|
Mali I Hekurave
Mali i Hekurave () is a massif in the Albanian Alps, within the limits of Tropojë municipality. Its main peak, ''Maja e Hekurave'', rises to a height of . Geology Mali i Hekurave is bounded by the central valley of Valbona in the northeast, the basin of Tropojë in the southeast, and the basin of Nikaj-Mërtur in the southwest. The mountain is composed entirely of Triassic limestone and dolomite. Its sharp pyramidal shape is due to the numerous glacial cirques that stretch on almost all sides and descend step by step into the valley of Motinë from the northeast, into the trough of the Liqeni stream from the southeast, and the Selbicë stream from the west. Other peaks in the massif include Alshina , Maja e Zezë and Maja e Dhive . The mountain mass is barren above , featuring only alpine pastures, while beech and cypress grow below this height. See also * List of mountains in Albania Albania is mostly mountainous, with the first alpine regions forming towards the end ... [...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] |
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] |
Triassic
The Triassic ( ; sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era and the seventh period of the Phanerozoic Eon. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the ... [...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] |
Valbona Valley
The Valbona Valley () is in the Albanian Alps in northern Albania. It is part of Alps of Albania National Park, one of the most impressive and notable topographic features of Albania. Being the southernmost continuation of the Dinaric Alps, it forms a section of the Alpine-Himalayan orogenic belt, which extend from the Atlantic Ocean to the Himalaya Mountains. The mountains are characterized by limestone and dolomite rocks and shows major karst features. Maja Jezercë sprawls to the west of the valley and is the highest mountain of the Dinaric Alps, with an altitude of . The Valbona River originate from several karst springs along the south of Maja Jezercë and the east of Valbona Pass. It is the largest river within the Albanian Alps and drains the entire eastern portion of the range. Over the past few million years, glaciers have at times covered most of the park. During the Würm period, the glacier of Valbona reached a total length of 9.5 kilometres. Nowadays, there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nikaj-Mërtur Region
The Nikaj-Mërtur region () is a regional nature park in northern Albania, strategically inside the southeastern Albanian Alps in Tropojë. It lies within the area of the historical Nikaj and Mërturi tribes. The park is an area of alpine landscapes, deep valleys, vertical cliffs, dense coniferous and deciduous forests, small lakes and rivers. The International Union for Conservation of Nature (IUCN) has listed the park as Category IV. Like most of the Albanian Alps, it is listed as an important Plant Area, because it supports significant plant species. The park lies within the Albanian Alps and borders Theth National Park in the northeast and Valbonë Valley National Park in the north and northeast. It is proposed to expand the park's boundaries and merge it with Valbonë Valley and Theth to establish the Balkan Peace Park. The Albanian Alps are a continuation of the Dinaric Alps, which extend from northeastern Italy down to northern Albania. Located between the steep and r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ) is an amphitheatre-like valley formed by Glacier#Erosion, glacial erosion. Alternative names for this landform are corrie (from , meaning a pot or cauldron) and ; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepening, overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (lake), tarn (small lake) behind a d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trough (geology)
In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a ''trench'', a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates. There are various oceanic troughs on the ocean floors. Examples of oceanic troughs * Benue Trough * Cayman Trough * Hesperides Trough * Kings Trough * Mariana Trough * Nankai Trough * Northumberland Trough * Okinawa Trough in the East China Sea * Rockall Trough and others along the rift of the mid-oceanic ridge * Salton Trough * South Shetland Trough * Suakin TroughDinwiddie, Robert et al. (2008) ''Ocean: The World's Last Wilderness Revealed'', London, Dorling Kindersley, page 452. in the Red Sea * Timor Trough See also * Oceanic basin * Thalweg * Walker Lane The Walker Lane is a geologic trough roughly aligned with the California/Nevada border southward to where Death Valley intersects the Garlock Fault, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beech
Beech (genus ''Fagus'') is a genus of deciduous trees in the family Fagaceae, native to subtropical (accessory forest element) and temperate (as dominant element of Mesophyte, mesophytic forests) Eurasia and North America. There are 14 accepted species in two distinct subgenera, ''Englerianae'' and ''Fagus''. The subgenus ''Englerianae'' is found only in East Asia, distinctive for its low branches, often made up of several major trunks with yellowish bark. The better known species of subgenus ''Fagus'' are native to Europe, western and eastern Asia and eastern North America. They are high-branching trees with tall, stout trunks and smooth silver-grey bark. The European beech ''Fagus sylvatica'' is the most commonly cultivated species, yielding a utility timber used for furniture construction, flooring and engineering purposes, in plywood, and household items. The timber can be used to build homes. Beechwood makes excellent firewood. Slats of washed beech wood are spread around ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
