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Lake Paralimni
Lake Paralimni ( el, Λίμνη Παραλίμνι, ''Limne Paralimni'', Latinised as ''Lacus Paralimnus''), formerly named Lake Ougria, Latinized to Uggria, is the easternmost of an east-west sequence of three ancient lakes in Central Greece that divided the mountains of Phocis from the plains of southern Boeotia on the east and the northern plains of Boeotia from the southern on the west. The westernmost and largest of the lakes, Lake Copais, was drained in the 19th century to make way for a large tract of fertile agricultural land, divided into plots. The ancient Bronze-age community on its northwestern shore, Orchomenos, is now a modern city at the edge of the farmland. The Cephissos River descending from Phocis to enter Copais has been rerouted through it to enter Lake Yliki from the north. Lake Yliki and Lake Paralimni are part of the water supply of the city of Athens, which houses one-third of the population of Greece. Hydrology of the three lakes The three lakes were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Greece (region)
Central Greece ( el, Περιφέρεια Στερεάς Ελλάδας, translit=Periféria Stereás Elládhas, , colloquially known as Ρούμελη (''Roúmeli'')) is one of the thirteen administrative regions of Greece. The region occupies the eastern half of the traditional Geographic regions of Greece, region of Central Greece, including the island of Euboea. To the south it borders the regions of Attica (region), Attica and the Peloponnese (region), Peloponnese, to the west the region of West Greece and to the north the regions of Thessaly and Epirus (region), Epirus. Its capital city is Lamia (city), Lamia. Administration The region was established in the 1987 administrative reform. With the 2010 Kallikratis plan, its powers and authority were redefined and extended. Along with Thessaly, it is supervised by the Decentralized Administration of Thessaly and Central Greece based at Larissa. The region is based at Lamia (city), Lamia and is divided into five regional units o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Greece
The geology of Greece is highly structurally complex due to its position at the junction between the European and African tectonic plates. Geologic history, stratigraphy & tectonics Some of the oldest rocks in Greece are from the Paleozoic and are usually metamorphosed with no fossils. The Rhodope Massif spans the northern mainland, divided into amphibolite schist and gneiss, with comparatively recent granite intrusions from the Oligocene and Miocene. West of the Strymonas River is the Serbo-Macedonian Massif, covering the Chalkidiki Peninsula with thick marble and gneiss, with granite intrusions. Alpine cycle Alpine cycle sedimentary rocks are situated between the European hinterland in the Rhodope Massif and Serbo-Macedonian Massif and northern fore-region of the African plate. External zones include the Paxi Zone, encompassing the islands in the Ionian Sea with dolomitized limestone from the Jurassic and Cretaceous-Miocene marl and gypsum. The Ionian Zone spans much of west ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakes Of Greece
This is a list of lakes of Greece. Natural lakes of Greece * Central Greece **Lake Amvrakia ** Lake Dystos, Euboea, presently largely drained **Lake Lysimachia ** Lake Ozeros ** Lake Saltini ** Lake Voulkaria **Lake Yliki **Lake Trichonida **Lake Vouliagmeni, Attica * Crete ** Lake Kournas ** Lake Voulismeni * Epirus **Lake Gistova **Lake Ioannina (Pamvotis) ** Lake Morfi * Macedonia **Lake Chimaditida **Lake Doirani, eastern portion **Lake Kastoria (Orestiada) **Lake Koronia **Lake Prespa, southeastern portion ** Lake Mikri Prespa **Lake Vegoritida **Lake Volvi ** Lake Zazari * Thrace ** Lake Mitrikou **Lake Vistonida * Peloponnese ** Lake Kaiafas ** Lake Lamia, Achaia ** Lake Stymfalia **Lake Vouliagmeni, Corinthia **Lake Taka Former natural lakes *Lake Copais, Boeotia *Lake Karla (Voivis), near Volos Artificial lakes * Central Greece **Evinos Lake ** Kastraki Lake ** Kremasta or Acheloos Lake **Marathon Lake **Mornos Lake ** Stratos Lake * Macedonia **Kerkini Lake ** Po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thebes, Greece
Thebes (; ell, Θήβα, ''Thíva'' ; grc, Θῆβαι, ''Thêbai'' .) is a city in Boeotia, Central Greece. It played an important role in Greek myths, as the site of the stories of Cadmus, Oedipus, Dionysus, Heracles and others. Archaeological excavations in and around Thebes have revealed a Mycenaean settlement and clay tablets written in the Linear B script, indicating the importance of the site in the Bronze Age. Thebes was the largest city of the ancient region of Boeotia and was the leader of the Boeotian confederacy. It was a major rival of ancient Athens, and sided with the Persians during the 480 BC invasion under Xerxes I. Theban forces under the command of Epaminondas ended Spartan hegemony at the Battle of Leuctra in 371 BC, with the Sacred Band of Thebes, an elite military unit of male lovers celebrated as instrumental there. Macedonia would rise in power at the Battle of Chaeronea in 338 BC, bringing decisive victory to Philip II over an alliance of Thebes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anthedon (Boeotia)
Anthedon (Ἀνθηδών) was a town in Boeotia, Ancient Greece, located on the coast of the Gulf of Euboea, about west of Chalcis, at the foot of Mount Messapius. It was member of the Amphictyonic League, and served as port for Thebes. In ancient times, it was believed to have had one of the mythical characters named Anthedon as its eponym. The ruins of the town are situated 1 1/2 mile from the village Loukisia. Ancient accounts The oldest mention of the city is found in Homer's ''Iliad'', Catalogue of Ships, where it is given the epithet "furthermost", i. e. the most geographically remote town of Boeotia to the northern Gulf of Euboea. Ancient inhabitants of Anthedon derived their origin from the sea-god Glaucus, who was believed to have been originally a native of the place. A surviving ancient coin now stored in the Archaeological Museum of Chalkis bears on one side a representation of Glaucus. The Anthedonians appear to have been a different race from the other people o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anthidona
Anthidona ( el, Ανθηδόνα) is a former municipality in the Euboea regional unit, Greece. It was named after the ancient Boeotian city Anthedon. During the 2011 local government reform, it became a municipal unit of Chalcis. The population was 7,309 inhabitants at the 2011 census, and the land area is 137.266 km². The seat of the municipality was in Drosia. Although part of the Euboea regional unit, it is not located on the island Euboea, but on the mainland, attached to the northeastern part of Boeotia Boeotia ( ), sometimes Latinized as Boiotia or Beotia ( el, Βοιωτία; modern: ; ancient: ), formerly known as Cadmeis, is one of the regional units of Greece. It is part of the region of Central Greece. Its capital is Livadeia, and its .... External linksMap References Populated places in Euboea (regional unit) {{CentralGreece-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Messapio
The Messapio ( el, Μεσσάπιο, also known as Ktypas (Κτυπάς)) is a small mountain range located in the northeastern part of Boeotia and the mainland part of Euboea regional unit in central Greece. It borders on the North Euboean Gulf and the Euripus Strait to the north and east. Its highest point is 1,021 m. It is 20 km long and 10 to 15 km wide and covers an area of 300 km². It separates the area around Chalcis from the Boeotian plains around Thebes. In the south, on the slope of the 740 m high mountain Ypato, there is the monastery of the Transfiguration of the Saviour. The nearest mountain ranges are the Ptoo to the northwest. The Motorway 1 (Athens - Larissa - Thessaloniki) passes south of the mountain. Settlements * North: Loukisia, Anthidona * East: Chalcis, Vathy and Ritsona * South: Ypato * West: Mouriki History The Messapion was mentioned by Pausanias in his ''Description of Greece''.Pausanias Pausanias ( el, Παυσανίας) m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ptoion
Ptoion (Ancient Greek ''Ptōïon'' , also ''Ptōon'' / , Modern Greek Ptoo Πτώο or ''Oros Pelagias'' Όρος Πελαγίας) is a mountain chain in northeastern Boiotia. It stretches from Akraiphia by the former Lake Copais in the west to the Gulf of Euboea in the east, reaching up to 725 m (Agia Pelagia) in the west and 781 m (Petalás) in the east. The massif is particularly famed for the oracle of Apollo, which was located in the sanctuary of Apollo Ptoios at the western end of the range and was among the most important Greek oracles up to the time of the Persian Wars. History of the Oracle of Apollo The oracle of Apollo Ptoios was located three kilometres northeast of Akraiphia. Pausanias reports that it was originally an oracle of Ptoios, a local hero who was son of Athamas and Themisto, but that he was displaced by Apollo.Pausania9.23.6 The name Ptoios was also that of the mountain which loomed over the oracle and was borne by Apollo as a local epithet. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pindus
The Pindus (also Pindos or Pindhos; el, Πίνδος, Píndos; sq, Pindet; rup, Pindu) is a mountain range located in Northern Greece and Southern Albania. It is roughly 160 km (100 miles) long, with a maximum elevation of 2,637 metres (8652') (Mount Smolikas). Because it runs along the border of Thessaly and Epirus, the Pindus range is known colloquially as the ''spine of Greece''. The mountain range stretches from near the Greek-Albanian border in southern Albania, entering the Epirus and Macedonia regions in northern Greece down to the north of the Peloponnese. Geologically it is an extension of the Dinaric Alps, which dominate the western region of the Balkan Peninsula. History of the name Historically, the name Pindos refers to the mountainous territory that separates the greater Epirus region from the regions of Macedonia and Thessaly. According to John Tzetzes (a 12th-century Byzantine writer), the Pindos range was then called Metzovon. When translated (bet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , 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 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 (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
