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Alfeios
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 source ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olympia, Greece
Olympia ( ; ), officially Archaia Olympia ( ), is a small town in Elis (regional unit), Elis on the Peloponnese peninsula in Greece, famous for the nearby archaeological site of the same name. The site was a major Panhellenic sanctuary, Panhellenic religious sanctuary of ancient Greece, where the ancient Olympic Games were held every Olympiad, four years throughout classical antiquity, from the 8th century BC to the 4th century AD. They were Olympic Games, restored on a global basis in 1894 in honor of the ideal of peaceful international contention for excellence. The sacred precinct, named the Altis, was primarily dedicated to Zeus, although other gods were worshipped there. The games conducted in his name drew visitors from all over the Greek world as one of a group of such "Panhellenic" centres, which helped to build the identity of the ancient Greeks as a nation. Despite the name, it is nowhere near Mount Olympus in northern Greece, where the twelve Olympians, the major deit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ladon (river)
The Ladon (Ancient Greek and Katharevousa: , ''Ládōn''; Demotic Greek: , ''Ládōnas'') is a river in the Peloponnese peninsula of Greece. It features in Greek mythology. It is a tributary to the river Alfeios, which empties into the Ionian Sea. It is long. Course The Ladon rises on the western slope of the Aroania mountain, near the village Kastriá, Kleitoria municipal unit, Achaea. It flows south, receives its left tributary Aroanios, flows along Kleitoria and turns southwest near the Arcadian border. It flows through the artificial Ladon Lake, and turns south again near Dimitra. It flows into the Alfeios 3 km southeast of the village Tripotamia. It joins the Tragus near Zevgolatio. Mythology The river was among those mentioned by Hesiod in ''Theogony;'' they were "all sons of Oceanus and queenly Tethys" for, according to the image of world hydrography common to the ancients, the fresh water that welled up in springs came from the underworld caverns and poo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lousios
The Lousios (; ), also known in antiquity as Gortynius or Gortynios (), is a river and a gorge in western Arcadia that stretches from Karytaina north to Dimitsana in Greece Greece, officially the Hellenic Republic, is a country in Southeast Europe. Located on the southern tip of the Balkan peninsula, it shares land borders with Albania to the northwest, North Macedonia and Bulgaria to the north, and Turkey to th .... The river begins near Lykochori and flows through the Lousios Gorge. The river is treacherous and flows rapidly. It empties into the Alfeios northwest of Karytaina and south of Atsicholos. The river forms a deep, narrow gorge. Its length is approximately from north to south and its width is approximately wide. The gorge is very popular amongst hikers. At the northern end of the gorge lies the town of Dimitsana. At the southern end is the ancient city of Gortys with the temple of Asclepius. Much of the gorge is heavily forested, and there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erymanthos (river)
The Erymanthos (, ) is a river in the western part of the Peloponnese in Greece. Its source is on the southern slope of Mount Erymanthos, near the village of Agrampela, Achaea. It flows towards the south through a rocky landscape and receives several small tributaries. The river flows into an area rich in pine trees and passes several small mountain villages including Tripotama. Beyond Tripotama it forms the border between Elis and Arcadia. It flows east of the Foloi oak forest. The river empties into the Alfeios 5 km west of the Ladon) confluence, near the village Tripotamia. Places along the river * Plaka *Tripotama Psofida (Greek: Ψωφίδα) is a village and a community in the municipal unit of Aroania in the southern part of Achaea, Greece. The community consists of the villages Psofida, Ano Psofida, Tripotama, Ano Tripotama, Kato Tripotama and Vasiliki. ... * Paralongoi * Achladini * Tripotamia External links Landforms of Achaea Landforms of Arcadia, Pelo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyrgos, Elis
Pyrgos () is a city in the northwestern Peloponnese, Greece, capital of the regional unit of Elis (regional unit), Elis and the seat of the Municipality of Pyrgos. The city is located in the middle of a plain, from the Ionian Sea. The river Alfeios flows into sea about south of Pyrgos. The population of the town Pyrgos is 26,052, and of the municipality 45,365 (2021). Pyrgos is west of Olympia, Greece, Olympia, southeast of Amaliada, southwest of Patras and west of Tripoli, Greece, Tripoli. Historical population Municipality The municipality Pyrgos was formed during the 2011 local government reform by the merger of the following 4 former municipalities, that became municipal units: *Iardanos *Oleni *Pyrgos *Volakas, Elis, Volakas The municipality has an area of 456.610 km2, the municipal unit 170.866 km2. Subdivisions The municipal unit of Pyrgos is divided into the following communities (settlements within the communities given in brackets): *Pyrgos (Pyrgos, A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elis (regional Unit)
Elis also known as Ellis or Ilia (, ''Eleia'') is a historic region in the western part of the Peloponnese peninsula of Greece. It is administered as a regional unit of the modern region of Western Greece. Its capital is Pyrgos. Until 2011 it was Elis Prefecture, covering the same territory. The modern regional unit is nearly coterminous with the ancient Elis of the classical period. Here lie the ancient ruins of cities of Elis, Epitalion and Olympia, known for the ancient Olympic Games which started in 776 BC. Geography The northernmost point of Elis is 38° 06'N, the westernmost is 22° 12′E, the southernmost is 37° 18′N, and the easternmost is 21° 54′E. The length from north to south is , and from east-to-west is around . The modern regional unit is not completely congruent with ancient Elis: Lampeia belonged to ancient Arcadia, and Kalogria is now part of Achaea. The longest river is the Alfeios. Other rivers are the Erymanthos, Pineios a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arcadia (region)
Arcadia (; ) is a region in the central Peloponnese, Greece. It takes its name from the mythological character Arcas, and in Greek mythology it was the home of the gods Hermes and Pan. In European Renaissance arts, Arcadia was celebrated as an unspoiled, harmonious wilderness; as such, it was referenced in popular culture. The modern regional unit of the same name more or less overlaps with the historical region, but is slightly larger. History Arcadia was gradually linked in a loose confederation that included all the Arcadian towns and was named League of the Arcadians. In the 7th century BC, it successfully faced the threat of Sparta and the Arcadians managed to maintain their independence. They participated in the Persian Wars alongside other Greeks by sending forces to Thermopylae and Plataea. During the Peloponnesian War, Arcadia allied with Sparta and Corinth. In the following years, during the period of the hegemony of Thebes, the Theban general Epaminondas re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peloponnese
The Peloponnese ( ), Peloponnesus ( ; , ) or Morea (; ) is a peninsula and geographic region in Southern Greece, and the southernmost region of the Balkans. It is connected to the central part of the country by the Isthmus of Corinth land bridge which separates the Gulf of Corinth from the Saronic Gulf. From the late Middle Ages until the 19th century, the peninsula was known as the Morea, a name still in colloquial use in its demotic form. The peninsula is divided among three administrative regions: most belongs to the Peloponnese region, with smaller parts belonging to the West Greece and Attica regions. Geography The Peloponnese is a peninsula located at the southern tip of the mainland, in area, and constitutes the southernmost part of mainland Greece. It is connected to the mainland by the Isthmus of Corinth, where the Corinth Canal was constructed in 1893. However, it is also connected to the mainland by several bridges across the canal, including two submers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift Valley
A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear depression may subsequently be further deepened by the forces of erosion. More generally the valley is likely to be filled with sedimentary deposits derived from the rift flanks and the surrounding areas. In many cases rift lakes are formed. One of the best known examples of this process is the East African Rift. On Earth, rifts can occur at all elevations, from the sea floor to plateaus and mountain ranges in continental crust or in oceanic crust. They are often associated with a number of adjoining subsidiary or co-extensive valleys, which are typically considered part of the principal rift valley geologically. Earth's rift valleys The most extensive rift valley is located along the crest of the mid-ocean ridge system and is the result ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depression (geology), depressed block of the Crust (geology), crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German language, German, meaning 'ditch' or 'trench'. The first known usage of the word in the geologic context was by Eduard Suess in 1883. The plural form is either ''graben'' or ''grabens''. Formation A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with Horst (geology), horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced by sets of normal faults that have parallel fault traces, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hjalmar Frisk
Hjalmar Frisk (4 August 1900, in Gothenburg – 1 August 1984, in Gothenburg) was a Swedish linguist and etymologist in Indo-European studies. He was also rector of the University of Gothenburg from 1951 to 1966.Göteborgs Universitet Early on, he became interested in Indo-European studies. Thus, as early as 1927, he published a translation of the historical account '' The Periplus of the Erythraean Sea'', written in under the title Περίπλους τῆς Ἐρυθρᾶς θαλάσσης. His most noted work was the three-volume ''Griechisches etymologisches Wö ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Extensional Tectonics
Extensional tectonics is concerned with the structures formed by, and the Tectonics, tectonic processes associated with, the stretching of a planetary body's Crust (geology), crust or lithosphere. Deformation styles The types of structure and the geometries formed depend on the amount of stretching involved. Stretching is generally measured using the parameter ''β'', known as the ''beta factor'', where : \beta = \frac \,, ''t''0 is the initial crustal thickness and ''t''1 is the final crustal thickness. It is also the equivalent of the Strain (materials science), strain parameter ''stretch''. Low beta factor In areas of relatively low crustal stretching, the dominant structures are high to moderate angle normal faults, with associated half grabens and tilted block faulting, tilted fault blocks. High beta factor In areas of high crustal stretching, individual extensional faults may become rotated to too low a dip to remain active and a new set of faults may be generated. Lar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
