Earth’s Surface: Chapter 4 Section 1 Mechanical and Chemical Weathering

1. Earth’s Surface: Chapter 4 Section 1Mechanical and Chemical Weathering • Learning Targets: • 1) I can describe how mechanical weathering breaks down rocks • 2) I can explain how chemical weathering breaks down rocks. • 3) I can identify factors that affect the rate at which weathering occurs

2. Weathering Breaks Rocks into Smaller Pieces • Weathering is a process by which natural forces break down rocks. • One kind of weathering occurs when a rock is physically broken apart • Another kind of weathering occurs when a chemical reaction changes the makeup of the rock

3. Mechanical Weathering Produces Physical Changes in Rocks • Mechanical weathering is the breaking up of rocks by natural forces • In this natural process, physical forces split rocks apart but do not change their composition • Ex: Ice wedging, pressure release, Plant root growth, and Abrasion

4. Mechanical Weathering Produces Physical Changes in Rocks • 1. Ice Wedging • When water freezes in the cracks and pores of rocks, the force of its expansion is strong enough to split rocks apart. • This process is strong enough to break up huge boulders. • Common where temperatures rise above and below the freezing point of water, 32 degrees F. • 2. Pressure Release • Over time, Earth’s forces can push rock up to the surface. • The pressure inside the rock is still high, but the pressure on the surface of the rock is released. • This release in pressure causes the rock to expand and form cracks in it. • Exfoliation is a process in which layers or sheets of rock gradually break off

5. ICE WEDGING

6. PRESSURE RELEASE

7. Mechanical Weathering Produces Physical Changes in Rocks • 3. Plant Root Growth • Trees, bushes, and other plants may take root in cracks in rocks. • As the roots of these plants grow, they wedge open the cracks. • The rock can be completely split apart • 4. Abrasion • Abrasion is the process of wearing down by friction • The force of moving water alone can wear away particles of rock. • Wateralso causes rocks to tumble downstream. • Tumbling rocks wear down as they grind against the riverbed and each other. * Ocean waves beating against a rocky shore also wears down rocks by abrasion

8. PLANT ROOT GROWTH

9. ABRASION

10. Chemical Weathering Changes the Mineral Composition of Rocks • Minerals and rocks also undergochemical changes when they react with water and air • Chemicalweathering is the breakdown of rocks by chemical reactions that change the rocks’ makeup, or composition. • When minerals in rocks come in contact with air and water some dissolve and others react and are changed into different minerals

11. DISSOLVING Wateris the main cause of chemical weathering Many more minerals dissolve in water that is slightly acidic. In the atmosphere, small amounts of carbon dioxide dissolve in rainwater creating a weak acid. The rainwater moves through the soil picking up more carbon dioxide from decaying plants. Air pollution can make water even more acidic.

12. Rusting • The oxygenin the air is also involved in chemical weathering. • Many common minerals contain iron • When the oxygen in the air and the watercombines with iron is produces rust (iron oxides)

13. RUSTING

14. Weathering Occurs at Different Rates • Most weathering occurs over long periods of time: hundreds, thousands or millions of years • Factors such as: surface area, rock composition, and climate influence the rate of weathering. • 1. Surface Area: The more of a rock’s surface that is exposed to air and water, the faster the rock will breakdown.

15. Weathering Occurs At Different Rates • 2. Rock Composition: Different kinds of rocksbreak down at differentrates • Ex: Granite breaks down much more slowly than limestone. • 3. Climate: Water is needed for chemical weather to occur. • Heat speeds up chemical weathering. • Therefore, chemical weathering occursfaster in hot, wetregions.