38:
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2100:
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method, the drainage basin is divided into polygons with the rain gauge in the middle of each polygon assumed to be representative for the rainfall on the area of land included in its polygon. These polygons are made by drawing lines between gauges, then making perpendicular bisectors of those lines
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The non-karstic impluvium comprises all elements of the ground surface and soils that are poorly permeable, on a part of which water is running while also infiltrating on another minor part. This superficial impluvium, if it exists, constitutes the first level of organization of the drainage system
705:
As water flows through the basin, it can form tributaries that change the structure of the land. There are three different main types, which are affected by the rocks and ground underneath. Rock that is quick to erode forms dendritic patterns, and these are seen most often. The two other types of
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located at the basin's outlet. Depending on the conditions of the drainage basin, as rainfall occurs some of it seeps directly into the ground. This water will either remain underground, slowly making its way downhill and eventually reaching the basin, or it will permeate deeper into the soil and
986:, meaning that any further rainfall will reach the river rather than being absorbed by the ground. If the surface is impermeable the precipitation will create surface run-off which will lead to higher risk of flooding; if the ground is permeable, the precipitation will infiltrate the soil.
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In order to preserve the long-term stability and purity of natural mineral water, bottlers have put in place "protection policies" for the impluviums (or catchment areas) of their sources. The catchment area is the territory on which the part of precipitated rainwater and/or
696:
system beneath the drainage basin may flow towards the outlet of another drainage basin because groundwater flow directions do not always match those of their overlying drainage network. Measurement of the discharge of water from a basin may be made by a
1517:
709:
Rain gauge data is used to measure total precipitation over a drainage basin, and there are different ways to interpret that data. If the gauges are many and evenly distributed over an area of uniform precipitation, using the
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Size will help determine the amount of water reaching the river, as the larger the catchment the greater the potential for flooding. It is also determined on the basis of length and width of the drainage basin.
1302:
that infiltrates the subsoil feeds the mineral aquifer and thus contributes to the renewal of the resource. In other words, a precipitated drop on the impluvium territory may join the mineral aquifer; ...
1272:
Efficient management is strongly correlated to the proper protection perimeter definition around springs and proactive regulation of land uses over the spring's catchment area ("impluvium").
838:, has affected the mouths of drainage basins. The minerals are carried by the drainage basin to the mouth, and may accumulate there, disturbing the natural mineral balance. This can cause
526:
or vary dramatically in size depending on climate and inflow. If water evaporates or infiltrates into the ground at its terminus, the area can go by several names, such playa, salt flat,
179:. Hydrologic units are defined to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins.
1006:. A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean.
1509:
1088: – type of water basin or retention area, implying a natural or geologic cistern in rock which retains water; often created by erosional processes within intermittent streams
723:
method involves contours of equal precipitation are drawn over the gauges on a map. Calculating the area between these curves and adding up the volume of water is time-consuming.
2136:
4031:
609:
Drainage basins have been historically important for determining territorial boundaries, particularly in regions where trade by water has been important. For example, the
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can be almost impermeable and therefore rainfall on clay soils will run off and contribute to flood volumes. After prolonged rainfall even free-draining soils can become
876:, the National Policy of Water Resources, regulated by Act n° 9.433 of 1997, establishes the drainage basin as the territorial division of Brazilian water management.
641:) or other political entities in a particular drainage basin to manage the body or bodies of water into which it drains. Examples of such interstate compacts are the
424:, and Canada and the United States west of the Continental Divide (including most of Alaska), as well as western Central America and South America west of the Andes.
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Because drainage basins are coherent entities in a hydrological sense, it has become common to manage water resources on the basis of individual basins. In the
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974:
Soil type will help determine how much water reaches the river. The runoff from the drainage area is dependent on the soil type. Certain soil types such as
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811:. With the water, they are transported towards the outlet of the basin, and can affect the ecological processes along the way as well as in the receiving
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Shape will contribute to the speed with which the runoff reaches a river. A long thin catchment will take longer to drain than a circular catchment.
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1619:
2735:
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1285:
4079:
4011:
1242:
Huneau, F.; Jaunat, J.; Kavouri, K.; Plagnes, V.; Rey, F.; Dörfliger, N. (2013-07-18). "Intrinsic vulnerability mapping for small mountainous
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When a river basin crosses at least one political border, either a border within a nation or an international boundary, it is identified as a
1629:
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where evaporation is the primary means of water loss, the water is typically more saline than the oceans. An extreme example of this is the
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are inland basins that do not drain to an ocean. Endorheic basins cover around 18% of the Earth's land. Some endorheic basins drain to an
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4074:
1601:
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1031:
781:
366:
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Land use can contribute to the volume of water reaching the river, in a similar way to clay soils. For example, rainfall on roofs,
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37:
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585:. Some of these, such as the Great Basin, are not single drainage basins but collections of separate, adjacent closed basins.
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areas will reach the primary river in the drainage basin faster than flat or lightly sloping areas (e.g., > 1% gradient).
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776:
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soils are very free-draining, and rainfall on sandy soil is likely to be absorbed by the ground. However, soils containing
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to reach the river, while catchment size, soil type, and development determine the amount of water to reach the river.
4235:
3979:
3336:
864:". In New Zealand, they are called catchment boards. Comparable community groups based in Ontario, Canada, are called
689:
142:, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide.
431:'s drainage basin also comprises about 13% of Earth's land. It drains the eastern coast of Africa, the coasts of the
902:
Management of shared drainage basins is also seen as a way to build lasting peaceful relationships among countries.
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2562:
1700:
685:. Finding the area and extent of a drainage basin is an important step in many areas of science and engineering.
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3298:
3181:
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1747:
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that moves from higher elevation through the river system to lower elevations as they reshape the channel forms.
240:
1446:
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within a drainage basin to reach a lake, reservoir or outlet, assuming constant and uniform effective rainfall.
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3048:
3013:
2855:
3754:
3341:
3033:
2798:
1917:
1577:
896:
614:
1726:
1391:"Global system of rivers: Its role in organizing continental land mass and defining land-to-ocean linkages"
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884:
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682:
287:
146:
1653:
1563:"A grid-based distributed flood forecasting model for use with weather radar data: Part 1. Formulation"
945:
Generally, topography plays a big part in how fast runoff will reach a river. Rain that falls in steep
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regions. Agricultural runoff and other water pollution that flows to the outlet is the cause of the
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156:, rather than flowing to the ocean, water converges toward the interior of the basin, known as a
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785:
677:, the drainage basin is a logical unit of focus for studying the movement of water within the
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306:, the islands of the Caribbean and the Gulf, and a small part of northern South America. The
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479:(3.17M km). The three rivers that drain the most water, from most to least, are the Amazon,
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30:"Catchment" and "Catchment basin" redirect here. For the human geography concept, see
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The catchment is the most significant factor determining the amount or likelihood of
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883:. Management of such basins becomes the responsibility of the countries sharing it.
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The five largest river basins (by area), from largest to smallest, are those of the
175:, which are drainage areas delineated so as to nest into a multi-level hierarchical
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aquifers, implementation of the new PaPRIKa method to
Western Pyrenees (France)".
760:
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2014:
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1314:
Labat, D.; Ababou, R.; Manginb, A. (2000-12-05). "Rainfall–runoff relations for
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are a few examples of arrangements involving management of shared river basins.
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693:
633:
political organization today includes agreements of states (e.g., international
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412:. Its basin includes much of China, eastern and southeastern Russia, Japan, the
228:
202:, showing how terrestrial drainage basins drain into the oceans. Grey areas are
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2019:
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The majority of water that discharges from the basin outlet originated as
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416:, most of Indochina, Indonesia and Malaysia, the Philippines, all of the
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Vörösmarty, C. J.; Fekete, B. M.; Meybeck, M.; Lammers, R. B. (2000).
1363:. Virginia Department of Conservation & Recreation. Archived from
3903:
3694:
3684:
3580:
3063:
2935:
2760:
2755:
2707:
2697:
2667:
2592:
2347:
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2250:
2149:
1955:
1902:
1897:
1649:
1200:"A Review of Earth Observation-Based Analyses for Major River Basins"
1085:
873:
634:
578:
480:
370:
339:
335:
319:
933:
areas). Catchment topography and shape determine the time taken for
1739:
706:
patterns that form are trellis patterns and rectangular patterns.
3744:
3699:
3689:
3669:
3620:
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3161:
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2391:
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1472:
1315:
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775:
759:
656:
582:
549:, and numerous smaller lakes. Other endorheic regions include the
490:
347:
248:
193:
96:
86:
36:
799:. As water flows over the ground and along rivers it can pick up
3898:
3719:
3595:
3191:
3156:
2712:
2672:
2637:
1993:
1034: – Principal hydrological divide of North and South America
999:
979:
975:
934:
930:
922:
888:
768:
drainage basin. The dashed line is the main water divide of the
741:
Drainage basins are the principal hydrologic unit considered in
538:
402:
100:
89:. A basin is separated from adjacent basins by a perimeter, the
82:
3376:
2118:
1743:
1002:
will be collected by rivers with almost no absorption into the
860:, governmental entities that perform this function are called "
681:. The process of finding a drainage boundary is referred to as
3538:
3449:
3111:
2552:
1983:
842:
where plant growth is accelerated by the additional material.
692:
falling on the basin. A portion of the water that enters the
103:. A basin may consist of smaller basins that merge at river
3372:
149:, a common task in environmental engineering and science.
1725:
bin Talal, Hassan; Waslekar, Sundeep (25 November 2013).
1046: – transfer of water from one river basin to another
95:, made up of a succession of elevated features, such as
1125:. University of Wisconsin–Stevens Point. Archived from
1082: – The forking of a river into its distributaries
1318:
springs. Part I: convolution and spectral analyses".
868:. In North America, this function is referred to as "
408:
Just over 13% of the land in the world drains to the
393:
in Europe, central and northern Russia, and parts of
286:
basin includes most of the U.S. interior between the
1198:
Uereyen, Soner; Kuenzer, Claudia (9 December 2019).
1090:
Pages displaying wikidata descriptions as a fallback
1048:
Pages displaying wikidata descriptions as a fallback
4107:
4052:
3993:
3965:
3934:
3881:
3853:
3813:
3417:
3410:
3261:
3200:
3082:
2944:
2916:
2817:
2789:
2721:
2543:
2410:
2327:
2249:
2160:
2043:
2007:
1974:
1946:
1828:
1777:
1607:from the original on Jan 18, 2024 – via HAL.
1166:
27:Land area where water converges to a common outlet
1701:"Twin Cities Metropolitan Area (TCMA) Watersheds"
1486:"drainage basin Definition, Example, & Facts"
1384:
1382:
405:, which totals to about 17% of the world's land.
171:Drainage basins are similar but not identical to
1070: – Final large channel of a riverine system
145:A drainage basin's boundaries are determined by
1053:International Journal of River Basin Management
748:. A drainage basin is the source for water and
223:, surface water drains to the Atlantic via the
215:About 48.71% of the world's land drains to the
138:. In North America, they are commonly called a
3975:A Directory of Important Wetlands in Australia
4060:Bangladesh Haor and Wetland Development Board
3985:Ramsar Classification System for Wetland Type
3388:
2130:
1755:
1237:
1235:
472:
389:in the United States, the north shore of the
251:also drains to the Atlantic, as does most of
8:
1141:"What is a watershed and why should I care?"
1063:International Network of Basin Organizations
537:The largest endorheic basins are in Central
294:, a small part of the Canadian provinces of
278:of the world also flow to the Atlantic. The
2086:List of rivers that have reversed direction
3999:
3414:
3395:
3381:
3373:
2137:
2123:
2115:
1762:
1748:
1740:
1355:
1353:
1595:
1585:
1414:
1223:
1143:. University of Delaware. Archived from
2736:International scale of river difficulty
1110:
729:can be used to show the time taken for
702:consolidate into groundwater aquifers.
73:converges to a single point, such as a
4080:Meadowview Biological Research Station
4012:Greenhouse gas emissions from wetlands
1727:"Water Cooperation for a Secure World"
1447:"Largest Drainage Basins in the World"
714:method will give good results. In the
114:Other terms for a drainage basin are
69:is an area of land where all flowing
7:
1475:Published by Microsoft in computers.
259:and the greatest portion of western
164:, or a point where surface water is
4075:Irish Peatland Conservation Council
1570:Hydrology and Earth System Sciences
1284:Lachassagne, Patrick (2019-02-07).
187:For a more comprehensive list, see
160:, which may be a permanent lake, a
1705:Minnesota Pollution Control Agency
1561:Bell, V. A.; Moore, R. J. (1998).
1550:from the original on Apr 15, 2024.
1076: – Water resources management
1032:Continental Divide of the Americas
553:in the United States, much of the
183:Major drainage basins of the world
25:
1624:. Tata McGraw-Hill. p. 298.
1463:Encarta Encyclopedia articles on
1288:. Encyclopédie de l'environnement
795:Drainage basins are important in
4200:
4199:
4188:
2099:
2098:
1510:"Watersheds and Drainage Basins"
1016:
3571:Flooded grasslands and savannas
2893:Flooded grasslands and savannas
1795:Drainage system (geomorphology)
1520:from the original on 2021-10-22
1038:Integrated catchment management
206:that do not drain to the oceans
189:List of drainage basins by area
152:In a closed drainage basin, or
45:drains the largest area of any
1805:Strahler number (stream order)
1040: – Environmental planning
647:Tahoe Regional Planning Agency
1:
4095:Wildfowl & Wetlands Trust
4085:Society of Wetland Scientists
1340:10.1016/S0022-1694(00)00321-8
3710:Peatland, mire, and quagmire
3059:Universal Soil Loss Equation
3009:Hydrological transport model
2903:Storm Water Management Model
1546:. BCcampus Open Publishing.
1538:Earle, Steven (2015-09-01).
1395:Global Biogeochemical Cycles
1268:10.1016/j.enggeo.2013.03.028
1173:. Checkmark Books. pp.
1074:River basin management plans
557:, the drainage basin of the
3980:National Wetlands Inventory
1361:"Hydrologic Unit Geography"
764:Top-down illustration of a
443:, Burma, and most parts of
338:, and the coastal areas of
4277:
4065:Delta Waterfowl Foundation
2563:Antecedent drainage stream
1731:www.strategicforesight.com
1169:The Field Guide to Geology
849:
522:. Many of these lakes are
504:
235:of the United States, the
186:
29:
4256:Water and the environment
4183:
4002:
3327:
3299:River valley civilization
3182:Riparian-zone restoration
2094:
487:Endorheic drainage basins
473:
420:, the northeast coast of
241:Newfoundland and Labrador
4044:Wetland indicator status
3362:Countries without rivers
3337:Rivers by discharge rate
3049:Runoff model (reservoir)
3014:Infiltration (hydrology)
1286:"Natural mineral waters"
1123:The Physical Environment
866:conservation authorities
77:, or flows into another
3755:Freshwater swamp forest
3034:River Continuum Concept
2799:Agricultural wastewater
1918:River channel migration
1646:"EN 0705 isochrone map"
1597:10.5194/hess-2-265-1998
1578:Copernicus Publications
1490:Encyclopedia Britannica
1165:Lambert, David (1998).
917:Catchment factors are:
897:Mekong River Commission
858:U.S. state of Minnesota
719:form the polygons. The
605:Geopolitical boundaries
4090:Wetlands International
3861:List of wetland plants
3357:River name etymologies
3284:Hydraulic civilization
3142:Floodplain restoration
2918:Point source pollution
2693:Sedimentary structures
1848:Bar (river morphology)
1618:Subramanya, K (2008).
1540:"13.2 Drainage Basins"
1514:U.S. Geological Survey
820:artificial fertilizers
792:
773:
670:
661:Drainage basin of the
643:Great Lakes Commission
625:basin, an area called
565:), highlands near the
502:
391:Scandinavian peninsula
207:
62:
3735:Salt pannes and pools
2969:Discharge (hydrology)
2931:Industrial wastewater
2412:Sedimentary processes
2030:Erosion and tectonics
2025:Degradation (geology)
1621:Engineering Hydrology
1345:of the karstic basin.
1095:Time of concentration
885:Nile Basin Initiative
850:Further information:
788:'s drainage basin in
779:
763:
683:watershed delineation
660:
494:
197:
147:watershed delineation
55:hypoxic, or dead zone
40:
3074:Volumetric flow rate
2658:Riffle-pool sequence
2051:Deposition (geology)
1778:Large-scale features
1656:on November 22, 2012
1416:10.1029/1999GB900092
1320:Journal of Hydrology
870:watershed management
852:Watershed management
637:and, within the US,
615:Hudson's Bay Company
483:, and Congo rivers.
471:(3.22M km), and the
451:Largest river basins
225:Saint Lawrence River
173:hydrologic unit code
109:hierarchical pattern
4195:Wetlands portal
3826:Constructed wetland
3411:Types and landforms
3248:Whitewater kayaking
3243:Whitewater canoeing
3044:Runoff curve number
2888:Flood pulse concept
1587:1998HESS....2..265B
1407:2000GBioC..14..599V
1367:on 14 December 2012
1332:2000JHyd..238..123L
1260:2013EngGe.161...81H
1254:. Elsevier: 81–93.
1248:Engineering Geology
1216:2019RemS...11.2951U
1100:Catchment hydrology
1044:Interbasin transfer
881:transboundary river
862:watershed districts
846:Resource management
639:interstate compacts
569:, the interiors of
567:African Great Lakes
441:Indian subcontinent
314:, includes much of
200:continental divides
18:Watershed (ecology)
4236:Freshwater ecology
4039:Salt marsh die-off
3957:Salt marsh dieback
3866:List of fen plants
3705:Palustrine wetland
3606:Intertidal wetland
3601:Interdunal wetland
3274:Aquatic toxicology
3187:Stream restoration
3152:Infiltration basin
3004:Hydrological model
2520:Sediment transport
2343:Estavelle/Inversac
2221:Subterranean river
2081:Sediment transport
2035:River rejuvenation
2008:Regional processes
1225:10.3390/rs11242951
1129:on March 21, 2004.
793:
774:
679:hydrological cycle
671:
617:a monopoly on the
503:
367:Continental Divide
276:mediterranean seas
261:Sub-Saharan Africa
237:Canadian Maritimes
208:
63:
49:river, much of it
4231:Fluvial landforms
4213:
4212:
4115:Aquatic ecosystem
4103:
4102:
4022:Ramsar Convention
3849:
3848:
3831:Converted wetland
3773:Peat swamp forest
3636:Inland salt marsh
3370:
3369:
3347:Whitewater rivers
3253:Whitewater slalom
3084:River engineering
2984:Groundwater model
2945:River measurement
2873:Flood forecasting
2688:Sedimentary basin
2545:Fluvial landforms
2450:Bed material load
2226:River bifurcation
2112:
2111:
1913:River bifurcation
1631:978-0-07-064855-5
1080:River bifurcation
906:Catchment factors
667:Mississippi River
575:Arabian Peninsula
308:Mediterranean Sea
43:Mississippi River
16:(Redirected from
4268:
4203:
4202:
4193:
4192:
4191:
4175:Will-o'-the-wisp
4108:Related articles
4000:
3800:Whitewater river
3750:Coniferous swamp
3631:Freshwater marsh
3524:Clearwater river
3440:Blackwater river
3415:
3397:
3390:
3383:
3374:
3332:Rivers by length
3167:River morphology
3069:Wetted perimeter
2974:Drainage density
2485:Headward erosion
2314:Perennial stream
2186:Blackwater river
2139:
2132:
2125:
2116:
2102:
2101:
1843:Avulsion (river)
1771:River morphology
1764:
1757:
1750:
1741:
1735:
1734:
1722:
1716:
1715:
1713:
1712:
1697:
1691:
1690:
1688:
1687:
1678:. Archived from
1672:
1666:
1665:
1663:
1661:
1652:. Archived from
1642:
1636:
1635:
1615:
1609:
1608:
1606:
1599:
1589:
1567:
1558:
1552:
1551:
1544:Physical Geology
1535:
1529:
1528:
1526:
1525:
1516:. June 8, 2019.
1506:
1500:
1499:
1497:
1496:
1482:
1476:
1461:
1455:
1454:
1443:
1437:
1436:
1418:
1386:
1377:
1376:
1374:
1372:
1357:
1348:
1347:
1326:(3–4): 123–148.
1311:
1305:
1304:
1294:
1293:
1281:
1275:
1274:
1239:
1230:
1229:
1227:
1195:
1189:
1188:
1172:
1162:
1156:
1155:
1153:
1152:
1137:
1131:
1130:
1119:"drainage basin"
1115:
1091:
1058:
1049:
1026:
1021:
1020:
1019:
716:Thiessen polygon
541:, including the
478:
477:
414:Korean Peninsula
310:basin, with the
243:. Nearly all of
233:Eastern Seaboard
204:endorheic basins
166:lost underground
21:
4276:
4275:
4271:
4270:
4269:
4267:
4266:
4265:
4226:Drainage basins
4216:
4215:
4214:
4209:
4189:
4187:
4179:
4099:
4070:Ducks Unlimited
4048:
4007:Clean Water Act
3989:
3967:Classifications
3961:
3930:
3877:
3845:
3809:
3760:Mangrove forest
3406:
3401:
3371:
3366:
3342:Drainage basins
3323:
3257:
3196:
3172:Retention basin
3132:Erosion control
3127:Detention basin
3078:
2994:Hjulström curve
2946:
2940:
2912:
2856:Non-water flood
2813:
2785:
2731:Helicoidal flow
2717:
2618:Fluvial terrace
2613:Floating island
2539:
2414:
2406:
2397:Rhythmic spring
2331:
2323:
2304:Stream gradient
2245:
2231:River ecosystem
2196:Channel pattern
2164:
2156:
2143:
2113:
2108:
2090:
2071:Helicoidal flow
2039:
2003:
1970:
1942:
1858:Channel pattern
1830:Alluvial rivers
1824:
1820:River sinuosity
1773:
1768:
1738:
1724:
1723:
1719:
1710:
1708:
1699:
1698:
1694:
1685:
1683:
1674:
1673:
1669:
1659:
1657:
1644:
1643:
1639:
1632:
1617:
1616:
1612:
1604:
1565:
1560:
1559:
1555:
1537:
1536:
1532:
1523:
1521:
1508:
1507:
1503:
1494:
1492:
1484:
1483:
1479:
1462:
1458:
1445:
1444:
1440:
1388:
1387:
1380:
1370:
1368:
1359:
1358:
1351:
1313:
1312:
1308:
1291:
1289:
1283:
1282:
1278:
1241:
1240:
1233:
1197:
1196:
1192:
1185:
1164:
1163:
1159:
1150:
1148:
1139:
1138:
1134:
1117:
1116:
1112:
1108:
1089:
1056:
1047:
1024:Wetlands portal
1022:
1017:
1015:
1012:
992:
972:
963:
955:
943:
921:, shape, size,
908:
854:
848:
758:
739:
712:arithmetic mean
655:
613:crown gave the
607:
602:
590:bodies of water
577:, and parts in
512:Endorheic basin
509:
507:Endorheic basin
496:Endorheic basin
489:
475:RĂo de la Plata
467:(3.4M km), the
453:
418:Pacific Islands
363:Northern Canada
357:drains most of
330:, Central, and
318:, east-central
304:Central America
292:Rocky Mountains
213:
192:
185:
177:drainage system
154:endorheic basin
120:catchment basin
92:drainage divide
35:
28:
23:
22:
15:
12:
11:
5:
4274:
4272:
4264:
4263:
4258:
4253:
4248:
4243:
4238:
4233:
4228:
4218:
4217:
4211:
4210:
4208:
4207:
4197:
4184:
4181:
4180:
4178:
4177:
4172:
4167:
4162:
4157:
4152:
4147:
4145:Drainage basin
4142:
4137:
4132:
4127:
4122:
4117:
4111:
4109:
4105:
4104:
4101:
4100:
4098:
4097:
4092:
4087:
4082:
4077:
4072:
4067:
4062:
4056:
4054:
4050:
4049:
4047:
4046:
4041:
4036:
4035:
4034:
4024:
4019:
4014:
4009:
4003:
3997:
3991:
3990:
3988:
3987:
3982:
3977:
3971:
3969:
3963:
3962:
3960:
3959:
3954:
3952:Paludification
3949:
3944:
3938:
3936:
3932:
3931:
3929:
3928:
3923:
3918:
3913:
3912:
3911:
3906:
3904:Sapric or muck
3901:
3891:
3885:
3883:
3882:Soil mechanics
3879:
3878:
3876:
3875:
3868:
3863:
3857:
3855:
3851:
3850:
3847:
3846:
3844:
3843:
3838:
3833:
3828:
3823:
3817:
3815:
3811:
3810:
3808:
3807:
3802:
3797:
3792:
3787:
3782:
3781:
3780:
3775:
3770:
3762:
3757:
3752:
3742:
3737:
3732:
3727:
3722:
3717:
3712:
3707:
3702:
3697:
3692:
3687:
3682:
3677:
3672:
3667:
3662:
3661:
3660:
3659:
3658:
3653:
3643:
3638:
3633:
3628:
3626:Brackish marsh
3618:
3613:
3608:
3603:
3598:
3593:
3588:
3583:
3578:
3573:
3568:
3563:
3558:
3557:
3556:
3551:
3546:
3536:
3531:
3526:
3521:
3516:
3515:
3514:
3504:
3499:
3498:
3497:
3492:
3487:
3482:
3477:
3472:
3467:
3462:
3457:
3447:
3442:
3437:
3432:
3427:
3421:
3419:
3412:
3408:
3407:
3402:
3400:
3399:
3392:
3385:
3377:
3368:
3367:
3365:
3364:
3359:
3354:
3349:
3344:
3339:
3334:
3328:
3325:
3324:
3322:
3321:
3316:
3311:
3306:
3301:
3296:
3291:
3286:
3281:
3276:
3271:
3265:
3263:
3259:
3258:
3256:
3255:
3250:
3245:
3240:
3235:
3233:Stone skipping
3230:
3225:
3220:
3215:
3210:
3204:
3202:
3198:
3197:
3195:
3194:
3189:
3184:
3179:
3174:
3169:
3164:
3159:
3154:
3149:
3144:
3139:
3134:
3129:
3124:
3119:
3117:Drop structure
3114:
3109:
3104:
3099:
3097:Balancing lake
3094:
3088:
3086:
3080:
3079:
3077:
3076:
3071:
3066:
3061:
3056:
3051:
3046:
3041:
3036:
3031:
3026:
3024:Playfair's law
3021:
3016:
3011:
3006:
3001:
2996:
2991:
2986:
2981:
2979:Exner equation
2976:
2971:
2966:
2964:Bradshaw model
2961:
2956:
2950:
2948:
2942:
2941:
2939:
2938:
2933:
2928:
2922:
2920:
2914:
2913:
2911:
2910:
2905:
2900:
2895:
2890:
2885:
2880:
2875:
2870:
2865:
2860:
2859:
2858:
2853:
2851:Urban flooding
2843:
2838:
2836:Crevasse splay
2833:
2831:100-year flood
2827:
2825:
2815:
2814:
2812:
2811:
2806:
2801:
2795:
2793:
2791:Surface runoff
2787:
2786:
2784:
2783:
2778:
2773:
2771:Stream capture
2768:
2763:
2758:
2753:
2748:
2743:
2738:
2733:
2727:
2725:
2719:
2718:
2716:
2715:
2710:
2705:
2700:
2695:
2690:
2685:
2683:Rock-cut basin
2680:
2675:
2670:
2665:
2660:
2655:
2650:
2645:
2640:
2635:
2630:
2625:
2620:
2615:
2610:
2605:
2600:
2595:
2590:
2585:
2580:
2575:
2570:
2565:
2560:
2555:
2549:
2547:
2541:
2540:
2538:
2537:
2532:
2527:
2525:Suspended load
2522:
2517:
2515:Secondary flow
2512:
2507:
2505:Retrogradation
2502:
2497:
2492:
2487:
2482:
2477:
2472:
2470:Dissolved load
2467:
2462:
2457:
2452:
2447:
2442:
2437:
2432:
2427:
2421:
2419:
2408:
2407:
2405:
2404:
2402:Spring horizon
2399:
2394:
2389:
2387:Mineral spring
2384:
2383:
2382:
2372:
2371:
2370:
2368:list in the US
2365:
2355:
2350:
2345:
2339:
2337:
2325:
2324:
2322:
2321:
2316:
2311:
2306:
2301:
2296:
2294:Stream channel
2291:
2286:
2281:
2276:
2271:
2266:
2261:
2255:
2253:
2247:
2246:
2244:
2243:
2238:
2233:
2228:
2223:
2218:
2216:Drainage basin
2213:
2208:
2203:
2198:
2193:
2188:
2183:
2178:
2176:Alluvial river
2172:
2170:
2158:
2157:
2144:
2142:
2141:
2134:
2127:
2119:
2110:
2109:
2107:
2106:
2095:
2092:
2091:
2089:
2088:
2083:
2078:
2076:Playfair's law
2073:
2068:
2063:
2061:Exner equation
2058:
2053:
2047:
2045:
2041:
2040:
2038:
2037:
2032:
2027:
2022:
2017:
2011:
2009:
2005:
2004:
2002:
2001:
1999:Current ripple
1996:
1991:
1986:
1980:
1978:
1972:
1971:
1969:
1968:
1963:
1958:
1952:
1950:
1944:
1943:
1941:
1940:
1935:
1930:
1928:Slip-off slope
1925:
1920:
1915:
1910:
1905:
1900:
1895:
1890:
1885:
1880:
1878:Meander cutoff
1875:
1870:
1865:
1860:
1855:
1850:
1845:
1840:
1834:
1832:
1826:
1825:
1823:
1822:
1817:
1812:
1807:
1802:
1797:
1792:
1790:Drainage basin
1787:
1785:Alluvial plain
1781:
1779:
1775:
1774:
1769:
1767:
1766:
1759:
1752:
1744:
1737:
1736:
1717:
1692:
1676:"Isochron Map"
1667:
1637:
1630:
1610:
1553:
1530:
1501:
1477:
1456:
1453:. 17 May 2018.
1438:
1401:(2): 599–621.
1378:
1349:
1306:
1276:
1231:
1204:Remote Sensing
1190:
1183:
1157:
1132:
1109:
1107:
1104:
1103:
1102:
1097:
1092:
1083:
1077:
1071:
1065:
1060:
1050:
1041:
1035:
1028:
1027:
1011:
1008:
991:
988:
971:
968:
962:
959:
954:
951:
942:
939:
907:
904:
847:
844:
840:eutrophication
818:Modern use of
786:Latorița River
757:
754:
738:
735:
727:Isochrone maps
669:drainage basin
665:, part of the
654:
651:
621:in the entire
606:
603:
601:
598:
563:Kalahari Basin
559:Okavango River
516:Endorheic lake
505:Main article:
488:
485:
452:
449:
359:Western Canada
332:Eastern Europe
284:Gulf of Mexico
274:The two major
265:Western Sahara
257:Central Europe
239:, and most of
217:Atlantic Ocean
212:
209:
184:
181:
116:catchment area
67:drainage basin
59:Gulf of Mexico
32:Catchment area
26:
24:
14:
13:
10:
9:
6:
4:
3:
2:
4273:
4262:
4261:Water streams
4259:
4257:
4254:
4252:
4249:
4247:
4244:
4242:
4241:Geomorphology
4239:
4237:
4234:
4232:
4229:
4227:
4224:
4223:
4221:
4206:
4198:
4196:
4186:
4185:
4182:
4176:
4173:
4171:
4168:
4166:
4163:
4161:
4158:
4156:
4155:Riparian zone
4153:
4151:
4148:
4146:
4143:
4141:
4138:
4136:
4133:
4131:
4128:
4126:
4123:
4121:
4118:
4116:
4113:
4112:
4110:
4106:
4096:
4093:
4091:
4088:
4086:
4083:
4081:
4078:
4076:
4073:
4071:
4068:
4066:
4063:
4061:
4058:
4057:
4055:
4053:Organizations
4051:
4045:
4042:
4040:
4037:
4033:
4030:
4029:
4028:
4025:
4023:
4020:
4018:
4015:
4013:
4010:
4008:
4005:
4004:
4001:
3998:
3996:
3992:
3986:
3983:
3981:
3978:
3976:
3973:
3972:
3970:
3968:
3964:
3958:
3955:
3953:
3950:
3948:
3945:
3943:
3940:
3939:
3937:
3933:
3927:
3924:
3922:
3919:
3917:
3914:
3910:
3909:Tropical peat
3907:
3905:
3902:
3900:
3897:
3896:
3895:
3892:
3890:
3887:
3886:
3884:
3880:
3874:
3873:
3869:
3867:
3864:
3862:
3859:
3858:
3856:
3852:
3842:
3839:
3837:
3834:
3832:
3829:
3827:
3824:
3822:
3819:
3818:
3816:
3812:
3806:
3803:
3801:
3798:
3796:
3793:
3791:
3790:Várzea forest
3788:
3786:
3783:
3779:
3776:
3774:
3771:
3769:
3767:
3763:
3761:
3758:
3756:
3753:
3751:
3748:
3747:
3746:
3743:
3741:
3738:
3736:
3733:
3731:
3728:
3726:
3723:
3721:
3718:
3716:
3713:
3711:
3708:
3706:
3703:
3701:
3698:
3696:
3693:
3691:
3688:
3686:
3683:
3681:
3678:
3676:
3673:
3671:
3668:
3666:
3663:
3657:
3654:
3652:
3649:
3648:
3647:
3644:
3642:
3639:
3637:
3634:
3632:
3629:
3627:
3624:
3623:
3622:
3619:
3617:
3614:
3612:
3609:
3607:
3604:
3602:
3599:
3597:
3594:
3592:
3589:
3587:
3584:
3582:
3579:
3577:
3574:
3572:
3569:
3567:
3564:
3562:
3559:
3555:
3552:
3550:
3547:
3545:
3542:
3541:
3540:
3537:
3535:
3532:
3530:
3527:
3525:
3522:
3520:
3517:
3513:
3510:
3509:
3508:
3505:
3503:
3500:
3496:
3493:
3491:
3488:
3486:
3483:
3481:
3480:Polygonal bog
3478:
3476:
3473:
3471:
3468:
3466:
3463:
3461:
3458:
3456:
3453:
3452:
3451:
3448:
3446:
3443:
3441:
3438:
3436:
3433:
3431:
3428:
3426:
3423:
3422:
3420:
3416:
3413:
3409:
3405:
3398:
3393:
3391:
3386:
3384:
3379:
3378:
3375:
3363:
3360:
3358:
3355:
3353:
3350:
3348:
3345:
3343:
3340:
3338:
3335:
3333:
3330:
3329:
3326:
3320:
3317:
3315:
3314:Surface water
3312:
3310:
3309:Sacred waters
3307:
3305:
3302:
3300:
3297:
3295:
3294:Riparian zone
3292:
3290:
3287:
3285:
3282:
3280:
3279:Body of water
3277:
3275:
3272:
3270:
3267:
3266:
3264:
3260:
3254:
3251:
3249:
3246:
3244:
3241:
3239:
3236:
3234:
3231:
3229:
3228:Riverboarding
3226:
3224:
3223:River surfing
3221:
3219:
3216:
3214:
3211:
3209:
3206:
3205:
3203:
3199:
3193:
3190:
3188:
3185:
3183:
3180:
3178:
3175:
3173:
3170:
3168:
3165:
3163:
3160:
3158:
3155:
3153:
3150:
3148:
3145:
3143:
3140:
3138:
3135:
3133:
3130:
3128:
3125:
3123:
3120:
3118:
3115:
3113:
3110:
3108:
3105:
3103:
3100:
3098:
3095:
3093:
3090:
3089:
3087:
3085:
3081:
3075:
3072:
3070:
3067:
3065:
3062:
3060:
3057:
3055:
3052:
3050:
3047:
3045:
3042:
3040:
3037:
3035:
3032:
3030:
3027:
3025:
3022:
3020:
3017:
3015:
3012:
3010:
3007:
3005:
3002:
3000:
2997:
2995:
2992:
2990:
2987:
2985:
2982:
2980:
2977:
2975:
2972:
2970:
2967:
2965:
2962:
2960:
2957:
2955:
2952:
2951:
2949:
2947:and modelling
2943:
2937:
2934:
2932:
2929:
2927:
2924:
2923:
2921:
2919:
2915:
2909:
2908:Return period
2906:
2904:
2901:
2899:
2896:
2894:
2891:
2889:
2886:
2884:
2881:
2879:
2876:
2874:
2871:
2869:
2868:Flood control
2866:
2864:
2863:Flood barrier
2861:
2857:
2854:
2852:
2849:
2848:
2847:
2844:
2842:
2839:
2837:
2834:
2832:
2829:
2828:
2826:
2824:
2820:
2816:
2810:
2807:
2805:
2802:
2800:
2797:
2796:
2794:
2792:
2788:
2782:
2779:
2777:
2774:
2772:
2769:
2767:
2764:
2762:
2759:
2757:
2754:
2752:
2749:
2747:
2744:
2742:
2739:
2737:
2734:
2732:
2729:
2728:
2726:
2724:
2720:
2714:
2711:
2709:
2706:
2704:
2701:
2699:
2696:
2694:
2691:
2689:
2686:
2684:
2681:
2679:
2676:
2674:
2671:
2669:
2666:
2664:
2661:
2659:
2656:
2654:
2651:
2649:
2646:
2644:
2641:
2639:
2636:
2634:
2631:
2629:
2626:
2624:
2621:
2619:
2616:
2614:
2611:
2609:
2606:
2604:
2601:
2599:
2596:
2594:
2591:
2589:
2586:
2584:
2581:
2579:
2576:
2574:
2571:
2569:
2566:
2564:
2561:
2559:
2556:
2554:
2551:
2550:
2548:
2546:
2542:
2536:
2533:
2531:
2528:
2526:
2523:
2521:
2518:
2516:
2513:
2511:
2508:
2506:
2503:
2501:
2498:
2496:
2495:Palaeochannel
2493:
2491:
2488:
2486:
2483:
2481:
2478:
2476:
2473:
2471:
2468:
2466:
2463:
2461:
2458:
2456:
2455:Granular flow
2453:
2451:
2448:
2446:
2443:
2441:
2438:
2436:
2433:
2431:
2428:
2426:
2423:
2422:
2420:
2418:
2413:
2409:
2403:
2400:
2398:
2395:
2393:
2390:
2388:
2385:
2381:
2378:
2377:
2376:
2373:
2369:
2366:
2364:
2361:
2360:
2359:
2356:
2354:
2351:
2349:
2346:
2344:
2341:
2340:
2338:
2335:
2330:
2326:
2320:
2317:
2315:
2312:
2310:
2307:
2305:
2302:
2300:
2297:
2295:
2292:
2290:
2287:
2285:
2282:
2280:
2277:
2275:
2272:
2270:
2267:
2265:
2262:
2260:
2257:
2256:
2254:
2252:
2248:
2242:
2239:
2237:
2234:
2232:
2229:
2227:
2224:
2222:
2219:
2217:
2214:
2212:
2209:
2207:
2204:
2202:
2201:Channel types
2199:
2197:
2194:
2192:
2189:
2187:
2184:
2182:
2181:Braided river
2179:
2177:
2174:
2173:
2171:
2168:
2163:
2159:
2155:
2151:
2147:
2140:
2135:
2133:
2128:
2126:
2121:
2120:
2117:
2105:
2097:
2096:
2093:
2087:
2084:
2082:
2079:
2077:
2074:
2072:
2069:
2067:
2064:
2062:
2059:
2057:
2056:Water erosion
2054:
2052:
2049:
2048:
2046:
2042:
2036:
2033:
2031:
2028:
2026:
2023:
2021:
2018:
2016:
2013:
2012:
2010:
2006:
2000:
1997:
1995:
1992:
1990:
1987:
1985:
1982:
1981:
1979:
1977:
1973:
1967:
1964:
1962:
1959:
1957:
1954:
1953:
1951:
1949:
1948:Bedrock river
1945:
1939:
1936:
1934:
1931:
1929:
1926:
1924:
1921:
1919:
1916:
1914:
1911:
1909:
1908:Riparian zone
1906:
1904:
1901:
1899:
1896:
1894:
1891:
1889:
1886:
1884:
1881:
1879:
1876:
1874:
1871:
1869:
1866:
1864:
1861:
1859:
1856:
1854:
1853:Braided river
1851:
1849:
1846:
1844:
1841:
1839:
1836:
1835:
1833:
1831:
1827:
1821:
1818:
1816:
1813:
1811:
1808:
1806:
1803:
1801:
1798:
1796:
1793:
1791:
1788:
1786:
1783:
1782:
1780:
1776:
1772:
1765:
1760:
1758:
1753:
1751:
1746:
1745:
1742:
1732:
1728:
1721:
1718:
1706:
1702:
1696:
1693:
1682:on 2021-09-03
1681:
1677:
1671:
1668:
1655:
1651:
1647:
1641:
1638:
1633:
1627:
1623:
1622:
1614:
1611:
1603:
1598:
1593:
1588:
1583:
1579:
1575:
1571:
1564:
1557:
1554:
1549:
1545:
1541:
1534:
1531:
1519:
1515:
1511:
1505:
1502:
1491:
1487:
1481:
1478:
1474:
1470:
1466:
1460:
1457:
1452:
1448:
1442:
1439:
1434:
1430:
1426:
1422:
1417:
1412:
1408:
1404:
1400:
1396:
1392:
1385:
1383:
1379:
1366:
1362:
1356:
1354:
1350:
1346:
1341:
1337:
1333:
1329:
1325:
1321:
1317:
1310:
1307:
1303:
1301:
1287:
1280:
1277:
1273:
1269:
1265:
1261:
1257:
1253:
1249:
1245:
1238:
1236:
1232:
1226:
1221:
1217:
1213:
1209:
1205:
1201:
1194:
1191:
1186:
1184:0-8160-3823-6
1180:
1176:
1171:
1170:
1161:
1158:
1147:on 2012-01-21
1146:
1142:
1136:
1133:
1128:
1124:
1120:
1114:
1111:
1105:
1101:
1098:
1096:
1093:
1087:
1084:
1081:
1078:
1075:
1072:
1069:
1066:
1064:
1061:
1054:
1051:
1045:
1042:
1039:
1036:
1033:
1030:
1029:
1025:
1014:
1009:
1007:
1005:
1001:
997:
989:
987:
985:
981:
977:
969:
967:
960:
958:
952:
950:
948:
940:
938:
936:
932:
928:
924:
920:
915:
913:
905:
903:
900:
898:
894:
893:Senegal River
890:
886:
882:
877:
875:
871:
867:
863:
859:
853:
845:
843:
841:
837:
833:
829:
825:
822:, containing
821:
816:
814:
810:
806:
802:
798:
791:
787:
783:
778:
771:
767:
762:
755:
753:
751:
747:
746:geomorphology
744:
737:Geomorphology
736:
734:
732:
728:
724:
722:
717:
713:
707:
703:
700:
695:
691:
690:precipitation
686:
684:
680:
676:
668:
664:
659:
652:
650:
648:
644:
640:
636:
632:
628:
627:Rupert's Land
624:
620:
616:
612:
604:
599:
597:
595:
591:
588:In endorheic
586:
584:
580:
576:
572:
568:
564:
560:
556:
555:Sahara Desert
552:
548:
544:
540:
535:
533:
529:
525:
521:
517:
513:
508:
501:
497:
493:
486:
484:
482:
476:
470:
466:
463:(4M km), the
462:
459:(7M km), the
458:
450:
448:
446:
442:
438:
434:
430:
425:
423:
419:
415:
411:
410:Pacific Ocean
406:
404:
400:
396:
392:
388:
384:
380:
376:
373:and parts of
372:
368:
364:
360:
356:
351:
349:
345:
341:
337:
333:
329:
325:
322:(through the
321:
317:
313:
309:
305:
301:
297:
293:
289:
285:
281:
280:Caribbean Sea
277:
272:
270:
266:
263:, as well as
262:
258:
254:
250:
246:
245:South America
242:
238:
234:
230:
226:
222:
221:North America
218:
210:
205:
201:
196:
190:
182:
180:
178:
174:
169:
167:
163:
159:
155:
150:
148:
143:
141:
137:
133:
129:
125:
124:drainage area
121:
117:
112:
110:
106:
102:
98:
94:
93:
88:
84:
80:
79:body of water
76:
72:
71:surface water
68:
60:
56:
52:
48:
44:
39:
33:
19:
4144:
4140:List of bogs
3995:Conservation
3926:Ombrotrophic
3870:
3841:Water-meadow
3765:
3576:Grass valley
3566:Flood-meadow
3529:Cypress dome
3460:Cataract bog
3435:Beach meadow
3352:Flash floods
3304:River cruise
3201:River sports
3054:Stream gauge
3039:Rouse number
3029:Relief ratio
2878:Flood-meadow
2809:Urban runoff
2723:Fluvial flow
2708:River valley
2678:River island
2643:Meander scar
2558:Alluvial fan
2500:Progradation
2375:Karst spring
2319:Winterbourne
2274:Chalk stream
2236:River source
2215:
2211:Distributary
1810:River valley
1789:
1730:
1720:
1709:. Retrieved
1707:. 2010-09-07
1704:
1695:
1684:. Retrieved
1680:the original
1670:
1658:. Retrieved
1654:the original
1640:
1620:
1613:
1573:
1569:
1556:
1543:
1533:
1522:. Retrieved
1513:
1504:
1493:. Retrieved
1489:
1480:
1465:Amazon River
1459:
1450:
1441:
1398:
1394:
1369:. Retrieved
1365:the original
1343:
1323:
1319:
1309:
1296:
1290:. Retrieved
1279:
1271:
1251:
1247:
1210:(24): 2951.
1207:
1203:
1193:
1168:
1160:
1149:. Retrieved
1145:the original
1135:
1127:the original
1122:
1113:
993:
973:
964:
956:
944:
916:
909:
901:
878:
855:
817:
794:
740:
731:runoff water
725:
708:
704:
699:stream gauge
687:
672:
608:
587:
536:
510:
500:Central Asia
454:
437:Persian Gulf
429:Indian Ocean
426:
407:
379:South Dakota
375:North Dakota
365:east of the
355:Arctic Ocean
352:
316:North Africa
300:Saskatchewan
273:
267:and part of
247:east of the
231:basins, the
214:
211:Ocean basins
170:
151:
144:
139:
131:
127:
123:
119:
115:
113:
107:, forming a
90:
81:, such as a
66:
64:
51:agricultural
4165:Telmatology
4160:River delta
4027:Ramsar site
4017:Marsh organ
3916:Hydric soil
3795:Vernal pool
3778:Shrub swamp
3646:Tidal marsh
3475:Plateau bog
3465:Coastal bog
3455:Blanket bog
3213:Fly fishing
3137:Fish ladder
3122:Daylighting
2841:Flash flood
2804:First flush
2751:Plunge pool
2475:Downcutting
2460:Debris flow
2435:Aggradation
2309:Stream pool
2015:Aggradation
1966:Plunge pool
1933:Stream pool
1923:River mouth
1815:River delta
1580:: 265–281.
1469:Congo River
1371:21 November
1004:groundwater
947:mountainous
782:terrain map
770:hydrography
694:groundwater
631:Bioregional
551:Great Basin
543:Caspian Sea
532:alkali sink
469:Mississippi
369:, northern
288:Appalachian
229:Great Lakes
132:water basin
128:river basin
105:confluences
75:river mouth
4220:Categories
4125:Bog butter
3821:Bog garden
3814:Artificial
3785:Wet meadow
3651:High marsh
3641:Salt marsh
3544:Fen-meadow
3512:Alder carr
3495:Upland bog
3490:String bog
3485:Raised bog
3319:Wild river
2999:Hydrograph
2989:Hack's law
2954:Baer's law
2898:Inundation
2883:Floodplain
2823:stormwater
2781:Whitewater
2653:Oxbow lake
2490:Knickpoint
2465:Deposition
2358:Hot spring
2299:Streamflow
2289:Stream bed
2206:Confluence
2066:Hack's law
2020:Base level
1961:Knickpoint
1888:Oxbow lake
1868:Floodplain
1711:2021-09-22
1686:2021-09-03
1524:2021-10-22
1495:2021-10-22
1451:WorldAtlas
1292:2019-06-10
1151:2008-02-11
1106:References
941:Topography
929:(paved or
925:type, and
919:topography
832:phosphorus
813:water body
809:pollutants
663:Ohio River
623:Hudson Bay
600:Importance
520:Inland sea
395:Kazakhstan
324:Nile River
302:, eastern
4246:Hydrology
3947:Hydrosere
3935:Processes
3921:Marsh gas
3766:Myristica
3656:Low marsh
3470:Kermi bog
3445:Bofedales
3425:Backswamp
3289:Limnology
3238:Triathlon
3208:Canyoning
3177:Revetment
3107:Check dam
3019:Main stem
2776:Waterfall
2663:Point bar
2648:Mouth bar
2588:Billabong
2535:Water gap
2530:Wash load
2510:Saltation
2430:Anabranch
2353:Holy well
2241:Tributary
2044:Mechanics
1893:Point bar
1883:Mouth bar
1838:Anabranch
1660:March 21,
1433:129463497
1425:1944-9224
1068:Main stem
996:pavements
984:saturated
970:Soil type
836:potassium
801:nutrients
766:dendritic
721:isohyetal
675:hydrology
653:Hydrology
619:fur trade
571:Australia
524:ephemeral
445:Australia
422:Australia
383:Minnesota
312:Black Sea
140:watershed
136:impluvium
4205:Category
4135:Bog-wood
4130:Bog iron
4120:Bog body
3942:Halosere
3894:Histosol
3889:Acrotelm
3872:Sphagnum
3730:Reed bed
3675:Moorland
3554:Rich fen
3549:Poor fen
3404:Wetlands
3092:Aqueduct
2959:Baseflow
2926:Effluent
2603:Cut bank
2568:Avulsion
2445:Bed load
2425:Abrasion
2104:Category
1989:Antidune
1976:Bedforms
1863:Cut bank
1602:Archived
1548:Archived
1518:Archived
1300:snowmelt
1010:See also
990:Land use
927:land use
912:flooding
828:nitrates
824:nitrogen
805:sediment
780:Digital
750:sediment
645:and the
635:treaties
594:Dead Sea
581:and the
573:and the
547:Aral Sea
528:dry lake
435:and the
399:Mongolia
328:Southern
162:dry lake
4170:Turbary
4150:Estuary
3725:Pothole
3715:Pocosin
3680:Mudflat
3519:Ciénega
3502:Callows
3418:Natural
3269:Aquifer
3262:Related
3218:Rafting
2746:Meander
2741:Log jam
2703:Thalweg
2608:Estuary
2480:Erosion
2417:erosion
2329:Springs
2284:Current
2251:Streams
2191:Channel
2154:springs
2150:streams
1938:Thalweg
1873:Meander
1800:Estuary
1582:Bibcode
1576:(2/3).
1403:Bibcode
1328:Bibcode
1316:karstic
1256:Bibcode
1212:Bibcode
797:ecology
790:Romania
784:of the
756:Ecology
743:fluvial
611:English
433:Red Sea
387:Montana
344:Lebanon
296:Alberta
269:Morocco
253:Western
57:in the
4251:Rivers
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3611:Kettle
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3064:WAFLEX
2936:Sewage
2819:Floods
2761:Riffle
2756:Rapids
2698:Strath
2668:Ravine
2593:Canyon
2348:Geyser
2279:Coulee
2264:Bourne
2259:Arroyo
2162:Rivers
2146:Rivers
1956:Canyon
1903:Rapids
1898:Riffle
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320:Africa
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2766:Shoal
2633:Gully
2628:Gulch
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2583:Bayou
2440:Armor
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2167:lists
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