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

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[[eo:Akvofalo]][[de:Wasserfall]]
 
A '''waterfall''' is a geological formation resulting from a [[stream]] flowing over an [[erosion]]-resistant rock formation that forms a  sudden break in elevation.
 
A '''waterfall''' is a geological formation resulting from a [[stream]] flowing over an [[erosion]]-resistant rock formation that forms a  sudden break in elevation.
  
 
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' worth 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-resistent 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]] under and behind the waterfall.
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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.
  
Waterfalls are a hindrance to river transportation. The [[Welland Canal]] was built in [[1829]] to allow ships to pass Niagra Falls in the Great Lakes.  
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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.  
  
 
Notable waterfalls include:
 
Notable waterfalls include:
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* [[Yosemite Falls]], the tallest in North America in [[Yosemite National Park]] in [[California]], [[United States]].
 
* [[Yosemite Falls]], the tallest in North America in [[Yosemite National Park]] in [[California]], [[United States]].
 
* [[Niagara Falls]], the best-known in [[North America]], located on the [[Niagara River]] on the border between [[New York]], [[United States]], and [[Ontario]], [[Canada]]
 
* [[Niagara Falls]], the best-known in [[North America]], located on the [[Niagara River]] on the border between [[New York]], [[United States]], and [[Ontario]], [[Canada]]
* [[Iguaçu Falls]], in [[South America]], on the [[Iguaçu River]] on the border between [[Brazil]] and [[Argentina]]
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* [[Iguaçú Falls]], in [[South America]], on the [[Iguaçu River]] on the border between [[Brazil]] and [[Argentina]]
 
* [[Cumberland Falls]], the only waterfall in [[North America]] featuring a "moonbow"; located in southeast [[Kentucky]]
 
* [[Cumberland Falls]], the only waterfall in [[North America]] featuring a "moonbow"; located in southeast [[Kentucky]]
 
* [[Rhine Falls]], [[Europe]]'s largest, located in [[Switzerland]]
 
* [[Rhine Falls]], [[Europe]]'s largest, located in [[Switzerland]]
 
* [[Reichenbach Falls]], [[Switzerland]], total drop 250 m (656 feet), at 90 m (300 feet) 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 feet), at 90 m (300 feet) 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.
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*The [[Falls of Saint Anthony]], the highest on the [[Mississippi]].
  
List of notable waterfalls[[http://home.earthlink.net/~geoffcon/facts.htm]]
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See also: [[List of waterfalls]]
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==External Link==
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*[http://home.earthlink.net/~geoffcon/facts.htm List of notable waterfalls]

Revision as of 21:18, 8 May 2003

eo:Akvofalode:Wasserfall A waterfall is a geological formation resulting from a stream flowing over an erosion-resistant rock formation that forms a sudden break in elevation.

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.

Notable waterfalls include:

See also: List of waterfalls

External Link