Editing Rapids (section)

== Physical factors ==
Rapids are [[hydrology|hydrological]] features between a ''run'' (a smoothly flowing part of a [[stream]]) and a ''[[waterfall#Types|cascade]]''. Rapids are characterized by the river becoming shallower with some [[Rock (geology)|rock]]s exposed above the flow surface.<ref>{{cite web |title=Rapids |url=https://education.nationalgeographic.org/resource/rapids/ |access-date=February 20, 2024 |website=National Geographic}}</ref> 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 [[stream bed|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.<ref name=":0">{{Cite web |title=Rapids - redzet.lv |url=https://www.redzet.lv/en/info/Rapids |access-date=2024-05-01 |website=www.redzet.lv |language=en}}</ref>

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.<ref name=":1">{{Cite web |title=Rapids |url=https://education.nationalgeographic.org/resource/rapids |access-date=2024-05-01 |website=education.nationalgeographic.org |language=en}}</ref> Gradients are typically measured in feet per mile.<ref>{{Cite book |url=https://sitesmedia.s3.amazonaws.com/creekconnections/files/2014/03/StreamGradient.pdf |title=Stream Gradient |publisher=Creek Connections Topographic Map Module}}</ref> This impacts the river's flow or [[Discharge (hydrology)|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.<ref name=":1" />

Rapids typically form due to differential erosion in the sloping strata forming the streambed in presence of a gradient, the softer rocks erode away faster whereas the harder rocks persist resulting in an uneven streambed.<ref>{{cite book|title=The Ultimate Visual Family Dictionary|chapter=Geology, Geography and Meteorology|page=290|publisher=[[DK (publisher)|DK. Pub]]|year=2012|location=New Delhi|language=en|isbn=978-0-1434-1954-9}}</ref><ref name=ng>{{cite web|title=Rapids|website=[[National Geographic Society|National Geographic]]|access-date=19 February 2025|url=https://education.nationalgeographic.org/resource/rapids/}}</ref><ref name=":1"/>

The safety of a section of river is measured by [[International Scale of River Difficulty|classes]] or levels, generally running from I to VI on basis of how navigable the rapids are.<ref name=":0" /><ref name=ng/> 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, often classified as 'U' for Uraftable.<ref>{{Cite web |date=2019-02-18 |title=Whitewater Rapid Classification System - River Difficulty Classification |url=https://kayakbase.com/whitewater-rapid-classification-system/ |access-date=2022-08-21 |website=kayakbase.com |language=en-US}}</ref><ref name=ng/> [[River rafting]] sports are carried out where many rapids are present in the course.

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.<ref>{{Cite book |last=Nelson |first=Stephen |url=https://www2.tulane.edu/~sanelson/eens1110/streams.htm |title=Streams and Drainage Systems |date=November 3, 2015}}</ref>