• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/23

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

23 Cards in this Set

  • Front
  • Back
Tectonic Earthquakes
caused by the stresses put on the plates (colliding, pulled apart, etc.) most common
Volcanic Earthquakes
as magma moves from the ground the rocks around it vibrate most common
Collapse Earthquakes
caves, landslides -> large blocks of rock moving create seismic activity
Explosion Earthquakes
Nuclear detonations, fuel plant explosions
Focus
where the earthquake originates on the fault
Wave Front
where the seismic waves have yet to reach
Epicenter
the focus projected onto a surface map
Ray Path
vector of one of the directions the wave travelled
Body Waves
move through the interior of the earth
Surface Waves
move along the surface of the earth
Body vs. Surface Waves
of the three types of earthquake waves, two travel though the interior of the planet and one travels along the surface
Shear Wave
- particle move up/down or left/right (can be surface or body waves) (string)
- shear body wave
- Rayleigh Wave = R-wave
- Love Wave = L-wave
Shear Body Wave
secondary wave (s-wave), second highest speed
Compressional Wave
- particle move back and forth parallel to the direction of wave motion (slinky), move faster than shear waves
- Compressional Body Wave
Body Waves
- Shear Body Waves
- Compressional Body Waves
Surface Waves
- expressed at the surface and dies down with depth, slowest of all earthquake waves, cause the most damage (ground moves up and down, side to side)
- Rayleigh Wave = R-wave
- Love Wave = L-wave
Seismometer
measures earthquakes, recording called a seismogram
Mercalli Intensity Scale
defines the intensity of an earthquake by the amount of damage it causes. Intensity ranges fro I to XII, somewhat subjective because number depends on damage, varies with distance. Measure of relative strength perceived and felt
Richter Magnitude Scale
- measures the relative amount of energy releases by determining the amplitude of the largest ground motion
- The limit of the Richter Scale is technically 0 to infinity but the scale become less and less precise past 8.9
- An increase of one unit of magnitude equals about 33 times more energy
- So a magnitude 8 earthquake does not release twice as much energy as a magnitude 4 quake but 1 million times as much
Modern Moment Magnitude Scale
- measures the total energy released by a quake more precisely than the historical richter scale
- Can precisely measure very large earthquakes including >8.9
- Calculation of energy in part includes:
- Length of the fault rupture
- Area of rupture surface
Hazards
- Ground Shaking
- Landslides
- Liquefaction
- Fire
- Disease
Liquefaction
- ground vibration cause water-logged soils and clayey sediments to become a slurry of mud and water
- Sandblows (sand volcanoes): water rushes to the surface, water can be boiling
Disease
disruption of infrastructure, lack of sanitation, food and water can quickly lead to outbreaks of disease