Title: Mercury
1Mercury
Best Ground-based Photo
2Mercury
- Observing Mercury from Earth is very difficult,
at - most 28o from the Sun. Even rotation period not
- known until 1965.
- 1965 Radar was used to determine rotation
period - Rotation period 58.7 days, exactly 2/3rd
orbital - period ? Mercury locked into 3-2 spin-orbital
- coupling.
33-2 Spin-Orbit Coupling
4In 1974, Mariner 10 made three flybys of
Mercury, and photographed 45 of its surface.
These photographs revealed that Mercury is very
much like the Moon, except for more extensive
intercrater plains, and the lack of large flat
lava beds called maria.
5Mercury
Moon
Moon
6Moon
Intercrater Plains on Mercury
7Caloris Basin
Opposite Caloris Basin
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9Mercury has almost no atmosphere.
The daytime average temperature is 350C The
nighttime average temperature is 170C The peak
dayside temperature is 550C
however, Mercury does have polar ice caps!
10Radar Image of Mercury, showing Ice Cap
11Magnetic Field
Mercury has a large iron core like the Earth, but
a much weaker magnetic field.
The reason the rotation rate is very slow,
meaning that the dynamo effect is very weak.
12The Moon
13The Moon
Diameter about ¼ that of the Earth Mass
about 1/80 M? No atmosphere, synchronous
rotation (1-1 spin-orbital coupling).
14Land Types
- Maria Lava Plains 15
- Cratered Highlands 85
Age of the Maria 3.1 3.8 Billion
years Highlands 4.0 4.3 Billion years
15Far Side
Moon Near Side
16Lunar Maria
17Lunar Highlands
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19Moon rocks have a similar composition to Earth
rocks except for slightly higher proportions of
refractory materials Moon formed at a higher
temperature.
20We believe the Moon was formed from the
collision of a Mars-sized object with the Earth.
21Collisional Formation of the Moon from the impact
of a Mars-sized body with the Earth
22A Brief History of the Moon
1) Formation 4.5 4.6 billion years ago
2) The Great Bombardment 3.8 4.5 billion
yrs ago
3) Formation of the Lunar Maria, 3.1 3.8
billion yrs ago.
4) Nothing much has happened for the last 3
billion years!