Tectonics Flashcards

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1
Q

What are the characteristics of an oceanic plate?

A
  • Between 5-8km thick
  • Deep beneath the oceans
  • Less than 200mln years old
  • Consists mainly of of dense/heavy rock (basalt)
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2
Q

What are the characteristics of a continental plate?

A
  • Between 30-70km thick
  • Beneath the earths continental land masses and under shallow seas
  • As old as 4bln years
  • Consists of less dense/lighter rock (granite)
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3
Q

What is a convergent plate margin?

A
  • Two plates moving away from each other
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4
Q

What is a divergent plate margin?

A
  • Two plates moving towards each other
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5
Q

What is a conservative plate margin?

A
  • Two plates moving in different directions at different speeds
  • Two plates moving in the same direction at different speeds
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6
Q

What processes influence plate movement?

A
  • Slab pull
  • Ridge push
  • Convection currents
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7
Q

What is slab pull?

A
  • Tectonic plate movement
  • Subduction of the plate at oceanic trenches into the mantle
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8
Q

What is ridge push?

A
  • Magma rising pushes the ocean floor upwards
  • Earth’s gravitational pull causes the crust to sink away from the ridge, causing it to cool and become more dense
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9
Q

What do divergent plate margins create with continental plates?

A
  • Rift Valleys
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10
Q

What are convection currents?

A
  • Movement of warm mantle magma
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11
Q

What is a hotspot?

A
  • Mantle plume of rising magma
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12
Q

What is a hazard profile?

A
  • Compares the physical processes of hazards
  • Magnitude, duration, speed at onset, spatial predictability, frequency and areal extent
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13
Q

What is the Mercalli scale?

A
  • Measures the effect of an earthquake through observable, subjective data
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14
Q

What is the Richter scale?

A
  • Quantitive measure of an earthquake’s magnitude
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15
Q

What is the VEI?

A
  • Volcanic explosivity index
  • Describes size of explosive volcanic eruptions based on intensity and magnitude
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16
Q

What are the qualities of basaltic lava?

A
  • Low in silica content - low viscosity
  • Fluid magma
  • Effusive eruptions
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17
Q

What type of volcano does basaltic lava come from?

A
  • Shield volcano
18
Q

What are the qualities of andesitic lava?

A
  • High in silica content - high viscosity
  • Solidifies on the way up to the surface
  • Very explosive due to trapped gas
19
Q

What type of lava does cinder cone and composite volcanoes produce?

A
  • Andesitic lava
20
Q

What are the characteristics of a composite volcano?

A
  • Associated with subduction at convergent plate boundaries
  • Slopes ranging up to 30 degrees
  • Consists of many layers of ash, lava, tephra, pumice
  • Violently explosive eruptions
21
Q

What are the characteristics of a shield volcano?

A
  • Effusive eruptions
  • Associated with mantle plumes
  • Built almost entirely of fluid lava flows
  • Gentle slopes of 2-10 degrees
22
Q

What are the characteristics of a cinder cone?

A
  • Generally explosive
  • Steep conical hill of tephra
  • Commonly found on the side of a volcano
  • Most are monogenetic
  • Mostly <200m high
  • Very little strength
23
Q

What are primary volcanic hazards?

A
  • Lava
  • Pyroclastic flows
  • Tephra
  • Volcanic gases
24
Q

What are secondary volcanic hazards?

A
  • Lahars
  • Jokulhaulps
25
Q

What is a P wave?

A
  • The fastest seismic wave
  • Can move through solids, liquids, and gases
  • Oscillate ground back and forth in direction of travel
26
Q

What is a S wave?

A
  • Shake the ground in a shearing motion, perpendicular to the direction of travel
  • Can travel through solids
27
Q

What is soil liquefaction?

A
  • Water saturated material can temporarily behave as a liquid
28
Q

What are landslides?

A
  • When material on a (near) vertical surface falls
29
Q

How deep is a deep focus?

A

300km - 700km

30
Q

How deep is an intermediate focus?

A

70km - 300km

31
Q

How deep is a shallow focus?

A

0km - 70km

32
Q

What is the disaster risk equation?

A
  • R = H x V / C
  • R = risk
  • H = hazard frequency
  • V = vulnerability
  • C = coping capacity
33
Q

What are the root causes of vulnerability?

A
  • Limited access to power, resources, structures
  • Political and economic systems
34
Q

What are the dynamic pressures of vulnerability?

A
  • Lack of training, local investment, press freedom
  • Deforestation
  • Rapid population change
  • Rapid urbanisation
35
Q

What are unsafe conditions for vulnerability?

A
  • Local economy
  • Physical environment
  • Social relations
  • Public actions
36
Q

How can you modify vulnerability and resilience?

A
  • Predictions and warnings
  • Community preparedness
  • Land use planning
37
Q

How can you modify the loss?

A
  • Accepting that hazards will occur
  • Responding to the loss via aid or insurance
38
Q

How can you modify the event?

A
  • Hazard prevention
  • Hazard resistant design
39
Q

What are some examples of hazard prevention?

A
  • Lubricate fault lines
  • Divert lava away
40
Q

What are some examples of hazard resistant design?

A
  • Cross bracing
  • Shear walls
  • Counter weights
  • Shock absorbers/base isolators
41
Q

What are the limitations of designing earthquake resistant infrastructure?

A
  • Difficult/unable to test infrastructure
  • Technology is rapidly developing and things can become out of date quickly
  • People living in low development countries can’t afford to build earthquake resistant infrastructures
42
Q

What are the limitations of strengthening existing structures to be more earthquake resistant?

A
  • Seismic retrofitting is not as strong as new earthquake resistant infrastructure