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57 Cards in this Set

  • Front
  • Back
sister planet of Earth
Venus
fastest moving planet
Mercury
"psychologically pleasing" planet
Mars
-same hours day/night
-seasons twice as long
slowest rotating planet
Venus
-days longer than years
retrograde motion
rotating in wrong direction
densities of materials
water (ice) = 1.0
rocks ~ 3.0
metals ~ 8-10
properties of terrestrial planets
-high density
-orbits closely spaced
-slow rotations
-masses/sizes much smaller
less massive terrestrial planets (2 of 4)
Mars and Mercury
robots have landed on...
-Moon
-Venus
-Mars
-Titan
-asteroids
we have probed the atomspheres of...
-Venus
-Mars
-Jupiter
-Titan
we mapped .... with radar
Venus and Titan
gas giants
Jupiter and Saturn
ice giants
Uranus and Neptune
dwarf planets (ice/rocky)
-Pluto
-Eris
-Ceres
new dwarf planets
-MakeMake
-Haumea
small icy bodies
-Kuiper Belt
-Comets
small rocky objects
-Asteroids
-Meteors
surface temp. of sun
6000K
most visible sun light:
UV and IR
age/life of sun
4.6 b years old
12 b years left
largest terrestrial planet
Earth
terrestrial planet w/out atmosphere
Mercury
density range of terrestrial planets
3.9-5.5 g/cc
range of Jovian planets distances
5 to 30 AU
density range of Jovian planets
0.7 to 1.7 g/cc
composition of Jupiter/Saturn
-thick H/He atmosphere
-liquid hydrogen mantle
-small rock core
composition of Uranus/Neptune
-thick H/He atmosphere
-ice mantle
-even smaller rock core
mass of Jovian planets
Jupiter - 318 M
Saturn - 95 M
Uranus - 15M
Neptune - 17M
mass of terrestrial planets
Mercury - .055 M
Venus - .82 M
Earth - 1 m
Mars - .11 M
dwarf planet properties
-Outer SS objects
-More elliptical, inclined orbits
-Massive enuf to be spheroidal
-Not dominant in their orbital neighborhoods
planets w/out moons
Mercury and Venus
Jupiter moons
Io
Europa
Ganymede
Callisto
Saturn moon
Titan
Neptune moon
Triton
properties of Asteroids
-Rock & metal (2-3 g/cc)
-Sizes: Few 100km to boulders
-Most are found in the Main Belt (2.1-3.2 AU)
properties of Meteors
-Vaporizing bits of rock and metal
-Sizes: grains of sand to boulders
-Enter our atmosphere
properties of Comets
-Long tails when near Sun
-"Dirty Snowballs"
Kuiper Belt objects
-Outer SS (30-100AU)
-1.2 to 2 g/cc (mostly ices)
-A source of:
short-period comets (<200 yrs)
dwarf planets
The Oort Cloud
-size: ≈ 100,000 AU
-source of long-period comets
Electromagnetic waves
Periodic changes in the strengths of electric & magnetic fields.
speed of light (c)
299,792.458 km/sec
relationship of frequency/wavelength
c = frequency x wavelength
EM spectrum
Low F, long WL
radio
microwave
IR
visible
UV
x-ray
gamma ray
High F, short WL
composition of Earth's atm.
Nitrogen - 78%
Oxygen - 21%
CO2 - .04% & rising
Earth's core
-extend to half-Earth radius
-inner: solid iron
-outer: liquid iron
Earth's mantle
-Silicate rock that can “flow
-most of Earth's mass
Earth's crust
-thin ~ 20 miles
-ocean: basalt (solid magma)
-continents: various rocks
silicate rocks
granite
quartz
geological activity
changes to surface of planet
Mercury spacecrafts
Mariner 10 (1974-5)
-1 flyby (half planet
Messenger
-orbits (has 3 flybys already)
smallest/fastest terrestrial planet
Mercury
Mercury orbit
-highest incline: 7 degrees
-highest eccentricity: 0.21
-2 orbits = 3 rotations
-> Tidal Resonance
Mercury surface
-largest temp D/N: 800F>-279F
-high crater count
Mercury interior
-huge iron core (75% radius)
60% mass
-rocky mantle: ~700 km
Venus atmosphere
96% Carbon Dioxide
0.15% Sulfur Dioxide
0.02% Water Vapor
-sulfuric acid clouds 48-58km high
-runaway Greenhouse effect
Venus surface
-891º F
-90 atm
-NO plate tectonics
-low impact craters
Venus terrain
85% rolling planes
15% highlands / mountains
-Ishtar Terra
-Aphrodite Terra