Chapter 10 Flashcards

(11 cards)

1
Q

How did earth form? And When?

A

Earth formed from accretion of solid materials that condensed out of the solar nebula soon after the Sun itself formed.

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2
Q

What’s the age of Earth?

A

4.55 billion years

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3
Q

How did Earth Core form?

A

Earth’s core probably formed as the Earth itself was forming as a result of heating and stirring by large impacts.

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4
Q

When did Jupiter form?

A

The giant planet Jupiter formed early during planetary accretion.

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5
Q

What did Jupiter help create?

A

Jupiter helped create the asteroid belt by preventing a planet from forming there.

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6
Q

How does Juipter affect Earth?

A

Jupiter’s gravity perturbs asteroids from the belt, putting some of them on Earth-crossing orbits and thereby causing mass extinctions like the one that killed of the dinosaurs 65 million years ago.

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7
Q

How did the moon forn?

A

The Moon is thought to have formed from a glancing impact by a Mars-sized planetesimal and hence is something of a cosmetic accident.

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8
Q

What does the moon do to Earth?

A

The moon stabilizes Earth’s obliquity, that is, the variation in the tilt of its spin axis. Without it, Earth’s obliquity would vary chaotically from 0º to 85º, making our planet much less habitable.

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9
Q

What does a moon not Always imply?

A

This doesn’t however imply that a planet must have a large moon to have a stable obliquity. Whether or not a planet’s obliquity is stable depends on relationships between the planet’s spin rate and the orbits of other planets in the system.

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10
Q

How did Earth’s atmosphere and ocean form?

A

Earth’s atmosphere and ocean formed along with the planet from impact degassing of incoming planetesimals and from volcanic outgassing. The resulting atmosphere was probably rich in N2 And CO2 but contained little O2 prior to the origin of life and the evolution of photosynthesis.

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11
Q

Why is Earth’s mantle relatively oxidizing?

A

Earth’s mantle is relatively oxidizing because of chemical reactions that occurred at great depths during accretion. Ferrous iron disproportionates to ferric iron plus metallic iron. The metallic iron sank to join the core, while the ferric iron remained in the mantle.

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