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Eurotas River
The Evrotas (Modern Greek: ) or Eurotas () is the main river of Laconia and one of the major rivers of the Peloponnese, in Greece. The river's springs are located just northwest of the border between Laconia and Arcadia, at Skortsinos. The river is also fed by underwater springs at Pellana and by tributaries coursing down from Mt. Taygetos and Mt. Parnon, which flank the Evrotas Valley to the west and east, respectively. The river is long, flowing in a north-south direction and emptying into the Laconian Gulf. Its drainage basin is . Etymology The classical Evrotas was changed to Iri in the Middle Ages and only changed back to Evrotas in recent times. Evrotas, however, is not the most ancient name of the river. It does not appear in the works of Homer, which purport to recount the stories and geography of Mycenaean Greece. In that legendary time, the Dorians are not known to have been present in the Evrotas Valley. At some time prior to being called Evrotas, the river was t ...
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Sparta
Sparta was a prominent city-state in Laconia in ancient Greece. In antiquity, the city-state was known as Lacedaemon (), while the name Sparta referred to its main settlement in the Evrotas Valley, valley of Evrotas (river), Evrotas river in Laconia, in southeastern Peloponnese. Around 650 BC, it rose to become the dominant military land-power in ancient Greece. Sparta was recognized as the leading force of the unified Greek military during the Greco-Persian Wars, in rivalry with the rising naval power of Classical Athens, Athens. Sparta was the principal enemy of History of Athens, Athens during the Peloponnesian War (431–404 BC), from which it emerged victorious after the Battle of Aegospotami. The decisive Battle of Leuctra against Thebes, Greece, Thebes in 371 BC ended the Spartan hegemony, although the city-state maintained its Independence, political independence until its forced integration into the Achaean League in 192 BC. The city nevertheless recovered m ...
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Mycenaean Greece
Mycenaean Greece (or the Mycenaean civilization) was the last phase of the Bronze Age in ancient Greece, spanning the period from approximately 1750 to 1050 BC.. It represents the first advanced and distinctively Greek civilization in mainland Greece with its palatial states, urban organization, works of art, and writing system.. The Mycenaeans were mainland Greek peoples who were likely stimulated by their contact with insular Minoan Crete and other Mediterranean cultures to develop a more sophisticated sociopolitical culture of their own. The most prominent site was Mycenae, after which the culture of this era is named. Other centers of power that emerged included Pylos, Tiryns, and Midea in the Peloponnese, Orchomenos, Thebes, and Athens in Central Greece, and Iolcos in Thessaly. Mycenaean settlements also appeared in Epirus, Macedonia, on islands in the Aegean Sea, on the south-west coast of Asia Minor, and on Cyprus, while Mycenaean-influenced settlements appear ...
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Pausanias (geographer)
Pausanias ( ; ; ) was a Greek traveler and geographer of the second century AD. He is famous for his '' Description of Greece'' (, ), a lengthy work that describes ancient Greece from his firsthand observations. ''Description of Greece'' provides crucial information for making links between classical literature and modern archaeology, which is providing evidence of the sites and cultural details he mentions although knowledge of their existence may have become lost or relegated to myth or legend. Biography Nothing is known about Pausanias apart from what historians can piece together from his own writing. However, it is probable that he was born into a Greek family and was probably a native of Lydia in Asia Minor. From until his death around 180, Pausanias travelled throughout the mainland of Greece, writing about various monuments, sacred spaces, and significant geographical sites along the way. In writing his '' Description of Greece'', Pausanias sought to put together ...
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Alpheios
The Alpheios (, , Latin Alpheus), sometimes spelled Alfeiós, is the main stream of the Alpheios Valley drainage system, a dendritic type, originating on the north slopes of Mount Taygetus, located in the center of the Peloponnesus of Greece, and flowing to the northwest to the vicinity of Olympia, where it turns to the west and, after being impounded by the Flokas Dam, a hydroelectric facility, empties into the Gulf of Kyparissia of the Ionian Sea south of Pyrgos. The entrance into the gulf through agricultural land and across an unpopulated, sandy beach partially blocked by a spit is hydrologically unspectacular, with the water too shallow to be navigable by any but the smallest craft. The concept of a single source has little meaning for most of the rivers of Greece, which begin as a confluence of multiple springs in the mountain valleys. There is almost never just one, although most may be unreported or neglected. Thus it is appropriate to speak "a source" or "the sources" ...
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Taygetus
The Taygetus, Taugetus, Taygetos or Taÿgetus () 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 Empire, 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 (geographer), Pausanias. The summit is an ultra-prominent peak. It is prominent ...
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Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ...
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ...
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Aquifer
An aquifer is an underground layer of water-bearing material, consisting of permeability (Earth sciences), permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt). Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called ''hydrogeology''. Related concepts include aquitard, a bed (geology), bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), a solid and impermeable region underlying or overlying an aquifer, the pressure of which could lead to the formation of a confined aquifer. Aquifers can be classified as saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; and transboundary aquifer. Groundwater from aquifers can be sustainably harvested by humans through the use of qanats leading to a well. This groundwater is a major source of fresh water for many regions, althoug ...
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Longanikos
Longanikos (, also transliterated as ''Logkanikos'') is a traditional Greek village, located in Laconia, in the ancient and historical Peloponnese area of southern Greece. It is also referred to sometimes in English as "Logganiko(s)" or "Longanico(s)". It is about 30 kilometers north of Sparta, the capital city of Lakonia, and is also very close to the cities of Kalamata, Tripolis and Megalopolis. It rests on the eastern slope of Mount Taigetos. The population of Longanikos is 404 inhabitants according to the 2021 census. This figure includes the population of the surrounding smaller villages Vergadeika, Kyparrissi, Giakoumaiika, and Kotitsa. Because of the small size of this village, residents of this town often identify themselves as Spartans to other Greeks or foreigners. For those who are familiar with this area, a resident or person from Longanikos is referred to as a "Longanikiotes" (masc) or "Longanikiotissa" (fem). Administration The village is administered as ...
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Spring (hydrosphere)
A spring is a natural exit point at which groundwater emerges from an aquifer and flows across the ground surface as surface water. It is a component of the hydrosphere, as well as a part of the water cycle. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and Hydrostatics#Hydrostatic pressure, hydrostatic pressure. A spring produced by the emergence of Geothermal activity, geothermally heated groundwater is known as a hot spring. The yield (hydrology), yield of spring water varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the water table reaches above the surface level, or if the terrain depression (geology), depresses sharply. Springs may also be formed ...
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Ionic Greek
Ionic or Ionian Greek () was a subdialect of the Eastern or Attic–Ionic dialect group of Ancient Greek. The Ionic group traditionally comprises three dialectal varieties that were spoken in Euboea (West Ionic), the northern Cyclades (Central Ionic), and from BC onward in Asiatic Ionia (East Ionic), where Ionian colonists from Athens founded their cities. Ionic was the base of several literary language forms of the Archaic and Classical periods, both in poetry and prose. The works of Homer and Hesiod are among the most popular poetic works that were written in a literary form of the Ionic dialect, known as Epic or Homeric Greek. The oldest Greek prose, including that of Heraclitus, Herodotus, Democritus, and Hippocrates, was also written in Ionic. By the end of the 5th century BC, Ionic was supplanted by Attic, which had become the dominant dialect of the Greek world. History The Ionic dialect appears to have originally spread from the Greek mainland across the A ...
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