EARTHQUAKES Flashcards
- Earthquake:
the ground shaking cases by stresses released in Earth
o Factors that determine destructiveness
Location, magnitude, depth, distance from epicenter, secondary effects, architecture
EQ stresses
seismic waves (kinetic energy), displacements along the fault (kinetic energy), heat and other energy
megathrust EQs
plate boundary EQ
up to M9 occurs every 200-800 years
causes large tsunamis
- Understand why most earthquakes IN Canada occur on the west coast
o Subduction zone at a convergent Boudry
North America plate w/ Juan de Fuca plate and pacific plate
North American plate EQs
* Large damage potential closer to surface =more shaking
Juan de Fuca plate EQs
* Deeper and very frequent
o Quantitative 1-10
measures magnitude
richter scale
moment magnitude scale
Richter’s scale
based on aptitude of seismic waves, which is related to energy released
* Not really used by geologists, despite being well known
Moment magnitude scale:
is based on the amount of fault slippage produces, the size of surface area that ruptured, and the nature of the materials that faulted, which is more accurate than Richter’s scale
qualitative
1-12 intensity
Modifies Mercalli scale
Modifies Mercalli scale
what we feel
* 1: felt by very few
* ~5: general panic
* 12: total destruction
o Magnitude
Characterizes an EQs relative size
Each whole number represents a tenfold increase in the measured amplitude and 32 times more energy release
- Use plate tectonics to predict where earthquakes occur, and how earthquake depth and magnitude is ties to different types of plate tectonic boundaries.
o Materials respond differently (strain) to stress. Brittle deformation leads to an earthquakes
o Deep focus at convergent boundaries
o Intermediate focus at transform boundaries?
o Shallow focus at divergent boundaries
o Subduction zone earthquakes (convergent boundaries)
Largest possible earthquakes/ deep focus (meteorite impacts can be larger)
Convergent boundaries
Type of stress here: compression
Type of faults: reverse (or thrust)
Three locations of earthquakes
* #1: subduction interface earthquakes.
o Can be huge @ M9.4) megathrust EQs
* #2 EQs in the subducting or overriding plate
o Moderate size, largest = ~M7
* #3 Benioff earthquakes
o Very deeps: 100s of km)
o Little/ no damages at surface
o Deeper focus as moved down the Benioff zone
Megathrust rupture zone located on the coast of Vancouver island
* 12-30 minutes from EQ till initial tsunami waves arrive
* Last one: jan 26 1700 @ M9 (records in Japan and first nations(oral) )
o Continent- continent convergent Eq zones
Very large (not as large as subduction) up to ~M8
Convergent boundaries
Type of stress: compression
Type of fault: reverse (or thrust)
India= thrust fault
o Divergent EQ zones
Small to moderate EQs usually less than M5
Most are underwater
Type of stress: tension/extension
Type of fault: normal
Ex: east African rift, mid Atlantic ridge
* Rift valley forms
o Transform boundaries
Oceanic (majority) very small Eqs
Continental- shallow mostly small earthquakes, some larger usually up to M6 or M7
Type of stress: shear
Type of fault: strike-slip
Ex: San Andreas fault, Queen Charlotte fault
o Body waves
P- wave (primary/ pressure)
* Particles move parallel to the direction wave propagates
* Can travel through all matter
* Is the fastest
S- waves ( shear/ secondary)
* Particles move perpendicular to direction wave propagates