motion.
Earthquakes occur where plate rub against one another
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Tectonic Plates
Volcanoes
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Tectonic Plates
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Tectonic Plates
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Tectonic Plates
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Tectonic Plates
Slide 41
Tectonic Plates
Another source of
evidence is based
on seafloor ages
which get younger
as we approach
sea floor ridges
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Tectonic Plates
Our final piece of
evidence is the
magnetic record
of the ocean floor.
This shows the
pattern of reversal
and we find a near
perfect mirror image
on opposing sides
of the ridge
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Tectonic Plates
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Tectonic Plates
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Tectonic Plates
Slide 46
We can look at the interior of the Earth based
on the composition of the rocks or based on the movement
Slide 47
Crust – solid, relatively low density silicate rock
Mantle – Semi fluid, denser, mafic (iron and magnesium bearing) rocks
Core – Liquid then solid iron and nickel with traces of heavier elements
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It turns out that the upper section of the mantle is adhered (stuck to the underside side of the crust to form what we call tectonic plates
Slide 49
Oceanic plates: basalt
Dark (black) and dense rock type composed of silicates, iron and magnesium
Continental plates – granite and andesite
Light colored (pink, white and gray) and low density rock type composed almost entirely of silicates.
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