Post midterm ! Flashcards
Protoplanetary disk inside frostline porpotions of materials..
0.2 metal
0.4 rock
1.4 hydrogen compounds
98 helium
Outside frost line porpotion of materials
0.2 metal (solid)
0.4 Rock (solid)
1.4 Hydrogen compounds
98 helium
Tiny small objects stick together to form
planetesimals
Planetesimals are the _____ of what will become planets
seeds
How does a crater form
planetesimal hits surface and vaporizes rock, creating explosion
heavy bombardment period
lots of planetisemals crashing everywhere after planets formed about 4 bil years ago
mercury and moon covered in
craters
LOOK UNDER SURFACE OF PLANET USING
SOUND WAVES
2 types of waves (vibrational travel)
P waves - compression
S waves - side to side
S wave paths
cant go past the liquid in the ball
what is the empty s wave parrt that cant be reached called
s - wave shadow zone
P wave paths
it goes through the liquid ball but everytime it goes through the curve of the line is like reflected
Timing for seismometers at different places depend on
how far and fast the wave traveled
Direction of ——– tell difference between S and P waves
vibrations
S wave on graph is
horizontal (east to west/ north to south)
P wave measured on graph is
verticle
Mercury is estimated from
density + spin rate variations
Venus is estimated from
density
Earth moon mars measured with
seismometers
Why do planets have cores
differentiation: lighter materials like rock float to top, heavier materails like iron sink
Why planet interiors hot:
accretion:
Dominant during formation
Why planet interiors hot:
differentiation:
more dominant earlier
Why planet interiors hot:
radioactive decay:
Dominant source of heat today
Planets cool via
convection
HOW PLANETS COOL step 1
convection:
Hot rock will rise, cool rock sink, hot rot goes surface and release heat
HOW PLANETS COOL step 2
Conduction:
carries the hot rock heat out cuz its thin and rigid
HOW PLANETS COOL step 3
radiation
energy gets radiated to space at surface as infrared light
smaller planets have less —— compared to surface area of a large planet
mass
craters get covered by, what does it indicate
molten lava spewing out and hardening, young surface
are any of earths craters result from heavy bombardement
no
mars has 384343 craters larger than _____km
1
Mares on the moon are
dark spots that used to be craters but got hard lava covered it
Mars has many volcanoes that are
NOT ACTIVE
Small terrestrial planets interior cools… leading to……
rapidly
quickly ending volcanic activity
lack of volcanic activity means no outgassing cuz low gravity allows gas to escape –> no atmosphere
LAck of volcanic activity on small terrestrial planets means
low outgassing, so gas leaves really easily and does not form atmosphere leading to NO EROSION
large terrestrial size and stuff is
opposite of little planet:
Slow cooling
volcanic activity
has atmosphere?
outgassing produces
atmosphere
Temperature changes can put stress on planets crust causing. (2things)
mountains and cracksq
PLate tectonic workings:
Subduction at CONVERGING plates
ocean plates get pushed under continent plates, making the continental plates high (mountain)
PLate tectonic workings:
diverging plates
causes undersea ridges
No erosion likely means
water stopped flowing
Trend in terrestrial planet atmospheres
larger planets have thicker atmospheres
NO h2 in the atmosphere
Higher temperature means what for average speed
faster average speed
higher mass means what for avg speed
slower avg speed
Objects going faster than a planets escape velocity will…..
escape into space
lower mass planets have lower…. soo….
escape velocity, easier to escape
It is easier to escape a —– planet’s gravity
small
low mass gas moves….. so…
faster, easier to escape
Hot gas moves…… so…..
faster, easier to escape
Mercury + Moon escapes velocities are
low
Venus escape velocity is
high
Mars escape velocity is
in the middle (between mercury and venus)
venus, mars, merury, moon escape velocities are all
too low to keep H2
Carbon cycle on earth (why is N2 left as dominant gas)
Co2 in air dissolves in rainwater
water flows into ocean with minerals
Co2 in water reacts with rocks/metals to form CARBONATE ROCKS
carbonate rock is pushed to ocean floor under tectonic plates
volcanos releases small amounts of this co2 back into atmosphere
why doesn’t earth have much CO2
it has water
Co2 levels on earth vary based on
volcanism
biological activity
have ben dropping for the past 50 mil years
The warmer the planet, the more ———– —— is emitted
infrared light
The planet will warm until the absorption of ——— —– and emission of —— —— are balanced
visible light
infrared light
Visible light from the sun shines on planet, some light is ——— and the rest is ——–
reflected (as infrared)
absorbed
Greenhouse effect (think of how blanket works)
“No u”
visible light gets in the atmosphere which is mostly absorbed and the planet gets hot so infrared light is emitted and the greenhouse gasses absorb and remit this back onto surface (blanket)
venus is EXTREMELY hot because
thickass atmosphere, traps lots of heat, greenhouse gas effect
PHOTODISSOCIATION:
– light from sun separates atmospheres’ ——
UV
atoms
PHOTODISSOCIATION:
the separated atoms from the UV light will——– asap after ——— each other
reconnect
refinding
individual atoms are lighter than molecule so……
can escape easier
Solar wind of high energy particles do what to the atoms on mars
knock thema way
define crust
low density rock
core
high density iron/nickel
mantle
medium density rock
Earth’s magnetic field deflect solar wind particles which…
stops the atmosphere from breaking
Asteroids orbit……….. they are not large enough to be…..
the sun
spherical
half an elliptical is called (YELLOW LINE DIVIDING ELLIPSE)
SEMI-MAJOR AXIS
Time of an orbit (period) depends on
semi major axis
Jupiter effects the —— of the asteroids
orbits
Orbits in —— ———— with Jupiter get ———
exact resonance
displaced
The displaced asteroids form —— — along the ring meaning that there are — asteroids
dark bands
no