Science 2nd Monthly Flashcards
Sudden shaking of the ground
Earthquake
Geoelogical Forces
Tectonic Earthquake
Volcanic earthquake
due to volcanic activities
Rock Explosions
Collapse Earthquake
Caused by nuclear or chemical device
Explosion Earthquake
Directly above focus
Epicenter
earthquake starts
hypocenter/focus
Size or strenght of an earthquake
Magnitude
To measure magnitude u need a?
seismograph
The amount of shaking and type of damage.
Intensity
this scale can also be used to know what type of magnitude.
Richter Scale
In order to measure intensity u need to use
Rossi Forel scale and Mercalli scale.
PEIS
PHIVOLCS Earthquake Intensity Scale
I
Scarcely Perciptable
II
slightly felt
III
weak
IV
moderately strong
V
strong
VI
very strong
VII
destructive
VIII
very destructive
IX
devastating
X
completely devastating
Caused by underwater earthquake or volcanic activity
Tsunami
soil loses its strength
Liquefaction
developed through short circuit
fire
Downward movement of the mass rock
Landslide
Does damage to man-made structures.
Structural Collapse
fracture found between 2 blocks of the earth’s crust
Fault
disturbance or crack
Fault trace/line
where the rupture has taken place
Fault Plane
wall above the fault plane
Hanging wall
wall below the fault plane
Foot Wall
The hanging wall moves down relative to the footwall (what kind of fault type is this?)
Normal
The hanging wall moves up relative to the footwall. (what kind of fault type is this?)
Reverse
motion of blocks moving either right or left. (what kind of fault type is this?)
Strike - Slip
It is considered active if they observe or have evidence that there has been activity in the last 10,000 years.
Active fault
cannot produce any more seismic activity or earthquakes
Inactive Fault
Mechanical waves that are caused by the sudden movement of materials within the Earth, such as slip along a fault during an earthquake.
Seismic Waves
travel through the interior part of the earth.
Body waves
travel through the surface part of the earth
Surface waves
Types of body waves
P wave & S wave
Types of surface wave
Rayleigh Wave & Love wave
Moves in a side-to-side motion perpendicular to the main propagation of the earthquake.
Love wave
Moves in an up and down and forward and backward motion
Rayleigh Wave
fastest out of all waves
P wave/ Primary Wave
They can displace rocks and are transverse waves.
S wave/ Secondary Wave
PHIVOLCS
Philippine Institute of Volcanology and Seismology