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Chapter 10, Part1: SunScorched Mercury

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Title: Chapter 10, Part1: SunScorched Mercury


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Chapter 10, Part1 Sun-Scorched Mercury
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87.9/58.6 32
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Earth-based optical observations of Mercury are
difficult.
  • Mercury never gets far from the Sun.
  • Mercury is briefly only visible right before
    sunrise (greatest western elongation) or just
    after sunset (greatest eastern elongation).

4
Earth-based optical observations of Mercury are
difficult.
The tilt of Earths axis and the inclination of
Mercurys orbit combine to make favorable and
unfavorable observations.
5
Earth-based optical observations of Mercury are
difficult.
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Mercury can be observed using radio telescopes
such as Arecibo.
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Mercury can be observed using radio telescopes
such as Arecibo, which bounce radio waves
revealing Mercurys rotation.
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Mercury rotates slowly and has an unusual 3-to-2
spin-orbiting coupling.
This tidal locking is exactly like the Earths
Moon (or Jupiters satellite Io), but has a 32
spin-obit coupling instead of 11
11
Mercury rotates slowly and has an unusual 3-to-2
spin-orbiting coupling.
12
Mercury rotates slowly and has an unusual 3-to-2
spin-orbiting coupling.
1 rotation completed
1.5 rotations completed
13
Mercurys surface is inhospitable
  • 88 days of daylight and 88 days of night.
  • Daytime temperatures are 430ºC (800ºF)
  • hot enough to melt lead
  • Nighttime temperatures are -170ºC (-270ºF)
  • Cold enough to freeze CO2 and CH4.
  • Earth typically has temperature differences
    between day and night of about 11ºC (or 20F) .

On Mercury, the Sun moves from east to west,
except at perihelion where Mercurys movement
around the Sun outpaces its rotation and the Sun
appears to move backwards through the sky.
14
Images from Mariner 10 reveal Mercurys heavily
cratered surface.
(Earths Moon on same scale at right for
comparison)
15
Images from Mariner 10 reveal Mercurys heavily
cratered surface.
16
Images from Mariner 10 reveal Mercurys heavily
cratered surface.
Mariner 10s three passes all resulted in the
same side of Mercury being photographed.
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Caloris Basin on Mercury
1300 km
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Edge of Caloris Basin 1300 km (810
mi) diameter
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The Focusing of Seismic Waves creates broken
hilly terrain opposite Caloris Basin
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Unusual, hilly terrain opposite the Caloris Basin.
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Radar Astronomy of Mercury1.
Determined rotation and 32 spin-obit coupling
(1964)2. Found evidence for ice in polar cap
craters (1999)
Arecibo (P.R.) Worlds largest radio telescope
24
Possible ice deposits at Mercurys North Pole in
permanently shadowed craters.
25
Like the Earth, Mercury has an iron core and a
magnetic field.
  • Mercury is the most iron rich planet in the solar
    system.
  • Mercurys core takes up 75 of the planets
    diameter.
  • At least part of Mercurys core must be liquid
    for a magnetic field to be present.
  • There must be a source of energy to make a liquid
    core flow to create a magnetic field.
  • Mercurys magnetic field is a source of great
    mystery.

26
Mercury likely had its outer layers (mantle)
stripped away by a catastrophic collision early
in its history leaving a planet made of mostly
iron.
The next mission to explore Mercury is the NASA
MESSENGER (MErcury Surface, Space ENvironment,
GEochemistry, and Ranging) Mission.
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Messenger Mission to Mercury
  • Launch 2004, arrival 2009
  • Science objectives
  • Complete surface mapping (only 50 now)
  • Is there water in polar cap craters?
  • Why is Mercury so dense? Is it mostly Iron?
  • Structure of magnetic field?
  • Is there a outer liquid core?

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Guiding Questions
  • What makes Mercury such a difficult planet to
    see? Too close to Sun greatest elongation only
    28
  • What is unique about Mercurys rotation? Has 32
    orbital (88d) to rotational (58.6d) period ratio
    (due to tidal locking). This is called spin-orbit
    coupling
  • How do the surface features on Mercury differ
    from those on the Moon? Very Similar (heavily
    cratered) but Mercurys plains are older,
    lighter in color.
  • What evidence is there for ice on Mercury? Radar
    signals show high reflectivity in polar craters
    (Arecibo 1999)
  • What is the Caloris basin? Huge 1300 km diameter
    crater, may have nearly split Mercury into
    pieces. Very old (4 Gyr)
  • Is Mercurys internal structure more like that of
    the Earth or the Moon? More like Earths (large
    iron core)
  • What spacecraft have visited Mercury? Future
    spacecraft? Only one (Mariner 10, 1974!)
    Messenger Mission will launch 2004, arrives 2009
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