WEATHERING TURNING ROCKS INTO SOIL Two types of Weathering A. Mechanical: physical breakdown of rock into smaller pieces 4 WAYS: 1.
Download ReportTranscript WEATHERING TURNING ROCKS INTO SOIL Two types of Weathering A. Mechanical: physical breakdown of rock into smaller pieces 4 WAYS: 1.
WEATHERING TURNING ROCKS INTO SOIL Two types of Weathering A. Mechanical: physical breakdown of rock into smaller pieces 4 WAYS: 1. Exfoliation: repeated heating/cooling – top layers of rock peels away 2. Frost Action: water seeps into cracks, freezes, expands – crack widens (ice wedging) 3. Organic Activity: plants & animals A. burrowing: digging exposes rock B. root pry: roots widen cracks in rocks 4. Abrasion: rocks hit each other – causing them to break (wind, running water, gravity) What happened here? Another type of weathering: Video Clip B. Chemical: a change in rock composition Happens in 5 ways: 1. Hydrolysis: rocks react with water 2. Carbonation: Carbon dioxide + water = carbonic acid (limestone caverns) 3. Oxidation: oxygen reacts with metallic elements (iron & oxygen = rust) 4. Sulfuric Acid: pollution/acid rain corrodes rock 5. Plant Acids: seep into rock & dissolve minerals (Lichen seen in video clip) Rates of Weathering Depends on: A. Composition of rock: - Sedimentary rock weather faster than igneous/metamorphic -Minerals present in rock: * quartz: very hard mineral – weather’s slowly * calcite: chemical weathering by carbonation B. Amount of exposure: -More surface area – increased rate of weathering -Less surface area – slower rate of weathering C. Climate: - lots of rain - hydrolysis - freezing climate – frost action/ice wedging Weathering and SOIL SOIL TYPES 1. Bedrock Solid rock at Bottom – “parent rock” 2. Soil Mix of minerals, water, gases, dead stuff Various layer within 3. Humus Dark organic matter of decaying stuff SOIL TEXTURES GRAVEL SANDY SILTY CLAY Based on particle sizes present in sample The spaces between the particles is called PORE SPACE What type of soil do YOU see? Gravel Silt Clay Sand Using the textbook at your desk, complete the following: Beginning at pg. 432 read each section and complete the section reviews for each section. The section reviews can be found on pages: 440, 442 and 446. On Pg. 450: do #’s 1-9 MC; 1-8 T/F and the Concept Map