Any plate with an area that are less than 20 million km^2 but greater than 1 million km^2 (e.g. Philippine plate, Indian plate, Scotia plate)
Tertiary plate
Any plate with an area that are less than 1 million km^2
Earthquake
Sudden slip on a fault
Focus
The point within the earth where the release of energy happens
Epicenter
The location on the surface of the earth directly above the focus
Seismograph
Used to record the motion of the ground
Seismic waves
Waves of acoustic energy that travel through the earth
Types of seismic waves
Body waves
Surface waves
Body waves
Seismic waves that move through the interior of the earth
Primary waves (p-wave)
The fastest seismic waves that can move through solid, liquid, or gas
Secondary waves (s-wave)
Slower than p-waves, also called shear waves because they don't change the volume of the material through which they propagate, travel through solid materials only
Surface waves
Can only travel on the surface of the earth and arrive after the body waves
Love waves
Shear waves trapped near the surface
Rayleigh waves
Have rock particle motion similar to the water particle in the ocean
Triangulation method
Uses distance information from three seismic stations to locate the earthquake epicenter by drawing circles on a map around each station and finding the intersection point
Seismologist
Determines the distance to the earthquake epicenter by multiplying the difference in the arrival time of p-wave and s-wave in seconds by 8 km/s
Theory of plate tectonics
Pieces of Earth's Lithosphere are in constant motion, driven by convection currents in the mantle
Convection current
Formed by rising of hot magma near the core towards the surface, while cooler magma near the crust sinks, setting up current that causes the plates to move
Convergent plate boundary
A plate boundary where two plates move toward each other, causing compression stress
Geological features/events in convergent boundary
Volcanoes
Volcanic island arc
Trench
Continental volcanic arc
Mountain ranges
Earthquakes
Types of convergent plate boundary
Oceanic-oceanic
Oceanic-continental
Continental-continental
Oceanic-oceanic convergent boundary
Two oceanic slabs converge and subduct the other, resulting in volcanoes, volcanic island arc, trench, and earthquakes
Oceanic-continental convergent boundary
Denser oceanic lithosphere sinks into the asthenosphere (subduction), resulting in continental volcanic arc, trench, and earthquakes
Continental-continental convergent boundary
No subduction happens, resulting in mountain ranges and earthquakes
Divergent plate boundary
Two plates that move away from each other, creating a tension zone causing shallow earthquakes and new crust