AY Honors/Waterfalls/Answer Key

Waterfalls redirects here. For the Paul McCartney single, see Waterfalls (Paul McCartney song).

Hopetoun Falls near Otway National Park, Victoria, Australia

A waterfall is usually a geological formation resulting from water, often in the form of 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 created as garden and landscape ornament.

Some waterfalls form in mountain 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 landslides, faults or volcanic action.

Formation

Formation of a waterfall

Typically, a stream flow across an area of formations 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 retreat upstream, creating a gorge of recession. Often, the rock strata just below the more resistant shelf will be of a softer type, meaning undercutting, due to splashback, will occur here to form a shallow cave-like formation known as a rock shelter (also known as a rock house) 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.

Waterfalls can also form due to glaciation, 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.

Streams 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.

Havasu Falls, near Supai, Arizona, is an example of a plunge waterfall.

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Examples of large waterfalls

• Angel Falls, the world's highest at 979 m (3212 ft), in Venezuela
• Tugela Falls, the world's second highest at 947 m (3110 ft), in KwaZulu-Natal province, Republic of South Africa.
• Ramnefjellsfossen, the world's third highest at 808m (2685 ft), at Stryn, Nesdalen, Norway.
• Victoria Falls, the world's widest, on the Zambezi River, on the border between Zambia and Zimbabwe
• Boyoma Falls, with the world's highest volume, 17,000 m³/s (600,000 ft³/s), on the Congo River, Democratic Republic of the Congo
• Gocta, the fifth highest in the world at 771 m (2533 ft), located in the province Chachapoyas, Peru
• Yosemite Falls, arguably the tallest in North America, located in Yosemite National Park, United States
• Niagara Falls, most voluminous in North America, on the border between the United States and Canada
• Rhine Falls, Europe's largest, located in Switzerland
• Iguazu Falls, a tall and extremely wide fall located in South America on the Argentina/Brazil border
• Jog Falls, India's highest and second highest in Asia, located in Karnataka state, India
• Jurong Falls in Singapore is said to be the tallest man-made waterfall in the world

External links

• World Waterfall Database