Plate tectonics

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Created by:

tfreeman14  on April 5, 2011

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earth science

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Plate tectonics

plate
a solid section of the Earth's lithosphere- 20 plates move relative to one another atop the asthenosphere
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plate a solid section of the Earth's lithosphere- 20 plates move relative to one another atop the asthenosphere
convection current circular motion of material due to heating and cooling
responsible for the movement of the plates
lithosphere crust very top of mantle plates
asthenosphere what plates float on top of - mantle
Alfred Wegener proposed that the continents were once joined together in a single land mass (called Pangea) in 1915
Pangea 200- 250 million years ago, it a was a single land mass- means all land in greek
Evidence for Pangaea 1. Continents fit together (puzzle)- Africa and South America.
2. Fossils of plants and animals of same species were found on different continents
3. Mountain Ranges -correlations
4. coal was found where it should not have been able to form
continental shelves continental edges underwater
Mesosaurus freshwater reptile whose fossil provided evidence for Pangea
Glossopteris a fern fossil, provided evidence for Pangea
Laurasia Northern part of Pangaea
Gondwana southern section of Pangea
Tethy's Sea sea in Pangea between the northern and southern parts
Panthalassa The single, large ocean that covered Earth's surface during the time the supercontinent Pangaea existed
Harry Hes proposed seafloor spreading in 1962
Iceland the only place where the midatlantic ridge crossed land
Paleomagnetism the study of changes in Earth's magnetic field, as shown by patterns of magnetism in rocks that have formed over time
remnant magnetism in rock bodies
Vine and Matthews the two people that came up with the magnetic discovery of paleomagnetism
Hot spots not associated with plate boundaries- a plume of magma that rises towards the surface of the earth usually in the center of the plate, causes a volcanoe- plate moves relative to ________
Seafloor spreading the mechanism responsible for producing the new seafloor between two diverging plates
convergent plate boundary where plates move together causing one of the slabs to be consumed into the mantle as it descends beneath an overriding plate.
normal polarity when rocks exhibit the same magnetism as the present magnetic feild
divergent plate boundaries the type of plate boundary where plates move apart, resulting in the upwelling of material from the mantle
examples rift valley, mid Atlantic ridge
oceanic crust crust formed from magma deep in the mantle DENSE
oceanic and continental subduction, oceanic slides under, pushing continental upward, forms Mountain ranges (example: Andes)
- site of volcanoes and earthquakes
(name the plates)
continental and continental overriding of one plate, formation of mountain ranges examples Himalayas
Oceanic and oceanic forms an island arc
ex; Japanese Islands, sites of volcanoes and earth quakes
Caledonia Mountains Mt. range formed at the same time as Appalachians
500,000 years how often do the magnetic pulls flip flop
North American and Eurasian two plates moving apart at the midatlantic ridge at iceland
deep ocean trench fracture in subduction zone
largest is Marianas trench
Transform Boundary fault zones
Ex San Andres fault
site of earthquakes
Curie point The temperature above which a material loses its magnetization.

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