Weathering is the natural process of breaking down rocks and minerals on the Earth's surface into smaller particles through environmental factors.
Differentiate between mechanical weathering and chemical weathering.
Describe how rocks undergo weathering.
Enumerate factors that contribute to weathering.
Weathering is the process of breaking down rocks found at Earth's surface.
Weathering is influenced by:
Rainwater
Extreme temperature fluctuations
Biological activities.
Definition: The breaking down of rocks into smaller pieces without altering their chemical composition.
Factors contributing to Mechanical Weathering:
Fluctuating temperatures and pressure.
Biological activity.
Examples: Rocks by the sea change shape due to the force of water during high tide.
Frost Wedging
Process: Involves repeated cycles of freezing and thawing of ice.
Conditions: Requires moisture, existing cracks, and fluctuating temperatures.
Salt Crystal Growth
Process: Occurs when seawater enters crevices in rocks, mainly in rocky shorelines and arid regions.
Mechanism: Salt crystals expand with temperature increases, widening cracks.
Biological Activity
Description: Activity of organisms (plants and animals) that reduce the size of rocks, making them more susceptible to chemical weathering.
Unloading
Process: Erosion or uplift removes thick layers of sediments over buried rocks, reducing pressure and leading to mechanical weathering.
Definition: process where rock materials are altered into different substances with distinct physical and chemical properties.
Dissolution
Process: A solid (e.g., halite) dissolves in a liquid (e.g., water).
Hydrolysis
Process: Water reacts with a mineral resulting in the formation of a new mineral.
Oxidation
Description: The chemical combination of oxygen with a mineral, forming a different mineral with a higher ionic charge.
Climate: The amount of moisture and temperature where weathering occurs affects the process.
Elevation: Higher elevations are more susceptible to weathering due to exposure to environmental factors.
Feature | Mechanical Weathering | Chemical Weathering |
---|---|---|
Definition | Physical breakdown of rocks without changing chemical composition | Chemical alteration of rocks involving reactions. |
Main Processes | Actions such as wind, water, ice, and temperature changes | Interactions with water, acids, oxygen, and organisms. |
Effect on Rocks | Breaks rocks into smaller fragments, altering size and shape | Alters chemical composition, dissolving minerals, weakening structure. |
Timescale | Can occur quickly | Typically gradual over time |
Examples | Frost wedging, water/wind abrasion, thermal expansion | Dissolution by acidic rain, oxidation, biological decay |
Outcome | Smaller rock fragments and sediment formation | Formation of new minerals, altered rock structure |
Weathering involves the breakdown of rocks through mechanical and chemical processes.
Factors influencing weathering include climate, surface area, topographic relief, and rock composition.
Distinction between chemical and mechanical weathering is critical for understanding rock degradation process.