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  2. Hjulström curve - Wikipedia

    en.wikipedia.org/wiki/Hjulström_curve

    The Hjulström curve, named after Filip Hjulström (1902–1982), is a graph used by hydrologists and geologists to determine whether a river will erode, transport, or deposit sediment. It was originally published in his doctoral thesis "Studies of the morphological activity of rivers as illustrated by the river Fyris. [1]" in 1935. The graph ...

  3. Template:Kennebec River diagram - Wikipedia

    en.wikipedia.org/.../Template:Kennebec_River_diagram

    This is a route-map template for the Kennebec River, a waterway in the United States.. For a key to symbols, see {{waterways legend}}.; For information on using this template, see Template:Routemap.

  4. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    A detailed diagram depicting the global water cycle. The direction of movement of water between reservoirs tends towards upwards movement through evapotranspiration and downward movement through gravity. The diagram also shows how human water use impacts where water is stored and how it moves. [1]

  5. Kawa model - Wikipedia

    en.wikipedia.org/wiki/Kawa_model

    The Kawa model (kawa ), named after the Japanese word for river, is a culturally responsive conceptual framework used in occupational therapy to understand and guide the therapeutic process. [1] Developed by Japanese occupational therapists (OTs), the model draws upon the metaphor of a river to describe human occupation, which according to OTs ...

  6. Stream - Wikipedia

    en.wikipedia.org/wiki/Stream

    As an essential symbol of the river formation environment, the river source needs an objective and straightforward and effective method of judging [clarification needed]. A calculation model of river source catchment area based on critical support flow (CSD) proposed, and the relationship between CSA and CSD with a minimum catchment area ...

  7. River - Wikipedia

    en.wikipedia.org/wiki/River

    A river that feeds into another is a tributary, and the place they meet is a confluence. [4] Rivers must flow to lower altitudes due to gravity. [3] The bed of a river is typically within a river valley between hills or mountains. Rivers flowing through an impermeable section of land such as rocks will erode the slopes on the sides of the river ...

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