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SOILS, WEATHERING, AND EROSION Where the geosphere and the biosphere meet Learning Targets 1. Define mechanical and chemical weathering 2. Discuss agents of weathering 3. Give examples of each type of weathering Soil Forming Processes 1. Weathering: process that changes solid rock into sediments 2. Erosion: process that moves sediments 3. Sedimentation: depositing of rock pieces Weathering Erosion Sedimentation Weathering 1. Large rocks and mountains sediment 2. Sediment sizes a) b) c) d) e) Boulders Gravel Sand Silt Clay 3. What processes act on weathered sediments? a) Erosion (movement) b) Sedimentation (deposition) Weathering 1. Weathering only happens at the surface 2. Occurs in 2 forms: a) Mechanical: change in shape or size Also known as physical weathering b) Chemical: change in composition Mechanical Weathering (Physical Weathering) Chemical weathering Mechanical Weathering (Physical Weathering) 1. 3 main types: a) Ice wedging Cycles of freezing and thawing b) Abrasion Physical contact and friction c) Biological weathering Roots, burrowing animals, fungi, lichens, humans Ice wedging Abrasion Biological weathering Mechanical Weathering 1. Increases surface area 2. Increased surface area leads to quicker weathering. Why? a) More rock is exposed to the atmosphere; less rock is protected from water and oxygen Increasing surface area Chemical weathering 1. Creates new minerals or compounds a) Different composition not just different size 2. Different minerals are stable at surface than at depth 3. Mainly caused by a) Water: dissolves minerals b) Oxygen: combines to form oxides c) Carbon Dioxide: makes water acidic Oxidation Hydrated obsidian Oxidized ultramafic rock Rust: chemical weathering of Iron Chemical Weathering 1. Some organisms release chemicals that break down rocks and minerals 2. Fungi and bacteria are very important parts of chemical weathering Lichens colonizing a lava flow Differential weathering 1. Weather rates speed up based on a) Rock and Mineral Type Sedimentary rocks weather fastest b) Climate type Temperature increases: Chemical reactions more rapid Precipitation increases: More water allows more chemical reactions