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Evrotas (river)

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677: 652:-type, with "less substantial walls" but "a massive foundation for what could be a defense tower." It was connected to the top by stairs. Period III, LH3A2–LH3B2, begins with 150 years of apparent abandonment and then a limited reconstruction of a one-story structure on the terrace. The staircase was blocked. The entire ridge was intensely occupied leaving a profusion of Mycenaean pottery. The villa was burned at the end of LH3B2, leaving a destruction level. Two persons buried in the associated rubble appear to have died violently. Occupation of the hill went on through the 47: 460:
stations. Consequently, the river is intermittent; large sections are typically dry of surface water, even though water still flows in the aquifers. Flash flooding is a problem. Through flood control, the riverbed has been widened in places and straightened, and the vegetation has been removed from its sides. The lower river runs between dikes in a long, straight course.
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Geologic analysis done in the 20th century hypothesized that the Evrotas Valley in the Late Pliocene was an inland sea over the lower and middle valley several hundred m deep at the current mouth of the river. The fault-block geology had developed earlier. During the Pleistocene the sea level dropped
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The excavators concluded that in the "later 15th century" (BC) the ridge was "the principal settlement site in Laconia." The shrine and its dedications identify it as the site of Homeric Sparta, capital of a ruling couple believed by the population of the Archaic Period to have been Menelaos and
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river in the northwestern Peloponnese). The flow is copious except in times of drought. A recent study measured the outflow through the catchment exit every 15 days for 540 days in 2006-2007. It recorded a maximum of 1748 cubic m per hour and a minimum of 310.5 cubic m per hour. From the catchment at
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The town was apparently continuously occupied from the late Neolithic to Byzantine times when it was drowned, perhaps by an earthquake. Neolithic ceramics were only 3% of the 444 items. The town was mainly Early Bronze Age, which had 40%. The early Helladic pottery is "standard ... some showing
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The current communities of Elos, Leimonas and Agioi Taxiarches have been constructed on aggraded land. As Pausanias mentions that Elos was a port city, the current Elos cannot be identified with it. Skala, on the other hand, means "place of embarkation." The location of the ancient port, however, is
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In the winter months, the Evrotas is prone to flooding. On 24 November 2005 heavy floods damaged buildings and stranded automobiles in the streets, and harmed orchards, including the valley's famous orange and olive groves. The floods affected many villages along the valley as well as the town
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Today, the river is hydromorphologically far from its natural state. The main problem is anthropogenic abstraction of water, by many methods, from the shallow aquifer through which it flows. The valley contains about 7000 wells. Water is directly removed by irrigation ditches, weirs, and pumping
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During Period IA, the hill settlement was rebuilt. The structures included kilns for smelting bronze. In Period II, dated to LH3A1, a villa-type structure was built of a terrace formed from previous building material further down to the south. It was probably two-story,
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500 m (1,600 ft) exposing a flat floor. Continued slippage along the Sparta Fault dropped the middle Eurotas valley further forcing the river to cut its way through the 100–250 m hills dividing the lower from the middle valley, creating Evrotas Ravine.
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island off Elafonisos. A subsequent survey in 2009 discovered even earlier parts of the town and recovered additional pottery. A chronological study was done on "442 ceramic items, an iron nail and an obsidian chip." More research on the site is planned.
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that were present were not overtly recorded by the surviving administrative records but by surviving copies of records. Hypothetically, if the Leleges really were in the Eurotas valley, the time of their ascendancy would have been before Mycenaean times.
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In modern times, much of the river water is used for irrigation, with the result that the Eurotas is almost dry during the summer months. The waters of the Eurotas are used to irrigate mainly citrus crops, for which Laconia is famous. The plain of
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pottery in "pockets in the bedrock." The archaeologists analyzing the site recognized a building Period I, dated between LH2B–LH3A1, the latter being brought to and end about 1425 BCE by a severe earthquake. Remains of a mansion with
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The rich alluvial soil through which the final 10 km of the Eurotas flows was not there in antiquity. The Eurotas has aggraded the innermost bay of the gulf. The old coastline can be approximated by a line on the periphery of the plain of
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Vathyrema (with Kastaniotiko, Vresiotiko, Kardaris), Voutikiotis, Rasina (with Gerakaris), Kakorema, Kerasiotiko, Kotitsanis, Magoulitsa, Mylopotamos, Nikova, Kserilas, Paroritis, Verias, Skatias, Tzitziniotiko, Tyflo,
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Logaras Spring supplies an anciently constructed catchment basin about the size of a pond, sometimes called a lake, which exits both to irrigation channels and to the Alpheios stream (not to be confused with the
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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
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The main roads from Sparta form a branching network leading out radially from the city to connect other cities and towns in the valley. A web of secondary roads fills in the spaces between the main roads.
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it was a lake. In classical times, according to the ancient authors, it was swampy, but the cultivatable land exposed was very fertile. Then, as now, it was used mainly for fruit trees, especially olive.
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was built on the west bank of the Eurotas about halfway down the valley. The Spartans made little use of the left bank of the river: Only one permanent bridge has been found that crossed to it, at
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road to Vlachiotis, southeast along the edge of the rising terrain to Asteri and south from there to the coast. Due to changes in sea level, some land on the flanks of the gulf has been drowned.
2201: 600:. This archaeological scenario is not incompatible with the Aegean distribution of the Leleges, although it is not possible to say who the early and middle Bronze Age inhabitants were. 723:, as in ancient times, at a site which dominated and still dominates the valley from its central position. However, the rich-soil plain is entirely divided into villages that practice 472:. The major ones have cut deep ravines into the Taygetus Massif. The few left-bank tributaries, receiving waters from the deep aquifer, are more substantial, but still intermittent. 1524:
from Taygetus cover half the valley, making it asymmetrical. On that account it is often called the Evrotas Furrow. The Evrotas flows over a flood plain and also through a shallow
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Skoulikidis, Nikos, Elias Dimitriou, and Ioannis Karaouzas (Eds.), The Rivers of Greece: Evolution, Current Status and Perspectives. Berlin: Springer, 2018. ISBN 978-3-662-55367-1
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station recorded 47.4°C. On average this station records 43 days annually with temperatures over 40.0°C. On July 30, 2021 the Kelefina Hydro Meteorological station of the
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The classical Oineus was changed to Kelefina in the Middle Ages and not restored to its ancient name until recent times. The current Magoulitsa was formerly the Trypiotiko.
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The late Bronze Age had 25% of the items. Classical and Byzantine items were minimal, indicating a probable near abandonment of the city at the end of the late Bronze Age.
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Archaeology has provided a more complete story for the Mycenaean period. On the left bank of the Eurotas, across from Sparta, is a ridge on which sits a temple called the
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Armstrong, Pamela; Cavanagh, W. G.; Shipley, Graham (1992). "Crossing the River: Observations on Routes and Bridges in Laconia from the Archaic to Byzantine Periods".
447:. The identity of their names comes from an ancient geologic misunderstanding that the Eurotas and the Apheios were connected underground, which deceived even 2019: 2005: 529:, one of the peoples of the eastern Aegean whom the classical writers saw as autochthonous; that is, indigenous and pre-Hellenic. His son or grandson was 1544:
beds, some of which are impermeable. Under the entire valley is a deep aquifer in the limestone floor, containing water permeating downward through the
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winds sweep Greece during the summer, both mountains provide a constant hot foehn winds effect which strongly affects the interior of the valley.
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and transmissivity are near the junction of the Xerias and the Evrotas south of Sparti. To the east are older and finer sediments of alternating
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Currently the nitrate waste from fertilizers is polluting the river, aggravated by diminished flow because of the irrigation demands on it.
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to the west and east, respectively. The river is 82 kilometres (51 mi) long, flowing in a north-south direction and emptying into the
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Skoulikidis, Nikolaos; Economou, Alcibiades; Karaouzas, Joannis; Amaxidis, Yorgos; Vardakas, Leonidas; Economou, Elena (May 2008),
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Taygetus is transected by deep ravines through which tributaries flow into the Eurotas. At the foot of the massif is a zone of
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an altitude of 430 m (1,410 ft) part of the water flows into the Alpheios stream, which enters the upper Eurotas.
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Until the late 20th century, evidence in the valley of earlier occupation seemed to be lacking. Beginning in 1968 the
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marking the border within which prehistoric archaeological sites are not found. The line on the west follows the
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Most of the numerous tributaries of the Eurotas are right-bank, feeding the shallow aquifer. They are, however,
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Massif, but, like the other mountains of Arcadia, is a nappe raised by the compressional forces on the
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mountains, completely cut out from the sea on all directions, some 30 km away from the shores. As the
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deep, graded with the deep end downstream. The gradient of the aquifer is a steep 1–3%. The highest
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eurōs (εὐρώς), "mold". The adjective, eurōeis, "moldy," is genuinely ancient, used as an epithet of
616: 76: 469: 2339: 1738:. Cambridge Library collection. Cambridge; New York, NY: Cambridge University Press. p. 196. 568: 533:, the last of the line. The latter had a daughter, Sparta, but no sons. An outsider married her, 444: 404: 306: 114: 85: 2268:. Taylor & Francis e-Library. London and New York: Routledge. pp. 13–14. Archived from 596:
and the northeastern Aegean." The "15% Middle Bronze Age" is represented by middle Helladic and
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in terms of summer average highs. This is due to the interior's geographical location between
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began a survey by underwater archaeology of a drowned town between Pounta on the mainland and
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In Greek legend, the human ancestor of all the peoples that inhabited the Eurotas Valley was
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Natural Environment and Human Settlement in Prehistoric Greece based on original fieldwork
1596:(in Greek). Ministry of Environment, Energy and Climate Change. p. 46. Archived from 1509:
ridges derived from a former sea bed. On the east side of Taygetus is the Sparta Fault, a
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The ruins of the ancient Theatre of Sparta. In the background, the modern town with Mount
8: 641: 362:. At some time prior to being called Evrotas, the river was the Bomycas and the Himeras. 2236: 2197: 1750: 759:). The interior of the valley records the highest summer mean maximum temperatures in 656:, reduced to the Menelaon shrine in the Archaic and Classical Periods. Dedications to 2066: 1999: 2228: 2193: 700:, which was the most convenient outlet. All others involved a trek over mountains. 624: 548: 540: 351: 305:. The river's springs are located just northwest of the border between Laconia and 399:
called Piges Evrota (Πηγές Ευρώτα, "Eurotas Springs") located near the village of
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registered a record mean max temperature of 42.3°C. On August 3, 2021 the
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registered 46.4°C which is the highest temperature ever recorded in the
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The Laconian Alpheios stream is unconnected with the Alpheios river in
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by the subduction of Africa. The spring is also called Logaras Spring.
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just south of the city. The main traffic was southward to the port of
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of Gytheio; 170 km (66 sq mi) of land was ruined.
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revealed that the entire ridge, located in the municipal unit of
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Analysis of bore holes in the valley indicate that in the
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near the river's mouth is particularly fertile farmland.
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During July 2023 the Hydro Meteorological station of the
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are found in its vicinity starting the Archaic period.
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in a northeast-southwest direction. The corresponding
1442:Source 2: Precipitation from Sparta N.O.A station 1433:Source 1: Hydro Meteorological station of Evrotas, 2262:Sparta and Lakonia: A regional history 1300–362 BC 2176: 2149: 2137: 2125: 719:with its coastal islands. Its seat is the city of 711:is a political subdivision of Greece covering the 623:, ancient Therapnē, had been covered by a walled 419:ridge at a locale called Kephalari. The ridge, a 313:. The river is also fed by underwater springs at 2356: 2177:Antonakos, Andreas; Lambrakis, Nicolaos (2000). 2004:: CS1 maint: bot: original URL status unknown ( 1984:"Impressive summer data from the Evrotas Valley" 1489:, created by extensional forces acting over the 365:One etymology derives the word Eurōtas from the 1662: 512: 1647:A Homeric Dictionary for Schools and Colleges 395:The source of the Evrotas River is a surface 2331: 2296:, Institute of Inland Waters, archived from 1669:Bulletin of the Geological Society of Greece 747:The Evrotas Valley enjoys a sunny and warm 615:. In the 20th century a survey by the 276: 2221:The Annual of the British School at Athens 1640: 1551: 1479:The Evrotas River occupies the floor of a 358:are not known to have been present in the 2258: 1721: 703: 407:, by the side of the road ascending from 2247: 2161: 1783: 1771: 1761:(1496). Ministry of Culture and Tourism. 1658: 1656: 675: 337:is 2,239 km (864 sq mi). 1613:Dictionary of Greek and Roman Geography 606: 14: 2357: 1808:Armstrong, Cavanagh & Shipley 1992 1796:Armstrong, Cavanagh & Shipley 1992 1748: 1663:Karalemas, N.; Lekkas, S. (May 2010). 1581:Greece in Figures January - March 2018 317:and by tributaries coursing down from 2227:. British School at Athens: 293–310. 1733: 1653: 1610: 1604: 2046:"World Meteorological Organization" 1594:"Preliminary Flood Risk Assessment" 671: 297:and one of the major rivers of the 224:2,239 km (864 sq mi) 24: 2315: 2290:2nd Progress Report: ENVI Friendly 1821:"Sparta: Greece's heat superpower" 1755:Ephorate of Underwater Antiquities 1611:Smith, William (1857). "Laconia". 575:island on the eastern side of the 25: 2391: 2325: 813:fan aspirated stations network. 803:World Meteorological Organization 373:in Homer. It is, however, in the 1749:Morgan, Catherine (2010-12-07). 1474: 411:. The spring is an outlet of an 45: 2342:from the original on 2021-12-13 2155: 2143: 2131: 2119: 2105: 2059: 2038: 2024:with temperatures reaching 48C" 2020:"Evrotas Valley: The Valley of 2012: 1976: 1955: 1930: 1905: 1884: 1859: 1834: 1813: 1801: 1789: 1777: 1765: 1759:Chronique des fouilles en ligne 1742: 1734:Leake, William Martin (2010) . 1727: 1715: 30:For the river in Thessaly, see 2375:Rivers of Peloponnese (region) 2150:Antonakos & Lambrakis 2000 2138:Antonakos & Lambrakis 2000 2126:Antonakos & Lambrakis 2000 2092:National Observatory of Athens 1942:National Observatory of Athens 1917:National Observatory of Athens 1871:National Observatory of Athens 1846:National Observatory of Athens 1703: 1691: 1679: 1634: 1586: 1574: 1528:of sand and gravel 10–60  1435:National Observatory of Athens 822:National Observatory of Athens 811:National Observatory of Athens 796:National Observatory of Athens 784:National Observatory of Athens 763:and is comparable to areas of 463: 454: 354:. In that legendary time, the 165: • coordinates 13: 1: 2198:10.1016/s0043-1354(00)00160-3 2170: 1363:Average rainfall mm (inches) 617:British School of Archaeology 92:Physical characteristics 644:pottery date from Period I. 513:Legendary pre-Hellenic tribe 507: 380: 340: 204: • elevation 129: • elevation 51:The Evrotas, outside modern 7: 1641:Autenrieth, Georg (2005) . 1501:Massif on the west and the 1153:Mean daily minimum °C (°F) 1013:Mean daily maximum °C (°F) 504:not yet known for certain. 385: 153: • location 110: • location 10: 2396: 2248:Bintliff, John L. (1977). 1938:"Kelefina Air Temperature" 1505:Massif on the east – both 1469: 1449: 1441: 1432: 820:Climate data for Evrotas ( 819: 742: 688:The classical-era city of 470:intermittent and ephemeral 390: 290: 133:430 m (1,410 ft) 29: 2233:10.1017/s0068245400015197 2113:"N.O.A Monthly Bulletins" 1913:"Evrotas Air Temperature" 1867:"Evrotas Air Temperature" 1842:"Evrotas Air Temperature" 1362: 1292: 1222: 1152: 1082: 1012: 942: 872: 867: 864: 861: 858: 855: 852: 849: 846: 843: 840: 837: 834: 831: 828: 496:road to Skala, the Skala- 277: 254: 241: 233: 228: 220: 212: 202: 163: 151: 141: 137: 127: 108: 100: 96: 91: 75: 65: 60: 44: 39: 2259:Cartledge, Paul (2002). 1568: 478: 415:located in the adjacent 256: • right 1710:Skoulikidis et al. 2008 1698:Skoulikidis et al. 2008 1629:Skoulikidis et al. 2008 1552:Recent geologic history 1437:(Mar 2020 - Feb 2024) 569:University of Cambridge 293:) is the main river of 243: • left 216:82 km (51 mi) 1534:hydraulic conductivity 1520:. To the east of that 704:Post-classical Laconia 685: 1686:Description of Greece 1495:fault-block mountains 1223:Mean minimum °C (°F) 943:Mean maximum °C (°F) 749:Mediterranean climate 679: 588:close links with the 423:, is not part of the 187:36.80417°N 22.69583°E 2365:Landforms of Laconia 2152:, pp. 3979–3982 1963:"47.1C Kelefina NOA" 1736:Travels in the Morea 1600:on 15 February 2020. 873:Record high °C (°F) 798:recorded 47.1°C. 637:middle Helladic (MH) 607:Mycenaean Lacedaemon 208:0 m (0 ft) 1892:"47.4C Evrotas NOA" 1293:Record low °C (°F) 1083:Daily mean °C (°F) 633:late Helladic (LH3) 627:town, dated to the 547:Greece is known as 229:Basin features 183: /  2335:Eurotas Canyon III 2332:kaloneroairfield. 2164:, pp. 373–374 1810:, pp. 294–295 1786:, pp. 379–380 1774:, pp. 377–378 686: 635:pottery with some 325:, which flank the 192:36.80417; 22.69583 2192:(16): 3977–3986. 1446: 1445: 801:In July 2023 the 557:Hittite documents 265: 264: 16:(Redirected from 2387: 2370:Rivers of Greece 2351: 2349: 2347: 2310: 2309: 2308: 2302: 2295: 2283: 2281: 2280: 2274: 2267: 2255: 2244: 2215: 2213: 2212: 2206: 2200:. 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741: 713:Evrotas Valley 709:Modern Laconia 705: 702: 673: 670: 654:Greek Dark Age 608: 605: 514: 511: 509: 506: 480: 477: 465: 462: 456: 453: 429:Hellenic Plate 392: 389: 387: 384: 382: 379: 360:Evrotas Valley 342: 339: 335:drainage basin 327:Evrotas Valley 263: 262: 258: 252: 251: 245: 239: 238: 235: 231: 230: 226: 225: 222: 218: 217: 214: 210: 209: 206: 203: 200: 199: 167: 164: 161: 160: 155: 152: 149: 148: 145: 139: 138: 135: 134: 131: 125: 124: 112: 106: 105: 102: 98: 97: 94: 93: 89: 88: 79: 73: 72: 67: 63: 62: 58: 57: 50: 42: 41: 26: 9: 6: 4: 3: 2: 2392: 2381: 2380:Eurotas basin 2378: 2376: 2373: 2371: 2368: 2366: 2363: 2362: 2360: 2341: 2337: 2336: 2330: 2329: 2320: 2319: 2303:on 2011-09-24 2299: 2292: 2291: 2285: 2275:on 2012-03-25 2271: 2264: 2263: 2257: 2253: 2252: 2246: 2242: 2238: 2234: 2230: 2226: 2222: 2217: 2207:on 2012-03-30 2203: 2199: 2195: 2191: 2187: 2180: 2175: 2174: 2163: 2162:Bintliff 1977 2158: 2151: 2146: 2139: 2134: 2127: 2122: 2114: 2108: 2093: 2089: 2083: 2068: 2062: 2047: 2041: 2026:. Notos Press 2025: 2023: 2015: 2007: 2001: 1985: 1979: 1964: 1958: 1943: 1939: 1933: 1918: 1914: 1908: 1893: 1887: 1872: 1868: 1862: 1847: 1843: 1837: 1822: 1816: 1809: 1804: 1798:, p. 301 1797: 1792: 1785: 1784:Bintliff 1977 1780: 1773: 1772:Bintliff 1977 1768: 1760: 1756: 1752: 1745: 1737: 1730: 1723: 1718: 1711: 1706: 1699: 1694: 1687: 1682: 1674: 1670: 1666: 1659: 1657: 1648: 1644: 1637: 1630: 1625: 1623: 1614: 1607: 1599: 1595: 1589: 1582: 1577: 1573: 1566: 1562: 1559: 1549: 1547: 1543: 1539: 1535: 1531: 1527: 1523: 1522:alluvial fans 1519: 1514: 1512: 1508: 1504: 1500: 1496: 1492: 1488: 1487: 1482: 1475:Geomorphology 1467: 1464: 1460: 1458: 1440: 1436: 1431: 1425: 1420: 1415: 1410: 1405: 1400: 1395: 1390: 1385: 1380: 1375: 1370: 1365: 1361: 1355: 1350: 1345: 1340: 1335: 1330: 1325: 1320: 1315: 1310: 1305: 1300: 1295: 1291: 1285: 1280: 1275: 1270: 1265: 1260: 1255: 1250: 1245: 1240: 1235: 1230: 1225: 1221: 1215: 1210: 1205: 1200: 1195: 1190: 1185: 1180: 1175: 1170: 1165: 1160: 1155: 1151: 1145: 1140: 1135: 1130: 1125: 1120: 1115: 1110: 1105: 1100: 1095: 1090: 1085: 1081: 1075: 1070: 1065: 1060: 1055: 1050: 1045: 1040: 1035: 1030: 1025: 1020: 1015: 1011: 1005: 1000: 995: 990: 985: 980: 975: 970: 965: 960: 955: 950: 945: 941: 935: 930: 925: 920: 915: 910: 905: 900: 895: 890: 885: 880: 875: 871: 827: 823: 818: 814: 812: 808: 804: 799: 797: 793: 789: 785: 780: 778: 774: 770: 766: 762: 758: 754: 750: 740: 736: 734: 733:arboriculture 730: 726: 722: 718: 717:Laconian Gulf 714: 710: 701: 699: 695: 691: 683: 678: 669: 665: 663: 659: 655: 651: 645: 643: 638: 634: 630: 626: 622: 618: 614: 604: 601: 599: 598:middle Minoan 595: 591: 585: 582: 578: 577:Laconian Gulf 574: 570: 565: 562: 558: 554: 551:based on the 550: 549:Achaean Greek 546: 542: 538: 536: 532: 528: 524: 520: 505: 501: 499: 495: 491: 487: 476: 473: 471: 461: 452: 450: 446: 441: 438: 432: 430: 426: 422: 418: 414: 410: 406: 402: 398: 378: 376: 375:Ionic dialect 372: 368: 367:ancient Greek 363: 361: 357: 353: 349: 338: 336: 332: 331:Laconian Gulf 328: 324: 320: 316: 312: 308: 304: 300: 296: 288: 287:Ancient Greek 284: 274: 270: 259: 253: 249: 246: 240: 236: 232: 227: 223: 219: 215: 211: 207: 201: 196: 168: 162: 159: 158:Laconian Gulf 156: 150: 146: 144: 140: 136: 132: 126: 123: 119: 116: 113: 107: 103: 99: 95: 90: 87: 83: 80: 78: 74: 71: 68: 64: 59: 54: 48: 43: 38: 33: 19: 2344:. Retrieved 2334: 2305:, retrieved 2298:the original 2289: 2277:. Retrieved 2270:the original 2261: 2250: 2224: 2220: 2209:. Retrieved 2202:the original 2189: 2185: 2157: 2145: 2133: 2121: 2107: 2095:. Retrieved 2082: 2070:. Retrieved 2061: 2049:. Retrieved 2040: 2028:. Retrieved 2021: 2014: 1988:. Retrieved 1978: 1966:. Retrieved 1957: 1945:. Retrieved 1932: 1920:. Retrieved 1907: 1895:. Retrieved 1886: 1874:. Retrieved 1861: 1849:. Retrieved 1836: 1824:. Retrieved 1815: 1803: 1791: 1779: 1767: 1758: 1751:"Pavlopetri" 1744: 1735: 1729: 1724:, p. 17 1717: 1705: 1693: 1685: 1681: 1672: 1668: 1646: 1636: 1612: 1606: 1598:the original 1588: 1576: 1563: 1555: 1515: 1511:normal fault 1484: 1478: 1465: 1461: 1453: 800: 781: 756: 746: 737: 707: 687: 666: 646: 612: 610: 602: 586: 566: 539: 525:king of the 516: 502: 482: 474: 467: 458: 442: 433: 394: 364: 344: 319:Mt. Taygetos 282: 273:Modern Greek 268: 266: 2338:. YouTube. 2072:27 November 2051:27 November 1826:27 November 1688:, 8.44.3-8. 1481:rift valley 805:station in 735:intensely. 729:viticulture 725:agriculture 464:Tributaries 455:Main stream 299:Peloponnese 234:Tributaries 190: / 122:Peloponnese 27:Greek river 2359:Categories 2307:2011-08-16 2279:2011-09-02 2211:2011-08-15 2171:References 592:, western 581:Pavlopetri 573:Elafonisos 535:Lacedaemon 401:Skortsinos 323:Mt. Parnon 311:Skortsinos 221:Basin size 178:22°41′45″E 175:36°48′15″N 32:Titarisios 2346:15 August 2088:"Evrotas" 1643:"εὺρῶεις" 1507:limestone 765:Andalusia 625:Mycenaean 621:Therapnes 541:Mycenaean 523:eponymous 508:Political 449:Pausanias 417:limestone 409:Kyparissi 381:Geography 341:Etymology 2340:Archived 2241:30103513 2097:12 March 2030:19 March 2000:cite web 1990:19 March 1968:12 March 1947:12 March 1922:12 March 1897:12 March 1876:12 March 1851:12 March 1558:Pliocene 1499:Taygetus 1497:are the 1428:(24.76) 1053:(103.6) 1048:(104.9) 1008:(113.5) 988:(105.6) 983:(113.0) 978:(113.5) 973:(108.1) 968:(103.1) 938:(117.3) 923:(103.3) 918:(107.8) 913:(117.3) 908:(116.6) 903:(112.8) 898:(109.0) 769:Taygetus 694:Therapne 682:Taygetus 658:Menelaus 613:Menelaon 590:Cyclades 553:Linear B 494:Gytheion 437:Alpheios 425:Taygetus 386:Physical 250:, Xerias 115:Arcadian 61:Location 1757:: BSA. 1583:, p. 12 1526:aquifer 1470:Geology 1450:Ecology 1423:(3.79) 1418:(3.89) 1413:(2.54) 1408:(1.55) 1403:(0.99) 1398:(0.44) 1393:(1.72) 1388:(0.84) 1383:(1.32) 1378:(2.20) 1373:(1.50) 1368:(3.98) 1358:(20.3) 1353:(27.3) 1348:(31.1) 1343:(42.4) 1338:(46.4) 1333:(59.0) 1328:(54.9) 1323:(48.7) 1318:(42.4) 1313:(30.2) 1308:(27.5) 1303:(22.8) 1298:(20.3) 1288:(25.0) 1283:(31.8) 1278:(35.4) 1273:(45.5) 1268:(51.4) 1263:(59.9) 1258:(58.8) 1253:(51.6) 1248:(44.4) 1243:(35.1) 1238:(29.8) 1233:(25.9) 1228:(25.0) 1218:(49.6) 1213:(41.2) 1208:(45.9) 1203:(52.0) 1198:(59.2) 1193:(64.6) 1188:(64.2) 1183:(59.0) 1178:(51.6) 1173:(44.4) 1168:(38.7) 1163:(37.2) 1158:(37.0) 1148:(66.2) 1143:(53.8) 1138:(60.6) 1133:(69.1) 1128:(77.5) 1123:(84.2) 1118:(84.6) 1113:(77.9) 1108:(70.5) 1103:(61.2) 1098:(53.2) 1093:(52.0) 1088:(50.2) 1078:(82.9) 1073:(66.4) 1068:(75.2) 1063:(86.4) 1058:(95.7) 1043:(97.0) 1038:(89.6) 1033:(77.7) 1028:(67.8) 1023:(66.6) 1018:(63.3) 1003:(77.4) 998:(90.3) 993:(99.5) 963:(90.9) 958:(82.6) 953:(79.7) 948:(76.5) 933:(81.7) 928:(94.1) 893:(97.7) 888:(90.5) 883:(83.7) 878:(77.7) 807:Gytheio 792:Evrotas 788:Evrotas 777:meltemi 743:Climate 698:Gytheio 668:Helen. 650:megaron 631:by the 561:Dorians 531:Eurotas 527:Leleges 445:Arcadia 413:aquifer 405:Arcadia 391:Sources 356:Dorians 315:Pellana 307:Arcadia 295:Laconia 291:Εὐρώτας 283:Eurotas 278:Ευρώτας 269:Evrotas 261:Fteroti 86:Arcadia 82:Laconia 77:Regions 66:Country 40:Evrotas 2239:  1546:horsts 1503:Parnon 1486:graben 829:Month 773:Parnon 761:Greece 753:Köppen 731:, and 721:Sparta 690:Sparta 642:Minoan 559:. The 498:Molaoi 397:spring 333:. Its 303:Greece 237:  213:Length 147:  104:  101:Source 70:Greece 53:Sparta 2301:(PDF) 2294:(PDF) 2273:(PDF) 2266:(PDF) 2237:JSTOR 2205:(PDF) 2182:(PDF) 1673:XLIII 1569:Notes 1518:scree 1483:, or 1426:629.2 1366:101.2 868:Year 662:Helen 594:Crete 543:, or 519:Lelex 490:Skala 479:Delta 421:karst 371:Hades 348:Homer 309:, at 301:, in 281:) or 248:Oenus 143:Mouth 118:Nappe 2348:2011 2099:2024 2074:2023 2053:2023 2032:2024 2022:fire 2006:link 1992:2024 1970:2024 1949:2024 1924:2024 1899:2024 1878:2024 1853:2024 1828:2023 1542:marl 1540:and 1538:clay 1457:Elos 1421:96.3 1416:98.9 1411:64.6 1406:39.3 1401:25.1 1396:11.2 1391:43.6 1386:21.3 1381:33.5 1376:56.0 1371:38.2 1356:−6.5 1351:−2.6 1346:−0.5 1331:15.0 1326:12.7 1311:−1.0 1306:−2.5 1301:−5.1 1296:−6.5 1286:−3.9 1281:−0.1 1266:10.8 1261:15.5 1256:14.9 1251:10.9 1236:−1.2 1231:−3.4 1226:−3.9 1201:11.1 1196:15.1 1191:18.1 1186:17.9 1181:15.0 1176:10.9 1146:19.0 1141:12.1 1136:15.9 1131:20.6 1126:25.3 1121:29.0 1116:29.2 1111:25.5 1106:21.4 1101:16.2 1096:11.8 1091:11.1 1086:10.1 1076:28.3 1071:19.1 1066:24.0 1061:30.2 1056:35.4 1051:39.8 1046:40.5 1041:36.1 1036:32.0 1031:25.4 1026:19.9 1021:19.2 1016:17.4 1006:45.3 1001:25.2 996:32.4 991:37.5 986:40.9 981:45.0 976:45.3 971:42.3 966:39.5 961:32.7 956:28.1 951:26.5 946:24.7 936:47.4 931:27.6 926:34.5 921:39.6 916:42.1 911:47.4 906:47.0 901:44.9 896:42.8 891:36.5 886:32.5 881:28.7 876:25.4 865:Dec 862:Nov 859:Oct 856:Sep 853:Aug 850:Jul 847:Jun 844:May 841:Apr 838:Mar 835:Feb 832:Jan 771:and 660:and 555:and 486:Elos 321:and 267:The 84:and 2229:doi 2194:doi 1341:5.8 1336:8.0 1321:9.3 1316:5.8 1276:1.9 1271:7.5 1246:6.9 1241:1.7 1216:9.8 1211:5.1 1206:7.7 1171:6.9 1166:3.7 1161:2.9 1156:2.8 786:in 757:Csa 2361:: 2235:. 2225:87 2223:. 2190:34 2188:. 2184:. 2090:. 2002:}} 1998:{{ 1940:. 1915:. 1869:. 1844:. 1753:. 1667:. 1655:^ 1645:. 1621:^ 755:: 727:, 521:, 403:, 377:. 289:: 275:: 120:, 2350:. 2311:. 2282:. 2243:. 2231:: 2214:. 2196:: 2115:. 2101:. 2076:. 2055:. 2034:. 2008:) 1994:. 1972:. 1951:. 1926:. 1901:. 1880:. 1855:. 1830:. 1530:m 751:( 684:. 492:- 285:( 271:( 55:. 34:. 20:)

Index

Eurotas (river)
Titarisios

Sparta
Greece
Regions
Laconia
Arcadia
Arcadian
Nappe
Peloponnese
Mouth
Laconian Gulf
36°48′15″N 22°41′45″E / 36.80417°N 22.69583°E / 36.80417; 22.69583
Oenus
Modern Greek
Ancient Greek
Laconia
Peloponnese
Greece
Arcadia
Skortsinos
Pellana
Mt. Taygetos
Mt. Parnon
Evrotas Valley
Laconian Gulf
drainage basin
Homer
Mycenaean Greece

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