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  2. List of fluvial landforms - Wikipedia

    en.wikipedia.org/wiki/List_of_fluvial_landforms

    Landforms related to rivers and other watercourses include: Channel (geography) – Narrow body of water; Confluence – Meeting of two or more bodies of flowing water; Cut bank – Outside bank of a water channel, which is continually undergoing erosion; Crevasse splay – Sediment deposited on a floodplain by a stream which breaks its levees

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

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

    Long-lived river systems can produce a series of terrace surfaces over the course of their geologic lifetime. When rivers flood, sediment deposits in sheets across the floodplain and build up over time. Later, during a time of river erosion, this sediment is cut into, or incised, by the river and flushed downstream. The previous floodplain is ...

  4. Runoff (hydrology) - Wikipedia

    en.wikipedia.org/wiki/Runoff_(hydrology)

    Furthermore, runoff can occur either through natural or human-made processes. [5] Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. [6] [7] The land area producing runoff that drains to a common point is called a drainage basin.

  5. Cycle of erosion - Wikipedia

    en.wikipedia.org/wiki/Cycle_of_erosion

    The geographic cycle, or cycle of erosion, is an idealized model that explains the development of relief in landscapes. [1] The model starts with the erosion that follows uplift of land above a base level and ends, if conditions allow, in the formation of a peneplain . [ 1 ]

  6. River rejuvenation - Wikipedia

    en.wikipedia.org/wiki/River_rejuvenation

    In geomorphology a river is said to be rejuvenated when it is eroding the landscape in response to a lowering of its base level. The process is often a result of a sudden fall in sea level or the rise of land. The disturbance enables a rise in the river's gravitational potential energy change per unit distance, increasing its riverbed erosion rate.

  7. Fluvial sediment processes - Wikipedia

    en.wikipedia.org/wiki/Fluvial_sediment_processes

    In geography and geology, fluvial sediment processes or fluvial sediment transport are associated with rivers and streams and the deposits and landforms created by sediments. It can result in the formation of ripples and dunes , in fractal -shaped patterns of erosion, in complex patterns of natural river systems, and in the development of ...

  8. Baer–Babinet law - Wikipedia

    en.wikipedia.org/wiki/Baer–Babinet_law

    In geography, the Baer–Babinet law, sometimes called Baer's law, [1] identifies a way in which the process of formation of rivers is influenced by the rotation of the Earth. According to the hypothesis, because of the rotation of the Earth, erosion occurs mostly on the right banks of rivers in the Northern Hemisphere , and in the Southern ...

  9. River incision - Wikipedia

    en.wikipedia.org/wiki/River_incision

    River incision is the natural process by which a river cuts downward into its bed, deepening the active channel. Though it is a natural process, it can be accelerated rapidly by human factors including land use changes such as timber harvest, mining, agriculture, and road and dam construction. The rate of incision is a function of basal shear ...

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