chapter 12 (pt. 1), 13 & 14 Flashcards
evidence for planet/star common origin comparative planetology of metallic/rock planets liquid-gas giant planets of the outer solar system (96 cards)
Earth
home, third rock from the Sun, water planet, thin atmosphere altered by life, large terrestrial
[mantle, plate tectonics, primary atmosphere, secondary atmosphere, greenhouse effect]
Moon
a planet-like companion to Earth made of the Earth’s ocean crust
[albedo, anorthosite, breccia, ejecta, maria, micrometeorite, large-impact hypothesis, magma ocean, multiringed basins, late heavy bombardment]
Mercury
a metal planet, cooling and shrinking against the cold of space, smallest planet in solar system
[fast, very dense, inactive]
Venus
initially a water planet, clouding over and heating which boiled off its water so its now dry
[runaway greenhouse effect, coronae]
Mars
small water planet unable to hold its atmosphere which boiled away water making a cold desert
[shield volcano, outflow channel, valley network, permafrost, moons]
Jupiter
massive, largest planet in solar system, ball of liquid metallic hydrogen, extensive moon system, sidereal rotation period 10 hours, spins the fastest of all planets
[oblate, liquid metallic hydrogen, magnetosphere, belt-zone circulation, forward scattering, Roche limit, tidal heating]
Saturn
massive, visibly bright ice-particle ring, ball of liquid metallic hydrogen, extensive moon system
[ring system, shepherd satellite, gap, Titan, liquid methane/ethane, Enceladus, tiger stripe]
Uranus
ice giant, rich in solid and liquid water, rotation inclined to ecliptic about 98º
[trace methane, occulation, moon with ovoids]
Neptune
ice giant, rich in solid and liquid water, rings NOT easily detactable from Earth, satellite system, 2 discovered from Earth, 6 by Voyager 2 (1989),
Great Dark Spot (dark blue) roughly the size of Earth, circulating hurricane
Plutino, Pluto
a dwarf planet (IAU defines ‘planet’ as gravitationally spherical, dominate orbit, bound to star)
[dwarf planet]
Terrestrial planets
Earth-like, small diameter, dense (of rock or metal), rocky, little or no atmosphere
[crater, asteroid, meteoroid (meteor, meteorite), meteor shower, carbonaceous chondrite, volatile, half-life]
Jovian Planets
“liquid” giants (compressed gas), worlds of the outer solar system (resemble Jupiter)
[comet, Kuiper Belt, Oort Cloud]
solar nebula theory
rotating cloud of gas/dust gravitationally collapse and flatten, around forming Sun disk rotates counter clockwise, all planets revolve in the same direction, rotate as well
[uncompressed density, ice line, condensation, condensation sequence, accretion, planetesimal, protoplanet, gravitational collapse, heat of formation, differentiation, outgassing, Late Heavy Bombardment, Near Earth Objects (NEO)]
evolutionary theory
phenomenon involving slow, steady, process of sort seen happening present day
catastrophic theory
phenomenon involving special, sudden, perhaps violent events
comparative planetology
comparison of one planet with another, Earth as the template
active core (Earth)
refers to geologically mobile, as heat stirs and makes its way out of the interior
mantle (Earth)
deep layer - Earth’s dense rock, properties of solid but capable of flowing slowly (like asphalt)
crust (Earth)
rocky low-density surface, radiates heat out into space
smooth surface is younger (lava flow) than cratered area (Late Heavy Bombardment)
plate tectonics (Earth)
crust plates floating on mantle (Greek for “builder”)
100s M.y. movement (0.1 G.y.) 1/45 age of Earth, so sections of crust in rapid motion
atmosphere (Earth)
larger size and cooler temperature of planet important to retaining gases
gases originate from formation, space deliveries, evolution of the planet, appearance of life
primary atmosphere (Earth)
planet’s first atmosphere, gases from solar system nebula (hydrogen, methane) outgassing of carbon dioxide, nitrogen, water vapour, etc., cooked-out of hot planet rock
accreting planetesimals rich volatile materials (water, ammonia, carbon dioxide, etc.)
secondary atmosphere (Earth)
replaces the primary atmosphere, e.g., outgassing, impactors, bioactivity
Earth’s relatively thin, mainly nitrogen, significant oxygen from biologucal processes
greenhouse effect (Earth)
carbon dioxide (CO2) rich atmosphere traps heat and raises planet surface temp. visible wavelength sunlight shines through glass roof of greenhouse, heats interior without greenhouse effect Earth would be 30ºC cooler, average temp. below freezing human action that add CO2, water, and gases, being researched for forcing of current climate