Theory of plate tectonics

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A Level (Plate tectonics and associated hazards) Geography Fichas sobre Theory of plate tectonics, creado por Nicola Bywater el 10/09/2014.
Nicola Bywater
Fichas por Nicola Bywater, actualizado hace más de 1 año
Nicola Bywater
Creado por Nicola Bywater hace alrededor de 10 años
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Define plate tectonics theory Explains global distribution of a geographical phenomena such as seismicity, volcanism, continental drift and mountain building in terms of the formation, destruction, movement and interaction of the Earth's lithospheric plates
1620 Frances Bacon, countries either side of the Atlantic fit together
1909 Mohorovicic, seismic waves change speed when travelling through the Earths centre
1912 Alfred Wenger, - Pangea - Laurasia and Gudwana - 7 major plates - 15 major and 40 minor - Continental drift
Name the 8 pieces of evidence for the plate tectonics theory 1. Continental fit 2. Geological evidence 3. Climatological evidence 4. Paleomagnetism 5. Convection Currents 6. Biological evidence 7. Mid Atlantic Ridge discovery, 1948 8. Sea floor spreading
Continental fit - Seem to fit together - Jigsaw fit - Not perfect due to the difference in erosion, weathering and sea levels - South America and Africa West Coast
Geological evidence - Rocks of the same age, type and formation in South East Brazil and South Africa - Glacial deposits in Antartica, South America and India - Mountain structures in Eastern USA and North West Europe are similar (Appalachian and GlenCo, Scotland)
Climatological evidence - Similar age coal deposits which all must have developed in tropical conditions in Antarctica, UK and North America - These moved apart and drifted away from tropical climates
Biological evidence - Similar fossil formations on either side of the Atlantic - Plant remains from humid swamps forming coal deposits in India and Antarctica - Mesosarus remains in South Africa and Eastern South America (fresh water animal) - Marsupials only in Australia as it drifted away before they were wiped out
Mid Atlantic Ridge, 1948 - Continuous mountain range along the ocean bed - 100km wide and 2.5 km high - Composed of recently formed volcanic rock, with newest rocks nearest ridge - Iceland has rocks under 1 million years - Oldest rocks in USA and Carribean - 5cm per year spreading
Paleomagnetism - Stripes of normal and reverse polarity rocks, a mirrored pattern either side of the ridge - Iron particles in the lava are aligned with the magnetic field of the Earth - The direction of the force changes every 400,000 years - New rocks added equally to either side
Convection currents - The driving force of the movement of plates - Caused as radioactive particles in the mantle decay and give off heat
Two adjacent convection currents sink Destructive
Two adjacent convection currents rise Constructive
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