Weathering, Erosion, and Soil

What you need to learn

l How the process of weathering breaks down rocks and how erosion transports weathered materials from one place to another

l How soil is formed and why soil is an important natural resource

Weathering

l Process by which rocks on or near Earth’s surface break down and change

l The movement of material is called erosion

 

 

 

Mechanical Weathering

l  Process by which rocks and minerals break down into smaller pieces

l  Also called physical weathering

l  Factors involved:

¡ Temperature – freezing and thawing

l Frost wedging

¡ Pressure – reduction of pressure or increase of pressure

l  Exfoliation: removing of rock layers

Chemical Weathering

l Process in which rocks undergo chemical change

l Often involve water (hydrolysis), oxygen (oxidation), carbon dioxide, and acids

l Temperature influences the rate

What else can effect the rate?

l Climate: warm temperatures, abundant rainfall, and lush vegetation increase the rate

l Cool, dry climates can also have abundant weathering

l Rock type and composition

l Surface area

l Topography and other variables

 

Erosion and Deposition

l  The final stage of erosion is deposition

l  Gravity is a major factor

l  Running water can move large particles

¡ Rill erosion: running water in small channels on sides slopes

¡ Gully erosion: enlarged channels

l  Coastal deposition and erosion

l  Glacial erosion

l  Wind erosion

l  Erosion by plants, animals, and humans

 

Formation of Soils

l Soil is found almost everywhere on Earth

l Soil is loose rock particles and decaying organic material (humus) overlaying the bedrock

l There are a large variety of different types of soils

Soil Composition

l Residual soil: found above the parent material

l Transported soil: moved from parent material to another location

 

l It can take hundreds of years for the formation of only 1cm of soil to form

Soil Profiles

l Vertical sequence of soil layers

l Soil horizon: distinct layer or zone within the profile

¡Horizon A: lots of organic matter and humus

¡Horizon B: found under A and contain subsoils

¡Horizon C: below B, contains weathered parent rock

Types of Soils

Other features of soils

lTexture

lFertility

lColor