Knowledge (XXG)

Isluga River

Source 📝

259:
Arabilla farther south; the Isluga River here passes through wetland territory. It flows past the towns of Chapicollo, Enquelca and Coraguane before turning sharply to the south. After this turn the river continues first southeast-east, then due east between Cachaguano and Isluga where it has a slight northeasterly tilt, and finally southeastward towards Sitani and Cotasaya. The penultimate part of the river runs irregularly eastward towards Colchani and Pisigua. After a total course of 54 kilometres (34 mi) before ending into the Laguna Mucalliri, which is part of a system of wetlands at
655: 1710: 33: 250:
The Isluga River (also known as Sitani or Arabilla) begins at the southern foot of the 4,940 metres (16,220 ft) high Cerro Alpajeres west of the town of Chaguane at the confluence of the Chaguane and Huinchuta. In its upper parts the Isluga River is also known as the Arabilla River. The Chaguane
417:
A stream gauge was active at Bocatoma (between the towns of Isluga and Sitani) between 1995 and 2001, and at Puente in 1998. At Bocatoma discharge is fairly constant with the exception of the spring months; average runoff is about 0.4–0.5 cubic metres per second (14–18 cu ft/s) but can
311:
vegetation above 3,000 metres (9,800 ft) elevation with about 300 millimetres per year (12 in/year) precipitation. Above 2,000 metres (6,600 ft) elevation lies a montane desert climate with precipitation amounting to 100–50 millimetres per year (3.9–2.0 in/year). During the
258:
After the confluence, the Isluga River proceeds in southeast-eastward direction save for a brief turn northeast, past the towns of Chaguane and Arabilla; between the two the Quebrada Taipicollo joins from the northwest. After Arabilla it turns more eastward and receives waters from the Laguna
771:. The Spanish Crown at that time was pursuing a plan to concentrate the native population in towns; in 1578 the border between the Corregimiento de Arica and Corregimiento de Caranga was drawn across the watershed and coincides with the present-day Chile-Bolivia border. 418:
increase to over 0.75 cubic metres per second (26 cu ft/s) or decrease to less than 0.3 cubic metres per second (11 cu ft/s). A more recent report indicated a discharge of 0.5 cubic metres per second (18 cu ft/s) at the Bocatoma station.
1506: 295:
and a further 145 square kilometres (56 sq mi) of Bolivia, and lies at an average elevation of 4,187 metres (13,737 ft) elevation. The catchment of Isluga is more gentle than Pacific-draining catchments, resulting in the formation of
237:
The watershed of the river lies mainly in Chile and has a dry climate, resulting in a small river discharge of about 0.4–0.5 cubic metres per second (14–18 cu ft/s). There are a number of towns and hamlets in the catchment, as well as
282:
from the north; the Alsare from Cabaray is a major tributary. From the south it receives tributaries from the Sierra Uscana, including the 54 kilometres (34 mi) long Mauque which joins the Isluga River in the Fisica Choque/Chaque wetland.
1559:
Márquez-García, Marcela; Vila, Irma; Hinojosa, Luis Felipe; Méndez, Marco A.; Carvajal, José Luis; Sabando, María Catalina (December 2009). "Distribution and seasonal fluctuations in the aquatic biodiversity of the southern Altiplano".
255:, which in turn is nourished from two creeks that join it from the west and north. The Huinchuta (also known as Pasijro) is also 12 kilometres (7.5 mi) long but comes from the northwest and turns south before joining the Chaguane. 1449: 1154:
Lüssen, Arne; Falk, Thomas M.; Villwock, Wolfgang (October 2003). "Phylogenetic patterns in populations of Chilean species of the genus Orestias (Teleostei: Cyprinodontidae): results of mitochondrial DNA analysis".
1637: 218:, and is also known as Sitani or Arabilla. It starts at the confluence of the rivers Chaguane and Huinchuta and flows for 54 kilometres (34 mi) before reaching the Laguna Mucalliri of the 263:. The Cariquima River ends into the same general area and is sometimes considered to be part of the Rio Isluga. From that area, the Sitani River continues into the Salar de Coipasa proper. 1441: 1630: 1623: 1303:"Hidden diversity in spring snails from the Andean Altiplano, the second highest plateau on Earth, and the Atacama Desert, the driest place in the world" 755:
envisaged transferring water from the headwaters of the Isluga River to the Quebrada de Camiña by way of a tunnel to increase the water supply to the
398:
Water temperatures at Ríos Arabilla at 3,850 metres (12,630 ft) elevation range 7–17 °C (45–63 °F). The salinity is dominated by
355:
and lacustrine deposits; these sedimentary formations are concentrated in the central parts of the catchment 5,501 metres (18,048 ft) high
1798: 1783: 1788: 948: 1600: 728:
of Colchane. There are further hamlets and villages in the catchment of the Isluga River. Most of the watershed is undeveloped, with
1209:"ANALISIS DE FORMAS EN ESPECIES CHILENAS DEL GENERO TRICHOMYCTERUS (Osteichthyes: Siluriformes) UTILIZANDO MORFOMETRIA GEOMETRICA" 1517: 1485: 359:
volcano is still active, with eruptions in 1900 and 1963; other important mountains are the 5,869 metres (19,255 ft) high
1709: 744: 1694: 865: 816: 1803: 1689: 1679: 1674: 670:; depending on the availability of water different places are dominated by different plants. Among the fauna are 1533: 1793: 512: 252: 1507:"Cuenca del Río Isluga. Diagnóstico yclasificación de los cursos y cuerpos de agua según objetivos de calidad" 386:
and the Isluga River drain the Altiplano. Part of the Isluga catchment was covered by lakes, which have left
631: 553: 1544: 953: 861: 812: 619: 559: 637: 271: 231: 686: 607: 595: 583: 565: 1760: 1248:
Moreno M, Rodrigo; Moreno, Jorge; Torres-Pérez, Fernando; Ortiz, Juan C.; Breskovic, Antonio (2001).
752: 643: 613: 497: 767:
During the 16th century the Isluga region was part of the Caranga confederation, which extended to
717: 654: 577: 487: 1650: 1534:"Primer Inventario de Levantamiento de información biológica en laguna Parinacota y Río Arabilla" 692: 517: 451: 1729: 32: 1587: 1324: 1271: 1230: 1172: 968: 725: 430: 332: 441: 1755: 1577: 1569: 1314: 1261: 1220: 1164: 958: 721: 260: 219: 94: 58: 759:
valley. Concerns have been raised in 2011 in Bolivia about diversions of the Isluga River.
1734: 1604: 521: 379: 292: 1724: 1478:"ESTIMACIÓN DE RECARGAS EN CUENCAS ALTIPLÁNICAS Y PRECORDILLERANAS DE VERTIENTE PACÍFICA" 410:
owing to high evaporation and the dissolution of salts in the catchment. The waters are
507: 503: 1168: 751:
takes place in the watershed, but there is little information on it. An old plan of a
1777: 1684: 1250:"Herpetological Catalogue of Museo del Mar of Arturo Prat University, Iquique, Chile" 316:, the Altiplano was at times wetter than today, resulting in the formation of lakes. 267: 1615: 1442:"Bolivianos acusan a Chile de remover hitos limítrofes y desviar un río en Colchane" 1266: 1249: 1225: 1208: 963: 545:
A number of different plant species grow in the waters of the Isluga River, such as
1739: 1699: 304: 1065: 1063: 1061: 1059: 986: 984: 982: 291:
The Isluga River drains 2,295 square kilometres (886 sq mi) of Chile's
1646: 1573: 1301:
Collado, Gonzalo A.; Valladares, Moisés A.; Méndez, Marco A. (1 December 2013).
949:"Percepción del espacio y apropiación del territorio entre los aymara de Isluga" 736: 729: 383: 371: 344: 88: 307:
and falls mainly during the summer months. This results in the region having a
768: 748: 625: 589: 529: 492: 482: 446: 324: 313: 1591: 1328: 1275: 1234: 1176: 972: 1669: 1319: 1302: 697: 680: 648: 533: 467: 411: 375: 343:. In the central and eastern parts there are also sedimentary formations of 320: 38: 756: 675: 1490: 1477: 713: 671: 571: 538: 472: 435: 426: 399: 367: 352: 348: 336: 1582: 740: 701: 525: 476: 462: 457: 407: 387: 360: 297: 279: 239: 227: 215: 1445: 667: 663: 662:
The steppes surrounding the catchment feature a flora which includes
601: 403: 356: 340: 328: 308: 275: 223: 303:
The region has an arid climate. Most precipitation arrives from the
1603:(Report). Hoyas hidrográficas de Chile (in Spanish). Archived from 647:. The wetlands along the river are an important environment in the 653: 547: 211: 1069: 990: 251:
is 12 kilometres (7.5 mi) long and receives water from the
1619: 378:
to heights of over 4,000 metres (13,000 ft). A number of
1141: 1093: 925: 844: 842: 363:
and the 4,944 metres (16,220 ft) high Cerro El Fraile.
1400: 1398: 201:
Mauque, sometimes Cariquima River is considered a tributary
1190: 1188: 1186: 885: 883: 881: 879: 788: 786: 784: 1562:
Limnologica - Ecology and Management of Inland Waters
1748: 1717: 1657: 195: 185: 177: 172: 158: 148: 138: 128: 120: 108: 100: 87: 75: 66: 46: 21: 270:. It receives several tributaries that drain the 1476:AQUATERRA INGENIEROS LIMITADA (September 2011). 747:is an important economic resource for the area. 704:faunas are little known, unlike the bird fauna. 164:More than 0.75 m/s (26 cu ft/s) 1631: 942: 940: 938: 936: 934: 735:Wetlands in the catchment were important for 154:Less than 0.3 m/s (11 cu ft/s) 112:2,450 square kilometres (950 sq mi) 50: 8: 495:flies further populate the waters. The fish 724:lie in the watershed, which is part of the 242:with a number of animal and plant species. 1638: 1624: 1616: 1416: 1404: 1389: 1365: 1194: 1129: 1117: 1105: 1081: 1038: 1026: 1014: 1002: 889: 817:"Salinas de Garci-Mendoza, Bolivia; Chile" 792: 445:while the faunal side is characterized by 144:0.4–0.5 m/s (14–18 cu ft/s) 1581: 1318: 1265: 1224: 962: 1428: 1050: 913: 901: 848: 833: 1207:Pardo, R.; Scott, S.; Vila, I. (2005). 870:Latin America, Joint Operations Graphic 821:Latin America, Joint Operations Graphic 780: 516:live in its waters. These fish are all 266:The Isluga River is entrenched between 222:. It receives water from the volcanoes 1377: 1353: 1341: 1288: 807: 805: 803: 801: 319:Much of the watershed is dominated by 18: 1157:Molecular Phylogenetics and Evolution 7: 524:has also been found, as are several 79:Confluence of Chaguane and Huinchuta 429:is dominated on the floral side by 1142:AQUATERRA INGENIEROS LIMITADA 2011 1094:AQUATERRA INGENIEROS LIMITADA 2011 926:AQUATERRA INGENIEROS LIMITADA 2011 520:or at the risk of extinction. The 14: 732:being the main form of land use. 1708: 1518:Ministry of Public Works (Chile) 1486:Ministry of Public Works (Chile) 37:The Isluga River flowing past a 31: 1452:from the original on 2018-02-27 1267:10.4067/S0717-65382001000200006 1226:10.4067/S0717-65382005000100023 964:10.4067/S0718-10432008000200007 1541:Biblioteca digital CEDOC-CIREN 234:as well as the Sierra Uscana. 1: 1169:10.1016/S1055-7903(03)00077-0 947:G, Aedo; Angel, Juan (2008). 374:, tectonic uplift raised the 327:age volcanic rocks formed by 67:Physical characteristics 1784:Rivers of Antofagasta Region 1505:CADE-IDEPE (December 2004). 1574:10.1016/j.limno.2009.06.007 745:Volcán Isluga National Park 658:Wetland on the Isluga River 191:Quebrada Taipicollo, Alsare 130: • location 1820: 1789:Rivers of Oruro Department 1599:Niemeyer, Hans F. (1980). 1532:Guzmán, Guillermo (2015). 1070:Márquez-García et al. 2009 991:Márquez-García et al. 2009 160: • maximum 150: • minimum 140: • average 104:54 kilometres (34 mi) 1799:Rivers of Tarapacá Region 1706: 1448:. emol.com. 17 May 2011. 168: 116: 83: 71: 30: 536:and snails of the genus 513:Trichomycterus rivulatus 197: • right 25:Rio Arabilla, Rio Sitani 1320:10.1186/1810-522X-52-50 872:(1 ed.). 1:250000. 823:(2 ed.). 1:250000. 678:, lizards of the genus 475:in shallower parts and 187: • left 1695:San Pedro de Inacaliri 1545:Arturo Prat University 862:Defense Mapping Agency 813:Defense Mapping Agency 659: 560:Deschampsia caespitosa 51: 687:Pleurodema marmoratum 657: 632:Sarcocornia pulvinata 554:Catabrosa verdermanni 1761:Salar de Punta Negra 1690:San Pedro de Atacama 1610:on 13 November 2018. 1514:Biblioteca Humedales 753:transbasin diversion 644:Triglochin palustris 620:Potamogeton strictum 528:species of the taxa 382:systems such as the 41:from Isluga Volcano. 1254:Gayana (Concepción) 1213:Gayana (Concepción) 954:Estudios Atacameños 916:, pp. 109–110. 851:, pp. 108–109. 739:, which along with 638:Scirpus atacamensis 578:Distichia muscoides 173:Basin features 1651:Antofagasta Region 1307:Zoological Studies 693:Rhinella spinulosa 660: 608:Lilaeopsis lineata 596:Festuca nardifolia 584:Distichlis humilis 93:Laguna Mucalliri, 1804:Rivers of Bolivia 1769: 1768: 1431:, p. 56,111. 431:bacillariophyceae 390:and small lakes. 333:basaltic andesite 253:Laguna Parinacota 205: 204: 1811: 1756:Salar de Atacama 1712: 1640: 1633: 1626: 1617: 1611: 1609: 1595: 1585: 1555: 1553: 1551: 1538: 1528: 1526: 1524: 1511: 1501: 1499: 1497: 1482: 1462: 1461: 1459: 1457: 1438: 1432: 1426: 1420: 1414: 1408: 1402: 1393: 1387: 1381: 1375: 1369: 1363: 1357: 1351: 1345: 1339: 1333: 1332: 1322: 1298: 1292: 1286: 1280: 1279: 1269: 1245: 1239: 1238: 1228: 1204: 1198: 1192: 1181: 1180: 1151: 1145: 1139: 1133: 1127: 1121: 1115: 1109: 1103: 1097: 1091: 1085: 1079: 1073: 1067: 1054: 1048: 1042: 1036: 1030: 1024: 1018: 1012: 1006: 1000: 994: 988: 977: 976: 966: 944: 929: 923: 917: 911: 905: 899: 893: 887: 874: 873: 866:"Pisagua, Chile" 858: 852: 846: 837: 831: 825: 824: 809: 796: 790: 566:Deyeuxia curvula 508:pencil catfishes 498:Orestias agassii 261:Salar de Coipasa 220:Salar de Coipasa 198: 188: 161: 151: 141: 131: 95:Salar de Coipasa 62: 54: 35: 19: 1819: 1818: 1814: 1813: 1812: 1810: 1809: 1808: 1794:Rivers of Chile 1774: 1773: 1770: 1765: 1744: 1735:Laguna Miscanti 1730:Laguna Miñiques 1713: 1704: 1653: 1644: 1614: 1607: 1598: 1558: 1549: 1547: 1536: 1531: 1522: 1520: 1509: 1504: 1495: 1493: 1480: 1475: 1471: 1466: 1465: 1455: 1453: 1440: 1439: 1435: 1427: 1423: 1417:CADE-IDEPE 2004 1415: 1411: 1405:CADE-IDEPE 2004 1403: 1396: 1390:CADE-IDEPE 2004 1388: 1384: 1376: 1372: 1366:CADE-IDEPE 2004 1364: 1360: 1352: 1348: 1340: 1336: 1300: 1299: 1295: 1287: 1283: 1247: 1246: 1242: 1206: 1205: 1201: 1195:CADE-IDEPE 2004 1193: 1184: 1153: 1152: 1148: 1140: 1136: 1130:CADE-IDEPE 2004 1128: 1124: 1118:CADE-IDEPE 2004 1116: 1112: 1106:CADE-IDEPE 2004 1104: 1100: 1092: 1088: 1082:CADE-IDEPE 2004 1080: 1076: 1068: 1057: 1049: 1045: 1039:CADE-IDEPE 2004 1037: 1033: 1027:CADE-IDEPE 2004 1025: 1021: 1017:, pp. 4–5. 1015:CADE-IDEPE 2004 1013: 1009: 1003:CADE-IDEPE 2004 1001: 997: 989: 980: 957:(36): 117–137. 946: 945: 932: 924: 920: 912: 908: 900: 896: 890:CADE-IDEPE 2004 888: 877: 860: 859: 855: 847: 840: 832: 828: 811: 810: 799: 793:CADE-IDEPE 2004 791: 782: 777: 765: 710: 614:Oxychloe andina 522:Peru water frog 424: 396: 293:Tarapaca Region 289: 248: 196: 186: 159: 149: 139: 129: 56: 42: 26: 23: 17: 12: 11: 5: 1817: 1815: 1807: 1806: 1801: 1796: 1791: 1786: 1776: 1775: 1767: 1766: 1764: 1763: 1758: 1752: 1750: 1746: 1745: 1743: 1742: 1737: 1732: 1727: 1721: 1719: 1715: 1714: 1707: 1705: 1703: 1702: 1697: 1692: 1687: 1682: 1677: 1672: 1667: 1661: 1659: 1655: 1654: 1645: 1643: 1642: 1635: 1628: 1620: 1613: 1612: 1601:Primera Región 1596: 1568:(4): 314–318. 1556: 1543:(in Spanish). 1529: 1516:(in Spanish). 1502: 1489:(in Spanish). 1472: 1470: 1467: 1464: 1463: 1444:(in Spanish). 1433: 1421: 1409: 1394: 1382: 1370: 1358: 1346: 1334: 1293: 1281: 1260:(2): 149–153. 1240: 1219:(1): 180–183. 1199: 1182: 1163:(1): 151–160. 1146: 1144:, p. 143. 1134: 1122: 1110: 1098: 1096:, p. 139. 1086: 1074: 1072:, p. 316. 1055: 1043: 1031: 1019: 1007: 995: 993:, p. 314. 978: 930: 918: 906: 904:, p. 109. 894: 875: 853: 838: 836:, p. 108. 826: 797: 779: 778: 776: 773: 764: 761: 709: 708:Human activity 706: 504:Trichomycterus 423: 420: 395: 392: 288: 285: 268:river terraces 247: 244: 210:is a river in 203: 202: 199: 193: 192: 189: 183: 182: 179: 175: 174: 170: 169: 166: 165: 162: 156: 155: 152: 146: 145: 142: 136: 135: 132: 126: 125: 122: 118: 117: 114: 113: 110: 106: 105: 102: 98: 97: 91: 85: 84: 81: 80: 77: 73: 72: 69: 68: 64: 63: 48: 44: 43: 36: 28: 27: 24: 15: 13: 10: 9: 6: 4: 3: 2: 1816: 1805: 1802: 1800: 1797: 1795: 1792: 1790: 1787: 1785: 1782: 1781: 1779: 1772: 1762: 1759: 1757: 1754: 1753: 1751: 1747: 1741: 1738: 1736: 1733: 1731: 1728: 1726: 1723: 1722: 1720: 1716: 1711: 1701: 1698: 1696: 1693: 1691: 1688: 1686: 1683: 1681: 1678: 1676: 1673: 1671: 1668: 1666: 1663: 1662: 1660: 1656: 1652: 1648: 1641: 1636: 1634: 1629: 1627: 1622: 1621: 1618: 1606: 1602: 1597: 1593: 1589: 1584: 1579: 1575: 1571: 1567: 1563: 1557: 1546: 1542: 1535: 1530: 1519: 1515: 1508: 1503: 1492: 1488: 1487: 1479: 1474: 1473: 1468: 1451: 1447: 1443: 1437: 1434: 1430: 1429:Niemeyer 1980 1425: 1422: 1419:, p. 14. 1418: 1413: 1410: 1407:, p. 11. 1406: 1401: 1399: 1395: 1392:, p. 10. 1391: 1386: 1383: 1380:, p. 10. 1379: 1374: 1371: 1367: 1362: 1359: 1355: 1350: 1347: 1343: 1338: 1335: 1330: 1326: 1321: 1316: 1312: 1308: 1304: 1297: 1294: 1291:, p. 18. 1290: 1285: 1282: 1277: 1273: 1268: 1263: 1259: 1255: 1251: 1244: 1241: 1236: 1232: 1227: 1222: 1218: 1214: 1210: 1203: 1200: 1196: 1191: 1189: 1187: 1183: 1178: 1174: 1170: 1166: 1162: 1158: 1150: 1147: 1143: 1138: 1135: 1132:, p. 21. 1131: 1126: 1123: 1120:, p. 19. 1119: 1114: 1111: 1108:, p. 12. 1107: 1102: 1099: 1095: 1090: 1087: 1084:, p. 46. 1083: 1078: 1075: 1071: 1066: 1064: 1062: 1060: 1056: 1052: 1051:Niemeyer 1980 1047: 1044: 1040: 1035: 1032: 1028: 1023: 1020: 1016: 1011: 1008: 1004: 999: 996: 992: 987: 985: 983: 979: 974: 970: 965: 960: 956: 955: 950: 943: 941: 939: 937: 935: 931: 927: 922: 919: 915: 914:Niemeyer 1980 910: 907: 903: 902:Niemeyer 1980 898: 895: 891: 886: 884: 882: 880: 876: 871: 867: 863: 857: 854: 850: 849:Niemeyer 1980 845: 843: 839: 835: 834:Niemeyer 1980 830: 827: 822: 818: 814: 808: 806: 804: 802: 798: 794: 789: 787: 785: 781: 774: 772: 770: 762: 760: 758: 754: 750: 746: 742: 738: 733: 731: 727: 723: 719: 715: 712:The towns of 707: 705: 703: 699: 695: 694: 690:and the toad 689: 688: 683: 682: 677: 673: 669: 665: 656: 652: 650: 646: 645: 640: 639: 634: 633: 628: 627: 622: 621: 616: 615: 610: 609: 604: 603: 598: 597: 592: 591: 586: 585: 580: 579: 574: 573: 568: 567: 562: 561: 556: 555: 550: 549: 543: 541: 540: 535: 531: 527: 523: 519: 515: 514: 509: 506: 505: 500: 499: 494: 490: 489: 485:of the genus 484: 480: 478: 474: 470: 469: 464: 460: 459: 454: 453: 448: 444: 443: 438: 437: 432: 428: 421: 419: 415: 413: 409: 405: 401: 393: 391: 389: 385: 381: 377: 373: 369: 364: 362: 358: 354: 350: 346: 342: 338: 334: 330: 326: 322: 317: 315: 310: 306: 301: 299: 294: 286: 284: 281: 277: 273: 269: 264: 262: 256: 254: 245: 243: 241: 235: 233: 229: 225: 221: 217: 213: 209: 200: 194: 190: 184: 180: 176: 171: 167: 163: 157: 153: 147: 143: 137: 133: 127: 123: 119: 115: 111: 107: 103: 99: 96: 92: 90: 86: 82: 78: 74: 70: 65: 60: 53: 49: 45: 40: 34: 29: 20: 1771: 1740:Tuyajto Lake 1725:Laguna Lejía 1675:San Salvador 1665:Isluga River 1664: 1605:the original 1583:10533/130603 1565: 1561: 1548:. Retrieved 1540: 1521:. Retrieved 1513: 1494:. Retrieved 1484: 1454:. Retrieved 1436: 1424: 1412: 1385: 1373: 1368:, p. 8. 1361: 1356:, p. 2. 1349: 1344:, p. 6. 1337: 1310: 1306: 1296: 1284: 1257: 1253: 1243: 1216: 1212: 1202: 1197:, p. 9. 1160: 1156: 1149: 1137: 1125: 1113: 1101: 1089: 1077: 1053:, p. 7. 1046: 1041:, p. 5. 1034: 1029:, p. 6. 1022: 1010: 1005:, p. 4. 998: 952: 928:, p. 4. 921: 909: 897: 892:, p. 7. 869: 856: 829: 820: 795:, p. 1. 766: 734: 711: 691: 685: 679: 661: 642: 636: 630: 624: 618: 612: 606: 600: 594: 588: 582: 576: 570: 564: 558: 552: 546: 544: 537: 511: 502: 496: 488:Australelmis 486: 481: 466: 456: 450: 440: 434: 425: 416: 397: 365: 351:, including 318: 302: 290: 265: 257: 249: 236: 208:Isluga River 207: 206: 22:Isluga River 1647:Hydrography 1550:26 February 1523:26 February 1496:27 February 1456:27 February 1378:Guzmán 2015 1354:Guzmán 2015 1342:Guzmán 2015 1289:Guzmán 2015 737:pastoralism 730:agriculture 684:, the frog 447:cladocerans 384:Lauca River 372:Pleistocene 366:During the 345:Pleistocene 272:Quimsachata 232:Quimsachata 178:Tributaries 47:Native name 1778:Categories 775:References 769:Lake Poopo 749:Irrigation 626:Ranunculus 590:Eleocharis 530:chilinidae 518:vulnerable 493:chironomid 483:Coleoptera 325:Quaternary 314:Quaternary 109:Basin size 52:Río Isluga 1749:Salt pans 1592:0075-9511 1329:1810-522X 1313:(1): 50. 1276:0717-6538 1235:0717-6538 1177:1055-7903 973:0718-1043 698:amphibian 681:Liolaemus 672:flamingos 649:Altiplano 534:veneroida 473:ostracods 468:Boeckella 412:eutrophic 394:Discharge 380:endorheic 376:Altiplano 321:Oligocene 287:Watershed 121:Discharge 39:lava flow 1491:Santiago 1450:Archived 864:(1997). 815:(1996). 714:Colchane 572:Drabella 539:Heleobia 510:such as 477:rotifers 463:copepods 436:Navicula 433:such as 427:Plankton 400:chloride 388:wetlands 368:Pliocene 353:alluvial 349:Holocene 337:andesite 298:wetlands 240:wetlands 134:Bocatoma 1685:Toconce 1469:Sources 868:(Map). 819:(Map). 763:History 743:of the 741:tourism 726:commune 702:reptile 676:vicuñas 526:mollusc 458:Bosmina 442:Synedra 422:Biology 408:sulfate 361:Cabaray 280:Cabaray 228:Cabaray 216:Bolivia 59:Spanish 1700:Silala 1680:Salado 1658:Rivers 1590:  1446:La Paz 1327:  1274:  1233:  1175:  971:  757:Camiña 722:Pisiga 718:Isluga 696:. The 668:yareta 664:quenoa 602:Juncus 404:sodium 357:Isluga 341:dacite 329:basalt 309:steppe 305:Amazon 276:Isluga 246:Course 224:Isluga 181:  124:  101:Length 76:Source 55:  1718:Lakes 1608:(PDF) 1537:(PDF) 1510:(PDF) 1481:(PDF) 548:Carex 452:Alona 212:Chile 89:Mouth 16:River 1588:ISSN 1552:2018 1525:2018 1498:2018 1458:2018 1325:ISSN 1272:ISSN 1231:ISSN 1173:ISSN 969:ISSN 720:and 700:and 674:and 666:and 641:and 532:and 501:and 491:and 455:and 439:and 406:and 339:and 278:and 230:and 214:and 1670:Loa 1649:of 1578:hdl 1570:doi 1315:doi 1262:doi 1221:doi 1165:doi 959:doi 471:), 461:), 347:to 323:to 1780:: 1586:. 1576:. 1566:39 1564:. 1539:. 1512:. 1483:. 1397:^ 1323:. 1311:52 1309:. 1305:. 1270:. 1258:65 1256:. 1252:. 1229:. 1217:69 1215:. 1211:. 1185:^ 1171:. 1161:29 1159:. 1058:^ 981:^ 967:. 951:. 933:^ 878:^ 841:^ 800:^ 783:^ 716:, 651:. 635:, 629:, 623:, 617:, 611:, 605:, 599:, 593:, 587:, 581:, 575:, 569:, 563:, 557:, 551:, 542:. 479:. 414:. 402:, 335:, 331:, 300:. 274:, 226:, 1639:e 1632:t 1625:v 1594:. 1580:: 1572:: 1554:. 1527:. 1500:. 1460:. 1331:. 1317:: 1278:. 1264:: 1237:. 1223:: 1179:. 1167:: 975:. 961:: 465:( 449:( 370:- 61:) 57:(

Index


lava flow
Spanish
Mouth
Salar de Coipasa
Chile
Bolivia
Salar de Coipasa
Isluga
Cabaray
Quimsachata
wetlands
Laguna Parinacota
Salar de Coipasa
river terraces
Quimsachata
Isluga
Cabaray
Tarapaca Region
wetlands
Amazon
steppe
Quaternary
Oligocene
Quaternary
basalt
basaltic andesite
andesite
dacite
Pleistocene

Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.