Hazards Flashcards

(41 cards)

1
Q

What is a natural hazard?

A

a natural process that could disrupt humans
e.g. could cause death, injury, damage property

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2
Q

What is a natural disaster?

A

a natural hazard that has happened

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3
Q

How do we class something as a hazard?

A

To be classed as a hazard, it needs to pose a threat to humans

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4
Q

What is a seismic hazard?

A

the hazard associated with potential earthquakes in particular areas

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5
Q

What are the different hazards/consequences associated with earthquakes? (seismic hazards)

A

Tsunamis
Subsidence
Liquefaction
Ground shaking
Landslides

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6
Q

Describe the process of an earthquake?

A
  1. Movement of bedrock either side of a fault line applies stress to the rock in the fault zone
  2. This movement transfers energy into the rock and increases the elastic strain energy stores in the rock, causing the rock to deform
  3. When this deformation exceeds the frictional force holding the rocks together, a sudden slip (movement) occurs along the fault (an earthquake)
  4. This releases the accumulated stress and the rocks on either side of the fault return to their original shape, this is known as elastic rebound
  5. The energy from this sudden slip sends seismic waves through the crust and Earth to the surface
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7
Q

What is an active fault?

A

a fault where there is a potential source of earthquakes
- some suggestions say where there has been movement in the past 100,000 years

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8
Q

Give an example of an active fault?

A

Anatolian Fault, Türkiye

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9
Q

In what ways do we measure earthquakes?

A

Magnitude
Intensity

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10
Q

What do we measure for magnitude?
What are we actually measuring?

A

seismometer, seismograph

actually measuring amplitude of waves

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11
Q

What is magnitude?

A
  • a number that characterises the relative size of an EQ
  • it is based on measurement of the maximum motion recorded by a seismograph (amplitude)
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12
Q

What issues arise when measuring earthquakes?

A

different levels of movement in different rocks

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13
Q

What ways can we measure magnitude?

A
  • Local or Richter (ML)
  • Moment (MW)
  • Surface wave (MS)
  • P-wave
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14
Q

What is the Local or Richter (ML) scale?

A

The original magnitude relationship defined in 1935 by Richter and Gutenberg
- based on the maximum amplitude of S-waves recorded on a Wood-Anderson torsion seismograph
- ML values can be calculated using data from modern instruments
- L stands for Local because it only applies to EQ relatively close to the seismic station

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15
Q

How does moment (MW) measure magnitude?

A

Based on the seismic moment of the EQ, which is equal to the average amount of displacement on the fault multiplied by the fault area that slipped.
- it can also be estimated from seismic data if the seismometer is tuned to detect long-period body waves

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16
Q

How can Surface Waves (MS) be used to measure magnitude?

A

A magnitude for distant earthquakes based on the amplitude of surface waves measured at a period near 20s

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17
Q

How can P-waves be used to measure magnitude?

A
  • based on P-wave AMPLITUDE

Technique is being increasingly used to provide very rapid magnitude estimates so that early warnings can be sent to utility and transportation operators to shut down equipment before the larger (but slower) S-waves arrive

18
Q

What are the similarities between all the magnitude measuring systems?

A

All are logarithmic
- amplitude of ground motion increases by x10 each time
- energy increases by x32 each time

19
Q

Why do earthquakes happen at transform plate boundaries?

A

as the jagged sides catch on each other/where a transform boundary meets a divergent boundary (fault) it creates a huge build up of pressure, then as it slips it will all be released at once, causing a big EQ

  • two conflicting movement types mean more movement is going on so it is more likely for pressure and impact
20
Q

Where do the very large earthquakes occur?
Why?

A

Convergent subduction boundaries
(often oceanic-oceanic)
because there is the potential for a greater width of rupture zone on a gently dipping boundary than on a steep transform boundary

21
Q

What happens to the depth of earthquakes with distance from the ocean trench?

A

further distance = deeper earthquakes because of subduction, but there are not many earthquakes at extreme depths due to melting during subduction. Deep = hot

22
Q

What scale is used to measure Earthquake intensity?
What is the range

A

Modified Mercalli Scale
goes from I-XII where I is ‘not felt’ and XII is ‘extreme’

23
Q

What are the factors affecting the intensity of an earthquake?

A
  • proximity to epicentre
  • depth of focus (distance)
  • geology = subsurface rocks and sediment (local ground conditions)
  • standard and design of buildings
  • magnitude/size of EQ at focus
24
Q

Why does an earthquake lose its power with distance from the focus? (depth and distance)

A

amplitude and frequency attenuate due to energy disspiating into the rock as it travels

25
What is a) amplitude b) frequency c) attenuation d) amplification
a) wave height b) wave speed c) decreasing/slowing of amplitude and frequency d) increasing/speeding up of amplitude and frequency
26
How does local ground conditions affect the intensity of an earthquake?
different rocks react differently to the energy applied by the force of an EQ - waves speed up/slow down depending on the medium/material its travelling through - competent vs incompetent WATER: amplitude is amplified by water saturated unconsolidated lake sediment
27
What is a competent rock? Give examples
a rock that is mechanically strong - rigid - compressible - shear strength e.g. Granite, Limestone, Sandstone
28
What is an incompetent rock? Give examples
a rock that is mechanically weak - not rigid - not compressible - poor shear strength e.g. shale, mudstone, clay, unconsolidated sediment
29
How do competent rocks affect the intensity of an earthquake?
LOWER INTENSITY - they don't absorb the energy of the EQ because the waves are 'propagated' through the rock due to its rigidity, compressibility and shear strength - therefore rocks don't deform and buildings are not damaged - competent rocks have a low level of attenuation
30
How do incompetent rocks affect the intensity of an earthquake?
HIGH INTENSITY - they absorb the energy of the EQ because the waves are dissipated and diminished through the rock due to its poor rigidity, compressibility and shear strength - therefore rocks deform and buildings are damaged - incompetent rocks have a high level of attenuation - ground shaking is amplified
31
What structural factors can influence earthquake intensity?
- local building standards - infrastructure (gas lines, water mains, roads)
32
How can building standards have an affect on earthquake intensity?
poor design = intensifies the effects - buildings that are not reinforced to be EQ proof will be more susceptible to damage - also may cause more damage to others through collapse e.g. crushing, cutting water pipes and electricity wires
33
Give an example of poor building design and standards having an adverse effect during an earthquake
Türkiye Izmit, Türkiye 1999, M7.6 - adherence to the strong building code was poor to cut costs - used inappropriate materials in concrete and reduced the amount of steel reinforcing - result: 17,000 deaths - code was strengthened again, but only in a few regions, still not obeyed strongly Still susceptible as seen in M7.1 EQ 2011, In cities of Van and Erciş - 644 deaths - 11,232+ buildings damaged - 6,017 uninhabitable - 4,152 injured - 60,000 homeless - severe shaking in Van, strong/severe shaking felt in less pop areas, lighter but well felt elsewhere in region
34
How does the building of infrastructure (gas lines, water mains, roads) have an impact on earthquake intensity? Give an example
FIRES - ground shaking means fuel pipelines rupture, electrical lines damaged, water mains burst - without water, we cannot fight the fires. Fire spreads quickly e.g. the 'great' San Francisco EQ 1906 - massive fires downtown - 25,000 buildings destroyed by fires fuelled by broken gas pipes - broken water pipes made response hard
35
How can the risk of fires during an earthquake be reduced?
P-wave early warning systems mean utility operators can reduce pipeline pressure and close electrical circuits
36
Why were there so many fires in the Kobe earthquake in Japan 1995?
84 fires with caused conjectured: 56 were related to broken electricity and gas pipes (66.7%) People were also cooking breakfast causing over 300 fires Took over 2 days to put them all out
37
What is a geohazard?
A natural hazard caused by geological processes
38
What are the geohazards?
- ground shaking - liquefaction - tsunami - landslide/mass movment
39
What is the primary cause of damage in an earthquake?
ground shaking
40
What causes ground shaking? What controls the level of shaking?
movement of the body and surface waves through the Earth's crust - waves respond differently to different types of rock and in some cases can be amplified by rocks which can then lead to more serious ground shaking and leads to other seismic hazards
41
How does the distribution of geohazards change with from a water source? What will intensity be like in each location?
- further towards mountains: landslides, mild intensity - sparse rural areas: ground shaking, amplification and liquefaction, intensity depends but could be strong - near the water source (could be in build up areas): ground shaking, amplification, liquefaction, intensity depends but could be strong/severe