A lake is an often naturally occurring, relatively large and fixed body of water on or near the Earth's surface. It is localized in a basin or interconnected basins surrounded by dry land.
Lakes are typically larger and deeper than , which are also water-filled basins on land, although there are no official definitions or scientific criteria distinguishing the two.
Natural lakes are generally found in areas (i.e. ), dormant volcano , and areas with ongoing glacier. Other lakes are found in depressed landforms or along the courses of mature rivers, where a river channel has widened over a basin formed by eroded and . Some lakes are found in caverns underground lake. 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.
Controlled lake are known as , 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.
Etymology, meaning, and usage of "lake"
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 the Proto-Indo-European root *leǵ- ('to leak, drain'). Cognates include
Dutch language laak ('lake, pond, ditch'), Middle Low German lāke ('water pooled in a riverbed, puddle') as in:
Wolfslake,
Butterlake,
German language Lache ('pool, puddle'), and Icelandic lækur ('slow flowing stream'). Also related are the English words
leak and
leach.
There is considerable uncertainty about defining the difference between lakes and , and neither term has an internationally accepted definition across scientific disciplines or political boundaries.
One hydrology book proposes to define the term "lake" as a body of water with the following five characteristics:
-
It partially or totally fills one or several basins connected by ;
-
It has essentially the same water level in all parts (except for relatively short-lived variations caused by wind, varying ice cover, large inflows, etc.);
-
It does not have regular intrusion of seawater;
-
A considerable portion of the sediment suspended in the water is captured by the basins (for this to happen they need to have a sufficiently small inflow-to-volume ratio);
-
The area measured at the mean water level exceeds an arbitrarily chosen threshold (for instance, one hectare).
With the exception of criterion 3, the others have been accepted or elaborated upon by other hydrology publications.
Distribution
The majority of lakes on Earth are
fresh water, and most lie in the Northern Hemisphere at higher
.
, with a deranged drainage system, has an estimated 31,752 lakes larger than in surface area.
The total number of lakes in Canada is unknown but is estimated to be at least 2 million.
has 168,000 lakes of in area, or larger, of which 57,000 are large ( 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.
Many lakes are artificial and are constructed for hydro-electric power generation, aesthetic purposes, 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.
Extraterrestrial lakes exist on the moon Titan, which orbits the planet Saturn.
Types
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 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
-
volcanic lakes
-
glacial lakes
-
fluvial lakes
-
solution lakes
-
landslide lakes
-
aeolian lakes
-
shoreline lakes
-
organic lakes
-
anthropogenic lakes
-
meteorite (extraterrestrial impact) lakes
Tectonic lakes
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 the largest lakes on Earth are
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 and horsts that form elongate basins alternating with mountain ranges. Not only does this promote the creation of lakes by the disruption of preexisting drainage networks, it also creates within arid regions that contain salt lakes (also called saline water 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 is .
Volcanic lakes
Volcanic lakes are lakes that occupy either local depressions, e.g. craters and
, or larger basins, e.g.
calderas, created by
volcanism. Crater lakes are formed in
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 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
or volcanic
.
The basin which is now
Malheur Lake,
Oregon was created when a lava flow dammed the
Malheur River.
Among all lake types, volcanic crater lakes most closely approximate a circular shape.
Glacial lakes
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 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
,
,
, and epishelf lakes. Epishelf lakes are highly stratified lakes in which a layer of freshwater, derived from ice and snow melt, is dammed behind an
ice shelf that is attached to the coastline. They are mostly found in Antarctica.
Fluvial lakes
Fluvial (or riverine)
lakes are lakes produced by running water. These lakes include
Plunge pool, fluviatile dams and meander lakes.
Oxbow 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 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 a higher perimeter to area ratio than other lake types.
Fluviatile dams
These form where sediment from a tributary blocks the main river.
Lateral lakes
These form where sediment from the main river blocks a tributary, usually in the form of a levee.
Floodplain lakes
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.
Solution lakes
A solution lake 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
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 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.[Neuendorf, K.K.E., Mehl Jr., J.P., and Jackson, J.A. (2005). Glossary of Geology, 5th revised and enlarged ed. Berlin: Springer. Approx. .] Limestone caves often contain pools of standing water, which are known as
. Classic examples of solution lakes are abundant in the karst regions at the
Dalmatia of
Croatia and within large parts of
Florida.
Landslide lakes
A landslide lake is created by the
Landslide dam of a
river valley by either
,
, or
. 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 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 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
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
. Aeolian lakes consist of lake basins dammed by wind-blown sand; interdunal lakes that lie between well-oriented
; and deflation basins formed by wind action under previously arid paleoenvironments.
Moses Lake in Washington, United States, 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
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 the mainland; lakes cut off from larger lakes by a bar; or lakes divided by the meeting of two spits.
Organic lakes
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
Peat lakes are 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
Artificial lakes or anthropogenic lakes are large waterbodies created by
human activity. They can be formed by the intentional
damming of rivers and streams, rerouting of water to inundate a previously dry basin, or the deliberate filling of abandoned
open-pit mine by either
precipitation surface runoff,
ground water, or a combination of both.
Artificial lakes may be used as storage reservoirs that provide
drinking water for nearby
human settlement, to generate
hydroelectricity, for
flood management, for supplying
agriculture or
aquaculture, or to provide an aquatic sanctuary for
and
.
The 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.
See: List of notable artificial lakes in the United States
Meteorite (extraterrestrial impact) lakes
Meteorite lakes, also known as
crater lakes (not to be confused with volcanic crater lakes), are created by catastrophic
Impact event with the Earth by extraterrestrial objects (either
or
).
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.
Other classification methods
In addition to 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 the morphology of the lakes' physical characteristics or other factors. Also, different cultures and regions of the world have their own popular nomenclature.
By thermal stratification
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, 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,[Forel, F.A., 1901. Handbuch der Seenkunde. Allgemeine Limnologie. J. von Engelhorn, Stuttgart, Germany.] also referred to as the "Father of limnology", was the first scientist to classify lakes according to their thermal stratification.
Based upon their thermal stratification, lakes are classified as either holomictic lake, with a uniform temperature and density from top to bottom at a given time of year, or meromictic lake, 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 . Consequently, 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 , cold , , warm monomictic lakes, , and oligomictic lakes.
Lake stratification does not always result from 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.
By seasonal variations in water level and volume
Lakes are informally classified and named according to the seasonal variation in their lake level and volume. Some of the names include:
-
Ephemeral lake is a short-lived lake or pond.
[Poehls, D.J. and Smith, G.J. eds. (2009). Encyclopedic dictionary of hydrogeology. Academic Press. p. 517. ] They often fill .
-
Dry lake is a popular name for an ephemeral lake that contains water only intermediately at irregular and infrequent intervals.
[Last, W.M. and Smol, J.P. (2001). Tracking environmental change using lake sediments. Volume 1: basin analysis, coring, and chronological techniques. Springer Science & Business Media.]
-
Perennial lake is a lake that has water in its basin throughout the year and is not subject to extreme fluctuations in level.
[Gangstad, E.O., (1979). Glossary of Biolimnological Terms. Washington, DC, United States Army Corps of Engineers.]
-
Playa lake is a typically shallow, intermittent lake that covers or occupies a playa either in wet seasons or in especially wet years but subsequently drying up in an arid or semiarid region.
-
Vlei is a name used in South Africa for a shallow lake which varies considerably in level with the seasons.
[Theal, G.M., 1877. Compendium of South African history and geography, 3rd. Institution Press, Lovedale, South Africa.]
By water chemistry
Lakes may be informally classified and named according to the general chemistry of their water mass. Using this classification method, the lake types include:
-
An acid lake contains water with a below-neutral pH of less than 6.5. A lake is considered to be highly acidic if its pH drops below 5.5, leading to biological consequences. Such lakes include: acidic pit lakes occupying abandoned mines and excavations; naturally acidic lakes of Igneous rock and Metamorphic rock landscapes; Raised bog in northern regions; crater lakes of active and dormant volcanoes; and lakes acidified by acid rain.
[Geller, W. et al. (eds.) (2013). Acidic Pit Lakes, Environmental Science and Engineering, Springer-Verlag Berlin Heidelberg][Rouwet, D. et al. (eds.) (2015). Volcanic Lakes, Advances in Volcanology, Springer-Verlag Berlin Heidelberg]
-
A salt lake, also known as a saline lake or brine lake, is an inland body of water situated in an arid or semiarid region, with no outlet to the sea, containing a high concentration of dissolved neutral salts (principally sodium chloride). Examples include the Great Salt Lake in Utah, and the Dead Sea in southwestern Asia.
-
An alkali sink, also known as an alkali flat or salt flat, is a shallow saline feature that can be found in low-lying areas of arid regions and in groundwater discharge zones. These features are typically classified as dry lakes, or playas, because they are periodically flooded by rain or flood events and then dry up during drier intervals, leaving accumulations of brines and evaporitic minerals.
-
A salt pan is a small shallow natural depression in which water accumulates and evaporates, leaving a salt deposit, or the shallow lake of brackish water that occupies a salt pan. (The term "salt pan" comes from open-pan salt making, a method of extracting salt from brine using large open pans.)
-
A saline pan is another name for an ephemeral acid saline lake which precipitates a bottom crust that is subsequently modified during subaerial exposure.
Composed of other liquids
-
Lava lake is a large volume of molten lava, usually basaltic, contained in a volcanic vent, crater, or broad depression.
-
Hydrocarbon lakes are bodies of liquid ethane and methane that occupy depressions on the surface of Titan. They were detected by the Cassini–Huygens space probe.
Paleolakes
A
paleolake (also
palaeolake) is a lake that existed in the past when hydrological conditions were different.
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
that might be contained in these sediments. The paleoshorelines and sedimentary deposits of paleolakes provide evidence for prehistoric hydrological changes during the times that they existed.
[Goudie, A. (2008). "Arid Climates and Indicators". Gornitz, V. ed., Encyclopedia of paleoclimatology and ancient environments. Springer Science & Business Media. pp. 45–51. ]
There are two types of paleolake:
-
A former lake is a paleolake that no longer exists. Such lakes include prehistoric lakes and those that have permanently dried up, often as the result of either evaporation or human intervention. An example of a former lake is Owens Lake in California, United States. Former lakes are a common feature of the Basin and Range area of southwestern North America.
-
A shrunken lake is a paleolake that still exists but has considerably decreased in size over geological time. An example of a shrunken lake is Lake Agassiz, which once covered much of central North America. Two notable remnants of Lake Agassiz are Lake Winnipeg and Lake Winnipegosis.
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.[Gierlowski-Kordesch, E. and Kelts, K.R. eds. (2000). Lake Basins Through Space and Time. AAPG Studies in Geology 46 (No. 46). The American Association of Petroleum Geologists, Tulsa, OK ]
Characteristics
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,
water pollution, pH, and
.
Changes in 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 drainage basin 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 the lake level.
Lakes can be also categorized on the basis of their richness in nutrients, which typically affect plant growth. Nutrient-poor lakes are said to be and are generally clear, having a low concentration of plant life. have good clarity and an average level of nutrients. Eutrophic lakes are enriched with nutrients, resulting in good plant growth and possible algal blooms. eutrophication lakes are bodies of water that have been excessively enriched with nutrients. These lakes typically have poor clarity and are subject to devastating algal blooms. Lakes typically reach this condition due to human activities, such as heavy use of fertilizers in the lake catchment area. Such lakes are of little use to humans and have a poor ecosystem due to decreased dissolved oxygen.
Due to the unusual relationship between water's temperature and its density, lakes form layers called , layers of drastically varying temperature relative to depth. Fresh water is most dense at about 4 degrees Celsius (39.2 °F) at sea level. When the temperature of the water at the surface of a lake reaches the same temperature as deeper water, as it does during the cooler months in temperate climates, the water in the lake can mix, bringing oxygen-starved water up from the depths and bringing oxygen down to decomposing sediments. Deep temperate lakes can maintain a reservoir of cold water year-round, which allows some cities to tap that reservoir for deep lake water cooling.
Since the surface water of deep tropical lakes never reaches the temperature of maximum density, there is no process that makes the water mix. The deeper layer becomes oxygen starved and can become saturated with carbon dioxide, or other gases such as sulfur dioxide if there is even a trace of volcano. Exceptional events, such as earthquakes or landslides, can cause mixing which rapidly brings the deep layers up to the surface and release a vast cloud of gas which lay trapped in solution in the colder water at the bottom of the lake. This is called a limnic eruption. An example is the disaster at Lake Nyos in Cameroon. The amount of gas that can be dissolved in water is directly related to pressure. As deep water surfaces, the pressure drops and a vast amount of gas comes out of solution. Under these circumstances carbon dioxide is hazardous because it is heavier than air and displaces it, so it may flow down a river valley to human settlements and cause mass asphyxiation.
The material at the bottom of a lake, or lake bed, may be composed of a wide variety of , such as silt or sand, and organic material, such as decaying plant or animal matter. The composition of the lake bed has a significant impact on the flora and fauna found within the lake's environs by contributing to the amounts and the types of nutrients available.
A paired (black and white) layer of the varved lake sediments correspond to a year. During winter, when organisms die, carbon is deposited down, resulting to a black layer. At the same year, during summer, only few organic materials are deposited, resulting to a white layer at the lake bed. These are commonly used to track past paleontological events.
Natural lakes provide a microcosm of living and nonliving elements that are relatively independent of their surrounding environments. Therefore, lake organisms can often be studied in isolation from the lake's surroundings.[ (First printed in Bulletin of the Peoria Scientific Association. 87 (1887): 77–87.)]
Limnology
Limnology is the study of inland bodies of water and related ecosystems. Limnology divides lakes into three zones: the
littoral zone, a sloped area close to land; the
photic zone or
open-water zone, where sunlight is abundant; and the deep-water
profundal zone or
benthic zone, where little sunlight can reach. The depth to which light can penetrate depends on the
turbidity of the water, which is determined by the density and size of suspended particles. A particle will be in suspension if its weight is less than the random turbidity
acting upon it. These particles can be sedimentary or
Biotic material in origin (including
algae and
detritus) and are responsible for the color of the water. Decaying plant matter, for instance, may account for a yellow or brown color, while algae may cause a greenish coloration. In very shallow water bodies, iron oxides make the water reddish brown. Bottom-dwelling
detritivorous fish stir the mud in search of food and can be the cause of turbid waters.
Piscivorous fish contribute to turbidity by eating plant-eating (
) fish, thus increasing the amount of algae (see aquatic
trophic cascade).
The light depth or transparency is measured using a Secchi disk, a 20-cm (8 in) disk with alternating white and black Circular sector. The depth at which the disk is no longer visible is the Secchi depth, a measure of transparency. The Secchi disk is commonly used to test for eutrophication. For a detailed look at these processes, see lentic ecosystems.
A lake moderates the surrounding region's temperature and climate because water has a very high specific heat capacity (4,186 J·kg−1·K−1). In the daytime a lake can cool the land beside it with local winds, resulting in a sea breeze; in the night it can warm it with a land breeze.
Biological properties
Lake zones:
-
Epilittoral: The zone that is entirely above the lake's normal water level and never submerged by lake water
-
Littoral: The zone that encompasses the small area above the normal water level (which is sometimes submerged when the lake's water level increases), reaching to the deepest part of the lake that still allows for submerged Aquatic plant growth
-
Littoriprofundal: Transition zone commonly aligned with stratified lakes' metalimnions – too deep for macrophytes but includes photosynthetic algae and bacteria
-
Profundal: Sedimentary zone containing no vegetation
Algal community types:
-
Epipelic: Algae that grow on sediments
-
Epilithic: Algae that grow on rocks
-
Epipsammic: Algae that grow on (or within) sand
-
Epiphytic: Algae that grow on macrophytes
-
Epizooic: Algae that grow on living animals
-
Metaphyton: Algae present in the littoral zone, not in a state of suspension nor attached to a substratum (such as a macrophyte)
Circulation
Flora and fauna
Disappearance
The lake may be infilled with deposited sediment and gradually become a
wetland such as a
swamp or
marsh. Large water plants, typically
Phragmites, accelerate this closing process significantly because they partially decompose to form peat soils that fill the shallows. Conversely, peat soils in a marsh can naturally burn and reverse this process to recreate a shallow lake resulting in a dynamic equilibrium between marsh and lake.
[ Ponds and Lakes. Lessons from Biologists . aquahabitat.com] This is significant since wildfire has been largely suppressed in the developed world over the past century. This has artificially converted many shallow lakes into emergent marshes. Turbid lakes and lakes with many plant-eating fish tend to disappear more slowly. A "disappearing" lake (barely noticeable on a human timescale) typically has extensive plant mats at the water's edge. These become a new habitat for other plants, like
Sphagnum when conditions are right, and animals, many of which are very rare. Gradually, the lake closes and young
peat may form, forming a
fen. In lowland river valleys where a river can
meander, the presence of peat is explained by the infilling of historical
. In the final stages of succession, trees can grow in, eventually turning the wetland into a forest.
Some lakes can disappear seasonally. These are called intermittent lakes, ephemeral lakes, or seasonal lakes and can be found in Karst. A prime example of an intermittent lake is Lake Cerknica in Slovenia or Lag Prau Pulte in Graubünden. Other intermittent lakes are only the result of above-average precipitation in a closed, or endorheic basin, usually filling dry lake beds. This can occur in some of the driest places on earth, like Death Valley. This occurred in the spring of 2005, after unusually heavy rains.[Chadwick, Alex (3 March 2005), " Wet Winter Brings Life to Death Valley". NPR.] The lake did not last into the summer, and was quickly evaporated (see photos to right). A more commonly filled lake of this type is Sevier Lake of west-central Utah.
Sometimes a lake will disappear quickly. On 3 June 2005, in Nizhny Novgorod Oblast, Russia, a lake called Lake Beloye vanished in a matter of minutes. News sources reported that government officials theorized that this strange phenomenon may have been caused by a shift in the soil underneath the lake that allowed its water to drain through channels leading to the Oka River.
The presence of ground permafrost is important to the persistence of some lakes. Thawing permafrost may explain the shrinking or disappearance of hundreds of large Arctic lakes across western Siberia. The idea here is that rising air and soil temperatures thaw permafrost, allowing the lakes to drain away into the ground.
Some lakes disappear because of human development factors. The shrinking Aral Sea is described as being "murdered" by the diversion for irrigation of the rivers feeding it. Between 1990 and 2020, more than half of the world's large lakes decreased in size, in part due to climate change.
Extraterrestrial lakes
Only one astronomical body other than Earth is known to harbor large lakes: Saturn's largest moon, Titan. Photographs and spectroscopic analysis by the
Cassini–Huygens spacecraft show liquid ethane on the surface, which is thought to be mixed with liquid methane. The largest lake on Titan is
Kraken Mare which, at an estimated 400,000 km
2,
is roughly five times the size of
Lake Superior (~80,000 km
2) and nearly the size of all five
Great Lakes of North America combined.
The second largest Titanean lake,
Ligeia Mare, is almost twice the size of Lake Superior, at an estimated 150,000 km
2.
Jupiter's large moon Io is volcanically active, leading to the accumulation of sulfur deposits on the surface. Some photographs taken during the Galileo mission appear to show lakes of liquid sulfur in volcanic caldera, though these are more analogous to lakes of lava than of water on Earth.[
]
The planet Mars has only one confirmed lake which is underground and near the south pole.
There are dark basaltic plains on the Moon, similar to lunar mare but smaller, which are called lacus (singular lacus, Latin for "lake") because they were thought by early astronomers to be lakes of water.
Notable lakes on Earth
-
The largest lake by surface area is Caspian Sea, which is despite its name considered as a lake from the point of view of geography.
-
The second largest lake by surface area, and the largest freshwater lake by surface area, is Lake Michigan-Huron, which is hydrologically a single lake. Its surface area is 45,300 sq. mi./117,400 km2. For those who consider Lake Michigan-Huron to be separate lakes, and Caspian Sea to be a sea, Lake Superior would be the largest lake at 82,100 km2 (31,700 square miles)
-
Lake Baikal is the deepest lake in the world, located in Siberia, with a bottom at . Its mean depth is also the greatest in the world (). It is also the world's largest freshwater lake by volume (, but much smaller than the Caspian Sea at ), and the second longest (about from tip to tip).
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The world's ancient lake is Lake Baikal, followed by Lake Tanganyika in Tanzania. Lake Maracaibo is considered by some to be the second-oldest lake on Earth, but since it lies at sea level and nowadays is a contiguous body of water with the sea, others consider that it has turned into a small bay.
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The longest lake is Lake Tanganyika, with a length of about (measured along the lake's center line).
It is also the third largest by volume, the second oldest, and the second deepest () in the world, after Lake Baikal.
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The world's highest lake, if size is not a criterion, may be the crater lake of Ojos del Salado, at .
[ Ojos del Salado 6893m. andes.org.uk]
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The highest large (greater than ) lake in the world is the Pumoyong Tso (Pumuoyong Tso), in the Tibet Autonomous Region of China, at , above sea level.
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The world's highest commercially navigable lake is Lake Titicaca in Peru and Bolivia at . It is also the largest lake in South America.
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The world's lowest lake is the Dead Sea, bordered by Jordan to the east and Israel and Palestine to the west, at below sea level. It is also one of the lakes with highest salt concentration.
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Lake Michigan–Huron has the longest lake coastline in the world: about , excluding the coastline of its many inner islands. Even if it is considered two lakes, Lake Huron alone would still have the longest coastline in the world at .
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The largest island in a lake is Manitoulin Island in Lake Michigan-Huron, with a surface area of . Lake Manitou, on Manitoulin Island, is the largest lake on an island in a lake.
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The largest lake on an island is Nettilling Lake on Baffin Island, with an area of and a maximum length of .
[ Largest island in a lake on an island in a lake on an island. elbruz.org]
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The largest lake in the world that drains naturally in two directions is Wollaston Lake.
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Lake Toba on the island of Sumatra is in what is probably the largest resurgent caldera on Earth.
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The largest lake completely within the boundaries of a single city is Lake Wanapitei in the city of Greater Sudbury, Ontario, Canada. Before the current city boundaries came into effect in 2001, this status was held by Lake Ramsey, also in Sudbury.
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Lake Enriquillo in Dominican Republic is the only saltwater lake in the world inhabited by .
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Lake Bernard, Ontario, Canada, claims to be the largest lake in the world with no islands.
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Lake Saimaa in both South Savonia and South Karelia, Finland, forms the much larger Saimaa basin, which have more shorelines per unit of area than anywhere else in the world, with the total length being nearly .
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The largest lake in one country is Lake Michigan, in the United States. However, it is sometimes considered part of Lake Michigan-Huron, making the record go to Great Bear Lake, Northwest Territories, in Canada, the largest lake within one jurisdiction.
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The largest lake on an island in a lake on an island is Crater Lake on Vulcano Island in Lake Taal on the island of Luzon, The Philippines.
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The northernmost named lake on Earth is Upper Dumbell Lake in the Qikiqtaaluk Region of Nunavut, Canada at a latitude of 82°28'N. It is southwest of Alert, the northernmost settlement in the world. There are also several small lakes north of Upper Dumbell Lake, but they are all unnamed and only appear on very detailed maps.
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There are only 20 - those over a million years old
Largest by continent
The largest lakes (surface area) by
continent are:
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Australia – Lake Eyre (salt lake)
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Africa – Lake Victoria, also the third-largest freshwater lake on Earth. It is one of the Great Lakes of Africa.
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Antarctica – Lake Vostok (subglacial)
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Asia – Lake Baikal (if the Caspian Sea is considered a lake, it is the largest in Eurasia, but is divided between the two geographic continents)
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Oceania – Lake Eyre when filled; the largest permanent (and freshwater) lake in Oceania is Lake Taupō.
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Europe – Lake Ladoga, followed by Lake Onega, both in northwestern Russia.
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North America – Lake Michigan–Huron, which is hydrologically a single lake. However, lakes Lake Huron and Lake Michigan are usually considered separate lakes, in which case Lake Superior would be the largest.
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South America – Lake Titicaca, which is also the highest navigable body of water on Earth at above sea level. (The much larger – and older – Lake Maracaibo is perceived by some to no longer be genuinely a lake, but a lagoon.)
See also
Notes
External links
