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Waterfall :: Waterfalls
 

Waterfalls redirects here.For the Paul McCartney single , see Waterfalls (Paul McCartney song).

A waterfall is usually a geological formation resulting from water, often in the form of a stream, flowing over an erosion-resistant rock formation that forms a sudden break in elevation. Waterfalls may also be artificial, and they are sometimes created as garden and landscape ornament.

Some waterfalls form in mountain environments where erosion is rapid and stream courses may be subject to sudden and catastrophic change. In such cases, the waterfall may not be the end product of many years of water action over a region, but rather the result of relatively sudden geological processes such as thrust faults or volcanic action.

The hobby of falls bagging is blossoming in many parts of the world.

Formation


Typically, a stream flow across an area of formations strata will form shelves across the streamway, elevated above the further stream bed when the less erosion-resistant rock around it disappears. Over a period of years, the edges of this shelf will gradually break away and the waterfall will steadily move upstream. Often, the rock strata just below the more resistant shelf will be of a softer type, and will erode out to form a shallow cave-like formation known as a rock shelter (also known as a rock house) under and behind the waterfall.

Waterfalls can also form due to glaciation, whereby a stream or river flowing into a glacier continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley are examples of this phenomenon.

Streams often become wider and more shallow just above waterfalls due to flowing over the rock shelf, and there is usually a deep pool just below the waterfall due to the kinetic energy of the water hitting the bottom.

Types of waterfalls


Block : Water descends from a relatively wide stream or river.
Cascade : Water descends a series of rock steps.
Cataract : A large waterfall. See Cataracts of the Nile for a well-known sequence of six.
Fan : Water spreads horizontally as it descends while remaining in contact with bedrock.
Horsetail : Descending water maintains some contact with bedrock.
Plunge : Water descends vertically, losing contact with the bedrock surface.
Punchbowl : Water descends in a constricted form, then spreads out in a wider pool.
Segmented : Distinctly separate flows of water form as it descends.
Tiered : Water drops in a series of distinct steps or falls.
Multi step : A series of waterfalls one after another of roughly the same size each with its own sunken plunge pool.

Examples of large waterfalls


Gallery


Image:Base of Tower Fall with rainbow-750px.JPG|Tower Fall in Yellowstone National Park, USA Image:Iceland_Godafoss 1972.jpg|Godafoss in Iceland Image:Angel falls.jpg|Angel Falls, Venezuela Image:Iguacu-004.jpg|Iguazu Falls, between Brazil and Argentina Image:Wailua_Falls_Hawii.JPG|Wailua Falls in Hawaii, USA Image:Staubbach_Falls_Summer.jpg|Staubbach Falls flows into the town of Lauterbrunnen, Switzerland Image:Iceland Dettifoss 1972-4.jpg|Dettifoss in Iceland Image:National botanical gardens09.jpg|Man-made waterfall at the Australian National Botanic Gardens in Canberra, Australia Image:Waterfall_near_Brienzersee.JPG|Waterfall near Brienzersee, Switzerland Image:Earthen Dam Waterfall Face.JPG|Earthen Dam Waterfall in Waverly, New York, USA Image:Kaieteur.jpg|Kaieteur Falls in Guyana Image:Niagara falls aerial.id.jpg|Niagara Falls, on the border between Canada and the USA Image:austrian.waterfall.at.krimml.arp.jpg|A small part of the Krimml Falls, Austria. Scale is given by the people on the right Image:Burney_Falls_504x402.JPG|Burney Falls, located near Burney, California, USA Image:Victoriafälle.jpg|Victoria Falls in Africa.

External links


Waterfalls

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This article is licensed under the GNU Free Documentation License. It uses material from the "Waterfall".

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