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Weathering

Weathering. Erosion, Rivers and Glaciers. Weathering. The breakup of rock due to exposure to the atmosphere Can be Physical/Mechanical or Chemical. I. Physical/Mechanical Weathering. When rocks are split or broken into smaller pieces of the same material without changing the composition

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Weathering

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  1. Weathering Erosion, Rivers and Glaciers

  2. Weathering • The breakup of rock due to exposure to the atmosphere • Can be Physical/Mechanical or Chemical

  3. I. Physical/Mechanical Weathering • When rocks are split or broken into smaller pieces of the same material without changing the composition • EXAMPLES: • Ice/frost wedging causes potholes • Root wedging lifts up sidewalks • Wetting and drying

  4. Ice/Frost Wedging

  5. Root Wedging

  6. II. Chemical Weathering • Decomposition of rock that takes place when the rock’s minerals are changed into new substances • EXAMPLES: • Hydrolysis is the chemical reaction of water with rocks • Oxidation is the reaction of oxygen and other substances: causes rusting • Carbonic Acid: dissolved carbon dioxide in water, changes minerals into clay minerals

  7. III. Acid Precipitation • Rain, snow, or sleet mixes with sulfuric and/or nitrogen compounds in pollution • Results in sulfuric and/or carbonic acid • Natural rain has a pH of about 5.7 due to natural CO2 in the atmosphere • Acid rain has a pH of between 4 and 5

  8. III. Acid Precipitation Cleopatra’s Needle, Central Park NYC

  9. Do Now: • What is it called when oxygen reacts with elements of rocks? • What is carbonic acid? • Obj: LWBAT continue your understanding of the processes of weathering.

  10. IV. Erosion • The removal and transportation of weathered materials by running water/waves, wind and ice (glaciers) • Carries and deposits sediment • Can form structures such as deltas, fins, and sandstone arches

  11. IV. Erosion Sandstone Arches, Arches National Park, UT Sandstone Fins, Arches National Park, UT

  12. V. Rate of Weathering • Weathering is affected by: • Amount of rock exposed at the surface • Type of rock • Igneous & Metamorphic – more resistant • Sedimentary – least resistant • Climate • Hot/Cold and dry – more physical weathering • Warm and moist – more chemical weathering

  13. VI. RIVERS • Running water • Comes from water cycle (precipitation to runoff) • Moves downhill from force of gravity • Breaking down of sediment and rock • Mechanical • Abrasion – rubbing of rocks against stream bed • Chemical • Rain and spring melt lowers pH of lakes – “Acid Shock” • Can be neutralized by dissolving soluble carbonate rocks (ex. Limestone)

  14. VI. RIVERS (con’t) • Erosion – water carries rock and sediment downstream • Solution – minerals dissolved in water • Suspension – small particles carried in water flow (“muddy water”) • Bed load – boulders and pebbles pushed along bottom of stream • Delta – fan shaped deposit of silt and sand at end of river

  15. Deltaand not the force

  16. VI. RIVERS (con’t) • Carrying Power • Amount of sediment and size of particles • Depends on speed and discharge • Increases as speed and discharge increase • Discharge – volume of water flowing past a certain point • Speed of stream • Depends on steepness of stream bed • Steeper = faster • “Graded River” – even/consistent slope

  17. E. Stages of Stream Development • Youth Stage • Steep V-shaped valley • Lowest discharge • Greatest speed

  18. E. Stages of Stream Development • Mature Stage • Wide valley • Erosion of valley walls • Floodplain developing

  19. E. Stages of Stream Development • Old-age Stage • Valley walls completely eroded • Large flat floodplain • Meanders and oxbow lakes • Maximum discharge floodplain Oxbow lake Meanders Tributary streams

  20. Colorado River, Grand Canyon, AZ

  21. F. Watersheds • Watershed – the entire land area drained by a river and its tributaries • Largest watershed in the US is the Mississippi

  22. VII. Glaciers • 2 types: • Valley aka Alpine Glacier • Long, slow-moving wedge-shaped stream of ice • Continental Glacier • Large sheets of ice covering a large part of a continent Ice Sheet on Ellesmere Island, Canada

  23. VII. Glaciers • Largest Glaciers • Antarctica • Continental Glacier • Last ice age • ~18,000 years ago • Ice covered Great Lakes and reached to IN, OH and NJ • Sea levels drop Great Lakes NJ

  24. C. Glacial Features Firn – granular snow atop a glacier Crevasses – deep cracks in the ice Snow line – lowest level of snow in summer Ice front – edge of a glacier **glaciers carve U-Shaped valleys**

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