A valley is an elongated low area often running between

hills A hill is a landform that extends above the surrounding terrain. It often has a distinct summit, and is usually applied to peaks which are above elevation compared to the relative landmass, though not as prominent as mountains. Hills fall und ...

mountains A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher ...

and typically containing a

river A river is a natural stream of fresh water that flows on land or inside Subterranean river, caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of ...

stream A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a strea ...

running from one end to the other. Most valleys are formed by

erosion Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, tran ...

of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during

ice age An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages, and g ...

s but now are ice-free and occupied by streams or rivers. In

desert A desert is a landscape where little precipitation occurs and, consequently, living conditions create unique biomes and ecosystems. The lack of vegetation exposes the unprotected surface of the ground to denudation. About one-third of the la ...

areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock,

dry valley A dry valley may develop on many kinds of permeable rock, such as limestone, chalk, sand stone and sandy terrains that do not regularly sustain surface water flow. Such valleys do not hold surface water because it sinks into the permeable bed ...

s may also result from drainage now taking place underground rather than at the surface.

Rift valley A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear ...

s arise principally from earth movements, 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.

Formation of valleys

Valleys may arise through several different processes. Most commonly, they arise from

over long periods by moving water 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 internal drainage basin. In polar areas and at high altitudes, valleys may be eroded by

glacier A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires ...

s; these typically have a U-shaped profile in cross-section, in contrast to river valleys, which tend to have a V-shaped profile. Other valleys may arise principally through tectonic processes such as

rifting In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear Fault (geology), downfaulted depression, called a graben, or more commonly ...

. 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 fluvial terraces.

River valleys

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 stream will most effectively erode its bed through

corrasion Corrasion is a geomorphological Geomorphology () is the scientific study of the origin and evolution of topography, topographic and bathymetry, bathymetric features generated by physical, chemical or biological processes operating at or near ...

to produce a steep-sided V-shaped valley. The presence of more resistant rock bands, of geological faults,

fractures Fracture is the appearance of a crack or complete separation of an object or material into two or more pieces under the action of stress (mechanics), stress. The fracture of a solid usually occurs due to the development of certain displacemen ...

, and folds may determine the course of the stream and result in a twisting course with interlocking spurs. 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. Conversely, deposition may take place on the inside of curves where the current is much slacker, the process leading to the river assuming a

meander A meander is one of a series of regular sinuous curves in the Channel (geography), channel of a river or other watercourse. It is produced as a watercourse erosion, erodes the sediments of an outer, concave bank (cut bank, cut bank or river cl ...

ing character. In the lower valley, gradients are lowest, meanders may be much broader and a broader

floodplain A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high Discharge (hydrolog ...

may result. Deposition dominates over erosion. A typical river basin or

drainage basin A drainage basin is an area of land in which 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. A basin is separated from adjacent basins by a perimeter, ...

will incorporate each of these different types of valleys. 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

gorge A canyon (; archaic British English spelling: ''cañon''), gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tend ...

ravine A ravine is a landform that is narrower than a canyon and is often the product of streambank erosion. Ravines are typically classified as larger in scale than gullies, although smaller than valleys. Ravines may also be called a cleuch, dell, ...

, or

canyon A canyon (; archaic British English spelling: ''cañon''), gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency t ...

. 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

. Such rejuvenation may also result in the production of river terraces.

Glacial valleys

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 U-shaped cross-section and are characteristic landforms of mountain areas where glaciation has occurred or continues to take place. The uppermost part of a glacial valley frequently consists of one or more 'armchair-shaped' hollows, or ' cirques', excavated by the rotational movement downslope of a cirque glacier. During glacial periods, for example, the

Pleistocene The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ...

ice ages, it is in these locations that glaciers initially form and then, as the

proceeds, extend downhill through valleys that have previously been shaped by water rather than ice. Abrasion 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. Interlocking spurs associated with the development of river valleys are preferentially eroded to produce truncated spurs, typical of glaciated mountain landscapes. The upper end of the trough below the ice-contributing cirques may be a trough-end. Valley steps (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 ribbon lake or else by sediments. Such features are found in coastal areas as

fjord In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the n ...

s. The shape of the valley which results from all of these influences may only become visible upon the recession of the glacier that forms it. A river or stream may remain in the valley; if it is smaller than one would expect given the size of its valley, it can be considered an example of a

misfit stream A misfit stream is a river that is either too large or too small to have eroded the valley or cave passage in which it flows. This term is also used for a stream or river with meanders that obviously are not proportional in size to the meanders ...

Other interesting glacially carved valleys include: *

Yosemite Valley Yosemite Valley ( ; ''Yosemite'', Miwok for "killer") is a U-shaped valley, glacial valley in Yosemite National Park in the western Sierra Nevada (U.S.), Sierra Nevada mountains of Central California, United States. The valley is about long a ...

(United States) * Side valleys of the Austrian river

Salzach The Salzach (Austrian: �saltsax ) is a river in Austria and Germany. It is in length and is a right tributary of the Inn (river), Inn, which eventually joins the Danube. Its drainage basin of comprises large parts of the Northern Limeston ...

for their parallel directions and hanging mouths. * That of the St. Mary River in Glacier National Park in

Montana Montana ( ) is a landlocked U.S. state, state in the Mountain states, Mountain West subregion of the Western United States. It is bordered by Idaho to the west, North Dakota to the east, South Dakota to the southeast, Wyoming to the south, an ...

, United States.

Tunnel

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 long, wide, and deep (its depth may vary along its length). Tunnel valleys were formed by subglacial water erosion. 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.

Meltwater

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 Urstromtäler. Unlike the other forms of glacial valleys, these were formed by glacial meltwaters.

Transition forms and shoulders

Depending on the

topography Topography is the study of the forms and features of land surfaces. The topography of an area may refer to the landforms and features themselves, or a description or depiction in maps. Topography is a field of geoscience and planetary sci ...

, the rock types, and the

climate Climate is the long-term weather pattern in a region, typically averaged over 30 years. More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years. Some of the meteoro ...

, 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 Tyrolean Inn 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 sunshine. In some stress-tectonic regions of the

Rocky Mountains The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch in great-circle distance, straight-line distance from the northernmost part of Western Can ...

or the Alps (e.g.

Salzburg Salzburg is the List of cities and towns in Austria, fourth-largest city in Austria. In 2020 its population was 156,852. The city lies on the Salzach, Salzach River, near the border with Germany and at the foot of the Austrian Alps, Alps moun ...

), the side valleys are parallel to each other, and are

hanging Hanging is killing a person by suspending them from the neck with a noose or ligature strangulation, ligature. Hanging has been a standard method of capital punishment since the Middle Ages, and has been the primary execution method in numerou ...

. Smaller streams flow into rivers as deep canyons or

waterfall A waterfall is any point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in seve ...

Hanging tributary

Closeup of Bridalveil Fall seen from Tunnel View in Yosemite NP

A hanging valley is a

tributary A tributary, or an ''affluent'', is a stream or river that flows into a larger stream (''main stem'' or ''"parent"''), river, or a lake. A tributary does not flow directly into a sea or ocean. Tributaries, and the main stem river into which they ...

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, makes a shallower U-shaped valley. Since the surfaces of the glaciers were originally at the same

elevation The elevation of a geographic location (geography), ''location'' is its height above or below a fixed reference point, most commonly a reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational equipotenti ...

, the shallower valley appears to be 'hanging' above the main valley. Often, waterfalls form at or near the outlet of the upper valley. Hanging valleys also occur in

systems underwater. The branches of

Sognefjord The Sognefjord or Sognefjorden (, ), nicknamed the King of the Fjords (), is the list of Norwegian fjords, longest and deepest fjord in Norway. Located in Vestland county in Western Norway, it stretches inland from the ocean to the small village ...

are much shallower than the main fjord. The mouth of Fjærlandsfjord is about deep while the main fjord nearby is deep. The mouth of Ikjefjord is only deep while the main fjord is around at the same point. 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 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.

Trough-shaped

Trough-shaped valleys also form in regions of heavy topographic

denudation Denudation is the geological process in which moving water, ice, wind, and waves erode the Earth's surface, leading to a reduction in elevation and in relief of landforms and landscapes. Although the terms erosion and denudation are used interchang ...

. 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

periglacial Periglaciation (adjective: "periglacial", referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing and freezing, very often in areas of permafrost. The meltwater may refreeze in ice wedg ...

regions and in

tropical The tropics are the regions of Earth surrounding the equator, where the sun may shine directly overhead. This contrasts with the temperate or polar regions of Earth, where the Sun can never be directly overhead. This is because of Earth's ax ...

regions of variable wetness. Both climates are dominated by heavy denudation.

Box

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.

Rift

Rift valleys, such as the Albertine Rift and Gregory Rift are formed by the expansion of the

Earth Earth is the third planet from the Sun and the only astronomical object known to Planetary habitability, harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all ...

's crust due to

tectonic Tectonics ( via Latin ) are the processes that result in the structure and properties of the Earth's crust and its evolution through time. The field of ''planetary tectonics'' extends the concept to other planets and moons. These processes ...

activity beneath the Earth's surface.

Terms for valleys

There are many terms used for different sorts of valleys. They include: *

Cove A cove is a small bay or coastal inlet. They usually have narrow, restricted entrances, are often circular or oval, and are often situated within a larger bay. Small, narrow, sheltered bays, inlets, creek (tidal), creeks, or recesses in a coast ...

: A small valley, closed at one or both ends, in the central or southern

Appalachian Mountains The Appalachian Mountains, often called the Appalachians, are a mountain range in eastern to northeastern North America. The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain ...

which sometimes results from the erosion of a geologic window. *

Dell Dell Inc. is an American technology company that develops, sells, repairs, and supports personal computers (PCs), Server (computing), servers, data storage devices, network switches, software, computer peripherals including printers and webcam ...

: A small, secluded, and often wooded valley. *

Dry valley A dry valley may develop on many kinds of permeable rock, such as limestone, chalk, sand stone and sandy terrains that do not regularly sustain surface water flow. Such valleys do not hold surface water because it sinks into the permeable bed ...

: A valley not created by sustained surface water flow. * Erosional valley: A valley formed by

. * Hollow: A term used regionally for a small valley surrounded by mountains or

ridge A ridge is a long, narrow, elevated geomorphologic landform, structural feature, or a combination of both separated from the surrounding terrain by steep sides. The sides of a ridge slope away from a narrow top, the crest or ridgecrest, wi ...

s. In

Ireland Ireland (, ; ; Ulster Scots dialect, Ulster-Scots: ) is an island in the North Atlantic Ocean, in Northwestern Europe. Geopolitically, the island is divided between the Republic of Ireland (officially Names of the Irish state, named Irelan ...

New England New England is a region consisting of six states in the Northeastern United States: Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, and Vermont. It is bordered by the state of New York (state), New York to the west and by the ...

Appalachia Appalachia ( ) is a geographic region located in the Appalachian Mountains#Regions, central and southern sections of the Appalachian Mountains in the east of North America. In the north, its boundaries stretch from the western Catskill Mountai ...

, and the

Ozarks The Ozarks, also known as the Ozark Mountains, Ozark Highlands or Ozark Plateau, is a physiographic region in the U.S. states of Missouri, Arkansas, and Oklahoma, as well as a small area in the southeastern corner of Kansas. The Ozarks cover ...

Arkansas Arkansas ( ) is a landlocked state in the West South Central region of the Southern United States. It borders Missouri to the north, Tennessee and Mississippi to the east, Louisiana to the south, Texas to the southwest, and Oklahoma ...

and

Missouri Missouri (''see #Etymology and pronunciation, pronunciation'') is a U.S. state, state in the Midwestern United States, Midwestern region of the United States. Ranking List of U.S. states and territories by area, 21st in land area, it border ...

, a hollow is a small valley or dry

stream bed A streambed or stream bed is the bottom of a stream or river and is confined within a Stream channel, channel or the Bank (geography), banks of the waterway. Usually, the bed does not contain terrestrial (land) vegetation and instead supports d ...

; often called a holler. * Longitudinal valley: An elongated valley found between two nearly-parallel mountain chains. *

Steephead valley A steephead valley, steephead or blind valley is a deep, narrow, flat bottomed valley with an abrupt ending. Such closed valleys may arise in limestone or karst landscapes, where a layer of permeable rock lies above an impermeable substrate such ...

: A deep, narrow, flat-bottomed valley with an abrupt ending. * Strike valley: A valley typically developed parallel to a

cuesta A cuesta () is a hill or ridge with a gentle slope on one side, and a steep slope on the other. In geology, the term is more specifically applied to a ridge where a harder sedimentary rock overlies a softer layer, the whole being tilted somew ...

from more readily eroded strata. *

Structural valley A structure is an arrangement and organization of interrelated elements in a material object or system, or the object or system so organized. Material structures include man-made objects such as buildings and machines and natural objects such as ...

: A valley formed by geologic events such as drop faults or the rise of highlands. Similar geographical features such as gullies,

chine A chine () is a steep-sided coastal gorge where a river flows to the sea through, typically, soft eroding cliffs of sandstone or clays. The word is still in use in central Southern England—notably in East Devon, Dorset, Hampshire and the Is ...

s, and kloofs, are not usually referred to as valleys.

British regional terms for valleys

The terms corrie, glen, and strath are all

Anglicisation Anglicisation or anglicization is a form of cultural assimilation whereby something non-English becomes assimilated into or influenced by the culture of England. It can be sociocultural, in which a non-English place adopts the English language ...

s of Gaelic terms and are commonly encountered in place-names in

Scotland Scotland is a Countries of the United Kingdom, country that is part of the United Kingdom. It contains nearly one-third of the United Kingdom's land area, consisting of the northern part of the island of Great Britain and more than 790 adjac ...

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 in parts of the world formerly colonized by Britain. ''Corrie'' is used more widely by geographers as a synonym for (glacial) ''

cirque A (; from the Latin word ) is an amphitheatre-like valley formed by Glacier#Erosion, glacial erosion. Alternative names for this landform are corrie (from , meaning a pot or cauldron) and ; ). A cirque may also be a similarly shaped landform a ...

'', as is the word '' cwm'' borrowed from Welsh. The word dale 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, the term typically refers to a wide valley, though there are many much smaller stream valleys within the

Yorkshire Dales The Yorkshire Dales are a series of valleys, or Dale (landform), dales, in the Pennines, an Highland, upland range in England. They are mostly located in the Ceremonial counties of England, ceremonial county of North Yorkshire, but extend into C ...

which are named "(specific name) Dale". Clough is a word in common use in northern England for a narrow valley with steep sides. ''

Gill A gill () is a respiration organ, respiratory organ that many aquatic ecosystem, aquatic organisms use to extract dissolved oxygen from water and to excrete carbon dioxide. The gills of some species, such as hermit crabs, have adapted to allow r ...

'' is used to describe a ravine containing a mountain stream in

Cumbria Cumbria ( ) is a ceremonial county in North West England. It borders the Scottish council areas of Dumfries and Galloway and Scottish Borders to the north, Northumberland and County Durham to the east, North Yorkshire to the south-east, Lancash ...

and the

Pennines The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of highland, uplands mainly located in Northern England. Commonly described as the "Vertebral column, backbone of England" because of its length and position, the ra ...

. The term

combe A combe (; also spelled coombe or coomb and, in place names, comb) can refer either to a steep, narrow valley, or to a small valley or large hollow on the side of a hill; in any case, it is often understood simply to mean a small valley through w ...

(also encountered as ''coombe'') is widespread in southern England and describes a short valley set into a hillside. Other terms for small valleys such as hope, dean, slade, slack and bottom are commonly encountered in place-names in various parts of England but are no longer in general use as synonyms for ''valley''. The term vale is used in England and Wales to describe a wide river valley, usually with a particularly wide

flood plain A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high Discharge (hydrolog ...

or flat valley bottom. In Southern England, vales commonly occur between the outcrops of different relatively erosion-resistant rock formations, where less resistant rock, often

claystone Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone and shale. Most of the particles of which the stone is composed are less than and are too small to ...

has been eroded. An example is the

Vale of White Horse The Vale of White Horse is a Non-metropolitan district, local government district of Oxfordshire in England. It Historic counties of England, was historically part of Berkshire. The area is commonly referred to as the 'Vale of ''the'' White Hors ...

in Oxfordshire.

Human settlement

Some of the first human complex societies originated in river valleys, such as that of the

Nile The Nile (also known as the Nile River or River Nile) is a major north-flowing river in northeastern Africa. It flows into the Mediterranean Sea. The Nile is the longest river in Africa. It has historically been considered the List of river sy ...

, Tigris–Euphrates river system, Tigris-Euphrates, Indus, Ganges, Yangtze, Yellow River, Mississippi River, Mississippi, and arguably the Amazon River, Amazon. In prehistory, the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the cradle of civilization, first civilizations 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.

Notable examples

Africa

* Albertine Rift * East African Rift * Ethiopian Rift Valley * Great Rift Valley * Nile Valley (Egypt/Sudan/Ethiopia/Uganda) * Nugaal Valley (Somalia) * Umba Valley (Tanzania) * Valley of the Kings (Egypt)

Asia

*List of valleys in India *List of valleys in Pakistan * Beqaa Valley (Lebanon) * Inner Terai Valleys of Nepal, Dang Valley (Western Nepal) * Emin Valley (Kazakhstan) * Ihlara valley, Ihlara, Turkey * Jordan Rift Valley (Jordan - Israel) * Jordan Valley (Middle East), Jordan Valley * Kathmandu Valley, Kathmandu (Nepal) * Klang Valley (Malaysia) * Mahaweli (Sri Lanka) * Panjshir Valley (Afghanistan) * Valleys of China **Baligou Valley **Emin Valley **Heizhu Valley **Insukati Valley **Jiuzhaigou Valley **Mutou Valley

Oceania

* Barossa Valley (Australia) * Bulolo Valley (Papua New Guinea) * Cagayan Valley (Philippines) * Capertee Valley (Australia) * Hunter Valley (Australia) * Hutt Valley (New Zealand) * Kangaroo Valley (Australia) * Markham Valley (Papua New Guinea) * Strath Taieri (New Zealand) * Swan Valley, Western Australia, Swan Valley (Australia)

Europe

* Bergensdalen (Vestland, Norway) * Dalen, Telemark (Telemark, Norway) * Danube Valley (Eastern Europe) * Evrotas Valley, Sparta, Laconia, Sparta (Greece) * Glen Coe (Scotland, United Kingdom) * Great Glen (Scotland, United Kingdom) * Gudbrandsdalen (Oppland, Norway) * Hallingdalen (Buskerud, Norway) * Heddal (Telemark, Norway) * Iron Gate (Danube), Iron Gate (Romania/Serbia) * Lauterbrunnen Valley (Bern, Switzerland) * Loire Valley with its famous castles (France) * Midt-Telemark (Telemark, Norway) * Nant Ffrancon (Wales, United Kingdom) * Numedalen (Buskerud, Norway) * Østerdalen (Hedmark, Norway) * Po Valley, (Italy) * Rhone Valley from the Matterhorn to Grenoble and Lyon (France) * Romsdalen (Møre Og Romsdal, Norway) * Setesdal (Agder, Norway) * South Wales Valleys (Wales, United Kingdom) * Upper Rhine Valley or Upper Rhine Plain, an old graben system. (France and Germany) * Vestfjorddalen (Norway)

North America

* Central Valley (California), Central Valley (California) * Coachella Valley (California) * Cumberland Valley (Maryland/Pennsylvania) * Cuyahoga Valley National Park, Cuyahoga Valley (Ohio) * Death Valley (California) * Fraser Canyon (British Columbia) * Fraser Valley (British Columbia) * Grand Canyon (Arizona, United States) * Hell's Gate, British Columbia, Hell's Gate (British Columbia) * Hudson Valley (New York) * Imperial Valley (California) * Las Vegas Valley (Nevada) * Missouri River Valley (Missouri) * Monument Valley (Arizona, Utah) * Napa Valley AVA, Napa Valley (California) * Okanagan Valley (British Columbia) * Ottawa Valley (Ontario/Quebec) * Palo Duro Canyon (Texas) * Phoenix, Arizona, Valley of the Sun (Arizona) * Rio Grande Valley (Texas), Rio Grande Valley (Texas) * Rocky Mountain Trench (British Columbia/Montana) * Saint Lawrence River, Saint Lawrence Valley (Ontario/Quebec/New York) * Salt Lake Valley (Utah) * San Fernando Valley (California) * Shenandoah Valley (Virginia/West Virginia) * Sonoma Valley (California) * Toluca Valley (Mexico) * Valley of the Gods (Utah) * Valley of Mexico (Mexico) * Willamette Valley (Oregon) *

(California)

South America

* Aburra Valley (Colombia) * Calchaquí Valleys (Argentina) * Cauca River, Cauca Valley (Colombia) * Ischigualasto ''Valley of the Moon'' (Argentina) * Paraíba Valley (Brazil)

Antarctica

*West Antarctic Rift System

Extraterrestrial valleys

Numerous elongate depressions have been identified on the surface of Mars, Venus, the Moon, and other Solar System, planets and their satellites and are known as vallis (planetary geology), valles (singular: 'vallis'). Deeper valleys with steeper sides (akin to canyons) on certain of these bodies are known as chasmata (singular: 'chasma'). Long narrow depressions are referred to as Fossa (planetary nomenclature), fossae (singular: 'fossa'). These are the Latin terms for 'valley, 'gorge' and 'ditch' respectively. The German term 'rille' or Latin term 'rima' (signifying 'cleft') is used for certain other elongate depressions on the Moon. See also: * List of valleys on Mars * List of chasmata on Mars * List of valleys on the Moon * List of largest rifts, canyons and valleys in the Solar System

References

Extraterrestrial valleys

Vallis Alpes, bisecting the Lunar Alps
Valles Marineris and Ophir Chasma
bilingual website (English language, English and German language, German) {{Authority control Valleys, Erosion landforms Fluvial landforms Slope landforms Bodies of water

Formation of valleys

River valleys

Glacial valleys

Tunnel

Meltwater

Transition forms and shoulders

Hanging tributary

Trough-shaped

Box

Rift

Terms for valleys

British regional terms for valleys

Human settlement

Notable examples

Africa

Asia

Oceania

Europe

North America

South America

Antarctica

Extraterrestrial valleys

See also

References

External links

Extraterrestrial valleys