EARTHQUAKES Flashcards

1
Q
  • Earthquake:
A

the ground shaking cases by stresses released in Earth

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2
Q

o Factors that determine destructiveness

A

 Location, magnitude, depth, distance from epicenter, secondary effects, architecture

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3
Q

EQ stresses

A

seismic waves (kinetic energy), displacements along the fault (kinetic energy), heat and other energy

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4
Q

megathrust EQs

A

plate boundary EQ
up to M9 occurs every 200-800 years
causes large tsunamis

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5
Q
  • Understand why most earthquakes IN Canada occur on the west coast
A

o Subduction zone at a convergent Boudry
 North America plate w/ Juan de Fuca plate and pacific plate
 North American plate EQs
* Large damage potential  closer to surface =more shaking
 Juan de Fuca plate EQs
* Deeper and very frequent

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6
Q

o Quantitative 1-10

A

measures magnitude
richter scale
moment magnitude scale

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7
Q

 Richter’s scale

A

based on aptitude of seismic waves, which is related to energy released
* Not really used by geologists, despite being well known

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8
Q

 Moment magnitude scale:

A

is based on the amount of fault slippage produces, the size of surface area that ruptured, and the nature of the materials that faulted, which is more accurate than Richter’s scale

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9
Q

qualitative

A

1-12 intensity
 Modifies Mercalli scale

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10
Q

 Modifies Mercalli scale

A

what we feel
* 1: felt by very few
* ~5: general panic
* 12: total destruction

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11
Q

o Magnitude

A

 Characterizes an EQs relative size
 Each whole number represents a tenfold increase in the measured amplitude and 32 times more energy release

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12
Q
  • Use plate tectonics to predict where earthquakes occur, and how earthquake depth and magnitude is ties to different types of plate tectonic boundaries.
A

o Materials respond differently (strain) to stress. Brittle deformation leads to an earthquakes
o Deep focus at convergent boundaries
o Intermediate focus at transform boundaries?
o Shallow focus at divergent boundaries

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13
Q

o Subduction zone earthquakes (convergent boundaries)

A

 Largest possible earthquakes/ deep focus (meteorite impacts can be larger)
 Convergent boundaries
 Type of stress here: compression
 Type of faults: reverse (or thrust)
 Three locations of earthquakes
* #1: subduction interface earthquakes.
o Can be huge @ M9.4) megathrust EQs
* #2 EQs in the subducting or overriding plate
o Moderate size, largest = ~M7
* #3 Benioff earthquakes
o Very deeps: 100s of km)
o Little/ no damages at surface
o Deeper focus as moved down the Benioff zone
 Megathrust rupture zone located on the coast of Vancouver island
* 12-30 minutes from EQ till initial tsunami waves arrive
* Last one: jan 26 1700 @ M9 (records in Japan and first nations(oral) )

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14
Q

o Continent- continent convergent Eq zones

A

 Very large (not as large as subduction) up to ~M8
 Convergent boundaries
 Type of stress: compression
 Type of fault: reverse (or thrust)
 India= thrust fault

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15
Q

o Divergent EQ zones

A

 Small to moderate EQs usually less than M5
 Most are underwater
 Type of stress: tension/extension
 Type of fault: normal
 Ex: east African rift, mid Atlantic ridge
* Rift valley forms

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16
Q

o Transform boundaries

A

 Oceanic (majority) very small Eqs
 Continental- shallow mostly small earthquakes, some larger usually up to M6 or M7
 Type of stress: shear
 Type of fault: strike-slip
 Ex: San Andreas fault, Queen Charlotte fault

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17
Q

o Body waves

A

 P- wave (primary/ pressure)
* Particles move parallel to the direction wave propagates
* Can travel through all matter
* Is the fastest
 S- waves ( shear/ secondary)
* Particles move perpendicular to direction wave propagates

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18
Q

surface waves

A

 Rayleigh wave: vertical and horizontal motion parallel to wave travel direction (like ocean wave)
 Can travel through all matter

19
Q

o Seismograph: the basic idea

A

 Mass suspended by a spring
 Seismograph moves, the mass does not
 Motion causes pen to move

20
Q

EQ detectors

A

 P waves arrive first
* Twice as fast as the others
* Over 300km (our distance from the subduction zone)
* P waves will take 60 sec to arrive
* Surface waves will take 100 sec to arrive
* If we can detect p waves, we have enough time to “take shelter”

21
Q

o Seismograph readings

A

 Three seismographs gives us triangulation
 The earthquake epicenter is where the three circles meet

22
Q

o EQ forecasting

A

 Scientists cannot yet predict EQs due to the complicated nature of subsurface stress and strain
* They use probability

23
Q

 Long-term forecasts

A

(10- few thousand years)

24
Q

 Medium range predictions

A

(few years to a few months)

25
Q

 Short range predictions

A

(few days or hours)

26
Q

paleoseismology

A

uses past earthquake data to predict future occurrences
o Areas which are overdue for an earthquake are in a seismic gap and have built up strain

27
Q
  • Paleo earthquakes:
A

rock records also show past EQs through disrupted sediment layering
o The faults

28
Q

o Measurements

A

(tiltmeters and radon detectors)

29
Q

 Measure dilatancy

A

increase in volume due to built up stress in a rock

30
Q

 Tiltmeters:

A

measures tilting and swelling (dilatancy) of rocks

31
Q

 Seismographs: BC has 30, 200 all over Canada

A

japan more than 4000

32
Q

 How we perceive earthquakes depends

A
  • Magnitude
  • Foundation (ground) material
  • Duration
  • Building construction
    o In general
     Brick and concrete- bad
     Wood, steal, and reinforces concrete – good
33
Q

5 EQ hazard types

A

ground shaking
liquefaction
fire
tsunami
landslides

34
Q

landslides

A

 very common after EQs
 Usually, people blame these deaths on the EQs not the landslide but
 Very common in BC and mountains around the world
 After EQs landslides can increase for up to 10 years

35
Q

tsunami

A

 Can be caused by vertical motion of tectonic plates (or landslide, or meteorites, or volcanoes)

36
Q

fire

A

 Shaking breaks gas and electrical lines (often at the same place)
 Van- secondary fire hydrant system- connected to ocean incase mountain connection fails

37
Q

liquefaction

A

 Shaking causes wet loose (unconsolidated) soils to liquify (act like a liquid)
 Ground loses cohesion and flows
 Bad for buildings
 Richmond and delta are at major risk to liquification since the ground is mostly loose sediments

38
Q

o Ground shaking

A

 Buildings may fall down
 Most deaths and injuries in EQs are from building collapse
 Bedrock is much more stable than sediments
 Building materials
* Wood is better than brick since it is flexible
* Building codes need to meet seismic standards in EQ prone areas

39
Q

o Interplate

A

EQs between two plates, initialed near plate boundaries

40
Q

o Intraplate

A

EQs that are large and damaging, located within a single plate, and can occur far from plate boundaries

41
Q

short term predictions

A

o Chinese scientists made the first successful prediction of major EQ in 1975 based on foreshocks: M7.5 haicheng earthquake
o Other precursory phenomena include pre-seismic deformation of the ground surface, emission of radon gas seismic gaps along faults, and anomalous animal behaviour

42
Q
  • EQ planning
A

o Development o hazard-reduction programs
o Engineering and land-use adjustments to earthquake activity
o Development of a warning system

43
Q
A