|
Široki Brijeg
Široki Brijeg () is a city and the regional capital of West Herzegovina Canton of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. the town itself had a population of 6,149 and the municipality of 28,929. Name Široki Brijeg means 'wide hill' in Croatian. It is sometimes called Široki Brig or Široki ('wide'). From 1952 until October 16, 1992, the town was officially called ''Lištica'' after the river that runs through it. Geography The town is from Mostar, from Međugorje, and from the Adriatic coast ( Ploče). The Široki Brijeg Municipality today numbers around 30,000 people, and the town itself about 13,000. The area of the municipality amounts to . The center of town is at above sea level, while its area is known as "lower Herzegovina". Almost the entire northern part of the municipality itself, however, belongs to "high Herzegovina", the highest point being the ''Bile stine'' ("White Rocks") near Donji Crnač. Climate Širo ... [...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 five official cities in Bosnia and Herzegovina (as of 2024): *Banja Luka *Bijeljina *Bihać *Bosanska Krupa *Brčko *Cazin *Čapljina *Derventa *Doboj *Goražde *Gračanica, Bosnia and Herzegovina, Gračanica *Gradačac *Gradi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lištica (river)
Lištica is a sinking river in Bosnia and Herzegovina. It starts under the name Ugrovača, and end its course as the Jasenica in Mostarsko Polje, before spills into the Neretva as its right-bank tributary. 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ,) 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 million years ago. It is the second period of the Cenozoic and the eleventh period of the Phanerozoic. 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). The earlier term Tertiary Period was used to define the span of time now covered by Paleogene and Neogene and, despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use. During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first human ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene Period ( ; also spelled Palaeogene or Palæogene) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period Ma (million years ago) to the beginning of the Neogene Period Ma. It is the first period of the Cenozoic Era, the tenth period of the Phanerozoic and is divided into the Paleocene, Eocene, and Oligocene epochs. The earlier term Tertiary Period was used to define the time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use. Paleogene is often abbreviated "Pg", although the United States Geological Survey uses the abbreviation "" for the Paleogene on the Survey's geologic maps. Much of the world's modern vertebrate diversity originated in a rapid surge of diversification in the early Paleogene, as survivors of the Cretaceous–Paleogene extinction event took advantage of empty ecolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), 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 largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...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 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon 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 (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trebišnjica
The Trebišnjica ( sr-cyrl, Требишњица) is a river in Bosnia and Herzegovina, and the right tributary of the Neretva. Before it was utilized for hydro exploitation via various hydrotechnical interventions and systems with different purposes, Trebišnjica used to be a sinking river, rising and sinking through its course before resurfacing at various places from the Neretva river below the Čapljina to the Adriatic Sea, Adriatic coast, and along the coast from the Neretva Delta to Sutorina. With a total length of above the ground, and roughly another below the surface, the Trebšnjica river is one of the longest sinking rivers in the world with the total of above and under the ground. In hydrological terms, it represents a sub-basin within the Neretva river basin. In classical antiquity, the river was known as the Arion, Sources The Trebišnjica river originate near town of Bileća. The source of the river is a system of strong karst spring, karstic wellsprings distr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), 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 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) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Subtropical Climate
A humid subtropical climate is a subtropical -temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia) or oceanic climates (in other continents). It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classific ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Donji Crnač
Donji Crnač () is a village in Bosnia and Herzegovina. According to the 1991 census, the village is located in the municipality of Široki Brijeg Široki Brijeg () is a city and the regional capital of West Herzegovina Canton of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. the town itself had a population of 6,149 and the municipality of 28,929. Name .... 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 (, ) 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 at an elevation of is the location of Croatia's high temperature record, measured at on 4 and 5 August 1981. Records for the Ploče weather station began in 1975. The coldest temperature was , on 13 January 1985. 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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
