• Join over 1.2 million students every month
  • Accelerate your learning by 29%
  • Unlimited access from just £6.99 per month

GCSE Geography Coursework: Strand 3 - Data Presentation

Extracts from this document...

Introduction

This is the Data Presentation part of the coursework folder. The results are presented in the form of graphs and annotations are used to explain them. The results were derived from the geographical investigation conducted on the River Calder; June 10th 2008. (1) The relation between the Channel With and Depth: According to the Bradshaw Model, the Channel width and depth are expected to increase moving downstream from the source. Theory as to why this happens is explained in the Applied Understanding section of the coursework folder: points 1 and 2. I have used a scatter-diagram in-order to compare both continuous variables against two factors. ...read more.

Middle

Reasons as to why the Velocity and Discharge decrease greatly between site 1 and 2 are probed into in the Data Interpretation section of the coursework folder. (3) Bed-load roundness: According to the Bradshaw Model, the bed load roundness is expected to increase going downstream. Theory as to why this happens is explained in the Applied Understanding section of the coursework folder: point 7. I have used pie-charts in order to easily compare and contrast the proportion of different rock types at the five different sites. Site one (4-Km from source): Site two (5.2-Km from source): Site three (8.3-Km from source): Site four (11.4-Km from source): Site five (14.3-Km from source): (4) ...read more.

Conclusion

(5) Comparison of the Bed-load size at the five different sites: According to the Bradshaw Model, the Bed-load size is expected to decline going downstream. Theory as to why this happens is explained in the Applied Understanding section of the coursework folder: point 6. I have used a scatter-graph to clearly compare the b-axis size of different rocks to their site. A reason as to why the bed-load size generally increases is explained in the Applied Understand. Reasons as to why the rocks at site 2 fluctuate greatly, some surpassing site 1's, is probed into in the Data Interpretation section of the coursework folder. ?? ?? ?? ?? Riyadh Abdulla Data Presentation Instructor: Mr Walker Candidate Number: - 4185 AQA GCSE Geography Spec. B Page 1 ...read more.

The above preview is unformatted text

This student written piece of work is one of many that can be found in our GCSE Physical Geography section.

Found what you're looking for?

  • Start learning 29% faster today
  • 150,000+ documents available
  • Just £6.99 a month

Not the one? Search for your essay title...
  • Join over 1.2 million students every month
  • Accelerate your learning by 29%
  • Unlimited access from just £6.99 per month

See related essaysSee related essays

Related GCSE Physical Geography essays

  1. Marked by a teacher

    River Chess Coursework

    4 star(s)

    Channel roughness - the rougher the channel the slower the water flows i.e. if there's big boulders in the river, the water will have to go round them, slowing the flow. If however, it was a smooth channel i.e. no boulders or obstructions, the river will flow quite faster.

  2. rivers coursework

    Diagram of tree Pollarding Hypothesis: 1. The Depth of the river will increase as you go downstream. To carry the extra flow of water volume from the tributaries the river depth must increase. Also upland, gravity forces the bedload of rocks to sever into the ground increasing the river depth.

  1. Hunstanton coursework

    Figure 1 Figure 2 Figure 1 is the model of a typical seaside resort and figure2 is the model of Hunstanton. As you can see they are similar in many ways Residential area is away from the sea in both figures because it's cheaper to buy there and the hotels, parks and entertainments are near the sea.

  2. Geography Coursework - Data Interpretation

    Finally, Pillow Mounds is directly across from a pub, a restaurant and a shop as well as the visitors centre. These attractions will mean that people will not want to move away from the area and will stay in Pillow Mounds.

  1. Swanage Geography Coursework

    and graphs about some of the relevant information on Swanage like population, Employment Rate, Age Structure etc. From these results it should give me a clear indication about Swanage and its history. Population of Swanage In Figure 2.1 it shows both the statistics and the graph of the Population of

  2. Debden Brook Rivers Coursework Data Collection Table

    Like all of the other measurements the results were recorded as quickly as possible. The difference between measuring the width of river and measuring the wetted perimeter of the river was that, when measuring the wetted perimeter we instead measured from where the river met the bank and not from where the bank met the river.

  1. Morpeth Coursework

    Morpeth is set out like a Burgess Model. Here is a diagram and an explanation of a Burgess Model. Burgess Model: Explanation: a) Central Business District: This zone is most assessable to the most amounts of people. It contains shops, offices, banks and doctors. It is high congestion and little vegetated areas.

  2. Lulworth Cove Coursework

    roughly tell us how many people have come to see Lulworth on that particular day. I made a tally chart of all the cars that were in Lulworth car park and assuming there was 3 people per car on average I then worked out the average number of people.

  • Over 160,000 pieces
    of student written work
  • Annotated by
    experienced teachers
  • Ideas and feedback to
    improve your own work