A waterfall is a place where flowing water rapidly drops in elevation as it flows over a steep region or a cliff. Waterfalls are considered to be one of the most beautiful phenomena in nature.[1] Some waterfalls are used to generate hydro-electric Hydroelectricity is the term referring to electricity generated by hydropower; the production of electrical power through the use of the gravitational force of falling or flowing water. It is the most widely used form of renewable energy. Once a hydroelectric complex is constructed, the project produces no direct waste, and has a considerably power.

Contents

Formation

Formation of a waterfall

Waterfalls are most commonly formed when a river is young.[1] At these times the channel is often narrow and deep. When the river courses over resistant bedrock, erosion happens slowly, while downstream the erosion occurs more rapidly.[1][2] As the watercourse increases its velocity at the edge of the waterfall, it plucks material from the riverbed. Whirlpools A whirlpool is a swirling body of water usually produced by ocean tides. The vast majority of whirlpools are not very powerful. More powerful ones are more properly termed maelstroms. Vortex is the proper term for any whirlpool that has a downdraft. (Technically, these approximate to a 'free vortex', in which the tangential velocity increases as created in the turbulence as well as sand and stones carried by the watercourse increase the erosion capacity.[1] This causes the waterfall to carve deeper into the bed and to recede upstream. Often over time, the waterfall will recede back to form a canyon or gorge downstream as it recedes upstream, and it will carve deeper into the ridge above it.[3] The rate of retreat for a waterfall can be as high as one and half metres per year.[1]

Often, the rock stratum In geology and related fields, a stratum is a layer of rock or soil with internally consistent characteristics that distinguishes it from contiguous layers. Each layer is generally one of a number of parallel layers that lie one upon another, laid down by natural forces. They may extend over hundreds of thousands of square kilometers of the Earth' just below the more resistant shelf will be of a softer type, meaning that undercutting due to splashback will occur here to form a shallow cave-like formation known as a rock shelter Rock shelters form because a rock stratum such as sandstone that is resistant to erosion and weathering has formed a cliff or bluff, but a softer stratum, more subject to erosion and weathering, lies just below the resistant stratum, and thus undercuts the cliff or plunge pool A Plunge pool can be a natural hydrologic Fluvial landform feature or a constructed recreational garden feature under and behind the waterfall. Eventually, the outcropping An outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth.[citation needed], 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 Abrasion is the mechanical scraping of a rock surface by friction between rocks and moving particles during their transport by wind, glacier, waves, gravity, running water or erosion. After friction, the moving particles dislodge loose and weak debris from the side of the rock. These particles can be dissolved in the water source, creating a deep plunge pool or gorge.

Baatara gorge waterfall near Tannurin, Lebanon Lebanon (pronounced /ˈlɛbənɒn/ or /ˈlɛbənən/; Arabic: لُبْنَان‎ Lubnān; French: Liban), officially the Republic of Lebanon[nb 1] (Arabic: اَلْجُمْهُورِيَّة اَللُّبْنَانِيَّة al-Jumhūrīyah al-Lubnānīyah; French: République libanaise), is a country on the eastern shore of the Mediterranean

Streams become wider and shallower 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 The kinetic energy of an object is the extra energy which it possesses due to its motion. It is defined as the work needed to accelerate a body of a given mass from rest to its current velocity. Having gained this energy during its acceleration, the body maintains this kinetic energy unless its speed changes. Negative work of the same magnitude of the water hitting the bottom. Waterfalls normally form in a rocky area due to erosion. After a long period of being fully formed, the water falling off the ledge will retreat, causing a horizontal pit parallel to the waterfall wall. Eventually, as the pit grows deeper, the waterfall collapses to be replaced by a steeply sloping stretch of river bed.[1]

A river sometimes flows over a large step in the rocks that may have been formed by a fault line In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement. Large faults within the Earth's crust result from the action of tectonic forces. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Waterfalls can occur along the edge of a glacial trough, whereby a stream or river flowing into a glacier A glacier is a perennial mass of ice which moves over land. A glacier forms in locations where the mass accumulation of snow and ice exceeds ablation over many years. The word glacier comes from French via the Vulgar Latin glacia, and ultimately from Latin glacies meaning ice. The corresponding area of study is called glaciology continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley Yosemite Valley is a glacial valley in the western Sierra Nevada mountains of California, carved out by the Merced River. The valley is about 8 miles (13 km) long and up to 8,000 feet (2,400 m) deep, surrounded by high granite summits such as Half Dome, El Capitan, and Cloud's Rest, and densely forested with pines. Tenaya, Illilouette and are examples of this phenomenon, which is referred to as a hanging valley. Another reason hanging valleys may form is where two rivers join and one is flowing faster than the other.[1]

Classification

Waterfalls are grouped into ten broad classes based on the average volume of water present on the fall using a logarithmic scale A logarithmic scale is a scale of measurement that uses the logarithm of a physical quantity instead of the quantity itself. Class 10 waterfalls include Niagara Falls The Niagara Falls are voluminous waterfalls on the Niagara River, straddling the international border between the Canadian province of Ontario and the U.S. state of New York. The falls are 17 miles north-northwest of Buffalo, New York and 75 miles (120 km) south-southeast of Toronto, Ontario, between the twin cities of Niagara Falls, Ontario, and, Paulo Afonso Falls and Khone Falls.

Classes of other well-known waterfalls include Victoria Falls The Victoria Falls or Mosi-oa-Tunya is a waterfall located in southern Africa on the Zambezi River between the countries of Zambia and Zimbabwe. The falls are some of the largest in the world and Kaieteur Falls (Class 9); Rhine Falls, Gullfoss and Sutherland Falls (Class 8); Angel Falls Angel Falls or Kerepakupai merú is the world's highest waterfall, with a height of 979 m (3,212 ft) and a plunge of 807 m (2,647 ft). The waterfall drops over the edge of the Auyantepui mountain in the Canaima National Park (Spanish: Parque Nacional Canaima), a UNESCO World Heritage site in the Gran Sabana region of Bolívar State, Venezuela and Dettifoss (Class 7); Yosemite Falls, Lower Yellowstone Falls Yellowstone Falls consist of two major waterfalls on the Yellowstone River, within Yellowstone National Park, Wyoming, United States. As the Yellowstone river flows north from Yellowstone Lake, it leaves the Hayden Valley and plunges first over Upper Yellowstone Falls and then a quarter mile downstream over Lower Yellowstone Falls, at which point and Umphang Thee Lor Sue Waterfall (Class 6).[4]

Types

Main article: List of waterfalls by type Dark Hollow Falls, near Skyline Drive, Virginia The area's history begins with several indigenous groups, including the Powhatan. In 1607 the London Company established the Colony of Virginia as the first permanent New World English colony. Land from displaced Native American tribes and slave labor each played significant roles in the colony's early politics and plantation economy. Virginia was, is an example of a cascade waterfall [6]">

Examples of large waterfalls[6]

Havasu Falls The Havasu ’Baaja , or more commonly the Havasupai, are a Native American tribe located in the northwestern part of the American state of Arizona. The tribe is well-known for being the only permanent inhabitants in the Grand Canyon, where they have lived for over 800 years. It also holds the distinction of being one of the only places left in, near Supai, Arizona Arizona is the 48th state and last of the contiguous states admitted to the Union, achieving statehood on February 14, 1912 - the 50th anniversary of Arizona's recognition as a territory of the United States. Arizona is noted for its desert climate, exceptionally hot summers, and mild winters, however it also features pine forests and mountain, is an example of a plunge waterfall Powerscourt Waterfall, near Enniskerry, Wicklow County County Wicklow is one of the traditional counties of Ireland and is located within the province of Leinster. It was named after the town of Wicklow (which derives from the Old Norse name Víkingalág or Wykynlo), Ireland Ireland (pronounced [ˈaɾlənd],; Irish: Éire, pronounced [ˈeːɾʲə] ( listen); Ulster Scots: Airlann) is the third largest island in Europe and the twentieth largest island in the world. It lies to the northwest of continental Europe and is surrounded by hundreds of islands and islets. To the east of Ireland is Great Britain, separated from, is an example of a horsetail waterfall Aerial view of Niagara Falls in the state of New York New York City, which is geographically the largest city in the state and most populous in the United States, is known for its history as a gateway for immigration to the United States and its status as a financial, cultural, transportation, and manufacturing center. According to the U.S. Department of Commerce, it is also a destination of choice, US ^ b. English is the de facto language of American government and the sole language spoken at home by 80% of Americans age five and older. Spanish is the second most commonly spoken language, and province of Ontario Ontario is bordered by Manitoba on its west, Hudson Bay on its north, and Quebec on its east, and by five States of the United States to its south : Minnesota, Michigan, Ohio, Pennsylvania (Lake Erie) and New York. All but a small portion of Ontario's 2,700 km (1,677 mi) border with the United States follow inland waterways: from the west at Lake, Canada The land occupied by Canada was inhabited for millennia by various groups of Aboriginal peoples. Beginning in the late 15th century, British and French expeditions explored, and later settled, along the Atlantic coast. France ceded nearly all of its colonies in North America in 1763 after the Seven Years' War. In 1867, with the union of three Duruitoarea waterfall in Ceahlău, Romania Romania (pronounced /roʊˈmeɪniə/ roe-MAY-nee-ə; dated: Rumania, Roumania; Romanian: România [romɨˈni.a] ( listen)) is a country located at the crossroads of Central and Southeastern Europe, north of the Balkan Peninsula, on the Lower Danube, within and outside the Carpathian arch, bordering on the Black Sea. Almost all of the Danube Delta Plitvice lakes, Croatia Croatia (pronounced /kroʊˈeɪʃə/ , kroe-AY-shə; Croatian: Hrvatska pronounced [xř̩ʋaːtskaː]), officially the Republic of Croatia (Croatian: Republika Hrvatska listen (help·info)), is a country in Central Europe and Southeastern Europe at the crossroads of the Pannonian Plain, the Balkans, and the Adriatic Sea. Its capital and largest Main articles: List of waterfalls by height and List of waterfalls by flow rate

Significant waterfalls are listed alphabetically:

See also

Wikimedia Commons has media related to: Waterfalls

References

  1. ^ a b c d e f g Carreck, Rosalind, ed (1982). The Family Encyclopedia of Natural History. The Hamlyn Publishing Group. pp. 246—248. ISBN 011202257.
  2. ^ a b c http://geography.howstuffworks.com/terms-and-associations/waterfall.htm/printable
  3. ^ http://www.classzone.com/books/earth_science/terc/content/visualizations/es1305/es1305page01.cfm?chapter_no=visualization
  4. ^ Richard H. Beisel Jr., International Waterfall Classification System, Outskirts Press, 2006 ISBN 1-59800-340-2
  5. ^ a b c d e f g h i j k l http://worldwaterfalls.com/waterfall_types.php
  6. ^ World Waterfall Database

Categories: Water | Waterfalls | Fluvial landforms

 

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How would I build a mini waterfall, rock garden, and plants for my desk?
Q. I have seen desk waterfalls for sale, and of course plans. But I'm thinking almost a mini-tank with a few water plants, with a waterfall that falls into it, with rocks around it. Wouldn't that be fantastic to have on your desk?! Any ideas on where to buy such a thing? Or to buy something that I could easily modify? Or how to build one? Thanks!
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