Mercury and Venus
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Transcript Mercury and Venus
The Innermost Planet
•
•
Inferior conjunction – inferior
planet and Earth on same side
of Sun
Superior conjunction –
inferior planet and Earth on
opposite sides of Sun
Smallest
of the planets (Pluto etc. does
not count)
Named for the swift messenger to the
Roman gods
Bright
in appearance but not easily seen:
• Only visible at morning or evening
• At most, 28.3º from the Sun
Ground
based telescopes give only
limited detail
Radius
Moon
1700 km
7.3 × 1022
kg
Density 3300 kg/m3
Mass
Escape
Speed
2.4 km/s
Mercury
1440 km
Earth
6380 km
3.3 × 1023 kg 6.0 × 1024 kg
5400 kg/m3
5500 kg/m3
4.3 km/s
11.2 km/s
Long
thought to be tidally locked to the Sun;
measurements in 1965 showed this to be false.
Mercury’s day and year are in a 3:2 resonance;
Mercury rotates three times while going around
the Sun twice.
Spin-orbit resonance – ratio of the periods can
be expressed as simple integers
most
eccentric
orbit of all the
planets
orbit is inclined by
7 degrees to the
plane of the
ecliptic
axial tilt is almost
zero
when
Mercury
comes between
the Sun and the
Earth
Mercury is seen
as a small black
dot moving
across the face of
the Sun
2016 May 9
Crust
2. Mantle
3. Core
Core occupies
42% of Mercury
(17% for Earth)
Has higher iron
content
1.
Mercury
is much denser than the Moon
Has a magnetic field – not well
understood!
Significant
for size
Planetwide
Dynamo effect?
MESSENGER will
measure
Features
of Mercury’s geology:
• Dorsa
• Impact basin’s and craters
• Pit floor craters
• Plains
• Scarps
• Volcanoes
Ridges
Caused
by faults
in crust
Mercury
is very
heavily
cratered. More
so than the
Moon.
Predominant
feature of
Mercury
Floors can be
smooth plains
Largest
crater
in solar system
1,550 Km in
diameter
Antipodal
of Caloris Basin
Where shock waves collided
Crater
floor has
collapsed
Possible magma
chamber under
crater?
Inter-crater
plains are
the oldest visible
surface
• occur in the regions
between larger craters
• Gently rolling hills
Smooth
plains are
widespread flat areas
• resemble lunar maria
• fill depressions
Scarps
are cliffs caused
by the terrain moving
vertically
On Mercury, caused by
crust shrinking as
planet cooled.
evidence
of
lava flows
Cinder cone
volcanoes
Second most
important
featureformer
Craters
at pole may
have water ice
Bottom of crater is
in permanent
shadow
Spotted with radar,
need confirmation
from MESSENGER
Very
tenuous
• about 2 trillionths of the
atmospheric pressure on
Earth
containing
hydrogen,
helium, oxygen, sodium,
calcium, potassium and
water vapor
Solar wind gives Mercury
a tail
Only
two missions have visited Mercury:
• Mariner 10 (1973)
• MESSENGER (MErcury Surface, Space ENvironment, GEochemistry
) (2004)
and Ranging
Last
of the Mariner missions
Explored both Venus and Mercury
Could only map about 45% of Mercury
• Same side was sunlit on each of the three flybys
Can
get better pictures of Mercury
Has performed 3 flybys so far
Will enter orbit of Mercury in March 2011
Smallest
planet
3:2 orbital resonance; most eccentric
orbit
Molten iron core
Small but significant magnetic field
Impact craters are biggest feature
Ice in polar craters
Very thin atmosphere