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

From Pathfinder Wiki
< AY Honors‎ | WaterfallsAY Honors/Waterfalls/Answer Key
(added m value)
Line 21: Line 21:
 
* [[Angel Falls]], the world's highest at 979 m (3230 ft), in [[Venezuela]] in [[South America]]
 
* [[Angel Falls]], the world's highest at 979 m (3230 ft), in [[Venezuela]] in [[South America]]
 
* [[Victoria Falls]], the world's largest, in [[Africa]], on the [[Zambezi River]] on the border between [[Zambia]] and [[Zimbabwe]]
 
* [[Victoria Falls]], the world's largest, in [[Africa]], on the [[Zambezi River]] on the border between [[Zambia]] and [[Zimbabwe]]
*[[Boyoma Falls]], the world's highest volume, 17,000 m&sup3/2 (600,000 ft&sup3/s), [[Congo River]], [[Democratic Republic of the Congo|Congo]]  
+
*[[Boyoma Falls]], the world's highest volume, 17,000 m&sup3/s (600,000 ft&sup3/s), [[Congo River]], [[Democratic Republic of the Congo|Congo]]  
 
* [[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]]

Revision as of 21:47, 17 February 2004

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

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