Geography Coursework On Rivers

Geography Coursework On Rivers-21
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.

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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!

The material on this section of the site is based mainly around AQA Syllabus A.

Basically I literally write the same thing over and over and over again for all 5 strands.

It will be published in pdf format, and encrypted to prevent unauthorised copying and printing.

Geography Coursework On Rivers

Data including text and images should be sent by email to: Word documents and images in jpg or gif format can be uploaded directly to this site by clicking here.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.Your coursework will be credited to you and will remain your intellectual property.It cannot be copied or used in any way without your express written permission.This anomaly is due to the abstraction of water from the Calder Intake to the Barnacre and Grizedale Lea reservoirs, grid-reference 5448.A reduce in water will make the channel width narrower.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.This is because less (lateral) erosion will occur, in-order to deepen the channel.From sites 3 to 5, the channel gradually re-widens; rising significantly from 2.7m to 6.7m.

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