Weathering

Weathering and Erosion

The earth’s surface is constantly changing. This is due to the forces of Weathering, Erosion and Deposition.

Weathering is the breaking down of rocks exposed to the elements.

Erosion means wearing away.

Deposition means dropping off.

There are two types of weathering- Mechanical and Chemical.

  • Mechanical      (Freeze-Thaw action)
  • Chemical          (Acid rain on Limestone)

Mechanical weathering

The main example of mechanical weathering is Freeze-Thaw Action.

This happens when water gets into cracks in the rock and freezes. Water expands when frozen and this causes the rocks to break into smaller pieces called Scree.

Freeze-Thaw Action by Adam Callaghan

Freeze thaw

A rock affected by Freeze-Thaw Action

in a mountainous region

Chemical Weathering

Chemical weathering occurs when acid rain weathers rock, i.e. Limestone. The acid in the rain slowly dissolves the limestone to form Calcium Carbonate. This white liquid then makes its way down through the permeable layers of the limestone to underground caves and caverns. As a result many features are formed. They include Stalagtites and Stalagmites, Pillars and Curtains.

Underground Limestone features formed by Chemical weathering by Nicole Mc Kenna.

Statue chemical weatheringA statue affected by Chemical Weathering (Acid Rain)

Advertisements