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Ostrovicë
Ostrovicë ( 'Ostrovica') is a massif situated on the border between Korçë and Skrapar municipalities, in southeastern Albania. Its highest peak, ''Çuka e Faqekuqit'', reaches a height of . It lies between the Çemericë river valley, a branch of Devoll river, in the east and the Çorovodë river valley, a branch of Osum river, in the west. Ostrovica boasts one of the tallest peaks of the southeastern region. Geology Composed primarily of Mesozoic limestone and 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 ep ..., the mountain mass features steep slopes with glacial and karst relief forms that can be observed on its ridge. On the foothills, numerous springs emerge, which feed several branches of Osum and Devoll. Biodiversity The vegetation consists mainly of alpine p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Albania
Albania is mostly mountainous, with the first alpine regions forming towards the end of the Jurassic, Jurassic period. During the Cenozoic, Cenozoic era, the malformation of the ''Albanides'' accelerated, causing the subterranean landscape to take its present form. The average altitude of the country is , almost three times that of Europe. Its highest summits are situated in the Accursed Mountains, Albanian Alps and the eastern mountain range, with Korab (mountain), Korab being the highest peak, at above sea level. The country's geography is unique due to its location and varied relief, with landscapes ranging from Mediterranean Basin, mediterranean in the west to a more Geographical midpoint of Europe, continental influence in the east and mountainous terrain in the interior and east. This combination of plains, hills and mountains has resulted in a diverse range of geographical features, extending horizontally and vertically. However, this complexity has made regionalization ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In Albania
Albania is mostly mountainous, with the first alpine regions forming towards the end of the Jurassic period. During the Cenozoic era, the malformation of the ''Albanides'' accelerated, causing the subterranean landscape to take its present form. The average altitude of the country is , almost three times that of Europe. Its highest summits are situated in the Albanian Alps and the eastern mountain range, with Korab being the highest peak, at above sea level. The country's geography is unique due to its location and varied relief, with landscapes ranging from mediterranean in the west to a more continental influence in the east and mountainous terrain in the interior and east. This combination of plains, hills and mountains has resulted in a diverse range of geographical features, extending horizontally and vertically. However, this complexity has made regionalization challenging, as different authors have used alternating criteria and methods. In the 1920s, Herbert Louis propo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baba (North Macedonia)
Baba (; or Baba Mountain, ), also known by the name of its highest peak, Pelister (), is a mountain in North Macedonia. The Pelister peak (2601 metres, or 8533 feet) overlooks the city of Bitola. Baba is the third highest mountain in North Macedonia. Other peaks besides Pelister are Dva Groba (2514 metres), Veternica (2420 metres), Musa (2350 metres), Ržana (2334 meters), Široka (2218 metres), Kozji Kamen (2199 metres), Griva (2198 metres) and Golema Čuka (2188 metres) in North Macedonia, and Belavoda (2.179 meters), Kirko. The Baba massif splits up the rivers in the region, so that they either flow towards the Adriatic Sea. Pelister National Park's flora include the five-needle pine molika (''Pinus peuce'') - a unique species of tertiary age being present on only a few mountains in the Balkan Peninsula. Fauna in the area include: bears, roe deer, wolves, chamois, deer, wild boars, rabbits, several species of eagles, partridges, redbilled jackdaws, and the endemic Macedonian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Prespa
The Lake Prespa is located on the tripoint of North Macedonia, Albania and Greece. It is a system of two lakes separated by an isthmus: the Great Prespa Lake, divided between the three countries, and the Little Prespa Lake, mostly within Greece. They are the highest tectonic lakes in the Balkans, at an elevation of . The area contains three national parks: Galičica National Park in North Macedonia, Prespa National Park in Albania, and Prespa National Park in Greece. The largest town in the region is Resen in North Macedonia. In 2014, Ohrid-Prespa Transboundary Biosphere Reserve between Albania and North Macedonia was added to UNESCO's World Network of Biosphere Reserves. Geography The Great Prespa Lake (, ''Prespansko Ezero'', , , ''Megáli Préspa'') has the total surface of . The largest part of it, belongs to North Macedonia; to Albania; and to Greece. To the south, the Little Prespa Lake (Greek: Μικρή Πρέσπα, ''Mikri Prespa''; Albanian: ''Prespa e Vog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Mountain Region (Albania)
The Southern Mountain Region () is a physiogeographical region in southern Albania. It is defined by high mountains and few valleys and plains between them. It is also one of the four geographical areas of Albania, the others being the Northern Mountain Range (Albania), Northern Mountain Range (the Albanian part of the Accursed Mountains), the Western Lowlands (), and the Central Mountain Range (Albania), Central Mountain Range (). The range notably includes two mountain chains: the Mount Trebeshinë, Trebeshinë-Mount Dhëmbel, Dhëmbel-Mount Nemërçkë, Nemërçkë and Mount Shëndelli, Shëndelli-Mount Lunxhëri, Lunxhëri-Mount Bureto, Bureto. It also includes the Tomorr in its northern part, and the Ceraunian Mountains with its summit Mount Çika, Çika in the west, two mountains which are close to the Llogara National Park. The mountainous region of Kurvelesh (region), Kurvelesh is part of the range, while its coastal region is part of the Albanian riviera. The only notab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Korçë
Korçë (; sq-definite, Korça) is the List of cities and towns in Albania, eighth most populous city of Albania and the seat of Korçë County and Korçë Municipality. The total population of the city is 51,152 and 75,994 of Korçë municipality (2011 census), in a total area of . It stands on a plateau some Above mean sea level, above sea level, surrounded by the Morava Mountains. The area of the Old Bazaar of Korçë, Old Bazaar, including Mirahori Mosque, Korçë, Mirahori Mosque, is considered as the urban core of the city. Founded by the local Ottoman Empire, Ottoman Albanians, Albanian nobleman Iljaz Bej Mirahori, Ilias Bey Mirahori, the urban area of Korçë dates back to the late 15th century and the beginning of the 16th century, however its actual physiognomy was realized in the 19th century, during a period that corresponds with the rapid growth and development of the city. The Old Bazaar has played a dominant role in Albania's market history. Korçë is the larges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skrapar
Skrapar ( sq-definite, Skrapari) is a Municipalities of Albania, municipality in Berat County, Southern Albania, southern Albania. It was created in 2015 by the merger of the former municipalities Bogovë, Çepan, Çorovodë, Gjerbës, Leshnjë, Potom, Qendër Skrapar, Vendreshë and Zhepë. The seat of the municipality is the town Çorovodë. The total population is 12,403 (2011 census), in a total area of 832.04 km2. It covers part of the area of the former Skrapar District, without the town Poliçan. It is also roughly contiguous with the Albanian "ethnographic region" of Skrapar which is known for its folklore, its Rakı, raki production, its high rate of those belonging to the Bektashi order and its scenic mountains. History The discovery of the cave settlements, graves, mosaics, coins and the ruins of bridges, churches, castles, have extended knowledge and evidence of an ancient human life in the area. Ancient objects are work tools belonging to the Neolithic period. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era is the Era (geology), era of Earth's Geologic time scale, geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles such as the dinosaurs, and of Gymnosperm, gymnosperms such as cycads, ginkgoaceae and Araucariaceae, araucarian conifers; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Massif
A massif () is a principal mountain mass, such as a compact portion of a mountain range, containing one or more summits (e.g. France's Massif Central). In mountaineering literature, ''massif'' is frequently used to denote the main mass of an individual mountain. As a purely scientific term in geology, however, a "massif" is separately and more specifically defined as a section of a planet's crust (geology), crust that is demarcated by geologic fault, faults or lithospheric flexure, flexures. In the plate tectonics, movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. A massif is a smaller structural unit than a tectonic plate and is considered the fourth-largest driving force in geomorphology. The word "massif" originates from French (in which the word also means "massive"), where it is used to refer to a large mountain mass or compact group of connected mountains forming an independent portion of a range. The Cydonia (regi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albania
Albania ( ; or ), officially the Republic of Albania (), is a country in Southeast Europe. It is located in the Balkans, on the Adriatic Sea, Adriatic and Ionian Seas within the Mediterranean Sea, and shares land borders with Montenegro to the northwest, Kosovo to the northeast, North Macedonia to the east and Greece to the south. With an area of , it has a varied range of climatic, geological, hydrological and morphological conditions. Albania's landscapes range from rugged snow-capped mountains in the Accursed Mountains, Albanian Alps and the Korab, Central Mountain Range, Albania#Skanderbeg Mountains, Skanderbeg, Pindus and Ceraunian Mountains, to fertile lowland plains extending from the Albanian Adriatic Sea Coast, Adriatic and Albanian Ionian Sea Coast, Ionian seacoasts. Tirana is the capital and largest city in the country, followed by Durrës, Vlorë, and Shkodër. Albania was inhabited by several List of Illyrian peoples and tribes, Illyrian tribes, among them the A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
