The Weathering Process

Weathering is the natural process that breaks down rocks and minerals on Earth's surface over time. It occurs through physical means, like temperature changes causing rocks to crack, or biological activity such as roots growing into cracks. Chemical weathering involves reactions with water, oxygen, or acids, altering the minerals' composition. Both processes weaken rocks, making them more prone to erosion and reshaping landscapes. Weathering is essential for soil formation and influences the landscape's evolving appearance. It happens gradually, driven by environmental factors like climate, moisture, and organisms, playing a key role in Earth's geological cycle.