Chapter 2- Center If The Earth Flashcards

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1
Q

Mars earth Venus and Mercury

A

Terrestrial planets

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2
Q

Saturn and Jupiter

A

Gas giant planets

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3
Q

Neptune and Uranus

A

Outer ice giant planets

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4
Q

Asteroids

A

Small bodies of rock or metal orbiting the sun.
Planetesimals that were never part of a larger planet
Most occur between Jupiter and mad

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5
Q

Comets

A

Icy planetesimals that orbit the sun.
When approaching the sun they develop a long coma (tail)
Tail= comprised of evaporating gas and dust and points away from sun

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6
Q

Dirty snowballs

A

H20 CO2 CH4 NH3
Other volatiles
Organic compounds
Dust

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7
Q

Our atmosphere

A

Mostly N2 and O2.

  • other gases argon, carbon dioxide, neon
  • less common hades ( helium, methane and krypton
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8
Q

Atmospheric layers

A

Troposphere - the lower mixing layer, weather is confined to this layer, temperature decreases upward
Stratosphere- no mixing occurs temp increases upward. Ozone area
Mesosphere- temp decreases upward
Thermosphere- outermost layer, temp increase upward farthest from earth

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9
Q

Earth is comprised of

A

Iron- 32.1%
Oxygen- 30.1%
Silicon- 15.1%
Magnesium- 13.9%

91.2%

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10
Q

Organic compounds

A

Carbon- containing compounds
Most are residue from once living creatures
These include wood, pear, liginite, coal and oil.

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11
Q

Earth minerals

A

Crystal- a single coherent mineral with geometric structure
Grain- an irregularly shaped fragment of a larger Crystal
Minerals- comprise rocks and therefore most of the earth

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12
Q

Glasses

A

Non crystalline soldiers

Rapid cooling- too fast for Crystal growth.

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13
Q

Rocks

A

Aggregates of minerals, grains and/or glass

  • igneous- cooked from a liquid (melt).
  • sedimentary- debris cemented from preexisting Rock grains
  • metamorphic- rock altered by pressure and temperature
  • rocks may be made of a single mineral
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14
Q

Volatiles

A

Materials that turn into gas at the surface. H2O CO2 CH4 and SO2

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15
Q

There are four fundamental silicate igneous rock types

A

Vary by silica (SiO4) to iron and magnesium.

  1. Felsic- Si rich poor in Fe and Mg, granite: Felsic rock with large grains
  2. Intermediate
  3. Mafic- Si poor but Fe and Mg rich, gabbro large grains and basalt small grains
  4. Ultramafic mostly Fe and mg ex: peridotite: small grains
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16
Q

Earth layers

A

Crust, |upper, transitional and lower mantle | liquid outer and solid inner cores

17
Q

The crust

A
  • thickest under mountain ranges thinnest under mid ocean ridges.
  • continental crust: Felsic, granitic, low Fe-Mg, to intermediate in composition.
  • oceanic crust: Mafic basalt and gabbro, high in Fe and mg.
  • overlain by sediments
18
Q

The mantle

A
  • upper, transitional and lower
  • Ultramafic rock peridotite
  • solid rock, 2,885 km thick 82% of earths volume
  • convection aids tectonic plate motion, lava lamp
19
Q

The core

A

-Iron rich sphere with a radius of 3,471 km.
-Outer core is liquid iron nickel and sulfur
- inner circle is solid iron nickel alloy
-

20
Q

Lithosphere

A

The outermost 100-150 km of earth

  • behaves rigidly as a no flowing material
  • compromised of two components: crust and upper mantle
  • this is what the tectonic plates are made of
21
Q

Asthenosphere

A
  • upper mantle below the lithosphere
  • shallow under oceanic lithosphere; deeper under continental
  • flows as a “soft” solid (ductile, malleable, capable of being easily deformed)
22
Q

One AU

A

Astronomical unit, the distance between the earth and the sun 93 million miles