From Infogalactic: the planetary knowledge core
Jump to: navigation, search
Rapids featuring whitewater, close to the Rhine Falls
Rapids on the Mississippi River, Pakehnham, Ontario, Canada

Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a run (a smoothly flowing part of a stream) and a cascade. Rapids are characterised 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 colour, 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 are categorized in classes, generally running from I to VI. A Class 5 rapid may be categorized as Class 5.1-5.9. While class I rapids are easy to negotiate and require no maneuvering, class VI rapids pose threat to life with little or no chance for rescue.

See also


  • Mason, Bill (1984). Path of the Paddle. Northword Press. ISBN 9781559710046.<templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>