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WEATHERING BY MS. HOUSTON ARMS 6 TH GRADE EARTH SCIENCE.

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Presentation on theme: "WEATHERING BY MS. HOUSTON ARMS 6 TH GRADE EARTH SCIENCE."— Presentation transcript:

1 WEATHERING BY MS. HOUSTON ARMS 6 TH GRADE EARTH SCIENCE

2 Weathering  Natural process that breaks down rock into sediment (sand, silt, clay)  Begins the process of forming soil from rock and sediment.  Affects sediment particle size and soil texture.

3 Mechanical Weathering Burrowing Animals Ice Wedging Plant Roots Wind Water Physical process that breaks down rock but does not change the composition of rock.

4 Mechanical Weathering  Ice wedging is the process that occurs when water freezes, expands and thaws in the cracks of a rock  Overtime the cracks will get wider and deeper and the rock will break  Plant growth causes rock to break by roots exerting pressure on the rock  Plant roots can seek their way into rock cracks and continue to grow creating pressure in the cracks of rock.

5 Mechanical Weathering  Burrowing animals dig tunnels in the ground loosening small rocks and sediment and eventually pushing them to the surface  Wind carries other sediment and potentially beat on the surface of other rock loosening or breaking other rock  Water can exert pressure on sediment and small rock thereby further breaking the rock.

6 Chemical Weathering  Chemical process that breaks down rock by chemical reactions that dissolve minerals or change them into different minerals.  Rock composition will change!  Carbonic acid  Natural plant acids  Oxidation  Acid rain

7 Chemical Weathering- Natural Acids  Carbonic acid forms when water reacts w/ carbon dioxide gas in the air.  Carbonic acid is a weak acid that can dissolve some minerals found in rock.  Carbonic acid dissolves calcite a mineral found in limestone  Ex: cave formation  Other natural acids can dissolve the mineral feldspar which is found in granite, some types of sandstone and other rocks.  Kaolinite is a clay mineral found in some soil and is formed from dissolved (broken down) feldspar.

8 Chemical Weathering- Plant Acids and Oxidation  Plant roots give off acids  These acids can dissolve some minerals found in rock making the rock weak and causing the rock to break into smaller pieces  Oxidation occurs when oxygen gas and moisture react with certain materials to form a new material  This new material looks like rust.  Oxidation of minerals gives some rock a red or rust color

9 Effects of Climate and Rock Type  Climate affects the rate (how fast) weathering occurs  Cold, polar climates increases MECHANCAL weathering  Warm, wet climates increases CHEMICAL weathering  Desert climate slows CHEMICAL weathering  Cold, polar climates slows CHEMICAL weathering

10 For Additional Information: See the Glencoe textbook. You may access the textbook online via the ARMS website. Click on Academics Click on Science Information Click on Online Textbook and look for the 6 th Grade textbook. Highlight and copy the code Click on the 6 th grade textbook and paste t he code the click submit. If you can not access the book, make sure that you have the latest version of Adobe reader then repeat the steps


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