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

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(Added link to waterfalls in Australia)
 
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{{otheruses}}
 
{{otheruses}}
[[Image:Hopetoun falls.jpg|thumb|right|250px|Hopetoun Falls near [[Otway National Park]], [[Victoria, Australia|Victoria]], [[Australia]]]]  
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[[Image:Hopetoun falls.jpg|thumb|right|350px|Hopetoun Falls near [[Otway National Park]], [[Victoria, Australia|Victoria]], [[Australia]]]]  
  
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 used for [[garden]] and [[landscape]] ornament.
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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. Waterfalls may also be artificial, and they are sometimes created as [[garden]] and [[landscape]] ornament.
 
 
Some waterfalls form in [[mountain|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 fault]]s or [[volcano|volcanic action]].
 
  
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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 fault]]s or [[volcano|volcanic action]].
  
 
==Formation ==
 
==Formation ==
 
[[Image:Waterfall formation23.png|thumb|350px|right|Formation of a waterfall]]
 
[[Image:Waterfall formation23.png|thumb|350px|right|Formation of a waterfall]]
Some waterfalls are the result of the underlying strata. 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.
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Some waterfalls are the result of the underlying [[stratum|strata]]. 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.
  
 
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.
 
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.
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; Cataract : A large waterfall. See [[Cataracts of the Nile]] for a well-known sequence of six.
 
; 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]].
 
; Fan : Water spreads horizontally as it descends while remaining in contact with [[bedrock]].
; Horsetail : Descending water maintains some contact with bedrock
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; Horsetail : Descending water maintains some contact with bedrock.
; Plunge : Water descends vertically, losing contact with the bedrock surface
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; Plunge : Water descends vertically, losing contact with the bedrock surface.
 
; Punchbowl : Water descends in a constricted form, then spreads out in a wider pool.
 
; Punchbowl : Water descends in a constricted form, then spreads out in a wider pool.
 
; Segmented : Distinctly separate flows of water form as it descends.
 
; Segmented : Distinctly separate flows of water form as it descends.
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* [[Angel Falls]], the world's highest at 979 m (3230 ft), in [[Venezuela]]
 
* [[Angel Falls]], the world's highest at 979 m (3230 ft), in [[Venezuela]]
* [[Ramnefjellsfossen]], the world's third highest, and highest on the European continent, at 808 m, located at Stryn, Nesdalen, Norway.
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* [[Ramnefjellsfossen]], the world's third highest, and highest on the [[Europea]]n continent, at 808 m, located at Stryn, Nesdalen, [[Norway]]
 
* [[Victoria Falls]], the world's widest, on the [[Zambezi River]], on the border between [[Zambia]] and [[Zimbabwe]]
 
* [[Victoria Falls]], the world's widest, on the [[Zambezi River]], on the border between [[Zambia]] and [[Zimbabwe]]
 
* [[Boyoma Falls]], with the world's highest volume, 17,000 m&sup3;/s (600,000 ft&sup3;/s), on the [[Congo River]], [[Democratic Republic of the Congo]]
 
* [[Boyoma Falls]], with the world's highest volume, 17,000 m&sup3;/s (600,000 ft&sup3;/s), on the [[Congo River]], [[Democratic Republic of the Congo]]
 
* [[Gocta]], the fifth highest in the world at 771 m, located in the province [[Chachapoyas Province|Chachapoyas]], [[Peru]]
 
* [[Gocta]], the fifth highest in the world at 771 m, located in the province [[Chachapoyas Province|Chachapoyas]], [[Peru]]
* [[Yosemite Falls]], the tallest in North America, located in [[Yosemite National Park]], [[United States]]
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* [[Yosemite Falls]], the tallest in [[North America]], located in [[Yosemite National Park]], [[United States]]
* [[Niagara Falls]], most voluminous in North America, on the border between the United States and Canada
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* [[Niagara Falls]], most voluminous in North America, on the border between the United States and [[Canada]]
* [[Rhine Falls]], [[Europe]]'s largest, located in [[Switzerland]]
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* [[Rhine Falls]], Europe's largest, located in [[Switzerland]]
 
* [[Iguazu Falls]], a tall and extremely wide fall located in [[South America]] on the [[Argentina]]/[[Brazil]] border
 
* [[Iguazu Falls]], a tall and extremely wide fall located in [[South America]] on the [[Argentina]]/[[Brazil]] border
* [[Jog Falls]], India's highest and second highest in Asia, located in [[Karnataka]] state, [[India]]
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* [[Jog Falls]], India's highest and second highest in [[Asia]], located in [[Karnataka]] state, [[India]]
 
* [[Jurong Falls]] in [[Singapore]] is said to be the tallest man-made waterfall in the world
 
* [[Jurong Falls]] in [[Singapore]] is said to be the tallest man-made waterfall in the world
  
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Image:Kaieteur.jpg|[[Kaieteur Falls]] in [[Guyana]]
 
Image:Kaieteur.jpg|[[Kaieteur Falls]] in [[Guyana]]
 
Image:Niagara falls aerial.id.jpg|[[Niagara Falls]], on the border between Canada and the USA
 
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  
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Image:austrian.waterfall.at.krimml.arp.jpg|A small part of the [[Krimml Falls]], Austria. Scale is given by the people on the right  
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Image:Burney_Falls_504x402.JPG|Burney Falls, located near [[Burney, California]], USA
 
</gallery>
 
</gallery>
  

Revision as of 13:08, 2 April 2006

Template:Otheruses

Hopetoun Falls near Otway National Park, Victoria, Australia

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.

Formation

Formation of a waterfall

Some waterfalls are the result of the underlying strata. 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.

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

Cascade-style waterfall in Oregon, United States.
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

Template:Main

Gallery

External links

Template:Commons

ca:Cascada cs:Vodopád da:Vandfald de:Wasserfall et:Juga es:Cascada eo:Akvofalo fr:Chute d'eau gu:ધોધ id:Air terjun it:Cascata he:מפל מים la:Cataracta nl:Waterval ja:滝 no:Foss nn:Foss pl:Wodospad pt:Cachoeira simple:Waterfall sl:Slap su:Curug fi:Vesiputous sv:Vattenfall uk:Водоспад zh:瀑布