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Shkëlzen
Shkëlzen ( 'Shkëlzeni') is a mountain situated in the Albanian Alps, bounded by the Tropojë river valley to the northeast, the Gashi river valley to the southwest, and the Tropojë basin to the southeast. Its highest of the two peaks, ''Maja e Shkëlzenit'', reaches a height of . Geology Composed primarily of Mesozoic limestone and dolomite, the mountain has an anticlinal structure, with a band of flysch emerging in the north and south. It forms a sharp ridge between the northeastern peak (Shkëlzen) and the southwestern peak of ''Radesha'' , marked by steep slopes that descend sharply into the valleys. Two glacial troughs divide the mountain's summit, and both peaks show distinctive pyramid-like shapes with sharp edges. Vegetation is scarce, with shrubs and pines found on its slopes. See also * 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 malfo ... [...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] |
Accursed Mountains
The Accursed Mountains (; sh-Latn-Cyrl, Prokletije, Проклетије, separator=" / ", ; both translated as "Cursed Mountains"), also known as the Albanian Alps (; sh-Latn-Cyrl, Albanski Alpi, Албански Алпи, separator=" / ", link=no), is a mountain range in coastal Southeast Europe adjacent to the Adriatic Sea. It is the southernmost subrange of the Dinaric Alps range (Dinarides), extending from northern Albania to western Kosovo and northeastern Montenegro. Maja Jezercë, standing at , is the highest point of the Accursed Mountains and of all Dinaric Alps, and the List of mountains in Albania, fifth highest peak in Albania. The range includes the mountain Zla Kolata, which, at , is the tallest mountain in Montenegro. The range also includes the mountain Gjeravica, which, at , is the second tallest mountain in Kosovo. One of the southernmost glaciers, glacial masses in Europe was discovered in the Albanian part of the range in 2009. Name The origin of the nam ... [...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] |
Gashi (river)
The Gashi () is a river located in Tropojë, northern Albania. It was a nature reserve, spanning an area of . The nature reserve forms a part of the European Green Belt and has been declared a UNESCO World Heritage Site within the Primeval Beech Forests of the Carpathians and Other Regions of Europe. In 2022, the protected area was amalgamated to form the Alps of Albania National Park. The river is located in the eastern part of the Albanian Alps at above sea level. It originates at the Dobërdol Pass and flows along numerous peaks including the Trekufiri in the north, Maja Bogiçaj in the northeast and Maja e Shpatit in the northwest. The various streams, flowing first to the north and northwest, merge with the Dobërdol pasture in the northwest, then leaving the basin westward. A few kilometres further, the river changes its course southwards and stops the direction in the sequence. It passes the Maja e Shkëlzenit on its western side. Farther south, the river passe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Mountain Region (Albania)
The Northern Mountain Region () is a geographical region in northern Albania. It is one of the four mountain regions of Albania, the others being Central Mountain Range (Albania), Central Mountain Range, Southern Mountain Range (Albania), Southern Mountain Range, and Western Lowlands. The northern range encompasses the Albanian Alps extending from the Lake Shkodër shared with Montenegro in the northwest through the Valbonë Valley National Park, Valbonë Valley to the Drin Valley in the east. The area falls within the Dinaric Mountains mixed forests and Balkan mixed forests terrestrial ecoregions of the Palearctic realm, Palearctic Temperate broadleaf and mixed forests. Inside the Northern Mountain Range, there are two national parks and a nature reserve, namely Theth National Park, Valbonë Valley National Park and Gashi River, Gashi River Nature Reserve. The International Union for Conservation of Nature (IUCN) has listed the nature reserve as Category I, while the national p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropojë
Tropojë (; sq-definite, Tropoja) is a municipality in Kukës County, northeastern Albania, within the historical ethnographic region of the Gjakova Highlands. The municipality consists of the administrative units of Bajram Curri, Bujan, Bytyç, Fierzë, Lekbibaj, Llugaj, Margegaj and Tropojë, that became municipal units. The seat of the municipality is the town Bajram Curri. As of the Institute of Statistics 2023 census, there were 2,560 people residing in the municipal unit Tropojë and 14,189 in the municipality. Etymology Tropojë's old name was ''Trebopolje'' and is recorded in Serbian medieval charters and Ottoman registers. The word itself comes from the old Slavic ''trebiti'', ‘to clean’, and ''polje'', ‘field’, i.e. ‘clean field’. History The region was inhabited by Illyrian tribes. Archaeological evidence found in the area, such as castles or tumuli, shows that the area has been populated since the ancient time. The region lies in the geo ... [...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] |
Mountain
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 above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ... [...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] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary rock, sedimentary carbonate rock that contains a high percentage of the mineral Dolomite (mineral), dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). One of the first geologists to distinguish dolomite from limestone was Déodat Gratet de Dolomieu, a French mineralogist and geologist after whom it is named. He recognized and described the distinct characteristics of dolomite in the late 18th century, differentiating it from limestone. Most dolomite was formed as a magnesium replacement of limestone or of Lime (mineral), lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the v ... [...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] |
Anticline
In structural geology, an anticline is a type of Fold (geology), fold that is an arch-like shape and has its oldest Bed (geology), beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex curve, convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that Strike and dip, dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various Stratum, rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geological map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold cau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
