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  2. Weathering - Wikipedia

    en.wikipedia.org/wiki/Weathering

    Furthermore, chemical and physical weathering often go hand in hand. For example, cracks extended by physical weathering will increase the surface area exposed to chemical action, thus amplifying the rate of disintegration. [6] Frost weathering is the most important form of physical weathering. Next in importance is wedging by plant roots ...

  3. Cheerios effect - Wikipedia

    en.wikipedia.org/wiki/Cheerios_effect

    The effect is observed in small objects which are supported by the surface of a liquid. There are two types of such objects: objects which are sufficiently buoyant that they will always float on the surface (for example, Cheerios in milk), and objects which are heavy enough to sink when immersed, but not so heavy as to overcome the surface tension of the liquid (for example, steel pins on water).

  4. Abrasion (geology) - Wikipedia

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

    Abrasion is a process of weathering that occurs when material being transported wears away at a surface over time, commonly occurring with ice and glaciers. The primary process of abrasion is physical weathering. Its the process of friction caused by scuffing, scratching, wearing down, marring, and rubbing away of materials.

  5. Frost weathering - Wikipedia

    en.wikipedia.org/wiki/Frost_weathering

    If there are small pores, a very quick freezing of water in parts of the rock may expel water, and if the water is expelled faster than it can migrate, pressure may rise, fracturing the rock. Since research in physical weathering begun around 1900, volumetric expansion was, until the 1980s, held to be the predominant process behind frost ...

  6. Hydraulic action - Wikipedia

    en.wikipedia.org/wiki/Hydraulic_action

    Hydraulic action, most generally, is the ability of moving water (flowing or waves) to dislodge and transport rock particles.This includes a number of specific erosional processes, including abrasion, at facilitated erosion, such as static erosion where water leaches salts and floats off organic material from unconsolidated sediments, and from chemical erosion more often called chemical ...

  7. Haloclasty - Wikipedia

    en.wikipedia.org/wiki/Haloclasty

    Haloclasty (also called salt weathering) is a type of physical weathering caused by the growth and thermal expansion of salt crystals. The process starts when saline water seeps into deep cracks and evaporates depositing salt crystals. When the rocks are then heated, the crystals will expand putting pressure on the surrounding rock which will ...

  8. The #1 Surprising Benefit of Drinking Enough Water That No ...

    www.aol.com/1-surprising-benefit-drinking-enough...

    Woman drinking water to stay hydrated. Virtually everyone knows that you can’t live without water. After all, water makes up more than half of our body weight. Hydration is important for every ...

  9. Properties of water - Wikipedia

    en.wikipedia.org/wiki/Properties_of_water

    The action of water on rock over long periods of time typically leads to weathering and water erosion, physical processes that convert solid rocks and minerals into soil and sediment, but under some conditions chemical reactions with water occur as well, resulting in metasomatism or mineral hydration, a type of chemical alteration of a rock ...