80-640: The Sangkulirang-Mangkalihat Karst is a karstique area in Sub Kelay, Biatan, Talisayan, Batu Putih, and Biduk-biduk Berau districts of East Kalimantan province on the island of Borneo in Indonesia . It covers an area of 105,000 hectares, including the Mangkalihat Peninsula . In May 2015, it has been nominated for inclusion in the UNESCO World Heritage Site list. The cave paintings within
160-461: A , an , the ) or German ( der, die, das, ein, eine ). A whole verb or a noun is described without articles and the grammatical gender is found from the word's termination. It is enough to say barka ('a' or 'the barge'), Noetova barka ('Noah's ark'). The gender is known in this case to be feminine. In declensions , endings are normally changed; see below. If one should like to somehow distinguish between definiteness or indefiniteness of
240-532: A mere 2.8%. During World War II , Slovenia was divided among the Axis Powers of Fascist Italy , Nazi Germany , and Hungary . Each of the occupying powers tried to either discourage or entirely suppress Slovene. Following World War II, Slovenia became part of the Socialist Federal Republic of Yugoslavia . Slovene was one of the official languages of the federation. In the territory of Slovenia, it
320-463: A noun, one would say (prav/natanko/ravno) tista barka ('that/precise/exact barge') for 'the barge' and neka/ena barka ('some/a barge') for 'a barge'. Definiteness of a noun phrase can also be discernible through the ending of the accompanying adjective. One should say rdeči šotor ('[exactly that] red tent') or rdeč šotor ('[a] red tent'). This difference is observable only for masculine nouns in nominative or accusative case. Because of
400-507: A pioneer of the study of karst in Slovenia and a fellow of the Royal Society , London, introduced the word karst to European scholars in 1689 to describe the phenomenon of underground flows of rivers in his account of Lake Cerknica . Jovan Cvijić greatly advanced the knowledge of karst regions to the point where he became known as the "father of karst geomorphology". Primarily discussing
480-620: A prominent Slovene linguist, commented that, although Slovene is not an endangered language, its scope has been shrinking, especially in science and higher education. The language is spoken by about 2.5 million people, mainly in Slovenia, but also by Slovene national minorities in Friuli-Venezia Giulia , Italy (around 90,000 in Venetian Slovenia , Resia Valley , Canale Valley , Province of Trieste and in those municipalities of
560-562: A proper noun, the Slovene form Grast was first attested in 1177. Ultimately, the word is of Mediterranean origin. It has also been suggested that the word may derive from the Proto-Indo-European root karra- 'rock'. The name may also be connected to the oronym Kar(u)sádios oros cited by Ptolemy , and perhaps also to Latin Carusardius . Johann Weikhard von Valvasor ,
640-601: A record of a proto-Slovene that was spoken in a more scattered territory than modern Slovene, which included most of the present-day Austrian states of Carinthia and Styria , as well as East Tyrol , the Val Pusteria in South Tyrol , and some areas of Upper and Lower Austria . By the 15th century, most of the northern areas were gradually Germanized : the northern border of the Slovene-speaking territory stabilized on
720-748: A relic from the now modern Russian yery character ⟨ы⟩ , which is itself usually transliterated as ⟨y⟩ ; /j/ as ⟨y⟩ ; /l/ as ⟨ll⟩ ; /ʋ/ as ⟨w⟩ ; /ʒ/ as ⟨ʃ⟩ , ⟨ʃʃ⟩ or ⟨ʃz⟩ . The standard Slovene orthography, used in almost all situations, uses only the letters of the ISO basic Latin alphabet plus ⟨č⟩ , ⟨š⟩ , and ⟨ž⟩ . The letters ⟨q⟩ , ⟨w⟩ , ⟨x⟩ , and ⟨y⟩ are not included: /uʷ/ The orthography thus underdifferentiates several phonemic distinctions: In
800-444: A singular participle combined with a plural auxiliary verb (known as polvikanje ) signals a somewhat more friendly and less formal attitude while maintaining politeness: The use of nonstandard forms ( polvikanje ) might be frowned upon by many people and would not likely be used in a formal setting. The use of the 3rd person plural oni ('they') form (known as onikanje in both direct address and indirect reference; this
880-401: A sport than a science and so the underground karst caves and their associated watercourses were, from a scientific perspective, understudied. Karst is most strongly developed in dense carbonate rock , such as limestone, that is thinly bedded and highly fractured . Karst is not typically well developed in chalk , because chalk is highly porous rather than dense, so the flow of groundwater
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#1732852683721960-576: A variety of spatial and temporal scales in karst regions, with the purpose of understanding karst aquifers and ecosystems, and the development of the surface and underground structure, so that the environment can be protected and human activities planned effectively. Slovene language Slovene ( / ˈ s l oʊ v iː n / SLOH -veen or / s l oʊ ˈ v iː n , s l ə -/ sloh- VEEN , slə- ) or Slovenian ( / s l oʊ ˈ v iː n i ə n , s l ə -/ sloh- VEE -nee-ən, slə- ; slovenščina )
1040-563: A violent policy of Fascist Italianization ; the same policy was applied to Slovene speakers in Venetian Slovenia , Gorizia and Trieste . Between 1923 and 1943, all public use of Slovene in these territories was strictly prohibited, and Slovene-language activists were persecuted by the state. After the Carinthian Plebiscite of 1920, a less severe policy of Germanization took place in the Slovene-speaking areas of southern Carinthia which remained under Austrian administration. After
1120-450: A vowel. Before a consonant or word-finally, they are reduced to /l/ , /n/ and /r/ respectively. This is reflected in the spelling in the case of /rj/ , but not for /lj/ and /nj/ . Under certain (somewhat unpredictable) circumstances, /l/ at the end of a syllable may become [w] , merging with the allophone of /ʋ/ in that position. Slovene has an eight-vowel (or, according to Peter Jurgec, nine-vowel) system, in comparison to
1200-519: A well in a fracture trace or intersection of fracture traces increases the likelihood to encounter good water production. Voids in karst aquifers can be large enough to cause destructive collapse or subsidence of the ground surface that can initiate a catastrophic release of contaminants. Groundwater flow rate in karst aquifers is much more rapid than in porous aquifers. For example, in the Barton Springs Edwards aquifer, dye traces measured
1280-710: Is a South Slavic language of the Balto-Slavic branch of the Indo-European language family . Most of its 2.5 million speakers are the inhabitants of Slovenia , majority of them ethnic Slovenes . As Slovenia is part of the European Union , Slovene is also one of its 24 official and working languages . Its syntax is highly fusional , and it has a dual grammatical number , an archaic feature shared with some other Indo-European languages . Two accentual norms (one characterized by pitch accent ) are used. Its flexible word order
1360-493: Is a UNESCO World Heritage Site. Many karst-related terms derive from South Slavic languages , entering scientific vocabulary through early research in the Western Balkan Dinaric Alpine karst. The study of the various aspects of karst regions is called karstology. This includes biological, chemical, ecological, geomorphological, hydrogeological, hydrological, political, socio-economical, and other processes over
1440-542: Is a development of karst observed in geological history and preserved within the rock sequence, effectively a fossil karst. There are for example palaeokarst surfaces exposed within the Clydach Valley Subgroup of the Carboniferous Limestone sequence of South Wales which developed as sub-aerial weathering of recently formed limestones took place during periods of non-deposition within the early part of
1520-409: Is a distinction between animate and inanimate nouns. This is only relevant for masculine nouns and only in the singular, at odds with some other Slavic languages, e.g. Russian, for which it is also relevant in the plural for all genders. Animate nouns have an accusative singular form that is identical to the genitive, while for inanimate nouns the accusative singular is the same as the nominative. Animacy
1600-525: Is a karst landscape which is developed beneath a cover of insoluble rocks. Typically this will involve a cover of sandstone overlying limestone strata undergoing solution. In the United Kingdom for example extensive doline fields have developed at Cefn yr Ystrad , Mynydd Llangatwg and Mynydd Llangynidr in South Wales across a cover of Twrch Sandstone which overlies concealed Carboniferous Limestone ,
1680-667: Is based mostly on semantics and is less rigid than gender. Generally speaking a noun is animate if it refers to something that is generally thought to have free will or the ability to move of its own accord. This includes all nouns for people and animals. All other nouns are inanimate, including plants and other non-moving life forms, and also groups of people or animals. However, there are some nouns for inanimate objects that are generally animate, which mostly include inanimate objects that are named after people or animals. This includes: There are no definite or indefinite articles as in English (
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#17328526837211760-468: Is developed in areas where salt is undergoing solution underground. It can lead to surface depressions and collapses which present a geo-hazard. Karst areas tend to have unique types of forests. The karst terrain is difficult for humans to traverse, so that their ecosystems are often relatively undisturbed. The soil tends to have a high pH, which encourages growth of unusual species of orchids, palms, mangroves, and other plants. Paleokarst or palaeokarst
1840-522: Is existence of ancient relics, among others, caves, palms, bones and teeth of ancient creatures. According to the results of a 2004 biological expedition by The Nature Conservancy and the Indonesian Institute of Sciences has identified 120 bird species, 200 species of insects, one giant cockroach, 400 species of flora and 50 species of fish. Even from the region precisely in Beriun Mountain, there
1920-612: Is frequently unseen until the roof of a cavern suddenly collapses. Such events have swallowed homes, cattle, cars, and farm machinery. In the United States, sudden collapse of such a cavern-sinkhole swallowed part of the collection of the National Corvette Museum in Bowling Green, Kentucky in 2014. The world's largest limestone karst is Australia's Nullarbor Plain . Slovenia has the world's highest risk of sinkholes, while
2000-407: Is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock , and much of this is found in porous karst systems. The English word karst was borrowed from German Karst in the late 19th century, which entered German usage much earlier, to describe a number of geological, geomorphological, and hydrological features found within
2080-399: Is not concentrated along fractures. Karst is also most strongly developed where the water table is relatively low, such as in uplands with entrenched valleys , and where rainfall is moderate to heavy. This contributes to rapid downward movement of groundwater, which promotes dissolution of the bedrock, whereas standing groundwater becomes saturated with carbonate minerals and ceases to dissolve
2160-580: Is often adjusted for emphasis or stylistic reasons, although basically it is an SVO language. It has a T–V distinction : the use of the V-form demonstrates a respectful attitude towards superiors and the elderly, while it can be sidestepped through the passive form. Standard Slovene is the national standard language that was formed in the 18th and 19th century, based on Upper and Lower Carniolan dialect groups , more specifically on language of Ljubljana and its adjacent areas. The Lower Carniolan dialect group
2240-407: Is orangutan habitat. Karst Karst ( / k ɑːr s t / ) is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite . It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering -resistant rocks such as quartzite given
2320-563: Is proved by the survival of certain ritual formulas in Slovene (such as the ritual installation of the Dukes of Carinthia). The words Buge waz primi, gralva Venus! ('God be With You, Queen Venus!'), with which Bernhard von Spanheim greeted the poet Ulrich von Liechtenstein , who was travelling around Europe in guise of Venus, upon his arrival in Carinthia in 1227 (or 1238), is another example of some level of Slovene knowledge among high nobility in
2400-505: Is similar to using Sie in German) as an ultra-polite form is now archaic or dialectal. It is associated with servant-master relationships in older literature, the child-parent relationship in certain conservative rural communities, and parishioner-priest relationships. Foreign words used in Slovene are of various types depending on the assimilation they have undergone. The types are: The loanwords are mostly from German and Italian , while
2480-611: Is the following: In very rare conditions, oxidation can play a role. Oxidation played a major role in the formation of ancient Lechuguilla Cave in the US state of New Mexico and is presently active in the Frasassi Caves of Italy. The oxidation of sulfides leading to the formation of sulfuric acid can also be one of the corrosion factors in karst formation. As oxygen (O 2 )-rich surface waters seep into deep anoxic karst systems, they bring oxygen, which reacts with sulfide present in
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2560-519: The Anschluss of 1938, the use of Slovene was strictly forbidden in Carinthia, as well. This accelerated a process of language shift in Carinthia, which continued throughout the second half of the 20th century: according to the Austro-Hungarian census of 1910, around 21% of inhabitants of Carinthia spoke Slovene in their daily communication; by 1951, this figure dropped to less than 10%, and by 2001 to
2640-530: The Protestant Reformation . The most prominent authors from this period are Primož Trubar , who wrote the first books in Slovene; Adam Bohorič , the author of the first Slovene grammar; and Jurij Dalmatin , who translated the entire Bible into Slovene. From the high Middle Ages up to the dissolution of the Austro-Hungarian Empire in 1918, in the territory of present-day Slovenia, German
2720-616: The Province of Gorizia bordering with Slovenia), in southern Carinthia , some parts of Styria in Austria (25,000) and in the western part of Croatian Istria bordering with Slovenia. It is also spoken in Rijeka and Zagreb (11,800-13,100), in southwestern Hungary (3-5,000), in Serbia (5,000), and by the Slovene diaspora throughout Europe and the rest of the world (around 300,000), particularly in
2800-800: The Slavic languages , together with Serbo-Croatian . It is close to the Chakavian and especially Kajkavian dialects of Serbo-Croatian, but genealogically more distant from the Shtokavian dialect , the basis for the Bosnian , Croatian , Montenegrin , and Serbian standard languages. Slovene in general, and Prekmurje Slovene in particular, shares the highest level of mutual intelligibility with transitional Kajkavian dialects of Hrvatsko Zagorje and Međimurje . Furthermore, Slovene shares certain linguistic characteristics with all South Slavic languages , including those of
2880-899: The Slovene Lands where compulsory schooling was in languages other than Standard Slovene, as was the case with the Carinthian Slovenes in Austria, and the Slovene minority in Italy . For example, the Resian and Torre (Ter) dialects in the Italian Province of Udine differ most from other Slovene dialects. Slovene is an Indo-European language belonging to the Western subgroup of the South Slavic branch of
2960-550: The United States (most notably Ohio , home to an estimated 3,400 speakers), Canada , Argentina , Australia and South Africa . Slovene is sometimes characterized as the most diverse Slavic language in terms of dialects , with different degrees of mutual intelligibility. Accounts of the number of dialects range from as few as seven dialects, often considered dialect groups or dialect bases that are further subdivided into as many as 50 dialects. Other sources characterize
3040-626: The range of the Dinaric Alps , stretching from the northeastern corner of Italy above the city of Trieste , across the Balkan peninsula along the coast of the eastern Adriatic to Kosovo and North Macedonia , where the massif of the Šar Mountains begins. The karst zone is at the northwesternmost section, described in early topographical research as a plateau between Italy and Slovenia . Languages preserving this form include Italian : Carso , German : Karst , and Albanian : karsti . In
3120-565: The 16th century, and ultimately led to the formation of more standard language. The Upper dialect was also used by most authors during the language revival in the 18th and early 19th centuries, and was also the language spoken by France Prešeren , who, like most of Slovene writers and poets, lived and worked in Ljubljana, where speech was growing closer to the Upper Carniolan dialect group. Unstandardized dialects are more preserved in regions of
3200-466: The 1910s is frequently closer to modern Slovene than a text from the 1920s and 1930s. Between 1920 and 1941, the official language of the Kingdom of Yugoslavia was defined as "Serbo-Croato-Slovene", which was in practice merely Serbo-Croatian. In Slovenia however, Slovene remained in use in education and administration. Many state institutions used only Serbo-Croatian, and a Slovene–Serbo-Croatian bilingualism
3280-404: The 2nd person singular ti form (known as tikanje ) is officially limited to friends and family, talk among children, and addressing animals, it is increasingly used among the middle generation to signal a relaxed attitude or lifestyle instead of its polite or formal counterpart using the 2nd person plural vi form (known as vikanje ). An additional nonstandard but widespread use of
Sangkulirang-Mangkalihat Karst - Misplaced Pages Continue
3360-550: The Eastern subgroup, namely Bulgarian , Macedonian and Torlakian dialects. Mutual intelligibility with varieties of Serbo-Croatian is hindered by differences in vocabulary, grammar, and pronunciation, Kajkavian being firmly the most mutually intelligible . Slovene has some commonalities with the West Slavic languages that are not found in other South Slavic languages. Like all Slavic languages , Slovene traces its roots to
3440-515: The areas around Trieste . During most of the Middle Ages, Slovene was a vernacular language of the peasantry, although it was also spoken in most of the towns on Slovenian territory, together with German or Italian. Although during this time, German emerged as the spoken language of the nobility, Slovene had some role in the courtly life of the Carinthian, Carniolan and Styrian nobility, as well. This
3520-511: The bedrock. The carbonic acid that causes karst features is formed as rain passes through Earth's atmosphere picking up carbon dioxide (CO 2 ), which readily dissolves in the water. Once the rain reaches the ground, it may pass through soil that provides additional CO 2 produced by soil respiration . Some of the dissolved carbon dioxide reacts with the water to form a weak carbonic acid solution, which dissolves calcium carbonate . The primary reaction sequence in limestone dissolution
3600-606: The caves in the Sangkulirang-Mangkalihat karsts was suggested to be a Geopark in April 2017. The paintings were researched extensively by Indonesia's Heritage Preservation Hall (BPCB) for its preservation. The closest major airport to the geopark is Samarinda International Airport . The area is upstream of five major rivers in Berau and East Kutai, namely Tabalar River, Lesan River, Pesab River, Bengalon River and Karangan River. There
3680-450: The complexity of karst aquifers, and need to be supplemented with dye traces , measurement of spring discharges, and analysis of water chemistry. U.S. Geological Survey dye tracing has determined that conventional groundwater models that assume a uniform distribution of porosity are not applicable for karst aquifers. Linear alignment of surface features such as straight stream segments and sinkholes develop along fracture traces . Locating
3760-542: The end of words unless immediately followed by a word beginning with a vowel or a voiced consonant. In consonant clusters, voicing distinction is neutralized and all consonants assimilate the voicing of the rightmost segment, i.e. the final consonant in the cluster. In this context, [v] , [ɣ] and [d͡z] may occur as voiced allophones of /f/ , /x/ and /t͡s/ , respectively (e.g. vŕh drevésa [ʋrɣ dreˈʋesa] ). /ʋ/ has several allophones depending on context. The sequences /lj/ , /nj/ and /rj/ occur only before
3840-483: The excessive usage of regionalisms. Regionalisms are mostly limited to culinary and agricultural expressions, although there are many exceptions. Some loanwords have become so deeply rooted in the local language that people have considerable difficulties in finding a standard expression for the dialect term (for instance, kremšnita meaning a type of custard cake is kremna rezina in Standard Slovene, but
3920-505: The first novel in Slovene in 1866. This tendency was reversed in the Fin de siècle period by the first generation of modernist Slovene authors (most notably the writer Ivan Cankar ), who resorted to a more "pure" and simple language without excessive Serbo-Croatian borrowings. During the Kingdom of Yugoslavia in the 1920s and 1930s, the influence of Serbo-Croatian increased again. This was opposed by
4000-557: The fissures. The enlarged fissures allow a larger quantity of water to enter which leads to a progressive enlargement of openings. Abundant small openings store a large quantity of water. The larger openings form a conduit system that drains the aquifer to springs. Characterization of karst aquifers requires field exploration to locate sinkholes, swallets , sinking streams , and springs in addition to studying geologic maps . Conventional hydrogeologic methods such as aquifer tests and potentiometric mapping are insufficient to characterize
4080-415: The five-vowel system of Serbo-Croatian. Slovene nouns retain six of the seven Slavic noun cases: nominative , accusative , genitive , dative , locative and instrumental . There is no distinct vocative ; the nominative is used in that role. Nouns, adjectives and pronouns have three numbers: singular, dual and plural. Nouns in Slovene are either masculine, feminine or neuter gender. In addition, there
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#17328526837214160-466: The global demand for drinkable water. Farming in karst areas must take into account the lack of surface water. The soils may be fertile enough, and rainfall may be adequate, but rainwater quickly moves through the crevices into the ground, sometimes leaving the surface soil parched between rains. The karst topography also poses peculiar difficulties for human inhabitants. Sinkholes can develop gradually as surface openings enlarge, but progressive erosion
4240-456: The karst groundwater flow rates from 0.5 to 7 miles per day (0.8 to 11.3 km/d). The rapid groundwater flow rates make karst aquifers much more sensitive to groundwater contamination than porous aquifers. Groundwater in karst areas is also just as easily polluted as surface streams, because Karst formations are cavernous and highly permeable, resulting in reduced opportunity for contaminant filtration. Well water may also be unsafe as
4320-525: The karst regions of the Balkans, Cvijić's 1893 publication Das Karstphänomen describes landforms such as karren, dolines and poljes . In a 1918 publication, Cvijić proposed a cyclical model for karst landscape development. Karst hydrology emerged as a discipline in the late 1950s and the early 1960s in France. Previously, the activities of cave explorers, called speleologists , had been dismissed as more of
4400-433: The lack of article in Slovene and audibly insignificant difference between the masculine adjective forms, most dialects do not distinguish between definite and indefinite variants of the adjective, leading to hypercorrection when speakers try to use Standard Slovene. Slovene, like most other European languages, has a T–V distinction , or two forms of 'you' for formal and informal situations. Although informal address using
4480-552: The last-named locality having been declared a site of special scientific interest in respect of it. Kegelkarst is a type of tropical karst terrain with numerous cone-like hills, formed by cockpits, mogotes , and poljes and without strong fluvial erosion processes. This terrain is found in Cuba, Jamaica, Indonesia, Malaysia, the Philippines, Puerto Rico, southern China, Myanmar, Thailand, Laos and Vietnam. Salt karst (or 'halite karst')
4560-549: The latter term is very rarely used in speech being considered inappropriate for non-literary registers ). Southwestern dialects incorporate many calques and loanwords from Italian, whereas eastern and northwestern dialects are replete with lexemes of German origin. Usage of such words hinders intelligibility between dialects and is greatly discouraged in formal situations. Slovene has a phoneme set consisting of 21 consonants and 8 vowels . Slovene has 21 distinctive consonant phonemes. All voiced obstruents are devoiced at
4640-476: The line going from north of Klagenfurt to south of Villach and east of Hermagor in Carinthia, while in Styria it was more or less identical with the current Austrian-Slovenian border. This linguistic border remained almost unchanged until the late 19th century, when a second process of Germanization took place, mostly in Carinthia. Between the 9th and 12th century, proto-Slovene spread into northern Istria and in
4720-412: The local South Slavic languages , all variations of the word are derived from a Romanized Illyrian base (yielding Latin : carsus , Dalmatian : carsus ), later metathesized from the reconstructed form * korsъ into forms such as Slovene : kras and Serbo-Croatian : krš , kras , first attested in the 18th century, and the adjective form kraški in the 16th century. As
4800-752: The more recently borrowed and less assimilated words are typically from English . This alphabet ( abeceda ) was derived in the mid-1840s from the system created by the Croatian linguist Ljudevit Gaj . Intended for the Serbo-Croatian language (in all its varieties), it was patterned on the Czech alphabet of the 1830s. Before that /s/ was, for example, written as ⟨ ʃ ⟩ , ⟨ʃʃ⟩ or ⟨ſ⟩ ; /tʃ/ as ⟨tʃch⟩ , ⟨cz⟩ , ⟨tʃcz⟩ or ⟨tcz⟩ ; /i/ sometimes as ⟨y⟩ as
4880-637: The most dramatic of these formations can be seen in Thailand 's Phangnga Bay and at Halong Bay in Vietnam . Calcium carbonate dissolved into water may precipitate out where the water discharges some of its dissolved carbon dioxide. Rivers which emerge from springs may produce tufa terraces, consisting of layers of calcite deposited over extended periods of time. In caves, a variety of features collectively called speleothems are formed by deposition of calcium carbonate and other dissolved minerals. Interstratal karst
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#17328526837214960-585: The number of dialects as nine or eight. The Slovene proverb "Every village has its own voice" ( Vsaka vas ima svoj glas ) depicts the differences in dialects. The Prekmurje dialect used to have a written norm of its own at one point. The Resian dialects have an independent written norm that is used by their regional state institutions. Speakers of those two dialects have considerable difficulties with being understood by speakers of other varieties of Slovene, needing code-switching to Standard Slovene. Other dialects are mutually intelligible when speakers avoid
5040-704: The period. Sedimentation resumed and further limestone strata were deposited on an irregular karst surface, the cycle recurring several times in connection with fluctuating sea levels over prolonged periods. Pseudokarsts are similar in form or appearance to karst features but are created by different mechanisms. Examples include lava caves and granite tors —for example, Labertouche Cave in Victoria, Australia —and paleocollapse features. Mud Caves are an example of pseudokarst. Karst formations have unique hydrology, resulting in many unusual features. A karst fenster (karst window) occurs when an underground stream emerges onto
5120-466: The post-breakup influence of Serbo-Croatian on Slovene continued to a lesser extent, most prominently in slang in colloquial language . Joža Mahnič , a literary historian and president of the publishing house Slovenska matica , said in February 2008 that Slovene is a language rich enough to express everything, including the most sophisticated and specialised texts. In February 2010, Janez Dular ,
5200-511: The region. The first printed Slovene words, stara pravda (meaning 'old justice' or 'old laws'), appeared in 1515 in Vienna in a poem of the German mercenaries who suppressed the Slovene peasant revolt : the term was presented as the peasants' motto and battle cry. Standard Slovene emerged in the second half of the 16th century, thanks to the works of Slovene Lutheran authors, who were active during
5280-418: The right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of paleokarst (buried karst in the stratigraphic column )
5360-533: The rise of Romantic nationalism in the 19th century, the cultural movements of Illyrism and Pan-Slavism brought words from Serbo-Croatian , specifically Croatian dialects, and Czech into standard Slovene, mostly to replace words previously borrowed from German. Most of these innovations have remained, although some were dropped in later development. In the second half of the 19th century, many nationalist authors made an abundant use of Serbo-Croatian words: among them were Fran Levstik and Josip Jurčič , who wrote
5440-757: The river flows into a cave in a formation known as the Madison Limestone and then rises again 800 m ( 1 ⁄ 2 mi) down the canyon in a placid pool. A turlough is a unique type of seasonal lake found in Irish karst areas which are formed through the annual welling-up of water from the underground water system. Main Article Aquifer#Karst Karst aquifers typically develop in limestone . Surface water containing natural carbonic acid moves down into small fissures in limestone. This carbonic acid gradually dissolves limestone thereby enlarging
5520-514: The same proto-Slavic group of languages that produced Old Church Slavonic . The earliest known examples of a distinct, written dialect connected to Slovene are from the Freising manuscripts , known in Slovene as Brižinski spomeniki . The consensus estimate of their date of origin is between 972 and 1039 (most likely before 1000). These religious writings are among the oldest surviving manuscripts in any Slavic language. The Freising manuscripts are
5600-625: The surface between layers of rock, cascades some distance, and then disappears back down, often into a sinkhole. Rivers in karst areas may disappear underground a number of times and spring up again in different places, even under a different name, like Ljubljanica , the "river of seven names". Another example of this is the Popo Agie River in Fremont County, Wyoming , where, at a site named "The Sinks" in Sinks Canyon State Park ,
5680-415: The surface, complex underground drainage systems (such as karst aquifers ) and extensive caves and cavern systems may form. Erosion along limestone shores, notably in the tropics , produces karst topography that includes a sharp makatea surface above the normal reach of the sea, and undercuts that are mostly the result of biological activity or bioerosion at or a little above mean sea level . Some of
5760-1002: The system ( pyrite or hydrogen sulfide ) to form sulfuric acid (H 2 SO 4 ). Sulfuric acid then reacts with calcium carbonate, causing increased erosion within the limestone formation. This chain of reactions is: This reaction chain forms gypsum . The karstification of a landscape may result in a variety of large- or small-scale features both on the surface and beneath. On exposed surfaces, small features may include solution flutes (or rillenkarren), runnels , limestone pavement (clints and grikes), kamenitzas collectively called karren or lapiez. Medium-sized surface features may include sinkholes or cenotes (closed basins), vertical shafts, foibe (inverted funnel shaped sinkholes), disappearing streams, and reappearing springs . Large-scale features may include limestone pavements , poljes , and karst valleys. Mature karst landscapes, where more bedrock has been removed than remains, may result in karst towers , or haystack/eggbox landscapes. Beneath
5840-414: The tonemic varieties of Slovene, the ambiguity is even greater: ⟨e⟩ in a final syllable can stand for any of /éː/ /èː/ /ɛ́ː/ /ɛ̀ː/ /ɛ/ /ə/ (although /ɛ̀ː/ is rare; and Slovene, except in some dialects, does not distinguished tonemic accentuation). The reader is expected to gather the interpretation of the word from the context, as in these examples: To compensate for the shortcomings of
5920-461: The water may have run unimpeded from a sinkhole in a cattle pasture, bypassing the normal filtering that occurs in a porous aquifer . Sinkholes have often been used as farmstead or community trash dumps . Overloaded or malfunctioning septic tanks in karst landscapes may dump raw sewage directly into underground channels. Geologists are concerned with these negative effects of human activity on karst hydrology which, as of 2007 , supplied about 25% of
6000-507: The western Highland Rim in the eastern United States is at the second-highest risk of karst sinkholes. In Canada, Wood Buffalo National Park , Northwest Territories contains areas of karst sinkholes. Mexico hosts important karst regions in the Yucatán Peninsula and Chiapas . The West of Ireland is home to The Burren , a karst limestone area. The South China Karst in the provinces of Guizhou , Guangxi , and Yunnan provinces
6080-414: The younger generations of Slovene authors and intellectuals; among the most fierce opponents of an excessive Serbo-Croatian influence on Slovene were the intellectuals associated with the leftist journal Sodobnost , as well as some younger Catholic activists and authors. After 1945, numerous Serbo-Croatian words that had been used in the previous decades were dropped. The result was that a Slovene text from
6160-476: Was applied in many spheres of public life in Slovenia. For example, at the post offices, railways and in administrative offices, Serbo-Croatian was used alongside Slovene. However, state employees were expected to be able to speak Slovene in Slovenia. During the same time, western Slovenia (the Slovenian Littoral and the western districts of Inner Carniola ) was under Italian administration and subjected to
6240-566: Was commonly used in almost all areas of public life. One important exception was the Yugoslav army , where Serbo-Croatian was used exclusively, even in Slovenia. National independence has further fortified the language: since 1991, when Slovenia gained independence, Slovene has been used as an official language in all areas of public life. In 2004 it became one of the official languages of the European Union upon Slovenia's admission. Nonetheless,
6320-434: Was the dialect used in the 16th century by Primož Trubar for his writings, while he also used Slovene as spoken in Ljubljana, since he lived in the city for more than 20 years. It was the speech of Ljubljana that Trubar took as a foundation of what later became standard Slovene, with small addition of his native speech, that is Lower Carniolan dialect . Trubar's choice was later adopted also by other Protestant writers in
6400-399: Was the language of the elite, and Slovene was the language of the common people. During this period, German had a strong influence on Slovene, and many Germanisms are preserved in contemporary colloquial Slovene. Many Slovene scientists before the 1920s also wrote in foreign languages, mostly German, which was the lingua franca of science throughout Central Europe at the time. During
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