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Weathering Processes that break down rocks, producing material that may eventually become sediment Chemical Weathering Involves chemical reactions that result in the formation of new materials (e.g. new minerals or ions carried off in solution. Baraboo quartzite, Wisconsin - note weathering rind Hydration of feldspars --> clays Modern soil developed on basalt, Oregon - Bruce Railsback http://www.gly.uga.edu/railsback/FieldImages/OregonModernSoil.jpeg Monument Valley, AZ - oxidation produces hematite Detail of artwork Detail of date Slate gravestone - Amherst, MA - note lack of weathering Slate stone - 1820 Marble stone - 1844 Note dissolution of calcite Marble stone - Amherst, MA - consists largely of calcite Differential weathering - lighter minerals more resistant Mechanical Weathering Breaks rocks down into smaller pieces, but without changing the mineralogy Lamphier Lake, Colorado - note talus slopes Frost wedging Water expands on freezing; liquid water gets into cracks in rocks, then freezes and expands - enlarging the crack & eventually breaking off pieces of the rock ☜ ☟ Water seeping into porous sandstone freezes - causing frost wedging and spalling off of parts of the surface Frost wedging and gravity produce talus slopes in mountainous areas Salt crystallization I-80 Bonneville salt flats, UT Salty water is drawn upward in these fenceposts by capillary action; crystallization of salt when the water evaporates splits the posts! (similar to frost wedging) The Old Man in the Mountain Exfoliation: Cannon Mountain, NH