Fault - a fracture or zone of fracture between two blocks of rocks.
Epicenter - the point on the earth's surface vertically above the focus of an earthquake.
Focus - point inside the earth where the earthquake started
Seismic wave - just like a wave that transports energy from one place to another
How to know if there is a fault?
There must be a movement between two blocks
Ex. The layers of sand and starch moved along with the cut/fracture/crack which represents fault.
A fault is a fault when there is a cut/fracture/crack on the surface which allows movement of the blocks of rocks.
Fault Plane - Surface that the movement has taken place within the fault
The plane that represents a fault's fracture surface.
Hanging Wall - The rock mass resting on the fault plane
the upper or overhanging wall of a vein, fault, or other geologic feature.
opposed to footwall.
Footwall - The mass of rock below the fault plane
the rocks beneath a fault plane that is inclined
Where we walk
Normal Fault
The hanging wall moves down relative to the footwall
Younger rocks are displaced above older blocks
Fault displaced caused by tension/extension/ pulling apart.
Reverse Fault
Hanging walls moves up relative to the footwall
Older rocks are displaced above younger blocks
Fault displacement caused by contraction or pushing together
Strike - slip fault
The plane of displacement is HORIZONTAL
Displacement occurs laterally, parallel to the strike of the fault, rather than up or down (parallel to each other)
Displacement caused by shearing or sliding past each other
Active Fault
a fault that is likely to have another earthquake sometime in the future.
Earthquake within 10k years
Inactive Fault
No record in 10k years
Can still be active
Structures that we can identify, but which do not have earthquakes. These faults do not show any signs.
Tensional Stress - When rocks are pushed away from each other
Compressional Stress - Towards each other created on the Earth’s surface
Shear Stress - Pushed perpendicular to the axis
Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea.
A tsunami is a series of waves. You may experience flood waters if this occurs. Walking or driving in floodwaters can be risky.
tsunami is caused by a large and sudden movement of the ocean
Tsunamis are usually triggered by huge earthquakes on the earth's surface, which cause slabs of rock to rapidly shift past each other and rise upward, resulting in a tsunami.
Reverse fault generates the strongest tsunami
Tsunami gets weaker as it reaches the shore
intensity is the strength of the earthquake to the observer
intensity Can be used to express the damage caused by an earthquake
Intensity can be determined from the shaking and the damage caused by an earthquake.
The severity of an earthquake can be determined using a Mercalli Intensity Scale.
Intensity varies depending on how close or far the location is from the epicenter of the earthquake, The closer it is to the epicenter the higher the intensity. The farther it is from the epicenter the lesser the intensity.
intensity is Qualitative(describable)
magnitude is Quantitative (measurable)
magnitude Does NOT vary with the distance from the epicenter of the earthquake
Magnitude values are calculated right after an earthquake
Can be recorded using an instrument called seismograph
The strength of an earthquake can be determined using the Ritcher’s Magnitude Scale
magnitude It describes the total amount of energy that is released by an earthquake
magnitude Cannot properly describe large scale of earthquakes
Body Wave
Traveling through the interior of the earth
Arrive before the surface waves
Higher Frequency
P-Waves or Primary Waves
Fastest kind of seismic wave
1ST to arrive at a seismic station
Can pass through solid and liquid layers of the Earth’s interior
They are longitudinal waves they compress and Expand like a spring in the direction of the wave propagation