 Weathering is the breaking down of rocks into

smaller and smaller pieces.

 There are two types of weathering:  

Mechanical Weathering Chemical Weathering

 

Mechanical weathering

is the breakdown of rock by physical means.

Some examples are:   Ice (Ice wedging/frost action is a series of freezing and thawing) Abrasion (wearing away of rock by the mechanical action of other rocks) 

Wind, Water, and Gravity

are different forms of abrasion.

  Chemical Weathering is when rocks break down as a result of chemical reactions causing the composition of rocks to change.

Some examples are   Acid (found in water, precipitation or lichens) Air (Oxygen reacts with iron in a process called Oxidation which forms

Rust).

    Some rocks and minerals are more resistant to weathering, while others experience weathering more

quickly.

Weathering happens more quickly in hot and wet climates.

Climate and rock type are the most important factors in the rate of weathering.

Weathering happens more quickly when there is more surface area.

 For example, a pile of pebbles will weather more

quickly than one large boulder.

 Erosion is the process through which soil and

sediment are transported from one place to another.

 Erosion is primarily responsible for the formation of river systems.

 Wind erosion occurs when wind blows over sand. The sand is deposited when the wind

hits an obstacle.

  The process of wind erosion is called

deflation.

The movement of wind erosion is a bouncing movement called

saltation.

 Wave erosion occurs along shorelines.  Glacial erosion is the mass movement of

glaciers.

 Mass movement is the movement of material down a slope through gravity.

 Examples: Landslide, Mudslide, Creep, Slump  Mass movement can occur quickly (landslide, rock falls) or slowly (creep).

  Soil is valuable because living things need it and fertile soil takes a long time to create. To prevent erosion of valuable soil, we can plant

plants to help hold the soil in place.

 If plants are removed, a situation like the dust bowl in the 1930’s could take place.  Farmers will also leave the stalks of previous year’s crops to help hold the soil in

place.

 Deposition is the process through which soil and sediment is dropped off or deposited.

 Two examples of where this occurs are on beaches and at river

deltas.