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The Terrestrial Planets, Part II The Earth
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EARTH
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Physical Data F Diameter: 12,756.3 km F Mass: 5.976x10 27 g F Density: 5.518 g/cm 3 F Rotation Period: 23.9 hours F Tilt of Axis: 23.5 o F Surface Temperature: 200-300 K
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Physical Data F Orbital Semi-Major Axis: 1.49x10 11 m (1 AU) F Orbital Period: 365.26 days F Orbital Inclination: 0 o F Orbital Eccentricity: 0.017 F Satellites: 1 F Magnetic Field: yes
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Earth’s Interior
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MANT L E CURR ENT S OCEAN F L OOR MOUNTAIN RANGE CONT I NE NT R I F F S T R ENCH F Currents in the Mantle Cause Plate Tectonics
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Earth’s Surface Continental Drift
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Earth’s Surface
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Earth’s Atmosphere F 75.5% Nitrogen F 23.1% Oxygen F 1.29% Argon F 1.7-0.06% Water Vapor F 0.05% Carbon Dioxide F 0.0013% Neon F 0.00007% Helium
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Earth’s Atmosphere ( I on os phere )
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The Ionosphere F2F2 F1F1 E D F layers combine at night
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The Ionosphere F Altitudes of the Ionospheric Layers
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The Ionosphere F Reflection of Radio Waves
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The Ionosphere F Creation of Ions
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Earth’s Magnetic Field S N S N F Dipolar Field F Magnetic South Pole is Located in the Geographic North Pole!
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Earth’s Magnetic Field F Van Allen Belts F Inner Belt - Positive Protons F Outer Belt - Negative Electrons e_e_ p+p+
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Aurorae F From the ground m
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Aurorae The Auroral Oval F From Space From the Space Shuttle
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Magnetosphere gjjikui Van Allen Belts
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The Moon
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Earth’s Moon F Average Distance to Earth: 384,400km (238,855 miles) F Orbital inclination: 5.1 o F Diameter: 3476 km (0.273 D Earth ) F Mass: 7.35x10 25 g (0.0123 M Earth ) F Surface Temperature: -274 o F (night) 266 o F (day) F Surface Gravity: 0.167 Earth’s
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The Moon’s Interior
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The Moon’s Surface Craters:Maria: Older TerrainYounger Terrain
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The Moon’s Surface Mare Orientale F Largest impact crater on the Moon F Has three concentric circular mountain ranges created by the impact
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