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rivers coursework
Member rating: No Rating | Words: 3000 | Submitted: Wed Jan 30 2008
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Contents Page 1: Aim Hydrological Cycle Page 3: Coppicing Pollarding Page 4: Hypothesis Location Page 5: Geology Epping Forest Page 5-8: Maps Page 9-12: Method Measuring the Width of the River Measuring the Depth of the River Measuring the Velocity of the River Measuring the River Channel Gradient Measuring the Pebble Size Equipment List Page 13-18: Data Presentation Water Width Water Depth Float Times of Cork Gradient of River Measuring the "Long Axis" Length of 10 Pebbles Page 18-20: Conclusion Evaluation Bibliography Pictures of our trip to Loughton Brook: Page 20 and over How does a river (Loughton brook) change with distance downstream? Aim: To investigate how a river (Loughton brook) changes with distance as you go downstream. Hydrological Cycle: • Sea water is heated by the sun which evaporates it and produces water vapour. • Then there are cloud formation and sea breezes blow clouds inland. • Clouds cool when rising over high mountains and lands. • Then...
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