An Earthquake is… the shaking and trembling that results from the movement of rock beneath Earth's...
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Transcript of An Earthquake is… the shaking and trembling that results from the movement of rock beneath Earth's...
An Earthquake is…
the shaking and trembling that results from the movement of rock beneath Earth's surface
The movement of Earth's plates produce strong forces that squeeze or pull the rock in the crust
This is an example of stress, a force that acts on rock to change its volume or shape
StressThere are three different
types of stress that occur
on the crust, shearing,
tension, and
compression
These forces cause some
rocks to become fragile
and they snap
Some other rocks tend to
bend slowly like road tar
softened by the suns
heat
Types of StressStress that pushes a mass of rock in two
opposite directions is called shearing.
- Forces in Earth’s Crust
- Forces in Earth’s Crust
Types of StressThe stress force called tension pulls on the
crust, stretching rock so that it becomes thinner in the middle.
Types of StressThe stress force called compression
squeezes rock until it folds or breaks.
- Forces in Earth’s Crust
FaultsA fault is a break in the crust where slabs of crust slip past each other. The rocks on both sides of a fault can move up or down or sideways
When enough stress builds on a rock, the rock shatters, creating faults
Faults usually occur along plate boundaries, where the forces of plate motion compress, pull, or shear the crust too much so the crust smashes
Kinds of FaultsTension in Earth’s crust pulls rock apart,
causing normal faults.
- Forces in Earth’s Crust
Kinds of FaultsA reverse fault has the same structure as a
normal fault, but the blocks move in the opposite direction.
- Forces in Earth’s Crust
Kinds of FaultsIn a strike-slip fault, the rocks on either side
of the fault slip past each other sideways, with little up and down motion.
- Forces in Earth’s Crust
Strike-Slip FaultsShearing creates this fault
In this fault, rocks on both sides of the fault slide past each other with a little up and down motion
When a strike-slip fault forms the boundary between two plates, it becomes a transform boundary
Mountains Formed by Folding
Folds are bends in rock that form when compression shortens and thickens part of Earth's crust
MOUNTAINS FORM
The crashing of two plates can cause folding and compression of crust
These plate collisions can produce earthquakes because rock folding can fracture and lead to faults
Anticlines and Synclines Geologists use the terms syncline and anticline to describe downward and upward folds in rock
An anticline is a fold in a rock that arcs upward
A syncline is a fold in a rock that arcs downward
These folds in rocks are found on many parts of the earths surface where compression forces have folded the crust
How Earthquakes FormEarthquakes will always begin in a rock beneath the surface
A lot of earthquakes begin in the lithosphere within 100 km of Earth's surface
The focus triggers an earthquake
Focus: the point beneath Earth's surface where rock that is under stress breaks
Seismic WavesSeismic Waves: vibrations that travel through Earth carrying the energy released during an earthquake
an earthquake produces vibrations called waves that carry energy while they travel out through solid material
During an earthquake, seismic waves go out in all directions to the focus
They ripple like when you through a stone into a lake or pond
Seismic Waves There are three different types of seismic waves:
P waves, Secondary or S
waves, and surface wavesAn earthquake sends out two of those waves, P and S wavesWhen they reach the top of the epicenter, surface waves form
Primary WavesAlso known as P WavesThe first waves to come are these wavesP waves are earthquake waves that compress and expand the ground like an accordion P waves cause buildings to expand and contract
Travel through BOTH liquids and solids
Secondary WavesAlso known as S Waves
After P waves, come S waves
S waves are earthquake waves that vibrate from one side to the other as well as down and up
They shake the ground back and forth
When S waves reach the surface, they shake buildings violently
Unlike P waves, which travel through both liquids and solids, S waves cannot move through any liquids
Surface WavesWhen S waves and P waves reach the top, some of them are turned into surface waves
Surface waves move slower than P waves and S waves, but they can produce violent ground movements
Some of them make the ground roll like ocean waves
Other surface waves move buildings from side to side
Detecting Seismic WavesGeologists use instruments called seismographs to measure the vibrations of seismic waves
Seismographs records the ground movements caused by seismic waves as they move through the Earth
Mechanical SeismographsUntil just recently, scientists have used a mechanical seismographa mechanical seismograph consists of a heavy weight connected to a frame by a wire or spring When the drum is not moving, the pen draws a straight line on paper wrapped around the drum Seismic waves cause the drum to vibrate during an earthquakethe pen stays in place and records the drum's vibrations The higher the jagged lines, the more severe earthquake
Instruments used to detect movementIn trying to predict earthquakes, geologists have
developed instruments to measure changes in elevation, tilting of the land surface, and ground movements along faults.
Measuring EarthquakesThere are at least 20 different types
of measures
Main 3: the Mercalli scale,
Richter scale,
and the Moment Magnitude scale
Magnitude is a measurement of earthquake strength based on seismic waves and movement along faults
Mercalli – INTENSITY, based on effects
The Richter ScaleThe Richter scale is a rating of the size of seismic waves as measured by a particular type of mechanical seismograph
Developed in the 1930’s
All over the world, geologists used this for about 50 years
Electric seismographs eventually replaced the mechanical ones used in this scale
Provides accurate measurements for small, nearby earthquakes
Does not work for big, far ones
The Moment Magnitude Scale
Geologists use this scale today
It’s a rating system that estimates the total energy released by an earthquake
Can be used for any kind of earthquakes, near or far
Some news reports may mention the Richter scale, but the magnitude number they quote is almost always the moment magnitude for that earthquake
Locating the EpicenterSince the P waves travel
faster than the S waves, scientists can use the difference in arrival times to see how far away the earthquake occurred.
It does not tell the direction however.
Determining DirectionOne station can
only learn how far away the quake occurred.
They would draw a circle at that radius.
If three stations combine their data, the quake occurred where the three circles overlap.
Locating the EpicenterTRIANGULATION is used to detect the
location of the epicenter
- Earthquakes and Seismic Waves
How Earthquakes Cause Damage
The severe shaking provided by seismic waves can damage or destroy buildings and bridges, topple utility poles, and damage gas and water mains.
With their side to side, up and down movement, S waves can damage or destroy buildings, bridges, and fracture gas mains.
Earthquake RiskGeologists can determine earthquake risk by
locating where faults are active and where past earthquakes have occurred.
- Earthquake Safety
How Earthquakes Cause DamageIn addition to the DANGERS of ground
shaking, earthquakes can cause tsunamis
A tsunami spreads out from an earthquake's epicenter and speeds across the ocean.
- Earthquake Safety
Designing Safer BuildingsTo reduce
earthquake damage, new buildings must be made stronger and more flexible.
- Earthquake Safety