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Inside the Commons - Episode 4Saturday, 28th February 2015 21:15 - BBC Two Scotland onlyIn the final part of Inside the Commons, battles break out over the future of the House. Read more: OU on the BBC: Inside the Commons - Episode 4
Wartime Farm Episode 1Sunday, 1st March 2015 08:00 - Yesterday
Wartime Farm Episode 2Sunday, 1st March 2015 08:30 - Yesterday
Thinking Allowed: Migration to London and South AfricaMonday, 2nd March 2015 00:15 - BBC Radio 4
BBC Inside Science - Trends in forensicsAvailable until Tuesday, 24th March 2015 14:30BBC Inside Science asks where the future of forensics lies this week. Read more: OU on the BBC: BBC Inside Science - Trends in forensics
Blackhat, dark night: Could hackers really cause a power outage?Although the nuclear meltdown depicted in Blackhat is fiction, Mike Richards warns there are... Read more: Blackhat, dark night: Could hackers really cause a power outage?
OU on the BBC: Inside the CommonsThis major four-part series from inside the House Of Commons gives viewers unparalleled access to... Read more: OU on the BBC: Inside the Commons
Succeed with maths – Part 1 [TEST]DO NOT ATTEMPT TO COMPLETE THIS COURSE. IT IS ENTIRELY FOR OPENLEARN TESTING PURPOSES. Try: Succeed with maths – Part 1 [TEST] now
Succeed with maths – Part 1[BETA] If you feel that maths is a mystery that you want to unravel then this short 8-week course... Try: Succeed with maths – Part 1 now
Plate tectonics is an earth sciences topic that attracts a good deal of interest, given...
Plate tectonics is an earth sciences topic that attracts a good deal of interest, given that it a topic very often featured in popular science programmes on TV and radio. It is a subject that have strong visual appeal. The coverage is self-contained, up to date and is written in a way that will be accessible to those with interest and motivation, all the more so for those who have some pre-existing scientific understanding.
After studying this unit you should be able to demonstrate a knowledge and understanding of:
- the theory of tectonic plates and the different forms of evidence (e.g. palaeontology, palaeomagnetism, continuity of structures etc.) that can be used to understand the movement of the lithospheric plates over geological time;
- the mechanisms of crustal growth and transfer of heat at spreading ocean ridges;
- the three main types of plate boundary (constructive, destructive and conservative) and how they interact at triple junctions;
- the difference between relative and true plate motion;
- the driving and retarding forces that influence plate motion at constructive, destructive and conservative plate boundaries.
- Current section: Introduction
- Learning outcomes
- 1 Preamble: the moving Earth
- 2 From continental drift to plate tectonics
- 2.1 Continental drift
- 2.2 Evidence for continental drift
- 2.3 Sea-floor spreading
- 3 The theory of plate tectonics
- 3.1 Assumptions
- 3.2 Heat flow within plates
- 3.3 Constructive plate boundaries
- 3.4 Destructive plate boundaries
- 3.5 Destructive plate boundaries, continued: ocean-ocean (island-arc) subduction
- 3.6 Destructive plate boundaries, continued: ocean-continent (Andean type) subduction
- 3.7 Destructive plate boundaries, continued: continent-continent destructive boundaries
- 3.8 Conservative plate boundaries and transform faults
- 3.9 Triple junctions
- 4 Plate tectonic motion
- 5 Plate driving forces
- 5.1 Why do plates move?
- 5.2 Forces acting upon lithospheric plates
- 5.6 Implications of plate tectonics
- 5.7 Summary
- 5.8 Further reading
In this unit, you will examine how the evidence for the movement of continents was gathered and how this movement relates to, and generates, geological features and phenomena such as ocean basins, mountain ranges, volcanoes and earthquakes. You will learn how and why the continents have moved, and continue to move, and the forces that drive them around our globe.
To get the most out of this unit you will need the latest Flash Player plug-in. You can download it here.
This unit is an adapted extract from the Open University course
This is an extract from an Open University course which is no longer available to new students. If you found this interesting you could explore more free Geology course units or view the range of currently available OU Geology courses.