| |
Time: 15 hours Level: Intermediate
| |
| |
Introduction Resource
- 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...
| |
| | Preamble: the moving Earth
Preamble: the moving Earth Resource
- The Earth's face is changing all the time, but at barely perceivable rates. It is now known that the Earth is a highly dynamic planet – far more so than the other terrestrial planets (Mercury, Venus and...
| |
| | 1 From continental drift to plate tectonics
1.1 Continental drift Resource
- The remarkable notion that the continents have been constantly broken apart and reassembled throughout Earth's history is now widely accepted. The greatest revolution in 20th century understanding of how...
1.2 Evidence for continental drift Resource
- Ever since the first global maps were drawn following the great voyages of discovery of the 15th and 16th centuries, it has been realised that the coastline geography of the continents on either side of...
1.3 Sea-floor spreading Resource
- During and just after World War II, the technological improvement to submarines led to an improvement in underwater navigation and surveying that revealed many intriguing underwater features. The most...
| |
| | 2 The theory of plate tectonics
2.1 Assumptions Resource
- The surface of the Earth is divided into a number of rigid plates that extend from the surface to the base of the lithosphere. A plate can comprise both oceanic and continental lithosphere. As you already...
2.2 Heat flow within plates Resource
- As newly formed lithosphere moves away from an oceanic ridge, it gradually cools and heat flow (Box 2) decreases away from constructive plate boundaries.
2.3 Constructive plate boundaries Resource
- Constructive plate boundaries or margins are regions where new oceanic crust is being generated. However, in order for the magma to ascend to the surface and build new lithosphere, the earlier formed crust...
2.4 Destructive plate boundaries Resource
- Destructive plate boundaries are regions where two lithospheric plates converge. This situation provides a more varied range of tectonic settings than do constructive plate boundaries. Firstly, and in...
2.4 Destructive plate boundaries, continued: ocean-ocean (island-arc) subduction Resource
- The convergence of two oceanic plates represents the simplest type of destructive plate boundary and exemplifies most of the features associated with the destruction of oceanic lithosphere. Around the...
2.4 Destructive plate boundaries, continued: ocean-continent (Andean type) subduction Resource
- When an oceanic plate converges with a continental plate, it is always the ocean plate that subducts beneath the continental plate. Continental lithosphere lies at a higher surface elevation than oceanic...
2.4 Destructive plate boundaries, continued: continent-continent destructive boundaries Resource
- When two continental plates meet at a destructive boundary, the continents themselves collide. These types of continental collision are typically the result of an earlier phase of subduction of intervening...
2.5 Conservative plate boundaries and transform faults Resource
- Conservative plate boundaries and transform faults occur when plates slide past each other in opposite directions, but without creating or destroying lithosphere. Transform faults connect the end of one...
2.6 Triple junctions Resource
- All of the plate boundaries discussed so far have involved junctions between two plates. However, there are some localities where three plates are in contact, and these are termed triple junctions. Triple...
| |
| |
3.1 Relative plate motions Resource
- Plates move relative to one another and relative to a fixed reference frame, such as the rotational axis of the Earth. Plates also move across the curved surface of the Earth and so should not be considered...
3.3 Hot-spot trails and true plate motions Resource
- In addition to volcanism associated with constructive and destructive plate boundaries there is a third important component to global volcanism. This occurs in the interior of plates and is associated...
3.4 Plate motion on a spherical Earth Resource
- Earth's tectonic plates are continuously in motion with respect to each other, and together they form the closed surface of a sphere (i.e. the Earth's surface). Understanding the movement of plates, therefore,...
| |
| |
4.1 Why do plates move? Resource
- One of the key questions associated with plate tectonics is why plates move and what drives them. Plate tectonics is an expression of the thermal state of the Earth's interior and is the way that the Earth...
4.2 Forces acting upon lithospheric plates Resource
- Figure 28 provides a very simplified overview of the forces that are thought to affect the movement of lithospheric plates. The relative contribution of these forces to plate motion needs to be...
| |
| | 5 Implications of plate tectonics
5.1 The Wilson cycle Resource
- High-quality, palaeomagnetic data are now sufficiently abundant that it is possible to reconstruct the movement of the continents throughout the past 500–600 million years (i.e. the Phanerozoic) and, with...
5.2 Plate tectonics and climate change Resource
- This unit began by considering the evidence in the Earth's past for the existence of supercontinents and how evidence of past climates recorded in continental rocks can be used to reassemble ancient continental...
| |
| |
6 Summary Resource
- Plate tectonics is the grand, unifying theory of Earth sciences, combining the concepts of continental drift and sea-floor spreading into one holistic theory that explains many of the major structural...
| |
| |
Further reading Resource
- Fowler, C.M.R. (2005) ‘The Solid Earth’ Cambridge University Press, pp. 685
| |
| | References and Acknowledgements
| |