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Mesaoria Map
The Mesaoria ( el, Μεσαορία, tr, Mesarya) is a broad, sweeping plain which makes up the north centre of the island of Cyprus. Geography The Mesaoria is the name given to the broad tract of plain which extends across the island from the Bay of Famagusta in the east to that of Morphou in the west, which is a length of 96 km, with a breadth varying from 16 to 32 km. The streams which traverse it are mere winter torrents, which descend from the southern chain but scarcely reach the sea. The Pedias (Pediaeus) and lalias (Yialias, Idalias) lose most of their flood waters in the marshes about Salamis, near the Bay of Famagusta. The Pedias rises near Machaira and passes close to Nicosia, indeed flowed through it before the river was diverted by the Venetians. The lalias rises very near the source of the Pedias, passes through Nisou, Dali (the ancient Idalion) and Pyroi, and traverses the Mesaoria in a direction more or less parallel with the Pedias. A smaller but ...
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Mesaoria Map
The Mesaoria ( el, Μεσαορία, tr, Mesarya) is a broad, sweeping plain which makes up the north centre of the island of Cyprus. Geography The Mesaoria is the name given to the broad tract of plain which extends across the island from the Bay of Famagusta in the east to that of Morphou in the west, which is a length of 96 km, with a breadth varying from 16 to 32 km. The streams which traverse it are mere winter torrents, which descend from the southern chain but scarcely reach the sea. The Pedias (Pediaeus) and lalias (Yialias, Idalias) lose most of their flood waters in the marshes about Salamis, near the Bay of Famagusta. The Pedias rises near Machaira and passes close to Nicosia, indeed flowed through it before the river was diverted by the Venetians. The lalias rises very near the source of the Pedias, passes through Nisou, Dali (the ancient Idalion) and Pyroi, and traverses the Mesaoria in a direction more or less parallel with the Pedias. A smaller but ...
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Island Of Cyprus
Cyprus is an island in the Eastern Basin of the Mediterranean Sea. It is the third largest island in the Mediterranean, after the Italian islands of Sicily and Sardinia, and the 80th largest island in the world by area. It is located south of the Anatolia peninsula, yet it belongs to the Cyprus arc. Cyprus is in West Asia in the Middle East. Cyprus also had lengthy periods of mainly Greek and intermittent Anatolian, Levantine, Byzantine, Turkish and Western European influence. The island is dominated by two mountain ranges, the Troodos Mountains and the Kyrenia Mountains or Pentadaktylos, and the central plain, the Mesaoria, between them. The Troodos Mountains cover most of the southern and western portions of the island and account for roughly half its area. The narrow Kyrenia Range extends along the northern coastline. It is not as high as the Troodos Mountains, and it occupies substantially less area. The two mountain ranges run generally parallel to the Taurus Mountains on ...
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Breadbasket
The breadbasket of a country or of a region is an area which, because of the richness of the soil and/or advantageous climate, produces large quantities of wheat or other grain. Rice bowl is a similar term used to refer to Southeast Asia; and California's Salinas Valley is sometimes referred to as America’s salad bowl. Such regions may be the subject of fierce political disputes, which may even escalate into full military conflicts. Breadbaskets have become important within the global food system by concentrating global food-production in a small number of countries and, in countries such as India, in small geographic regions. As effects of climate change, climate change increases weather variability around the world, the effects of climate change on agriculture, likelihood of multiple breadbaskets failing at a time increases dramatically. The 2022 food crises has been in part facilitated by a series of failures in key breadbasket regions, and the 2022 Russian invasion of Uk ...
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Mesara
The Messara Plain or simply Messara ( el, Μεσσαρά) is an alluvial plain in southern Crete, stretching about 50 km west-to-east and 7 km north-to-south, making it the largest plain in Crete. On a hill at its west end are the ruins of Phaistos, Phaestus, near the middle are the ruins of the ancient city of Gortys. Since 1500 BC the plain has extended by up to 6 km due to a buildup of alluvial sediment. Clays from Messara have been found to be the source of significant amounts of Minoan pottery; soil and rock types from the fringes of Messara, particularly the foothills of the Asterousia Mountains at the south and the foothills to the north within the Psiloritis Mountains. In the Messara, olive trees, vineyards and horticultural crops are grown here. Part of the products grown here are placed on the domestic market. Α substantial part of the produced olive oil is then exported to European markets. The Messara Plain is also home to the indigenous Messara hors ...
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Karavostasi
Karavostasi ( el, Καραβοστάσι; tr, Gemikonağı) is a town in Cyprus, north of Lefka. It is under the ''de facto'' control of Northern Cyprus. Karavostasi is home to the port of Gemikonağı, which was historically used for exporting copper but is inactive since 1992. Before the conflict in Cyprus, Karavostasi had been a mixed village. Its name means "boat stop" in both Greek and Turkish. See also * Port of Gemikonağı The Gemikonağı Port or Karavostasi Port is a port at Karavostasi, in Morphou Bay, on the north side of the island of Cyprus. Until the 1930s, before the Lefka mines began operating, the port was mainly used for exporting Lefka's world-famous cit ... References Communities in Nicosia District Populated places in Lefke District {{Cyprus-geo-stub ...
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Copper
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form ( native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create ...
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Ptolemaic Dynasty
The Ptolemaic dynasty (; grc, Πτολεμαῖοι, ''Ptolemaioi''), sometimes referred to as the Lagid dynasty (Λαγίδαι, ''Lagidae;'' after Ptolemy I's father, Lagus), was a Macedonian Greek royal dynasty which ruled the Ptolemaic Kingdom in Ancient Egypt during the Hellenistic period. Their rule lasted for 275 years, from 305 to 30 BC. The Ptolemaic was the last dynasty of ancient Egypt. Ptolemy, one of the seven somatophylakes (bodyguard companions), a general and possible half-brother of Alexander the Great, was appointed satrap of Egypt after Alexander's death in 323 BC. In 305 BC, he declared himself Pharaoh Ptolemy I, later known as ''Sōter'' "Saviour". The Egyptians soon accepted the Ptolemies as the successors to the pharaohs of independent Egypt. Ptolemy's family ruled Egypt until the Roman conquest of 30 BC. Like the earlier dynasties of ancient Egypt, the Ptolemaic dynasty practiced inbreeding including sibling marriage, but this did not start ...
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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 ...
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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 ...
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Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multiply by ...
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Subtropical Climate
The subtropical zones or subtropics are geographical and climate zones to the north and south of the tropics. Geographically part of the temperate zones of both hemispheres, they cover the middle latitudes from to approximately 35° north and south. The horse latitudes lie within this range. Subtropical climates are often characterized by hot summers and mild winters with infrequent frost. Most subtropical climates fall into two basic types: humid subtropical (Koppen climate Cfa), where rainfall is often concentrated in the warmest months, for example Southeast China and the Southeastern United States, and dry summer or Mediterranean climate (Koppen climate Csa/Csb), where seasonal rainfall is concentrated in the cooler months, such as the Mediterranean Basin or Southern California. Subtropical climates can also occur at high elevations within the tropics, such as in the southern end of the Mexican Plateau and in Da Lat of the Vietnamese Central Highlands. The six climate clas ...
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Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ...
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