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Mornos
The Mornos ( el, Μόρνος) is a river in Phocis and Aetolia-Acarnania in Greece. It is long. Its source is in the southwestern part of the Oiti mountains, near the village Mavrolithari, Phocis. It flows towards the south, and enters the Mornos Reservoir near the village Lefkaditi. The dam was completed in 1979.ΕΥΔΑΠ It leaves the reservoir towards the west, near Perivoli. The river continues through a deep, sparsely populated valley, and turns south near Trikorfo. The lower course of the Mornos forms the boundary between Phocis and Aetolia-Acarnania. The Mornos empties into the |
Mornos
The Mornos ( el, Μόρνος) is a river in Phocis and Aetolia-Acarnania in Greece. It is long. Its source is in the southwestern part of the Oiti mountains, near the village Mavrolithari, Phocis. It flows towards the south, and enters the Mornos Reservoir near the village Lefkaditi. The dam was completed in 1979.ΕΥΔΑΠ It leaves the reservoir towards the west, near Perivoli. The river continues through a deep, sparsely populated valley, and turns south near Trikorfo. The lower course of the Mornos forms the boundary between Phocis and Aetolia-Acarnania. The Mornos empties into the |
Lidoriki
Lidoriki ( el, Λιδωρίκι, Katharevousa: Λιδωρίκιον) is a village and a former municipality in Phocis, Greece. Since the 2011 local government reform it is part of the municipality Dorida, of which it is the seat and a municipal unit. In 2011 the population was 3,388. Its area is 409.577 km² covering nearly one-fifth of Phocis. Lidoriki is built on the western slopes of Mount Giona and over the Mornos river valley. It is the centre of the mountains of Dorida. Location Lidoriki is located west of Amfissa, northwest of Itea and east-northeast of Nafpaktos. Lidoriki is located above the Mornos artificial reservoir, formed by the Mornos Dam, completed in 1974. The reservoir supplies most of the drinking water used in Athens. Lidoriki is also connected to Amfissa via the largest tunnel in Greece with 16.5 km length. This is not a street tunnel, but an aquaeduct for the water from the Mornos reservoir. History Lidoriki is attested since the late 9th century ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phocis
Phocis ( el, Φωκίδα ; grc, Φωκίς) is one of the regional units of Greece. It is part of the administrative region of Central Greece. It stretches from the western mountainsides of Parnassus on the east to the mountain range of Vardousia on the west, upon the Gulf of Corinth. It is named after the ancient region of Phocis, but the modern regional unit also includes parts of ancient Aetolia, Locris and Doris. Geography Modern Phocis has an area of 2120 km² (819 mi²), of which 560 km² (216 mi²) are forested, 36 km² (14 mi²) are plains, and the remainder is mountainous. The massive ridge of Parnassus (2,459 m/8,068 ft), which traverses the heart of the country, divides it into two distinct portions. The neighbouring prefectures are Aetolia-Acarnania to the west, Phthiotis to the north and Boeotia to the east. It also shares a tiny border with Evrytania. Much of the south and east are deforested and rocky and mountainous while th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Corinth
The Gulf of Corinth or the Corinthian Gulf ( el, Κορινθιακός Kόλπος, ''Korinthiakόs Kόlpos'', ) is a deep inlet of the Ionian Sea, separating the Peloponnese from western mainland Greece. It is bounded in the east by the Isthmus of Corinth which includes the shipping-designed Corinth Canal and in the west by the Strait of Rion which widens into the shorter Gulf of Patras (part of the Ionian Sea) and of which the narrowest point is crossed since 2004 by the Rio–Antirrio bridge. The gulf is bordered by the large administrative divisions (regional units): Aetolia-Acarnania and Phocis in the north, Boeotia in the northeast, Attica in the east, Corinthia in the southeast and south and Achaea in the southwest. The gulf is in tectonic movement comparable to movement in parts of Iceland and Turkey, growing by per year. In the Middle Ages, the gulf was known as the Gulf of Lepanto (the Italian form of Naupactus). Shipping routes between the Greek commercial port ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Oeta
Mount Oeta (; el, Οίτη, polytonic , ''Oiti'', also transcribed as ''Oite'') is a mountain in Central Greece. A southeastern offshoot of the Pindus range, it is high. Since 1966, the core area of the mountain is a national park, and much of the rest has been declared a special area under Natura 2000. Location and description Mount Oeta is located on the boundaries of the prefectures of Phocis in the south and Phthiotis in the north. Its northern side displays a steep and inaccessible terrain as it descends to the valley of the river Spercheios, forming a series of deep gorges—most famous of which is that of the Gorgopotamos river—a few of which boast large waterfalls, including the Kremastos waterfall, considered the highest in Central Greece. To the east, Oeta is defined by the gorge of the Asopos (Ασωπός) river, which forms its boundary with the neighbouring Mount Kallidromo. The southern slopes of Oeta are very gentle, bordering with the mountains Vardousia to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Efpalio
Efpalio ( el, Ευπάλιο) is a village and a former municipality in Phocis, Greece. Since the 2011 local government reform it is part of the municipality Dorida, of which it is a municipal unit. The municipal unit has an area of 204.207 km2. Population 6,086 (2011). The municipal unit Efpalio consists of sixteen communities: Kastraki, Efpalio, Managouli, Trikorfo, Malamata, Marathias, Monastiraki, Klima, Sergoula, Filothei, Kampos, Potidaneia, Teichio, Drosato, Palaioxari, and Pyrgos. Monasteries The area is also known for several important monasteries such as: * The monastery of Panagia of Varnakova. It is a Byzantine monastery, built in 1077 A.D. by Saint Arsenios. Varnakova was a centre of Orthodoxy and Greek culture The culture of Greece has evolved over thousands of years, beginning in Minoan and later in Mycenaean Greece, continuing most notably into Classical Greece, while influencing the Roman Empire and its successor the Byzantine Empire. Other cult ... ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nafpaktos
Nafpaktos ( el, Ναύπακτος) is a town and a former municipality in Aetolia-Acarnania, West Greece, situated on a bay on the north coast of the Gulf of Corinth, west of the mouth of the river Mornos. It is named for Naupaktos (, Latinized ''Naupactus''), an important Athenian naval station in the Peloponnesian war. As a strategically crucial possession controlling access to the Gulf of Corinth, Naupaktos changed hands many times during the Crusades and the Ottoman–Venetian Wars. It was under Venetian control in the 15th century, and came to be known by the Venetian form of its name, Lepanto. It fell to the Ottoman Empire in 1499 and was used as naval station by the Ottoman Navy in the 16th century, being the site of the decisive victory by the Holy League in the Battle of Lepanto in 1571. Except a brief period of Venetian control in 1687–1699, Lepanto remained under Ottoman control until Greek independence in 1829. The modern municipality was incorporated in 19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greece
Greece,, or , romanized: ', officially the Hellenic Republic, is a country in Southeast Europe. It is situated on the southern tip of the Balkans, and is located at the crossroads of Europe, Asia, and Africa. Greece shares land borders with Albania to the northwest, North Macedonia and Bulgaria to the north, and Turkey to the northeast. The Aegean Sea lies to the east of the Geography of Greece, mainland, the Ionian Sea to the west, and the Sea of Crete and the Mediterranean Sea to the south. Greece has the longest coastline on the Mediterranean Basin, featuring List of islands of Greece, thousands of islands. The country consists of nine Geographic regions of Greece, traditional geographic regions, and has a population of approximately 10.4 million. Athens is the nation's capital and List of cities and towns in Greece, largest city, followed by Thessaloniki and Patras. Greece is considered the cradle of Western culture, Western civilization, being the birthplace of Athenian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aegean Sea
The Aegean Sea ; tr, Ege Denizi (Greek language, Greek: Αιγαίο Πέλαγος: "Egéo Pélagos", Turkish language, Turkish: "Ege Denizi" or "Adalar Denizi") is an elongated embayment of the Mediterranean Sea between Europe and Asia. It is located between the Balkans and Anatolia, and covers an area of some 215,000 square kilometres. In the north, the Aegean is connected to the Marmara Sea and the Black Sea by the straits of the Dardanelles and the Bosphorus. The Aegean Islands are located within the sea and some bound it on its southern periphery, including Crete and Rhodes. The sea reaches a maximum depth of 2,639m to the west of Karpathos. The Thracian Sea and the Sea of Crete are main subdivisions of the Aegean Sea. The Aegean Islands can be divided into several island groups, including the Dodecanese, the Cyclades, the Sporades, the Saronic Islands, Saronic islands and the North Aegean islands, North Aegean Islands, as well as Crete and its surrounding islands. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Back-arc Region
The back-arc region is the area behind a volcanic arc. In island volcanic arcs, it consists of back-arc basins of oceanic crust with abyssal depths, which may be separated by remnant arcs, similar to island arcs. In continental arcs, the back-arc region is part of continental platform, either dry land ( subaerial) or forming shallow marine basins. Formation Back-arc deformation is a product of subduction at convergent plate tectonic boundaries. It initiates and evolves behind the volcanic arc on the overriding plate of a subduction zone. The stresses responsible for the deformation in this region of a subduction zone result from a combination of processes. The absolute motion of the upper plate as it moves towards or away from the trench strongly contributes to deformation in the back-arc region. Since the downgoing slab is partly anchored in the viscous layers of the mantle, and therefore its lateral movement is significantly slower than the surface plate, then any motion of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hellenic Arc
The Hellenic arc or Aegean arc is an arcuate mountain chain of the southern Aegean Sea located on the southern margin of the Aegean Sea Plate. Geologically it results from the subduction of the African Plate under it along the Hellenic subduction zone. The Hellenic Trench trends parallel to its southern side. The Aegean Sea Plate, a microplate, is often considered part of the Eurasian Plate from which it is in the process of diverging. The arc itself is mainly marine, the mountaintops appearing as islands in the Ionian Sea, Crete and its environs, or in the Dodecanese group. It encroaches on mainland terrain in the Peloponnesus, on Crete, on Rhodes, and on the southern coast of Anatolia, thus being encompassed by both Greece and Turkey. The direction of subduction is northward. Locations on the arc or near it on the north side are therefore called "outer" as they are at the outer margin of the plate. Locations further north are "inner." Generally the motion of subduction is from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
