1. Chapter 7 Weathering and Soil
Section 7-1 Weathering Study Guide

2. Weathering
The breaking down of rock due to surface processes like plants, animals, air, and water, is called weathering.
Weathering breaks rocks into smaller pieces such as sand, silt, and clay.
These smaller pieces of rock are called sediment.
Over millions of years, weathering has changed Earth’s surface.
There are two different types of weathering.

3. Mechanical Weathering
Mechanical weathering occurs when rocks are broken apart by physical processes.
The chemical makeup of the rock stays the same; each fragment has the same characteristics of the original rock.
The roots of plants grow in the cracks of rocks and enlarge the cracks.
Burrowing animals loosen sediment and bring it to the surface where weathering can act on it.
Ice wedging occurs in temperate and cold climates where water enters cracks in rocks and freezes.
-Water expands when it turns to ice, which breaks rocks apart.
-This process wears down pavement and causes potholes in roads.
-Mechanical weathering breaks rocks into smaller pieces. These smaller pieces have more surface area than the original rock, and more rock is exposed to weathering.

4. Burrowing Animals

5. Ice Wedging

6. Chemical Weathering
Chemical weathering occurs when chemical reactions dissolve the minerals in rocks or change them into different minerals.
This changes the chemical composition of the rock, which weakens the rock.
Natural acids weather rock.
When water reacts with carbon dioxide gas in the air or soil, carbonic acid forms (found in soft drinks).
Carbonic acid dissolves calcite, the main mineral in limestone.

7. Chemical Weathering Cont.
This forms caves.
Feldspar, found in granite, is weathered to form Kaolinite clay in soils.
Roots and decaying plants give off plant acids that dissolve minerals in rocks.
Oxygen causes chemical weathering.
Oxidation occurs when materials are exposed to oxygen and water.
Rust forms when materials containing iron are exposed to water and oxygen in air.
Oxidation gives some rock layers a red color.

8. Weathering 1
Plant Acids
Some roots and decaying plants give off acids that also dissolve minerals in rock. When these minerals dissolve, the rock is weakened.
One good example is a lichen. Lichens are most like plants that secrete acid to eat rocks. Yes, a plant that eats a rock!!

9. Caves

10. Rust/Oxidation

11. Climate Climate affects the rate of weathering.
Climate is the pattern of weather that occurs in a particular area over many years.
Mechanical weathering is more rapid where freezing and thawing are frequent.
Chemical weathering is more rapid and warm, wet climates.

12. Warm Climate=Lots of Weathering

13. Rock Type
Rock type also affects the rate of chemical weathering in a particular climate.
In wet climates, marble weathers more rapidly than granite.

15. Surface Area
The amount of area exposed at the surface will speed up both chemical and mechanical weathering.