|
|
waterfall
|
Sponsored Links
-
Home and Garden Decor, Furniture & More. waterfalls on Sale.
-
Find Top-Rated Local Water Pros & Get 4 Free Bids Today.
-
Solid bronze spouts, made in Italy. Many unique designs available.
-
Low prices on waterfall. Qualified orders over $25 ship free.
-
Find the Right Contractor for the Job with 1800Contractor«.
-
State of the art fitness ctr. Swim pool, squash and basketball courts.
-
Get back to nature at Georgia's official travel & tourism website.
|
A waterfall is a place where flowing water rapidly drops in elevation as it flows over a steep region or a cliff. Formation  Formation of a waterfall Typically, a river flows over a large step in the rocks that may have been formed by a fault line. As it increases its velocity at the edge of the waterfall, it plucks material from the riverbed. 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. Often, the rock stratum 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 or plunge pool under and behind the waterfall. Eventually, the outcropping, 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, creating a deep plunge pool or gorge.  Baatara gorge waterfall near Tannurin, Lebanon. 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 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. Waterfalls can occur along the edge of a glacial trough, whereby a stream or river flowing into a glacier continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley are examples of this phenomenon. The rivers are flowing from hanging valleys. Classifying WaterfallsWaterfalls are grouped into ten broad classes based on the average volume of water present on the fall using a logarithmic scale. Class 10 waterfalls include Niagara Falls, Paulo Afonso Falls and Khone Falls. Classes of other well-known waterfalls include Victoria Falls and Kaieteur Falls (Class 9); Rhine Falls, Gullfoss and Sutherland Falls (Class 8); Angel Falls and Dettifoss (Class 7); Yosemite Falls, Lower Yellowstone Falls and Umphang Thee Lor Sue Waterfall (Class 6). Types of waterfalls- Block: Water descends from a relatively wide stream or river.
- Cascade: Water descends a series of rock steps.
- Cataract: A large, powerful waterfall.
- 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.
left|220px|thumb|Frozen waterfall in southeast New York- Punchbowl: Water descends in a constricted form and 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 Niagara Falls in the province of Ontario, Canada and state of New York, USA Significant waterfalls are listed alphabetically: - Bridalveil Fall in Yosemite Valley is 189 m (620 ft) high with a sheer drop when flowing.
- Dettifoss, Northeast Iceland is the largest waterfall in Europe in terms of volume discharge, having an average water flow of 200 m3/s.The falls are 100 m wide and have a drop of 44 m down to the Jökulsárgljúfur canyon.
- Gocta is the fifth tallest in the world at 771 m (2532 ft) and located in the province Chachapoyas, Peru.
- Jog Falls is India's tallest (listed as 314 ranking on the World Waterfall Database), located in Karnataka state, India.
- Kaieteur Falls (Potaro River in central Guyana), located in the Kaieteur National Park, is 226 m (741 ft).
See also right|thumb|Plitvice lakes, Croatia
|
|
|
|
|