Acarnanian Mountains
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Acarnanian Mountains
The Acarnanian Mountains ( el, Ακαρνανικά όρη, ''Akarnanika ori'') is a mountain range in the northwestern part of the Aetolia-Acarnania regional unit in western Greece. It stretches from the village Monastiraki, near Vonitsa, in the north to Astakos in the south, with a total length of nearly 40 km. The Ionian Sea lies to the west. Peaks The mountains are composed of limestone and are generally barren with the exception of the northern faces. The highest peak is Psili Koryfi ( el, Ψηλή Κορυφή, meaning "high peak") at 1589 meters.Oreivatein.com
Directly to the southeast of Psili Koryfi is Boumistos mountain which stands at 1573 meters. Boumistos received its name because of the many lightning strikes that land near the summit. To the west of Boumistos and Psili Korfi is Misovouni whic ...
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Regional Units Of Greece
The 74 regional units of Greece ( el, περιφερειακές ενότητες, ; sing. , ) are the country's Seventy-four second-level administrative units. They are divisions of the country's 13 regions, and are further divided into municipalities. They were introduced as part of the Kallikratis administrative reform on 1 January 2011 and are comparable in area and, in the mainland, coterminous with the 'pre-Kallikratis' prefectures of Greece During the first administrative division of independent Greece in 1833–1836 and again from 1845 until their abolition with the Kallikratis reform in 2010, the prefectures ( el, νομοί, sing. νομός, translit=nomoi, sing. nomós) were .... List References {{Articles on second-level administrative divisions of European countries Regional units Greece transport-related lists Subdivisions of Greece ...
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Landforms Of Aetolia-Acarnania
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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Korpi
Korppi is a Finnish-language surname. Notable people with the surname include: * Henrik Korpi, Swedish songwriter and record producer *Janne Korpi, Finnish snowboarder and harness racing driver *Kiira Korpi, Finnish figure skater *Norman Korpi, American painter, fashion designer, filmmaker and reality television star *Pekka Korpi, Finnish harness racing trainer and driver *Rauno Korpi Rauno "Rane" Korpi (born June 25, 1951 in Tampere, Finland) is a Finnish ice hockey coach. He coached Tappara to three consecutive Finnish Championships in SM-liiga during the years 1986-1988. He has also won one additional Finnish Championship Gol ..., Finnish ice hockey coach * Sture Korpi, Swedish politician * Walter Korpi, Swedish sociologist {{surname Finnish-language surnames ...
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Spring Water
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ...
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Medeon
Medeon ( el, Μεδεών) is a former municipality in Aetolia-Acarnania, West Greece, Greece. Since the 2011 local government reform it is part of the municipality Aktio-Vonitsa, of which it is a municipal unit. The municipal unit has an area of 213.217 km2. Population 3,858 (2011). The seat of the municipality was in Katouna. Medeon was named after the nearby ancient city of Medeon. Subdivisions The municipal unit Medeon is subdivided into the following communities (constituent villages in brackets): * Katouna (Katouna, Agios Nikolaos, Loutraki) * Aetos *Achyra Achyra ( el, Αχυρά) is a village in the Medeon municipal unit, Aetolia-Acarnania, Greece. Its population at the 2011 census was 117. It was originally situated on a mountain slope, 7 km west of Katouna, 13 km east of Palairos and 37 km north ... *Kompoti * Konopina * Tryfos References Populated places in Aetolia-Acarnania {{WGreece-geo-stub ...
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Kandila, Aetolia-Acarnania
Kandila ( el, Κανδήλα) is a town in the western part of Aetolia-Acarnania, Greece. Kandila was the seat of the former municipality Alyzia. Its population was 1,048 in 2011. It is situated 3 km from the Ionian Sea, in a plain at the western foot of the Acarnanian Mountains. It is 4 km north of Mytikas, 40 km west of Agrinio and 33 km southeast of Preveza. The ruins of ancient Alyzia are located here. Population References V. Liagko, Ένας μικρός τόπος, μια μεγάλη ιστορία = ''One Small Place, One Huge History''. External links Kandila on GTP Travel Pages See also *List of settlements in Aetolia-Acarnania This is a list of settlements in Aetolia-Acarnania, Greece. * Achladokastro * Achyra * Aetopetra * Aetos * Afrato * Afroxylia * Agalianos * Agia Paraskevi * Agia Sofia * Agia Varvara * Agios Andreas * Agios Dimitrios * Agios Georgios * ... {{Alyzia Populated places in Aetolia-Acarnania ...
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Palairos
Palairos ( el, Πάλαιρος) is an ancient city and a modern town in Aetolia-Acarnania, Greece. The modern village is also known locally by the name of Zaverda (Ζαβέρδα), in official use till 1928. Since the 2011 local government reform Palairos is part of the municipality Aktio-Vonitsa, of which it is a municipal unit. The municipal unit has an area of 205.843 km2. The municipal unit was formed as the independent municipality ''Kekropia'' in 1994 from the former communities Palairos and Pogonia, and was expanded with the former communities Vatos, Plagia and Peratia as a part of the 1997 Kapodistrias reform. The name of the municipal unit was changed to Palairos in 2004. History Palairos ( grc, Παλαιρός, la, Palaerus) was a city of ancient Greece, situated in the southern part of the region of Epirus. The city, ruinous for centuries, is thought to have existed during the Mycenean period, since parts of the city walls appear to date back to 2000 B.C. The co ...
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Abies Cephalonica
''Abies cephalonica'' or Greek fir is a fir native to the mountains of Greece, primarily in the Peloponnesos and the island of Kefallonia, intergrading with the closely related Bulgarian fir further north in the Pindus mountains of northern Greece. It is a medium-size evergreen coniferous tree growing to – rarely – tall and with a trunk diameter of up to . It occurs at altitudes of , on mountains with a rainfall of over . The leaves are needle-like, flattened, long and wide by thick, glossy dark green above, and with two blue-white bands of stomata below. The tip of the leaf is pointed, usually fairly sharply but sometimes with a blunt tip, particularly on slow-growing shoots on older trees. The cones are long and broad, with about 150–200 scales, each scale with an exserted bract and two winged seeds; they disintegrate when mature to release the seeds. It is also closely related to Nordmann fir to the east in northern Turkey. Uses Greek fir was important in the p ...
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Aetolia-Acarnania
Aetolia-Acarnania ( el, Αιτωλοακαρνανία, ''Aitoloakarnanía'', ) is one of the regional units of Greece. It is part of the geographic region of Central Greece and the administrative region of West Greece. A combination of the historical regions of Aetolia and Acarnania, it is the country's largest regional unit. Its capital is Missolonghi for historical reasons, with its biggest city and economic centre at Agrinio. The area is now connected with the Peloponnese peninsula via the Rio-Antirio Bridge. The surrounding regional units take in Arta in Epirus, a narrow length bordering Karditsa of Thessaly, Evrytania to the northeast, and Phocis to the east. Geography Mountains dominate the north, northeast, west and southeast, especially the Acarnanian Mountains. The longest and main river is the Acheloos, which ends as a delta in wetlands to the southwest on a rich fertile valley. The second longest is Evinos; others include the Ermitsa, the Inachos, and the Morn ...
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Ambracian Gulf
The Ambracian Gulf, also known as the Gulf of Arta or the Gulf of Actium, and in some official documents as the Amvrakikos Gulf ( el, Αμβρακικός κόλπος, translit=Amvrakikos kolpos), is a gulf of the Ionian Sea in northwestern Greece. About long and wide, it is one of the largest enclosed gulfs in Greece, and due to its ecological importance is one of the National Parks of Greece. The towns of Preveza, Amphilochia (formerly Karvassaras), and Vonitsa lie on its shores. Name The gulf takes its name from the ancient city of Ambracia located near its shores. Its alternative name comes from the medieval (and modern) city of Arta, located in the same place as ancient Ambracia. Geography The entrance to the gulf is through a -wide channel between Aktio (ancient Actium) on the south and Preveza on the north; a recent road tunnel connects the two. The gulf is quite shallow, and its northern shore is broken by numerous marshes, large parts of which form an estuary syst ...
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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 ...
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