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Profitis Ilias (Peloponnese)
The Taygetus, Taugetus, Taygetos or Taÿgetus ( el, Ταΰγετος, Taygetos) is a mountain range on the Peloponnese peninsula in Southern Greece. The highest mountain of the range is Mount Taygetus, also known as "Profitis Ilias", or "Prophet Elias" ( Elijah). The name is one of the oldest recorded in Europe, appearing in the Odyssey. In classical mythology, it was associated to the nymph Taygete and it was named after her. During Byzantine times and up until the 19th century, the mountain was also known as Pentadaktylos (Πενταδάκτυλος; Greek for ''five-fingered'', a common name during that period). Geography Physical The Taygetus Massif is about long, extending from the center of the Peloponnese to Cape Matapan, its southernmost extremity. It contains the tallest mountain in the Peloponnese, the Profitis Ilias summit, reaching ; this is probably the classical Mount Taléton mentioned by Pausanias. The summit is an ultra-prominent peak. It is prominent above ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ultra Prominent Peak
An ultra-prominent peak, or Ultra for short, is a mountain summit with a topographic prominence of or more; it is also called a P1500. The prominence of a peak is the minimum height of climb to the summit on any route from a higher peak, or from sea level if there is no higher peak. There are approximately 1,524 such peaks on Earth. Some well-known peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence. The term "Ultra" originated with earth scientist Steve Fry, from his studies of the prominence of peaks in Washington (state), Washington in the 1980s. His original term was "ultra major mountain", referring to peaks with at least of prominence. Distribution Currently, 1,518 Ultras have been identified above sea level: 639 in Asia, 356 in North America, 209 in South America, 120 in Europe (including 12 in the Caucasus), 84 in Africa, 69 in Oceania, and 41 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kardamyli
Kardamili ( el, Καρδαμύλη, variously transliterated as ''Kardamyle'', ''Cardamyle'', ''Kardhamili'', and ''Kardamyli'', and sometimes called "Skardamoula", especially on old maps) is a town by the sea thirty-five kilometers southeast of Kalamata, Greece. It is the seat of the municipality of Lefktro in the region of Messenia on the Mani Peninsula. In the ''Iliad'' (Book 9The Iliad by Homer Book IX. ''Ἑπτὰ δέ οί δώσω εύναιόμενα πτολίεθρα, Καρδαμύλην, Ένόπην τε καὶ Ίρήν ποιήεσσαν,'' And will give him seven well established cities, Cardamyle, Enope, and Hire, where there is grass; (translation by Samuel Butler).), Homer cites Kardamili as one of the seven cities offered by Agamemnon to Achilles as a condition to rejoin the fight during the Trojan War. The village preserves its ancient name. The area is filled with beaches: Ritsa, Belogianni, Salio, Tikla, Amoni, Santava. The older town includes a mediaev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eurasian Plate
The Eurasian Plate is a tectonic plate that includes most of the continent of Eurasia (a landmass consisting of the traditional continents of Europe and Asia), with the notable exceptions of the Indian subcontinent, the Arabian subcontinent and the area east of the Chersky Range in eastern Siberia. It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge. The eastern edge is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south and possibly with the Okhotsk Plate and the Amurian Plate. The southern edge is a boundary with the African Plate to the west, the Arabian Plate in the middle and the Indo-Australian Plate to the east. The western edge is a divergent boundary with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge, which is straddled by Iceland. All volcanic eruptions in Iceland, such as the 1973 eruption of Eldfell, the 1783 eruptio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
African Plate
The African Plate is a major tectonic plate that includes much of the continent of Africa (except for its easternmost part) and the adjacent oceanic crust to the west and south. It is bounded by the North American Plate and South American Plate to the west (separated by the Mid-Atlantic Ridge); the Arabian Plate and Somali Plate to the east; the Eurasian Plate, Aegean Sea Plate and Anatolian Plate to the north; and the Antarctic Plate to the south. Between and , the Somali Plate began rifting from the African Plate along the East African Rift. Since the continent of Africa consists of crust from both the African and the Somali plates, some literature refers to the African Plate as the Nubian Plate to distinguish it from the continent as a whole. Boundaries The western edge of the African Plate is a divergent boundary with the North American Plate to the north and the South American Plate to the south which forms the central and southern part of the Mid-Atlantic Ridge. The A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fold (geology)
In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic sets (known as ''fold trains''). Synsedimentary folds are those formed during sedimentary deposition. Folds form under varied conditions of stress, pore pressure, and temperature gradient, as evidenced by their presence in soft sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar fault (''fault bend fold''), at the tip of a propagating fault (''fault propagation fold''), by differential compaction or due to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Sea
The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Western and Southern Europe and Anatolia, on the south by North Africa, and on the east by the Levant. The Sea has played a central role in the history of Western civilization. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was partly or completely desiccated over a period of some 600,000 years during the Messinian salinity crisis before being refilled by the Zanclean flood about 5.3 million years ago. The Mediterranean Sea covers an area of about , representing 0.7% of the global ocean surface, but its connection to the Atlantic via the Strait of Gibraltar—the narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates the Iberian Peninsula in Europe from Morocco in Africa—is only wide. The Mediterranean Sea e ... [...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] |
Mani Peninsula
The Mani Peninsula ( el, Μάνη, Mánē), also long known by its medieval name Maina or Maïna (Μαΐνη), is a geographical and cultural region in Southern Greece that is home to the Maniots (Mανιάτες, ''Maniátes'' in Greek), who claim descent from the ancient Spartans. The capital city of Mani is Areopoli. Mani is the central peninsula of the three which extend southwards from the Peloponnese in southern Greece. To the east is the Laconian Gulf, to the west the Messenian Gulf. The Mani peninsula forms a continuation of the Taygetos mountain range, the western spine of the Peloponnese. Etymology The name "Mani" may come from the Albanian language, albanian word mani meaning mullbery Geography The terrain is mountainous and inaccessible. Until recent years many Mani villages could be reached only by sea. Today a narrow and winding road extends along the west coast from Kalamata to Areopoli, then south to Akrotainaro (the pointed cape, which is the southernmost poin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greek National Road 82
National Road 82 ( el, Εθνική Οδός 82, abbreviated as EO82) is a single carriageway road in southern Greece. It connects Pylos with Sparti via Kalamata. It passes through the regional units Messenia and Laconia, on the Peloponnese peninsula. Its length is 110 km. Route The western end of the GR-82 is in the port town Pylos, on the Ionian Sea, where it is connected with the Greek National Road 9. It runs to the east through low hills, passing north of the Lykodimo mountain. It reaches the Messenian Gulf near Velika, and continues near the north shore of the gulf. It passes along Messini and through the city Kalamata, where it is connected with the Greek National Road 7. It leaves Kalamata towards the northeast, and crosses the Taygetus mountains over a pass of about 1300 m elevation. It descends to the city of Sparti, its eastern terminus. Here it is connected with the Greek National Road 39. National Road 82 passes through the following places: *Pylos * Chandrin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Messenia
Messenia or Messinia ( ; el, Μεσσηνία ) is a regional unit (''perifereiaki enotita'') in the southwestern part of the Peloponnese region, in Greece. Until the implementation of the Kallikratis plan on 1 January 2011, Messenia was a prefecture (''nomos'') covering the same territory. The capital and largest city of Messenia is Kalamata. Geography Physical Messenia borders on Elis to the north, Arcadia to the northeast, and Laconia to the southeast. The Ionian Sea lies to the west, and the Gulf of Messinia to the south. The most important mountain ranges are the Taygetus in the east, the Kyparissia mountains in the northwest and the Lykodimo in the southwest. The main rivers are the Neda in the north and the Pamisos in central Messenia. Off the south coast of the southwesternmost point of Messenia lie the Messinian Oinousses islands. The largest of these are Sapientza, Schiza and Venetiko. The small island Sphacteria closes off the bay of Pylos. All these islands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laconia
Laconia or Lakonia ( el, Λακωνία, , ) is a historical and administrative region of Greece located on the southeastern part of the Peloponnese peninsula. Its administrative capital is Sparta. The word ''laconic''—to speak in a blunt, concise way—is derived from the name of this region, a reference to the ancient Spartans who were renowned for their verbal austerity and blunt, often pithy remarks. Geography Laconia is bordered by Messenia to the west and Arcadia to the north and is surrounded by the Myrtoan Sea to the east and by the Laconian Gulf and the Mediterranean Sea to the south. It encompasses Cape Malea and Cape Tainaron and a large part of the Mani Peninsula. The Mani Peninsula is in the west region of Laconia. The islands of Kythira and Antikythera lie to the south, but they administratively belong to the Attica regional unit of islands. The island, Elafonisos, situated between the Laconian mainland and Kythira, is part of Laconia. The Eurotas is the lon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arcadia (regional Unit)
Arcadia ( el, Αρκαδία, ''Arkadía'' ) is one of the regional units of Greece. It is part of the administrative region of Peloponnese. It is in the central and eastern part of the Peloponnese peninsula. It takes its name from the mythological figure Arcas. In Greek mythology, it was the home of the god Pan. In European Renaissance arts, Arcadia was celebrated as an unspoiled, harmonious wilderness. Geography Arcadia is a rural, mountainous regional unit comprising about 18% of the land area of the Peloponnese peninsula. It is the peninsula's largest regional unit. According to the 2011 census, it has about 86,000 inhabitants; its capital, Tripoli, has about 30,000 residents in the city proper, and about 47,500 total in the greater metropolitan area. Arcadia consists partly of farmland, and to a larger extent grassland and degenerated shrubland. It also has three mountain ranges, with forestation mainly at altitudes above 1000 meters: Mainalo, a winter ski resort, situat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
