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Polisi Patroli
Polisi is a mountain range in Elbasan County, central Albania. It stretches along the upper valley of the Shkumbin river. Polisi reaches an elevation of 1,974 m (6,476 ft) above sea level at its highest peak, Fage e Madhe. Another peak of the massif is Mali Plak, which reaches an elevation of 1,943 m (6,375 ft) above sea level. In classical antiquity it was a central mountain range in southern Illyria, and was known as Kandavia (Kandauia) or Candaviae Montes (Candauiae Montes). It likely gave the name to the part of Via Egnatia The Via Egnatia was a road constructed by the Romans in the 2nd century BC. It crossed Illyricum, Macedonia, and Thracia, running through territory that is now part of modern Albania, North Macedonia, Greece, and European Turkey as a continu ... that followed the convergence of its two branches from Dyrrhachium and Apollonia, which was attested as "επί Κανδαουίας" (''epí Kandaouías'') in Strabo's ''Geography''.. References Cit ... [...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] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...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] |
Magmatic Rock
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms, orogens, basins, large igneous provinces, extended crust and oceanic crust. Geological significance Igneous and metamorphic rocks make up 90–95% of the top of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elbasan County
Elbasan County () is one of the 12 counties of Albania. The population is 266,245 (2021), in an area of 3199 km². Its capital is the city Elbasan. Administrative divisions Until 2000, Elbasan County was subdivided into four districts: Elbasan, Gramsh, Librazhd, and Peqin. Since the 2015 local government reform, the county consists of the following 7 municipalities: Belsh, Cërrik, Elbasan, Gramsh, Librazhd, Peqin and Prrenjas. Before 2015, it consisted of the following 50 municipalities: * Belsh * Bradashesh * Cërrik * Elbasan * Fierzë * Funarë * Gjergjan * Gjinar * Gjoçaj * Gostimë * Gracen * Gramsh * Grekan * Hotolisht * Kajan * Karinë * Klos * Kodovjat * Kukur * Kushovë * Labinot-Fushë * Labinot-Mal * Lenie * Librazhd * Lunik * Mollas * Orenjë * Pajovë * Papër * Peqin * Përparim * Pishaj * Polis * Poroçan * Prrenjas * Qendër Librazhd * Qukës * Rrajcë * Rrasë * Shalës * Shezë * Shirgjan * Shushicë * Skënderbegas * Steb ... [...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, Veneti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shkumbin
The Shkumbin (; ; la, Genusus, also la, Genessus, label=none or la, Scampis, label=none), also commonly Shkembi, is a river in Southern Europe. It is long and its drainage basin is . Its average discharge is . Etymology It derives from Latin ''Scampinus'' which replaced Illyrian ''Genusus'', as recorded in Latin and ancient Greek literature. A Slavic intermediation has been rejected. Its inclusion in Latin loanwords into Proto-Albanian and phonetic evolution coincides with the historical existence of a large Roman town (near present-day Elbasan) which gave the river its new name. Overview The river originates in the eastern Valamara Mountains between ''Maja e Valamarës'' () and ''Gur i Topit'' () in Southeastern Albania. After descending from the Valamaras, it flows northwards through Proptisht and Qukës with many deep gorges and canyons and passes the Gora Mountains. A significant inflow comes from ''Gur i Kamjës'' () southwest of Pogradec. Over the course, it flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Illyria
In classical antiquity, Illyria (; grc, Ἰλλυρία, ''Illyría'' or , ''Illyrís''; la, Illyria, ''Illyricum'') was a region in the western part of the Balkan Peninsula inhabited by numerous tribes of people collectively known as the Illyrians. Illyrians spoke the Illyrian language, an Indo-European language, which in ancient times perhaps also had speakers in some parts of Southern Italy. The geographical term Illyris (distinct from ''Illyria'') was sometimes used to define approximately the area of northern and central Albania down to the Aoös valley (modern Vjosa), including in most periods much of the lakeland area. In Roman times the terms Illyria / Illyris / Illyricum were extended from the territory that was roughly located in the area of the south-eastern Adriatic coast (modern Albania and Montenegro) and its hinterland, to a broader region stretching between the Adriatic Sea and the Danube, and from the upper reaches of the Adriatic down to the Ardiaei. From ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Via Egnatia
The Via Egnatia was a road constructed by the Romans in the 2nd century BC. It crossed Illyricum, Macedonia, and Thracia, running through territory that is now part of modern Albania, North Macedonia, Greece, and European Turkey as a continuation of the Via Appia. Starting at Dyrrachium (now Durrës) on the Adriatic Sea, the road followed a difficult route along the river Genusus (Shkumbin), over the '' Candaviae'' ( Jablanica) mountains and thence to the highlands around Lake Ohrid. It then turned south, following several high mountain passes to reach the northern coastline of the Aegean Sea at Thessalonica. From there it ran through Thrace to the city of Byzantium (later Constantinople, now Istanbul). It covered a total distance of about 1,120 km (696 miles/746 Roman miles). Like other major Roman roads, it was about six metres (19.6 ft) wide, paved with large polygonal stone slabs or covered with a hard layer of sand. Construction and usage The main literary ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apollonia (Illyria)
Apollonia (Ancient Greek, Koine Greek: Ἀπολλωνία, ἡ; city-ethnic: Ἀπολλωνιάτης, ''Apolloniates''; la, Apollonia; sq, Apollonia or ''Apolonia'') was an Ancient Greek trade colony which developed into an independent polis, and later a Roman city, in southern Illyria. It was located on the right bank of the Aoös/Vjosë river, approximately 10 km from the eastern coast of the Adriatic Sea. Its ruins are situated in the county of Fier, close to the village of Pojan, in Albania. Apollonia was founded around 600 BC by Ancient Greek colonists from Corinth and possibly Corcyra as a trading settlement after an invitation by local Illyrians on a largely abandoned coastal site. It was perhaps the most important of the several classical towns known as '' Apollonia''. Corinthian colonial policy seems to have been relatively liberal, and was more focused towards resource extraction so as to support the growing Corinthian population, rather than exploitation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
