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Maja E Kendrevices
Griba is a massif situated in the Upper Kurvelesh region, within the boundaries of Tepelenë municipality, in southern Albania. Its highest peak, ''Maja e Këndrevicës'', reaches a height of . Other high peaks include Maja e Tartarit , Maja e Kulthit , Maja e Sorrës , Maja e Lopsit , etc. Geology The massif features a cone-shaped body with steep inclines and a flat peak and is composed primarily of Mesozoic and Paleogene limestones, with lesser amounts of flysch, giving it an asymmetrical anticlinal structure. Its ridge is marked by numerous karst pits and evidence of quaternary glaciations can be seen with the presence of cirques and moraines. Biodiversity Vegetation is sparse but there are plenty of summer pastures and a variety of medicinal plants. In Dhëmblan, the laurel forest has been designated a protected nature reserve. The area is home to a thriving population of quail. See also * List of mountains in Albania With an average elevation of above sea l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Mountain Region (Albania)
The Southern Mountain Region ( sq, Krahina Malore Jugore) 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 (the Albanian part of the Prokletije), the Western Lowlands ( sq, Ultësira Bregdetare), and the Central Mountain Range ( sq, Krahina Malore Qendrore). The range notably includes two mountain chains: the Trebeshinë- Dhëmbel- Nemërçkë and Shëndelli- Lunxhëri- Bureto. It also includes the Tomorr in its northern part, and the Ceraunian Mountains with its summit Çika in the west, two mountains which are close to the Llogara National Park. The mountainous region of Kurvelesh is part of the range, while its coastal region is part of the Albanian riviera. The only notable plain in the region is the Vurg plain. The mean precipitation for November through January is 1,000 mm. Nemërçkë ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tepelenë
Tepelenë ( sq-definite, Tepelena) is a city and a municipality in Gjirokastër County, in the south of Albania. The town is located on the left bank of the Vjosa River, about three kilometres downstream from its union with the Drino. Until the abolition of Districts of Albania, Districts in 2000, Tepelenë was the seat of the Tepelenë District. Its location is strategically important and there is a ruined citadel occupying a point 300 metres above the river. Ali Pasha of Tepelenë was born at the nearby village of Beçisht. In 1847, the British writer Edward Lear visited the town and noted the devastated buildings. History The Byzantines built a defensive tower which was successively developed during the Ottoman Empire epoch in the 15th century and by Ali Pasha in the early 19th century. In early July 1833 the inhabitants of Tepelenë Albanian revolts of 1833-1839, rose in revolt against Emin Pasha. The Young Turks, Young Turk revolutionaries met in Tepelenë in February 190 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles, like the dinosaurs; an abundance of conifers and ferns; 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 well-documented 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Massif
In geology, a massif ( or ) is a section of a planet's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. The term also refers to a group of mountains formed by such a structure. In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain. The massif is a smaller structural unit of the crust than a tectonic plate, and is considered the fourth-largest driving force in geomorphology. The word is taken from French (in which the word also means "massive"), where it is used to refer a large mountain mass or compact group of connected mountains forming an independent portion of a range. One of the most notable European examples of a massif is the Massif Central of the Auvergne region of France. The Face on Mars is an example of an extraterrestrial massif. Massifs may also form underwater, as with the Atlanti ... [...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] |
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 to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kurvelesh (region)
Kurvelesh is a region in southern Albania, within the Southern Mountain Range. In the region, which is divided into the communes of Brataj, Horë-Vranisht, Kurvelesh and Picar, fifteen villages are located. It is considered to be the heart of the larger Labëria region. The Kurvelesh region is inhabited by Lab Albanians. Traditionally neighbourhoods of local villages in the region had houses built as fortresses lacking windows on the ground floor while the blood feud used to be a common feature of the area. The people of Kurvelesh practised endogamy by intermarrying within the villages of the region. "by the vendetta, which is very strong in the whole of Kurevelesh... For example the Albanians of the Kurvelesh call themselves a group of the Liaps (Liapidhes in the Greek form) and hold their neighbour in contempt. The intermarry only within the villages of the Kurvelesh; they are all Mohammedan, some families are polygamous, and the houses in the mahaladhes are built as for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albania
Albania ( ; sq, Shqipëri or ), or , also or . officially the Republic of Albania ( sq, Republika e Shqipërisë), is a country in Southeastern Europe. It is located on the 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. Tirana is its capital and largest city, followed by Durrës, Vlorë, and Shkodër. Albania displays varied climatic, geological, hydrological, and morphological conditions, defined in an area of . It possesses significant diversity with the landscape ranging from the snow-capped mountains in the Albanian Alps as well as the Korab, Skanderbeg, Pindus and Ceraunian Mountains to the hot and sunny coasts of the Albanian Adriatic and Ionian Sea along the Mediterranean Sea. Albania has been inhabited by different civilisations over time, such as the Illyrians, Thracians, Greeks, Romans, Byzantines, Venetians, and Ot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is 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 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 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 geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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