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Valley

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1458: 725: 713: 1242: 610: 136: 448: 518: 642: 432: 338: 966: 323: 39: 208: 181: 196: 150: 1169: 1374: 1644: 166: 669:, a variety of transitional forms between V-, U- and plain valleys can form. The floor or bottom of these valleys can be broad or narrow, but all valleys have a shoulder. The broader a mountain valley, the lower its shoulders are located in most cases. An important exception is canyons where the shoulder almost is near the top of the valley's slope. In the Alps – e.g. the 1973: 1003:
and other areas where Gaelic was once widespread. Strath signifies a wide valley between hills, the floor of which is either level or slopes gently. A glen is a river valley which is steeper and narrower than a strath. A corrie is a basin-shaped hollow in a mountain. Each of these terms also occurs
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Glaciated terrain is not the only site of hanging streams and valleys. Hanging valleys are also simply the product of varying rates of erosion of the main valley and the tributary valleys. The varying rates of erosion are associated with the composition of the adjacent rocks in the different valley
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valley that is higher than the main valley. They are most commonly associated with U-shaped valleys, where a tributary glacier flows into a glacier of larger volume. The main glacier erodes a deep U-shaped valley with nearly vertical sides, while the tributary glacier, with a smaller volume of ice,
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A tunnel valley is a large, long, U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages. Such valleys can be up to 100 km (62 mi) long,
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The development of a river valley is affected by the character of the bedrock over which the river or stream flows, the elevational difference between its top and bottom, and indeed the climate. Typically the flow will increase downstream and the gradient will decrease. In the upper valley, the
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In the middle valley, as numerous streams have coalesced, the valley is typically wider, the flow slower and both erosion and deposition may take place. More lateral erosion takes place in the middle section of a river's course, as strong currents on the outside of its curve erode the bank.
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locations. The tributary valleys are eroded and deepened by glaciers or erosion at a slower rate than that of the main valley floor; thus the difference in the two valleys' depth increases over time. The tributary valley, composed of more resistant rock, then hangs over the main valley.
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In northern Central Europe, the Scandinavian ice sheet during the various ice ages advanced slightly uphill against the lie of the land. As a result, its meltwaters flowed parallel to the ice margin to reach the North Sea basin, forming huge, flat valleys known as
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There are various forms of valleys associated with glaciation. True glacial valleys are those that have been cut by a glacier which may or may not still occupy the valley at the present day. Such valleys may also be known as glacial troughs. They typically have a
310:. All three processes can contribute to the development of a valley over geological time. The flat (or relatively flat) portion of a valley between its sides is referred to as the valley floor. The valley floor is typically formed by river sediments and may have 787:. By contrast with glacial U-shaped valleys, there is less downward and sideways erosion. The severe downslope denudation results in gently sloping valley sides; their transition to the actual valley bottom is unclear. Trough-shaped valleys occur mainly in 502:(or 'rock steps') can result from differing erosion rates due to both the nature of the bedrock (hardness and jointing for example) and the power of the moving ice. In places, a rock basin may be excavated which may later be filled with water to form a 609: 676:
valley – the shoulders are quite low (100–200 meters above the bottom). Many villages are located here (esp. on the sunny side) because the climate is very mild: even in winter when the valley's floor is filled with fog, these villages are in
404:. Rapid down-cutting may result from localized uplift of the land surface or rejuvenation of the watercourse as a result for example of a reduction in the base level to which the river is eroded, e.g. lowered global sea level during an 584:. They once served as subglacial drainage pathways carrying large volumes of meltwater. Their cross-sections exhibit steep-sided flanks similar to fjord walls, and their flat bottoms are typical of subglacial glacial erosion. 483:
by rock material embedded within the moving glacial ice causes the widening and deepening of the valley to produce the characteristic U or trough shape with relatively steep, even vertical sides and a relatively flat bottom.
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developed from these river valley communities. Siting of settlements within valleys is influenced by many factors, including the need to avoid flooding and the location of river crossing points.
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Santa Clara Valley is a structural valley, created by mountain building, as opposed to an erosional valley, or one which has undergone the wearing away of the earth's surface by natural agents.
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and are known as river valleys. Typically small valleys containing streams feed into larger valleys which in turn feed into larger valleys again, eventually reaching the ocean or perhaps an
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Box valleys have wide, relatively level floors and steep sides. They are common in periglacial areas and occur in mid-latitudes, but also occur in tropical and arid regions.
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or flat valley bottom. In Southern England, vales commonly occur between the outcrops of different relatively erosion-resistant rock formations, where less
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Some sections of a stream or river valleys may have vertically incised their course to such an extent that the valley they occupy is best described as a
282:, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. 1044: 580:
4 km (2.5 mi) wide, and 400 m (1,300 ft) deep (its depth may vary along its length). Tunnel valleys were formed by subglacial
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Conversely, deposition may take place on the inside of curves where the current is much slacker, the process leading to the river assuming a
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occurs widely in place names in the north of England and, to a lesser extent, in southern Scotland. As a generic name for a type of valley,
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Jþrgensen, Flemming; Peter B.E. Sandersen (June 2006). "Buried and open tunnel valleys in Denmark—erosion beneath multiple ice sheets".
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Rowley, Taylor; Giardino, John R.; Granados-Aguilar, Raquel; Vitek, John D. (2015-01-01), Giardino, John R.; Houser, Chris (eds.),
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is about 400 meters (1,300 ft) deep while the main fjord nearby is 1,200 meters (3,900 ft) deep. The mouth of
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is only 50 meters (160 ft) deep while the main fjord is around 1,300 meters (4,300 ft) at the same point.
494:, typical of glaciated mountain landscapes. The upper end of the trough below the ice-contributing cirques may be a 3901: 1703: 1647: 553: 75: 1920:(singular: 'vallis'). Deeper valleys with steeper sides (akin to canyons) on certain of these bodies are known as 712: 3432: 471:', excavated by the rotational movement downslope of a cirque glacier. During glacial periods, for example, the 3896: 2502: 2477: 2430: 2405: 2380: 2355: 2143: 2096: 2043: 1925: 1444: 1241: 60: 3457: 1076:
The term vale is used in England and Wales to describe a wide river valley, usually with a particularly wide
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and are characteristic landforms of mountain areas where glaciation has occurred or continues to take place.
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of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by
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The uppermost part of a glacial valley frequently consists of one or more 'armchair-shaped' hollows, or '
1936:' or Latin term 'rima' (signifying 'cleft') is used for certain other elongate depressions on the Moon. 89: 3932: 3927: 3102: 2636: 1917: 1889: 3886: 3838: 3721: 1769: 479:
proceeds, extend downhill through valleys that have previously been shaped by water rather than ice.
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and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated
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makes a shallower U-shaped valley. Since the surfaces of the glaciers were originally at the same
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character. In the lower valley, gradients are lowest, meanders may be much broader and a broader
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typically refers to a wide valley, though there are many much smaller stream valleys within the
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showing a characteristic U-shape, the bottom's rocky 'rubble' accretion and the broad shoulders
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to produce a steep-sided V-shaped valley. The presence of more resistant rock bands, of
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associated with the development of river valleys are preferentially eroded to produce
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Valleys may arise through several different processes. Most commonly, they arise from
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This article is about the physical-geographic term. For places named "Valley", see
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is a word in common use in northern England for a narrow valley with steep sides.
941:: A valley formed by geologic events such as drop faults or the rise of highlands. 517: 447: 247:. These glaciers may remain present in valleys in high mountains or polar areas. 3711: 3671: 3666: 3270: 3157: 3152: 2936: 2873: 2843: 2808: 2803: 2770: 2735: 2706: 2648: 2292: 1835: 1745: 1739: 1733: 1715: 1500: 1484: 1426: 1408: 1349: 1325: 1101: 1040: 1036: 1032: 996: 859: 830: 697: 685: 536: 475:
ice ages, it is in these locations that glaciers initially form and then, as the
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regions of variable wetness. Both climates are dominated by heavy denudation.
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Place-names in the Landscape: the Geographical roots of Britain's place-names
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Place-names in the Landscape: the Geographical roots of Britain's place-names
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Hollow: A term used regionally for a small valley surrounded by mountains or
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may determine the course of the stream and result in a twisting course with
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areas, valleys may be entirely dry or carry a watercourse only rarely. In
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Nesje, A., & Whillans, I. M. (1994). Erosion of Sognefjord, Norway.
2073: 916:: An elongated valley found between two nearly-parallel mountain chains. 841:
There are many terms used for different sorts of valleys. They include:
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may result. Deposition dominates over erosion. A typical river basin or
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terms for 'valley, 'gorge' and 'ditch' respectively. The German term '
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Chapter 13 - Periglacial Processes and Landforms in the Critical Zone
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Numerous elongate depressions have been identified on the surface of
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or else by sediments. Such features are found in coastal areas as
195: 3808: 3757: 3285: 3280: 3242: 3147: 3019: 2956: 1924:(singular: 'chasma'). Long narrow depressions are referred to as 1121: 1054: 883: 872: 666: 561: 546: 476: 468: 405: 378: 342: 331: 327: 307: 303: 302:. In polar areas and at high altitudes, valleys may be eroded by 295: 291: 255: 244: 240: 212: 188: 158: 1168: 783:
Trough-shaped valleys also form in regions of heavy topographic
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List of largest rifts, canyons and valleys in the Solar System
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is used more widely by geographers as a synonym for (glacial)
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running from one end to the other. Most valleys are formed by
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is used to describe a ravine containing a mountain stream in
950: 946: 922:: A deep, narrow, flat-bottomed valley with an abrupt ending. 879: 826: 756: 522: 507: 393: 263: 232: 30:
Low area between hills, often with a river running through it
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will incorporate each of these different types of valleys.
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but now are ice-free and occupied by streams or rivers. In
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Pages displaying short descriptions of redirect targets
868:: A valley not created by sustained surface water flow. 700:. Smaller streams flow into rivers as deep canyons or 999:
terms and are commonly encountered in place-names in
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are much shallower than the main fjord. The mouth of
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Other interesting glacially carved valleys include:
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A panoramic view of two merging U-shaped valleys in
2350:(First ed.). Edinburgh: Birlinn. p. 203. 353:stream will most effectively erode its bed through 63:. Unsourced material may be challenged and removed. 23:"River valley" redirects here. For other uses, see 2400:(First ed.). Edinburgh: Birlinn. p. 53. 2375:(First ed.). Edinburgh: Birlinn. p. 99. 2250: 1104:originated in river valleys, such as that of the 636: 549:for their parallel directions and hanging mouths. 254:valleys may have been created or enlarged during 3914: 2497:(First ed.). London: J M Dent. p. 99. 2472:(First ed.). London: J M Dent. p. 88. 2684: 2425:(First ed.). London: Penguin. p. 83. 270:may also result from drainage now taking place 223:is an elongated low area often running between 199:The Frades Valley in the mountainous region of 2559:"Gazetteer of Planetary Nomenclature, Welcome" 852:which sometimes results from the erosion of a 2670: 2620: 2420: 862:: A small, secluded, and often wooded valley. 1895: 931:A valley typically developed parallel to a 2677: 2663: 957:, are not usually referred to as valleys. 2133: 2086: 2033: 341:Valley of Palakaria river springing from 123:Learn how and when to remove this message 2421:Whitten, D.G.A.; Brooks, J.R.V. (1972). 2058: 1642: 1456: 1372: 1240: 1167: 1043:which are named "(specific name) Dale". 964: 723: 711: 640: 516: 446: 430: 419:For various lists of river valleys, see 336: 321: 250:At lower latitudes and altitudes, these 206: 194: 179: 164: 148: 134: 3276:International scale of river difficulty 2492: 2467: 972:running through the Kohistan Valley in 684:In some stress-tectonic regions of the 285: 3915: 2592:, Glossary of Alpine Glacial Landforms 2290: 2197:. U.S. Geological Survey. May 28, 2004 1140:, the rivers were used as a source of 945:Similar geographical features such as 833:activity beneath the Earth's surface. 2658: 871:Erosional valley: A valley formed by 412:may also result in the production of 345:Mountain, seen in the background, in 2395: 2370: 2345: 2062:(1968). Rhodes W. Fairbridge (ed.). 906:, a hollow is a small valley or dry 836: 759:systems underwater. The branches of 707: 696:are parallel to each other, and are 645:Look from Paria View to a valley in 61:adding citations to reliable sources 32: 2319:"Early History, Santa Clara County" 2311: 1928:(singular: 'fossa'). These are the 1163: 1148:extremes and provided a source for 1095: 1088:has been eroded. An example is the 825:are formed by the expansion of the 13: 2561:. International Astronomical Union 2539:. International Astronomical Union 2263:10.1016/B978-0-444-63369-9.00013-6 961:British regional terms for valleys 426: 14: 3954: 2637:Valles Marineris and Ophir Chasma 2577: 2195:"Glossary of Glacier Terminology" 1989: â€“ Deep chasm between cliffs 1152:, stimulating the development of 621:Aoraki / Mount Cook National Park 2297:. Psychology Press. p. 98. 2152: 2136:Principles of Physical Geography 2089:Principles of Physical Geography 2036:Principles of Physical Geography 1971: 1843: 1638: 1551:with its famous castles (France) 935:from more readily eroded strata. 778: 608: 317: 37: 3433:Flooded grasslands and savannas 2551: 2529: 2511: 2486: 2461: 2439: 2414: 2389: 2364: 2339: 2284: 2242: 2181:10.1016/j.quascirev.2005.11.006 1004:in parts of the world formerly 619:New Zealand's Hooker Valley at 326:The valley of Halikko River in 48:needs additional citations for 2221: 2208: 2187: 2127: 2105: 2080: 2052: 2027: 755:Hanging valleys also occur in 653:, with very striking shoulders 637:Transition forms and shoulders 1: 2294:Encyclopedia of Geomorphology 2020: 1883: 1648:Hell's Gate, British Columbia 1213:(Egypt/Sudan/Ethiopia/Uganda) 720:flowing from a hanging valley 3599:Universal Soil Loss Equation 3549:Hydrological transport model 3443:Storm Water Management Model 2523:Merriam–Webster's Dictionary 2291:Goudie, Andrew, ed. (2004). 2016: â€“ Narrow body of water 1914:planets and their satellites 1627:system. (France and Germany) 587: 274:rather than at the surface. 7: 1964: 1954:List of valleys on the Moon 1265:List of valleys in Pakistan 231:and typically containing a 10: 3959: 3103:Antecedent drainage stream 2633:, bisecting the Lunar Alps 2493:Gelling, Margaret (1984). 2468:Gelling, Margaret (1984). 2161:Quaternary Science Reviews 1890:West Antarctic Rift System 1778:(British Columbia/Montana) 1515:(Scotland, United Kingdom) 1509:(Scotland, United Kingdom) 1368: 817:Rift valleys, such as the 810: 591: 572: 451:A glaciated valley in the 418: 264:areas of limestone bedrock 176:has almost vertical walls. 22: 15: 3867: 3839:River valley civilization 3801: 3740: 3722:Riparian-zone restoration 3622: 3484: 3456: 3357: 3329: 3261: 3083: 2950: 2867: 2789: 2700: 2586:, University of Wisconsin 1784:(Ontario/Quebec/New York) 1601:(MĂžre Og Romsdal, Norway) 1452: 1183: 568: 3902:Countries without rivers 3877:Rivers by discharge rate 3589:Runoff model (reservoir) 3554:Infiltration (hydrology) 2621:Extraterrestrial valleys 2525:. Merriam–Webster. 2011. 2134:Monkhouse, F.J. (1971). 2087:Monkhouse, F.J. (1971). 2065:Classification of Rivers 2034:Monkhouse, F.J. (1971). 1949:List of chasmata on Mars 1896:Extraterrestrial valleys 1802:(Virginia/West Virginia) 1700:(Arizona, United States) 1260:List of valleys in India 1100:Some of the first human 3574:River Continuum Concept 3339:Agricultural wastewater 1944:List of valleys on Mars 1670:(Maryland/Pennsylvania) 1613:(Wales, United Kingdom) 1563:(Wales, United Kingdom) 1236: 806: 435:U-shaped valley on the 300:internal drainage basin 278:arise principally from 18:Valley (disambiguation) 3897:River name etymologies 3824:Hydraulic civilization 3682:Floodplain restoration 3458:Point source pollution 3233:Sedimentary structures 2610:, Valleys of the World 1650: 1473: 1385: 1254: 1180: 976: 798: 743:A hanging valley is a 740: 721: 718:Yosemite National Park 654: 545:of the Austrian river 529: 462:U-shaped cross-section 456: 444: 421:Category:River valleys 349: 334: 216: 204: 192: 191:, a rather flat valley 177: 162: 146: 3509:Discharge (hydrology) 3471:Industrial wastewater 2952:Sedimentary processes 2423:Dictionary of Geology 2323:National Park Service 1782:Saint Lawrence Valley 1776:Rocky Mountain Trench 1728:Missouri River Valley 1646: 1460: 1376: 1244: 1201:Ethiopian Rift Valley 1171: 1065:(also encountered as 968: 850:Appalachian Mountains 727: 716:Bridal Veil Falls in 715: 644: 558:Glacier National Park 520: 453:Mount Hood Wilderness 450: 434: 340: 325: 294:over long periods by 210: 198: 183: 168: 155:Glacier National Park 152: 138: 3614:Volumetric flow rate 3198:Riffle-pool sequence 2398:Scottish Place-names 2396:Ross, David (2001). 2373:Scottish Place-names 2371:Ross, David (2001). 2348:Scottish Place-names 2346:Ross, David (2001). 2167:(11–12): 1339–1363. 1543:Lauterbrunnen Valley 1377:The Harau Valley in 1006:colonized by Britain 286:Formation of valleys 211:Baemsagol valley of 201:Rio de Janeiro state 57:improve this article 3788:Whitewater kayaking 3783:Whitewater canoeing 3584:Runoff curve number 3428:Flood pulse concept 2173:2006QSRv...25.1339J 1794:San Fernando Valley 1611:South Wales Valleys 1545:(Bern, Switzerland) 1229:Valley of the Kings 1158:first civilizations 1132:, and arguably the 1090:Vale of White Horse 914:Longitudinal valley 153:U-shaped valley in 3814:Aquatic toxicology 3727:Stream restoration 3692:Infiltration basin 3544:Hydrological model 3060:Sediment transport 2883:Estavelle/Inversac 2761:Subterranean river 2614:Valley definitions 1871:Valley of the Moon 1818:Valley of the Gods 1748:(British Columbia) 1706:(British Columbia) 1694:(British Columbia) 1688:(British Columbia) 1651: 1569:(Buskerud, Norway) 1557:(Telemark, Norway) 1533:(Telemark, Norway) 1527:(Buskerud, Norway) 1487:(Telemark, Norway) 1481:(Vestland, Norway) 1474: 1435:(Papua New Guinea) 1399:(Papua New Guinea) 1386: 1297:Jordan Rift Valley 1255: 1181: 977: 741: 722: 688:or the Alps (e.g. 655: 530: 488:Interlocking spurs 457: 445: 371:interlocking spurs 350: 335: 217: 205: 193: 178: 163: 147: 3933:Fluvial landforms 3928:Erosion landforms 3910: 3909: 3887:Whitewater rivers 3793:Whitewater slalom 3624:River engineering 3524:Groundwater model 3485:River measurement 3413:Flood forecasting 3228:Sedimentary basin 3085:Fluvial landforms 2990:Bed material load 2766:River bifurcation 2272:978-0-444-63369-9 1916:and are known as 1856:CalchaquĂ­ Valleys 1830:Willamette Valley 1800:Shenandoah Valley 1770:Rio Grande Valley 1764:Valley of the Sun 1668:Cumberland Valley 1621:Upper Rhine Plain 1575:(Hedmark, Norway) 1521:(Oppland, Norway) 1355:Jiuzhaigou Valley 1331:Valleys of China 1299:(Jordan - Israel) 1247:Valley of Flowers 1206:Great Rift Valley 1196:East African Rift 1102:complex societies 1018:, as is the word 939:Structural valley 837:Terms for valleys 708:Hanging tributary 657:Depending on the 631:in the background 359:geological faults 133: 132: 125: 107: 3950: 3872:Rivers by length 3707:River morphology 3609:Wetted perimeter 3514:Drainage density 3025:Headward erosion 2854:Perennial stream 2726:Blackwater river 2679: 2672: 2665: 2656: 2655: 2616:, YourDictionary 2603: 2601: 2571: 2570: 2568: 2566: 2555: 2549: 2548: 2546: 2544: 2533: 2527: 2526: 2515: 2509: 2508: 2490: 2484: 2483: 2465: 2459: 2458: 2456: 2454: 2449:. Microsoft Bing 2443: 2437: 2436: 2418: 2412: 2411: 2393: 2387: 2386: 2368: 2362: 2361: 2343: 2337: 2336: 2331: 2329: 2315: 2309: 2308: 2288: 2282: 2281: 2280: 2279: 2256: 2246: 2240: 2239: 2237: 2236: 2225: 2219: 2212: 2206: 2205: 2203: 2202: 2191: 2185: 2184: 2156: 2150: 2149: 2131: 2125: 2124: 2122: 2120: 2109: 2103: 2102: 2084: 2078: 2077: 2056: 2050: 2049: 2031: 2010: 1981: 1979:Geography portal 1976: 1975: 1974: 1824:Valley of Mexico 1788:Salt Lake Valley 1758:Palo Duro Canyon 1754:(Ontario/Quebec) 1722:Las Vegas Valley 1662:Coachella Valley 1591:to Grenoble and 1539:(Romania/Serbia) 1493:(Eastern Europe) 1164:Notable examples 1110:Tigris-Euphrates 1096:Human settlement 1092:in Oxfordshire. 920:Steephead valley 829:'s crust due to 728:Hanging valley, 612: 564:, United States. 312:fluvial terraces 252:glacially formed 140:CalchaquĂ­ Valley 128: 121: 117: 114: 108: 106: 65: 41: 33: 3958: 3957: 3953: 3952: 3951: 3949: 3948: 3947: 3943:Bodies of water 3938:Slope landforms 3913: 3912: 3911: 3906: 3882:Drainage basins 3863: 3797: 3736: 3712:Retention basin 3672:Erosion control 3667:Detention basin 3618: 3534:Hjulström curve 3486: 3480: 3452: 3396:Non-water flood 3353: 3325: 3271:Helicoidal flow 3257: 3158:Fluvial terrace 3153:Floating island 3079: 2954: 2946: 2937:Rhythmic spring 2871: 2863: 2844:Stream gradient 2785: 2771:River ecosystem 2736:Channel pattern 2704: 2696: 2683: 2623: 2599: 2595: 2580: 2575: 2574: 2564: 2562: 2557: 2556: 2552: 2542: 2540: 2535: 2534: 2530: 2517: 2516: 2512: 2505: 2491: 2487: 2480: 2466: 2462: 2452: 2450: 2445: 2444: 2440: 2433: 2419: 2415: 2408: 2394: 2390: 2383: 2369: 2365: 2358: 2344: 2340: 2327: 2325: 2317: 2316: 2312: 2305: 2289: 2285: 2277: 2275: 2273: 2247: 2243: 2234: 2232: 2227: 2226: 2222: 2213: 2209: 2200: 2198: 2193: 2192: 2188: 2157: 2153: 2146: 2132: 2128: 2118: 2116: 2111: 2110: 2106: 2099: 2085: 2081: 2060:Morisawa, Marie 2057: 2053: 2046: 2032: 2028: 2023: 2008: 1977: 1972: 1970: 1967: 1898: 1886: 1846: 1841: 1836:Yosemite Valley 1746:Okanagan Valley 1736:(Arizona, Utah) 1734:Monument Valley 1716:Imperial Valley 1674:Cuyahoga Valley 1641: 1636: 1607:(Agder, Norway) 1485:Dalen, Telemark 1455: 1450: 1427:Kangaroo Valley 1409:Capertee Valley 1371: 1366: 1350:Insukati Valley 1326:Panjshir Valley 1278:(Western Nepal) 1239: 1234: 1186: 1166: 1098: 1041:Yorkshire Dales 963: 854:geologic window 839: 815: 809: 801: 791:regions and in 781: 710: 686:Rocky Mountains 639: 634: 633: 632: 627:'s terminus at 618: 613: 596: 590: 577: 571: 539:(United States) 537:Yosemite Valley 492:truncated spurs 429: 427:Glacial valleys 424: 320: 288: 280:earth movements 161:, United States 129: 118: 112: 109: 66: 64: 54: 42: 31: 28: 21: 12: 11: 5: 3956: 3946: 3945: 3940: 3935: 3930: 3925: 3908: 3907: 3905: 3904: 3899: 3894: 3889: 3884: 3879: 3874: 3868: 3865: 3864: 3862: 3861: 3856: 3851: 3846: 3841: 3836: 3831: 3826: 3821: 3816: 3811: 3805: 3803: 3799: 3798: 3796: 3795: 3790: 3785: 3780: 3775: 3773:Stone skipping 3770: 3765: 3760: 3755: 3750: 3744: 3742: 3738: 3737: 3735: 3734: 3729: 3724: 3719: 3714: 3709: 3704: 3699: 3694: 3689: 3684: 3679: 3674: 3669: 3664: 3659: 3657:Drop structure 3654: 3649: 3644: 3639: 3637:Balancing lake 3634: 3628: 3626: 3620: 3619: 3617: 3616: 3611: 3606: 3601: 3596: 3591: 3586: 3581: 3576: 3571: 3566: 3564:Playfair's law 3561: 3556: 3551: 3546: 3541: 3536: 3531: 3526: 3521: 3519:Exner equation 3516: 3511: 3506: 3504:Bradshaw model 3501: 3496: 3490: 3488: 3482: 3481: 3479: 3478: 3473: 3468: 3462: 3460: 3454: 3453: 3451: 3450: 3445: 3440: 3435: 3430: 3425: 3420: 3415: 3410: 3405: 3400: 3399: 3398: 3393: 3391:Urban flooding 3383: 3378: 3376:Crevasse splay 3373: 3371:100-year flood 3367: 3365: 3355: 3354: 3352: 3351: 3346: 3341: 3335: 3333: 3331:Surface runoff 3327: 3326: 3324: 3323: 3318: 3313: 3311:Stream capture 3308: 3303: 3298: 3293: 3288: 3283: 3278: 3273: 3267: 3265: 3259: 3258: 3256: 3255: 3250: 3245: 3240: 3235: 3230: 3225: 3223:Rock-cut basin 3220: 3215: 3210: 3205: 3200: 3195: 3190: 3185: 3180: 3175: 3170: 3165: 3160: 3155: 3150: 3145: 3140: 3135: 3130: 3125: 3120: 3115: 3110: 3105: 3100: 3095: 3089: 3087: 3081: 3080: 3078: 3077: 3072: 3067: 3065:Suspended load 3062: 3057: 3055:Secondary flow 3052: 3047: 3045:Retrogradation 3042: 3037: 3032: 3027: 3022: 3017: 3012: 3010:Dissolved load 3007: 3002: 2997: 2992: 2987: 2982: 2977: 2972: 2967: 2961: 2959: 2948: 2947: 2945: 2944: 2942:Spring horizon 2939: 2934: 2929: 2927:Mineral spring 2924: 2923: 2922: 2912: 2911: 2910: 2908:list in the US 2905: 2895: 2890: 2885: 2879: 2877: 2865: 2864: 2862: 2861: 2856: 2851: 2846: 2841: 2836: 2834:Stream channel 2831: 2826: 2821: 2816: 2811: 2806: 2801: 2795: 2793: 2787: 2786: 2784: 2783: 2778: 2773: 2768: 2763: 2758: 2756:Drainage basin 2753: 2748: 2743: 2738: 2733: 2728: 2723: 2718: 2716:Alluvial river 2712: 2710: 2698: 2697: 2682: 2681: 2674: 2667: 2659: 2653: 2652: 2634: 2622: 2619: 2618: 2617: 2611: 2605: 2593: 2587: 2579: 2578:External links 2576: 2573: 2572: 2550: 2528: 2510: 2503: 2485: 2478: 2460: 2438: 2431: 2413: 2406: 2388: 2381: 2363: 2356: 2338: 2310: 2303: 2283: 2271: 2241: 2220: 2218:, 9(1), 33-45. 2207: 2186: 2151: 2144: 2126: 2113:"Vale of Eden" 2104: 2097: 2079: 2051: 2044: 2025: 2024: 2022: 2019: 2018: 2017: 2014:Stream channel 2011: 2002: 1996: 1990: 1983: 1982: 1966: 1963: 1962: 1961: 1956: 1951: 1946: 1897: 1894: 1893: 1892: 1885: 1882: 1881: 1880: 1877:ParaĂ­ba Valley 1874: 1865: 1859: 1853: 1845: 1842: 1840: 1839: 1833: 1827: 1821: 1815: 1809: 1803: 1797: 1791: 1785: 1779: 1773: 1767: 1761: 1755: 1749: 1743: 1737: 1731: 1725: 1719: 1713: 1707: 1701: 1695: 1689: 1683: 1677: 1671: 1665: 1659: 1656:Central Valley 1652: 1640: 1637: 1635: 1634: 1631:Vestfjorddalen 1628: 1614: 1608: 1602: 1596: 1582: 1576: 1570: 1564: 1558: 1552: 1546: 1540: 1534: 1528: 1522: 1519:Gudbrandsdalen 1516: 1510: 1504: 1497:Evrotas Valley 1494: 1488: 1482: 1475: 1463:Gudbrandsdalen 1454: 1451: 1449: 1448: 1442: 1436: 1433:Markham Valley 1430: 1424: 1418: 1412: 1406: 1403:Cagayan Valley 1400: 1394: 1391:Barossa Valley 1387: 1370: 1367: 1365: 1364: 1363: 1362: 1357: 1352: 1347: 1342: 1337: 1335:Baligou Valley 1329: 1323: 1317: 1311: 1305: 1300: 1294: 1285: 1279: 1273: 1267: 1262: 1256: 1238: 1235: 1233: 1232: 1226: 1220: 1214: 1208: 1203: 1198: 1193: 1191:Albertine Rift 1187: 1185: 1182: 1165: 1162: 1156:. Most of the 1097: 1094: 1024:borrowed from 993:Anglicisations 962: 959: 943: 942: 936: 923: 917: 911: 876: 869: 863: 857: 838: 835: 819:Albertine Rift 811:Main article: 808: 805: 800: 797: 780: 777: 765:FjĂŠrlandsfjord 709: 706: 638: 635: 625:Hooker Glacier 615: 614: 607: 606: 605: 592:Main article: 589: 586: 573:Main article: 570: 567: 566: 565: 554:St. Mary River 550: 540: 428: 425: 414:river terraces 387:drainage basin 319: 318:River valleys 316: 287: 284: 174:Western Norway 131: 130: 45: 43: 36: 29: 9: 6: 4: 3: 2: 3955: 3944: 3941: 3939: 3936: 3934: 3931: 3929: 3926: 3924: 3921: 3920: 3918: 3903: 3900: 3898: 3895: 3893: 3890: 3888: 3885: 3883: 3880: 3878: 3875: 3873: 3870: 3869: 3866: 3860: 3857: 3855: 3854:Surface water 3852: 3850: 3849:Sacred waters 3847: 3845: 3842: 3840: 3837: 3835: 3834:Riparian zone 3832: 3830: 3827: 3825: 3822: 3820: 3819:Body of water 3817: 3815: 3812: 3810: 3807: 3806: 3804: 3800: 3794: 3791: 3789: 3786: 3784: 3781: 3779: 3776: 3774: 3771: 3769: 3768:Riverboarding 3766: 3764: 3763:River surfing 3761: 3759: 3756: 3754: 3751: 3749: 3746: 3745: 3743: 3739: 3733: 3730: 3728: 3725: 3723: 3720: 3718: 3715: 3713: 3710: 3708: 3705: 3703: 3700: 3698: 3695: 3693: 3690: 3688: 3685: 3683: 3680: 3678: 3675: 3673: 3670: 3668: 3665: 3663: 3660: 3658: 3655: 3653: 3650: 3648: 3645: 3643: 3640: 3638: 3635: 3633: 3630: 3629: 3627: 3625: 3621: 3615: 3612: 3610: 3607: 3605: 3602: 3600: 3597: 3595: 3592: 3590: 3587: 3585: 3582: 3580: 3577: 3575: 3572: 3570: 3567: 3565: 3562: 3560: 3557: 3555: 3552: 3550: 3547: 3545: 3542: 3540: 3537: 3535: 3532: 3530: 3527: 3525: 3522: 3520: 3517: 3515: 3512: 3510: 3507: 3505: 3502: 3500: 3497: 3495: 3492: 3491: 3489: 3487:and modelling 3483: 3477: 3474: 3472: 3469: 3467: 3464: 3463: 3461: 3459: 3455: 3449: 3448:Return period 3446: 3444: 3441: 3439: 3436: 3434: 3431: 3429: 3426: 3424: 3421: 3419: 3416: 3414: 3411: 3409: 3408:Flood control 3406: 3404: 3403:Flood barrier 3401: 3397: 3394: 3392: 3389: 3388: 3387: 3384: 3382: 3379: 3377: 3374: 3372: 3369: 3368: 3366: 3364: 3360: 3356: 3350: 3347: 3345: 3342: 3340: 3337: 3336: 3334: 3332: 3328: 3322: 3319: 3317: 3314: 3312: 3309: 3307: 3304: 3302: 3299: 3297: 3294: 3292: 3289: 3287: 3284: 3282: 3279: 3277: 3274: 3272: 3269: 3268: 3266: 3264: 3260: 3254: 3251: 3249: 3246: 3244: 3241: 3239: 3236: 3234: 3231: 3229: 3226: 3224: 3221: 3219: 3216: 3214: 3211: 3209: 3206: 3204: 3201: 3199: 3196: 3194: 3191: 3189: 3186: 3184: 3181: 3179: 3176: 3174: 3171: 3169: 3166: 3164: 3161: 3159: 3156: 3154: 3151: 3149: 3146: 3144: 3141: 3139: 3136: 3134: 3131: 3129: 3126: 3124: 3121: 3119: 3116: 3114: 3111: 3109: 3106: 3104: 3101: 3099: 3096: 3094: 3091: 3090: 3088: 3086: 3082: 3076: 3073: 3071: 3068: 3066: 3063: 3061: 3058: 3056: 3053: 3051: 3048: 3046: 3043: 3041: 3038: 3036: 3035:Palaeochannel 3033: 3031: 3028: 3026: 3023: 3021: 3018: 3016: 3013: 3011: 3008: 3006: 3003: 3001: 2998: 2996: 2995:Granular flow 2993: 2991: 2988: 2986: 2983: 2981: 2978: 2976: 2973: 2971: 2968: 2966: 2963: 2962: 2960: 2958: 2953: 2949: 2943: 2940: 2938: 2935: 2933: 2930: 2928: 2925: 2921: 2918: 2917: 2916: 2913: 2909: 2906: 2904: 2901: 2900: 2899: 2896: 2894: 2891: 2889: 2886: 2884: 2881: 2880: 2878: 2875: 2870: 2866: 2860: 2857: 2855: 2852: 2850: 2847: 2845: 2842: 2840: 2837: 2835: 2832: 2830: 2827: 2825: 2822: 2820: 2817: 2815: 2812: 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: 2741:Channel types 2739: 2737: 2734: 2732: 2729: 2727: 2724: 2722: 2721:Braided river 2719: 2717: 2714: 2713: 2711: 2708: 2703: 2699: 2695: 2691: 2687: 2680: 2675: 2673: 2668: 2666: 2661: 2660: 2657: 2650: 2646: 2642: 2638: 2635: 2632: 2628: 2625: 2624: 2615: 2612: 2609: 2606: 2598: 2594: 2591: 2588: 2585: 2582: 2581: 2560: 2554: 2538: 2532: 2524: 2520: 2514: 2506: 2500: 2496: 2489: 2481: 2475: 2471: 2464: 2448: 2442: 2434: 2428: 2424: 2417: 2409: 2403: 2399: 2392: 2384: 2378: 2374: 2367: 2359: 2353: 2349: 2342: 2335: 2324: 2320: 2314: 2306: 2304:9780415327381 2300: 2296: 2295: 2287: 2274: 2268: 2264: 2260: 2255: 2254: 2245: 2230: 2224: 2217: 2216:Geomorphology 2211: 2196: 2190: 2182: 2178: 2174: 2170: 2166: 2162: 2155: 2147: 2141: 2137: 2130: 2114: 2108: 2100: 2094: 2090: 2083: 2075: 2071: 2067: 2066: 2061: 2055: 2047: 2041: 2037: 2030: 2026: 2015: 2012: 2006: 2003: 2000: 1997: 1994: 1991: 1988: 1985: 1984: 1980: 1969: 1960: 1957: 1955: 1952: 1950: 1947: 1945: 1942: 1941: 1940: 1937: 1935: 1931: 1927: 1923: 1919: 1915: 1911: 1907: 1903: 1891: 1888: 1887: 1878: 1875: 1872: 1869: 1868:Ischigualasto 1866: 1863: 1860: 1857: 1854: 1851: 1850:Aburra Valley 1848: 1847: 1844:South America 1837: 1834: 1831: 1828: 1825: 1822: 1819: 1816: 1813: 1812:Toluca Valley 1810: 1807: 1806:Sonoma Valley 1804: 1801: 1798: 1795: 1792: 1789: 1786: 1783: 1780: 1777: 1774: 1771: 1768: 1765: 1762: 1759: 1756: 1753: 1752:Ottawa Valley 1750: 1747: 1744: 1741: 1738: 1735: 1732: 1729: 1726: 1723: 1720: 1717: 1714: 1711: 1710:Hudson Valley 1708: 1705: 1702: 1699: 1696: 1693: 1692:Fraser Valley 1690: 1687: 1686:Fraser Canyon 1684: 1681: 1678: 1675: 1672: 1669: 1666: 1663: 1660: 1657: 1654: 1653: 1649: 1645: 1639:North America 1632: 1629: 1626: 1622: 1618: 1615: 1612: 1609: 1606: 1603: 1600: 1597: 1594: 1590: 1586: 1583: 1580: 1577: 1574: 1571: 1568: 1565: 1562: 1561:Nant Ffrancon 1559: 1556: 1555:Midt-Telemark 1553: 1550: 1547: 1544: 1541: 1538: 1535: 1532: 1529: 1526: 1523: 1520: 1517: 1514: 1511: 1508: 1505: 1502: 1498: 1495: 1492: 1491:Danube Valley 1489: 1486: 1483: 1480: 1477: 1476: 1472: 1468: 1464: 1459: 1446: 1443: 1441:(New Zealand) 1440: 1439:Strath Taieri 1437: 1434: 1431: 1428: 1425: 1423:(New Zealand) 1422: 1419: 1416: 1415:Hunter Valley 1413: 1410: 1407: 1405:(Philippines) 1404: 1401: 1398: 1397:Bulolo Valley 1395: 1392: 1389: 1388: 1384: 1380: 1375: 1361: 1358: 1356: 1353: 1351: 1348: 1346: 1345:Heizhu Valley 1343: 1341: 1338: 1336: 1333: 1332: 1330: 1328:(Afghanistan) 1327: 1324: 1321: 1318: 1315: 1312: 1309: 1306: 1304: 1303:Jordan Valley 1301: 1298: 1295: 1293: 1289: 1286: 1283: 1280: 1277: 1274: 1271: 1268: 1266: 1263: 1261: 1258: 1257: 1252: 1248: 1243: 1230: 1227: 1224: 1221: 1218: 1217:Nugaal Valley 1215: 1212: 1209: 1207: 1204: 1202: 1199: 1197: 1194: 1192: 1189: 1188: 1179: 1175: 1170: 1161: 1159: 1155: 1151: 1147: 1143: 1139: 1135: 1131: 1127: 1123: 1119: 1115: 1111: 1107: 1103: 1093: 1091: 1087: 1083: 1079: 1074: 1072: 1068: 1064: 1060: 1056: 1052: 1051: 1046: 1042: 1038: 1034: 1029: 1027: 1023: 1022: 1017: 1016: 1011: 1007: 1002: 998: 994: 990: 986: 982: 975: 971: 967: 958: 956: 952: 948: 940: 937: 934: 930: 927: 926:Strike valley 924: 921: 918: 915: 912: 909: 905: 901: 897: 893: 889: 885: 881: 877: 874: 870: 867: 864: 861: 858: 855: 851: 847: 844: 843: 842: 834: 832: 828: 824: 820: 814: 804: 796: 794: 790: 786: 779:Trough-shaped 776: 772: 770: 766: 762: 758: 753: 751: 746: 739: 735: 731: 726: 719: 714: 705: 703: 699: 695: 691: 687: 682: 680: 675: 672: 668: 664: 660: 652: 648: 643: 630: 626: 622: 617: 611: 604: 602: 595: 585: 583: 582:water erosion 576: 575:Tunnel valley 563: 559: 555: 551: 548: 544: 541: 538: 535: 534: 533: 528: 524: 519: 515: 513: 512:misfit stream 509: 505: 501: 497: 493: 489: 485: 482: 478: 474: 470: 465: 463: 454: 449: 442: 438: 433: 422: 417: 415: 411: 407: 403: 399: 395: 390: 388: 384: 380: 374: 372: 368: 364: 360: 356: 348: 344: 339: 333: 329: 324: 315: 313: 309: 305: 301: 297: 293: 283: 281: 277: 273: 269: 265: 261: 257: 253: 248: 246: 242: 238: 234: 230: 226: 222: 214: 209: 202: 197: 190: 186: 182: 175: 171: 167: 160: 156: 151: 145: 141: 137: 127: 124: 116: 105: 102: 98: 95: 91: 88: 84: 81: 77: 74: â€“  73: 69: 68:Find sources: 62: 58: 52: 51: 46:This article 44: 40: 35: 34: 26: 19: 3892:Flash floods 3844:River cruise 3741:River sports 3594:Stream gauge 3579:Rouse number 3569:Relief ratio 3418:Flood-meadow 3349:Urban runoff 3263:Fluvial flow 3248:River valley 3247: 3218:River island 3183:Meander scar 3098:Alluvial fan 3040:Progradation 2915:Karst spring 2859:Winterbourne 2814:Chalk stream 2776:River source 2751:Distributary 2631:Vallis Alpes 2563:. Retrieved 2553: 2541:. Retrieved 2531: 2522: 2513: 2494: 2488: 2469: 2463: 2451:. Retrieved 2441: 2422: 2416: 2397: 2391: 2372: 2366: 2347: 2341: 2333: 2326:. Retrieved 2322: 2313: 2293: 2286: 2276:, retrieved 2252: 2244: 2233:. Retrieved 2223: 2215: 2210: 2199:. Retrieved 2189: 2164: 2160: 2154: 2135: 2129: 2117:. Retrieved 2115:. Britannica 2107: 2088: 2082: 2064: 2054: 2035: 2029: 1993:Grass valley 1938: 1912:, and other 1899: 1870: 1862:Cauca Valley 1838:(California) 1808:(California) 1796:(California) 1742:(California) 1718:(California) 1698:Grand Canyon 1682:(California) 1680:Death Valley 1664:(California) 1658:(California) 1585:Rhone Valley 1549:Loire Valley 1525:Hallingdalen 1479:Bergensdalen 1379:West Sumatra 1360:Mutou Valley 1314:Klang Valley 1284:(Kazakhstan) 1270:Beqaa Valley 1126:Yellow River 1099: 1084:rock, often 1075: 1070: 1066: 1048: 1030: 1019: 1013: 1009: 978: 944: 928: 840: 823:Gregory Rift 816: 802: 782: 773: 754: 742: 694:side valleys 683: 656: 647:Bryce Canyon 601:UrstromtĂ€ler 597: 578: 552:That of the 543:Side valleys 531: 500:Valley steps 486: 466: 458: 410:rejuvenation 391: 375: 351: 296:moving water 289: 276:Rift valleys 249: 220: 218: 119: 110: 100: 93: 86: 79: 67: 55:Please help 50:verification 47: 25:River Valley 3753:Fly fishing 3677:Fish ladder 3662:Daylighting 3381:Flash flood 3344:First flush 3291:Plunge pool 3015:Downcutting 3000:Debris flow 2975:Aggradation 2849:Stream pool 2608:Valleys.com 2597:"BGU.ac.il" 2565:20 December 2543:20 December 2453:20 December 2447:"Bing maps" 2328:January 16, 2231:. .uwsp.edu 2119:20 December 2005:Paleovalley 1873:(Argentina) 1858:(Argentina) 1740:Napa Valley 1704:Hell's Gate 1617:Upper Rhine 1465:in Eastern 1447:(Australia) 1445:Swan Valley 1429:(Australia) 1421:Hutt Valley 1417:(Australia) 1411:(Australia) 1393:(Australia) 1340:Emin Valley 1322:(Sri Lanka) 1282:Emin Valley 1276:Dang Valley 1251:Uttarakhand 1223:Umba Valley 1211:Nile Valley 1154:agriculture 1146:temperature 1142:fresh water 1130:Mississippi 1078:flood plain 1061:. The term 970:Indus River 888:New England 813:Rift valley 789:periglacial 730:Ibar (lake) 629:Hooker Lake 504:ribbon lake 473:Pleistocene 437:Afon Fathew 272:underground 268:dry valleys 245:glacial ice 185:FljĂłtsdalur 3917:Categories 3859:Wild river 3539:Hydrograph 3529:Hack's law 3494:Baer's law 3438:Inundation 3423:Floodplain 3363:stormwater 3321:Whitewater 3193:Oxbow lake 3030:Knickpoint 3005:Deposition 2898:Hot spring 2839:Streamflow 2829:Stream bed 2746:Confluence 2504:0460860860 2479:0460860860 2432:0140510494 2407:1841581739 2382:1841581739 2357:1841581739 2278:2023-10-19 2235:2011-10-03 2201:2007-05-24 2145:0340090227 2098:0340090227 2045:0340090227 2021:References 1939:See also: 1884:Antarctica 1864:(Colombia) 1852:(Colombia) 1730:(Missouri) 1712:(New York) 1619:Valley or 1589:Matterhorn 1573:Østerdalen 1513:Great Glen 1316:(Malaysia) 1225:(Tanzania) 1178:Costa Rica 1172:A view of 1150:irrigation 1138:prehistory 979:The terms 908:stream bed 894:, and the 892:Appalachia 866:Dry valley 785:denudation 761:Sognefjord 736:Mountain, 702:waterfalls 665:, and the 663:rock types 659:topography 594:Urstromtal 525:mountain, 496:trough-end 383:floodplain 379:meandering 83:newspapers 3829:Limnology 3778:Triathlon 3748:Canyoning 3717:Revetment 3647:Check dam 3559:Main stem 3316:Waterfall 3203:Point bar 3188:Mouth bar 3128:Billabong 3075:Water gap 3070:Wash load 3050:Saltation 2970:Anabranch 2893:Holy well 2781:Tributary 2643:website ( 2641:bilingual 2627:ESA image 1766:(Arizona) 1623:, an old 1599:Romsdalen 1587:from the 1581:, (Italy) 1579:Po Valley 1567:Numedalen 1537:Iron Gate 1383:Indonesia 1308:Kathmandu 1272:(Lebanon) 1219:(Somalia) 1086:claystone 1082:resistant 1031:The word 769:Ikjefjord 750:elevation 745:tributary 588:Meltwater 363:fractures 355:corrasion 229:mountains 170:Romsdalen 144:Argentina 3632:Aqueduct 3499:Baseflow 3466:Effluent 3143:Cut bank 3108:Avulsion 2985:Bed load 2965:Abrasion 2590:UWSP.edu 1965:See also 1922:chasmata 1879:(Brazil) 1832:(Oregon) 1826:(Mexico) 1814:(Mexico) 1724:(Nevada) 1633:(Norway) 1605:Setesdal 1595:(France) 1507:Glen Coe 1503:(Greece) 1320:Mahaweli 1059:Pennines 1057:and the 1037:the term 1001:Scotland 991:are all 974:Pakistan 904:Missouri 900:Arkansas 831:tectonic 793:tropical 738:Bulgaria 732:valley, 690:Salzburg 679:sunshine 671:Tyrolean 527:Bulgaria 481:Abrasion 347:Bulgaria 304:glaciers 256:ice ages 203:, Brazil 187:in East 113:May 2013 72:"Valley" 3923:Valleys 3809:Aquifer 3802:Related 3758:Rafting 3286:Meander 3281:Log jam 3243:Thalweg 3148:Estuary 3020:Erosion 2957:erosion 2869:Springs 2824:Current 2791:Streams 2731:Channel 2694:springs 2690:streams 2645:English 2584:NPS.gov 2519:"Combe" 2169:Bibcode 1772:(Texas) 1760:(Texas) 1369:Oceania 1310:(Nepal) 1253:, India 1231:(Egypt) 1122:Yangtze 1055:Cumbria 947:gullies 884:Ireland 873:erosion 698:hanging 692:), the 667:climate 623:, with 562:Montana 547:Salzach 477:ice age 469:cirques 443:, Wales 441:Dolgoch 408:. Such 406:ice age 343:Vitosha 332:Finland 328:Halikko 308:rifting 292:erosion 241:erosion 215:, Korea 213:Jirisan 189:Iceland 159:Montana 97:scholar 3604:WAFLEX 3476:Sewage 3359:Floods 3301:Riffle 3296:Rapids 3238:Strath 3208:Ravine 3133:Canyon 2888:Geyser 2819:Coulee 2804:Bourne 2799:Arroyo 2702:Rivers 2686:Rivers 2649:German 2501:  2476:  2429:  2404:  2379:  2354:  2301:  2269:  2142:  2095:  2072:  2042:  1987:Canyon 1926:fossae 1918:valles 1908:, the 1820:(Utah) 1790:(Utah) 1676:(Ohio) 1625:graben 1531:Heddal 1501:Sparta 1467:Norway 1453:Europe 1292:Turkey 1288:Ihlara 1184:Africa 1134:Amazon 1118:Ganges 1071:valley 1067:coombe 1045:Clough 1015:cirque 1010:Corrie 997:Gaelic 989:strath 987:, and 981:corrie 955:kloofs 953:, and 951:chines 933:cuesta 896:Ozarks 880:ridges 661:, the 569:Tunnel 508:fjords 402:canyon 398:ravine 365:, and 260:desert 237:stream 221:valley 99:  92:  85:  78:  70:  3702:Levee 3687:Flume 3642:Canal 3386:Flood 3306:Shoal 3173:Gully 3168:Gulch 3138:Chine 3123:Bayou 2980:Armor 2932:Ponor 2707:lists 2600:(PDF) 1999:Gully 1934:rille 1930:Latin 1906:Venus 1469:near 1174:OrosĂ­ 1136:. In 1114:Indus 1063:combe 1026:Welsh 882:. In 827:Earth 757:fjord 523:Pirin 439:near 400:, or 394:gorge 367:folds 233:river 225:hills 104:JSTOR 90:books 3732:Weir 3697:Leat 3361:and 3253:Wadi 3213:Rill 3178:Glen 3163:Gill 3113:Bank 2955:and 2920:list 2903:list 2874:list 2809:Burn 2692:and 2647:and 2567:2020 2545:2020 2499:ISBN 2474:ISBN 2455:2020 2427:ISBN 2402:ISBN 2377:ISBN 2352:ISBN 2330:2015 2299:ISBN 2267:ISBN 2140:ISBN 2121:2020 2093:ISBN 2074:2968 2070:OCLC 2040:ISBN 1910:Moon 1902:Mars 1593:Lyon 1471:GĂ„lĂ„ 1461:The 1245:The 1237:Asia 1106:Nile 1050:Gill 1033:dale 985:glen 902:and 860:Dell 846:Cove 821:and 807:Rift 734:Rila 651:Utah 76:news 3652:Dam 3118:Bar 3093:Ait 2259:doi 2177:doi 1249:in 1021:cwm 995:of 898:of 799:Box 674:Inn 560:in 556:in 235:or 227:or 172:in 142:in 59:by 3919:: 2688:, 2639:, 2629:: 2521:. 2332:. 2321:. 2265:, 2175:. 2165:25 2163:. 1904:, 1499:, 1381:, 1290:, 1176:, 1128:, 1124:, 1120:, 1116:, 1112:, 1108:, 1073:. 1028:. 1008:. 983:, 949:, 890:, 886:, 704:. 681:. 649:, 514:. 498:. 416:. 396:, 373:. 361:, 330:, 314:. 266:, 219:A 157:, 2876:) 2872:( 2709:) 2705:( 2678:e 2671:t 2664:v 2651:) 2602:. 2569:. 2547:. 2507:. 2482:. 2457:. 2435:. 2410:. 2385:. 2360:. 2307:. 2261:: 2238:. 2204:. 2183:. 2179:: 2171:: 2148:. 2123:. 2101:. 2076:. 2048:. 929:: 910:. 875:. 856:. 423:. 126:) 120:( 115:) 111:( 101:· 94:· 87:· 80:· 53:. 27:. 20:.

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