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Degree: Physical Geography (Masters) - Durham University
I am a Physical Geography student at Durham University. I have always had a passion for this subject, and love how versatile it is for teaching skills in a variety of subjects. Hopefully I will be able to instill this in you as well!
I have tutored at my school and have been lucky enough to volunteer as a Scout leader for some years where teaching and working with children of all ages has been key. This has allowed me to gain a lot of experience and hopefully make my tutoring style fun and informative.
These will be guided by you. We can focus on improving knowledge and understanding, developing techniques for answering questions and analytical skills, as well as anything else you want to work on or that I feel would really benefit you.
This will be done in as many ways as possible, from diagrams and examples, to discussing ideas and debating the key concepts. This is especially key for Geography, but has applications in science as well.
German tuition can be done entirely in German. I will be looking to stretch and improve your writing and vocabulary, as well as provide a medium for conversation and proof reading.
Additionally I can help you with your UCAS application and CV’s, as well as any other applications and forms you need.
Ultimately my aim in the sessions is to inspire you to be a better student of your subjects and of life, and to develop passion and enjoyment in learning.
To find out more…
Please contact me via “Webmail” or book a “Meet the Tutor Session”
I look forward to meeting you!
|Geography||A Level||£20 /hr|
|German||A Level||£20 /hr|
Ann (Student) January 17 2017
Mona (Parent) January 17 2017
Ann (Student) November 29 2016
Ann (Student) November 17 2016
This question is a 10 marker and comes at the end of the 25 mark section on Plate Tectonics.
When answering a Discuss question it is important to remeber that it is in essence a mini essay, however, it is shorter, approximately 2-3 pages. This may seem daunting for a 10 marker but hopefully over time you will realise that it is actually a challenge to keep the answer short.
This introuction requires the student to state that this theory has been worked on as early as 1620 by Francis Bacon, and that it is constantly evolving and that new evidence is constantly being found. This furthers eplanations of various tectonic and volcanic processess.
1912 Alfred Wegener. Super continet (called Pangea). Evidence includes
continental fit (e.g. South America and Africa-This is particuarly the case if continental shelfs (often below the suface of the sea) are matched together)
Geological evidence-same rock types, same formations found only in Africa and SA.
Similar glacial depostis in Antarctica, SA, and India.
Mountain types and compostion same in eastern USA and NW Europe.
Climatological evidence-Antarctica, N America, Svarlbard, UK all contain coal depostis of similar age formed in tropical conditions, therefore continets must have drifted apart since the carboniferous period.
Biological evidence-same fossils on eithe side of Atlantic. e.g. Mesosaurus only in southern Africa and in SA. More specifically found in sediments from permian age, 280 million years ago.
plant remains in India and Antarctica identical. Obviously different climates now, so must have once been joined and sharing same climate.
Seperate evidence found from paleomagnetism.
This expands on Wegener's theory's by explaining how continents could move over a solid earth.
1948 survey of Atlantic ocean floor revealed Mid Atlantic Ridge (MAR). 1000 km wide, heights of up to 2.5 km. volcanic rocks. Similar range found in pacific later, extending over 5000 km.
Later surveys showed paleomagnetic stiping to either side of MAR.
Volcanic rocks/lava, is rich in iron. This iron becomes aligned with magnetic field of earth. Every 400,000 years polarity of earth changes. This is mirrored by bands of rock in normal and reverse polarity orrientation being found either side of the MAR going spreading outwards.
Lots of fieldwork on Iceland (sits and is being created currently by the MAR) gives us further evidence.
Subduction of crust in other areas shows us that tectonic plates are moving.
So far the evidence has just been listed. However, it is necessary to discuss this. The stundent needs to discuss what conutations this evidence has on us. For example, it allows us to trace plate boundaris and so where there are potentially hazardous tectonic areas-earthquakes, volcanoes, tsunamis. etc.
In essence more than just basic fact listing is needed. Some flare is required as long as the essay remains logical and concise.see more