite lakes, also known as crater lakes (not to be confused with volcanic crater lakes ), are created by catastrophic impacts with

2244-489: The area was frequented by fur traders. By the early nineteenth century, there were several small communities along the river, including Kalamazoo. With the introduction of the railroad in the 1840s, the importance of the river for transportation diminished. By the mid-19th century, several communities had grown up along the River as mill towns and commercial centers: Battle Creek, Kalamazoo, Parchment, Plainwell, and Otsego. After

2312-866: The base of the valley has remained in place for more than 100 years but the terrain below the lake is in danger of a catastrophic flood if the dam were to fail during a future earthquake. Tal-y-llyn Lake in north Wales is a landslide lake dating back to the last glaciation in Wales some 20000 years ago. Aeolian lakes are produced by wind action . These lakes are found mainly in arid environments, although some aeolian lakes are relict landforms indicative of arid paleoclimates . Aeolian lakes consist of lake basins dammed by wind-blown sand; interdunal lakes that lie between well-oriented sand dunes ; and deflation basins formed by wind action under previously arid paleoenvironments. Moses Lake in Washington , United States,

2380-551: The cause of cold and warm water only a few feet apart. In the 1890s a few cottagers stocked the lake with fish of desirable kinds for eating and one year brought in some choice eels. That started stories comparable to those told about the Loch Ness Monster . But the stories disappeared as did the eels. Only one catch, harmless enough, has been reported in the last quarter century. In 1851 the New York Mercury,

2448-915: The courses of mature rivers, where a river channel has widened over a basin formed by eroded floodplains and wetlands . Some lakes are found in caverns underground . Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice age . All lakes are temporary over long periods of time , as they will slowly fill in with sediments or spill out of the basin containing them. Artificially controlled lakes are known as reservoirs , and are usually constructed for industrial or agricultural use, for hydroelectric power generation, for supplying domestic drinking water , for ecological or recreational purposes, or for other human activities. The word lake comes from Middle English lake ('lake, pond, waterway'), from Old English lacu ('pond, pool, stream'), from Proto-Germanic * lakō ('pond, ditch, slow moving stream'), from

2516-518: The creation of lakes by the disruption of preexisting drainage networks, it also creates within arid regions endorheic basins that contain salt lakes (also called saline lakes). They form where there is no natural outlet, a high evaporation rate and the drainage surface of the water table has a higher-than-normal salt content. Examples of these salt lakes include Great Salt Lake and the Dead Sea . Another type of tectonic lake caused by faulting

2584-622: The difference between lakes and ponds , and neither term has an internationally accepted definition across scientific disciplines or political boundaries. For example, limnologists have defined lakes as water bodies that are simply a larger version of a pond, which can have wave action on the shoreline or where wind-induced turbulence plays a major role in mixing the water column. None of these definitions completely excludes ponds and all are difficult to measure. For this reason, simple size-based definitions are increasingly used to separate ponds and lakes. Definitions for lake range in minimum sizes for

2652-475: The early 20th Century, Goguac Lake was once home to a small amusement park, called Liberty Amusement Park. It boasted a wooden roller coaster as well as a large dance hall. Construction started in the late 1890s and the park operated at least through the 1912 season. Goguac Lake has figured in a surprising number of stories: pure fiction, legends based on a thread of fact and some fantasied logic. George Willard guessed that La Salle had camped beside Goguac Lake;

2720-429: The early days when the lake level was lower. Ward's cottage stood on it several decades, as did the first Goguac Boat Club for about three years. Occasional picnickers use it now as trespassers, although those who recognize poison ivy generally stay away. Before its graceful elms died it became quite a bird sanctuary. Hummingbirds that fed in gardens on the mainland nested there. The lake was originally spelled Coguagiack,

2788-536: The exception of criterion 3, the others have been accepted or elaborated upon by other hydrology publications. The majority of lakes on Earth are freshwater , and most lie in the Northern Hemisphere at higher latitudes . Canada , with a deranged drainage system , has an estimated 31,752 lakes larger than 3 square kilometres (1.2 sq mi) in surface area. The total number of lakes in Canada

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2856-405: The handsome manor house he built there. Peach Island was so named for the peach orchard planted there by Hermes Sweet. It was sometimes used for cockfights because both the sport and betting were against the law and this was a good hideaway from the sheriff. The island was subsequently known as Hulbert's, then Clark's, then Gould's for the owners of the single cottage. Ward's Island is smaller than in

2924-422: The hypolimnion is a transition zone known as the metalimnion . Finally, overlying the metalimnion is a surface layer of warmer water with a lower density, called the epilimnion . This typical stratification sequence can vary widely, depending on the specific lake or the time of year, or a combination of both. The classification of lakes by thermal stratification presupposes lakes with sufficient depth to form

2992-907: The intentional damming of rivers and streams, rerouting of water to inundate a previously dry basin , or the deliberate filling of abandoned excavation pits by either precipitation runoff , ground water , or a combination of both. Artificial lakes may be used as storage reservoirs that provide drinking water for nearby settlements , to generate hydroelectricity , for flood management , for supplying agriculture or aquaculture , or to provide an aquatic sanctuary for parks and nature reserves . The Upper Silesian region of southern Poland contains an anthropogenic lake district consisting of more than 4,000 water bodies created by human activity. The diverse origins of these lakes include: reservoirs retained by dams, flooded mines, water bodies formed in subsidence basins and hollows, levee ponds, and residual water bodies following river regulation. Same for

3060-471: The karst regions at the Dalmatian coast of Croatia and within large parts of Florida . A landslide lake is created by the blockage of a river valley by either mudflows , rockslides , or screes . Such lakes are most common in mountainous regions. Although landslide lakes may be large and quite deep, they are typically short-lived. An example of a landslide lake is Quake Lake , which formed as

3128-780: The lake level. Kalamazoo River The north and south branches of the Kalamazoo River originate within a few miles of each other. The south branch begins near North Adams in Moscow Township in northeastern Hillsdale County and flows north and west through Homer before joining the north branch at the forks of the Kalamazoo River in Albion . The North Branch begins near Farwell and Pine Hills lakes in southern Jackson County and flows north and west through Concord before reaching Albion in Calhoun County. It then flows through Kalamazoo and Allegan counties. After Albion,

3196-657: The largest lakes on Earth are rift lakes occupying rift valleys, e.g. Central African Rift lakes and Lake Baikal . Other well-known tectonic lakes, Caspian Sea , the Sea of Aral , and other lakes from the Pontocaspian occupy basins that have been separated from the sea by the tectonic uplift of the sea floor above the ocean level. Often, the tectonic action of crustal extension has created an alternating series of parallel grabens and horsts that form elongate basins alternating with mountain ranges. Not only does this promote

3264-662: The late 1950s, a developer at the North Branch headwaters (Farwell and Pinehill Lakes) was allowed to build a dam which raised the level of both of those lakes so that he might operate a commercial marina. The dam caused many soil sediments to enter the lake through the raised water level and resultant erosion. The residents of Farwell Lake have been very actively working to restore the once pristine quality of that lake. A municipal area sewer system branch has been added and great efforts are being made to educate lake users about keeping fuels, lawn chemicals and fertilizers, etc. out of

3332-528: The layers of sediment at the bottom of a meromictic lake remain relatively undisturbed, which allows for the development of lacustrine deposits . In a holomictic lake, the uniformity of temperature and density allows the lake waters to completely mix. Based upon thermal stratification and frequency of turnover, holomictic lakes are divided into amictic lakes , cold monomictic lakes , dimictic lakes , warm monomictic lakes, polymictic lakes , and oligomictic lakes. Lake stratification does not always result from

3400-560: The level of a lake are controlled by the difference between the input and output compared to the total volume of the lake. Significant input sources are precipitation onto the lake, runoff carried by streams and channels from the lake's catchment area, groundwater channels and aquifers, and artificial sources from outside the catchment area. Output sources are evaporation from the lake, surface and groundwater flows, and any extraction of lake water by humans. As climate conditions and human water requirements vary, these will create fluctuations in

3468-481: The mainland; lakes cut off from larger lakes by a bar; or lakes divided by the meeting of two spits. Organic lakes are lakes created by the actions of plants and animals. On the whole they are relatively rare in occurrence and quite small in size. In addition, they typically have ephemeral features relative to the other types of lakes. The basins in which organic lakes occur are associated with beaver dams, coral lakes, or dams formed by vegetation. Peat lakes are

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3536-424: The mode of origin, lakes have been named and classified according to various other important factors such as thermal stratification , oxygen saturation, seasonal variations in lake volume and water level, salinity of the water mass, relative seasonal permanence, degree of outflow, and so on. The names used by the lay public and in the scientific community for different types of lakes are often informally derived from

3604-485: The moon Titan , which orbits the planet Saturn . The shape of lakes on Titan is very similar to those on Earth. Lakes were formerly present on the surface of Mars, but are now dry lake beds . In 1957, G. Evelyn Hutchinson published a monograph titled A Treatise on Limnology , which is regarded as a landmark discussion and classification of all major lake types, their origin, morphometric characteristics, and distribution. Hutchinson presented in his publication

3672-415: The morphology of the lakes' physical characteristics or other factors. Also, different cultures and regions of the world have their own popular nomenclature. One important method of lake classification is on the basis of thermal stratification, which has a major influence on the animal and plant life inhabiting a lake, and the fate and distribution of dissolved and suspended material in the lake. For example,

3740-406: The most numerous lakes in the world. Most lakes in northern Europe and North America have been either influenced or created by the latest, but not last, glaciation, to have covered the region. Glacial lakes include proglacial lakes , subglacial lakes , finger lakes , and epishelf lakes. Epishelf lakes are highly stratified lakes in which a layer of freshwater, derived from ice and snow melt,

3808-543: The name Goguac meant Ancient Fort and was given to the lake by the Indians. A mound of earth that cut across Waupakisco peninsula was designated Ancient Fort on early maps. Indians seldom gave names to bodies of water and we now know that it was the prairie that was 'undulating' — the meaning of the Indian word Coghwagiak. The larger bay, in one place 66 feet (20 m) deep, is spring fed, but any number of stories arose as to

3876-791: The names include: Lakes may be informally classified and named according to the general chemistry of their water mass. Using this classification method, the lake types include: A paleolake (also palaeolake ) is a lake that existed in the past when hydrological conditions were different. Quaternary paleolakes can often be identified on the basis of relict lacustrine landforms, such as relict lake plains and coastal landforms that form recognizable relict shorelines called paleoshorelines . Paleolakes can also be recognized by characteristic sedimentary deposits that accumulated in them and any fossils that might be contained in these sediments. The paleoshorelines and sedimentary deposits of paleolakes provide evidence for prehistoric hydrological changes during

3944-562: The organic-rich deposits of pre-Quaternary paleolakes are important either for the thick deposits of oil shale and shale gas contained in them, or as source rocks of petroleum and natural gas . Although of significantly less economic importance, strata deposited along the shore of paleolakes sometimes contain coal seams . Lakes have numerous features in addition to lake type, such as drainage basin (also known as catchment area), inflow and outflow, nutrient content, dissolved oxygen , pollutants , pH , and sedimentation . Changes in

4012-443: The pollution of the river. For many years in the 1940s to 1960s, the river was an "eyesore" and most people did their best to avoid it. Beginning in the 1970s with the federal Clean Water Act , serious efforts were made to clean up the river. Although today the river is cleaner, the persistent PCB contamination has led to Superfund designation of a 35-mile (56 km) section from Kalamazoo to Allegan Dam. Many species of fish inhabit

4080-516: The river, including smallmouth bass , largemouth bass , catfish , carp , and many types of panfish. Though populations have increased in recent years due to the cleanup of the river, it is still advised for people to not eat large amounts of fish from the Kalamazoo River, and pregnant women are also advised not to eat any fish from the river due to lingering effects of the pollution in the diets of many fish (particularly bottom feeding fish like catfish which can accumulate high levels of mercury ). In

4148-400: The story grew to La Salle's committing himself on the beauty of this particular body of water. After slogging through swamps around hundreds of lakes in his hasty escape across southern Michigan. It is doubtful if La Salle had bothered to look at Goguac, much less to comment on its superiority. Of course he had to sleep someplace, Willard figured, so why not beside this lake? Willard also thought

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4216-404: The thermal stratification, as well as the degree and frequency of mixing, has a strong control over the distribution of oxygen within the lake. Professor F.-A. Forel , also referred to as the "Father of limnology", was the first scientist to classify lakes according to their thermal stratification. His system of classification was later modified and improved upon by Hutchinson and Löffler. As

4284-456: The times that they existed. There are two types of paleolake: Paleolakes are of scientific and economic importance. For example, Quaternary paleolakes in semidesert basins are important for two reasons: they played an extremely significant, if transient, role in shaping the floors and piedmonts of many basins; and their sediments contain enormous quantities of geologic and paleontologic information concerning past environments. In addition,

4352-658: The water. The property owners are hopeful that the dam will be removed and allow the headwaters to flow naturally again and restore the lake to its natural sandy shoreline. Although the word Kalamazoo appears to be Native American in origin, the exact meaning is obscure and various definitions have been suggested. See the article on the Etymology of Kalamazoo for a detailed discussion of name origin theories. On 26 July 2010, an Enbridge Energy pipeline leaked more than 1 million US gallons (3,800 m ) of tar sands also known as dilbit into Talmadge Creek that flows into

4420-467: The word pond , and a lesser number of names ending with lake are, in quasi-technical fact, ponds. One textbook illustrates this point with the following: "In Newfoundland, for example, almost every lake is called a pond, whereas in Wisconsin, almost every pond is called a lake." One hydrology book proposes to define the term "lake" as a body of water with the following five characteristics: With

4488-995: The world's surface freshwater, but some are salt lakes with salinities even higher than that of seawater . Lakes vary significantly in surface area and volume of water. Lakes are typically larger and deeper than ponds , which are also water-filled basins on land, although there are no official definitions or scientific criteria distinguishing the two. Lakes are also distinct from lagoons , which are generally shallow tidal pools dammed by sandbars or other material at coastal regions of oceans or large lakes. Most lakes are fed by springs , and both fed and drained by creeks and rivers , but some lakes are endorheic without any outflow, while volcanic lakes are filled directly by precipitation runoffs and do not have any inflow streams. Natural lakes are generally found in mountainous areas (i.e. alpine lakes ), dormant volcanic craters , rift zones and areas with ongoing glaciation . Other lakes are found in depressed landforms or along

4556-617: Was originally a shallow natural lake and an example of a lake basin dammed by wind-blown sand. China's Badain Jaran Desert is a unique landscape of megadunes and elongated interdunal aeolian lakes, particularly concentrated in the southeastern margin of the desert. Shoreline lakes are generally lakes created by blockage of estuaries or by the uneven accretion of beach ridges by longshore and other currents. They include maritime coastal lakes, ordinarily in drowned estuaries; lakes enclosed by two tombolos or spits connecting an island to

4624-459: Was sucked into the outlet at the bottom of the lake. he was swept all the way to the Kalamazoo River. Badly bruised but uninjured, he was not only able to walk but to run back to the hotel and sneak unobserved in the back way. His suit was shamefully torn. Just how he breathed all of that time in a tunnel of water he did not bother to explain. Lake A lake is an often naturally occurring, relatively large and fixed body of water on or near

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