When.com Web Search

  1. Ads

    related to: how are levees formed geography worksheet

Search results

  1. Results From The WOW.Com Content Network
  2. List of fluvial landforms - Wikipedia

    en.wikipedia.org/wiki/List_of_fluvial_landforms

    Levee § Natural levees; Meander – One of a series of curves in a channel of a matured stream; Oxbow lake – U-shaped lake or pool left by an ancient river meander; Pendant bar – fluvial landform formed on the downstream side of a weathering-resistant protrusion

  3. Levee - Wikipedia

    en.wikipedia.org/wiki/Levee

    The side of a levee in Sacramento, California. A levee (/ ˈ l ɛ v i / or / ˈ l ɛ v eɪ /), [a] [1] dike (American English), dyke (British English; see spelling differences), embankment, floodbank, or stop bank is an elevated ridge, natural or artificial, alongside the banks of a river, often intended to protect against flooding of the area adjoining the river.

  4. Backswamp - Wikipedia

    en.wikipedia.org/wiki/Backswamp

    Levees form as a result of the flooding process. Large amounts of rainfall cause the river to become too full during the flooding, where it overflows, carrying sediments into the floodplain. [ 2 ] As the flooding slows and stops, the sediments are deposited, with the largest deposited closer to the river channel and the smaller ones deposited ...

  5. Floodplain - Wikipedia

    en.wikipedia.org/wiki/Floodplain

    Higher rates were found on the levees (4 kg/m 2 or more) and on low-lying areas (1.6 kg/m 2). [8] Sedimentation from the overbank flow is concentrated on natural levees, crevasse splays, and in wetlands and shallow lakes of flood basins. Natural levees are ridges along river banks that form from rapid deposition from the overbank flow.

  6. Abyssal channel - Wikipedia

    en.wikipedia.org/wiki/Abyssal_channel

    Flood (2001) defines a channel-levee system as a single channel with a levee at each side. [13] These levees are formed by the overspilling and flow stripping of turbidity currents. These are most likely to occur during sea level lowstands. A collection of these channels and levees along with overbank sediments form a channel-levee complex.

  7. Crevasse splay - Wikipedia

    en.wikipedia.org/wiki/Crevasse_splay

    Breaches that form a crevasse splay deposits occur most commonly on the outside banks of meanders where the water has the highest energy. Crevasse splay deposits can range in size. Larger deposits can be 6 m (20 ft) thick at the levee and spread 2 km (1.2 mi) wide, while smaller deposits may only be 1 cm (0.39 in) thick. [2]