Physical Geology: Chapter 1&23 (introduction to geology & earths companions) Flashcards

1
Q

geology

A

is a science that studies the origin and evolution of Earth and solar system bodies

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2
Q

geocentric model

A

model that places Earth at the center of the solar system

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3
Q

heliocentric model

A

model that places the Sun at the center of the solar system

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4
Q

differentiation

A
  • the process through which the Earth transformed into a different planet with a zoned interior (the crust, the mantle, and the core)
  • partial melting or complete melting of earth allowed heavier more dense minerals and elements like: iron (Fe) & nickel (Ni) to sink to down a produce the core; also allowed the reverse, lighter less dense minerals and elements like: silicates, and plagioclase feldspar
  • the energy to partially/completely melt the earth came from:
    1) impacts; and 2) radioactive decay
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5
Q

The Core

A
  • inner most zone of the Earth
  • gravity, seismic, and geochemical data strongly suggest its mostly made up of iron
  • core molten on outside (ouster-core) and solid on the inside (inner-core) where the pressures are highest (5200 to 6400 km in depth)
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6
Q

The Mantle

A
  • is material in the middle zone
  • makes up the bulk of solid earth
  • seismic and geochemical data strongly suggest is has an intermediate density and is formed mostly of compounds of O2 with Mg, Fe, and Si
  • about 40 to 2900km in depth
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7
Q

The Crust

A
  • materials that floated toward the surface of magma ocean formed Earths solid crust
  • thin outer layer up to about 40 + Km thick
  • contains relatively light materials with low melting temperatures
  • most easily melted compounds are Si, Al, Fe, Ca, Mg, Na, and k
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8
Q

Earth has two heat engines

A
  • internal: (comes from the initial formation of Earth and form radioactivity)
  • external: (comes from sun a.k.a. solar energy)
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9
Q

Internal Energy

A
  • drives volcanism and other interior processes
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10
Q

External Heat

A
  • energizes the atmosphere and oceans which are responsible for climate and weather
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11
Q

Earths surface: 1) the continents

A
  • its not clear what caused the initial formation of the continents; hypothesis :
    1) repeated melting and solidification of initial cooled surface: allowed lighter elements to become separated form heavier ones and float to surface
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12
Q

2) oceans and atmosphere

A
  • origin traceable to water and gases that boiled off during initial heating/ differentiation of earth (water, H, N, C initially bound in minerals , then freed by partial melting, carried to surface by magmas and then released through volcanic activity)
  • gases released from volcanos in early Earth history are believed to have been the same as those released today in modern volcanoes
  • today the atmosphere is mostly made up of N and O, but O apparently only persisted in atmosphere after photosynthetic algae developed and began releasing substantial O was a waste product
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13
Q

Earth is composed of a system of interacting components

A

1) heat from interior drives mantle convection
2) solar energy drives most of biosphere and atmosphere
3) interactions between atmosphere, hydrosphere, biosphere, geosphere

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14
Q

Lithosphere

A
  • (crust and upper mantle): strong, solid, outermost shell; 100-200 Km thick; cool and brittle with roughly a dozen of plates
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15
Q

Asthenosphere

A
  • weak layer upon which lithosphere rides; weak because its almost at melting point; 100 to 200 Km thick and can also flow
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16
Q

Earths age

A
  • about 4.5 billion years old