Lesson 13- What are the hazards associated with seismicity? Flashcards

1
Q

Ground Shaking +Case study

A
  • Ground shaking is brought by seuismic waves
  • an area that shurken by waves (P and S) and surface can move a structure in an alternate way
  • Mexico City suffered from an earthquake in 1985 where numerous structures crumbled and over 20,000 people lost their lives
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2
Q

Ground displacement

A
  • When the ground moves up, down, sideways to at least 10m
  • Can cause distrubance of streets and utilities
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3
Q

Earth rupture

A
  • Delivers an issue scarp of up to a few metres of vertical uprooting
  • This burst of the earth during a tremor may happen on auxiliary issues
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4
Q

Avalanches and Landslides

A
  • On soak inclines ans rocky territories, enormous tremors can set off numerous avalanches, rockfalls or torrential slides.
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5
Q

Liquefaction

A
  • When there is unconsolidated residue immersed in groundwater, the shaking provided by a seismic tremor may cause the dreg drains to lose contact with one another and become suspended in the water
    -transforms solid ground into fluid ground causing structures to sink, tilt or slide
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6
Q

Fires

A
  • The violent shaking can damage infrastructure such as gas lines and electrical networks. When these are severed or damaged, it can lead to gas leaks, which may ignite and cause fires.
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7
Q

Tsunami + Case study

A
  • A tsunami is a lot of waves in the sea with a very long wavelength, commonly more than 100km long. Torrents can be set off by seismic tremors that enormously shake the sea depths, which usually occurs at subduction zones.
  • The tsunamis from the Sumatra seismic tremor of 2004 excecuted more than 100,000 individuals in seaside territories
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8
Q

Can we predict earthquakes

A
  • Dont currently posses the resoucres to accuratley predict earthquakes
  • But well understood faults can be given approximate probabilities of earthquake ruptions
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9
Q

Method of prediction- Precursors/foreshocks

A
  • The Haicheng in 1975 earthquake produced foreshocks and the city was successfully evacuated
  • However the Tnagshang earthquake in 1976 produced no foreshocks and killed 500,000
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10
Q

Method of prediction- Radon gas

A

Small half life (3.5 days), only found shortly after its emitted
-increased radon gas could mean EQ

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11
Q

Method of prediction-Ground water

A
  • Levels of this in wells are known to dramitally change
    -noted as precursors in China and the USA
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12
Q

Method of prediction- Remote sensing

A
  • Changes in the earths crust from satalittes which measure change in electromagnetism; not accuratley predicting probabilities
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13
Q

Methods of prediction- Electro-magnetism signals

A
  • VAN method
  • Tracks electric signals (better for small EQ’s)
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14
Q

Method of Prediction-Seismic gap theory

A
  • Area of a fault line that has’nt erupted in a long time
  • Tried to prove this at Parkfield but didnt happen the way they expected
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15
Q

Method of prediction- Fault line unzipping

A
  • Used on Instabull to predict an earthquake along the North American fault.
  • Measures the stress transfer along a faultline to predict where the next EQ will occur
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16
Q

Is EQ prediction useful?

A
  • Not very useful as no form of prediction method can tell us when or where specifically it will happen
17
Q

Preperation method- Tuned mass dampers

A
  • Taipei-101
  • A large concrete block mounted in the skyscraper which wave in the opposite direction
18
Q

Preperation method-Shock absorbers

A
  • Springs with damper base designed to absorb the seismic shocks during the earthquake.
19
Q

Case studies of earthquake resistant buildings

A
  • Istanbull Airport- can withstand a magnitude 8 airport and has isolating device that moves the entire building off of the ground
  • Wellington Central Police Statiuon- The exterior walls have X-shaped bracing that enables the building to move as a rigid body. The building rests on 24 flexible piles, isolating it from the ground, and it has lead dampers to reduce shaking.