Earthquake Activity Flashcards

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1
Q

Earthquake Formation

A
  1. Two plates move alongside eachother (convection currents)
  2. The plates get stuck and a build up of stress forms
  3. Released pressure at the focus.
  4. Seismic waves from the focus travel through the crust to the surface causing earthquake.
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2
Q

Define:
-Focus
-Epicentre
-Shallow focus
-Intermediate focus
-Deep focus

A

-Point at which the pressure is released from crust
-The Point immediately above focus on surface
-(0-70km deep) greatest damage
-(70-300km deep) milder
-(300-700km deep) weak

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3
Q

Convergant Plate boundaries

A

Massive friction, layers of rock at subduction zone, rough edges of rock lock together while subducting, stress builds up which eventually breaks , releasing tension this can lead to large earthquakes and potential tsunamis

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4
Q

Divergent plate boundaries

A

Occur along fractures along mid ocean ridges, weak quakes

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5
Q

Transform plate boundaries

A

Sliding plates, stress builds up as they try to push past eachother, energy is released, powerful quakes, e.g San Andreas Fault

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6
Q

Seismograph

A

Seismologists (people who measure s activity) use this to detect and record earthquake activity, measure INTENSITY of seismic waves, generate graph called seismogram

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7
Q

Body waves Vs
Surface waves

A

Body waves - Travel through inner layers of earth, arriving at different times

Surface waves - Last to arrive and travel at the slowest speed, moving like ripples along the surface, most damage done.

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8
Q

The Richter Scale

A

Records magnitude of s activity, seismograph readings to calculate mag, open ended scale (no limit)

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9
Q

Mercalli Scale

A

Measures the intensity of quake from table of events, Roman numerals, Intensity I - not severe damage
Intensity XII - extremely severe damage
- Less accurate than richter as other things can impact the degree of destruction such as poor build quality

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10
Q

Earthquake prediction, Dating patterns

A

Previous earthquake activity along fault lines predict likelihood, magnitude and intensity of next quake,
look at patterns, seismic gaps etc

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11
Q

Electromagnetic fields Prediction

A

Changes in these fields near fault lines, satellite laser beams and other sensors placed within crust pick up these changes.

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12
Q

Gas Emissions

A

Rising levels of radon gas can indicate…, Radioactive gas found in rocks and soils. Can be released shortly before quakes by subterranean movements, easily detected by instruments

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13
Q

Reducing the impact of earthquakes
(Come up with how? for each in your head)

A
  • Early warning systems (seismographs)
  • Earthquake drills (practice)
  • Power stations kept far from fault lines
  • Earthquake proof buildings
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14
Q

How to earthquake proof a building

A
  • Shock absorbers
  • Base isolator
  • Moat
  • Cross bracing
  • fireproof windows
  • Shear core
  • Weights on roof
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15
Q

Case study: Haiti

A
  • 2010
  • 70% lived under poverty
  • Few building regulations made impacts worse
  • 7.0 Mag
  • Epicentre approx 25km from Port-au-Prince
  • At least 52 aftershocks
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16
Q

Short term effects of Haiti quake

A
  • 3.5 M people affected
  • 230,000 deaths, 300,000 injuries
  • 250,000 homes destroyed (1.5m left homeless)
  • Shortage of clean water
  • Overcrowded hospital
  • 4,000 escape prison and cause havoc
17
Q

Long term effects Haiti

A
  • Contaminated water lead to cholera epidemic which claimed almost 6,000 lives
  • Unemployment rose to 20%
  • Landmark buildings destroyed like the presidents palace and cathedral
18
Q

Japan 2011 Tsunami

A
  • 9.0 magnitude
  • 72km from coast
  • Eurasian jolted upwards creating megathrust with 24km deep focus
  • Ocean rose more than 10 metres while travelling 500 km/h
  • flooded 561 km²
19
Q

Japan short term effects

A
  • 16,000 deaths
  • 25,000 injured
  • contaminated water
  • 4.4 Million with no electricity
20
Q

Long term effects Japan

A
  • 2,500 still missing
  • 125,000 buildings collapsed
  • Fukushima nuclear power plant, 3 explosions evacuated 20km radius (exclusion zone)