Lecture 2 Flashcards

1
Q

What spheres are within the atmosphere

A

T.M.S.T: Thor Must Save Thor

Thermosphere, Mesosphere, Stratosphere, Troposphere

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2
Q

What spheres are within the Hydrosphere

A

C.H.B: Chris Hates Blue

Cryosphere, Hydrosphere, Biosphere

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3
Q

What spheres are within the Geosphere

A

L.A.M.C: L.A. mostly cracks

Lithosphere, asthenosphere, mesosphere, core

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4
Q

What parts of the geosphere affects the biosphere

A

Lithosphere and Astehnosphere

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5
Q

The crust is part of what geosphere?

A

Lithosphere

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6
Q

Lithosphere vs. Asthenosphere. How do they affect the biosphere

A

Lithosphere:

  • solid and rigid
  • because it’s rigid, it’s easy to break creating physical changes on the biosphere

Asthenosphere:

  • solid, but mobile
  • because it’s mobile, it affects the surface.
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7
Q

Explain this double oxymoron: “The Earth’s materials are fixed into changing processes that are in a state of dynamic equilibrium”

A

1st:
- Earth’s materials change by following a natural law

2nd:
- dynamic equilibrium means that materials are actively changing, however, there is a balance that is being maintained (i.e. water cycle)

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8
Q

Explain the water cycle

A
  • physical change
  • evaporation —> condensation —> precipitation —> surface runoff
  • perfect example of dynamic equilibrium
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9
Q

What are the differences between the two types of Igneous rocks?

A
  1. Basalt
    - Fe
    - extrusive
    • magma is crystalized outside
  2. Granite
    - Si
    - intrusive
    • magma is crystalized inside
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10
Q

Explain the creation of igneous rocks

A

Magma —> crystallization (cools + solidifies)

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11
Q

Explain the creation of sedimentary rocks

A

Weathering breaks down rock —> sediment —> lithification (sediment is compacted + cemented)

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12
Q

Explain the creation of metamorphic rocks

A

Heat and pressure

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13
Q

Density formula

A

D = Mass / Volume

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14
Q

Velocity formula

A

V = Distance / Time

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15
Q

What are Convection Cells

A

Redistribution of heat because of density differences due to temperature

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16
Q

Continental crust vs. oceanic crust

A

Continental:
- lesser density because of granite which contains Si (light element)

Oceanic crust
- More dense because of basalt which contains Fe (heavy element)

17
Q

Explain how density can change by temperature

A

Density has an inverse relationship with volume

Hot = expand = volume increase = lower density 
Cold = contraction = volume decrease = higher density
18
Q

Define plates

A

Pieces of lithosphere moving as a coherent mass

19
Q

Characteristics of divergent margins. Continental and oceanic.

A
  • asthenosphere rising
  • constructive
  • In continental…
    • creates rift-valley on the lithosphere
  • In mid-oceanic ridges…
    • oceanic crust on lithosphere
20
Q

Characteristics of convergent margins

A
  • asthenosphere sinking
  • destructive
  • Trench (oceanic)
  • volcanic island arc/chain
  • mountain chains (cont. + cont. collision)
  • earthquakes
21
Q

Characteristics of transform fault

A
  • plates sliding past one another horizontally
  • pieces of continents slices off (San Andres fault)
  • off-set on Mid-oceanic ridge
22
Q

Three plates that border “North American Plate”

A
  • Caribbean Plate
  • Pacific Plate
  • Eurasian Plate