Seismicity Flashcards

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1
Q

What is the definition of an earthquake

A
  • when there is a slow build up of stress within the rocks, there is a sudden release where parts of the surface experience an intense shaking motion that lasts between a few seconds and a few minutes
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2
Q

What is the focus

A
  • the point within the crust where the pressure release occurs
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3
Q

What are the different depths that the focus can be located at

A
  • shallow: 0-70km deep- greatest damage
  • intermediate: 70-300km
  • deep: 300-700km
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4
Q

What are fault lines

A
  • cracks in the earth which are small
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5
Q

What are seismic waves

A
  • parts of the crust are forced to move in opposite directions
  • huge masses get stuck but the force of them continues
  • building up stress
  • strain overcomes friction and the rocks move
  • releasing large amounts of energy
  • energy is transferred to surrounding rocks travelling through Them as seismic waves
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6
Q

Seismic shock waves characteristics

A
  • highest level of energy at the focus

- energy decreases as the waves spread outwards

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7
Q

What is the epicentre

A
  • the place on the earths surface immediately above the focus
  • receives highest amount of energy
  • potentially hazardous location
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8
Q

How are seismic waves measured

A
  • seismometer

- tell us the internal structure of the earth

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9
Q

What are the three main types of seismic waves

A
  • primary
  • secondary
  • surface
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10
Q

What are primary seismic waves

A
  • fastest and move earth backwards and forwards

- travel better in liquids and solids

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11
Q

What are secondary seismic waves

A
  • travel half the speed of p waves
  • move sideways
  • shake the earth at right angles to the direction of travel
  • cannot move through liquids
  • do more damage than p waves
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12
Q

What are surface waves

A
  • travel the slowest
  • nearest to the ground
  • most destructive
  • love waves- make the ground move up and down
  • Raleigh waves- complex rolling motion
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13
Q

Distribution of earthquakes

A
  • not evenly distributed
  • broad uneven belts
  • majority of earthquakes relate to plate movement
  • found along plate boundaries
  • most powerful- destructive plate margin: frequent shallow to deep focus
  • constructive: submarine often distant to people
  • conservative: series of faults
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14
Q

How is human activity the cause of some earthquakes

A
  • minor earthquakes
  • building large reservoirs- water puts pressure on the rocks
  • deep mining work
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15
Q

What is the magnitude

A
  • amount of energy released by an event

- measured on the Richter scale

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16
Q

What is the Richter scale

A
  • logarithmic scale
  • ## each unit represents a 10 fold increase in stress and a 30 fold increase in release of energy
17
Q

What is the seconds scale used to measure earthquakes

A
  • mercalli scale
  • measures intensity of the event and the impact
  • 12 point scale
  • level1- detected but felt by few people
  • level12- total destruction
18
Q

What is the frequency

A
    • varies between seismically active regions
19
Q

What are aftershocks

A
  • follow on from the main event and May last for months afterwards
  • generated from the earth settling back after the disruption
  • some are significant
20
Q

What is the initial effect of an earthquake

A
  • ground shaking

- how sever depends on the magnitude

21
Q

What are the consequences from this initial effect

A
  • people are buried under buildings

- many more dying in fires, chaos and confusion

22
Q

What does the earthquake depend on for how sever it will be

A
  • magnitude and depth
  • geological conditions
  • distance from epicentre
  • population density
  • time of day
  • design and strength of buildings
23
Q

What are some secondary effects of an earthquake

A
  • soil liquefaction: soils with high water contents lose their mechanical strength and start to become like a fluid
  • landslides: slope failure as a result of the shaking: further deaths and injury
  • tsunamis: giant sea wave generated by a shallow/0-focus underwater earthquake
24
Q

What are the long term effects of an earthquake

A
  • higher unemployment as not all businesses recover
  • repair of build pings may take months or years
  • longer term illness/lower life expectancy
  • loss of farmland and food production
  • permanent disruption to natural drainage patterns
25
Q

What is a tsunami

A
  • giant sea wave
  • generated by seismic activity
  • caused by ocean floor earthquakes
26
Q

Characteristics of a tsunami

A
  • open seas- long wavelength and a low wave height and they travel really quickly
  • on reaching shallow waters they rise rapidly in height
27
Q

When a tsunami reaches the land the effects will depend on

A
  • height of the wave and the distance it has traveled
  • length of the event
  • extent to which warnings were given
  • coastal physical geography
  • coastal landuse and population density
28
Q

What are the methods used to try and predict an earthquake

A
  • seismic records: studying patterns of earthquakes and using them to predict the next one: seismometer
  • radon gas emissions: radon is an inert gas that is released from rocks such as granite at a faster rate when they are fractured or deformed
  • ground water: deformation of the ground can cause water levels to rise or fall
29
Q

Examples of protection from earthquakes

A
  • better evacuation routes
  • fire resistant buildings
  • building strategies such as only having one story buildings
  • keep supplies on slate such as water and blankets and food - land use planning to identify the places at most risk and move them
  • some insurance companies are willing to dedicate earthquake damage control
30
Q

How do people protect from earthquakes

A
  • making buildings more resistant
  • raising public awareness
  • improving earthquake prediction.
31
Q

Give examples of a building which has been lrotected by an earthquakes

A
  • shorter buildings: Shake less
  • open areas where people can assemble if evacuated, a.so avoids the domino effect
  • steel frames which can sway during earth movement
  • raids so the services can get there easily