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Maja Radohimës
Radohina is a massif situated in the Albanian Alps, within the boundaries of Shkodër municipality. Its main peak, ''Maja e Radohinës'', reaches a height of . Geology Radohina lies between the valleys of Theth in the southeast and Cemi i Vuklit in the northwest. A dome-shaped mountain mass composed entirely of Mesozoic limestone and dolomite, it features steep slopes that drop into the Bogë meadow and Theth pits, with the glacial cirques of Kllogjen and Radohina pits surrounding it in the northeast and southwest. Two other peaks rise on both sides of the mountain, Vishnje in the northeast and Maja e Thatë in the southwest. Like many other massifs in the Albanian Alps, Radohina is mostly devoid of vegetation. 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 malformation of the ''Albanides'' accelerated, causing the subterranean landscape to ... [...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] |
Shkodër
Shkodër ( , ; sq-definite, Shkodra; historically known as Scodra or Scutari) is the List of cities and towns in Albania, fifth-most-populous city of Albania and the seat of Shkodër County and Shkodër Municipality. Shkodër has been List of oldest continuously inhabited cities, continuously inhabited since the Early Bronze Age ( 2250–2000 BC), and has roughly 2,200 years of recorded history. The city sprawls across the Plain of Mbishkodra between the southern part of Lake Skadar, Lake Shkodër and the foothills of the Albanian Alps on the banks of the Buna (Adriatic Sea), Buna, Drin (river), Drin and Kir (river), Kir rivers. Due to its proximity to the Adriatic Sea, Shkodër is affected by a seasonal Mediterranean climate with Continental climate, continental influences. An urban settlement called ''Skodra'' was founded by the Illyrians, Illyrian tribe of Labeatae in the 4th century BCE. It became the capital of the Illyrian kingdom under the Ardiaei and Labeatae and was one ... [...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] |
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] |
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] |
Theth
Theth () is a small village within Shkodër County, Albania. Following the 2015 local government reform it became part of the municipality Shkodër, and has been declared a Protected Historic Center and a National Park by the Albanian Government. The community is at the centre of the Theth National Park, an area of outstanding natural beauty. A new official information center on Rruga Fushe near the Thethi bridge is set to open by the Albanian Protected Areas Agency (AKZM), and administered by the Shkoder County Protected Areas Administratio(ADZM Shkoder . History Local tradition asserts a single common ancestor for the community (one Ded Nika) and suggests that the population moved to Theth some 300 to 350 years ago in order to preserve their (Catholic) Christian traditions.Antonia Young''Ethnographic Report'' (Shala Valley Project, December 2005) Visiting Theth in the early 20th century, the traveller Edith Durham said:I think no place where human beings live has given me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maja E Thatë
Maja e Thatë () is a mountain peak of the Albanian Alps (Accursed Mountains) in Albania.Military topographic map of Albania (1:25 000): K-34-52-D-a (M. JEZERCES) It is located within Valbonë Valley National Park, roughly northwest of Valbonë and rises more than above the village. The mountain's southern and western lower slopes are relatively rich in beech and pine forests, while the higher slopes consist of very steep dolomite and limestone rock walls, suitable for mountaineering and rock climbing. Overview Maja e Thatë has an elevation of and is located northwest of Valbonë village, in the district of Tropojë, Kukës county, in Albania. It lies within the massif of Kolata, in the eastern part of the Albanian Alps (Accursed Mountains) range. Maja e Thatë rises above the village of Valbonë by more than , but being surrounded by higher peaks within its massif and because high-altitude mountain passes connect it with them, Maja e Thatë's topographic prominence is ... [...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] |
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] |
