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    • Erosion and weathering

      Image courtesy of flickr.com

      flickr.com

      • River rocks tend to be smooth and round because of a combination of the geologic processes of erosion and weathering. Rocks are eroded from surrounding areas and are initially rough and jagged, but over many years they are weathered via transport-induced abrasion to become smooth and rounded.
      communityliteracy.org/why-are-rocks-in-a-river-smooth/
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  2. River rocks tend to be smooth and round because of a combination of the geologic processes of erosion and weathering. Rocks are eroded from surrounding areas and are initially rough and jagged, but over many years they are weathered via transport-induced abrasion to become smooth and rounded.

  3. Apr 30, 2021 · Physical forces like wind, water, ice, and gravity move rocks and smash and bump them against each other. Just like a rock tumbler, the rocks lose their jagged edges and then abrasion rounds out all the points that stick out or protrude as they tumble down mountains and through rivers.

  4. Feb 12, 2014 · Transport of pebbles in a stream causes them to collide and rub against one another and the stream bed, and the resulting abrasion produces the familiar smooth and rounded shape of river rocks.

    • Gabor Domokos, Douglas J. Jerolmack, Andras Á. Sipos, Ákos Török
    • 10.1371/journal.pone.0088657
    • 2014
    • PLoS One. 2014; 9(2): e88657.
  5. Apr 12, 2024 · River rocks are smooth and round because natural forces initiate the abrasion process on the rocks that continue for years. The rocks are not round when they form. Only some types of igneous rocks have smooth surfaces because they cool rapidly from lava during the formation process.

  6. For centuries, geologists have recognized that the rocks that line riverbeds tend to be smaller and rounder further downstream. But these experts have not agreed on the reason these patterns exist. Abrasion causes rocks to grind down and become rounder as they are transported down the river.

  7. Feb 12, 2014 · River-bed sediments display two universal downstream trends: fining, in which particle size decreases; and rounding, where pebble shapes evolve toward ellipsoids. Rounding is known to result from...

  8. For centuries, geologists have recognized that the rocks that line riverbeds tend to be smaller and rounder further downstream. But these experts have not agreed on the reason these patterns...

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