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There are two main types of weathering: mechanical/physical weathering and chemical weathering. Mechanical/physical weathering includes exfoliation, ice wedging, organic wedging, and abrasion which break rocks into smaller pieces through forces like heat, freezing water, plant and animal activity, and rocks rubbing together. Chemical weathering involves processes like hydrolysis, oxidation, dissolution, and reactions with acids that cause rocks to decompose and break down on an atomic scale when in contact with water and acids from sources like carbon dioxide, pollution, and decaying plants.













Introduction to the types of weathering: mechanical/physical and chemical, presented by four individuals.
Overview of mechanical weathering including exfoliation, ice wedging, organic activity, and abrasion.
Exfoliation describes the separation of rock layers due to heat and pressure.
Ice wedging occurs when water freezes in rock cracks, causing the rock to fracture.
Organic activity involves burrowing animals, humans, or plants breaking down rocks.
Abrasion is the process of rocks rubbing against each other, leading to rounding.
Introduction to chemical weathering processes: hydrolysis, oxidation, dissolution, and plant acids.
Hydrolysis occurs when rocks break down in water over time, giving a clay-like texture.
Oxidation involves the reaction of oxygen with iron in rocks, resulting in rust and red-orange coloration.
Dissolution happens when rocks dissolve in acidic water, evidenced by small holes.
Carbonation involves rainwater absorbing CO2, forming carbonic acid that reacts with minerals.
Acid precipitation occurs when atmospheric water absorbs pollutants converting them into acids.
Plant decay releases acids that chemically interact with minerals in the rocks.