plate tectonics Flashcards

1
Q

crust

A
  • outer layer
  • thick
  • 5-50 km thick
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2
Q

mantle

A
  • 2900km thick
  • upper sections solid and part of lithosphere
  • asthenosphere > movement in the asthenosphere causes plates to move
  • lower mantle = solid due to density
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3
Q

outer core

A
  • provided heat
  • solid, iron, nickel
  • 2400km thick
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4
Q

inner core

A
  • solid, iron, nickel

- very hot, 2400km thick

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5
Q

features of continental crust

A
  • 35 to 70 km thick
  • very old, 1500 million yrs
  • light, less dense
  • light in colour, granite
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6
Q

features of oceanic crust

A
  • 6 to 10km thick
  • young, less than 200 million yrs
  • heavier, more dense
  • dark, crystals are very small, basalt
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7
Q

types of boundaries

A
  • convergent = can be two oceans or two continental plates as well as one oceanic and one continental
  • divergent
  • transform
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8
Q

divergent plate boundary - names

A

North American and eurasian plates

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9
Q

features of divergent boundary

A
  • mid ocean ridge
  • shield volcanoes (lave, basic runny)
  • transform faults
  • rift valleys
  • earthquakes
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10
Q

convergent boundary - names

A

Nazca and South American plates

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11
Q

features of convergent boundary

A
  • earthquakes
  • fold mountains
  • acid lava cones
  • deep ocean trenches
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12
Q

transform boundary - names

A

pacific and North American plates

- san Andreas fault

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13
Q

features of transform boundary

A
  • earthquakes

- transform faults

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14
Q

epicentre

A

the point on the ground surface directly above the focus.

This is where most of the damage happens

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15
Q

focus

A
  • the point in the crust where the movement actually takes place
  • the most damaging quakes are those where the focus is shallow i.e. near the surface
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16
Q

p - waves

A
  • Arrive first, spread outwards on all sides from the focus of the quake
  • they compress and stretch the material they move through
  • travel quickly, hear them as a boom
17
Q

s - waves

A
  • Come later and shift the materials up and down causing major damage
  • only travel through solids but can cause liquefaction of the soil
  • liquefaction can cause major landslides
18
Q

surface waves

A
  • Travel along the Earth’s surface, arrived last
  • can be most destructive
  • travels slow
19
Q

fault strike

A
  • Fracture in the rocks of earth’s crust in which rock masses slip past one another parallel to the strike
  • due to the movement of two plates against one another and the release of built up strain
20
Q

fault plane

A
  • the line of opening that takes place from the focal point, along which the crustal rock may slide
21
Q

Richter scale

A
  • quantifies the strength of the earthquake (the amount of energy released). it uses a logarithmic scale
22
Q

moment magnitude scale

A
  • more accurate

- gives an estimate of the total energy released by an earthquake

23
Q

mercalli scale

A
  • measures the intensity of an earthquake

- bases its measurements on the observed effects of the earthquake and describes its intensity

24
Q

faulting

A
  • where part of the crustal rock layers crack and break, opening and moving in different directions
  • Direction of movement depends on the type of pressure under which the rocks are placed
25
Q

landslides and earthquakes

A
  • a landslide is the movement of rock, debris or earth down a slope. They result in failure of the materials which make up the Hill slope and are driven by the force of gravity
  • earthquakes are often one of the major natural causes of landslides. The sudden movement of the crustal rocks or the shock waves that follow can trigger the movement of loose material down steep slopes