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Published byAlban Cunningham Modified over 9 years ago
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The Earth as a Terrestrial Planet Mass -- 6 x 10 27 gm (6 x 10 24 kg) Size -- diameter 12,756 km (eq.) Density – mean 5.5 gm/cm 3 Surface -- 71% water
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Interior Crust Mantle Core Densities – crust < 3 gm/cm 3 -- mantle 3.5 gm/cm 3 ? Very dense core ~ 15 gm/cm 3 Fe/Ni Outer core – molten (5000-7000K) Inner core – solid ~ 7000K Rotating molten core produces magnetic field Why ? – differentiation of elements
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Age Dating of Earth Radioactive decay -- uranium, plutonium, thorium U 238 Pb 206 Th 232 Pb 208 using known half-life Rocks on Earth -- newly formed to ~ 3.5 - 4 x 10 9 yrs Oldest Moon rocks – 4.5 – 4.6 x 10 9 yrs
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Our Active Earth – Plate Tectonics or Continental Drift
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Consequences– earthquakes, volcanoes, mountain building
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San Andreas Fault
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Caused by convective currents in mantle transfers heat to crust
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The Earth at Night
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The Earth and Moon as a Double Planet Mmoon/Mearth = 0.012 (1/80 th ) Rmoon/Rearth = 0.27 (1/4 th ) Largest in Solar System
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Surface Features Craters Mare Highlands
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Origin of the Moon Sister planet – by fission Co-accretion – at same distance, same material Capture – not dynamically feasible Current theory – massive collision – computer modeling
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Lunar rocks and soil samples
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Age Dating Lunar rocks and soil samples Mare – 3.8 x 10 9 yrs Highlands – 4.3 – 4.6 x 10 9 yrs What does this imply?
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