Unit 7 Day 1 Weathering Mechanical Weathering Weathering Mechanical weathering (also called ) is the process by which rocks and minerals break down into Mechanical weathering does not change the composition, only the the rock and of SOL 8 The student will investigate and understand geologic processes…... Key concepts include b. processes (…weathering, erosion, deposition, and sedimentation) and their resulting features. Objective 1 Summarize weathering as the process by which rocks are broken down by the action of water, air, and organisms. 2 Distinguish between physical ( ) and weathering. 3 Recognize factors that affect the rate of weathering. Enduring Understandings Weathering, erosion, and deposition are interrelated processes that form a cycle of forces that and the Earth’s surface. Weathering Immediately after the first rocks on earth crystallized billions of years ago the process of weathering began to take effect to break them down again. Weathering is the process by which rocks on or near the Earths surface and Erosion is the and weathered material from one location to another. – plays a significant role in mechanical weathering. As water it and will crack rocks is another factor in mechanical weathering as overlying layers of rock are removed the pressure is reduced and the exposed surface will expand and crack is the process by which the outer layers of rocks are stripped off of Materials are transported by moving 5 Chemical Weathering Factors Affecting the rate of Weathering Exposed rocks can undergo changes in their as well and result in the formation of new minerals and the release of substances. Water, Natural weathering is a very process. Certain conditions and interactions can accelerate or slow the process significantly is a major influence. The interaction between temperature and precipitation has the greatest effect on a region’s rate of weathering and acids are common agents is the chemical reaction of weathering rates are highest in cool, areas where water undergoes repeated and oxygen with other substances Carbon Dioxide combines with water in the atmosphere to form the surface as precipitation that falls to Carbonic acid reacts with minerals such as calcite in limestone and marble to weathering rates are highest in areas with warm temperatures and abundant and heavy vegetation and composition also affects the weathering rate. Some are quite resilient (Quartz) while some are easily broken down (Talc) interacts with both mechanical and physical weathering as pieces break up through mechanical weathering more surface area is for chemical weathering is the shape and slope of the Earth’s surface. Materials that lie on steep slopes are more likely to move and expose even more surface area (acid rain) is another agent of chemical weathering caused by the oxidation of sulfur dioxide and nitrogen oxides released into the atmosphere by human activities These gasses combine with water and oxygen in the atmosphere to form . and nitric 6