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  2. Floodplain - Wikipedia

    en.wikipedia.org/wiki/Floodplain

    A floodplain or flood plain or bottomlands [1] is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high discharge . [ 2 ]

  3. List of fluvial landforms - Wikipedia

    en.wikipedia.org/wiki/List_of_fluvial_landforms

    Floodplain – Land adjacent to a water body which is flooded during periods of high water; Fluvial landforms of streams; Fluvial terrace – Elongated terraces that flank the sides of floodplains and river valleys; Canyon – Deep chasm between cliffs (Gorge) Gully – Landform created by running water and/or mass movement eroding sharply into ...

  4. Terrace (geology) - Wikipedia

    en.wikipedia.org/wiki/Terrace_(geology)

    Sediments underlying fluvial terrace exposed in cutbanks along the Manú River, Peru. In geology, a terrace is a step-like landform. A terrace consists of a flat or gently sloping geomorphic surface, called a tread, that is typically bounded on one side by a steeper ascending slope, which is called a "riser" or "scarp".

  5. What to know about floodplain forests, a struggling ... - AOL

    www.aol.com/news/know-floodplain-forests...

    A floodplain is the land around a river that can flood if the river jumps its banks. Forests that grow on the floodplain are called floodplain forests, sometimes also called bottomland forests.

  6. Fluvial terrace - Wikipedia

    en.wikipedia.org/wiki/Fluvial_terrace

    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".

  7. River morphology - Wikipedia

    en.wikipedia.org/wiki/River_morphology

    The terms river morphology and its synonym stream morphology are used to describe the shapes of river channels and how they change in shape and direction over time. The morphology of a river channel is a function of a number of processes and environmental conditions, including the composition and erodibility of the bed and banks (e.g., sand, clay, bedrock); erosion comes from the power and ...

  8. River terraces (tectonic–climatic interaction) - Wikipedia

    en.wikipedia.org/wiki/River_terraces_(tectonic...

    A series of terraces along a river. The oldest terraces (T1) are higher standing than the younger terraces (T3). The present floodplain (T4) will soon become the youngest terrace surface as the river incises. Terraces can be formed in many ways and in several geologic and environmental settings. By studying the size, shape, and age of terraces ...

  9. Alluvial plain - Wikipedia

    en.wikipedia.org/wiki/Alluvial_plain

    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 ...