Earthquakes Flashcards
Converge
Collide
What are the two types of earthquakes
Caused by volcanic activity
Caused by tectonic plate movement
Focus
Where the fault initially ruptures under the ground and the origin of seismic waves
Epicentre
Where the seismic waves first reach the surface
What are the types of faults
Normal fault
Reverse fault
Strike slip fault
Oblique slip fault
A normal fault and eg.
Crust is being pulled apart, the land slumps downwards and away from the block on the other side, eg. Taupo volcanic zone and bay of plenty
A reverse fault eg.
When two blocks are driven together/compressed so one side climbs up the sloping fault and overlaps the other. Eg. South Island and lower north island
Strike slip fault and eg.
Blocks move sideways past each other. Sinistral when far side moves left and dextral when far side moves right eg. many major faults in New Zealand
Oblique slip fault and eg.
Different movements are combined. Eg. Wairarapa fault caused 1855 earthquake with reverse and strike slip movement
Deep earthquakes
Only occur when a tectonic plate subducts deeply into the mantle
Shallow earthquakes
Occur along tectonic plate boundary caused by beginning of subduction of oceanic crust
Two main types of waves
Body waves and surface waves
Two types of body waves
P wave
S wave
Two types of surface waves
Love wave
Rayleigh wave
Primary waves
Travel through the earth
Fastest, arriving at seismometer first. Moves rock particles backwards and forwards in the direction the wave is travelling
Secondary waves
Move more slowly arriving second Result in a rolling motion
Travel through earth
Move rocks particles perpendicular to the path of the waves
Love and Rayleigh waves
Arrive last
Being near surface and MIRV along surface only
Destructive waves because most intense
The two scales for measuring earthquakes
Richter scale
Mercalli scale