Plate Tectonic theories
Slides do conjunto (4)
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- Proposed the theory of continental drift. He suggested that all the plates were joined together in a super continent called Pangaea which drifted apart.
- Wegener based his theory on geological evidence and fossil records.
- But couldn't back it up with a mechanism that explained how the continents moved.
- But in the 1950s, palaeomagnetism provided evidence that supported continental drift.
- And in the 1960s the process of sea floor spreading was discovered-it provided the mechanism for continental drift.
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Evidence for Continental drift
- Geology
- -Areas of South America and Africa have rocks of the same age and composition- if you fit these continents together, the distribution of the rocks matches up.
- -You can also match up mountain ranges, eg Mountains in Scotland, Norway, Sweden and Finland are similar to the east coast of North America.
- -These rocks and mountains must have been formed under the smae conditions and the same place in order to match so well- this would only be possible if the continents were once joined.
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- Fossil Records
- By fitting land masses you can match up the distribution of some fossils eg fossils of Lystrosaurus and Mesosaurus
- Living Species
- The same living organisms can be found on different continents.
- Climatology
- There's evidence that the past climates of some continents were similar, despite being thousands of miles apart now. This suggests that they were located together and in different places
- Poalaeomagnetism
- Study of earths magnetic field
- Once every 200,000 years the Earth's magnetic field reverses polarity
- Provides evidence for sea floor spreading
- As magma erupts from the mid-ocean ridges, magnetic minerals in the molten rock align themselves with the direction of the earths magnetic field.
Informações
- Descrição
- A-Level Geography (Plate tectonics) Slides sobre Plate Tectonic theories , criado por Ross Newman em 14-01-2016.
- Criado por
- Ross Newman · jan 2016
- Atualizado
- 10 jun 2016
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