506:
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263:
to be given its own name, perhaps one already known to the people who live upon its banks. Conversely, explorers approaching a new land from the sea encounter its rivers at their mouths, where they name them on their charts, then, following a river upstream, encounter each tributary as a forking of the stream to the right and to the left, which then appear on their charts as such; or the streams are seen to diverge by the
40:
156:
422:
533:
466:
262:
These naming conventions are reflective of the circumstances of a particular river's identification and charting: people living along the banks of a river, with a name known to them, may then float down the river in exploration, and each tributary joining it as they pass by appears as a new river,
360:
344:
315:
of first, second, third and higher orders, with the first-order tributary being typically the least in size. For example, a second-order tributary would be the result of two or more first-order tributaries combining to form the second-order tributary.
206:
or other vessel in the main stream, this would be the side the tributary enters from as one floats past; alternately, if one were floating down the tributary, the main stream meets it on the
194:, describe the orientation of the tributary relative to the flow of the main stem river. These terms are defined from the perspective of looking downstream, that is, facing the direction the
743:
523:) is a highlighted example of a tributary of the Wabash River. The Wabash River is also a tributary of the Ohio River, which in turn is a tributary of the
403:
736:
974:
1342:
384:
252:'s North Branch has the East, West, and Middle Fork; the South Branch has its South Fork, and used to have a West Fork as well (now filled in).
255:
Forks are sometimes designated as right or left. Here, the handedness is from the point of view of an observer facing upstream. For instance,
645:
729:
125:
is the largest tributary river by volume in the world with an average discharge of 31,200 m/s (1.1 million cu ft/s).
604:. The American Heritage Dictionary of the English Language, Fourth Edition. Houghton Mifflin Company, 2004. Viewed 30 September 2008.
267:(north, south, east, or west) in which they proceed upstream, sometimes a third stream entering between two others is designated the
1968:
433:
1499:
551:. It flows almost parallel to the Ganges about its right bank for 1,376 kilometres (855 mi) before merging with it at the
1963:
354:
is a system made up of many tributary streams. The streams shown on the map besides the Amazon are tributaries of the Amazon.
1665:
1615:
1509:
684:
240:
In the United States, where tributaries sometimes have the same name as the river into which they feed, they are called
160:
143:, a river or stream that branches off from and flows away from the main stream. Distributaries are most often found in
1943:
256:
1169:
271:
fork; or the streams are distinguished by the relative height of one to the other, as one stream descending over a
33:
1989:
1953:
1905:
1788:
1938:
1655:
1620:
1462:
677:
121:
river and is also the longest tributary river in the world with a length of 4,248 km (2,640 mi). The
1948:
1640:
1405:
432:
is a much simpler example of a river basin with tributaries. The main tributaries noted on this map are the
2004:
1890:
1748:
1299:
1184:
1728:
1575:
1537:
986:
925:
324:
1999:
1958:
1680:
1504:
1264:
1071:
865:
374:; many of the highest tributaries are seasonal streams. The Benue is itself a major tributary of the
441:
1854:
1849:
1650:
1494:
1116:
969:
890:
797:
698:
Stewart, George R. (1939). "Nomenclature of Stream-Forks on the West Slope of the Sierra Nevada".
445:
1880:
1793:
1758:
1610:
1126:
1031:
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457:
264:
1600:
1859:
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481:
199:
1773:
1675:
1580:
1179:
1174:
1091:
920:
792:
707:
663:. PhysicalGeography.net, Michael Pidwirny & Scott Jones, 2009. Viewed 17 September 2012.
592:. PhysicalGeography.net, Michael Pidwirny & Scott Jones, 2009. Viewed 17 September 2012.
221:
is a tributary that joins the main stem river closer to its source than its mouth, that is,
195:
164:
1994:
1778:
1738:
1733:
1524:
1337:
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1219:
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910:
875:
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837:
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773:
619:
548:
477:
453:
371:
308:
133:
233:
joins the main stem further downstream, closer to its mouth than to its source, that is,
155:
1839:
1723:
1703:
1585:
1570:
1457:
1442:
1437:
1397:
1377:
1289:
1131:
1121:
1111:
1076:
1008:
993:
900:
822:
782:
614:
552:
327:
320:
245:
103:
660:
589:
1983:
1920:
1915:
1900:
1885:
1834:
1829:
1595:
1560:
1514:
1474:
1469:
1229:
1101:
1061:
807:
787:
409:
249:
168:
122:
51:
1910:
1660:
1645:
1635:
1484:
1415:
1284:
1249:
1164:
1106:
981:
880:
842:
817:
512:
449:
351:
300:
287:
fork, the larger either retaining its name unmodified, or receives the designation
140:
102:. Tributaries, and the main stem river into which they flow, drain the surrounding
601:
678:"Olympic Experimental State Forest Synthesis of Riparian Research and Monitoring"
17:
1819:
1743:
1447:
1410:
1357:
1081:
1066:
1041:
915:
437:
375:
367:
304:
144:
107:
39:
1925:
1605:
1489:
1429:
1387:
1259:
1096:
964:
905:
895:
812:
721:
520:
516:
429:
390:
214:
water by moving towards the opposite bank before approaching the confluence.
211:
129:
118:
486:
319:
Another method is to list tributaries from mouth to source, in the form of a
1895:
1844:
1814:
1783:
1713:
1625:
1382:
1269:
1254:
1194:
1141:
1136:
1036:
959:
949:
556:
496:
312:
272:
82:
1565:
1532:
1209:
1051:
1018:
248:
in
California receives flow from its North, Middle, and South forks. The
226:
43:
244:. These are typically designated by compass direction. For example, the
1875:
1824:
1352:
1347:
1329:
1309:
1214:
1151:
1086:
1023:
570:
413:
394:
1670:
1542:
1367:
1362:
1314:
1304:
1274:
1199:
954:
885:
857:
756:
544:
540:
519:) are tributaries of the Wabash River. The Vermillion River (and its
473:
171:, which flows from bottom left to top right, making the Shenandoah a
114:
73:
47:
460:. The Xiliao River's tributaries are the Xar Moron and Laoha rivers.
299:
Tributaries are sometimes listed starting with those nearest to the
711:
1768:
1753:
1708:
1452:
1425:
1372:
1239:
1234:
1204:
1189:
998:
768:
752:
492:
154:
99:
77:
38:
32:
This article is about a lesser flow of water. For other uses, see
1798:
1763:
1319:
1279:
1244:
203:
91:
55:
725:
1718:
1159:
259:
has a left tributary which is called Right Fork Steer Creek.
95:
210:
bank of the tributary. This information may be used to avoid
495:, but the tributaries that feed its lower reaches (e.g. the
283:; or by relative volume: the smaller stream designated the
29:
Stream or river that flows into a main stem river or lake
136:
meet, usually refers to the joining of tributaries.
1868:
1807:
1689:
1551:
1523:
1424:
1396:
1328:
1150:
1017:
934:
856:
767:
676:Bisson, Peter; Wondzell, Steven (1 December 2009).
370:is fed by multiple tributaries originating in the
339:A gallery of major river basins with tributaries
476:is a trans-boundary river, originating in the
737:
543:is the second-largest tributary river of the
311:examines the arrangement of tributaries in a
8:
94:. A tributary does not flow directly into a
744:
730:
722:
480:. Its upper tributary river systems (e.g.
279:fork, and the one it descends into, the
1343:International scale of river difficulty
582:
337:
110:, leading the water out into an ocean.
515:; the other rivers (not including the
303:and ending with those nearest to the
7:
671:
669:
202:context, if one were floating on a
25:
139:The opposite to a tributary is a
80:that flows into a larger stream (
532:
504:
465:
421:
402:
383:
359:
343:
198:of the main stem is going. In a
1500:Flooded grasslands and savannas
640:. Greenwood Publishing Group.
1:
547:and the longest tributary in
1666:Universal Soil Loss Equation
1616:Hydrological transport model
1510:Storm Water Management Model
685:United States Forest Service
161:Harpers Ferry, West Virginia
117:is a chief tributary of the
637:The Basics of Earth Science
491:) are restricted to narrow
412:(itself a tributary of the
393:(itself a tributary of the
2021:
1170:Antecedent drainage stream
163:, looking downstream, the
34:Tributary (disambiguation)
31:
1934:
1906:River valley civilization
1789:Riparian-zone restoration
661:"opposite to a tributary"
634:Krebs, Robert E. (2003).
615:"Definition of TRIBUTARY"
275:into another becomes the
167:(bottom right) meets the
106:of its surface water and
1969:Countries without rivers
1944:Rivers by discharge rate
1656:Runoff model (reservoir)
1621:Infiltration (hydrology)
295:Ordering and enumeration
1641:River Continuum Concept
1406:Agricultural wastewater
511:The water basin of the
1964:River name etymologies
1891:Hydraulic civilization
1749:Floodplain restoration
1525:Point source pollution
1300:Sedimentary structures
176:
59:
1576:Discharge (hydrology)
1538:Industrial wastewater
1019:Sedimentary processes
499:) cover larger areas.
309:Strahler stream order
158:
42:
1681:Volumetric flow rate
1265:Riffle-pool sequence
184:right-bank tributary
132:, where two or more
1855:Whitewater kayaking
1850:Whitewater canoeing
1651:Runoff curve number
1495:Flood pulse concept
301:source of the river
192:left-bank tributary
1881:Aquatic toxicology
1794:Stream restoration
1759:Infiltration basin
1611:Hydrological model
1127:Sediment transport
950:Estavelle/Inversac
828:Subterranean river
305:mouth of the river
265:cardinal direction
177:
60:
1977:
1976:
1954:Whitewater rivers
1860:Whitewater slalom
1691:River engineering
1591:Groundwater model
1552:River measurement
1480:Flood forecasting
1295:Sedimentary basin
1152:Fluvial landforms
1057:Bed material load
833:River bifurcation
647:978-0-313-31930-3
525:Mississippi River
416:) and tributaries
397:) and tributaries
350:The basin of the
18:Right tributaries
16:(Redirected from
2012:
1990:River morphology
1939:Rivers by length
1774:River morphology
1676:Wetted perimeter
1581:Drainage density
1092:Headward erosion
921:Perennial stream
793:Blackwater river
746:
739:
732:
723:
716:
715:
695:
689:
688:
682:
673:
664:
658:
652:
651:
631:
625:
624:
611:
605:
599:
593:
587:
536:
508:
490:
469:
425:
406:
387:
363:
347:
165:Shenandoah River
21:
2020:
2019:
2015:
2014:
2013:
2011:
2010:
2009:
1980:
1979:
1978:
1973:
1949:Drainage basins
1930:
1864:
1803:
1779:Retention basin
1739:Erosion control
1734:Detention basin
1685:
1601:Hjulström curve
1553:
1547:
1519:
1463:Non-water flood
1420:
1392:
1338:Helicoidal flow
1324:
1225:Fluvial terrace
1220:Floating island
1146:
1021:
1013:
1004:Rhythmic spring
938:
930:
911:Stream gradient
852:
838:River ecosystem
803:Channel pattern
771:
763:
750:
720:
719:
700:American Speech
697:
696:
692:
680:
675:
674:
667:
659:
655:
648:
633:
632:
628:
620:Merriam-Webster
613:
612:
608:
600:
596:
588:
584:
579:
567:
560:
537:
528:
509:
500:
484:
478:Tibetan Plateau
470:
461:
454:Xar Moron River
426:
417:
407:
398:
388:
379:
372:Adamawa Plateau
364:
355:
348:
336:
297:
219:early tributary
180:Right tributary
175:of the Potomac.
173:right tributary
153:
134:bodies of water
90:), river, or a
46:flows into the
37:
30:
23:
22:
15:
12:
11:
5:
2018:
2016:
2008:
2007:
2002:
1997:
1992:
1982:
1981:
1975:
1974:
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1971:
1966:
1961:
1956:
1951:
1946:
1941:
1935:
1932:
1931:
1929:
1928:
1923:
1918:
1913:
1908:
1903:
1898:
1893:
1888:
1883:
1878:
1872:
1870:
1866:
1865:
1863:
1862:
1857:
1852:
1847:
1842:
1840:Stone skipping
1837:
1832:
1827:
1822:
1817:
1811:
1809:
1805:
1804:
1802:
1801:
1796:
1791:
1786:
1781:
1776:
1771:
1766:
1761:
1756:
1751:
1746:
1741:
1736:
1731:
1726:
1724:Drop structure
1721:
1716:
1711:
1706:
1704:Balancing lake
1701:
1695:
1693:
1687:
1686:
1684:
1683:
1678:
1673:
1668:
1663:
1658:
1653:
1648:
1643:
1638:
1633:
1631:Playfair's law
1628:
1623:
1618:
1613:
1608:
1603:
1598:
1593:
1588:
1586:Exner equation
1583:
1578:
1573:
1571:Bradshaw model
1568:
1563:
1557:
1555:
1549:
1548:
1546:
1545:
1540:
1535:
1529:
1527:
1521:
1520:
1518:
1517:
1512:
1507:
1502:
1497:
1492:
1487:
1482:
1477:
1472:
1467:
1466:
1465:
1460:
1458:Urban flooding
1450:
1445:
1443:Crevasse splay
1440:
1438:100-year flood
1434:
1432:
1422:
1421:
1419:
1418:
1413:
1408:
1402:
1400:
1398:Surface runoff
1394:
1393:
1391:
1390:
1385:
1380:
1378:Stream capture
1375:
1370:
1365:
1360:
1355:
1350:
1345:
1340:
1334:
1332:
1326:
1325:
1323:
1322:
1317:
1312:
1307:
1302:
1297:
1292:
1290:Rock-cut basin
1287:
1282:
1277:
1272:
1267:
1262:
1257:
1252:
1247:
1242:
1237:
1232:
1227:
1222:
1217:
1212:
1207:
1202:
1197:
1192:
1187:
1182:
1177:
1172:
1167:
1162:
1156:
1154:
1148:
1147:
1145:
1144:
1139:
1134:
1132:Suspended load
1129:
1124:
1122:Secondary flow
1119:
1114:
1112:Retrogradation
1109:
1104:
1099:
1094:
1089:
1084:
1079:
1077:Dissolved load
1074:
1069:
1064:
1059:
1054:
1049:
1044:
1039:
1034:
1028:
1026:
1015:
1014:
1012:
1011:
1009:Spring horizon
1006:
1001:
996:
994:Mineral spring
991:
990:
989:
979:
978:
977:
975:list in the US
972:
962:
957:
952:
946:
944:
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931:
929:
928:
923:
918:
913:
908:
903:
901:Stream channel
898:
893:
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883:
878:
873:
868:
862:
860:
854:
853:
851:
850:
845:
840:
835:
830:
825:
823:Drainage basin
820:
815:
810:
805:
800:
795:
790:
785:
783:Alluvial river
779:
777:
765:
764:
751:
749:
748:
741:
734:
726:
718:
717:
712:10.2307/451418
690:
665:
653:
646:
626:
606:
594:
581:
580:
578:
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574:
573:
566:
563:
562:
561:
553:Triveni Sangam
538:
531:
529:
510:
503:
501:
471:
464:
462:
442:Dongliao River
427:
420:
418:
408:
401:
399:
389:
382:
380:
365:
358:
356:
349:
342:
340:
335:
332:
328:data structure
323:, stored as a
321:tree structure
296:
293:
246:American River
237:the midpoint.
231:late tributary
188:left tributary
152:
149:
104:drainage basin
28:
24:
14:
13:
10:
9:
6:
4:
3:
2:
2017:
2006:
2005:Water streams
2003:
2001:
1998:
1996:
1993:
1991:
1988:
1987:
1985:
1970:
1967:
1965:
1962:
1960:
1957:
1955:
1952:
1950:
1947:
1945:
1942:
1940:
1937:
1936:
1933:
1927:
1924:
1922:
1921:Surface water
1919:
1917:
1916:Sacred waters
1914:
1912:
1909:
1907:
1904:
1902:
1901:Riparian zone
1899:
1897:
1894:
1892:
1889:
1887:
1886:Body of water
1884:
1882:
1879:
1877:
1874:
1873:
1871:
1867:
1861:
1858:
1856:
1853:
1851:
1848:
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1841:
1838:
1836:
1835:Riverboarding
1833:
1831:
1830:River surfing
1828:
1826:
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1821:
1818:
1816:
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1700:
1697:
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1667:
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1649:
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1629:
1627:
1624:
1622:
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1617:
1614:
1612:
1609:
1607:
1604:
1602:
1599:
1597:
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1589:
1587:
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1582:
1579:
1577:
1574:
1572:
1569:
1567:
1564:
1562:
1559:
1558:
1556:
1554:and modelling
1550:
1544:
1541:
1539:
1536:
1534:
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1530:
1528:
1526:
1522:
1516:
1515:Return period
1513:
1511:
1508:
1506:
1503:
1501:
1498:
1496:
1493:
1491:
1488:
1486:
1483:
1481:
1478:
1476:
1475:Flood control
1473:
1471:
1470:Flood barrier
1468:
1464:
1461:
1459:
1456:
1455:
1454:
1451:
1449:
1446:
1444:
1441:
1439:
1436:
1435:
1433:
1431:
1427:
1423:
1417:
1414:
1412:
1409:
1407:
1404:
1403:
1401:
1399:
1395:
1389:
1386:
1384:
1381:
1379:
1376:
1374:
1371:
1369:
1366:
1364:
1361:
1359:
1356:
1354:
1351:
1349:
1346:
1344:
1341:
1339:
1336:
1335:
1333:
1331:
1327:
1321:
1318:
1316:
1313:
1311:
1308:
1306:
1303:
1301:
1298:
1296:
1293:
1291:
1288:
1286:
1283:
1281:
1278:
1276:
1273:
1271:
1268:
1266:
1263:
1261:
1258:
1256:
1253:
1251:
1248:
1246:
1243:
1241:
1238:
1236:
1233:
1231:
1228:
1226:
1223:
1221:
1218:
1216:
1213:
1211:
1208:
1206:
1203:
1201:
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1102:Palaeochannel
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1088:
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1080:
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1062:Granular flow
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808:Channel types
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788:Braided river
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687:. p. 15.
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19:
1959:Flash floods
1911:River cruise
1808:River sports
1661:Stream gauge
1646:Rouse number
1636:Relief ratio
1485:Flood-meadow
1416:Urban runoff
1330:Fluvial flow
1315:River valley
1285:River island
1250:Meander scar
1165:Alluvial fan
1107:Progradation
982:Karst spring
926:Winterbourne
881:Chalk stream
847:
843:River source
818:Distributary
703:
699:
693:
656:
636:
629:
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609:
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585:
513:Wabash River
450:Xiliao River
446:Xinkai River
352:Amazon River
318:
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200:navigational
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145:river deltas
141:distributary
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87:
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2000:Tributaries
1820:Fly fishing
1744:Fish ladder
1729:Daylighting
1448:Flash flood
1411:First flush
1358:Plunge pool
1082:Downcutting
1067:Debris flow
1042:Aggradation
916:Stream pool
590:"tributary"
485: [
458:Laoha River
438:Taizi River
368:Benue River
257:Steer Creek
151:Terminology
108:groundwater
1984:Categories
1926:Wild river
1606:Hydrograph
1596:Hack's law
1561:Baer's law
1505:Inundation
1490:Floodplain
1430:stormwater
1388:Whitewater
1260:Oxbow lake
1097:Knickpoint
1072:Deposition
965:Hot spring
906:Streamflow
896:Stream bed
813:Confluence
706:(3): 191.
602:"affluent"
577:References
517:Ohio River
430:Liao River
391:Huai River
130:confluence
1896:Limnology
1845:Triathlon
1815:Canyoning
1784:Revetment
1714:Check dam
1626:Main stem
1383:Waterfall
1270:Point bar
1255:Mouth bar
1195:Billabong
1142:Water gap
1137:Wash load
1117:Saltation
1037:Anabranch
960:Holy well
848:Tributary
557:Allahabad
497:Mun River
434:Hun River
313:hierarchy
212:turbulent
83:main stem
64:tributary
1699:Aqueduct
1566:Baseflow
1533:Effluent
1210:Cut bank
1175:Avulsion
1052:Bed load
1032:Abrasion
565:See also
482:ngom chu
456:and the
273:cataract
227:midpoint
208:opposite
88:"parent"
69:affluent
66:, or an
44:Nam Khan
1876:Aquifer
1869:Related
1825:Rafting
1353:Meander
1348:Log jam
1310:Thalweg
1215:Estuary
1087:Erosion
1024:erosion
936:Springs
891:Current
858:Streams
798:Channel
761:springs
757:streams
571:Estuary
414:Yangtze
395:Yangtze
334:Gallery
72:, is a
1995:Rivers
1671:WAFLEX
1543:Sewage
1426:Floods
1368:Riffle
1363:Rapids
1305:Strath
1275:Ravine
1200:Canyon
955:Geyser
886:Coulee
871:Bourne
866:Arroyo
769:Rivers
753:Rivers
644:
545:Ganges
541:Yamuna
493:gorges
474:Mekong
307:. The
285:little
269:middle
223:before
186:, and
115:Irtysh
74:stream
48:Mekong
1769:Levee
1754:Flume
1709:Canal
1453:Flood
1373:Shoal
1240:Gully
1235:Gulch
1205:Chine
1190:Bayou
1047:Armor
999:Ponor
774:lists
681:(PDF)
549:India
521:forks
489:]
376:Niger
281:lower
277:upper
242:forks
235:after
190:, or
182:, or
100:ocean
78:river
1799:Weir
1764:Leat
1428:and
1320:Wadi
1280:Rill
1245:Glen
1230:Gill
1180:Bank
1022:and
987:list
970:list
941:list
876:Burn
759:and
642:ISBN
539:The
472:The
428:The
366:The
325:tree
229:; a
204:raft
113:The
92:lake
56:Laos
1719:Dam
1185:Bar
1160:Ait
708:doi
291:.
289:big
217:An
159:At
98:or
96:sea
86:or
76:or
54:in
50:at
1986::
755:,
704:14
702:.
683:.
668:^
617:.
559:.
555:,
487:zh
452:,
448:,
444:,
440:,
436:,
330:.
147:.
128:A
119:Ob
62:A
943:)
939:(
776:)
772:(
745:e
738:t
731:v
714:.
710::
650:.
623:.
527:.
378:.
58:.
36:.
20:)
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