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  2. Fjaðrárgljúfur - Wikipedia

    en.wikipedia.org/wiki/Fjaðrárgljúfur

    Fjaðrárgljúfur (pronounced [ˈfjaðrˌaurˌkljuː(v)ʏr̥], "feather river canyon") is a canyon in south east Iceland.The Fjaðrá river flows through it. The canyon has steep walls and winding water. It is up to 100 m (330 ft) deep [1] and about 2

  3. Stream - Wikipedia

    en.wikipedia.org/wiki/Stream

    A segment where the water is deeper and slower moving. Rapids A turbulent, fast-flowing stretch of a stream or river. Riffle A segment where the flow is shallower and more turbulent. River A large natural stream, which may be a waterway. [34] Run A somewhat smoothly flowing segment of the stream. Spring

  4. Stokes flow - Wikipedia

    en.wikipedia.org/wiki/Stokes_flow

    Stokes flow (named after George Gabriel Stokes), also named creeping flow or creeping motion, [1] is a type of fluid flow where advective inertial forces are small compared with viscous forces. [2] The Reynolds number is low, i.e. R e ≪ 1 {\displaystyle \mathrm {Re} \ll 1} .

  5. Bernard Gitton - Wikipedia

    en.wikipedia.org/wiki/Bernard_Gitton

    Modern water clock by Bernard Gitton Bernard Gitton ( French pronunciation: [bɛʁnaʁ ʒitɔ̃] ); born 24 June 1935 [ 1 ] ) is a French physicist and artist who has built modern water clocks , fountains and other devices relating art and science.

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  7. Eddy (fluid dynamics) - Wikipedia

    en.wikipedia.org/wiki/Eddy_(fluid_dynamics)

    Reynolds Experiment (1883). Osborne Reynolds standing beside his apparatus. In 1883, scientist Osborne Reynolds conducted a fluid dynamics experiment involving water and dye, where he adjusted the velocities of the fluids and observed the transition from laminar to turbulent flow, characterized by the formation of eddies and vortices. [5]

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