Eaeth Quakes Flashcards
(25 cards)
Faults
Faults are breaks in the lithosphere usually found along tectonic plate boundaries
Earthquakes occur due to what
Movement on faults
Mechanism for earthquakes is known as the…
Elastic rebound theory
Steps to elastic rebound theory
Rocks get locked and deformed by forces
Rocks bend and store elastic energy
Friction resistance is overcome
Stored energy is released all at once and rocks snap back to its original shape
Type of seismic waves body waves
P -waves Primary/pressure Push pull Solids liquids gas Faster wave
2nd Types of waves body waves
S waves Right angles to their direction Only thru solids Slower Sideways More dangerous
Surface waves
Couples
Great destruction
High amplitude and low velocity
A seismograph
Records ground motion
Seismogram
Is the actual recording
What is used to determine distance from epicentre
Arrival of p and S waves
How many circles u need to pinpoint earthquake
3
How does wave speed increase
Increase with density
Refraction
Change in direction with changing medium
Medium=
Material that a wave of energy passes through
Moho
Crust/mantle boundary
Plastic asthenosphere =
Decrease in wave velocity (low velocity zone)
P wave shadow zone
103* to 143* from epicentre due to refraction accross layers
S shadow
Due to liquid layer 103-103
Seismic risks
Geopraphic location (boundaries) Topography (mudslides) Ground strength (rock type) Construction (buildings)
Predictions
Micro seismicity+ Bulging + Electrical - Groundwater - Radon +
Faults move past each other slowly
Fault creep
Measure of earthquake 1
Mercali (intensity)
Measure of scale 2
Richter (magnitude)
Buoyancy
Low density rock masses floating on high density accounts for roots of mountain belts