Journey to Center of the Earth
Draw a model of the inside of earth On loose leaf paper Art supplies available
THE LAYERS What was right about your model? What was wrong about your model?
CRUST What we know? Rocky- mainly silicates (quartz, feldspar) Brittle Broken into pieces (plates) Continental- granite (less dense)- thicker Ocean- basalt (more dense)-thinner
CRUST How do we know it? Direct samples ( drill cores) sonograms
Drill cores Deepest 12 km Tried to reach Moho failed
drilling attempts to the Moho Russia- 1989- 12km 7 miles $100 million 190° C US- 1988 3.5 km
Drilling program April 2005- drilled 1416 meters Gabbro rocks Near Mid-Atlantic Ridge $1.5 billion budget
Lithosphere Rigid- crust + upper mantle Makes up Earth’s plates
Asthenosphere Solid rocks that flow Plates “float” on asthenosphere
MANTLE What we know? Solid that flows (plasticity) magma Composed of iron, magnesium (olivine) Has convection currents
Mantle
MANTLE How do we know it? S waves travel through mantle Volcanoes give us a “peek”
OUTER CORE What we know? Liquid iron How we know it? S-waves do not travel through outer core Magnetic field
Seismic waves P waves S waves Travel through liquids and solids Travel slower thru liquids than solids S waves Do NOT travel through LIQUIDS
INNER CORE What we know? Solid iron How we know it? P-waves speed up Study meteorites