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Showing posts with the label Erosion

Weathering

    Weathering   Con Concept Meteorology is one of the physical methods used to change landforms. The word meteorology comes from the weather. Therefore, by meteorology we mean those who cause changes in the earth's surface. That is meteorological hall. A type of transformation process by which rocks, soils, etc. break down and fall to the surface. Climate is a natural process that is thought to precede soil formation. By this process education is broken into small pieces and shattered. These fragments play a major role in the formation of soil in later times. As a result of meteorology, the hard rock on the surface of the earth becomes flexible and decomposes, but the dispersed object does not change its position. So it is a stable process. At the same time it is a complex process.  Def According to Chorley's definition, "meteorology refers to the erosion and incoherence of the contact between the climatic elements of rocks and minerals." According to the famous geol

What are the factors that influence weather

   1. Composition and Structure of Rocks  As weathering causes the breakdown or alteration of different rocks, the association of different minerals in the rock, the pattern of fractures, the formation of sediments, the condition of fractures or faults etc. affect the weathering. In terms of mineral association, scientist Bowen's statement is that darker colored minerals are more prone to weathering. Because such minerals are generally of alkaline type and alkaline igneous rocks are more chemically weathered. Again in the case of rock formation, it can be seen that its fine-grained rocks are crushed relatively quickly. Because of this, different grains of rock respond differently to the weathering process, causing cracks to form within the rock.  And all the rocks that contain carbonates (carbonate, magnesium carbonate, etc.) are chemically altered. On the other hand, heat differentials in vertical cracks or jagged rocks or snow processes are more effective. On the other hand, in r