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Salar de Uyuni

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650: 931: 901: 307: 825: 636: 955: 2258: 46: 402: 669: 560: 62: 622: 779: 2075: 967: 919: 424: 607: 943: 579: 818:, who believed Bolivia would flourish with a good transport system, but it was also constantly sabotaged by the local Aymara indigenous Indians who saw it as an intrusion into their lives. The trains were mostly used by the mining companies. In the 1940s, the mining industry collapsed, partly because of mineral depletion. Many trains were abandoned, producing the train cemetery. There are proposals to build a museum from the cemetery. 277: 593: 865:) for ultraviolet light is relatively high at 0.69 and shows variations of only a few percent during the daytime. The combination of all these features makes Salar de Uyuni about five times better for satellite calibration than the surface of an ocean. Using Salar de Uyuni as the target, ICESat has already achieved the short-term elevation measurement accuracy of below 2 centimeters (0.79 in). 69: 857:
April to November, due to the absence of industry and its high elevation, the skies above Salar de Uyuni are very clear, and the air is dry (relative humidity is about 30%; rainfall is roughly 1 millimetre or 0.039 inches per month). It has a stable surface, smoothed by seasonal flooding — water dissolves the salt surface and thus keeps it leveled.
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low and constant throughout the year at 30% to 45%. The rainfall is also low at 1 to 3 mm (0.039 to 0.118 in) per month between April and November, but it may increase up to 80 mm (3.1 in) in January. However, except for January, even in the rainy season the number of rainy days is fewer than 5 per month.
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As a result, the variation in the surface elevation over the 10,582-square-kilometer (4,086 sq mi) area of Salar de Uyuni is less than 1 meter (3 ft 3 in) normal to the Earth's circumference, and there are few square kilometers on Earth that are as flat. The surface reflectivity
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Salt flats are ideal for calibrating the distance measurement equipment of satellites because they are large, stable surfaces with strong reflection, similar to that of ice sheets. As the largest salt flat on Earth, Salar de Uyuni is especially suitable for this purpose. In the low-rain period from
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The area has a relatively stable average temperature with a peak at 21 °C (70 °F) in November to January, and a low of 13 °C (55 °F) in June. The nights are cold all through the year, with temperatures between −9 and 5 °C (16 and 41 °F). The relative humidity is rather
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Sudden rains leave a layer of dead calm water just an inch deep, turning the salt flat into a natural wonder: the world's largest mirror, eighty miles across. At night, the landscape is transformed again into a 360-degree starscape. This dazzling show is only possible because the Salar de Uyuni is
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The Salar was formed as a result of transformations between several prehistoric lakes that existed around forty thousand years ago but had all evaporated over time. It is now covered by a few meters of salt crust, which has an extraordinary flatness with the average elevation variations within one
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images, and still in the same places decades later), and a moat around the periphery that is 1–3 kilometers (0.6–2 mi) wide and 20 to 50 centimetres (8 to 20 in) deep. They originate from the variation in material density, and thus the gravitational force, beneath the Salar's sediments.
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One major tourist attraction is an antique train cemetery. It is 3 km (1.9 mi) outside Uyuni and is connected to it by the old train tracks. The town served in the past as a distribution hub for the trains carrying minerals en route to Pacific Ocean ports. The rail lines were built by
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Salar de Uyuni is a popular tourist destination, and consequently a number of hotels have been built in the area. Due to lack of conventional construction materials, many of them are almost entirely (walls, roof, furniture) built with salt blocks cut from the Salar. The first such hotel, named
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satellite and confirmed in ground drilling tests. Following those findings, an American-based international corporation has invested $ 137 million to developing lithium extraction. However, lithium extraction in the 1980s and 1990s by foreign companies met strong opposition from the local
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having a maximal depth of 140 meters (460 ft), and an estimated age of 13,000 to 18,000 or 14,900 to 26,100 years, depending on the source. The youngest prehistoric lake was Coipasa, which was radiocarbon dated to 11,500 to 13,400 years ago. When it dried, it left behind two modern lakes,
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in water. It is covered with a solid salt crust varying in thickness between tens of centimeters and a few meters. The center of the Salar contains a few islands, which are the remains of the tops of ancient volcanoes submerged during the era of Lake Minchin. They include unusual and fragile
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No mining plant is currently at the site, and the Bolivian government does not want to allow exploitation by foreign corporations. Instead, it intends to reach an annual production of 35,000 t by 2023 in a joint venture with ACI Systems Alemania GmbH.
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of Bolivia in South America. The Altiplano is a high plateau, which was formed during uplift of the Andes mountains. The plateau includes fresh and saltwater lakes as well as salt flats and is surrounded by mountains with no drainage outlets.
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Salar de Uyuni is estimated to contain 10 billion tonnes (9.8 billion long tons; 11 billion short tons) of salt, of which less than 25,000 t is extracted annually. All miners working in the Salar belong to
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Fatal incidents have occurred at the salt flat as a result of poorly maintained vehicles, untrained drivers, speeding, a disregard for the inhospitable conditions, and lack of regulation for tour companies.
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community. Locals believed that the money infused by mining would not reach them. The lithium in the salt flats contains more impurities, and the wet climate and high altitude make it harder to process.
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British engineers arriving near the end of the 19th century and formed a sizeable community in Uyuni. The engineers were invited by the British-sponsored Antofagasta and Bolivia Railway Companies, now
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Science and technology for development: prospects entering the twenty-first century : a symposium in commemoration of the twenty-fifth anniversary of the U.S. Agency for International Development
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The geological history of the Salar is associated with a sequential transformation between several vast lakes. Some 30,000 to 42,000 years ago, the area was part of a giant prehistoric lake,
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can be loosely translated as a salt flat with enclosures, the latter possibly referring to the "islands" of the Salar; or as "salt-flat at Uyuni (the town named 'pen for animals')".
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body lying under the brine; however, the liquid brine is easier to extract, by boring into the crust and pumping out the brine. The brine distribution has been monitored by the
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National Research Council (U.S.). Board on Science and Technology for International Development, National Research Council (U.S.). Office of International Affairs (1988).
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During the rainy season (December to April) the flat turns into a shallow lake and becomes the world's largest natural mirror, featuring a stunning reflection to the sky.
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of Earth observation satellites. Following rain, a thin layer of dead calm water transforms the flat into the world's largest mirror, 129 km (80 mi) across.
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Lithium is concentrated in the brine under the salt crust at a relatively high concentration of about 0.3%. It is also present in the top layers of the porous
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Around 2007, a new hotel was built, under the name Palacio de Sal, in a new location at the eastern edge of Salar de Uyuni, 25 km away from the town of
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Borsa, A. A; et al. (2002). "GPS Survey of the salar de Uyuni, Bolivia, for Satellite Altimeter Calibration". American Geophysical Union, Fall Meeting.
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clouds that form in the eastern part of the salt flat during the summer cannot permeate beyond its drier western edges, near the Chilean border and the
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Lacustrine mud that is interbedded with salt and saturated with brine underlies the surface of Salar de Uyuni. The brine is a saturated solution of
2301: 1201:"Investigations on the effect of high surface albedo on erythemally effective UV irradiance: Results of a campaign at the Salar de Uyuni, Bolivia" 1200: 559: 88: 900: 1711: 930: 2104: 408: 1566: 1272: 2291: 2296: 954: 370:. During the wet season, Titicaca overflows and discharges into Poopó, which in turn, floods Salar De Coipasa and Salar de Uyuni. 2097: 2286: 1650: 502:
s cooperative. Because of its location, large area, and flatness, the Salar is a major car transport route across the Bolivian
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when the flat is flooded and calibrating the resultant water depth model with topographical data from the laser altimeter of
869: 1989: 811: 668: 478:, Bolivia holds about 22% of the world's known lithium resources (105 mln. tons); most of those are in the Salar de Uyuni. 635: 1270:
Lamparelli, R. A. C.; et al. (2003). "Characterization of the Salar de Uyuni for in-orbit satellite calibration".
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and the larger Salar de Uyuni. Salar de Uyuni spreads over 10,582 km, which is roughly 100 times the size of the
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Hexagonal formations on the surface of the Salar de Uyuni as a result of salt crystallization from evaporating water
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and varies between reported studies. Lake Minchin (named after Juan B. Minchin of Oruro) later transformed into
216:. The large area, clear skies, and exceptional flatness of the surface make the Salar ideal for calibrating the 2281: 2032:"MISR-based passive optical bathymetry from orbit with few-cm level of accuracy on the Salar de Uyuni, Bolivia" 1401: 1938:"Modeling the topography of the salar de Uyuni, Bolivia, as an equipotential surface of Earth's gravity field" 2036: 1741: 1153: 533:; Uyuni is a surname and the name of a town that serves as a gateway for tourists visiting the Salar. Thus 1896: 1821: 966: 1635: 1231: 1937: 1104: 2218: 682:
The Salar is virtually devoid of any wildlife or vegetation. The latter is dominated by giant cacti (
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meter over the entire area of the Salar. The crust serves as a source of salt and covers a pool of
918: 1130: 232: 1553: 2213: 1397: 942: 621: 311: 189: 123: 2078: 1844: 1786: 1527: 606: 578: 2182: 2177: 2004: 1580: 363: 988: 2045: 1952: 1776: 1473: 1280: 1249: 1162: 889:, the salt flat surface also rises and falls to reflect the subsurface density variations. 254: 1151:
Fricker, H. A. (2005). "Assessment of ICESat performance at the salar de Uyuni, Bolivia".
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Every November, Salar de Uyuni is the breeding ground for three South American species of
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Satellite-based Estimates of Sea Ice Volume Flux: Applications to the Fram Strait Region
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and say that the place should be called Salar de Tunupa rather than Salar de Uyuni.
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Box, Ben; Kunstaetter, Robert; Kunstaetter, Daisy; Groesbeck, Geoffrey (2007).
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Traditional salt production at Salar. Such salt blocks are used for building
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coral-like structures and deposits that often consist of fossils and algae.
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Bowman, Isaiah (1914). "Results of an Expedition to the Central Andes".
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in the United States. Lake Poopó is a neighbor of the much larger
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The Salar serves as the major transport route across the Bolivian
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at an elevation of 3,656 m (11,995 ft) above sea level.
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The Salar has been used as a filming location for movies such as
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Mountains surrounding the Uyuni salt flat during sunrise,
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and is a prime breeding ground for several species of
1923:"Updated List of Accidents on Salar de Uyuni Tours -" 1990:"The Hills And Valleys Of Earth's Largest Salt Flat" 1814:"Photo in the News: New Salt Hotel Built in Bolivia" 1936:Borsa, A. A.; Bills, B. G.; Minster, J. B. (2008). 1604: 1602: 2238:Other paleolakes and lake expansions in the region 2029: 1778: 271: 1935: 2273: 1599: 1704:"Bolivian Hotel Truly Is the Salt of the Earth" 704:), which is burned as a fuel. Also present are 1532:. Bradt Travel Guides. pp. 170, 174–176. 1422: 180:(or "Salar de Tunupa") is the world's largest 2105: 1425:Bulletin of the American Geographical Society 506:, except when seasonally covered with water. 474:. As of 2024, with an estimated 23 mln.  1945:Journal of Geophysical Research: Solid Earth 1339:"Crait: The Salar de Uyuni Star Wars Planet" 1208:Journal of Photochemistry and Photobiology B 885:Just as the ocean surface rises over denser 150:10,582 square kilometres (1,058,200 ha) 1984: 1982: 1651:"Bolivia's Almost Impossible Lithium Dream" 2119: 2112: 2098: 1610:"Bolivia holds key to electric car future" 1047: 1045: 1043: 1754: 1124: 1122: 1092: 2307:Tourist attractions in Potosí Department 1979: 1772: 1770: 1734:"Don't Lick the Walls of the Salt Hotel" 1698: 1696: 1525: 1521: 1519: 1517: 1515: 1513: 1511: 851: 777: 422: 305: 275: 2302:Tourist attractions in Oruro Department 1388: 1386: 1150: 1040: 540:Aymara legend tells that the mountains 435:, the Salar contains a large amount of 2274: 2002: 1867: 1628: 1451: 1265: 1263: 1194: 1192: 1119: 1053:"Lithium Harvesting at Salar de Uyuni" 68: 2093: 2030:Bills, Bruce G.; et al. (2007). 1808: 1806: 1767: 1748: 1726: 1693: 1679:"Lithium – ACI Systems Alemania GmbH" 1671: 1508: 1247: 1199:Reuder, Joachim; et al. (2007). 1146: 1144: 1073: 418: 1842: 1629:Eisler, Matthew (15 November 2019). 1554:"Lithium Statistics and Information" 1383: 1128: 834:Cemetery of trains near the town of 812:Ferrocarril de Antofagasta a Bolivia 1785:. Footprint Travel Guides. p.  1757:"Salt hotel has a rule: No licking" 1260: 1189: 1131:"The salt flat with curious curves" 13: 1803: 1585:. National Academies. p. 60. 1567:other Lithium statistics from USGS 1458:Baker, P. A.; et al. (2001). 1363: 1345:. salardeuyuni.com. 24 August 2018 1141: 569:inside the Salar, featuring giant 551: 14: 2323: 2067: 1755:McFarrren, Peter (4 March 1999). 1710:. 27 January 2009. Archived from 804: 212:, which is exceptionally rich in 2297:Endorheic lakes of South America 2256: 2073: 1846:The Rough Guide to South America 1526:Atkinson, David (1 March 2007). 1273:IEEE Trans. Geosci. Remote Sens. 1220:10.1016/j.jphotobiol.2006.12.002 965: 960:Reflection on the Salar de Uyuni 953: 941: 929: 917: 899: 823: 667: 648: 634: 620: 605: 591: 577: 558: 400: 322:, not far from the crest of the 67: 60: 44: 2085:Salar de Uyuni official website 2023: 1996: 1929: 1915: 1889: 1836: 1643: 1622: 1572: 1546: 1529:Bolivia: The Bradt Travel Guide 1416: 1357: 1331: 1307: 1129:Hand, Eric (30 November 2007). 755:) host colonies of rabbit-like 272:Formation, geology, and climate 2292:Landforms of Potosí Department 1992:. GPS Daily. 29 November 2007. 1820:. 25 July 2007. Archived from 1241: 1067: 1024:. 29 July 2011. Archived from 1010: 451:(all in the chloride forms of 358:, and two major salt deserts, 293:Salar de Uyuni is part of the 1: 2287:Landforms of Oruro Department 2037:Remote Sensing of Environment 1740:. 19 May 2009. Archived from 1004: 171:3,663 m (12,018 ft) 2081:travel guide from Wikivoyage 1899:(in Spanish). Archived from 1897:"Homepage of Palacio de Sal" 1154:Geophysical Research Letters 910:Panoramic view of the Salar. 842: 677:near the Salar De Uyuni 2017 470:, respectively), as well as 427:Salt production at the Salar 268:(2017), and several others. 7: 2009:. GRIN Verlag. p. 22. 1881:(in German). Archived from 1781:Peru, Bolivia & Ecuador 977: 872:to perform passive optical 333:. Its age was estimated by 283:as viewed from space, with 10: 2328: 936:Piles of salt at the Salar 892: 771: 762: 389: 301: 2253: 2237: 2191: 2162: 2128: 2058:10.1016/j.rse.2006.11.006 1394:"Salar de Uyuni, Bolivia" 972:Sky reflections at sunset 767: 252:(2017; as planet Crait), 167: 159: 154: 146: 141: 133: 119: 104:20.1337750°S 67.4891333°W 84: 55: 43: 30: 23: 1293:10.1109/TGRS.2003.810713 337:shells from outcropping 249:Star Wars: The Last Jedi 200:, near the crest of the 163:130 metres (430 ft) 109:-20.1337750; -67.4891333 2003:Spreen, Gunnar (2008). 1105:Encyclopædia Britannica 509: 76:Location within Bolivia 2129:Present-day lakes and 1398:NASA Earth Observatory 1074:Mills, Andrea (2015). 786: 428: 326: 312:Daniel Campos Province 290: 289:in the top left corner 190:Daniel Campos Province 124:Daniel Campos Province 2282:Salt flats of Bolivia 852:Satellite calibration 781: 747:. The Andean fox, or 691:Echinopsis tarijensis 426: 364:Bonneville Salt Flats 309: 279: 1965:10.1029/2007jb005445 1843:Adès, Harry (2004). 1175:10.1029/2005GL023423 1022:Iris en Tore op reis 687:atacamensis pasacana 662:, south of the Salar 525:originates from the 18:Salt flat in Bolivia 2163:Lake expansions of 2050:2007RSEnv.107..240B 1957:2008JGRB..11310408B 1903:on 26 February 2012 1885:on 6 December 2008. 1818:National Geographic 1478:2001Natur.409..698B 1285:2003ITGRS..41.1461C 1254:2002AGUFMOS52A0193B 1235:(free-download pdf) 1167:2005GeoRL..3221S06F 948:Llamas in the Salar 924:Salar de Uyuni 2013 868:By using data from 100: /  1618:. 9 November 2008. 1028:on 19 January 2016 787: 429: 419:Economic influence 383:magnesium chloride 335:radiocarbon dating 327: 291: 237:cumulonimbus incus 160: • Depth 147: • Total 2269: 2268: 2245:Cancosa paleolake 2016:978-3-640-13064-1 1875:"Palacio del Sal" 1796:978-1-906098-06-3 1659:. 3 December 2018 1539:978-1-84162-165-4 1472:(6821): 698–701. 1404:on 1 October 2006 1237:on 14 April 2014. 1100:"Uyuni Salt Flat" 1085:978-3-8310-3074-3 1057:Earth Observatory 1018:"Salar de Tunupa" 733:James's flamingos 719:feeding on local 316:Potosí Department 233:cumulus congestus 175: 174: 128:Potosí Department 2319: 2263:Lakes portal 2261: 2260: 2259: 2154:Salar de Coipasa 2114: 2107: 2100: 2091: 2090: 2077: 2062: 2061: 2044:(1–2): 240–255. 2027: 2021: 2020: 2000: 1994: 1993: 1986: 1977: 1976: 1942: 1933: 1927: 1926: 1919: 1913: 1912: 1910: 1908: 1893: 1887: 1886: 1871: 1865: 1864: 1840: 1834: 1833: 1831: 1829: 1810: 1801: 1800: 1784: 1774: 1765: 1764: 1761:Associated Press 1752: 1746: 1745: 1730: 1724: 1723: 1721: 1719: 1708:hotelchatter.com 1700: 1691: 1690: 1688: 1686: 1675: 1669: 1668: 1666: 1664: 1647: 1641: 1640: 1636:The Conversation 1626: 1620: 1619: 1606: 1597: 1596: 1576: 1570: 1564: 1558: 1550: 1544: 1543: 1523: 1506: 1505: 1486:10.1038/35055524 1455: 1449: 1448: 1420: 1414: 1413: 1411: 1409: 1400:. Archived from 1390: 1381: 1380: 1378: 1376: 1361: 1355: 1354: 1352: 1350: 1335: 1329: 1328: 1323:. 25 July 2018. 1311: 1305: 1304: 1279:(6): 1461–1468. 1267: 1258: 1257: 1245: 1239: 1238: 1236: 1230:. Archived from 1205: 1196: 1187: 1186: 1148: 1139: 1138: 1126: 1117: 1116: 1114: 1112: 1096: 1090: 1089: 1076:Strange but True 1071: 1065: 1064: 1063:. 12 April 2013. 1049: 1038: 1037: 1035: 1033: 1014: 969: 957: 945: 933: 921: 903: 827: 753:Incahuasi Island 671: 656:Andean flamingos 652: 638: 624: 609: 595: 585:James's flamingo 581: 567:Incahuasi Island 562: 433:Lithium Triangle 404: 379:lithium chloride 360:Salar de Coipasa 347:Paleo Lake Tauca 286:Salar de Coipasa 115: 114: 112: 111: 110: 105: 101: 98: 97: 96: 93: 71: 70: 64: 48: 21: 20: 2327: 2326: 2322: 2321: 2320: 2318: 2317: 2316: 2272: 2271: 2270: 2265: 2257: 2255: 2249: 2233: 2187: 2158: 2124: 2118: 2070: 2065: 2028: 2024: 2017: 2001: 1997: 1988: 1987: 1980: 1940: 1934: 1930: 1921: 1920: 1916: 1906: 1904: 1895: 1894: 1890: 1879:hbernreuther.de 1873: 1872: 1868: 1861: 1853:. p. 259. 1841: 1837: 1827: 1825: 1824:on 28 July 2007 1812: 1811: 1804: 1797: 1775: 1768: 1753: 1749: 1744:on 23 May 2009. 1732: 1731: 1727: 1717: 1715: 1702: 1701: 1694: 1684: 1682: 1677: 1676: 1672: 1662: 1660: 1649: 1648: 1644: 1627: 1623: 1608: 1607: 1600: 1593: 1577: 1573: 1556: 1552: 1551: 1547: 1540: 1524: 1509: 1456: 1452: 1421: 1417: 1407: 1405: 1392: 1391: 1384: 1374: 1372: 1362: 1358: 1348: 1346: 1337: 1336: 1332: 1326:perfectly flat. 1313: 1312: 1308: 1268: 1261: 1246: 1242: 1234: 1203: 1197: 1190: 1149: 1142: 1127: 1120: 1110: 1108: 1098: 1097: 1093: 1086: 1072: 1068: 1051: 1050: 1041: 1031: 1029: 1016: 1015: 1011: 1007: 994:Great Salt Lake 980: 973: 970: 961: 958: 949: 946: 937: 934: 925: 922: 913: 912: 911: 909: 904: 895: 854: 845: 840: 839: 838: 833: 828: 807: 776: 770: 765: 745:Andean hillstar 702:dracunculifolia 678: 672: 663: 660:Laguna Colorada 653: 644: 642:Andean hillstar 639: 630: 625: 616: 610: 601: 596: 587: 582: 573: 563: 554: 552:Flora and fauna 531:pen (enclosure) 527:Aymara language 512: 468: 431:Located in the 421: 416: 415: 414: 413: 410: 405: 392: 375:sodium chloride 343:carbonate reefs 318:, southwestern 304: 274: 108: 106: 102: 99: 94: 91: 89: 87: 86: 80: 79: 78: 77: 74: 73: 72: 51: 39: 26: 19: 12: 11: 5: 2325: 2315: 2314: 2309: 2304: 2299: 2294: 2289: 2284: 2267: 2266: 2254: 2251: 2250: 2248: 2247: 2241: 2239: 2235: 2234: 2232: 2231: 2226: 2221: 2216: 2211: 2206: 2201: 2195: 2193: 2189: 2188: 2186: 2185: 2180: 2175: 2173:Lake Ballivián 2169: 2167: 2160: 2159: 2157: 2156: 2151: 2149:Salar de Uyuni 2146: 2141: 2135: 2133: 2126: 2125: 2117: 2116: 2109: 2102: 2094: 2088: 2087: 2082: 2079:Salar de Uyuni 2069: 2068:External links 2066: 2064: 2063: 2022: 2015: 1995: 1978: 1928: 1914: 1888: 1866: 1859: 1835: 1802: 1795: 1766: 1747: 1738:Tripcrazed.com 1725: 1714:on 15 May 2013 1692: 1670: 1642: 1621: 1598: 1591: 1571: 1545: 1538: 1507: 1450: 1437:10.2307/201641 1431:(3): 161–183. 1415: 1382: 1364:Butler, Alex. 1356: 1330: 1306: 1259: 1240: 1188: 1161:(21): L21S06. 1140: 1118: 1091: 1084: 1066: 1039: 1008: 1006: 1003: 1002: 1001: 996: 991: 986: 979: 976: 975: 974: 971: 964: 962: 959: 952: 950: 947: 940: 938: 935: 928: 926: 923: 916: 906: 905: 898: 897: 896: 894: 891: 853: 850: 844: 841: 830: 829: 822: 821: 820: 806: 805:Train cemetery 803: 792:Palacio de Sal 774:Palacio de Sal 769: 766: 764: 761: 680: 679: 673: 666: 664: 654: 647: 645: 640: 633: 631: 626: 619: 617: 611: 604: 602: 597: 590: 588: 583: 576: 574: 564: 557: 553: 550: 535:Salar de Uyuni 511: 508: 466: 420: 417: 411: 407: 406: 399: 398: 397: 391: 388: 303: 300: 281:Salar de Uyuni 273: 270: 241:Atacama Desert 178:Salar de Uyuni 173: 172: 169: 165: 164: 161: 157: 156: 152: 151: 148: 144: 143: 139: 138: 135: 131: 130: 121: 117: 116: 82: 81: 75: 66: 65: 59: 58: 57: 56: 53: 52: 49: 41: 40: 31: 28: 27: 25:Salar de Uyuni 24: 17: 9: 6: 4: 3: 2: 2324: 2313: 2310: 2308: 2305: 2303: 2300: 2298: 2295: 2293: 2290: 2288: 2285: 2283: 2280: 2279: 2277: 2264: 2252: 2246: 2243: 2242: 2240: 2236: 2230: 2227: 2225: 2222: 2220: 2217: 2215: 2212: 2210: 2207: 2205: 2202: 2200: 2197: 2196: 2194: 2192:Ancient lakes 2190: 2184: 2181: 2179: 2176: 2174: 2171: 2170: 2168: 2166: 2165:Lake Titicaca 2161: 2155: 2152: 2150: 2147: 2145: 2142: 2140: 2139:Lake Titicaca 2137: 2136: 2134: 2132: 2127: 2123: 2120:Lakes on the 2115: 2110: 2108: 2103: 2101: 2096: 2095: 2092: 2086: 2083: 2080: 2076: 2072: 2071: 2059: 2055: 2051: 2047: 2043: 2039: 2038: 2033: 2026: 2018: 2012: 2008: 2007: 1999: 1991: 1985: 1983: 1974: 1970: 1966: 1962: 1958: 1954: 1950: 1946: 1939: 1932: 1924: 1918: 1902: 1898: 1892: 1884: 1880: 1876: 1870: 1862: 1860:1-85828-907-6 1856: 1852: 1848: 1847: 1839: 1823: 1819: 1815: 1809: 1807: 1798: 1792: 1788: 1783: 1782: 1773: 1771: 1762: 1758: 1751: 1743: 1739: 1735: 1729: 1713: 1709: 1705: 1699: 1697: 1681:. August 2019 1680: 1674: 1658: 1657: 1652: 1646: 1638: 1637: 1632: 1625: 1617: 1616: 1611: 1605: 1603: 1594: 1592:9780309320023 1588: 1584: 1583: 1575: 1568: 1562: 1555: 1549: 1541: 1535: 1531: 1530: 1522: 1520: 1518: 1516: 1514: 1512: 1503: 1499: 1495: 1491: 1487: 1483: 1479: 1475: 1471: 1467: 1466: 1461: 1454: 1446: 1442: 1438: 1434: 1430: 1426: 1419: 1403: 1399: 1395: 1389: 1387: 1371: 1370:Lonely Planet 1367: 1360: 1344: 1340: 1334: 1327: 1322: 1321: 1316: 1310: 1302: 1298: 1294: 1290: 1286: 1282: 1278: 1275: 1274: 1266: 1264: 1255: 1251: 1244: 1233: 1229: 1225: 1221: 1217: 1213: 1209: 1202: 1195: 1193: 1184: 1180: 1176: 1172: 1168: 1164: 1160: 1156: 1155: 1147: 1145: 1136: 1132: 1125: 1123: 1107: 1106: 1101: 1095: 1087: 1081: 1077: 1070: 1062: 1058: 1054: 1048: 1046: 1044: 1027: 1023: 1019: 1013: 1009: 1000: 999:Rann of Kutch 997: 995: 992: 990: 987: 985: 982: 981: 968: 963: 956: 951: 944: 939: 932: 927: 920: 915: 914: 908: 902: 890: 888: 883: 879: 875: 871: 866: 864: 858: 849: 837: 832: 826: 819: 817: 813: 802: 800: 795: 793: 785: 780: 775: 760: 758: 754: 750: 746: 742: 738: 734: 730: 726: 722: 721:brine shrimps 718: 713: 711: 707: 703: 701: 697:, and Thola ( 696: 692: 688: 686: 676: 670: 665: 661: 657: 651: 646: 643: 637: 632: 629: 623: 618: 615: 608: 603: 600: 594: 589: 586: 580: 575: 572: 568: 561: 556: 555: 549: 547: 543: 538: 536: 532: 528: 524: 520: 516: 507: 505: 501: 495: 491: 488: 484: 479: 477: 473: 469: 462: 458: 454: 450: 446: 442: 438: 434: 425: 409: 403: 396: 387: 384: 380: 376: 371: 369: 368:Lake Titicaca 365: 361: 357: 353: 348: 344: 340: 336: 332: 325: 321: 317: 313: 308: 299: 296: 288: 287: 282: 278: 269: 267: 263: 262: 261:Salt and Fire 257: 256: 251: 250: 244: 242: 238: 234: 230: 226: 221: 219: 215: 211: 205: 203: 199: 196:in southwest 195: 191: 187: 183: 179: 170: 166: 162: 158: 153: 149: 145: 140: 136: 132: 129: 125: 122: 118: 113: 95:67°29′20.88″W 92:20°08′01.59″S 85:Coordinates: 83: 63: 54: 47: 42: 38: 34: 29: 22: 16: 2209:Lake Minchin 2148: 2041: 2035: 2025: 2005: 1998: 1948: 1944: 1931: 1917: 1905:. 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Index

Salt pan
dry lake
Hexagonal formations on the surface of the Salar de Uyuni as a result of salt crystallization from evaporating water
Salar de Uyuni is located in Bolivia
20°08′01.59″S 67°29′20.88″W / 20.1337750°S 67.4891333°W / -20.1337750; -67.4891333
Daniel Campos Province
Potosí Department
salt flat
playa
Daniel Campos Province
Potosí
Bolivia
Andes
brine
lithium
altimeters
Altiplano
flamingos
cumulus congestus
cumulonimbus incus
Atacama Desert
Star Wars: The Last Jedi
The Fall
Salt and Fire

Salar de Coipasa
Altiplano

Daniel Campos Province
Potosí Department

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