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The biota of floodplains has high annual growth and mortality rates, which is advantageous for the rapid colonization of large areas of the floodplain. This allows them to take advantage of shifting floodplain geometry. [19] For example, floodplain [20] trees are fast-growing and tolerant of root disturbance. Opportunists (such as birds) are ...
A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health.
Floodplain (centre) within the alluvial plain of the Waimakariri River, New Zealand (part of the Canterbury Plains). A small, incised alluvial plain from Red Rock Canyon State Park (California) . An alluvial plain is a plain (an essentially flat landform ) created by the deposition of sediment over a long period by one or more rivers coming ...
Willamette Floodplain; Y. Yolo Bypass This page was last edited on 10 April 2019, at 15:38 (UTC). Text is available under the Creative Commons Attribution ...
1996 China flood, torrential floods, mud-rock flows China: 1996 2,566 1953 Japan flood (1953 Northern Kyushu flood and 1953 Wakayama flood), mainly Kitakyushu, Kumamoto, Wakayama, Kizugawa, massive rain, flood, mudslide Japan: 1953 2,400 [citation needed] North Sea flood, storm surge Netherlands: 838 2,379 [citation needed] 1988 Bangladesh ...
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".
Floodplain restoration is the process of fully or partially restoring a river's floodplain to its original conditions before having been affected by the construction of levees (dikes) and the draining of wetlands and marshes.
The floodplain is within the William L. Finley National Wildlife Refuge and located about 10 miles (16 km) south of Corvallis in Benton County, Oregon. It is the largest remaining native unplowed example of bottomland interior valley grassland in the North Pacific Border natural region.
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