Get Cambridge International AS and A Level Geography: Revision PDF

By Garrett Nagle

Get your most sensible grades with this Cambridge foreign AS and a degree Geography Revision advisor. - deal with your individual revision with step by step help from skilled examiners Garrett Nagle and Paul Guinness - Use particular case stories to enhance your wisdom of geographical styles, tactics and adjustments - Get the head marks through utilising geographical phrases safely with assistance from definitions and key phrases Use the Revision consultant to arrange for the large day: - Plan and velocity your revision with the revision planner - Use the professional the way to make clear key issues - steer clear of making regular error with specialist recommendation - try your self with end-of-topic questions and solutions and tick off each one subject as you whole it - preparation your examination talents with exam-style AS and A2 questionsThe Revision advisor additionally has: - assurance of the total syllabus, together with all eight innovations - a world concentration, together with examples and case reports from world wide. additionally to be had: Cambridge overseas A and AS point Geography textbook (ISBN: 9781444123166) by way of Garrett Nagle and Paul Guinness and counseled through collage of Cambridge overseas Examinations. This name has no longer been in the course of the Cambridge endorsement technique.

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Extra resources for Cambridge International AS and A Level Geography: Revision Guide

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3). But it is very difficult to isolate the exact relationship, at any scale, between climate type and rate of process. 4). l The efficiency of freeze–thaw, salt crystallisation and insolation weathering is influenced by critical temperature changes, frequency of cycles, and diurnal and seasonal variations in temperature. 4 Peltier’s diagram, showing variations of chemical and mechanical weathering with climate Geology In general, frost shattering increases as the number of freeze–thaw cycles increases rather than according to average temperatures.

These are caused by the solution of limestone but can also be formed by the enlargement of a grike system, by carbonation or fluvial activity, or by the collapse of a cavern. Rivers can disappear into these holes, hence the term ‘sink’. Resurgent streams arise when the limestone is underlain by an impermeable rock, such as clay. Stalactites develop from the top of the cave, whereas stalagmites are formed on the base of the cave. 16 What are the two main theories about tor formation? 17 What is equifinality?

Where a trench occurs off continental margins, the turbidites (sediments) from the slope are trapped, forming a hadal plain on the floor of the trench. Now test yourself 4 What processes happen at (a) a mid-ocean ridge and (b) a subduction zone? 5 With which types of plate boundary is volcanic activity associated? 214 Tested Expert tip Mountain building is often associated with crustal thickening, deformation and volcanic activity, although in the case of the Himalayas, volcanic activity is relatively unimportant.

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