A ravine is a landform narrower than a canyon and is often the product of streamcutting erosion. Ravines are typically classified as larger in scale than gullies, although smaller than valleys. A ravine is generally a fluvial slope landform of relatively steep (cross-sectional) sides, on the order of twenty to seventy percent in gradient. Ravines may or may not have active streams flowing along the downslope channel which originally formed them; moreover, often they are characterized by intermittent streams, since their geographic scale may not be sufficiently large to support a perennial watercourse. A ravine is a deep valley which is formed due to linear/dendritic fluvial erosion of loose unconsolidated and bare soils byes.
Other terms for ravine include
- ghost (Nevis)
- gill or ghyll
- Gravina in Puglia
- kloof (South Africa)
- chine (Isle of Wight)
References / notes
- Definition of "ravine" at Merriam-Webster.
- Christopher G. Morris; Academic Press (1992). Academic Press Dictionary of Science and Technology. Gulf Professional Publishing. pp. 1802–. ISBN 978-0-12-200400-1. Retrieved 1 October 2012.
- Ravine. Wikipedia: The free encyclopedia. Accessed 5 November, 2017.
Glossary of terms and customs
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