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Dragonja
The Dragonja (; it, Dragogna) is a long river in the northern part of the Istrian peninsula. It is a meandering river with a very branched basin and a small quantity of water. It has a pluvial regime and often dries up in summer. It features very diverse living environments and is home to a number of animal and plant species. The Dragonja has been a matter of a territorial dispute between Croatia and Slovenia, with its lowest portion ''de facto'' the border of the two countries. Course The river is the third-longest river in Istria, after the Raša and Mirna rivers. It is the largest river of the Slovenian coast that flows into the Adriatic Sea. It is also the only Slovenian river that does not flow through settlements and that flows in its entirety over the flysch terrain. The Dragonja originates from several sources in the Šavrin Hills and flows west to the Gulf of Piran, part of the northern Adriatic Sea. It is joined by two larger tributaries from the right side (Rok ...
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Croatia–Slovenia Border Disputes
Following the breakup of Yugoslavia in 1991, Slovenia and Croatia became independent countries. As the border between the countries had not been determined in detail prior to independence, several parts of the border were disputed, both on land and at the sea, namely in the Gulf of Piran. According to the Croatian Bureau of Statistics, the two countries share about of border. According to the Statistical Office of the Republic of Slovenia, the border spans . The border mostly runs along a southwest-northeast axis. The countries have attempted to resolve the dispute, most notably with the Drnovšek–Račan agreement in 2001 that was ratified by Slovenia but not by Croatia. Because of the disputed border, Slovenia blocked Croatia's EU accession talks until the agreement was reached by both countries and the EU to settle the dispute by a binding arbitration. On 29 June 2017, the Permanent Court of Arbitration issued a binding ruling on the border, ruling on the disputed parts o ...
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Adriatic Sea
The Adriatic Sea () is a body of water separating the Italian Peninsula from the Balkan Peninsula. The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po Valley. The countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Italy, Montenegro, and Slovenia. The Adriatic contains more than 1,300 islands, mostly located along the Croatian part of its eastern coast. It is divided into three basins, the northern being the shallowest and the southern being the deepest, with a maximum depth of . The Otranto Sill, an underwater ridge, is located at the border between the Adriatic and Ionian Seas. The prevailing currents flow counterclockwise from the Strait of Otranto, along the eastern coast and back to the strait along the western (Italian) coast. Tidal movements in the Adriatic are slight, although larger amplitudes are known to occur occasi ...
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Gulf Of Piran
The Gulf of Piran or Piran Bay ( sl, Piranski zaliv, hr, Piranski zaljev, it, Baia di Pirano) is located in the northern part of the Adriatic Sea, and is a part of the southernmost tip of the Gulf of Trieste. Overview It was named after the town of Piran, and its shores are shared by Croatia and Slovenia. It is delimited by a line connecting Cape Savudrija ('' Savudrijski rt'') in the south to the Cape Madona (''Rt Madona'') in the north and measures around . On the eastern Slovenian coast lies the town of Piran, and the settlements Portorož and Lucija. On the southern Croatian coast are tourist camps of Crveni Vrh and Kanegra, built in the 1980s. The main river flowing into the gulf is the Dragonja, whose mouth is on the border. Along the mouth of the Dragonja lie the Sečovlje saltpans, covering an area of . The Gulf area has been a theatre of a maritime and land border dispute between Slovenia and Croatia. External links Conditions in the Gulf of Piran- graphs, in the ...
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Sečovlje Saltworks
The Sečovlje Saltworks ( sl, Sečoveljske soline; it, Saline di Sicciole) is the largest Slovenian salt evaporation pond. Along with the Strunjan Saltworks, they are the northernmost Mediterranean saltworks and one of the few where salt is still produced in a traditional way, as well as a wetland of international importance and a breeding place for waterbirds. They are part of the Piran Saltworks and are located at Parecag in Slovenian Istria, the southwest of the country, at the Adriatic Sea, along the mouth of the Dragonja River near Sečovlje. The saltworks have been active since the 13th century. Nowadays, the salt production is carried on in order to preserve natural and cultural heritage. The area of the saltworks and the Seča peninsula have been declared the Sečovlje Salina Landscape Park. The Museum of Salt-Making in Sečovlje received the Europa Nostra Prize, bestowed by the European Union to outstanding initiatives for the preservation of cultural heritage in 2 ...
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Municipality Of Piran
The Municipality of Piran (; sl, Občina Piran, it, Comune di Pirano) is a municipality in the traditional region of the Littoral in southwestern Slovenia. The seat of the municipality is the town of Piran. Piran became a municipality in 1994. Geography The Municipality of Piran borders Croatia to the south and the municipalities of Izola and Koper to the east, and it faces Italy across the Gulf of Trieste and the Adriatic Sea. The highest point, Baretovec pri Padni, is high. Settlements In addition to the municipal seat of Piran, the municipality also includes the following settlements: * Dragonja * Lucija * Nova Vas nad Dragonjo * Padna * Parecag * Portorož * Seča * Sečovlje * Strunjan * Sveti Peter Language The municipality is bilingual; both Slovene and Italian are official languages. According to the Austrian language census of 1910, in the surrounding countryside within the municipal limits, the population was mixed, both Italian and Slovene, with some vill ...
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Istria
Istria ( ; Croatian language, Croatian and Slovene language, Slovene: ; ist, Eîstria; Istro-Romanian language, Istro-Romanian, Italian language, Italian and Venetian language, Venetian: ; formerly in Latin and in Ancient Greek) is the largest peninsula within the Adriatic Sea. The peninsula is located at the head of the Adriatic between the Gulf of Trieste and the Kvarner Gulf. It is shared by three countries: Croatia, Slovenia, and Italy.Marcel Cornis-Pope, John Neubauer''History of the literary cultures of East-Central Europe: junctures and disjunctures in the 19th And 20th Centuries'' John Benjamins Publishing Co. (2006), Alan John Day, Roger East, Richard Thomas''A political and economic dictionary of Eastern Europe'' Routledge, 1sr ed. (2002), Croatia encapsulates most of the Istrian peninsula with its Istria County. Geography The geographical features of Istria include the Učka/Monte Maggiore mountain range, which is the highest portion of the Ćićarija/Cicceria ...
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Border
Borders are usually defined as geographical boundaries, imposed either by features such as oceans and terrain, or by political entities such as governments, sovereign states, federated states, and other subnational entities. Political borders can be established through warfare, colonization, or mutual agreements between the political entities that reside in those areas; the creation of these agreements is called boundary delimitation. Some borders—such as most states' internal administrative borders, or inter-state borders within the Schengen Area—are open and completely unguarded. Most external political borders are partially or fully controlled, and may be crossed legally only at designated border checkpoints; adjacent border zones may also be controlled. Buffer zones may be setup on borders between belligerent entities to lower the risk of escalation. While ''border'' refers to the boundary itself, the area around the border is called the frontier. History In the ...
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Proto-Indo-European Language
Proto-Indo-European (PIE) is the reconstructed common ancestor of the Indo-European language family. Its proposed features have been derived by linguistic reconstruction from documented Indo-European languages. No direct record of Proto-Indo-European exists. Far more work has gone into reconstructing PIE than any other proto-language, and it is the best understood of all proto-languages of its age. The majority of linguistic work during the 19th century was devoted to the reconstruction of PIE or its daughter languages, and many of the modern techniques of linguistic reconstruction (such as the comparative method) were developed as a result. PIE is hypothesized to have been spoken as a single language from 4500 BC to 2500 BC during the Late Neolithic to Early Bronze Age, though estimates vary by more than a thousand years. According to the prevailing Kurgan hypothesis, the original homeland of the Proto-Indo-Europeans may have been in the Pontic–Caspian steppe of ...
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Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to th ...
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Slavic Liquid Metathesis And Pleophony
The Slavic liquid metathesis refers to the phenomenon of metathesis of liquid consonants in the Common Slavic period in the South Slavic and West Slavic area. The closely related corresponding phenomenon of pleophony (also known as polnoglasie or full vocalization) occurred in parallel, in the East Slavic languages. The change acted on syllables in which the Proto-Slavic liquid consonants *''r'' and *''l'' occurred in a coda position. The result of the change is dependent upon the phonological environment and accents, and it varies in different Slavic languages. The change has been dated to the second half of the 8th century, before any Slavic languages were recorded in writing. Therefore, the change itself cannot be observed, but it can be inferred by comparing words in different Slavic languages. Evidence of the earlier state of affairs is also preserved in loanwords into and from Early Slavic as well as in cognates in other Indo-European languages, particularly Baltic lang ...
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Ablative Case
In grammar, the ablative case (pronounced ; sometimes abbreviated ) is a grammatical case for nouns, pronouns, and adjectives in the grammars of various languages; it is sometimes used to express motion away from something, among other uses. The word "ablative" derives from the Latin ''ablatus'', the (irregular) perfect, passive participle of ''auferre'' "to carry away". The ablative case is found in several language families, such as Indo-European (e.g., Sanskrit, Latin, Albanian, Armenian), Turkic (e.g., Turkish, Turkmen, Azerbaijani, Uzbek, Kazakh, Kyrgyz, Tatar), and Uralic (e.g., Hungarian). There is no ablative case in modern Germanic languages such as German and English. There ''was'' an ablative case in the early stages of Ancient Greek, but it quickly fell into disuse by the classical period. Indo-European languages Latin The ablative case in Latin (''cāsus ablātīvus'') appears in various grammatical constructions, including following various prepositio ...
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Natural Monument
A natural monument is a natural or natural/cultural feature of outstanding or unique value because of its inherent rarity, representative of aesthetic qualities or cultural significance. Under World Commission on Protected Areas guidelines, natural monuments are level III, described as: :"Areas are set aside to protect a specific natural monument, which can be a landform, sea mount, submarine cavern, geological feature such as a cave or even a living feature such as an ancient grove. They are generally quite small protected areas and often have high visitor value." This is a lower level of protection than level II (national parks) and level I (wilderness areas). The European Environment Agency's guidelines for selection of a natural monument are: * The area should contain one or more features of outstanding significance. Appropriate natural features include waterfalls, caves, craters, fossil beds, sand dunes and marine features, along with unique or representative fauna and flo ...
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