earth
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The Terrestrial Planets,
Part II
The Earth
EARTH
Physical Data
Diameter: 12,756.3 km
Mass: 5.976x1027 g
Density: 5.518 g/cm3
Rotation Period: 23.9 hours
o
Tilt of Axis: 23.5
Surface Temperature: 200-300 K
Physical Data
Orbital Semi-Major Axis: 1.49x1011 m
(1 AU)
Orbital Period: 365.26 days
o
Orbital Inclination: 0
Orbital Eccentricity: 0.017
Satellites: 1
Magnetic Field: yes
Earth’s Interior
Earth’s Interior
MOUNTAIN RANGE
RIFFS
OCEAN F L OOR T R ENCH CONT I NE NT
MANT L E CURR ENT S
in the Mantle Cause Plate
Currents
Tectonics
Earth’s Surface
Continental Drift
Earth’s Surface
Earth’s Atmosphere
75.5% Nitrogen
23.1% Oxygen
1.29% Argon
1.7-0.06% Water Vapor
0.05% Carbon Dioxide
0.0013% Neon
0.00007% Helium
Earth’s Atmosphere
( I on os phere )
The Ionosphere
F2
F1
E
D
F layers
combine
at night
The Ionosphere
Altitudes of the Ionospheric Layers
The Ionosphere
Reflection of Radio Waves
The Ionosphere
Creation of Ions
Earth’s Magnetic Field
Dipolar Field
S
S
N
N
South Pole is Located in the
Magnetic
Geographic North Pole!
Earth’s Magnetic Field
Van Allen Belts
Inner Belt - Positive
Protons
_ Outer Belt - Negative
e p+
Electrons
Aurorae
From the ground
m
Aurorae
From Space
From the Space Shuttle
The Auroral Oval
Magnetosphere
Van Allen Belts
gjjikui
The Moon
Earth’s Moon
Average Distance to Earth: 384,400km
(238,855 miles)
o
Orbital inclination: 5.1
Diameter: 3476 km (0.273 DEarth)
Mass: 7.35x1025 g (0.0123 MEarth)
o
Surface Temperature: -274 F (night)
o
266 F (day)
Surface Gravity: 0.167 Earth’s
The Moon’s Interior
The Moon’s Surface
Craters: Maria:
Older Terrain Younger Terrain
The Moon’s Surface
Mare Orientale
Largest impact
crater on the Moon
Has three
concentric circular
mountain ranges
created by the
impact
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