as101 lesson 8

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Last updated 1:13 AM on 4/21/26
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30 Terms

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Sources of universe’s first elements

Big Bang produced mostly hydrogen, helium, and a little lithium

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Sources of heavier elements

Made in stars and spread when stars die

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Galactic recycling

Old stars eject heavy elements that become part of new stars and planets

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Trigger for solar system formation

Probably shock wave from nearby nova or supernova

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Solar nebular theory

Solar system formed from collapsing cloud of gas and dust

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Three main nebular processes

Heating, spinning faster, flattening into disk

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Why nebula heated up

Infalling material gained kinetic energy as it collapsed

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Why nebula spun faster

Conservation of angular momentum

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Why nebula flattened into disk

Natural result of rotation during collapse

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Nebular theory explains

Planets orbit in same direction, same plane, and mostly circular orbits

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Temperature gradient

Inner nebula hotter, outer nebula cooler

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Why inner planets became terrestrial

Only rock and metal could condense close to Sun

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Why outer planets became jovian

Beyond frost line ices could condense and build massive cores

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Frost line (ice line)

Distance from Sun beyond which water and other volatiles could freeze

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Planetesimal

Kilometre-sized building block of planets

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How planetesimals formed

Condensation + accretion of small particles

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Condensation

Atoms/molecules added to growing grains

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Accretion

Small solid particles stuck together to make larger bodies

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Inner planetesimals composition

Mostly rock and metal

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Outer planetesimals composition

Rock, metal, and lots of ice

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Asteroids

Rocky/metallic leftover planetesimals

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Comets

Icy leftover planetesimals with dust and rock

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Solar wind

Stream of charged particles from young Sun

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Effect of solar wind

Blew out leftover gas and dust from solar system

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Why jovian planets grew larger

Ice-rich cores formed beyond frost line and captured lots of gas

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Why terrestrial planets stayed smaller

Only rock/metal available in hot inner solar system

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Heavy bombardment

Leftover debris kept striking planets early in solar system history

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Kuiper Belt

Region beyond Neptune holding many icy bodies/comets

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Oort Cloud

Distant spherical reservoir of comets

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Nebular theory best fits solar system because

Explains major solar system features better than rival ide