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Cut banks are located in the Missouri river basin watershed, in northwestern Montana. Cut banks are found in abundance along mature or meandering streams. They are shaped much like a small cliff, and are formed by the erosion of soil as the stream collides with the river bank.

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At Lokoja, Nigeria, the Benue River flows into the Niger. River confluences are crucial parts of the river networks, which connect different rivers and promote material exchange between them.

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Impactivate is the Glenmede-sponsored platform for sustainability and impact related news, debates, and original interviews. Learn more.

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Many side canyons are located in clear creek.  Side canyons are very narrow canyons that often have smooth walls.

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Monument Valley which extends through Utah and Arizona has the most famous collection of buttes in the world. Buttes are smaller flat topped mountains or hills with steep slopes on all sides.

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This is a well known mesa. A mesa is a flat-topped mountain or hill. It is a wide, flat, elevated landform with steep sides.

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One of the most extensive plateaus. A plateau is a flat, elevated landform that rises sharply above the surrounding area on at least one side.

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A shale slope is located here. Shale slopes are very rare open woodlands of steep slopes on calcareous shale or similar fine-bedded, crumbly rock that forms an unstable surface of small rock fragments.

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The Great Escarpment is located within the border region of South Africa and Lesotho. An escarpment is a steep slope or long cliff that formed as an effect of erosion or faulting.

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This is a very well known canyon. A canyon is a deep, steep-walled, V-shaped valley cut by a river through resistant rock.

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Denali National Park and Preserve, Parks Highway, Denali National Park and Preserve, AK

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Many Braided streams are found in Denali National Park. Braided streams have multi-threaded channels that branch and merge to create the characteristic braided pattern.

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This is a well known Delta. A delta extends a river's mouth into the body of water into which it is emptying.

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Floodplains are very common in this location. A flood plain is a an area of low-lying ground adjacent to a river, formed mainly of river sediments and subject to flooding.

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Many oxbow lakes are located alongside the Mississippi River. Oxbow lakes are stillwater lakes. This means that water does not flow into or out of them. There is no stream or spring feeding the lake, and it doesn't have a natural outlet.

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Horseshoe Bend is one of the most famous meander. A meander is when water flows in a curvy, bendy path, like a snake.

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Zambezi River is one of the largest rapids in the world. Rapids are areas of shallow, fast-flowing water in a stream. Rapids tend to form in younger streams, with water flow that is straight and fast.

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The Panama Canal is one of the biggest canals. Canals consist of a trench filled with water.

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A river is a ribbon-like body of water that flows downhill from the force of gravity. A river can be wide and deep, or shallow enough for a person to wade across.

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Water gaps are common in the Ridge-and-Valley Appalachians of eastern North America. A water gap is a gap that flowing water has carved through a mountain range or mountain ridge and that still carries water today.

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One place cuestas are found is in New Mexico. A cuesta is a hill or ridge with a gentle slope on one side, and a steep slope on the other.

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The Lauterbrunnen valley in Switzerland. A valley is elongated depression of the Earth's surface. Valleys are most commonly drained by rivers and may occur in a relatively flat plain or between ranges of hills or mountains.

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Ridges are seen in the Appalachian Mountain ranges. A ridge is a long, narrow, elevated geomorphologic landform, structural feature, and steep sides.

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Anticline Mountains are seen in the Rocky Mountains. An anticline is a fold that is convex upward

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Syncline mountains are located on the shared border between Okanogan County and Whatcom County in Washington state. A syncline mountain is a fold that is concave upward.

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The Himalayas are an active fold mountain.  Folded Mountains extend for great lengths whereas their width is considerably small. Generally, fold mountains have a concave slope on one side and a convex slope on the other.

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The Desert Basin is found in Nevada, but touches others states such as California and Utah. A desert basin is a low-lying area surrounded by land of a higher elevation that receives less than 25 centimeters of rainfall per year.

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The chalk bournes of southern England have many intermittent streams. An Intermittent Stream is a stream or part of a stream that has flowing water during certain times of the year when groundwater provides water for streamflow.

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Taklamakan Desert, 和田县 Hotan Prefecture, Xinjiang, China

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Alluvial fans are located between the Kunlun and Altun mountain ranges that form the southern border of the Taklimakan Desert. An alluvial fan is a triangle-shaped deposit of gravel, sand, and even smaller pieces of sediment, such as silt.

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Horsts are found in Black Forest, Germany. Horsts and Graben go hand and hand; you can't find one without the other. A Horst is a fault block, that has been raised without major tilting or folding.

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Grabens are found in Death Valley. Grabens are valleys with a distinct escarpment on each side caused by the displacement of a block of land downward.

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The Great Basin is located in Nevada where Fault Block Mountains are located. Fault block mountains have no folding of the rocks. Rock blocks are pushed upwards, creating summits and valleys.