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Široki Brijeg
, , nickname = , motto = , image_map = BiH municipality location Široki Brijeg.svg , map_alt = , map_caption = Location of Široki Brijeg in Bosnia and Herzegovina , pushpin_map = Bosnia and Herzegovina , pushpin_map_alt = , pushpin_map_caption = , coordinates = , coor_pinpoint = , coordinates_footnotes = , subdivision_type = Country , subdivision_name = , subdivision_type1 = Entity , subdivision_name1 = Federation of Bosnia and Herzegovina , subdivision_type2 = Canton , subdivision_name2 = West Herzegovina , subdivision_type3 = Geographical region , subdivision_name3 = Herzegovina , established_title = , established_date = , founder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Cities In Bosnia And Herzegovina
This is a list of city, cities and towns with over 10,000 inhabitants (or lower if the municipality has over 20,000 inhabitants) in Bosnia and Herzegovina. For the full list of populated places, see List of populated places in Bosnia and Herzegovina. Organization Apart from entities, cantons and municipalities, Bosnia and Herzegovina also has officially designated cities. Official cities have their own mayor and city council, which is a big difference to the municipalities of Bosnia and Herzegovina, which have a municipal council and mayor. Powers of city councils of official cities are between the government of municipalities and government cantons in the Federation of Bosnia and Herzegovina or a government entity in Republika Srpska. There are thirty two official cities in Bosnia and Herzegovina (as of 2022): *Banja Luka *Bijeljina''Službeni glasnik Republike Srpske br. 70/12'' *Bihać *Bosanska Krupa *Cazin *Čapljina *Derventa *Doboj *Goražde *Gračanica, Bosnia and He ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lištica (river)
Lištica (also: ''Jasenica'') is a sinking river in Bosnia and Herzegovina. It is listed as the second coldest river in Europe, and is prone to constant flooding mostly during winter. The Lištica river connects with the Borak wellspring, which rises at the base of the mountainside on the outskirts of town of Široki Brijeg. The town of Široki Brijeg was named Lištica after the Lištica River during the SFR Yugoslavia (1945–1990) but changed its name when the country dissolved back into Bosnia and Herzegovina. Course The river begins as the Ugrovača river, runs through canyon where it pick-ups a new name, the Brina, and flows into the town of Široki Brijeg. Here it connects with the Borak wellspring, thus creating the Lištica river. The Lištica sinks in the area of Mostarsko Blato seasonal lake, and appears again in Rodoč suburb of Mostar as the Jasenica. After short course it empties into the Neretva near Ortiješ, south of Mostar. Water utilization The river Lištica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Cretaceous
The Early Cretaceous ( geochronological name) or the Lower Cretaceous (chronostratigraphic name), is the earlier or lower of the two major divisions of the Cretaceous. It is usually considered to stretch from 145 Ma to 100.5 Ma. Geology Proposals for the exact age of the Barremian-Aptian boundary ranged from 126 to 117 Ma until recently (as of 2019), but based on drillholes in Svalbard the defining early Aptian Oceanic Anoxic Event 1a (OAE1a) was carbon isotope dated to 123.1±0.3 Ma, limiting the possible range for the boundary to c. 122–121 Ma. There is a possible link between this anoxic event and a series of Early Cretaceous large igneous provinces (LIP). The Ontong Java-Manihiki-Hikurangi large igneous province, emplaced in the South Pacific at c. 120 Ma, is by far the largest LIP in Earth's history. The Ontong Java Plateau today covers an area of 1,860,000 km2. In the Indian Ocean another LIP began to form at c. 120 Ma, the Kerguelen P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trebišnjica
The Trebišnjica ( sr-cyrl, Требишњица) is a river in Bosnia and Herzegovina. It used to be a sinking river, long above the ground. With a total length of above and under the ground, it is one of the longest sinking rivers in the world. In classical antiquity, the river was known as the Arion, rising and sinking through its course before resurfacing at various places from the Neretva to the coast. Sources The Trebišnjica river originate near town of Bileća. The source of the river is a system of strong karstic wellsprings distributed in two principal aquifer zones, geographically and hydrologically distinct albeit in relatively close proximity to each other. In both zones group of wellsprings raises from the underground, consisting of a number of large, abundant founts each. The first, at the head of the river and at the outskirts of Bileća town, is the Trebišnjica wellsprings group, consisting of three large wellsprings, with Dejanova Pećina as primer outflow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, 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) 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. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Donji Crnač
Donji Crnač ( sr, Доњи Црнач) is a village in Bosnia and Herzegovina. According to the 1991 census, the village is located in the municipality of Široki Brijeg , , nickname = , motto = , image_map = BiH municipality location Široki Brijeg.svg , map_alt = , map_caption = Location o .... Donji Crnač has about 740 inhabitants. Demographics According to the 2013 census, its population was 569. References Populated places in Široki Brijeg {{WestHerzegovinaCanton-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ploče
Ploče (; it, Porto Tolero) is a town and seaport in the Dubrovnik-Neretva County of Croatia. Geography Ploče is located on the Adriatic coast in Dalmatia just north of the Neretva Delta and is the natural seaside endpoint of most north-south routes through the central Dinaric Alps. This makes it the primary seaport used by Bosnia and Herzegovina and the endpoint of the Pan-European corridor 5C. Čeveljuša is a toponym in Ploče, located to the east of the town, on the intersection of the D8 highway and the D425. Climate Ploče is the location of Croatia's high temperature record, measured at on 4 and 5 August 1981. History The town was first mentioned in 1387 as ''Ploča''. During the Kingdom of Yugoslavia, a port named ''Aleksandrovo'' after Alexander I of Yugoslavia was constructed in 1939. During the socialist Yugoslavia, between 1950 and 1954, and again from 1980 to 1990, Ploče was named ''Kardeljevo'' after the Yugoslav politician Edvard Kardelj. Some locals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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