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 and 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 earthquake and has isolating device that moves the entire building off of the ground
  • Wellington Central Police Station- 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.