Ladon (river) in the context of "Lasion"

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⭐ Core Definition: Ladon (river)

The Ladon (Ancient Greek and Katharevousa: Λάδων, Ládōn; Demotic Greek: Λάδωνας, 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 70 km (43 mi) long.

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👉 Ladon (river) in the context of Lasion

Lasion (Greek: Λασίων or Λασιών) was the chief town of the mountainous district of Acroreia in ancient Elis proper, situated upon the frontiers of Arcadia near Psophis. Lasion was a frequent object of dispute between the Arcadians and Eleians, both of whom laid claim to it. In the war which the Spartans carried on against Elis at the close of the Peloponnesian War, Pausanias, king of Sparta, took Lasion. The invasion of Pausanias is not mentioned by Xenophon in his account of this war; but the latter author relates that, by the treaty of peace concluded between Elis and Sparta in 400 BCE, the Eleians were obliged to give up Lasion, in consequence of its being claimed by the Arcadians. In 366 BCE, the Eleians attempted to recover Lasion from the Arcadians; they took the town by surprise, but were shortly afterwards driven out of it again by the Arcadians. In 219 BCE, Lasion was again a fortress of Elis, but upon the capture of Psophis by Philip V of Macedon, the Eleian garrison at Lasion straightway deserted the place; after Philip took the town, he gave it to the Achaeans. Polybius mentions along with Lasion a fortress called Pyrgus, which he places in a district named Perippia.

It is located in the upper Ladon valley, north of modern Koumani.

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Ladon (river) in the context of Ladon (river of Elis)

The Ladon (Ancient Greek and Katharevousa: Λάδων, Ládōn; Demotic Greek: Λάδωνας, Ládōnas), or Pineiakos Ladonas (Greek: Πηνειακός Λάδωνας), to distinguish it from the river of the same name in Arcadia, is a river of Elis in Greece. It rises in the highlands to the south of Mount Erymanthus; it flows at first through a narrow ravine, and, anciently flowed into the Peneius, but now flows into the Pineios Reservoir [el], a man-made lake created by the Peneus Dam. It is 37.7 km (23.4 mi) long. The river is called the Selleeis (Σελλήεις) by Homer.

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Ladon (river) in the context of Erymanthos (river)

The Erymanthos (Greek: Ερύμανθος, Latin: Erymanthus) 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.

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Ladon (river) in the context of Pelagon

There are several figures named Pelagon (Ancient Greek: Πελάγων, -ονος) in Greek mythology.

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Ladon (river) in the context of Pheneus

Pheneus or Pheneos (Ancient Greek: Φένεος or Φενεός) was a town in the northeast of ancient Arcadia. Its territory, called Pheniatis (ἡ Φενεατική or ἡ Φενεᾶτις or η Φενική), was bounded on the north by that of the Achaean towns of Aegeira and Pellene, east by the Stymphalia, west by the Cleitoria, and south by the Caphyatis and Orchomenia. This territory is shut in on every side by lofty mountains, offshoots of Mount Cyllene and the Aroanian chain; and it is about 7 miles (12 km) in length and the same in breadth. Two streams descend from the northern mountains, and unite their waters about the middle of the valley; the united river bore in ancient times the name of Olbius and Aroanius. There is no opening through the mountains on the south; but the waters of the united river are carried off by subterranean channels (katavóthra) in the limestone rocks, and, after flowing underground, reappear as the sources of the river Ladon. In order to convey the waters of this river in a single channel to the katavóthra, the inhabitants at an early period constructed a canal, 50 stadia in length, and 30 feet (9 m) in breadth.

This great work, which was attributed to Heracles, had become useless in the time of Pausanias, and the river had resumed its ancient and irregular course; but traces of the canal of Heracles are still visible, and one bank of it was a conspicuous object in the valley when it was visited by William Martin Leake in 1806. The canal of Heracles, however, could not protect the valley from the danger to which it was exposed, in consequence of the katavóthra becoming obstructed, and the river finding no outlet for its waters. The Pheneatae related that their city was once destroyed by such an inundation, and in proof of it they pointed out upon the mountains the marks of the height to which the water was said to have ascended. Pausanias evidently refers to the yellow border which is still visible upon the mountains and around the plain: but in consequence of the great height of this line upon the rocks, it is difficult to believe it to be the mark of the ancient depth of water in the plain, and it is more probably caused by evaporation; the lower parts of the rock being constantly moistened, while the upper are in a state of comparative dryness, thus producing a difference of colour in process of time. It is, however, certain that the Pheneatic plain has been exposed more than once to such inundations. Pliny the Elder says that the calamity had occurred five times; and Eratosthenes related a memorable instance of such an inundation through the obstruction of the katavóthra, when, after they were again opened, the water rushing into the Ladon and the Alpheius overflowed the banks of those rivers at Olympia. The account of Eratosthenes has been confirmed by a similar occurrence in modern times. In 1821 the katavóthra became obstructed, and the water continued to rise in the plain till it had destroyed 7 to 8 square miles (18 to 21 km) of cultivated country. Such was its condition till 1832, when the subterraneous channels again opened, the Ladon and Alpheius overflowed, and the plain of Olympia was inundated. Other ancient writers allude to the katavóthra and subterraneous course of the river of Pheneus.

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Ladon (river) in the context of Ismenus

In Greek mythology, the name Ismenus (Ancient Greek: Ἰσμηνός) or Ismenius may refer to:

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Ladon (river) in the context of Corcyra (mythology)

In Greek mythology and religion, Corcyra (/kɔːrˈsaɪərə/) or Korkyra (/kɔːrˈkaɪərə/; Ancient Greek: Κόρκυρα, romanizedKórkura) is the naiad daughter of the river-god Asopos and the nymph Metope, herself the daughter of the river-god Ladon. She is the personification and tutelary goddess of the ancient Greek city and island of Korkyra, now better known as Corfu.

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