Mechanical Weathering

1. Mechanical Weathering • Mechanical weathering affects all rock on Earth’s surface. • Release of Pressure As rock erodes, release of pressure causes the outside of the rock to crack and flake off. • Freezing and Thawing When water freezes in a crack in a rock, it expands and makes the crack bigger. • Animal Actions Burrowing animals like this mole can loosen and break apart rocks and soil. • Plant Growth Roots of plants enter cracks in rocks, forcing the cracks farther apart. • Abrasion Rock particles carried by wind, water, or ice and wear away exposed rock surfaces like sandpaper on wood.

2. Chemical Weathering WATER (H2O) Water dissolves rock. I can also mix with other chemicals to dissolve rock quicker. OXYGEN (O2) Combines with iron to cause rust CARBON DIOXIDE (CO2) Combines with water to cause Type of acid rain LIVING ORGANISMS Grow in cracks in rock and cause additional cracking. Some roots produce weak acids ACID RAIN Air pollution mixes with water to form sulfur, nitrogen and carbon compounds that cause rapid chemical weathering

3. Chemical Weathering • As weathering breaks apart rock, the surface area exposed to weathering increases.

4. Chemical or Mechanical? Chemical Reddish soil Rock in a desert breaking because of repeated heating and cooling Mechanical Ants making large hills Mechanical

5. Rate of Weathering The most important factors that determine the rate at which weathering occurs are the type of rock and the climate. Some rocks weather more easily because they are permeable, which means filled with tiny connected air spaces. Define “permeable” in your notebook, include examples

6. Which Weathered Faster? • The graph shows the rate of weathering for two identical pieces of limestone that weathered in different locations.

7. Time in years Reading Graphs: What does the x-axis of the graph represent? Which Weathered Faster?

8. The thickness of stone lost to weathering Reading Graphs: What does the y-axis of the graph represent? Which Weathered Faster?

9. Stone A lost about 8.5 millimeters; Stone B lost slightly more than 4 millimeters. Reading Graphs: How much thickness did Stone A lose in 1,000 years? How much thickness did Stone B lose in the same period? Which Weathered Faster?

10. Stone A weathered at a faster rate. Drawing Conclusions: Which stone weathered at a faster rate? Which Weathered Faster?

11. They were exposed to different climate conditions. Inferring: Since the two identical pieces of limestone weathered at different rates, what can you infer caused the difference in their rates of weathering? Which Weathered Faster?

12. Soil • Loam, a type of soil, is made up of air, water, and organic matter as well as materials from weathered rock. How is the high percentage of air and water related to the amount of organic matter in the loam? Organic matter helps create space for air and water.

13. Soil • Soil particles range in size from gravel to clay particles too small to be seen by the unaided eye. The sand, silt, and clay shown here have been enlarged.

14. The Process of Soil Formation • Soil forms as rock is broken down by weathering and mixes with other materials on the surface. Soil is constantly being formed wherever bedrock is exposed.

15. The Process of Soil Formation Which soil horizon is most similar to bedrock? Which soil horizon forms last? Which is most important for growing food? C B A

16. Living Organisms in Soil • Some soil organisms make humus, the material that makes soil fertile. Other soil organisms mix the soil and make spaces in it for air and water.

17. Soil Damage and Loss - • Wind erosion is one cause of soil loss. For example, wind erosion contributed to the Dust Bowl on the Great Plains. The Dust Bowl ruined farmland in western Oklahoma and parts of the surrounding states. Wind blew dry particles of soil into great clouds of dust that traveled thousands of kilometers.