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An
Earthquake
is a weak to violent shaking of the ground caused by the sudden movement of rocks below the surface of Earth.
Earth’s surface is composed of a solid material called the
crust.
The crust is made up of
TECTONIC
PLATES.
There are about
20
plates along the surface of Earth that move continously and slowly.
The movement of tectonic plates are caused by the
mantle.
The
mantle
is the layer underneath the crust.
The
crust
together with the
upper
mantle
form
lithosphere.
Earthquakes usually originate from a
tectonic
plate
boundary.
Faults
are lines or cracks in Earth’s surface that are caused by the movement of tectonic plates.
Focus
is the point below the surface of Earth where the trembling started.
Focus is also known as
Hypocenter.
The place above the focus is the
epicenter.
The
epicenter
is where the earthquake is strongest on the surface.
There are three types of earthquake.
Volcanic
Earthquake
Tectonic
Earthquake
Collapse
Earthquake
Explosion
Earthquake
The most common type of earthquake is
Tectonic
Earthquake.
Volcanic
Earthquakes
are caused by volcanic activities such as rising of magma or lava beneath active volcanoes.
Collapse earthquake
are small quakes that occur in caverns or mines.
Explosion earthquakes
result from the explosion of a nuclear or chemical material or device.
The plates under the ocean are called
oceanic
plates.
Stress
is the force applied to a rock and may cause deformation.
Seismology
is the study of seismic waves
The scientists who specialize on this discipline are called
seismologist
Seismologist use an instrument called
seismograph
to detect and record earthquakes.
A
seismogram
is the recording of the ground shaking at the specific location of the instrument
Primary waves
are the fastest seismic waves and can move through any phase of matter.
Secondary waves
can only move through solids.
Those waves that are the most destructive are the
surface waves
which generally have the strongest vibration.
Surface
waves
are the last to reach the seismograph and occur the longest.
The
magnitude
refers to the size of the seismic waves that are recorded in the seismograph
The
Richter scale
measures the intensity or magnitude of an earthquake
The larger the magnitude the stronger the Earthquake is
The
intensity
is the strength of the earthquake based on its ob effects on humans and animals
The intensity is represented by
Roman numerals
The intensity of an earthquake is generally near the
epicenter
An earthquake is usually followed by
aftershocks
Aftershocks
is within one or two lengths from the main shock fault