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Sinjajevina
Sinjajevina ( cnr, Сињајевина, ), also known as Sinjavina () is a mountain in northern Montenegro. The highest point of Sinjajevina is ''Jablanov vrh'', which is high. Features Sinjajevina Mountain stretches from SE to NW, between town of Kolašin and village of Njegovuđa, near Žabljak. The massif is 40 km long and 15 km wide. Geologically, its composition is cretaceous limestone. The high mountain plain averages in height, with only a few peaks of higher elevation. Peaks The highest peaks of Mt Sinjajevina are: * Jablanov vrh * Torna * Gradiste * Sto * Savina greda * Veliki Pecarac * Veliki Starac * Babin vrh * Sto * Korman * Mali Starac Lakes Mt Sinjajevina is home to two lakes, both in a process of natural extinction: * Zabojsko Lake * Zminičko Lake See also *Durmitor *Kolašin Kolašin (Montenegrin Cyrillic: Колашин, ) is a town in northern Montenegro. It has a population of 2,989 (2003 census). Kolašin is the centre of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kolašin
Kolašin (Montenegrin Cyrillic: Колашин, ) is a town in northern Montenegro. It has a population of 2,989 (2003 census). Kolašin is the centre of Kolašin Municipality (population 9,949) and an unofficial centre of Morača region, named after Morača River. History Ottoman period Kolašin, fortress-settlement, was raised by the Turks in the middle of the 17th century in the namesake village in Nikšić district ( nahiye). The village of Kolašin was first mentioned in the Sultan's Decree in 1565, by which the deceased Grand Duke Miloš was replaced by his son Todor. The Turkish town was named after the former village of Kolašin. In 1651, Patriarch Gavrilo assigned Eparch of Zahumsko, the Eparchy of Nikšić, Plana, the Kolašinovićevs and the Morača to Basil of Ostrog. This document also, like the one from 1667, shows that the Orthodox Christian population of this region called the Kolašinovići, was organized in a recognized and respected tribal community of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montenegro
) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = Montenegrin , languages2_type = Languages in official use , languages2 = , ethnic_groups = , ethnic_groups_year = 2011 , religion = , religion_year = 2011 , demonym = Montenegrin , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Milo Đukanović , leader_title2 = Prime Minister , leader_name2 = Dritan Abazović (acting) , leader_title3 = Speaker , leader_name3 = Danijela Đurović , legislature = Skupština , sovereignty_type = Establishment history , established_event1 = Principality of Duklja , established_date1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southeast (direction)
The four cardinal directions, or cardinal points, are the four main compass directions: north, east, south, and west, commonly denoted by their initials N, E, S, and W respectively. Relative to north, the directions east, south, and west are at 90 degree intervals in the clockwise direction. The ordinal directions (also called the intercardinal directions) are northeast (NE), southeast (SE), southwest (SW), and northwest (NW). The intermediate direction of every set of intercardinal and cardinal direction is called a secondary intercardinal direction. These eight shortest points in the compass rose shown to the right are: # West-northwest (WNW) # North-northwest (NNW) # North-northeast (NNE) # East-northeast (ENE) # East-southeast (ESE) # South-southeast (SSE) # South-southwest (SSW) # West-southwest (WSW) Points between the cardinal directions form the points of the compass. Arbitrary horizontal directions may be indicated by their azimuth angle value. Determination Ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northwest (direction)
The four cardinal directions, or cardinal points, are the four main compass directions: north, east, south, and west, commonly denoted by their initials N, E, S, and W respectively. Relative to north, the directions east, south, and west are at 90 degree intervals in the clockwise direction. The ordinal directions (also called the intercardinal directions) are northeast (NE), southeast (SE), southwest (SW), and northwest (NW). The intermediate direction of every set of intercardinal and cardinal direction is called a secondary intercardinal direction. These eight shortest points in the compass rose shown to the right are: # West-northwest (WNW) # North-northwest (NNW) # North-northeast (NNE) # East-northeast (ENE) # East-southeast (ESE) # South-southeast (SSE) # South-southwest (SSW) # West-southwest (WSW) Points between the cardinal directions form the points of the compass. Arbitrary horizontal directions may be indicated by their azimuth angle value. Determination Ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Njegovuđa
Njegovuđa ( sr-cyr, Његовуђа, ) is a village in the municipality of Žabljak, Montenegro ) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = M .... Demographics According to the 2003 census, the town had a population of 227 people. According to the 2011 census, its population was 216. Ethnicity in 2011 References Serb communities in Montenegro Populated places in Žabljak Municipality {{Montenegro-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Žabljak
Žabljak ( Serbian / Montenegrin: Жабљак, ) is a small town in northern Montenegro. It has a population of 1,723. Žabljak is the seat of Žabljak Municipality (2011 population: 3,569). The town is in the centre of the Durmitor mountain region and with an altitude of 1,456 metres, it is the highest situated Balkan town. History The first Slav name of the place was ''Varezina voda'' (Варезина вода) possibly because of the strong source of drinkable water nearby, making a settlement possible. Later, the town was renamed ''Hanovi'' because it was where caravans rested. The modern name dates from 1870, when in a single day the building of a school, church and captain's home began. However, almost all the original buildings were destroyed during the Balkan Wars. All that has remained is the old church of Sv. Preobraženje (Holy Transfiguration), built in 1862 as a monument to a Montenegrin victory in the battle against the Ottoman Empire. After Žabljak was establi ... [...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] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durmitor
Durmitor ( Montenegrin: Дурмитор, or ) is a massif located in northwestern Montenegro. It is part of the Dinaric Alps. Its highest peak, Bobotov Kuk, reaches a height of . The massif is limited by the Tara River Canyon on the north, the Piva River Canyon on the west, and by the Komarnica River Canyon on the south. To the east, the Durmitor opens to a high plateau, called ''Jezerska površ'' (Plateau of Lakes). The Sinjavina mountain is located to the east of the ''Jezerska površ'' plateau. The Durmitor is for the most part located in the Žabljak municipality. The massif gives its name to the national park that comprises it. Durmitor National Park was founded in 1952, and designated as a World Heritage Site in 1980. Peaks The massif has 48 peaks above . Highest peaks are: * Bobotov kuk * Bezimeni vrh (Nameless Peak) * Šljeme * Istočni vrh Šljemena (East Peak of Sljeme) * Soa / Đevojka * Milošev tok * Bandijerna * Rbatina * Lučin vrh * Prutaš * Minin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Montenegro
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
