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  1. Sub-aerial processes – weathering. Weathering is the decay and disintegration of rock in situ. There are two main types of weathering that affect the coast. These are mechanical and biological weathering.

  2. Wetting and Drying. Rocks containing clay minerals, such as clays and shales. At high tide minerals on the rock surface are soaked with sea water and expand in volume. At low tide, minerals dry and shrink. Repeated cycles of expansion and contraction eventually cause the rock to fragment and crumble. Chemical Weathering

  3. The processes that may cause mechanical rupture are abrasion, crystallization, thermal insolation, wetting and drying, and pressure release. Abrasion occurs when some force causes two rock surfaces to come together causing mechanical wearing or grinding of their surfaces.

  4. 24 kwi 2024 · Weathering is the breaking down or dissolving of rocks and minerals on Earth's surface. Once a rock has been broken down, a process called erosion transports the bits of rock and minerals away. Water, acids, salt, plants, animals, and changes in temperature are all agents of weathering and erosion.

  5. 3 paź 2024 · Wetting and drying. In warmer climates where the water doesn’t freeze, a similar process called wetting and drying occurs which works in the same way, just without the ice. This often occurs in the inter-tidal zone; the area is exposed at low tide but covered at high tide. Rocks expand when they are wet and contract again when dry Salt ...

  6. A wetting-drying cycle refers to a process where soil samples are alternately saturated with water and then dried, simulating natural conditions such as rainfall followed by dry periods. This cycle helps investigate the durability of soil stabilization methods under changing moisture conditions.

  7. Weathering and Mass Wasting. 7.1 Introduction. environment (Bland and Rolls, 1998). This process involves both decomposition (chemical breakdown) and dis-integration (phys. cal breakdown) of rocks and minerals. When particles are moved from their place of formation (either by moving water, wind, glaciers, and gr.

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