EARTHQUAKE Flashcards
(30 cards)
is the vibration of earth’s surface caused by waves coming from a source of disturbance inside the earth
EARTHQUAKE
The typical characteristics of earthquake depends on
- Stress drop during the slip
- Total fault displacement
- Size of slipped area
- Roughness of the slipping process
- Fault shape (Normal fault, Reverse fault, Strike slip fault)
- Proximity of the slipped area to the ground surface
- Soil condition
As the waves radiate from the fault, they undergo geometric ________________ due to loss of energy in the rocks.
SPREADING AND ATTENUATION
These vibrations travel through the rocks in the form of
ELASTIC WAVES
there are three types of waves associated with propagation of an elastic stress wave generated by an earthquake.
primary (P) waves, secondary (S) waves and surface waves
These waves propagate by longitudinal or compressive action, which mean that the
ground is alternately compressed and dilated in the direction of propagation
PRIMARY WAVES
are transverse or shear waves, which mean that
the ground is displaced perpendicularly to the direction of propagation
SECONDARY WAVES
are tension-compression waves similar to the P-waves expect that their amplitude diminishes with distance below the surface of the ground.
RAYLEIGH WAVES
are the counterpart of the “S” body waves
LOVE WAVES
the rupture causing earthquakes initiates from a point
HYPOCENTER OR FOCUS
point on earth’s surface diametrically opposite to the epicenter
ANTI-CENTER
An imaginary line which joins the points at which the earthquake waves have arrived at the earth’s surface at the same time is called a
CO-SEISMAL
The instruments measure the ground displacements and are called
SEISMOGRAPH
The record obtained from a seismograph is called a
SEISMOGRAM
The seismograph has three components
the sensor, the recorder and the timer
The devises that measure the ground accelerations are called
ACCELEROMETER
This scale is more comprehensive and describes the intensity of earthquake more precisely.
Mendvedev-Spoonheuer-Karnik scale (MSK 64)
Numerous intensity scales have been developed over the last several hundred years to evaluate the effects of earthquakes, the most popular is
MODIFIED MERCALLI INTENSITY SCALE (MMI)
In the Philippines, we use the __________________________ which composed of 10 increasing levels of
intensity.
PHIVOLCS Earthquake Intensity Scale (PEIS)
Perceptible to people under favorable circumstances. Delicately balanced objects are disturbed slightly. Still Water in containers oscillates slowly.
INTENSITY I - SCARCELY PERCEPTIBLE
Felt by few individuals at rest indoors. Hanging objects swing slightly. Still Water in containers oscillates noticeably.
INTENSITY II - SLIGHTLY FELT
Felt by many people indoors especially in upper floors of buildings. Vibration is felt like one passing of a light truck. Dizziness and nausea are experienced by some people. Hanging objects swing moderately. Still water in containers oscillates moderately.
INTENSITY III - WEAK
Felt generally by people indoors and by some people outdoors. Light sleepers are awakened. Vibration is felt like a passing of heavy truck. Hanging objects swing considerably. Dinner, plates, glasses, windows and doors rattle. Floors and walls of wood framed buildings creak. Standing motor cars may rock slightly. Liquids in containers are slightly disturbed. Water in containers oscillate strongly. Rumbling sound may sometimes be heard.
INTENSITY IV - MODERATELY STRONG
Generally felt by most people indoors and outdoors. Many sleeping people are awakened. Some are frightened, some run outdoors. Strong shaking and rocking felt throughout building. Hanging objects swing violently. Dining utensils clatter and clink; some are broken. Small, light and unstable objects may fall or overturn. Liquids spill from filled open containers. Standing vehicles rock noticeably. Shaking of leaves and twigs of trees are noticeable.
INTENSITY V - STRONG