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70-488: Kozani borders the regional units of Kastoria to the west and northwest, Florina to the north, Pella to the northeast, Imathia and Pieria to the east, Larissa (part of Thessaly ) to the southeast, and Grevena to the south. The main mountain ranges are Askio in the northwest, Voio in the west, Vermio in the northeast and the Pierian Mountains in the southeast. The river Aliakmon flows through

140-664: A Bulgarian national consciousness. Colonel Anastasios Dalipis in 1945 stated Kastoria prefecture had a total of 110 villages with 75 populated by Slavophones. During 1951, the Greek census recorded 1,009 Slavophones in Kastoria district. The Greek National Intelligence Service conducted a secret census in 1954 and Slavophones in Kastoria district numbered 17,229. Information supplied to diplomat Dimitrios Bitsios and academic Evangelos Kofos by local representatives in 1965 estimated Slavophones in Kastoria district numbered 40,000. In

210-465: A Greek national consciousness. Language groups: 76,370 Slavophones; 38,844 Grecophones (natives and refugees); 3,508 Turcophones (refugees); 4,500 Aromanians and 2,500 Albanians. Greek sentiments among language groups: 14,420 Slavophones; 38,854 Grecophones (natives and refugees); 3,508 Turcophones (refugees); 3,000 Aromanians and 1,800 Albanians. In 1940, Kastoria district had a population of 68,237. The Greek ministers for Military Affairs, Justice and

280-409: 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

350-500: 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

420-402: 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

490-538: 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

560-510: 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,

630-428: 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

700-470: 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

770-489: 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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840-671: A prosperous area in the course of its history. Its merchants are known to have dominated the commerce of the Balkan peninsula , expanding their trade activities to the north and along the Danube . Nowadays, Kozani is still among the most prosperous areas of the Greek province, but for a different reason, its rich mining industry . Kozani produces lignite , which is the main source of the electric power produced in Greece, nitrous salts which are processed into fertilizers , and chromium . There

910-403: 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

980-535: 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

1050-422: 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

1120-443: 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

1190-403: 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

1260-468: 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

1330-452: 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

1400-447: Is mountainous with a pronounced continental climate, characterised by cold winters and hot summers. The regional unit Kastoria is subdivided into 3 municipalities. These are (number as in the map in the infobox): Kastoria was created as a prefecture ( Greek : Νομός Καστοριάς ) in 1941. As a part of the 2011 Kallikratis government reform , the regional unit Kastoria was created out of the former prefecture Kastoria. The prefecture had

1470-428: Is one of the 74 regional units of Greece and is part of the region of Western Macedonia . Its capital is the homonymous city of Kastoria . Kastoria is situated at the western end of Macedonia in the far north of the country. It borders the regional units of Florina to the north, Kozani to the southeast, Grevena to the south and Ioannina to the southwest. The area of the regional unit roughly corresponds to

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1540-429: 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

1610-724: The Kastoria regional units. Refugees from Asia Minor and Pontus during the Greco-Turkish War of 1919 to 1922 brought refugees to the area including Kozani and villages and towns that removed the Turkish population to the country which later became only known as Turkey. The economy boomed and was disrupted later on. After World War II and the Greek Civil War , most of the buildings were repaired. Kozani opened its airport and later its hospital. Kozani has been

1680-759: 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

1750-554: 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

1820-510: The ancient Greek region of Orestis of Upper Macedonia . The international border with the Albanian district of Korçë lies on the western edge of the regional unit. The main mountain ranges are Gramos and Voio in the west (both part of the Pindus range) and Verno in the northeast. The Haliacmon river flows through the area. Lake Orestiada is the largest lake. The regional unit

1890-399: 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

1960-518: The 1923 census as "the least unreliable" for its numbers of language groups in the area. A quarter of all inhabitants in the Kastoria region were Muslims and they, including Muslim Albanophones were sent to Turkey as part of the Greek–Turkish population exchange based on religious criteria. A small number of Muslim Albanians were excluded from the population exchange and remained in the Kastoria region. In 1924, Greek authorities compiled data of

2030-411: The 1924 data by Greek authorities. Greek refugees arrived in the Kastoria area, while their settlement was limited by the lack of fertile land and the need for stable bilateral relations with Yugoslavia which also prevented mass Slavophone emigration. In Greek Macedonia, Kastoria province remained an area in the interwar period where Slavophones were a large part of the population. A 1925 study by

2100-745: The 1990s, the European Commission 's Euromosaic project documenting minority languages recorded 77 (Slavo) Macedonian/Bulgarian villages in the Prefecture of Kastoria, spread among its subdivisions, Kastoria and Argos Orestiko. Slavophones were concentrated in certain areas within the prefecture and a significant small part of the population had knowledge of and used the Macedonian language , being aware of its cultural value. A survey (1999–2005) conducted by linguist Christian Voss of Slavic speaking villages in Greece, counted 117 villages in

2170-597: 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

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2240-547: The Greek 10th Army Division of Western Macedonia recorded 1,866 refugee families were settled in 28 villages within the Kastoria region. Greek refugee families in Kastoria prefecture were from East Thrace (41), Asia Minor (441), Pontus (1,417), the Caucasus (23) and unidentified locations (9) in 1926. In 1928, there were 1,928 refugee families (7,554 people). In the Kastoria region, the number of refugees reached 8,370. The official and unpublished Greek census (1925) for

2310-530: The Interior ordered a census (1945) of citizens with "Bulgarian sentiments" who numbered 11,380 in Kastoria Prefecture. Greek Foreign Minister Ioannis Politis ordered the compilation of demographic data by a committee from the Greek political establishment regarding the Prefecture of Kastoria in 1945. The total prefecture population was 58,590, and Slavophones numbered 21,867 with 13,517 having

2380-470: The Kastoria district recorded 17,737 native Greeks and 5,962 Greek refugees; 14,807 Slavophone former Exarchists; 7,339 Slavophone former Patriarchists; 2,195 Aromanian speakers (pro–Greek), 135 Aromanian speakers (pro–Romanian); 525 Jews, 213 Muslim Albanians and 29 foreigners. A report (January 1925) by the Florina prefect stated the total Kastoria district population was 47,500. Slavophones (29,500) were

2450-571: 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

2520-418: The administrative region of Western Macedonia which included the prefecture of Kastoria. Artificial lake 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 lie completely on land and are separate from the ocean , although they may be connected with

2590-866: 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,

2660-417: The coastline, it is rainier than the south. Temperatures range from 25 to 30 °C (77 to 86 °F) during the summer months. The regional unit Kozani is subdivided into 5 municipalities. These are (number as in the map in the infobox): Kozani was created as a prefecture ( Greek : Νομός Κοζάνης ) in 1915. As a part of the 2011 Kallikratis government reform , the regional unit Kozani was created out of

2730-915: 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

2800-518: 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

2870-622: 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

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2940-411: The ethnological composition of Greek Macedonia . Kastoria district had a total of 68,340 inhabitants composed of 22,768 Greeks; 14,448 Muslims; 7,519 Slavophone former Patriarchists ; 22,079 Slavophone former Exarchists ; 220 Aromanian speakers (pro–Romanian); 1,211 Jews and 95 refugees. Political categories from a nationalist perspective were used to describe ethnic groups or religious affiliations in

3010-536: 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

3080-407: The former prefecture Kozani. The prefecture had the same territory as the present regional unit. At the same time, the municipalities were reorganised. The municipality Servia-Velventos was split into the municipalities Servia and Velventos in 2019. Kozani had three provinces : The area was part of several kingdoms of Upper Macedonia , including the ancient Eordaia and Elimiotis , and it

3150-422: 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

3220-907: 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

3290-471: 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

3360-657: 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

3430-528: 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

3500-560: 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

3570-481: 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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3640-472: The majority population and divided between Exarchists or "Schismatics" (22,000) who supported Bulgaria and Patriarchists (7,500) who supported Greece. Native Greeks numbered 10,500 and refugees were 7,500. A refugee committee report (1942) from Bulgarian occupied northern Greece using League of Nations data covering 1913 to 1928 stated the numbers of Slav Macedonian emigrants from Kastoria district to Bulgaria were 4,070. Koliopoulos commented 4,200 emigrants

3710-424: 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

3780-485: 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

3850-415: 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,

3920-406: 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,

3990-791: 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

4060-789: The north was largely, though not entirely populated by Slavic speakers, while the south mainly had Grecophones. The demographics of the Kastoria region were affected by the population exchanges Greece had with Bulgaria (voluntary, 1919) and Turkey (compulsory, 1923) . Numbers of Slavic speakers decreased. After 1913, a few Christian families from the new state of Albania settled in several villages within Kastoria district. The official and unpublished Greek census (1923) recorded 68,245 people in Kastoria district, with 29,598 Slav Macedonian Christians and 22,768 Greeks who also included Aromanian speakers and Albanian speakers. Muslims numbered either 13,767 people (or 2425 families) or 14,448 inhabitants and 1,794 Jews. Historian John Koliopoulos described

4130-556: 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 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

4200-562: 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

4270-602: The same territory as the present regional unit. At the same time, the municipalities were reorganised, according to the table below. The Kastoria region was part of the Ottoman Empire for several centuries and following the Balkan Wars (1912–1913) became part of Greece. There were religious communities such as Christians, Muslims and Jews and groups of Turcophones, Greeks , Aromanians and Slavophones . The rural areas of Kastoria province were multi–ethnic, as

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4340-404: The southern part, and through the large reservoir Lake Polyfytos . Lignite is mined in the north, around Ptolemaida . Its climate ranges from continental to mountainous. Kozani has warm to hot summers and cool winters, cooler than Thessaloniki, the mountainous, the western and the eastern portions receive cold winters and features snow. Its sunshine days are days shorter than the south and by

4410-404: 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

4480-456: 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,

4550-641: 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

4620-467: 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

4690-548: Was a figure reflecting nearer the realities of the period. The 1942 report wrote the combined number of Slav Macedonians of the interwar period in Kastoria and Florina districts was 37,000. Another estimate on the interwar period put the number of Slav Macedonians in Kastoria district at 12,000. A report in 1930 by Florina prefect P. Kalligas recorded the combined population of the Florina/Kastoria region as 125,722 and 58,882 had Greek sentiments and 61,950 were without

4760-517: Was also an asbestos mine that remained operational until the mid-1990s, which has now ceased its operation. In the regional unit of Kozani there is also the artificial lake and hydroelectric dam of Polyfytos , which further contributes to the electricity production of Greece. The region's vast industrial advancement in a short period of time has raised environmentalist concerns. Kastoria (regional unit) Kastoria ( Greek : Περιφερειακή Ενότητα Καστοριάς , Perifereiakí Enótita Kastoriás )

4830-728: Was later part of the kingdom of Macedonia . After the Third Macedonian War it was ruled by the Roman Empire . It later became a part of the Byzantine Empire after the breakup into the West and the East . In the early 14th to the 15th century, it was ruled by the Ottoman Empire and lasted until the Balkan Wars of 1913. The Kozani Prefecture was created in 1915 and also included the present Florina , Grevena and

4900-617: 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

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