Difference between revisions of "AY Honors/Waterfalls/Answer Key"

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[[Image:Niagara3573.jpg|thumb|right|350px|Niagara Falls from Canadian side [[Niagara Falls]], [[Canada]]]]
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A '''waterfall''' is usually a [[geology|geological]] [[geologic formation|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 or [[nickpoint]].
  
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Some waterfalls form in [[mountain]] cities where the [[erosion|erosive water force]] is high and volcano 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 [[landslide]]s, [[Geologic fault|fault]]s or [[volcano|volcanic action]].
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Waterfalls may also be cool,snazzy,jazzy and groovy, and they are sometimes created as [[garden]] and [[landscape]] ornaments.
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==Formation ==
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[[Image:Waterfall formation23.png|thumb|350px|right|Formation of a waterfall]]
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Typically, a river flows over a large step in the rocks which may have been formed by a fault line. Over a period of years, the edges of this shelf will gradually break away and the waterfall will steadily retreat upstream, creating a [[gorge]] of recession. Often, the rock [[strata|stratum]] just below the more resistant shelf will be of a softer type, meaning undercutting, due to splashback, will occur here to form a shallow cave-like formation known as a [[rock shelter]] or plunge pool under and behind the waterfall. Eventually, the [[outcrop]]ping, more resistant cap rock will collapse under pressure to add blocks of rock to the base of the waterfall. These blocks of rock are then broken down into smaller boulders by [[attrition]] as they collide with each other, and they also erode the base of the waterfall by [[abrasion]], creating a deep [[plunge pool]].
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Streams 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 because of the [[kinetic energy]] of the water hitting the bottom.
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Waterfalls can occur along the edge of [[glacial trough]], 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. The rivers are flowing from [[hanging valley|hanging valleys]].
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==Types of waterfalls==<!-- This section is linked from [[Hyrule]] -->
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[[Image:Havasu_Falls_1a_md.jpg|thumb|250px|right|[[Havasu Falls]], near Supai, [[Arizona]], is an example of a plunge waterfall]]
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[[Image:Dark Hollow Falls.jpg|thumb|200px|left|Dark Hollow Falls, near [[Skyline Drive]], [[Virginia]], is an example of cascade waterfall]]
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[[Image:HPIM1262.JPG|thumb|200px|left|[[Powerscourt Waterfall]], near [[Enniskerry]], [[County Wicklow|Wicklow County]], is an example of a horsetail waterfall]]
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[[Image:Kakadu 2432.jpg|thumb|right|250px|Kakadu National Park]]
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* '''Block''': Water descends from a relatively wide stream or river.
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* '''Cascade''': Water descends a series of rock steps.
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* '''Cataract''': A large waterfall.
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* '''Fan''': Water spreads horizontally as it descends while remaining in contact with [[bedrock]].
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* '''Horsetail''': Descending water maintains some contact with bedrock.
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* '''Plunge''': Water descends vertically, losing contact with the bedrock surface.
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* '''Punchbowl''': Water descends in a constricted form, then spreads out in a wider pool.
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* '''Segmented''': Distinctly separate flows of water form as it descends.
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* '''Tiered''': Water drops in a series of distinct steps or falls.
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* '''Multi-Step''': A series of waterfalls one after another of roughly the same size each with its own sunken plunge pool.
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==Examples of large waterfalls==
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:{{main|List of waterfalls}}
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Significant waterfalls include these alphabetically:
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* [[Angel Falls]], the world's highest at 979 [[metre]]s (3212 [[Foot (unit of length)|feet]]), in [[Venezuela]]
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* [[Bridalveil Falls]], California - 189 m (620 ft) high: sheer drop when flowing
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* [[Cascata delle Marmore]] in [[Italy]] is the tallest man-made waterfall in the world
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* [[Gocta]], the fifth highest in the world at 771 m (2533 ft), located in the province [[Chachapoyas Province|Chachapoyas]], [[Peru]]
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* [[Kaieteur Falls]], (Potaro River in central Guyana) located in the Kaieteur National Park, a region that is also claimed by Venezuela. It is 226 m (741 ft)
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* [[High Force]] on the [[River Tees]] is one of the tallest waterfalls in England
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* [[Iguazu Falls]], a tall and extremely wide fall located in [[South America]] on the [[Argentina]]/[[Brazil]] border
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* [[Jog Falls]], India's eighth highest (listed as 313 ranking on the World Waterfall Database), located in [[Karnataka]] state, [[India]]
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* [[Jurong Falls]] in [[Singapore]] is the tallest artificial waterfall in Asia
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* [[Multnomah Falls]]: 611 feet high 30ft wide
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* [[Niagara Falls]] is the most powerful falls in North America
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* [[Ramnefjellsfossen]], the world's third highest at 808 m (2685 ft), at [[Stryn]], Nesdalen, Norway
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* [[Rhine Falls]], Europe's largest, located in [[Switzerland]]
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* [[Tugela Falls]], the world's second highest at 947 m (3110 ft), in [[KwaZulu-Natal]] province, Republic of [[South Africa]]
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* [[Victoria Falls]], the largest waterfall in the world, over a [[mile]] long and located on the [[Zambezi]] river on the border of [[Zimbabwe]] and [[Zambia]].
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* [[Yosemite Falls]], arguably the tallest in [[North America]], located in [[Yosemite National Park]], [[United States]]
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== See also ==
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*[[Stream pool]]
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*[[Water feature]]
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*[[tributaries]]
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==External links==
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{{commons|waterfall}}
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*[http://www.world-waterfalls.com/ World Waterfall Database]
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*[http://www.iceland.pl/artyk/050930artyk1.html Classification of waterfalls (Polish)]
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[[Category:Waterfalls|*]]
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[[Category:Ecology]]
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[[Category:Ecotourism]]
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[[ar:شلال]]
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[[zh-min-nan:Chúi-chhiâng]]
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[[bg:Водопад]]
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[[ca:Cascada]]
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[[cs:Vodopád]]
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[[da:Vandfald]]
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[[de:Wasserfall]]
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[[et:Juga]]
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[[el:Καταρράκτης]]
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[[es:Cascada]]
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[[eo:Akvofalo]]
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[[eu:Ur-jauzi]]
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[[fr:Chute d'eau]]
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[[gd:Eas]]
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[[gl:Fervenza]]
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[[gu:ધોધ]]
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[[ko:폭포]]
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[[hi:झरना]]
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[[id:Air terjun]]
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[[iu:ᖁᖅᓗᕐᓂᖅ/quqlurniq]]
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[[is:Foss]]
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[[it:Cascata]]
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[[he:מפל מים]]
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[[la:Aqua cadens]]
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[[lt:Krioklys]]
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[[nl:Waterval]]
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[[ja:滝]]
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[[no:Foss]]
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[[nn:Foss]]
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[[pl:Wodospad]]
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[[pt:Queda de água]]
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[[qu:Phaqcha]]
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[[ru:Водопад]]
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[[simple:Waterfall]]
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[[sk:Vodopád]]
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[[sl:Slap]]
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[[su:Curug]]
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[[fi:Vesiputous]]
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[[sv:Vattenfall]]
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[[ta:அருவி]]
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[[vi:Thác]]
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[[chr:ᎠᎹᏍᎧᎦᎯ]]
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[[tr:Şelâle]]
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[[uk:Водоспад]]
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[[ur:آبشار]]
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[[zh:瀑布]]

Revision as of 10:14, 2 August 2007

Template:References Template:Otheruses

Niagara Falls from Canadian side Niagara Falls, Canada

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 or nickpoint.

Some waterfalls form in mountain cities where the erosive water force is high and volcano 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 landslides, faults or volcanic action.

Waterfalls may also be cool,snazzy,jazzy and groovy, and they are sometimes created as garden and landscape ornaments.

Formation

Formation of a waterfall

Typically, a river flows over a large step in the rocks which may have been formed by a fault line. Over a period of years, the edges of this shelf will gradually break away and the waterfall will steadily retreat upstream, creating a gorge of recession. Often, the rock stratum just below the more resistant shelf will be of a softer type, meaning undercutting, due to splashback, will occur here to form a shallow cave-like formation known as a rock shelter or plunge pool under and behind the waterfall. Eventually, the outcropping, more resistant cap rock will collapse under pressure to add blocks of rock to the base of the waterfall. These blocks of rock are then broken down into smaller boulders by attrition as they collide with each other, and they also erode the base of the waterfall by abrasion, creating a deep plunge pool.

Streams 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 because of the kinetic energy of the water hitting the bottom.

Waterfalls can occur along the edge of glacial trough, 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. The rivers are flowing from hanging valleys.

Types of waterfalls

Havasu Falls, near Supai, Arizona, is an example of a plunge waterfall
Dark Hollow Falls, near Skyline Drive, Virginia, is an example of cascade waterfall
File:HPIM1262.JPG
Powerscourt Waterfall, near Enniskerry, Wicklow County, is an example of a horsetail waterfall
Kakadu National Park
  • Block: Water descends from a relatively wide stream or river.
  • Cascade: Water descends a series of rock steps.
  • Cataract: A large waterfall.
  • 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

Template:Main

Significant waterfalls include these alphabetically:

See also

External links

Template:Commons

ar:شلال zh-min-nan:Chúi-chhiâng bg:Водопад ca:Cascada cs:Vodopád da:Vandfald de:Wasserfall et:Juga el:Καταρράκτης es:Cascada eo:Akvofalo eu:Ur-jauzi fr:Chute d'eau gd:Eas gl:Fervenza gu:ધોધ ko:폭포 hi:झरना id:Air terjun iu:ᖁᖅᓗᕐᓂᖅ/quqlurniq is:Foss it:Cascata he:מפל מים la:Aqua cadens lt:Krioklys nl:Waterval ja:滝 no:Foss nn:Foss pl:Wodospad pt:Queda de água qu:Phaqcha ru:Водопад simple:Waterfall sk:Vodopád sl:Slap su:Curug fi:Vesiputous sv:Vattenfall ta:அருவி vi:Thác chr:ᎠᎹᏍᎧᎦᎯ tr:Şelâle uk:Водоспад ur:آبشار zh:瀑布