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Journey to Center of the Earth
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Draw a model of the inside of earth
On loose leaf paper Art supplies available
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THE LAYERS What was right about your model?
What was wrong about your model?
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CRUST What we know? Rocky- mainly silicates (quartz, feldspar) Brittle
Broken into pieces (plates) Continental- granite (less dense)- thicker Ocean- basalt (more dense)-thinner
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CRUST How do we know it? Direct samples ( drill cores) sonograms
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Drill cores Deepest 12 km Tried to reach Moho failed
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drilling attempts to the Moho
Russia km 7 miles $100 million 190° C US km
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Drilling program April drilled 1416 meters Gabbro rocks Near Mid-Atlantic Ridge $1.5 billion budget
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Lithosphere Rigid- crust + upper mantle Makes up Earth’s plates
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Asthenosphere Solid rocks that flow Plates “float” on asthenosphere
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MANTLE What we know? Solid that flows (plasticity)
magma Composed of iron, magnesium (olivine) Has convection currents
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Mantle
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MANTLE How do we know it? S waves travel through mantle
Volcanoes give us a “peek”
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OUTER CORE What we know? Liquid iron How we know it?
S-waves do not travel through outer core Magnetic field
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Seismic waves P waves S waves Travel through liquids and solids
Travel slower thru liquids than solids S waves Do NOT travel through LIQUIDS
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INNER CORE What we know? Solid iron How we know it? P-waves speed up
Study meteorites
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