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Zakros Mountains, Crete
The Zakros Mountains are a mountain range in Lasithi in eastern Crete, Greece. It trends to the northeast from Diaskari Beach in the southwest in the direction of Toplou Monastery near Cape Sidero. This range are considered to be the east side of the Sitia mountains (Σητειακά βουνά), divided from the west side by the Rema Pentelis ("Pentelis river"), a stream with its valley that flows S-N across most of Crete at that point, entering the Bay of Sitia just east of Sitia. On the west side of the valley are three ranges more or less in a SW-NE line: the Thrypti mountains, the Ornon Mountains, and the Western Siteia Foothills The Western Siteia Foothills are a range of foothills in Lasithi in eastern Crete, Greece. They are transitional in altitude between the Ornon Mountains, which trends from west to east starting at Kavousi in Ierapetra and ending at Praesos in .... The four ranges together are considered the Sitia mountains The 1975 creation of Sitia UNESCO G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zakros
Zakros ( el, Ζάκρος; Linear B: zakoro) is a site on the eastern coast of the island of Crete, Greece, containing ruins from the Minoan civilization. The site is often known to archaeologists as Zakro or Kato Zakro. It is believed to have been one of the four main administrative centers of the Minoans, and its protected harbor and strategic location made it an important commercial hub for trade to the east. Flinders Petrie related Zakro with Tjeker of the Sea Peoples. The town was dominated by the Palace of Zakro, originally built around 1900 BC, rebuilt around 1600 BC, and destroyed around 1450 BC along with the other major centers of Minoan civilization. Extensive ruins of the palace remain, and are a popular tourist destination. Geography Zakros is sometimes divided into ''Epano Zakros'' (''Upper Zakros''), the portion higher up on the hillside, and ''Kato Zakros'' (''Lower Zakros''), the part near the sea. A ravine known as the "Ravine of the Dead" runs through both the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Hill Range, East Crete
The Coastal Hill Range, East Crete is a mountain range in Lasithi in eastern Crete, Greece. It trends to the northeast from Xerokampos in the southwest in the direction of Cape Sidero. The range, however is drowned on the eastern slopes by the Kasos Strait, a deepwater channel between the island of Kasos and the island of Crete. Its peaks thus become headlands, islands, or near-surface elevations, while the cols between them are typically beaches. Geography The Coastal Hill Range is one of three SW-NE trending ranges of east Crete, the other two being called the Siteia Mountains. It consists of the Zakros Mountains on the east and, south to north in a row, the Thrypti, Ornon, and Western Siteia Foothills The Western Siteia Foothills are a range of foothills in Lasithi in eastern Crete, Greece. They are transitional in altitude between the Ornon Mountains, which trends from west to east starting at Kavousi in Ierapetra and ending at Praesos in ... on the west, the two ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crete
Crete ( el, Κρήτη, translit=, Modern: , Ancient: ) is the largest and most populous of the Greek islands, the 88th largest island in the world and the fifth largest island in the Mediterranean Sea, after Sicily, Sardinia, Cyprus, and Corsica. Crete rests about south of the Greek mainland, and about southwest of Anatolia. Crete has an area of and a coastline of 1,046 km (650 mi). It bounds the southern border of the Aegean Sea, with the Sea of Crete (or North Cretan Sea) to the north and the Libyan Sea (or South Cretan Sea) to the south. Crete and a number of islands and islets that surround it constitute the Region of Crete ( el, Περιφέρεια Κρήτης, links=no), which is the southernmost of the 13 top-level administrative units of Greece, and the fifth most populous of Greece's regions. Its capital and largest city is Heraklion, on the north shore of the island. , the region had a population of 636,504. The Dodecanese are located to the no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lasithi
Lasithi ( el, Λασίθι) is the easternmost regional unit on the island of Crete, to the east of Heraklion. Its capital is Agios Nikolaos, the other major towns being Ierapetra and Sitia. The mountains include the Dikti in the west and the Thrypti in the east. The Sea of Crete lies to the north and the Libyan Sea to the south. To the east of the village of Elounda lies the island of Spinalonga, formerly a Venetian fortress and a leper colony. On the foot of Mount Dikti lies the Lasithi Plateau, famous for its windmills. Vai is well known for its datepalm forest. Thanks to its beaches and its mild climate year-long, Lasithi attracts many tourists. Mass tourism is served by places like Vai, Agios Nikolaos and the island of Chrissi. More off-beat tourism can be found in villages on the south coast like Myrtos, Makrys Gialos or Makrigialos, Xerokambos and Koutsouras. Lasithi is home to a number of ancient remains. Vasiliki, Fournou Korifi, Pyrgos, Zakros and Gournia are ruin ... [...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] |
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] |
Cape Sidero
Cape Sideros or Cape Sidero ( el, Άκρα Σίδερος, Akra Sideros) is a cape at the eastern end of the island of Crete, Greece. Anciently it was known as Samonium or Samonion ( grc, Σαμώνιον), Sammonium or Sammonion ( grc, Σαμμώνιον), Salmonium or Salmonion (Σαλμώνιον) and Salmone (Σαλμώνη). The cape shares the name Sideros or Sidero with the island-like peninsula of which it is a projection, but which had the name first remains unknown, as does the provenance of either name. Cape Sidero is often not confined to the peninsula Sideros, but might refer to the entire northeast promontory. Etymology Semantic interpretations The meaning of Sidero seems transparent at first glance, as the modern Greek meaning of sidero with a short e is "ferruginous." The ancient Greek word has a long e, but the shortening of the e is no linguistic obstacle to common descent. There is no evidence of the sense. What about the island or the cape is "iron" remains un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrypti
Thrypti ( el, Θρυπτή) is a mountain range in Lasithi in eastern Crete, Greece. It trends to the northeast from Ierapetra in the southwest in the direction of Sitia. However, it only goes half-way in that direction. The rest of the distance is completed by the distinct Ornon mountains, separated from the Thrypti by the Bebonas river valley, and the lower Western Siteia Foothills covering the space between the Ornon range and Sitia itself. The highest peak of Thrypti is ''Afentis'', which is 1,476 m amsl. The three ranges constitute the West Sitia Mountains. Geography The Thrypti mountains are virtually 100% under the municipality of Ierapetra in Lasithi regional unit. The NE border of Ierapetra is so irregular that some small pockets of Thrypti might inadvertently be in neighboring Siteia municipality. Certainly the Sitia Mountains include ranges from both municipalities. The Thripti mountains run diagonally SW from the southern coast at the city of Ierapetra (where they ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ornon
Ornon () is a commune in the Isère department in southeastern France. Population See also *Communes of the Isère department The following is a list of the 512 Communes of France, communes in the French Departments of France, department of Isère. The communes cooperate in the following Communes of France#Intercommunality, intercommunalities (as of 2020): References Communes of Isère Isère communes articles needing translation from French Wikipedia {{Isère-geo-stub ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Siteia Foothills
The Western Siteia Foothills are a range of foothills in Lasithi in eastern Crete, Greece. They are transitional in altitude between the Ornon Mountains, which trends from west to east starting at Kavousi in Ierapetra and ending at Praesos in the east, and the north coastal plain around and west of Sitia. Part of the Sitia Mountains, they complete the SW-NE trending massif of ridges from Ierapetra to the plain of Sitia itself. Geologically, there is little difference between the Ornon Mountains and their northern foothills, which are west of Sitia. The same ravines cut through them both, draining from the Ornon into the Sea of Crete. The Ornon, however, are nearly uninhabitable for villages, due to their altitudes and steep slopes. On the northern side, there are no hills greater than . This is not a good line of demarcation, however, as the hills are all much lower than 800 m. The occupation line for villages is about the contour line. These villages are in the Western Foo ... [...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] |
Mountains Of Crete
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
