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Evrotas (river)

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666: 641:-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 36: 449:
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
440:, one of the best ancient geographers. He believed they had the same source but that the outflow stream disappeared into a chasm only to emerge at different locations as different streams. In the most exaggerated form of the myth, the Alpheios continues under the Mediterranean to Sicily or elsewhere. 428:
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.
2190: 589:. 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. 712:, 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 461:. 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. 1513:
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".
436:. The identity of their names comes from an ancient geologic misunderstanding that the Eurotas and the Apheios were connected underground, which deceived even 2008: 1994: 518:, 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 1533:
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
605: 65: 458: 2328: 1727:. Cambridge Library collection. Cambridge; New York, NY: Cambridge University Press. p. 196. 557: 522:, the last of the line. The latter had a daughter, Sparta, but no sons. An outsider married her, 433: 393: 295: 103: 74: 2257:. Taylor & Francis e-Library. London and New York: Routledge. pp. 13–14. Archived from 585:
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
1585:(in Greek). Ministry of Environment, Energy and Climate Change. p. 46. Archived from 1498:
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: 630: 351:. At some time prior to being called Evrotas, the river was the Bomycas and the Himeras. 2225: 2186: 1739: 748:). The interior of the valley records the highest summer mean maximum temperatures in 645:, reduced to the Menelaon shrine in the Archaic and Classical Periods. Dedications to 2055: 1988: 2217: 2182: 689:, which was the most convenient outlet. All others involved a trek over mountains. 613: 537: 529: 340: 294:. The river's springs are located just northwest of the border between Laconia and 388:
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
1431:Source 2: Precipitation from Sparta N.O.A station 1422:Source 1: Hydro Meteorological station of Evrotas, 2251:Sparta and Lakonia: A regional history 1300–362 BC 2165: 2138: 2126: 2114: 708:with its coastal islands. Its seat is the city of 700:is a political subdivision of Greece covering the 612:, ancient Therapnē, had been covered by a walled 408:ridge at a locale called Kephalari. The ridge, a 302:. The river is also fed by underwater springs at 2345: 2166:Antonakos, Andreas; Lambrakis, Nicolaos (2000). 1993:: CS1 maint: bot: original URL status unknown ( 1973:"Impressive summer data from the Evrotas Valley" 1478:, created by extensional forces acting over the 354:One etymology derives the word Eurōtas from the 1651: 501: 1636:A Homeric Dictionary for Schools and Colleges 384:The source of the Evrotas River is a surface 2320: 2285:, Institute of Inland Waters, archived from 1658:Bulletin of the Geological Society of Greece 736:The Evrotas Valley enjoys a sunny and warm 604:. In the 20th century a survey by the 265: 2210:The Annual of the British School at Athens 1629: 1540: 1468:The Evrotas River occupies the floor of a 347:are not known to have been present in the 2247: 1710: 692: 396:, by the side of the road ascending from 2236: 2150: 1772: 1760: 1750:(1496). Ministry of Culture and Tourism. 1647: 1645: 664: 326:is 2,239 km (864 sq mi). 1602:Dictionary of Greek and Roman Geography 595: 2346: 1797:Armstrong, Cavanagh & Shipley 1992 1785:Armstrong, Cavanagh & Shipley 1992 1737: 1652:Karalemas, N.; Lekkas, S. (May 2010). 1570:Greece in Figures January - March 2018 306:and by tributaries coursing down from 2216:. British School at Athens: 293–310. 1722: 1642: 1599: 1593: 2035:"World Meteorological Organization" 1583:"Preliminary Flood Risk Assessment" 660: 286:and one of the major rivers of the 213:2,239 km (864 sq mi) 13: 2304: 2279:2nd Progress Report: ENVI Friendly 1810:"Sparta: Greece's heat superpower" 1744:Ephorate of Underwater Antiquities 1600:Smith, William (1857). "Laconia". 564:island on the eastern side of the 14: 2380: 2314: 802:fan aspirated stations network. 792:World Meteorological Organization 362:in Homer. It is, however, in the 1738:Morgan, Catherine (2010-12-07). 1463: 400:. The spring is an outlet of an 34: 2331:from the original on 2021-12-13 2144: 2132: 2120: 2108: 2094: 2048: 2027: 2013:with temperatures reaching 48C" 2009:"Evrotas Valley: The Valley of 2001: 1965: 1944: 1919: 1894: 1873: 1848: 1823: 1802: 1790: 1778: 1766: 1754: 1748:Chronique des fouilles en ligne 1731: 1723:Leake, William Martin (2010) . 1716: 1704: 19:For the river in Thessaly, see 2364:Rivers of Peloponnese (region) 2139:Antonakos & Lambrakis 2000 2127:Antonakos & Lambrakis 2000 2115:Antonakos & Lambrakis 2000 2081:National Observatory of Athens 1931:National Observatory of Athens 1906:National Observatory of Athens 1860:National Observatory of Athens 1835:National Observatory of Athens 1692: 1680: 1668: 1623: 1575: 1563: 1517:of sand and gravel 10–60  1424:National Observatory of Athens 811:National Observatory of Athens 800:National Observatory of Athens 785:National Observatory of Athens 773:National Observatory of Athens 752:and is comparable to areas of 452: 443: 343:. In that legendary time, the 154: • coordinates 1: 2187:10.1016/s0043-1354(00)00160-3 2159: 1352:Average rainfall mm (inches) 606:British School of Archaeology 81:Physical characteristics 633:pottery date from Period I. 502:Legendary pre-Hellenic tribe 496: 369: 329: 193: • elevation 118: • elevation 40:The Evrotas, outside modern 7: 1630:Autenrieth, Georg (2005) . 1490:Massif on the west and the 1142:Mean daily minimum °C (°F) 1002:Mean daily maximum °C (°F) 493:not yet known for certain. 374: 142: • location 99: • location 10: 2385: 2237:Bintliff, John L. (1977). 1927:"Kelefina Air Temperature" 1494:Massif on the east – both 1458: 1438: 1430: 1421: 809:Climate data for Evrotas ( 808: 731: 677:The classical-era city of 459:intermittent and ephemeral 379: 279: 122:430 m (1,410 ft) 18: 2222:10.1017/s0068245400015197 2102:"N.O.A Monthly Bulletins" 1902:"Evrotas Air Temperature" 1856:"Evrotas Air Temperature" 1831:"Evrotas Air Temperature" 1351: 1281: 1211: 1141: 1071: 1001: 931: 861: 856: 853: 850: 847: 844: 841: 838: 835: 832: 829: 826: 823: 820: 817: 485:road to Skala, the Skala- 266: 243: 230: 222: 217: 209: 201: 191: 152: 140: 130: 126: 116: 97: 89: 85: 80: 64: 54: 49: 33: 28: 2248:Cartledge, Paul (2002). 1557: 467: 404:located in the adjacent 245: • right 1699:Skoulikidis et al. 2008 1687:Skoulikidis et al. 2008 1618:Skoulikidis et al. 2008 1541:Recent geologic history 1426:(Mar 2020 - Feb 2024) 558:University of Cambridge 282:) is the main river of 232: • left 205:82 km (51 mi) 1523:hydraulic conductivity 1509:. To the east of that 693:Post-classical Laconia 674: 1675:Description of Greece 1484:fault-block mountains 1212:Mean minimum °C (°F) 932:Mean maximum °C (°F) 738:Mediterranean climate 668: 577:close links with the 412:, is not part of the 176:36.80417°N 22.69583°E 2354:Landforms of Laconia 2141:, pp. 3979–3982 1952:"47.1C Kelefina NOA" 1725:Travels in the Morea 1589:on 15 February 2020. 862:Record high °C (°F) 787:recorded 47.1°C. 626:middle Helladic (MH) 596:Mycenaean Lacedaemon 197:0 m (0 ft) 1881:"47.4C Evrotas NOA" 1282:Record low °C (°F) 1072:Daily mean °C (°F) 622:late Helladic (LH3) 616:town, dated to the 536:Greece is known as 218:Basin features 172: /  2324:Eurotas Canyon III 2321:kaloneroairfield. 2153:, pp. 373–374 1799:, pp. 294–295 1775:, pp. 379–380 1763:, pp. 377–378 675: 624:pottery with some 314:, which flank the 181:36.80417; 22.69583 2181:(16): 3977–3986. 1435: 1434: 790:In July 2023 the 546:Hittite documents 254: 253: 2376: 2359:Rivers of Greece 2340: 2338: 2336: 2299: 2298: 2297: 2291: 2284: 2272: 2270: 2269: 2263: 2256: 2244: 2233: 2204: 2202: 2201: 2195: 2189:. Archived from 2172: 2154: 2148: 2142: 2136: 2130: 2124: 2118: 2112: 2106: 2105: 2098: 2092: 2091: 2089: 2087: 2073: 2067: 2066: 2064: 2062: 2056:"Gytheio record" 2052: 2046: 2045: 2043: 2041: 2031: 2025: 2024: 2022: 2020: 2005: 1999: 1998: 1992: 1984: 1982: 1980: 1969: 1963: 1962: 1960: 1958: 1948: 1942: 1941: 1939: 1937: 1923: 1917: 1916: 1914: 1912: 1898: 1892: 1891: 1889: 1887: 1877: 1871: 1870: 1868: 1866: 1852: 1846: 1845: 1843: 1841: 1827: 1821: 1820: 1818: 1816: 1806: 1800: 1794: 1788: 1782: 1776: 1770: 1764: 1758: 1752: 1751: 1735: 1729: 1728: 1720: 1714: 1708: 1702: 1696: 1690: 1684: 1678: 1672: 1666: 1665: 1649: 1640: 1639: 1627: 1621: 1615: 1606: 1605: 1597: 1591: 1590: 1579: 1573: 1567: 806: 805: 661:Classical Sparta 341:Mycenaean Greece 281: 269: 268: 246: 233: 187: 186: 184: 183: 182: 177: 173: 170: 169: 168: 165: 119: 100: 38: 26: 25: 2384: 2383: 2379: 2378: 2377: 2375: 2374: 2373: 2344: 2343: 2334: 2332: 2317: 2307: 2305:Further reading 2295: 2293: 2289: 2282: 2267: 2265: 2261: 2254: 2199: 2197: 2193: 2170: 2162: 2157: 2149: 2145: 2137: 2133: 2125: 2121: 2113: 2109: 2100: 2099: 2095: 2085: 2083: 2075: 2074: 2070: 2060: 2058: 2054: 2053: 2049: 2039: 2037: 2033: 2032: 2028: 2018: 2016: 2007: 2006: 2002: 1986: 1985: 1978: 1976: 1971: 1970: 1966: 1956: 1954: 1950: 1949: 1945: 1935: 1933: 1925: 1924: 1920: 1910: 1908: 1900: 1899: 1895: 1885: 1883: 1879: 1878: 1874: 1864: 1862: 1854: 1853: 1849: 1839: 1837: 1829: 1828: 1824: 1814: 1812: 1808: 1807: 1803: 1795: 1791: 1783: 1779: 1771: 1767: 1759: 1755: 1736: 1732: 1721: 1717: 1709: 1705: 1697: 1693: 1689:, Introduction. 1685: 1681: 1673: 1669: 1664:(4): 1707–1715. 1650: 1643: 1628: 1624: 1616: 1609: 1598: 1594: 1581: 1580: 1576: 1568: 1564: 1560: 1543: 1466: 1461: 1441: 1436: 1416: 1411: 1406: 1401: 1396: 1391: 1386: 1381: 1376: 1371: 1366: 1361: 1356: 1346: 1341: 1336: 1331: 1326: 1321: 1316: 1311: 1306: 1301: 1296: 1291: 1286: 1276: 1271: 1266: 1261: 1256: 1251: 1246: 1241: 1236: 1231: 1226: 1221: 1216: 1206: 1201: 1196: 1191: 1186: 1181: 1176: 1171: 1166: 1161: 1156: 1151: 1146: 1136: 1131: 1126: 1121: 1116: 1111: 1106: 1101: 1096: 1091: 1086: 1081: 1076: 1066: 1061: 1056: 1051: 1046: 1041: 1036: 1031: 1026: 1021: 1016: 1011: 1006: 996: 991: 986: 981: 976: 971: 966: 961: 956: 951: 946: 941: 936: 926: 921: 916: 911: 906: 901: 896: 891: 886: 881: 876: 871: 866: 813:) 224 m a.s.l. 734: 695: 663: 618:late Bronze Age 598: 534:late Bronze Age 504: 499: 470: 455: 446: 382: 377: 372: 332: 244: 231: 194: 180: 178: 174: 171: 166: 163: 161: 159: 158: 155: 143: 117: 98: 45: 24: 17: 12: 11: 5: 2382: 2372: 2371: 2366: 2361: 2356: 2342: 2341: 2316: 2315:External links 2313: 2312: 2311: 2306: 2303: 2302: 2301: 2273: 2245: 2234: 2205: 2175:Water Research 2161: 2158: 2156: 2155: 2143: 2131: 2129:, p. 3978 2119: 2117:, p. 3982 2107: 2093: 2068: 2047: 2026: 2000: 1964: 1943: 1918: 1893: 1872: 1847: 1822: 1801: 1789: 1777: 1765: 1753: 1730: 1715: 1711:Cartledge 2002 1703: 1701:, Section 3.1. 1691: 1679: 1667: 1641: 1622: 1620:, Section 3.2. 1607: 1592: 1574: 1561: 1559: 1556: 1542: 1539: 1480:Hellenic Plate 1465: 1462: 1460: 1457: 1440: 1437: 1433: 1432: 1428: 1427: 1419: 1418: 1413: 1408: 1403: 1398: 1393: 1388: 1383: 1378: 1373: 1368: 1363: 1358: 1353: 1349: 1348: 1343: 1338: 1333: 1328: 1323: 1318: 1313: 1308: 1303: 1298: 1293: 1288: 1283: 1279: 1278: 1273: 1268: 1263: 1258: 1253: 1248: 1243: 1238: 1233: 1228: 1223: 1218: 1213: 1209: 1208: 1203: 1198: 1193: 1188: 1183: 1178: 1173: 1168: 1163: 1158: 1153: 1148: 1143: 1139: 1138: 1133: 1128: 1123: 1118: 1113: 1108: 1103: 1098: 1093: 1088: 1083: 1078: 1073: 1069: 1068: 1063: 1058: 1053: 1048: 1043: 1038: 1033: 1028: 1023: 1018: 1013: 1008: 1003: 999: 998: 993: 988: 983: 978: 973: 968: 963: 958: 953: 948: 943: 938: 933: 929: 928: 923: 918: 913: 908: 903: 898: 893: 888: 883: 878: 873: 868: 863: 859: 858: 855: 852: 849: 846: 843: 840: 837: 834: 831: 828: 825: 822: 819: 815: 814: 804: 733: 730: 702:Evrotas Valley 698:Modern Laconia 694: 691: 662: 659: 643:Greek Dark Age 597: 594: 503: 500: 498: 495: 469: 466: 454: 451: 445: 442: 418:Hellenic Plate 381: 378: 376: 373: 371: 368: 349:Evrotas Valley 331: 328: 324:drainage basin 316:Evrotas Valley 252: 251: 247: 241: 240: 234: 228: 227: 224: 220: 219: 215: 214: 211: 207: 206: 203: 199: 198: 195: 192: 189: 188: 156: 153: 150: 149: 144: 141: 138: 137: 134: 128: 127: 124: 123: 120: 114: 113: 101: 95: 94: 91: 87: 86: 83: 82: 78: 77: 68: 62: 61: 56: 52: 51: 47: 46: 39: 31: 30: 15: 9: 6: 4: 3: 2: 2381: 2370: 2369:Eurotas basin 2367: 2365: 2362: 2360: 2357: 2355: 2352: 2351: 2349: 2330: 2326: 2325: 2319: 2318: 2309: 2308: 2292:on 2011-09-24 2288: 2281: 2280: 2274: 2264:on 2012-03-25 2260: 2253: 2252: 2246: 2242: 2241: 2235: 2231: 2227: 2223: 2219: 2215: 2211: 2206: 2196:on 2012-03-30 2192: 2188: 2184: 2180: 2176: 2169: 2164: 2163: 2152: 2151:Bintliff 1977 2147: 2140: 2135: 2128: 2123: 2116: 2111: 2103: 2097: 2082: 2078: 2072: 2057: 2051: 2036: 2030: 2015:. Notos Press 2014: 2012: 2004: 1996: 1990: 1974: 1968: 1953: 1947: 1932: 1928: 1922: 1907: 1903: 1897: 1882: 1876: 1861: 1857: 1851: 1836: 1832: 1826: 1811: 1805: 1798: 1793: 1787:, p. 301 1786: 1781: 1774: 1773:Bintliff 1977 1769: 1762: 1761:Bintliff 1977 1757: 1749: 1745: 1741: 1734: 1726: 1719: 1712: 1707: 1700: 1695: 1688: 1683: 1676: 1671: 1663: 1659: 1655: 1648: 1646: 1637: 1633: 1626: 1619: 1614: 1612: 1603: 1596: 1588: 1584: 1578: 1571: 1566: 1562: 1555: 1551: 1548: 1538: 1536: 1532: 1528: 1524: 1520: 1516: 1512: 1511:alluvial fans 1508: 1503: 1501: 1497: 1493: 1489: 1485: 1481: 1477: 1476: 1471: 1464:Geomorphology 1456: 1453: 1449: 1447: 1429: 1425: 1420: 1414: 1409: 1404: 1399: 1394: 1389: 1384: 1379: 1374: 1369: 1364: 1359: 1354: 1350: 1344: 1339: 1334: 1329: 1324: 1319: 1314: 1309: 1304: 1299: 1294: 1289: 1284: 1280: 1274: 1269: 1264: 1259: 1254: 1249: 1244: 1239: 1234: 1229: 1224: 1219: 1214: 1210: 1204: 1199: 1194: 1189: 1184: 1179: 1174: 1169: 1164: 1159: 1154: 1149: 1144: 1140: 1134: 1129: 1124: 1119: 1114: 1109: 1104: 1099: 1094: 1089: 1084: 1079: 1074: 1070: 1064: 1059: 1054: 1049: 1044: 1039: 1034: 1029: 1024: 1019: 1014: 1009: 1004: 1000: 994: 989: 984: 979: 974: 969: 964: 959: 954: 949: 944: 939: 934: 930: 924: 919: 914: 909: 904: 899: 894: 889: 884: 879: 874: 869: 864: 860: 816: 812: 807: 803: 801: 797: 793: 788: 786: 782: 778: 774: 769: 767: 763: 759: 755: 751: 747: 743: 739: 729: 725: 723: 722:arboriculture 719: 715: 711: 707: 706:Laconian Gulf 703: 699: 690: 688: 684: 680: 672: 667: 658: 654: 652: 648: 644: 640: 634: 632: 627: 623: 619: 615: 611: 607: 603: 593: 590: 588: 587:middle Minoan 584: 580: 574: 571: 567: 566:Laconian Gulf 563: 559: 554: 551: 547: 543: 540:based on the 539: 538:Achaean Greek 535: 531: 527: 525: 521: 517: 513: 509: 494: 490: 488: 484: 480: 476: 465: 462: 460: 450: 441: 439: 435: 430: 427: 421: 419: 415: 411: 407: 403: 399: 395: 391: 387: 367: 365: 364:Ionic dialect 361: 357: 356:ancient Greek 352: 350: 346: 342: 338: 327: 325: 321: 320:Laconian Gulf 317: 313: 309: 305: 301: 297: 293: 289: 285: 277: 276:Ancient Greek 273: 263: 259: 248: 242: 238: 235: 229: 225: 221: 216: 212: 208: 204: 200: 196: 190: 185: 157: 151: 148: 147:Laconian Gulf 145: 139: 135: 133: 129: 125: 121: 115: 112: 108: 105: 102: 96: 92: 88: 84: 79: 76: 72: 69: 67: 63: 60: 57: 53: 48: 43: 37: 32: 27: 22: 2333:. Retrieved 2323: 2294:, retrieved 2287:the original 2278: 2266:. Retrieved 2259:the original 2250: 2239: 2213: 2209: 2198:. Retrieved 2191:the original 2178: 2174: 2146: 2134: 2122: 2110: 2096: 2084:. Retrieved 2071: 2059:. Retrieved 2050: 2038:. Retrieved 2029: 2017:. Retrieved 2010: 2003: 1977:. Retrieved 1967: 1955:. Retrieved 1946: 1934:. Retrieved 1921: 1909:. Retrieved 1896: 1884:. Retrieved 1875: 1863:. Retrieved 1850: 1838:. Retrieved 1825: 1813:. Retrieved 1804: 1792: 1780: 1768: 1756: 1747: 1740:"Pavlopetri" 1733: 1724: 1718: 1713:, p. 17 1706: 1694: 1682: 1674: 1670: 1661: 1657: 1635: 1625: 1601: 1595: 1587:the original 1577: 1565: 1552: 1544: 1504: 1500:normal fault 1473: 1467: 1454: 1450: 1442: 789: 770: 745: 735: 726: 696: 676: 655: 635: 601: 599: 591: 575: 555: 528: 514:king of the 505: 491: 471: 463: 456: 447: 431: 422: 383: 353: 333: 308:Mt. Taygetos 271: 262:Modern Greek 257: 255: 2327:. YouTube. 2061:27 November 2040:27 November 1815:27 November 1677:, 8.44.3-8. 1470:rift valley 794:station in 724:intensely. 718:viticulture 714:agriculture 453:Tributaries 444:Main stream 288:Peloponnese 223:Tributaries 179: / 111:Peloponnese 16:Greek river 2348:Categories 2296:2011-08-16 2268:2011-09-02 2200:2011-08-15 2160:References 581:, western 570:Pavlopetri 562:Elafonisos 524:Lacedaemon 390:Skortsinos 312:Mt. Parnon 300:Skortsinos 210:Basin size 167:22°41′45″E 164:36°48′15″N 21:Titarisios 2335:15 August 2077:"Evrotas" 1632:"εὺρῶεις" 1496:limestone 754:Andalusia 614:Mycenaean 610:Therapnes 530:Mycenaean 512:eponymous 497:Political 438:Pausanias 406:limestone 398:Kyparissi 370:Geography 330:Etymology 2329:Archived 2230:30103513 2086:12 March 2019:19 March 1989:cite web 1979:19 March 1957:12 March 1936:12 March 1911:12 March 1886:12 March 1865:12 March 1840:12 March 1547:Pliocene 1488:Taygetus 1486:are the 1417:(24.76) 1042:(103.6) 1037:(104.9) 997:(113.5) 977:(105.6) 972:(113.0) 967:(113.5) 962:(108.1) 957:(103.1) 927:(117.3) 912:(103.3) 907:(107.8) 902:(117.3) 897:(116.6) 892:(112.8) 887:(109.0) 758:Taygetus 683:Therapne 671:Taygetus 647:Menelaus 602:Menelaon 579:Cyclades 542:Linear B 483:Gytheion 426:Alpheios 414:Taygetus 375:Physical 239:, Xerias 104:Arcadian 50:Location 1746:: BSA. 1572:, p. 12 1515:aquifer 1459:Geology 1439:Ecology 1412:(3.79) 1407:(3.89) 1402:(2.54) 1397:(1.55) 1392:(0.99) 1387:(0.44) 1382:(1.72) 1377:(0.84) 1372:(1.32) 1367:(2.20) 1362:(1.50) 1357:(3.98) 1347:(20.3) 1342:(27.3) 1337:(31.1) 1332:(42.4) 1327:(46.4) 1322:(59.0) 1317:(54.9) 1312:(48.7) 1307:(42.4) 1302:(30.2) 1297:(27.5) 1292:(22.8) 1287:(20.3) 1277:(25.0) 1272:(31.8) 1267:(35.4) 1262:(45.5) 1257:(51.4) 1252:(59.9) 1247:(58.8) 1242:(51.6) 1237:(44.4) 1232:(35.1) 1227:(29.8) 1222:(25.9) 1217:(25.0) 1207:(49.6) 1202:(41.2) 1197:(45.9) 1192:(52.0) 1187:(59.2) 1182:(64.6) 1177:(64.2) 1172:(59.0) 1167:(51.6) 1162:(44.4) 1157:(38.7) 1152:(37.2) 1147:(37.0) 1137:(66.2) 1132:(53.8) 1127:(60.6) 1122:(69.1) 1117:(77.5) 1112:(84.2) 1107:(84.6) 1102:(77.9) 1097:(70.5) 1092:(61.2) 1087:(53.2) 1082:(52.0) 1077:(50.2) 1067:(82.9) 1062:(66.4) 1057:(75.2) 1052:(86.4) 1047:(95.7) 1032:(97.0) 1027:(89.6) 1022:(77.7) 1017:(67.8) 1012:(66.6) 1007:(63.3) 992:(77.4) 987:(90.3) 982:(99.5) 952:(90.9) 947:(82.6) 942:(79.7) 937:(76.5) 922:(81.7) 917:(94.1) 882:(97.7) 877:(90.5) 872:(83.7) 867:(77.7) 796:Gytheio 781:Evrotas 777:Evrotas 766:meltemi 732:Climate 687:Gytheio 657:Helen. 639:megaron 620:by the 550:Dorians 520:Eurotas 516:Leleges 434:Arcadia 402:aquifer 394:Arcadia 380:Sources 345:Dorians 304:Pellana 296:Arcadia 284:Laconia 280:Εὐρώτας 272:Eurotas 267:Ευρώτας 258:Evrotas 250:Fteroti 75:Arcadia 71:Laconia 66:Regions 55:Country 29:Evrotas 2228:  1535:horsts 1492:Parnon 1475:graben 818:Month 762:Parnon 750:Greece 742:Köppen 720:, and 710:Sparta 679:Sparta 631:Minoan 548:. The 487:Molaoi 386:spring 322:. Its 292:Greece 226:  202:Length 136:  93:  90:Source 59:Greece 42:Sparta 2290:(PDF) 2283:(PDF) 2262:(PDF) 2255:(PDF) 2226:JSTOR 2194:(PDF) 2171:(PDF) 1662:XLIII 1558:Notes 1507:scree 1472:, or 1415:629.2 1355:101.2 857:Year 651:Helen 583:Crete 532:, or 508:Lelex 479:Skala 468:Delta 410:karst 360:Hades 337:Homer 298:, at 290:, in 270:) or 237:Oenus 132:Mouth 107:Nappe 2337:2011 2088:2024 2063:2023 2042:2023 2021:2024 2011:fire 1995:link 1981:2024 1959:2024 1938:2024 1913:2024 1888:2024 1867:2024 1842:2024 1817:2023 1531:marl 1529:and 1527:clay 1446:Elos 1410:96.3 1405:98.9 1400:64.6 1395:39.3 1390:25.1 1385:11.2 1380:43.6 1375:21.3 1370:33.5 1365:56.0 1360:38.2 1345:−6.5 1340:−2.6 1335:−0.5 1320:15.0 1315:12.7 1300:−1.0 1295:−2.5 1290:−5.1 1285:−6.5 1275:−3.9 1270:−0.1 1255:10.8 1250:15.5 1245:14.9 1240:10.9 1225:−1.2 1220:−3.4 1215:−3.9 1190:11.1 1185:15.1 1180:18.1 1175:17.9 1170:15.0 1165:10.9 1135:19.0 1130:12.1 1125:15.9 1120:20.6 1115:25.3 1110:29.0 1105:29.2 1100:25.5 1095:21.4 1090:16.2 1085:11.8 1080:11.1 1075:10.1 1065:28.3 1060:19.1 1055:24.0 1050:30.2 1045:35.4 1040:39.8 1035:40.5 1030:36.1 1025:32.0 1020:25.4 1015:19.9 1010:19.2 1005:17.4 995:45.3 990:25.2 985:32.4 980:37.5 975:40.9 970:45.0 965:45.3 960:42.3 955:39.5 950:32.7 945:28.1 940:26.5 935:24.7 925:47.4 920:27.6 915:34.5 910:39.6 905:42.1 900:47.4 895:47.0 890:44.9 885:42.8 880:36.5 875:32.5 870:28.7 865:25.4 854:Dec 851:Nov 848:Oct 845:Sep 842:Aug 839:Jul 836:Jun 833:May 830:Apr 827:Mar 824:Feb 821:Jan 760:and 649:and 544:and 475:Elos 310:and 256:The 73:and 2218:doi 2183:doi 1330:5.8 1325:8.0 1310:9.3 1305:5.8 1265:1.9 1260:7.5 1235:6.9 1230:1.7 1205:9.8 1200:5.1 1195:7.7 1160:6.9 1155:3.7 1150:2.9 1145:2.8 775:in 746:Csa 2350:: 2224:. 2214:87 2212:. 2179:34 2177:. 2173:. 2079:. 1991:}} 1987:{{ 1929:. 1904:. 1858:. 1833:. 1742:. 1656:. 1644:^ 1634:. 1610:^ 744:: 716:, 510:, 392:, 366:. 278:: 264:: 109:, 2339:. 2300:. 2271:. 2232:. 2220:: 2203:. 2185:: 2104:. 2090:. 2065:. 2044:. 2023:. 1997:) 1983:. 1961:. 1940:. 1915:. 1890:. 1869:. 1844:. 1819:. 1519:m 740:( 673:. 481:- 274:( 260:( 44:. 23:.

Index

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
Dorians

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