Krivošije ( Cyrillic : Кривошије , pronounced [kriv̞ɔ̌ʃijɛ] ) is a microregion in southwestern Montenegro , located on a high plateau belonging to the Orjen mountain range, north of the Bay of Kotor . Krivošije was historically located at a tripoint between the Principality of Montenegro , Austro-Hungarian (formerly Venetian ) Bay of Kotor and Ottoman Sanjak of Herzegovina .
58-466: Krivošije are a mountainous karst region above Risan , located at around 1000 metres above the sea level, spanning on 114 km of land. It is a high plateau on the northern and eastern branches of Mount Orjen (1894 m) in southwest Montenegro , near in the hinterland of the Bay of Kotor . A significant geological and geomorphological feature of the region are the glacial deposits distributed across
116-476: A meal, the contents of which depends on whether or not the celebration falls in a period of fasting . During a fast ( post ), the meal would not contain any meat but seafood ( pesco-vegan ). Outside of a fasting period, these restrictions would not apply and the Slava is considered mrsna . Thus, colloquially, slavas can be referred to as posna or mrsna . Appropriately-made sweets are consumed, as well. Alcohol
174-519: 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
232-582: 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 ,
290-418: A resurgence. It is recognized as a distinctly (if not quite exclusively) Serbian custom, and today it is quite common for nonobservant Christians or even atheists to celebrate it in one form or another, as a hereditary family holiday and a mark of ethnocultural identification. The custom is also helpful in genealogical studies as an indicator in kinship relations between families, such as tracing one's family to
348-590: A specific region. It "becomes a simultaneous signifier of national and spiritual kinship and a core expression of the Serbian cosmology, whereby the dialectics of temporal, physical, and spiritual continuity converge into validated perceptions of cultural and social reality—re-enacted on a recurrent (annual) basis. In November 2014 it was inscribed in the UNESCO Intangible Cultural Heritage Lists of Serbia . The tradition
406-401: 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
464-580: A total of three times. In other traditions the bread is "broken" together by the guests after being ritually turned. The koljivo is a symbol of the Resurrection of Christ (cf. "if the grain does not die..." in the Gospel ) and partaken in memory of the dead (deceased family members). The cutting into the bread three times is a symbolism of the Holy Trinity . The rest of the feast consists of
522-410: 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. Krsna slava Overseas Slava ( Serbian : Слава , lit. 'Celebration', pronounced [ˈslâʋa] )
580-529: 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
638-456: Is Serbian ethnic identification marker is simply delusion of the romantic and patriotic citizenry". The increased effective geographic mobility brought about by the post World War II urbanization of a previously highly agrarian society, combined with the suppression of Serbian Orthodox traditions under the Communist rule, has made some aspects of the custom more relaxed. In particular, in
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#1732765263908696-505: 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
754-562: 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
812-411: Is a family's annual ceremony and veneration of their patron saint . The ceremony is found mainly among Orthodox Serbs . Although its origin is unknown, this old tradition is an important ethnic marker of Serbian identity . It is a tribute to the family's first ancestor, through the male lineage, who was baptized into Christianity, with its presiding saint. The family celebrates the Slava annually on
870-538: 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 ,
928-495: Is a reinterpretation of a Serbian pagan rite: the ancestor-protector became a Christian saint, frequently St. Nicholas , with the pagan rite being reduced of many religious elements and frequent ceremonies and becoming a social event with the annual meeting of the family and friends. In the scientific literature exists a discussion about the historical and ethnological origin of the Slava, which has not been completed. According to some Serbian researchers, "the thesis of how Slava
986-478: Is also very well preserved among the Serb diaspora . Besides present day Serbia, Slava is commonly celebrated amongst ethnic Serbs living in neighbouring Croatia, Bosnia and Montenegro. Despite the tradition being inherently tied to Serbian Orthodox Christianity it is also practiced to a lesser extent amongst some Catholic and Muslim ethnicities in the region, occasionally among Croats , as well as Catholics from
1044-418: Is an important ethnic marker of Serbian identity . The slogan: Где је слава, ту је Србин ( Gde je slava, tu je Srbin , lit. ' Where there is a Slava, there is a Serb ' ) was raised as a Serbian national identifier by Miloš Milojević after his travel to Kosovo and Metohija in 1871–1877. Serbs usually regard the Slava as their most significant and most solemn feast day . The tradition
1102-468: 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
1160-636: 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
1218-399: 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
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#17327652639081276-419: Is passed down from father to son and only males are allowed to carry out the Slava's rituals. Upon marriage, women typically adopt the patron saint of their spouse although it is not uncommon for them to continue celebrating their native family's saint as well (in which case the secondary one is known as preslava ). Close friends and family gather at the home for a ritual feast. Although a religious ceremony for
1334-515: Is served to adults. The most common feast days are St. Nicholas ( Nikoljdan , 19 December), St. George ( Đurđevdan , 6 May), St. John the Baptist ( Jovanjdan , 20 January), St. Demetrius ( Mitrovdan , 8 November), St. Michael ( Aranđelovdan , 21 November) and St. Sava ( Savindan , 27 January). Dates given are according to the Gregorian calendar . The Serbian Orthodox Church uses
1392-491: Is some evidence that karst may occur in more weathering -resistant rocks such as quartzite given 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
1450-621: 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
1508-480: The Ascension of Jesus Christ as its patronal feast. A Slava celebration incorporates aspects of pagan traditions with minimal clerical involvement. The ritual foods that are prepared for the feast are the slavski kolač (or simply kolač ), a ritual bread, and koljivo (or žito ), a dish of minced boiled wheat, sweetened and sometimes mixed with chopped walnuts. A beeswax candle stamped with an image of
1566-613: The Bay of Kotor . As of 2018, Krivošije, which covers roughly a third of the Kotor Municipality , has only around 110 permanent residents, in comparison with 1,053 inhabitants recorded in 1953. Most common slava (patron saint day) of the Krivošije clan is St. John the Baptist ( Jovanjdan ), celebrated on 20 January. The following churches were built in Krivošije: A species of funnel-web spider called Histopona krivosijana
1624-487: The Christian cross , the peace dove , and other symbols. The kolač symbolizes the body of Jesus , and the wine with which the kolač is eaten represents his blood. The parish priest, either at the home or at the church, consecrates the kolač with wine; afterwards the man of the household cuts it into quarters and turns it cut-side up. It is further cut into pieces by other family members and oldest or most important guests,
1682-636: 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
1740-435: The stratigraphic column ) 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
1798-538: The Bay of Kotor , and Gorani living in present-day southern Kosovo. Furthermore, similar tradition can be found in Western Bulgaria and North Macedonia and also among some Vlachs and Aromanians . The Slava is a family 's annual ceremony and veneration of their patron saint. It is a tribute to the family's first ancestor who was baptized into Christianity, with its presiding saint. The family's patron saint
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1856-629: The Slava has its origin in Medieval Serbia , connected to Saint Sava , the first Archbishop of the Serbs . There are indications that the institution of the Slava in the Serbian Orthodox Church dates from Saint Sava, that "in his understanding and tactful approach to Serbian folk religion", he "seems to have found a compromise formula satisfactory to both his people's pagan tradition and the requirements of theology". The slava
1914-587: The Slava has its origins in Greek and Roman hero cult. Proponents of the Greek hypothesis point to etymology in that the Serbian word for wheat, koljivo , an indispensable item of the Slava, is derived from the Greek term for gain of wheat, koliva . Proponents of the Roman hypothesis point to the fact that Slava customs mimic Roman forms of celebration including bread breaking and toasting. Another hypothesis states that
1972-511: 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
2030-450: 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
2088-557: 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
2146-466: 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
2204-583: The highest annual precipitation in the Europe), Dragalj , Han , Malov Do , Knežlaz , Ubli [ sr ] , Unijerina and Zvečava . Krivošije was under Austro-Hungarian control (as part of the Kingdom of Dalmatia ) since the Congress of Vienna in 1814. In 1869 an uprising of the local population, which was Orthodox Serb defeated an expedition force of the powerful Austro-Hungarian army that
2262-456: 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
2320-534: 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
2378-562: 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')
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2436-412: 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
2494-647: 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
2552-709: 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
2610-399: The purpose of saint veneration, the family's intent behind the celebration is for "the good health of the living" as well as for a "general remembrance of the souls of the departed family members". Many Serbian communities (villages, cities, organizations, political parties, institutions, companies, professions) also celebrate their patron saint . For example, the city of Belgrade celebrates
2668-985: The region. However, two Partisan detachments were also established in Krivošije under the Communist Party cell in Herceg Novi . In September 1944, the battles of the 10th Montenegrin NOV brigade in Krivošije had the largest echo in the Bay of Kotor and Paštrovići . Mountainous Krivošije region was mostly inhabited by the tribes of Old Montenegro , but also partially by settlers from Herzegovina . The following families were listed as inhabitants of Krivošije: Radulović , Vučurović , Samardžić , Odalović, Kovač , Radojičić , Ilić , Bojanić , Kokotović , Vukićević , Komnenović , Tomović , Vodovar, Žmukić, Popović , Blagojević , Lakićević, Subotić , Miletić , Vidović and Lazović . Krivošije region faced significant demographic outflows in recent decades, particularly towards
2726-780: 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
2784-406: The saint is also a staple at the celebration. Prior to the slava, a priest surrounded by family members blesses the house. This is done in front of the saint's icon and the lit candle whereby the priest recites a prayer. Every room in the house is then sprinkled with holy water along with the members of the family who are each named and wished good health. The top of the kolač is adorned with
2842-409: The saint's day . In 2014, it was inscribed on UNESCO Intangible Cultural Heritage Lists of Serbia . Slavski kolač , also known simply as kolač , is a ritual bread often prepared during the celebration of the Slava. Serbian historians consider that records of Slava amongst Serbs can be traced back at least to 1018. However, the true origin of the Slava is unknown. According to one hypothesis,
2900-462: The second half of the 20th century it became common to see traditional patriarchal families separated by great distances, so by necessity Slava came to occasionally be celebrated at more than one place by members of the same family . While the Slava kept something of a grassroots underground popularity during the Communist period, the post-Communist revival of Serbian Orthodox traditions has brought it
2958-649: 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 ,
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#17327652639083016-415: 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
3074-1002: 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
3132-461: 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
3190-515: 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
3248-524: The whole of the plateau. They were deposited by valley glaciers coming from Orjen during the Ice Age . Krivošije is the region with the greatest rainfall in Europe. Reovačka greda is a mountain ridge located near Crkvice in central Krivošije, is the location of the region's highest peak Pazua (1769 m), which is used for trad climbing . Settlements in the region include Crkvice (inhabited location with
3306-638: Was attempting to enforce compulsory military service ; Austria-Hungary abandoned its efforts, for the time being. Volunteers from the region joined the Serb rebels in the Herzegovina Uprising (1875–77) . During World War II, population of Krivošije was equally divided between Partisans and Chetniks . After 1942 and before capitulation of Italy, region was Chetnik stronghold. Local merchant Miloš Kovač organized an armed band of 80 men in Krivošije which threatened Yugoslav Partisan access and control in
3364-444: Was named after the region after its discovery there in 1935. 42°33′N 18°39′E / 42.55°N 18.65°E / 42.55; 18.65 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
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