Thermopylae Shoreline Changes Map
Thermopylae (; Ancient Greek and Katharevousa: (''Thermopylai'') , Demotic Greek (Greek): , (''Thermopyles'') ; "hot gates") is a place in Greece where a narrow coastal passage existed in antiquity. It derives its name from its hot sulphur springs."Thermopylae" in: S. Hornblower & A. Spawforth (eds.) ''The Oxford Classical Dictionary'', 3rd ed. (Oxford, 1996). In Greek mythology the Hot Gates is one of the entrances to Hades. Thermopylae is the site of a battle between the Greek forces (including Spartans, Thebans and Thespians) and the invading Persian forces, commemorated by Simonides of Ceos in the epitaph, "Go tell the Spartans, stranger passing by, That here obedient to their laws we lie." Thermopylae is the only land route large enough to bear any significant traffic between Lokris and Thessaly. To go from north to south along the east coast of the Balkans requires use of the pass. In ancient times it was called Malis, named after the Malians ( grc, Μαλιεῖς), ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Thermopylae Ancient Coastline Large
Thermopylae (; Ancient Greek and Katharevousa: (''Thermopylai'') , Demotic Greek (Greek): , (''Thermopyles'') ; "hot gates") is a place in Greece where a narrow coastal passage existed in antiquity. It derives its name from its hot sulphur springs."Thermopylae" in: S. Hornblower & A. Spawforth (eds.) ''The Oxford Classical Dictionary'', 3rd ed. (Oxford, 1996). In Greek mythology the Hot Gates is one of the entrances to Hades. Thermopylae is the site of a battle between the Greek forces (including Spartans, Thebans and Thespians) and the invading Persian forces, commemorated by Simonides of Ceos in the epitaph, "Go tell the Spartans, stranger passing by, That here obedient to their laws we lie." Thermopylae is the only land route large enough to bear any significant traffic between Lokris and Thessaly. To go from north to south along the east coast of the Balkans requires use of the pass. In ancient times it was called Malis, named after the Malians ( grc, Μαλιεῖς), ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Balkans
The Balkans ( ), also known as the Balkan Peninsula, is a geographical area in southeastern Europe with various geographical and historical definitions. The region takes its name from the Balkan Mountains that stretch throughout the whole of Bulgaria. The Balkan Peninsula is bordered by the Adriatic Sea in the northwest, the Ionian Sea in the southwest, the Aegean Sea in the south, the Turkish Straits in the east, and the Black Sea in the northeast. The northern border of the peninsula is variously defined. The highest point of the Balkans is Mount Musala, , in the Rila mountain range, Bulgaria. The concept of the Balkan Peninsula was created by the German geographer August Zeune in 1808, who mistakenly considered the Balkan Mountains the dominant mountain system of Southeast Europe spanning from the Adriatic Sea to the Black Sea. The term ''Balkan Peninsula'' was a synonym for Rumelia in the 19th century, the European provinces of the Ottoman Empire. It had a ge ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Travertine
Travertine ( ) is a form of terrestrial limestone deposited around mineral springs, especially hot springs. It often has a fibrous or concentric appearance and exists in white, tan, cream-colored, and even rusty varieties. It is formed by a process of rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. In the latter, it can form stalactites, stalagmites, and other speleothems. It is frequently used in Italy and elsewhere as a building material. Similar (but softer and extremely porous) deposits formed from ambient-temperature water are known as tufa. Definition Travertine is a sedimentary rock formed by the chemical precipitation of calcium carbonate minerals from fresh water, typically in springs, rivers, and lakes; that is, from surface and ground waters. In the broadest sense, travertine includes deposits in both hot and cold springs, including the porous, spongy rock known as tufa, and also the cave features known as speleot ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Deposition (sediment)
Deposition is the geological process in which sediments, soil and rocks are added to a landform or landmass. Wind, ice, water, and gravity transport previously weathered surface material, which, at the loss of enough kinetic energy in the fluid, is deposited, building up layers of sediment. Deposition occurs when the forces responsible for sediment transportation are no longer sufficient to overcome the forces of gravity and friction, creating a resistance to motion; this is known as the null-point hypothesis. Deposition can also refer to the buildup of sediment from organically derived matter or chemical processes. For example, chalk is made up partly of the microscopic calcium carbonate skeletons of marine plankton, the deposition of which has induced chemical processes (diagenesis) to deposit further calcium carbonate. Similarly, the formation of coal begins with the deposition of organic material, mainly from plants, in anaerobic conditions. Null-point hypothesis The null ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Amphictyonic League
In Archaic Greece, an amphictyony ( grc-gre, ἀμφικτυονία, a "league of neighbors"), or amphictyonic league, was an ancient religious association of tribes formed before the rise of the Greek ''poleis''. The six Dorian cities of coastal southwest Anatolia and the twelve Ionian cities to the north that formed the Ionian League after a Meliac war in the mid-7th century BC, were already of considerable antiquity when the first written records emerge. An amphictyony consisting of polities under the aegis of Apollo's shrine at Delos was apparently well-established in the seventh century, as the Homeric Hymn to Delian Apollo of that approximate date lists them, those cities and islands that trembled and refused to offer themselves for the birthplace of Apollo when pregnant Leto went to each in turn; the Homeric hymn presents an origin myth for the cult of Apollo on Delos. The joint Ionian festival celebrated there was the Delia. The Delian Amphictyony arose in the 4t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Temple Of Demeter Amphictyonis
The Temple of Demeter Amphictyonis was an extra-urban sanctuary in ancient Anthele in Thermopylae, dedicated to Demeter. It was an important Panhellenic shrine of Demeter and one of her main cult centers in Greece. It was also known as a center of the Amphictyonic League. The sanctuary is mentioned by Herodotus in the 5th century BC: :Between the river Asopos River">Asopos_(Thessaly).html" ;"title="hoinix, a tributary of the Asopos (Thessaly)">Asopos Riverand Thermopylai there is a village named Anthele, past which the Asopos flows out into the sea, and there is a wide space around it in which stand a temple of Demeter Amphiktyonis, seats for the Amphiktyones, and a temple of Amphiktyon himself. Excavations has dated the structures to the 5th-century BC. The archeological remains include a trapezoidal ''peribolos'', identified as a large stoa and stadium, which measures north side 66.30m, south side 65.30m, east side 6.20m, west side 7.65m. The Sanctuary of Demeter Amphyctionis ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Anthela (Thessaly)
Anthela or Anthele ( grc, Ἀνθήλη) was a town and polis (city-state) of Malis in Ancient Thessaly. Herodotus places the town between the small river Phoenix and Thermopylae which was a celebrated pass between Thessaly and Phocis. He also mentions that the Thessalian Asopus river passed through its surroundings and that there was a sanctuary of Demeter, a place where the Amphictyonic League celebrated its meetings and a temple of Amphictyon. According to legend, the league was founded, in part, to protect the temple of Demeter at Anthela. Anthela is in the immediate vicinity of the pass of Thermopylae, celebrated for the temples of Amphictyon and of the Amphictyonic Demeter, containing seats for the members of the Amphicytonic council, who held here their autumnal meetings. At Anthela, Mount Oeta recedes a little from the sea, leaving a plain a little more than half a mile in breadth, but again contracts near Alpeni, the first town of the Locrians, where the space is again o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Trachis
Trachis ( grc-gre, , ''Trakhís'') was a region in ancient Greece. Situated south of the river Spercheios, it was populated by the Malians. It was also a polis (city-state). Its main town was also called ''Trachis'' until 426 BC, when it was refounded as a Spartan colony and became Heraclea Trachinia. It is located to the west of Thermopylae. Trachis is located just west of the westernmost tip of the island of Euboea, north of Delphi. Near this place archaeologists discovered tombs from the Mycenaean period. According to Greek mythology Trachis was the home of Ceyx and Alcyone. Heracles went to Trachis after the death of Eunomus. The town is mentioned by Homer (as one of the cities subject to Achilles) and for the last time in antiquity by Pausanias. Trachis/Heraclea in ancient and modern times In antiquity the settlement was famous for being at the base of the mountain where Heracles is said to have died (Mount Oeta) as well as being the place where the descendants of Heracl ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Aenianes
Ainis (Ancient Greek Αἰνίς, , Modern Greek Αινίδα, ) or Aeniania, was a region of ancient Greece located near Lamia in modern Central Greece, roughly corresponding to the upper Valley of Spercheios. Name The region takes its name from the tribe of the Ainianians, who dwelt in the area. The name ''Ainis'' first occurs in Roman times; the only known earlier name of the region was "land of the Aenianians", ''Ainianōn khōra'' (Theopompus). Geography Ainis is located in the upper Spercheios valley, bordering with Dolopia in the west, Oita in the south, Malis in the east and Achaia Phthiotis in the north.H. Kramolisch, "Ainianes" ''Der Neue Pauly'', Brill Online, 2013. The exact borders with Oita and Malis have never been established.M. H. Hansen & T. Heine Nielsen (eds.), ''An inventory of Archaic and Classical poleis'', Oxford 2004. The river Spercheios floats through the region on its way down to the Maliac Gulf, and is joined in Ainis by its chief tributary the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Malian Gulf
The Malian or Maliac Gulf ( el, Μαλιακός Κόλπος, Maliakós Kólpos) is a gulf in the western Aegean Sea. It forms part of the coastline of Greece's region of Phthiotis. The gulf stretches east to west to a distance of , depending on the definition, and is very shallow, with a maximum depth of . The only harbour is that of Stylida, which serves the city of Lamia. To its east is Cape Lichada, the northwesternmost point of the island of Euboea. Name The gulf is named after the ancient Malians who lived on its shores. History Due to the constant accretion of silt from the river the Spercheios and smaller streams, the gulf has been shrinking over the centuries. In the summer of 426 BC, a tsunami hit the gulf between the northwest tip of Euboea and Lamia. The ancient strait of Thermopylae, which at the time the famous battle was fought, was delineated by Mount Kallidromo and the Malian Gulf, has now become a broad coastal plain. Under the London Protocol of 1830 Th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Spercheios
The Spercheios (, ''Sperkheiós''), also known as the Spercheus from its Latin name, is a river in Phthiotis in central Greece. It is long, and its drainage area is . It was worshipped as a god in the ancient Greek religion and appears in some collections of Greek mythology. In antiquity, its upper valley was known as Ainis. In AD 997, its valley was the site of the Battle of Spercheios, which ended Bulgarian incursions into the Byzantine Empire. It is referenced in a surviving fragment of Aeschylus' play ''Philoctetes'', quoted in ''The Frogs'', as a place for cattle. River The river begins in the Tymfristos mountains on the border with Evrytania and flows to the east through the village Agios Georgios Tymfristou, entering a wide plain. It flows along the towns Makrakomi and Leianokladi, and south of the Phthiotidan capital Lamia. The river flows through an area of former wetlands, that have been reclaimed for agriculture. It empties into the Malian Gulf of the Aegean Se ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |