Rapids

Rapids of Kern River, California, USA.

Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Flow, gradient, constriction, and obstacles are four factors that are needed for a rapid to be created.

Rapids are hydrological features between a run (a smoothly flowing part of a stream) and a cascade. Rapids are characterized by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river, resulting in better water quality.[1]

Rapids are categorized in classes, generally running from I to VI.[2] A Class 5 rapid may be categorized as Class 5.1-5.9. While Class I rapids are easy to navigate and require little maneuvering, Class VI rapids pose threat to life with little or no chance for rescue.[3] River rafting sports are carried out where many rapids are present in the course.

Physical factors

For a rapid to form, a necessary condition is the presence of a gradient, which refers to the river or stream's downward slope. When a river has a larger gradient, the water flows downhill faster. Gradients are typically measured in feet per mile. This impacts the river's flow or discharge, which is measured as a volume of water per unit of time. The faster the water flows, the more likely a rapid will form.

Constriction refers to when rivers flow through narrower channels, thus increasing the velocity of the water. This may also lead to the creation of obstructions due to sediment transportation and erosion. Obstacles may occur by human activity, natural landslides and earthquakes, or accumulation of sediment or debris. The more prominent these four factors are present in a river, the more likely that river is to be a rapid river.

Gallery

See also

References

Wikimedia Commons has media related to Rapids.
  1. ^ "Rapids". National Geographic. Retrieved February 20, 2024.
  2. ^ Walbridge, Charlie; Singleton, Mark (2005). "International Scale of River Difficulty". American Whitewater. Archived from the original on 2 April 2018. Retrieved 16 June 2018.
  3. ^ "Whitewater Rapid Classification System - River Difficulty Classification". kayakbase.com. 2019-02-18. Retrieved 2022-08-21.
  • "River Flow Changes Over Time | EARTH 111: Water: Science and Society". Retrieved 2023-03-03.
  • "Understanding Rivers". Retrieved 2023-03-03.
  • "Rivers and Streams, and erosional processes". Retrieved 2023-03-03.
  • Wright, Nick (2020-08-14). "How Do Rapids Form in a River?". Whitewater Guidebook. Retrieved 2023-03-03.
  • Attal, Mikaël (2021-09-24). "Impacts by Moving Gravel Cause River Channels to Widen or Narrow". Eos. Retrieved 2023-03-03.
  • "Water flow obstructions in watercourses - World Problems & Global Issues". The Encyclopedia of World Problems. Retrieved 2023-03-03.
  • Mason, Bill (1984). Path of the Paddle. Northword Press. ISBN 9781559710046.
  • Brocard, G.Y.; van der Beek, P.A. (2006-01-01). "Influence of incision rate, rock strength, and bedload supply on bedrock river gradients and valley-flat widths: Field-based evidence and calibrations from western Alpine rivers (southeast France)". In Willett, Sean D.; Hovius, Niels; Brandon, Mark T.; Fisher, Donald M. (eds.). Tectonics, Climate, and Landscape Evolution (PDF). Vol. 398. Geological Society of America. doi:10.1130/2006.2398(07). ISBN 978-0-8137-2398-3. Retrieved 2023-03-03.

External links

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