Geoscience Flashcards

1
Q

Layers of the Earth’s interior

A

Crust
Mantle
Outer core
Inner core

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2
Q

Plate tectonics

A

Aka the geological Grand Unifying Theory

  • describes how plates and continents contained by them are pushed and pulled around the surface of the earth
  • explains processes that build mountains
  • explains patterns of distribution of earthquakes and volcanoes
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3
Q

Three types of tectonic plate boundaries

A

Convergent (colliding)
Divergent (spreading)
Transform (sliding)

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4
Q

Convergent boundary outputs

A

Oceanic-oceanic
- volcanic island chains

Continental-oceanic
- mountain ranges along edge of continent
- oceanic plate is always subducted below (oceanic crust is denser)

Continental-continental
- mountain ranges

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5
Q

Rocks

A

Naturally occuring aggregates of minerals

*manmade objects are never considered rocks or minerals

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6
Q

Mineral

A

A naturally occuring homogenous solid with a definite (but generally not fixed) chemical composition and a crystalline structure

Formed by inorganic processes

*manmade objects are never considered rocks or minerals

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7
Q

Gemstone

A

A valuable mineral that originated from an original source rock

Exceptions
- broadly, any mineral highly valued for its beauty, durability, and rarity
- can include non-minerals (organic or biological origin), eg. pearl, amber
- can include some rocks

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8
Q

Relationship between rocks, minerals, and gemstones

A

Rocks = aggregates of minerals
Gems = highly valued minerals (and some non-mineral materials)

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9
Q

Igneous rock

A

Crystallizes when molten material (melt/magma) cools

  • rock is composed of interlocking crystals
  • can be volcanic/extrusive or plutonic/intrusive
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10
Q

Volcanic/extrusive rock

A

Rock formed from melt cooling at the surface of the Earth

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11
Q

Plutonic/intrusive rock

A

Rock formed from melt cooling and solidifying inside the Earth

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12
Q

Metamorphic rock

A

Formed by the alteration of pre-existing rocks

Rock transformation involves heat and/or pressure, and often fluid percolating through subsurface; does not involve melting

  • compression can generate heat
  • compression often results from plate collision
  • pressure and temperature increases with depth
  • newly generated minerals may be more stable at new temperature/pressure conditions
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13
Q

Sedimentary rock

A

Physical - erosion
- weathering forms clastic sedimentary rock (eg sandstone, siltstone, mudstone –> fragments and grains of eroded rock)

Chemical - precipitation
- evaporite formed when body of water evaporates to form layers of salt

Biological - precipitation
- production of coral reefs, sediments composed of shells, and deposition of plant material in swamps (forms coal)

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14
Q

Diagenesis/lithification

A

Processes that physically cements sedimentary grains together

Involves heat, pressure, and percolating fluids (like metamorphism), but not to the extent of drastic transformation of mineralogy or structure

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15
Q

Rock cycle

A

Rock in mantle –> magma

Magma –> igneous rock (solidification)

Igneous rock –> metamorphic rock -or- sediment (weathering and erosion)

Metamorphic rock –> sediment -or- magma (partial melting)

Sediment –> sedimentary rock (lithification)

Sedimentary rock –> sediment -or- metamorphic rock (metamorphism)

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16
Q

The Earth system

A

Atmosphere and oceans
Biosphere
Lithosphere
- crust (rigid)
- upper mantle (ductile)
- lower mantle (ductile)
Core (mantle boundary)
- fluid outer core
- solid inner core

17
Q

Lithosphere

A

Rigid layer composed of the crust and uppermost part of mantle

  • contains tectonic plates
18
Q

Asthenosphere

A

Upper mantle just below lithosphere

  • soft, lubricating layer over which tectonic plates move