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  • Understanding Weathering: How Rocks Change Over Time
    Weathering is the process of breaking down the rocks, soils and minerals of the Earth's crust, and transforming them into smaller particles and different materials. There are many different types of weathering, but some of the most common include:

    Physical weathering: This type of weathering is caused by the physical forces of temperature changes and ice. When rocks are exposed to extreme temperatures, they can expand and contract, causing them to crack. When water seeps into cracks in rocks and then freezes, it can also cause them to break apart.

    Chemical weathering: This type of weathering is caused by the chemical reactions of water, oxygen and other elements with the minerals in rocks. For example, when water reacts with iron-containing minerals, it can cause the minerals to rust, which can eventually break down the rock.

    Biological weathering: This type of weathering is caused by the activities of plants, animals and microorganisms. For example, when plant roots grow into cracks in rocks, they can cause the rocks to break apart. When animals burrow into rocks, they can also cause them to break down.

    Weathering can have a number of effects on rocks, including:

    * Changing their texture and composition: Weathering can cause rocks to become more porous and less cohesive, and can also change their chemical composition.

    * Producing new materials: Weathering can produce new materials, such as clays and soils.

    * Exposing underlying rocks: Weathering can remove overlying layers of rock, exposing the underlying rocks.

    * Creating new landforms: Weathering can create new landforms, such as valleys and mountains.

    Weathering is an important process that plays a role in the Earth's surface processes and the development of landscapes.

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