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Karteikarten

Geography - Earthquakes

Sydney Routley Geography A Level Englisch 38 Karten

Karten in diesem Stapel (38)

  1. 1What is a earthquake?Plate movement cause by friction and pressure building up then suddenly releasing. This causes seismic waves that travel through the plate to the surface
  2. 2What is the Focus?The point where the pressure is released. The ground ruptures at this spot, then seismic waves radiate outward in all directions.
  3. 3What is the epicenter?The point on the earth's surface vertically above the focus of an earthquake.
  4. 4Shallow earthquake?0-70km deep
    These cause the most damage
  5. 5Deep earthquake?300-700km deep
  6. 6Describe the Mexico City earthquake?Shallow Earthquake
    1985
    10,000 people died
    50,000 injured
    35% city destroyed
  7. 7Describe the Iran earthquake?Shallow Earthquake
    1990
    35,000 died
    100,000 injured
    400,000 homeless
  8. 8Describe the Tangshan earthquake?NOT associated with plate boundaries
    1976
    240,000 people killed
    7.8 M initial quake, 7.1 M aftershock
  9. 9Describe the Killari earthquake?Potentially caused by the building of a reservoir putting pressure on a fault
    India, Killari
    1993
    10,000 people died
  10. 10What are the Primary Hazards of earthquakes?Seismic waves - Magnitude and Frequency
    Aftershocks
  11. 11What is a seismic wave?a wave of energy that is generated by an earthquake that travels within the earth or along its surface causing buildings to collapse which kills
  12. 12What is the aftershock?a small earthquake or tremor that follows a major earthquake which causes further damage to already weakened buildings
  13. 13Secondary Hazards of an earthquake?Tsunamis
    Landslides
    Liquefaction
    Flooding - sometimes caused by burst water pipes
    Fire - caused by damaged gas+electrics
  14. 14What is a Tsunami?Large sea waves generated by disturbance of the sea floor caused by earthquakes or submarine landslides.
    eg. Indonesia, Dec 2004
  15. 15What is Liquefaction?Violent disruption of the ground causes it to become liquid-like due to increased pore water pressure which weakens the ground. Groundwater mixes with soil and comes through the newly formed cracks
    eg. 1989 San Francisco
  16. 16What are landslides and avalanches?When slope failure occurs due to ground shking
  17. 17What are the 3 types of seismic shock waves?P-waves
    S-waves
    Surface waves -> Love waves and Rayleigh waves
  18. 18Whats a P-wave?Can travel through solids and liquids (mantle and core). The waves push and pull the earth in the same direction the earth is travelling. Fastest type of wave. High frequency.
  19. 19Whats a S-wave?Can travel through solids only (mantle only). The waves move the earth at 90* to the direction of travel. These waves cause a lot of damage because of their shearing effect.
  20. 20Whats a love wave?Can only travel through solids. They move the surface from side to side causing a lot of damage due to their shearing effect. Slowest waves.
  21. 21Whats a Rayleigh wave?Can travel through liquids and solids. They move the surface in a low frequency rolling motion radiating from the epicenter
  22. 22Define magnitude?Is the amount of energy released by the event and is usually measured on the Richter scale.
  23. 23Physical factors effecting an earthquake?Distance from epicenter
    Depth of focus
    Time of Day
    Duration of shaking
    Magnitude of earthquake
    Geology of land
  24. 24Human factors effecting an earthquake?Community preparedness
    Emergency relief services
    Economic + social structure of country
    Building design
    Gas and electricity supply
    Land use planning
  25. 25How do you prepare for an earthquake?Modify the event -> Controlling physical variables and hazard resistant design
    Modify the vulnerability -> Prediction and Warning and community preparedness
    Modify the loss
  26. 26How do you modify the event -> Controlling physical variables?Geophysical event - it can NOT be stopped
    Human induced earthquakes (eg. dam construction) could be prevented by consideration of the seismic hazard when siting the structure.
  27. 27How do you modify the event -> Hazard-Resistant design?Aseismic designs
    Not possible to rebuild whole cities
    Economically developed nations and put in strict planning/building regulations - poor can't
    Aseismic designs expensive to replace and repair after a quake
  28. 28What are some aseismic designs?Concrete counterweight - moves in the opposite direction to quake, power failure means it cant move
    Rubber shock absorbers - allows building to move with quake
    Cross bracing - allows the tower to twist easier
  29. 29Define modify the vulnerability?The aim is to lessen the impacts of the earthquake by prediction and warning, community preparedness and land use planning
  30. 30How do you modify the vulnerability -> Prediction and warning?Regional - use previous recorded data to pinpoint areas at risk (where)
    'Gap theory' - predicts when a quake will happen based on how long the plates have been 'locked'
    short term - changing water levels and released radon gas
  31. 31How do you modify the vulnerability -> community preparedness?General public - must have supplies, move under protective furniture, await rescue, first-aid training valuable as 'self help only' period crucial
    Emergency services - well organised, know where to deploy people in the area with disrupted transport routes and communication
  32. 32Describe Tangshen earthquake?1976
    250,000 people died + 160,000 injured
    16% above due to trying to escape
    25% above due to heat, thirst + hunger
    Further 250,000 tried rescuing others
    Most survivors were under heavy furniture
  33. 33Whats a tsunami?Giant waves caused by earthquakes under the sea. Out in the depths of the ocean, tsunami waves do not dramatically increase in height. But as the waves travel inland, they build up to higher and higher heights as the depth of the ocean decreases.
  34. 34Describe a tsunami wave in open ocean?Very deep water
    High speed - 700km/h
    long wavelength - 200km
    small amplitude - 1m
  35. 35Describe a tsunami wave closer to land?Shallower water
    Waves compress = energy more concentrated
    slower - 80km/h
    wavelength decreases - 20km
    amplitude increases - many meters
  36. 36Hydrostatic effect?Debris in the water that kills being moved by the water
  37. 37Hydrodynaimc effect?power in the wave destroying buildings and infastructure
  38. 38Describe the Indonesian tsunami?9.1 magnitude quake
    Sunda trench off SW coast Indonesia
    Australia plate subducted under Burma plate
    20m slip along 1600km faultline
    epicenter 160kn offshore - focus 30km down

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Beschreibung
A Level Geography Karteikarten am Geography - Earthquakes, erstellt von Sydney Routley am 04/04/2015.
Erstellt von
Sydney Routley
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