131-623: Lake Dyupkun (Дюпкун) is a vast, isolated lake stretching for 90 kilometres (56 mi) in the southwest of the Putorana Plateau in Northern Siberia . The Kureika River flows through the lake from south to north. It lies on marshy ground at the bottom of a valley and has an area of 199 km. The lake's left bank is the location of the Talnikovy Waterfall , claimed to be the highest in all of Asia . It
262-578: A common ancestor with languages such as English, German, and the Scandinavian languages . All Germanic languages are subject to the Grimm's law and Verner's law sound shifts, which originated in the Proto-Germanic language and define the basic features differentiating them from other Indo-European languages. This is assumed to have taken place in approximately the mid-first millennium BCE in
393-467: A schwa . The Middle Dutch dialect areas were affected by political boundaries. The sphere of political influence of a certain ruler often also created a sphere of linguistic influence, with the language within the area becoming more homogenous. Following the contemporary political divisions they are in order of importance: A process of standardisation started in the Middle Ages , especially under
524-601: A synod taking place in Corbridge , England , where the decisions are being written down " tam Latine quam theodisce " meaning "in Latin as well as common vernacular". According to a hypothesis by De Grauwe, In northern West Francia (i.e. modern-day Belgium) the term would take on a new meaning during the Early Middle Ages , when, within the context of a highly dichromatic linguistic landscape, it came to be
655-409: 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
786-576: A comparison between the West Germanic languages, see the sections Phonology, Grammar, and Vocabulary. Dutch dialects are primarily the dialects that are both related with the Dutch language and are spoken in the same language area as the Dutch standard language . Although heavily under the influence of the standard language, some of them remain diverse and are found in the Netherlands and in
917-500: 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
1048-467: A consequence evolve (along with Alemannic , Bavarian and Lombardic ) into Old High German. At more or less the same time the Ingvaeonic nasal spirant law, moving over Western Europe from west to east, led to the development of Old English (or Anglo-Saxon), Old Frisian and Old Saxon . Hardly influenced by either development, Old Dutch probably remained relatively close to the original language of
1179-402: 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
1310-538: 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
1441-510: 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,
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#17327831125091572-428: 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
1703-470: 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
1834-582: A minority language in Germany and northern France's French Flanders . Though Belgium as a whole is multilingual, three of the four language areas into which the country is divided ( Flanders , francophone Wallonia , and the German-speaking Community ) are largely monolingual, with Brussels being bilingual. The Netherlands and Belgium produce the vast majority of music , films , books and other media written or spoken in Dutch. Dutch
1965-670: A minority) and the province of Walloon Brabant . Brabantian expands into small parts in the west of Limburg while its strong influence on the East Flemish of East Flanders and eastern Zeelandic Flanders weakens towards the west. In a small area in the northwest of North Brabant ( Willemstad ), Hollandic is spoken. Conventionally, the Kleverlandish dialects are distinguished from Brabantian, but there are no objective criteria apart from geography to do so. Over 5 million people live in an area with some form of Brabantian being
2096-489: 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,
2227-420: A number of closely related, mutually intelligible dialects spoken in the former Old Dutch area. Where Old Dutch fragments are very hard to read for untrained Modern Dutch speakers, the various literary works of Middle Dutch are somewhat more accessible. The most notable difference between Old and Middle Dutch is in a feature of speech known as vowel reduction , whereby vowels in unstressed syllables are leveled to
2358-579: A political border, because the traditional dialects are strongly influenced by the national standard varieties. While a somewhat heterogeneous group of Low Franconian dialects, Limburgish has received official status as a regional language in the Netherlands and Germany, but not in Belgium. Due to this official recognition, it receives protection by chapter 2 of the European Charter for Regional or Minority Languages . Afrikaans , although to
2489-403: 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
2620-535: 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
2751-413: A result, Nederduits no longer serves as a synonym for the Dutch language. In the 19th century, the term " Diets " was revived by Dutch linguists and historians as well, as a poetic name for Middle Dutch and its literature . Old Dutch can be discerned more or less around the same time as Old English (Anglo-Saxon), Old High German , Old Frisian , and Old Saxon . These names are derived from
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#17327831125092882-509: A result, when West Flemings try to talk Standard Dutch, they are often unable to pronounce the g-sound, and pronounce it similar to the h-sound. This leaves, for example, no difference between " held " (hero) and " geld " (money). Or in some cases, they are aware of the problem, and hyper-correct the "h" into a voiced velar fricative or g-sound, again leaving no difference. The West Flemish variety historically spoken in adjacent parts in France
3013-522: A significant degree mutually intelligible with Dutch, is usually not considered a dialect but instead a separate standardised language . It is spoken in South Africa and Namibia. As a daughter language of 17th-century Dutch dialects, Afrikaans evolved in parallel with modern Dutch, but was influenced by various other languages in South Africa. West Frisian ( Westerlauwers Fries ), along with Saterland Frisian and North Frisian , evolved from
3144-479: A somewhat different development since the late Middle Ages. Two dialect groups have been given the official status of regional language (or streektaal ) in the Netherlands. Like several other dialect groups, both are part of a dialect continuum that continues across the national border. The Dutch Low Saxon dialect area comprises the provinces of Groningen , Drenthe and Overijssel , as well as parts of
3275-424: A source language, mainly for law and history students. In Indonesia this involves about 35,000 students. Unlike other European nations, the Dutch chose not to follow a policy of language expansion amongst the indigenous peoples of their colonies. In the last quarter of the 19th century, however, a local elite gained proficiency in Dutch so as to meet the needs of expanding bureaucracy and business. Nevertheless,
3406-552: A unique prestige dialect and has a large dialectal continuum consisting of 28 main dialects, which can themselves be further divided into at least 600 distinguishable varieties. In the Netherlands, the Hollandic dialect dominates in national broadcast media while in Flanders Brabantian dialect dominates in that capacity, making them in turn unofficial prestige dialects in their respective countries. Outside
3537-422: 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
3668-537: Is kantor , handdoek "towel" in Indonesian is handuk , or bushalte "bus stop" in Indonesian is halte bus . In addition, many Indonesian words are calques of Dutch; for example, rumah sakit "hospital" is calqued on the Dutch ziekenhuis (literally "sickhouse"), kebun binatang "zoo" on dierentuin (literally "animal garden"), undang-undang dasar "constitution" from grondwet (literally "ground law"). These account for some of
3799-443: 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
3930-466: Is a calque of the aforementioned Roman province Germania Inferior and an attempt by early Dutch grammarians to give their language more prestige by linking it to Roman times. Likewise, Hoogduits ("High German") and Overlands ("Upper-landish") came into use as a Dutch exonym for the various German dialects used in neighboring German states. Use of Nederduytsch was popular in the 16th century but ultimately lost out over Nederlands during
4061-544: Is a monocentric language , at least what concerns its written form, with all speakers using the same standard form (authorised by the Dutch Language Union ) based on a Dutch orthography defined in the so-called " Green Booklet " authoritative dictionary and employing the Latin alphabet when writing; however, pronunciation varies between dialects. Indeed, in stark contrast to its written uniformity, Dutch lacks
Lake Dyupkun - Misplaced Pages Continue
4192-403: 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
4323-537: Is also an official language of several international organisations, such as the European Union , Union of South American Nations and the Caribbean Community . At an academic level, Dutch is taught in about 175 universities in 40 countries. About 15,000 students worldwide study Dutch at university. In Europe, Dutch is the majority language in the Netherlands (96%) and Belgium (59%) as well as
4454-468: 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
4585-587: Is found in the Salic law . In this Frankish document written around 510 the oldest Dutch sentence has been identified: Maltho thi afrio lito ("I say to you, I free you, serf") used to free a serf. Another old fragment of Dutch is Visc flot aftar themo uuatare ("A fish was swimming in the water"). The oldest conserved larger Dutch text is the Utrecht baptismal vow (776–800) starting with Forsachistu diobolae ... ec forsacho diabolae (litt.: "Forsake you
4716-414: Is located southeast of Lake Khantayskoye . This Krasnoyarsk Krai location article is a stub . You can help Misplaced Pages by expanding it . 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
4847-452: 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
4978-522: Is mostly Germanic; it incorporates slightly more Romance loans than German, but far fewer than English. In Belgium, the Netherlands and Suriname, the native official name for Dutch is Nederlands (historically Nederlandsch before the Dutch orthographic reforms ). Sometimes Vlaams (" Flemish ") is used as well to describe Standard Dutch in Flanders , whereas Hollands (" Hollandic ")
5109-487: Is occasionally used as a colloquial term for the standard language in the central and northwestern parts of the Netherlands. English uses the adjective Dutch as a noun for the language of the Netherlands and Flanders. The word is derived from Proto-Germanic *þiudiskaz . The stem of this word, *þeudō , meant "people" in Proto-Germanic, and *-iskaz was an adjective-forming suffix, of which -ish
5240-569: Is so distinct that it might be considered as a separate language variant, although the strong significance of language in Belgian politics would prevent the government from classifying them as such. An oddity of the dialect is that, the voiced velar fricative (written as "g" in Dutch) shifts to a voiced glottal fricative (written as "h" in Dutch), while the letter "h" becomes mute (like in French). As
5371-585: Is sometimes called French Flemish and is listed as a French minority language . However, only a very small and aging minority of the French-Flemish population still speaks and understands West Flemish. Hollandic is spoken in Holland and Utrecht , though the original forms of this dialect (which were heavily influenced by a West Frisian substratum and, from the 16th century on, by Brabantian dialects ) are now relatively rare. The urban dialects of
Lake Dyupkun - Misplaced Pages Continue
5502-637: Is spoken in Limburg (Belgium) as well as in the remaining part of Limburg (Netherlands) and extends across the German border. West Flemish ( Westvlaams ) is spoken in West Flanders , the western part of Zeelandic Flanders and also in French Flanders , where it virtually became extinct to make way for French. The West Flemish group of dialects, spoken in West Flanders and Zeeland ,
5633-595: Is taught in various educational centres in Indonesia, the most important of which is the Erasmus Language Centre (ETC) in Jakarta . Each year, some 1,500 to 2,000 students take Dutch courses there. In total, several thousand Indonesians study Dutch as a foreign language. Owing to centuries of Dutch rule in Indonesia, many old documents are written in Dutch. Many universities therefore include Dutch as
5764-662: Is the Modern English form. Theodiscus was its Latinised form and used as an adjective referring to the Germanic vernaculars of the Early Middle Ages . In this sense, it meant "the language of the common people". The term was used as opposed to Latin , the non -native language of writing and the Catholic Church . It was first recorded in 786, when the Bishop of Ostia writes to Pope Adrian I about
5895-404: Is the case with the ( standardised ) West Frisian language . It is spoken alongside Dutch in the province of Friesland . Dutch dialects and regional languages are not spoken as often as they used to be, especially in the Netherlands. Recent research by Geert Driessen shows that the use of dialects and regional languages among both Dutch adults and youth is in heavy decline. In 1995, 27 percent of
6026-448: Is the native language of the majority of the population of Suriname , and spoken as a second or third language in the polyglot Caribbean island countries of Aruba , Curaçao and Sint Maarten . All these countries have recognised Dutch as one of their official languages, and are involved in one way or another in the Dutch Language Union . The Dutch Caribbean municipalities ( St. Eustatius , Saba and Bonaire ) have Dutch as one of
6157-530: Is the sole official language, and over 60 percent of the population speaks it as a mother tongue . Dutch is the obligatory medium of instruction in schools in Suriname, even for non-native speakers. A further twenty-four percent of the population speaks Dutch as a second language . Suriname gained its independence from the Netherlands in 1975 and has been an associate member of the Dutch Language Union since 2004. The lingua franca of Suriname, however,
6288-429: 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
6419-531: The 2006 New Zealand census , 26,982 people, or 0.70 percent of the total population, reported to speak Dutch to sufficient fluency that they could hold an everyday conversation. In contrast to the colonies in the East Indies , from the second half of the 19th century onwards, the Netherlands envisaged the expansion of Dutch in its colonies in the West Indies . Until 1863, when slavery was abolished in
6550-578: The Bergakker inscription , found near the Dutch city of Tiel , which may represent a primary record of 5th-century Frankish. Although some place names recorded in Roman texts such as vadam (modern Dutch: wad , English: "mudflat"), could arguably be considered as the oldest single "Dutch" words, the Bergakker inscription yields the oldest evidence of Dutch morphology. However, interpretations of
6681-455: The Brussels and Flemish regions of Belgium . The areas in which they are spoken often correspond with former medieval counties and duchies. The Netherlands (but not Belgium) distinguishes between a dialect and a streektaal (" regional language "). Those words are actually more political than linguistic because a regional language unites a large group of very different varieties. Such is
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#17327831125096812-554: The High German consonant shift , does not use Germanic umlaut as a grammatical marker, has largely abandoned the use of the subjunctive , and has levelled much of its morphology , including most of its case system . Features shared with German, however, include the survival of two to three grammatical genders – albeit with few grammatical consequences – as well as the use of modal particles , final-obstruent devoicing , and (similar) word order . Dutch vocabulary
6943-493: The Low Countries , its meaning being largely implicitly provided by the regional orientation of medieval Dutch society: apart from the higher echelons of the clergy and nobility, mobility was largely static and hence while "Dutch" could by extension also be used in its earlier sense, referring to what today would be called Germanic dialects as opposed to Romance dialects , in many cases it was understood or meant to refer to
7074-591: The Low Franconian languages, paired with its sister language Limburgish or East Low Franconian. Its closest relative is the mutually intelligible daughter language Afrikaans. Other West Germanic languages related to Dutch are German , English and the un-standardised languages Low German and Yiddish . Dutch stands out in combining some Ingvaeonic characteristics (occurring consistently in English and Frisian and reduced in intensity from west to east over
7205-759: 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
7336-499: 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
7467-531: The Randstad , which are Hollandic dialects, do not diverge from standard Dutch very much, but there is a clear difference between the city dialects of Rotterdam , The Hague , Amsterdam and Utrecht . In some rural Hollandic areas more authentic Hollandic dialects are still being used, especially north of Amsterdam. Another group of dialects based on Hollandic is that spoken in the cities and larger towns of Friesland , where it partially displaced West Frisian in
7598-543: The Southern Netherlands (now Belgium and Luxembourg), developments were different. Under subsequent Spanish , Austrian and French rule , the standardisation of Dutch language came to a standstill. The state, law, and increasingly education used French, yet more than half the Belgian population were speaking a variety of Dutch. In the course of the 19th century, the Flemish Movement stood up for
7729-497: The antonym of *walhisk (Romance-speakers, specifically Old French ). The word, now rendered as dietsc (Southwestern variant) or duutsc (Central and Northern Variant), could refer to the Dutch language itself, as well as a broader Germanic category depending on context. During the High Middle Ages " Dietsc / Duutsc " was increasingly used as an umbrella term for the specific Germanic dialects spoken in
7860-471: The continental West Germanic plane) with dominant Istvaeonic characteristics, some of which are also incorporated in German. Unlike German, Dutch (apart from Limburgish) has not been influenced at all by the south to north movement of the High German consonant shift and had some changes of its own. The cumulation of these changes resulted over time in separate, but related standard languages with various degrees of similarities and differences between them. For
7991-399: 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
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#17327831125098122-434: The differences in vocabulary between Indonesian and Malay. Some regional languages in Indonesia have some Dutch loanwords as well; for example, Sundanese word Katel or "frying pan" origin in Dutch is " ketel ". The Javanese word for "bike/ bicycle " " pit " can be traced back to its origin in Dutch " fiets ". The Malacca state of Malaysia was also colonized by the Dutch in its longest period that Malacca
8253-605: 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 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
8384-642: The pre-Roman Northern European Iron Age . The Germanic languages are traditionally divided into three groups: East (now extinct), West , and North Germanic. They remained mutually intelligible throughout the Migration Period . Dutch is part of the West Germanic group, which also includes English, Scots , Frisian , Low German (Old Saxon) and High German . It is characterised by a number of phonological and morphological innovations not found in North or East Germanic. The West Germanic varieties of
8515-518: The 14th to 15th century onward, its urban centers ( Deventer , Zwolle , Kampen , Zutphen and Doesburg ) have been increasingly influenced by the western written Dutch and became a linguistically mixed area. From the 17th century onward, it was gradually integrated into the Dutch language area. Dutch Low Saxon used to be at one end of the Low German dialect continuum . However, the national border has given way to dialect boundaries coinciding with
8646-538: The 16th century and is known as Stadsfries ("Urban Frisian"). Hollandic together with inter alia Kleverlandish and North Brabantian , but without Stadsfries, are the Central Dutch dialects . Brabantian is named after the historical Duchy of Brabant , which corresponded mainly to the provinces of North Brabant and southern Gelderland , the Belgian provinces of Antwerp and Flemish Brabant , as well as Brussels (where its native speakers have become
8777-688: The 7th century. It was replaced in France by Old French (a Romance language with a considerable Old Frankish influence). However, the Old Franconian language did not die out at large, as it continued to be spoken in the Low Countries, and subsequently evolved into what is now called Old Low Franconian or Old Dutch in the Low Countries. In fact, Old Frankish could be reconstructed from Old Dutch and Frankish loanwords in Old French. The term Old Dutch or Old Low Franconian refers to
8908-417: The Dutch adult population spoke a dialect or regional language on a regular basis, but in 2011, that was no more than 11 percent. In 1995, 12 percent of children of primary school age spoke a dialect or regional language, but in 2011, that had declined to four percent. Of the officially recognised regional languages Limburgish is spoken the most (in 2011 among adults 54%, among children 31%) and Dutch Low Saxon
9039-490: The Dutch government remained reluctant to teach Dutch on a large scale for fear of destabilising the colony. Dutch, the language of power, was supposed to remain in the hands of the leading elite. After independence, Dutch was dropped as an official language and replaced by Indonesian , but this does not mean that Dutch has completely disappeared in Indonesia: Indonesian Dutch , a regional variety of
9170-415: The Dutch standard language is largely absent, and speakers of these Dutch dialects will use German or French in everyday speech. Dutch is not afforded legal status in France or Germany, either by the central or regional public authorities, and knowledge of the language is declining among younger generations. As a foreign language , Dutch is mainly taught in primary and secondary schools in areas adjacent to
9301-531: The Dutch standard language, it is not mutually intelligible with Dutch and considered a sister language of Dutch, like English and German. Approximate distribution of native Dutch speakers worldwide: Dutch is an official language of the Netherlands proper (not enshrined in the constitution but in administrative law ), Belgium, Suriname, the Dutch Caribbean municipalities (St. Eustatius, Saba and Bonaire), Aruba , Curaçao and Sint Maarten . Dutch
9432-408: The Dutch, was still spoken by about 500,000 half-blood in Indonesia in 1985. Yet the Indonesian language inherited many words from Dutch: words for everyday life as well as scientific and technological terms. One scholar argues that 20% of Indonesian words can be traced back to Dutch words, many of which are transliterated to reflect phonetic pronunciation e.g. kantoor "office" in Indonesian
9563-597: 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
9694-602: The Franks. However, the language did experience developments of its own, such as very early final-obstruent devoicing . In fact, the find at Bergakker indicates that the language may already have experienced this shift during the Old Frankish period. Attestations of Old Dutch sentences are extremely rare. The language is mostly recorded on fragmentary relics, and words have been reconstructed from Middle Dutch and loan words from Old Dutch in other languages. The oldest recorded
9825-571: 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
9956-576: The Netherlands and Flanders . In French-speaking Belgium , over 300,000 pupils are enrolled in Dutch courses, followed by over 23,000 in the German states of Lower Saxony and North Rhine-Westphalia , and about 7,000 in the French region of Nord-Pas-de-Calais (of which 4,550 are in primary school). At an academic level, the largest number of faculties of neerlandistiek can be found in Germany (30 universities), followed by France (20 universities) and
10087-412: The Netherlands and Belgium, the dialect spoken in and around the German town of Kleve ( Kleverlandish ) is historically and genetically a Low Franconian variety. In North-Western France, the area around Calais was historically Dutch-speaking (West Flemish), of which an estimated 20,000 are daily speakers. The cities of Dunkirk , Gravelines and Bourbourg only became predominantly French-speaking by
10218-539: The Netherlands, although there are recognisable differences in pronunciation, comparable to the pronunciation differences between standard British and standard American English. In 1980 the Netherlands and Belgium concluded the Language Union Treaty . This treaty lays down the principle that the two countries must gear their language policy to each other, among other things, for a common system of spelling. Dutch belongs to its own West Germanic sub-group,
10349-674: The United Kingdom (5 universities). Despite the Dutch presence in Indonesia for almost 350 years, as the Asian bulk of the Dutch East Indies , the Dutch language has no official status there and the small minority that can speak the language fluently are either educated members of the oldest generation, or employed in the legal profession such as historians, diplomats, lawyers, jurists and linguists/polyglots, as certain law codes are still only available in Dutch. Dutch
10480-621: The West Indies, slaves were forbidden to speak Dutch, with the effect that local creoles such as Papiamento and Sranan Tongo which were based not on Dutch but rather other European languages, became common in the Dutch West Indies. However, as most of the people in the Colony of Surinam (now Suriname ) worked on Dutch plantations, this reinforced the use of Dutch as a means for direct communication. In Suriname today, Dutch
10611-661: The area known as the Low Countries goes back further in time, with the Romans referring to the region as Germania Inferior ("Lower" Germania). It is a reference to the Low Countries' downriver location at the Rhine–Meuse–Scheldt delta near the North Sea . From 1551, the designation Nederlands received strong competition from the name Nederduytsch (literally "Low Dutch", Dutch being used in its archaic sense covering all continental West Germanic languages). It
10742-866: 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,
10873-624: The borders of other standard language areas. In most cases, the heavy influence of the standard language has broken the dialect continuum . Examples are the Gronings dialect spoken in Groningen as well as the closely related varieties in adjacent East Frisia (Germany). Kleverlandish is a dialect spoken in southern Gelderland , the northern tip of Limburg , and northeast of North Brabant (Netherlands), but also in adjacent parts of North Rhine-Westphalia (Germany). Limburgish ( Limburgs )
11004-479: The case with the Gronings dialect , which is considered a variety of the Dutch Low Saxon regional language, but it is relatively distinct from other Dutch Low Saxon varieties. Also, some Dutch dialects are more remote from the Dutch standard language than some varieties of a regional language are. Within the Netherlands, a further distinction is made between a regional language and a separate language, which
11135-553: The close of the 18th century, with (Hoog)Duytsch establishing itself as the Dutch exonym for German during this same period. In the 19th century Germany saw the rise of the categorisation of dialects, with German dialectologists terming the German dialects spoken in the mountainous south of Germany as Hochdeutsch ("High German"). Subsequently, German dialects spoken in the north were designated as Niederdeutsch ("Low German"). The names for these dialects were calqued by Dutch linguists as Nederduits and Hoogduits . As
11266-413: The course of fifteen centuries. During that period, they forced Old Frisian back from the western coast to the north of the Low Countries, and influenced or even replaced Old Saxon spoken in the east (contiguous with the Low German area). On the other hand, Dutch has been replaced in adjacent lands in present-day France and Germany. The division into Old, Middle and Modern Dutch is mostly conventional, since
11397-915: 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
11528-518: 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
11659-540: The declaration of independence of Indonesia, Western New Guinea , the "wild east" of the Dutch East Indies , remained a Dutch colony until 1962, known as Netherlands New Guinea . Despite prolonged Dutch presence, the Dutch language is not spoken by many Papuans, the colony having been ceded to Indonesia in 1963. Dutch-speaking immigrant communities can also be found in Australia and New Zealand. The 2011 Australian census showed 37,248 people speaking Dutch at home. At
11790-603: The development of a separate Dutch language. It was spoken by the descendants of the Salian Franks who occupied what is now the southern Netherlands , northern Belgium , part of northern France, and parts of the Lower Rhine regions of Germany. The High German consonant shift, moving over Western Europe from south to west, caused a differentiation with the Central and High Franconian in Germany. The latter would as
11921-474: The devil? ... I forsake the devil"). If only for its poetic content, the most famous Old Dutch sentence is probably Hebban olla vogala nestas hagunnan, hinase hic enda tu, wat unbidan we nu ("All birds have started making nests, except me and you, what are we waiting for"), is dated to around the year 1100, written by a Flemish monk in a convent in Rochester , England . Since the sentence speaks to
12052-622: 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
12183-489: The end of the 19th century. In the countryside, until World War I , many elementary schools continued to teach in Dutch, and the Catholic Church continued to preach and teach the catechism in Dutch in many parishes. During the second half of the 19th century, Dutch was banned from all levels of education by both Prussia and France and lost most of its functions as a cultural language. In both Germany and France,
12314-536: 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
12445-422: 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
12576-415: The imagination, it is often erroneously stated as the oldest Dutch sentence. Old Dutch naturally evolved into Middle Dutch . The year 1150 is often cited as the time of the discontinuity, but it actually marks a time of profuse Dutch writing; during this period a rich Medieval Dutch literature developed. There was at that time no overarching standard language ; Middle Dutch is rather a collective name for
12707-711: The influence of the Burgundian Ducal Court in Dijon ( Brussels after 1477). The dialects of Flanders and Brabant were the most influential around this time. The process of standardisation became much stronger at the start of the 16th century, mainly based on the urban dialect of Antwerp . The 1585 fall of Antwerp to the Spanish army led to a flight to the northern Netherlands, where the Dutch Republic declared its independence from Spain. This influenced
12838-907: 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
12969-471: 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
13100-510: The lake level. Dutch language Dutch ( endonym : Nederlands [ˈneːdərlɑnts] ) is a West Germanic language of the Indo-European language family , spoken by about 25 million people as a first language and 5 million as a second language and is the third most spoken Germanic language. In Europe, Dutch is the native language of most of the population of the Netherlands and Flanders (which includes 60% of
13231-563: The language now known as Dutch. In the Low Countries Dietsch or its Early Modern Dutch form Duytsch as an endonym for Dutch gradually went out of common use and was gradually replaced by the Dutch endonym Nederlands . This designation (first attested in 1482) started at the Burgundian court in the 15th century, although the use of neder , laag , bas , and inferior ("nether" or "low") to refer to
13362-657: 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
13493-528: 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
13624-629: The least (adults 15%, children 1%). The decline of the West Frisian language in Friesland occupies a middle position (adults 44%, children 22%). Dialects are most often spoken in rural areas, but many cities have a distinct city dialect. For example, the city of Ghent has very distinct "g", "e" and "r" sounds that greatly differ from its surrounding villages. The Brussels dialect combines Brabantian with words adopted from Walloon and French . Some dialects had, until recently, extensions across
13755-560: 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
13886-481: 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
14017-424: 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
14148-437: The modern standard languages . In this age no standard languages had yet developed, while a perfect West Germanic dialect continuum remained present; the division reflects the contingent future contribution dialect groups would have to the later languages. The early form of Dutch was a set of Franconian dialects spoken by the Salian Franks in the 5th century. These happened to develop through Middle Dutch to Modern Dutch over
14279-485: 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
14410-415: 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,
14541-406: 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,
14672-791: 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
14803-501: The official languages. In Asia, Dutch was used in the Dutch East Indies (now mostly Indonesia ) by a limited educated elite of around 2% of the total population, including over 1 million indigenous Indonesians, until it was banned in 1957, but the ban was lifted afterwards. About a fifth of the Indonesian language can be traced to Dutch, including many loan words . Indonesia's Civil Code has not been officially translated, and
14934-562: 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
15065-533: The original Dutch language version dating from colonial times remains the authoritative version. Up to half a million native speakers reside in the United States, Canada and Australia combined, and historical linguistic minorities on the verge of extinction remain in parts of France and Germany. Dutch is one of the closest relatives of both German and English, and is colloquially said to be "roughly in between" them. Dutch, like English, has not undergone
15196-524: The population of Belgium ). Dutch was one of the official languages of South Africa until 1925, when it was replaced by Afrikaans , a separate but partially mutually intelligible daughter language of Dutch. Afrikaans, depending on the definition used, may be considered a sister language , spoken, to some degree, by at least 16 million people, mainly in South Africa and Namibia , and evolving from Cape Dutch dialects. In South America, it
15327-527: The predominant colloquial language out of the area's 22 million Dutch-speakers. Limburgish , spoken in both Belgian Limburg and Netherlands Limburg and in adjacent parts in Germany, is considered a dialect in Belgium, while having obtained the official status of regional language in the Netherlands. Limburgish has been influenced by the Ripuarian varieties like the Colognian dialect , and has had
15458-411: The provinces of Gelderland , Flevoland , Friesland and Utrecht . This group, which is not Low Franconian but instead Low Saxon and close to neighbouring Low German, has been elevated by the Netherlands (and by Germany) to the legal status of streektaal ( regional language ) according to the European Charter for Regional or Minority Languages . It is regarded as Dutch for a number of reasons. From
15589-515: The rest of the text lack any consensus. The Franks emerged in the southern Netherlands ( Salian Franks ) and central Germany ( Ripuarian Franks ), and later descended into Gaul . The name of their kingdom survives in that of France. Although they ruled the Gallo-Romans for nearly 300 years, their language, Frankish , became extinct in most of France and was replaced by later forms of the language throughout Luxembourg and Germany in around
15720-423: The rights of Dutch speakers, mostly referred to as "Flemish". However, the dialect variation was a serious disadvantage in the face of the standardised francophony . Since standardisation is a lengthy process, Dutch-speaking Belgium associated itself with the standard language that had already developed in the Netherlands over the centuries. Therefore, the situation in Belgium is essentially no different from that in
15851-524: The same branch of the West Germanic languages as Old English (i.e. Anglo-Frisian ) and are therefore genetically more closely related to English and Scots than to Dutch. The different influences on the respective languages, however, particularly that of Norman French on English and Dutch on West Frisian, have rendered English quite distinct from West Frisian, and West Frisian less distinct from Dutch than from English. Although under heavy influence of
15982-455: The set of Franconian dialects (i.e. West Germanic varieties that are assumed to have evolved from Frankish ) spoken in the Low Countries during the Early Middle Ages , from around the 5th to the 12th century. Old Dutch is mostly recorded on fragmentary relics, and words have been reconstructed from Middle Dutch and Old Dutch loanwords in French. Old Dutch is regarded as the primary stage in
16113-404: 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
16244-545: The time are generally split into three dialect groups: Ingvaeonic (North Sea Germanic), Istvaeonic (Weser–Rhine Germanic) and Irminonic (Elbe Germanic). It appears that the Frankish tribes fit primarily into the Istvaeonic dialect group with certain Ingvaeonic influences towards the northwest, which are still seen in modern Dutch. The Frankish language itself is not directly attested, the only possible exception being
16375-456: 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,
16506-466: The transition between them was very gradual. One of the few moments when linguists can detect something of a revolution is when the Dutch standard language emerged and quickly established itself. The development of the Dutch language is illustrated by the following sentence in Old, Middle and Modern Dutch: Among the Indo-European languages , Dutch is grouped within the Germanic languages , meaning it shares
16637-641: 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
16768-484: The urban dialects of the province of Holland . In 1637, a further important step was made towards a unified language, when the Statenvertaling , the first major Bible translation into Dutch, was created that people from all over the new republic could understand. It used elements from various, even Dutch Low Saxon , dialects but was predominantly based on the urban dialects of Holland of post 16th century. In
16899-467: 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
17030-617: 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
17161-527: Was under foreign control. In the 19th century, the East Indies trade started to dwindle, and with it the importance of Malacca as a trading post. The Dutch state officially ceded Malacca to the British in 1825. It took until 1957 for Malaya to gain its independence. Despite this, the Dutch language is rarely spoken in Malacca or Malaysia and only limited to foreign nationals able to speak the language. After
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