Things I'd like you to remember are in bold italics.
Mercury
• a = 0.4 AU
• Always appears close
to Sun - thus hard to see from ground-based scopes
• 59-day sidereal period
of rotation - 2/3 (exactly) of its 88-day year - it rotates 3 times for each 2
revolutions - not a synchronous motion like our moon
• Temperatures range
from 427 °C (800 °F) to -183 °C (-300 °F); huge temp difference (>1000
degrees F) between night and day). Even
so – NOT THE HOTTEST PLANET
• On rare occasions,
Mercury transits across Sun (eclipsing it) - 2016
• Albedo (ratio of
reflected light to total light hitting body) = 6%
• Similarly, Moon only
appears bright to use because it is surrounded by dark sky
• Mariner 10 spacecraft
visited in 1974
• less than 1/2 Earth
diameter, but similar density (42% iron core)
• Heavily cratered, but
flatter craters
• Fine dust on surface; no
water, but maybe a little ice?
• Weak magnetic field
• Iron core, 50% of
volume and 70% of mass of Mercury
• Thin atmosphere,
detectable from Mercury’s spectra - primarily Sodium (and some Helium, Oxygen,
Potassium, Hydrogen)
• Lines of cliffs
hundreds of miles long - scarps; a wrinkle in the crust
• Features named after
historical ships (scarps), the name of Mercury in different languages (plains),
nonscientific authors/composers/artists (craters – unlike the craters on the
moon which are named for scientists)
VENUS
Atmosphere
• Sulfuric acid clouds
(this takes up much water) - must use radar to “see” surface
• Carbon Dioxide
atmosphere (>90%)
• Surface air pressure
is 90x Earth air pressure
Rotation and Revolution
• Backwards rotation,
relative to other planets (perhaps it was struck while being formed)
• 225 day year
• 243 day rotation
period
Misc
• a = 0.7 AU; closest
planet to us
• 750 K surface
(greenhouse effect from thick clouds); hottest and brightest planet (only the Moon
is brighter in the night sky)
• Similar density and
features
• Venusquakes?
• No magnetic field
• Many probes have been
sent to visit Venus
• Basalt surface
• Large rolling plains
• Very active cloud
system
• Not highly cratered -
smallest meteoroids could have burned up in atmosphere; perhaps some vulcanism
• Probably lightning and
volcanic activity
• Only about 16% of
Venus below plain
• Huge mountain Maxwell
(11 km, 2 km higher than Mt. Everest)
• One continental plate
• Similar gravity to
Earth
• No satellites
• Features named after
mythical goddesses (major), mythical female figures (minor), and famous women like
Sacajawea (other features)
Earth
General – the water
planet (71% covered)
• Inner core - iron and
nickel (about the size of our
Moon) - rotates a bit
quicker than outer core (by 2/3 of a second)
• studied by seismic
action
• outer core is liquid,
the motion of which causes the magnetic field
• mantle (outside the
core) - many silicates; this is the bulk of the Earth
• crust on top (thin)
• crust and outer mantle
= lithosphere
• Below lithosphere is
aesthenosphere, which is partly melted
• 1/3 of Earth mass is
iron
• Gravitational
acceleration (local) of 9.8 m/s/s
An active planet
• Natural radiation from
within
• Continental drift from
geothermal energy
• Plates about 50 km
thick
• Plate tectonic
activity
• Continents probably
once formed Pangaea (“all lands”), which in turn split into Gondwanaland and
Laurasia
• Ultimately, California
may split from USA, Australia may become linked to Asia, etc.
• Two plates come
together, one is often forced under another - volcanoes formed
• Tides are the result
of motion around sun and lunar motion - differences between gravitational
forces between Moon and Earth at different locations on Earth
Atmosphere
• Nitrogen, Oxygen
(>99% total)
• Troposphere (0-15 km, 285-225K) - Earth weather occurs here
• Stratosphere (15-50
km, 225-260K) - upper strat and lower mes contain Ozone layer
• Mesosphere (50-90 km,
260-190K)
• Thermosphere (90+ km, 190-260K) - aka ionosphere; not
temperature rise here
Relatively thin when
compared to Earth’s radius of 6400 km
Van Allen Belts
• Like a trio of donuts
made of charged particles (e-, etc.) held byEarth’s magnetic field
• When hit by solar
particles, our atmosphere may glow - aurora borealis, aurora australis
(hundreds of km above Earth)
• Earth has strongest
magnetic field of the terrestrial planets, and it is not all that strong
Mars
• The red planet (iron
oxide?)
• Possible water in its
past
• Surface pressure ~ 1%
of Earth’s
• 23 Earth month period
• Seasonal, since it has
a 25° tilt to axis
• Polar ice cap in the
winter (Carbon dioxide, some water?)
• Global dust storm -
hundreds of km/hr!
• Changes in appearance
possibly once thought to be due to a type of vegetation
• Four types of
regions: volcanic regions, canyon areas,
expanses of craters, terraced areas near poles
• Channels (some 200 km
wide and 7 km deep), some thousands of km long – possibly cut by water in past
• Olympus Mons (25 km
high volcano, 600 km at the base!)
• 90% Carbon dioxide
atmosphere
• No tectonics
• Yellowish-brown sky,
dust abounds
• Once water; once
life??
• Temps from 150-300 K
with great variation depending on storms
• Originally thought to
have canals, but no longer
• about 1/2 Earth
diameter; 1/10 Earth mass; 2/5 Earth gravity
• Length of day a bit
longer than Earth’s; same for axial tilt
• Smaller core and
thicker crust than Earth
• Viking landers, Mars
Pathfinder, Mars Global Surveyor, Mars Observer (failed), Spirit, Opportunity,
Phoenix, Mars Reconnaissance Orbiter, Curiosity,
• 2 satellites (captured
asteroids?) - Phobos, Deimos; cratered asymmetric rocks (15-20 km across –
smaller than some asteroids)
• Major features named
for Greek mythology (Olympus Mons); smaller features have been named for
cartoon and children’s literature figures; some craters name for dead people
associated with Mars
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