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

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[[da:Vandfald]] [[de:Wasserfall]] [[eo:Akvofalo]] [[nl:Waterval]]
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: ''See [[Waterfall, New South Wales]] for the [[suburb]] of [[Sydney]], [[Australia]]''
  
 
[[image:Base of Tower Fall with rainbow-750px.JPG|thumb|right|Tower Fall in Yellowstone National Park]]
 
[[image:Base of Tower Fall with rainbow-750px.JPG|thumb|right|Tower Fall in Yellowstone National Park]]
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Some waterfalls form in montane 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]].
 
Some waterfalls form in montane 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]].
  
Most waterfalls are the result of many years of action of water on the underlying strata.  Typically, a stream will flow across an area of formations, and more resistant rock 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. AND MONKS MONKS ARE SO GREAT EVERYONE LOVES MONKS! MONKS MONKS MONKS! OH YA MONKS!
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Most waterfalls are the result of many years of action of water on the underlying strata.  Typically, a stream will flow across an area of formations, and more resistant rock 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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* [[Rhine Falls]], [[Europe]]'s largest, located in [[Switzerland]]
 
* [[Rhine Falls]], [[Europe]]'s largest, located in [[Switzerland]]
 
* [[Reichenbach Falls]], [[Switzerland]], total drop 250 m (656 ft), at 90 m (300 ft) the Upper Reichenbach Falls is one of the highest cataracts in the [[Alps]].  Scene of the final fictional meeting between [[Sherlock Holmes]] and Professor Moriarty.
 
* [[Reichenbach Falls]], [[Switzerland]], total drop 250 m (656 ft), at 90 m (300 ft) the Upper Reichenbach Falls is one of the highest cataracts in the [[Alps]].  Scene of the final fictional meeting between [[Sherlock Holmes]] and Professor Moriarty.
*The [[Falls of Saint Anthony]], the highest on the [[Mississippi]].
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* [[Saint Anthony Falls]], the only waterfall on the [[Mississippi River]].
  
 
See also: [[List of waterfalls]]
 
See also: [[List of waterfalls]]
  
==External Link==
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==External link==
 
*[http://www.world-waterfalls.com/ World Waterfall Database]
 
*[http://www.world-waterfalls.com/ World Waterfall Database]
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[[Category:Landforms]]
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[[Category:Rivers]]
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[[da:Vandfald]]
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[[de:Wasserfall]]
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[[eo:Akvofalo]]
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[[it:Cascata]]
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[[nl:Waterval]]

Revision as of 16:28, 17 July 2004

See Waterfall, New South Wales for the suburb of Sydney, Australia
File:Base of Tower Fall with rainbow-750px.JPG
Tower Fall in Yellowstone National Park

A waterfall is usually a geological formation resulting from 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.

Some waterfalls form in montane 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.

Most waterfalls are the result of many years of action of water on the underlying strata. Typically, a stream will flow across an area of formations, and more resistant rock 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.

Waterfalls are a hindrance to river transportation. The Welland Canal was built in 1829 to allow ships to pass Niagara Falls in the Great Lakes.

File:Waterfall formation.png

Notable waterfalls include:

See also: List of waterfalls

External link

da:Vandfald de:Wasserfall eo:Akvofalo it:Cascata nl:Waterval