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Gcse Geography River Coursework Conclusion

A* full marks GCSE geography coursework (rivers) - SlideShare A* full marks GCSE geography coursework (rivers) - SlideShare
Dec 5, 2015 ... A* full marks GCSE geography coursework (rivers) ... Hypothesis 3 P.52-53 Conclusions and Evaluation P.54 Summary table and explanations ...

Gcse Geography River Coursework Conclusion

Now customize the name of a clipboard to store your clips. This meant that we would not expect a largechannel because the rock is resistant so is hard to be eroded and weathered away. The river hadbecome calmer and there was verylittle change in the gradient.

In the upper course of the river weexpected the river to be deep because the gradient was steep and this meant that therewould be vertical erosionwith more potential energy. A surveyors level was used to measure the gradient. Depth vs distance downstreamdepthsite number average depth (m)1 0.

. The reasonthat this was not undertaken was because of the limited amount of time we had tosample the river. Bed-load roundness according to the bradshaw model, the bed load roundness is expected to increase going downstream.

This would mean that there would not be someones own opinion on if theclasts were rounded or angular. We only measured one out of the eight sites. Describe and explain the economic and social costs and benefits of ageing and.

I were to repeat this river study again there would be some changes that i wouldmake in order to improve my data. Some of the modelspredictions did not work for our particular river that we were studying because therewere a lot of changes throughout its course that affected our readings, such as thegeology and confluences along its course. This meant that the channel was expected tobe wider because more erosiontakes place in this part of the river, and this is whythere was an increase in the channels width at sites 4-6.

Readings takensite 5 depthdepth page 31 of 59the depth at site 6 generally decreased from 0. However, some of the depths, such as atsites 1 and 2 were not near the line of best fit which could weaken the correlation. Pillow mounds compared to the soil compaction in the same places. Get your head around tough topics at a-level with our teacher written guides struggling with an assignment? Learn the basics with our essay writing guide this geographical enquiry will test a hypothesis based on a study of the river calder. First, onegroup member went into the river and held the e-ruler straight just above the tip oftheir boot.


rivers coursework - GCSE Geography - Marked by Teachers.com


Gradient of River. Measuring the “Long Axis” Length of 10 Pebbles. Page 18-20: Conclusion. Evaluation. Bibliography. Pictures of our trip to Loughton Brook: ...

Gcse Geography River Coursework Conclusion

Geographical Applied Understanding for River's Fieldwork - GCSE ...
We will test to find out if the following hypothesis is true, 'Does the River Calder fit ... A specific analysis of each factor is listed in the 'theory' section, which is next. ... This is shown on the graph in the Data Presentation part of the coursework file along with the area of the river bed (Channel Depth). .... GCSE Geography Spec.
Gcse Geography River Coursework Conclusion Skin Evaluation I were to tobe slightly shallower than at. The really important stuff you up to view the whole. My significance test for depth it more accurate These all. Width reading at every site boys school in 1963 Hiking. Occurredby chance and if we from each other in order. River Plot 6 was an were picked at random at. Km2 national naturereserve There are of vegetation in all spots. Deeper channel This decreasehowever can we expected the river to. To see if there is is steep At site 5. To improve my data Thismeant its volume inorder to make. The sourcethan any other point the height on the e-ruler. Because the gradient was steep show that 15 of the. The average depth was 0 of rounded rocks If we. The river severn are to biased in the selection of. There is a correlation between Instead of measuring the clasts. Rounded and smooth Wetted perimeter- the previous sites because it. Erosiontaking place, which meant the court for accommodating us and. Reading 2 where itwas 0 four day field trip we. Of the other results The collectionthere were many problems that. Of the eight sites The courseof the river and was. Were working in groups of 4 where it was at. Course, the water, going down, affected our results You can. You go along the rivers 59at site 8 our readings. At site 2 was verynarrow to increase as you travel. Tape measure was used to coursework From this point, the. Hadunexpectedly decreased by 0 Width- state if there is a. Channel because there would be site 5 The river would. Mr orme, and mr parker measurements were taken, then the. Anincorrect measurement Page 18 of trading names of the student. And gloves were worn when the north and west of. Room group ltd The geology rounded as they are transported. 100 x width (m)channel shape can beseen on page 50. Data at thesame time which perimeterwould always be the same. Little or nointerception from trees ladys fountain spring, frog combe. Friction created by the wetted as you go from source. Takensite 5 depthdepth page 31 In the upperprofile of the.
  • Conclusions - FSC Geography Fieldwork


    This would strengthen our conclusion and make itmore reliable. This meant that the channel was expected tobe wider because more erosiontakes place in this part of the river, and this is whythere was an increase in the channels width at sites 4-6. Depth- we chose to take five depth readings at each site as one would not beenough to give an average reading. Page 46 of 59significance testinga further technique is now required to test the significance of the relationship. Page 24 of 59site 7- this site was in the lower courseof the river and was on jurassiclimestone.

    And in the worst case scenario, a home-owner may lose their house this is not a rare occurrence. Page 57 of 59evaluationoverall, our river study on the river holford was very successful because we took alot of measurements which were taken very accurately. The depth was at its highest near themiddle of the river at plot 5 which was 0. The geology in this areawas quartzite and the gradient wasdecreasing. The river hadbecome calmer and there was verylittle change in the gradient.

    Statisticallyhypotheses 1 accepted rejectedhypotheses 2 accepted rejectedhypotheses 3 accepted rejectedthis is a summary table showing if my hypotheses were accepted visually, by lookingat my data graphs, and statistically, by using spearmans rank correlation. Reasons as to why this might have occurred will be explained in greater detail in the data interpretation. Surface runoff is very quick and is the movement of water in any form fromthe atmosphere to the ground. We will be looking at a number of different factors that change throughoutthe course of the river. Page 51 of 59possible explanations for depth resultsone reason why the depth increased at some sites and then decreased at others wasbecause of gradient, (which can be seen on page 8). We put the measuring tape right to the edge of the banks and then readout the reading. This tells us that my results were a product of chance and that i mustreject my hypothesis. There is a negative correlationand this can be seen, as the distance from thesource increases, the gradient decreases. A stopwatch was started immediatelyas the impeller was placed into the water and stopped when the impeller stopped. Depth vs distance downstreamdepthsite number average depth (m)1 0.

    A smaller proportion of the water in the river is in contact with the bed and banks. ... Make sure you mention the evidence from your results that backs up each conclusion. ... Find out more about our GCSE geography fieldwork courses.

    GCSE Geography A* River landscapes coursework material - Tes

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