Geography Coursework On Rivers

There is an increase in the velocity between sites 2 and 3 because some of the water initially abstracted is pumped back into the river; additional water is also added as the river starts to meet its tributaries downstream. At site 4 we measured inside the inner-bend of the meander; which flows faster than the outer-bend. I'm in my A2 Year of Geography and your're using terms that I used in AS! Did you have to go on your own, if you wanted to do your own 'original research'?This increase continues until site 5, where the speed, from sites 4 to 5, decreases by 0.7 m/sec. This anomaly can be caused by the confluence of the River Calder and the River Wyre, 300 metres from the A6 Catterall playing fields, at an angle. you have included all the relevent info without waffling on and you have stats to show x y z... oh yeah of course you can get full marks, the place we went to visit was so far away from everyone that it was impossible to go there again, that was the annoying bit, but yeah thats what the teacher said also because she told us what measurements to take... lol For fun (im in year 11) we went with the year 10 geographers to the river they are studying (no idea what its called put its in the peak district).Please give your full name and school address, together with your study title.

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Data collected in the field provides an invaluable contemporary and historical resource that can form the basis and inspiration for further studies.

Assist future students and at the same time enhance your University entrance application and Curriculum Vitae by publishing the data from your Barcelona geography fieldwork on this site.

It is so boring; there is nothing new to say about the stupid river which I investigated.

Just a little rant - I am starting to think that I won't do well on my coursework for Geography; for example, most of it talks about one thing constantly!

According to the Bradshaw Model, the channel width is expected to increase moving downstream from the source.

Site Width in meters Site 1 6.1 Site 2 2.7 Site 3 5.8 Site 4 5.9 Site 5 6.7 There is an abnormal decrease of 3.4m in the channel width between sites 2 and 3; approximately 7KM from source.This area has been developed to assist students completing GCSE Geography Coursework Projects.It does not and will never replace the expertise of your Geography teacher.This increase happens, especially from site 4 to 5, because River Calder’s 34 tributaries are constantly adding water back to the river; thence increasing erosive processes, mainly hydraulic action and abrasion, widening the channel.This can be linked to show an overall increase of the Discharge.' by Jung Hoon Lee and Mitzi Laszlo van Harreveld, Kensington School, GCSE Geography Edexcel Syllabus A) can be found in the menu to the left. A Level coursework examples include 'Has the Universal Forum of Cultures improved the quality of life in La Mina, Barcelona? ' by Ross Jones and 'How and why does the quality of life differ between the Diagonal Mar and La Mina districts of Barcelona? Site Velocity (m/sec) Site 1 0.67 Site 2 0.04 Site 3 0.11 Site 4 0.26 Site 5 0.19 However, this significant decrease in velocity between the two sites is caused by the abstraction of water between the two sites from the Calder Intake at to the Barnacre and Grizedale Lea reservoirs at grid-reference 5488.This makes the Channel Width narrower and the flow of water shallower.You should also be aware that some variations exist between exam boards as to the way in which geographical enquiry is undertaken.You should always follow the guidelines offered by your teachers.

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