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A riparian zone or riparian area is the interface between land and a river or stream. [2] In some regions, the terms riparian woodland , riparian forest , riparian buffer zone , riparian corridor , and riparian strip are used to characterize a riparian zone.
The term riparian comes from the Latin word ripa, 'river bank'; technically it refers only to areas adjacent to flowing bodies of water such as rivers, streams, sloughs and estuaries. However, the terms riparian forest and riparian zone have come to include areas adjacent to non-flowing bodies of water such as ponds, lakes, playas and reservoirs.
The Riparian terrestrial Biome, and the ecoregions within it around the world. The riparian zone's fluvial and landform geography; hydrology and engineering; and restoration and conservation . Riparian forest ecology, plant communities and habitats .
Fluvial terraces are elongated terraces that flank the sides of floodplains and fluvial valleys all over the world. They consist of a relatively level strip of land, called a "tread", separated from either an adjacent floodplain, other fluvial terraces, or uplands by distinctly steeper strips of land called "risers".
A riparian buffer of vegetation lining a farm creek in Story County, Iowa. A riparian buffer or stream buffer is a vegetated area (a "buffer strip") near a stream, usually forested, which helps shade and partially protect the stream from the impact of adjacent land uses.
In some regions the terms riparian woodland, riparian forest, riparian buffer zone, or riparian strip are used to characterize a riparian zone. The perceived need for riparian-zone restoration has come about because riparian zones have been altered and/or degraded throughout much of the world [ 1 ] by the activities of mankind affecting natural ...
An old fallacy exists regarding the formation of point bars and oxbow lakes which suggests they are formed by the deposition (dropping) of a watercourse's suspended load claiming the velocity and energy of the stream decreases toward the inside of a bend.
A wide variety of river and stream channel types exist in limnology, the study of inland waters.All these can be divided into two groups by using the water-flow gradient as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.