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Cnemis
Cnemis or Knemis ( grc, Κνῆμις; el, Κνημίς) was either a range of mountains between the Cephissus Valley and the Gulf of Euboea combined with the Malian Gulf, or was a single mountain located in the northwest of that range. The valley formed the heartland of Phocis, where the river originated, before entering Boeotia north of Orchomenos. The uncertainty of what terrain was meant by "Cnemis" derives from the varying accounts of the many sources. The narrower meaning is based on the home territory of the Epicnemidian Locrians, who received their distinguishing name from this mountain, on the northern slopes of which they made their homes. Mount Cnemis was a continuation of Callidromus, with which it was connected by a ridge, at the foot of which is the modern village of Mendenitsa. Callidromus is the mountain that overhangs Thermopylae. It is usually not counted as part of Cnemis, which is the next mountain east. The account of Cnemis in Smith, based on some of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Epicnemidian Locrians
Opuntian Locris or Eastern Locris was an ancient Greek region inhabited by the eastern division of the Locrians, the so-called tribe of the Locri Epicnemidii ( el, ) or Locri Opuntii (Greek: ). Geography Opuntian Locris consisted of a narrow slip upon the eastern coast of central Greece, from the pass of Thermopylae to the mouth of the river Cephissus. The northern frontier town was Alpeni, which bordered upon the Malians, and the southern frontier town was Larymna, which at a later time belonged to Boeotia. The Locrians, however, did not inhabit this coast continuously, but were separated by a narrow slip of Phocis, which extended to the North Euboean Gulf, and contained the Phocian seaport town of Daphnus. The Locrians north of Daphnus were called ''Epicnemidii'', from Mount Cnemis; and those south of this town were named ''Opuntii'', from Opus, their principal city. On the west, the Locrians were separated from Phocis and Boeotia by a range of mountains, extending from Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Cnemides
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Cape Cnemides or Knemides ( grc, Κνημῖδες; el, Κνημίς, Knemis ''or'' Knimis or Κνημίδος) in ancient times was a spur of Mount Cnemis, running out into the sea, opposite the islands called Lichades and the Euboean promontory Cenaeum. Upon Cape Cnemides stood a fortress, also called Cnemides (or Cnemis), distant 20 stadia from Thronium. Apart from some ambiguity about the extent of Cnemis, whether it was the entire range along the Gulf of Euboea or just one mountain in it, Smith's description certainly applies to the modern Cnemis. The Lichades bear the same name as they did in ancient times, identifying the promontory of Euboea. Attribution References Geography of ancient Phocis Cnemides Cnemides or Knemides ( grc, Κνημῖδες), also Cnemis or Knemis (Κνῆμις),''Periplus of Pseudo-Scylax'', p. 23; is the name of a fortress, and probably of a town, in ancient Phocis. Strabo places Cnemides on Cape Cnemides opposite t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cnemides
Cnemides or Knemides ( grc, Κνημῖδες), also Cnemis or Knemis (Κνῆμις),''Periplus of Pseudo-Scylax'', p. 23; is the name of a fortress, and probably of a town, in ancient Phocis. Strabo places Cnemides on Cape Cnemides opposite the islands called Lichades and the Euboean promontory Cenaeum, distant 20 stadia from Thronium and from Daphnus. The Periplus of Pseudo-Scylax, successively describing towns along the Phocian coast, places Cnemides after Thronium and before Elateia and Panopeus Panopeus (), or Phanoteus (the name is given in a variety of forms in the ancient sources), was a Greek town of ancient Phocis, near the frontier of Boeotia, and on the road from Daulis to Chaeronea. Pausanias said that Panopeus was 20 stadia fro .... The site of Cnemides is near the modern Gouvali. References Populated places in ancient Phocis Populated places in Opuntian Locris Former populated places in Greece {{ancientPhocis-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Euboea
Evia (, ; el, Εύβοια ; grc, Εὔβοια ) or Euboia (, ) is the second-largest Greek island in area and population, after Crete. It is separated from Boeotia in mainland Greece by the narrow Euripus Strait (only at its narrowest point). In general outline it is a long and narrow island; it is about long, and varies in breadth from to . Its geographic orientation is from northwest to southeast, and it is traversed throughout its length by a mountain range, which forms part of the chain that bounds Thessaly on the east, and is continued south of Euboia in the lofty islands of Andros, Tinos and Mykonos. It forms most of the regional unit of Euboea, which also includes Skyros and a small area of the Greek mainland. Name Like most of the Greek islands, Euboea was known by other names in antiquity, such as ''Macris'' (Μάκρις) and ''Doliche'' (Δολίχη) from its elongated shape, or ''Ellopia'', ''Aonia'' and ''Abantis'' from the tribes inhabiting it. Its ancie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Central Greece
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] |
Mountains Of Greece
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] |
Thronium (Locris)
Thronium or Thronion ( grc, Θρόνιον) was an ancient Greek town, the chief town of the Locrians, situated 20 ''stadia'' from the coast and 30 ''stadia'' from Scarpheia, upon the Boagrius River, which is described by Strabo as sometimes dry, and sometimes flowing with a stream two ''plethra'' in breadth. It is mentioned in the Catalogue of Ships of the ''Iliad'', by Homer, who speaks of it as near the river Boagrius. At the beginning of the Peloponnesian War (431 BCE) Thronium was taken by the Athenians. It was at one time partly destroyed by an earthquake in 426 BCE. In the Third Sacred War it was taken by Onomarchus, the Phocian general, who sold its inhabitants into slavery, and hence it is called a Phocian city by the author of the ''Periplus of Pseudo-Scylax''. Thronium is also mentioned by Polybius, Euripides, Livy, Pausanias, Lycophron, Ptolemy, Pliny the Elder, and Stephanus of Byzantium Stephanus or Stephan of Byzantium ( la, Stephanus Byzantinus; grc-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stadion (unit)
The stadion (plural stadia, grc-gre, ; Romanization, latinized as stadium), also anglicized as stade, list of obsolete units of measurement, was an ancient Greek units of measurement, ancient Greek unit of length, consisting of 600 Ancient Greek feet (''podes''). Calculations According to Herodotus, one stadium was equal to 600 pous, Greek feet (''podes''). However, the length of the foot varied in different parts of the Greek world, and the length of the stadion has been the subject of argument and hypothesis for hundreds of years. An empirical determination of the length of the stadion was made by Lev Vasilevich Firsov, who compared 81 distances given by Eratosthenes and Strabo with the straight-line distances measured by modern methods, and averaged the results. He obtained a result of about . Various equivalent lengths have been proposed, and some have been named. Among them are: Which measure of the stadion is used can affect the interpretation of ancient texts. For e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Periplus Of Pseudo-Scylax
The ''Periplus of Pseudo-Scylax'' is an ancient Greek periplus (περίπλους ''períplous'', 'circumnavigation') describing the sea route around the Mediterranean and Black Sea. It probably dates from the mid-4th century BC, specifically the 330s, and was probably written at or near Athens. Its author is often included among the ranks of 'minor' Greek geographers. There is only one manuscript available, which postdates the original work by over 1500 years. The author's name is written Pseudo-Scylax or Pseudo-Skylax, often abbreviated as Ps.-Scylax or Ps.-Skylax. Author The only extant, medieval manuscript names the author as "Scylax"' (or "Skylax"), but scholars have proven that this attribution is to be treated as a so-called "pseudepigraphy, pseudepigraphical appeal to authority": Herodotus mentions a Scylax of Caryanda, a Greek navigator who in the late sixth century BC explored the coast of the Indian Ocean on behalf of the Achaemenid Persia, Persians.Herodotus. ''His ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenaeum
Mount Lichada and Cape Lichada ( el, Χερσόνησος Λιχάδα, Chersonesos Lichada) is a mountain and cape forming the northwest tip of the island of Euboea, Greece. Their ancient name was Κήναιον ''Kenaion'', Latinized as Cenaeum. There is a village called Lichada on the slopes of Mount Lichada. Not far from the mount is the site of the ancient town of Dium. Mount Lichada is high. On top of Mount Kenaion, there was an altar and sanctuary of Zeus Kenaios (Ζεύς Κήναιος). It was here, Sophocles tells us, that Heracles dedicated altars to Ζεύς Πατρῴος (Zeus Patroos), made sacrifices, and donned the Shirt of Nessus brought to him by Lichas.Arthur Bernard Cook, ''Zeus: A Study in Ancient Religion'', 1925, p. 90Google Books/ref> When he realized that it was a lethal gift, he flung Lichas into the sea. Notes Locations in Greek mythology Lichada Lichada ( el, Λιχάδα, ''Licháda'') is a village in Euboea, Greece. Since the 2011 local gover ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cephissus (Boeotia)
The Cephissus ( grc, Κήφισσος), called the Boeotian Cephissus to distinguish it from other rivers of the same name, or Kifisos ( el, Βοιωτικός Κηφισός) is a river in central Greece. Its drainage basin is . In Greek mythology, the river god Cephissus (mythology), Cephissus was associated with this river. The river rises at Lilaia in Phocis, on the northwestern slope of Mount Parnassus. It flows east through the Boeotian plain, passing the towns Amfikleia, Kato Tithorea and Orchomenus (Boeotia), Orchomenos. It drained into Lake Copais, which was therefore also called the Cephisian Lake, until 1887, when the lake was drained. An artificial outflow has been created to Lake Yliki (ancient Hylice), further east. Pausanias (geographer), Pausanias records a Thebes, Greece, Theban tradition that the river Cephissus formerly flowed under a mountain and entered the sea until Heracles blocked the passage and diverted the water into the Orchomenus (Boeotia), Orchomenian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lichades
Lichades or Lichadonisia ( el, Λιχάδες or Λιχαδονήσια) is an island complex off the north west of Euboea, in the North Euboean Gulf. The islands located opposite Lichada cape in the north-western extreme of Euboea and opposite of small town Kamena Vourla in Central Greece mainland. Administratively, they belong to Istiaia-Aidipsos municipality, in Euboea regional unit. Description The complex consists of seven islands and islets. The biggest of them is Manolia and is the only that had residents in the past. The other six are Strongyli, Mikri Strongyli, Steno, Vagia, Vorias and Limani. The biggest island, Manolia has a beautiful beach and is visited by many tourists in the summer. In the past had a small settlement but nowadays is forsaken. Strongyli is the second largest island and on top has a big lighthouse. History Lichades were formed after the huge earthquake of 426 B.C., when the land between them sank in the Euboean Sea. According to Greek mythology, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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