WorksheetsChapter 5 Earthquakes
Total questions: 56
Worksheet time: 28mins
What are the types of stress and how do they change the crust of the Earth’s surface?
Tension - type of stress that pulls the crust and stretches rock so that it gets thinner in the middle.
Compression - type of stress that squeezes rock until it folds or breaks
Shearing - type of stress that pushes rock into two opposite directions. Cause racks to break and slip apart.
All of the above
Where are faults usually found and why do they form?
A. Faults occur along plate boundaries.
B. Faults form because of the continuous movement of the plate boundaries.
C. Faults form because of Earthquakes.
D. They form on the ring of fire
b and a
d and a
a and c
d and c
a and b
The rocks are pushed apart causing a normal fault. The fault is at an angle so one block of rock lies above the other block of rock. The rock that hangs above (or is pushed up) is the hanging wall and the rock that is below is called the footwall (stays in its regular position).
Normal Fault
Reverse Fault
Strike-Slip Fault
These are all good ideas
The rocks are pushed together so compression causes a reverse fault. A reverse fault also has the same structure as a normal fault, however the blocks of rock move in opposite direction. This causes the hanging wall to move up relative to the footwall.
Normal Fault
Reverse Fault
Strike-Slip Fault
These are all good ideas
In places where rocks move past each other creates shearing. The rocks slip past each other sideways without any up and down motion. The San Andreas fault is an example of a strike-slip fault.
Normal Fault
Reverse Fault
Strike-Slip Fault
All of these are good ideas
The first waves to arrive. They compress and expand the ground like an accordian. They can move through both solids and liquids.
P waves
S waves
Surface Waves
P waves
The first waves to arrive. They compress and expand the ground like an accordian. They can move through both solids and liquids.
The second waves to arrive. They vibrate from side to side as well as up and down. S waves can not move through liquids
When P waves and S waves make it to the surface, they become surface waves. The move slower than P and S waves but can produce more ground movements
S Waves
The first waves to arrive. They compress and expand the ground like an accordian. They can move through both solids and liquids.
The second waves to arrive. They vibrate from side to side as well as up and down. S waves can not move through liquids
When P waves and S waves make it to the surface, they become surface waves. The move slower than P and S waves but can produce more ground movements.
The second waves to arrive. They vibrate from side to side as well as up and down. S waves can not move through liquids
P waves
S waves
Surface waves
Surface Waves
The first waves to arrive. They compress and expand the ground like an accordian. They can move through both solids and liquids.
The second waves to arrive. They vibrate from side to side as well as up and down. S waves can not move through liquids
When P waves and S waves make it to the surface, they become surface waves. The move slower than P and S waves but can produce more ground movements.
When P waves and S waves make it to the surface, they become surface waves. The move slower than P and S waves but can produce more ground movements.
P wave
S wave
Surface Wave
Measure an earthquake's intensity or strength at a given place. This scale uses roman numerals I - XII. Each group of roman numerals are used for each area affected by an earthquake because the intensity varies at different locations. So the smaller the roman numeral, the further it is from the epicenter. And the higher the roman numeral the closer it is to the epicenter.
Mercalli Scale
Richter Scale
Moment Magnitude Scale
It measures the magnitude of an earthquake. This number is determined by geologist measuring the both the seismic waves and fault movements. The seismic waves are measured by a seismograph. It provides accurate measurements for small and nearby earthquakes.
Mercalli Scale
Richter Scale
Moment Magnitude Scale
Estimates the total energy released by an earthquake. This scale can be used to measure all sizes of earthquakes both near and far. Geologist use both the data from seismographs and the data from the movement and the strength of the rocks that broke when the fault slipped.
Mercalli Scale
Richter Scale
Moment Magnitude Scale
To monitor faults, geologist use instruments to measure changes in...
elevation
water
tilting of the land surface
ground movements along faults
temperature outside
Like a carpenter's level, tiltmeters measure the tilting or raising of the ground. They use containers of water that are connected with a smaller tube. As the earth has vertical movement along a fault the water will move from one container of water to another.
Tiltmeters
Creep Meters
Laser
GPS satellites
use wire stretched across a fault to measure horizontal movement.
Tiltmeters
Creep Meters
Laser
GPS satellites
Ranging devices - uses a laser beam that is pointed to a reflector. It also measures horizontal movements of a fault.
Tiltmeters
Creep Meters
Laser
GPS satellites
Measures changes in elevation as well as horizontal movement of a fault. Scientist can measure tiny movements of markers that are set up on both side of a fault.
Tiltmeters
Creep Meters
Laser
GPS satellites
Seismographs and _____monitoring devices provide date used to make faults and detect changes along faults. Geologist are using this data to to develop a method of predicting earthquakes.
fault
temperature
computerized
plates
crust
Geologist can determine _____ risk by locating where faults are active, where past earthquakes have occured, and where the most ________ was caused
earthquake and damage
damage and earthquake
radiation and damage
earthquake and radiation
Can trigger landslides or avalanches and destroy buildings and bridges. It can also topple utility poles and fracture gase and water mains. Loose soil shakes more violently than rock.
Shaking
Liquefaction
Aftershocks
Tsunamis
Shaking
Can trigger landslides or avalances and destroy buildings and bridges. It can also topple utility poles and fracture gase and water mains. Loose soil shakes more violently than rock.
occurs when earthquakes violet shaking suddenly turns loose soft soil into liquid mud. Happens most where the soil is full of moisture. The ground will give way and buildings will sink and pull apart.
an earthquake that occurs after a larger earthquake in the same area. The can strike hours, days or even months later.
The water that is displaced by an earthquake on the ocean floor. The height of the wave is small in the ocean but as the wave approaches shallow water the wave grows into a mountain of water.
occurs when earthquakes violet shaking suddenly turns loose soft soil into liquid mud. Happens most where the soil is full of moisture. The ground will give way and buildings will sink and pull apart.
Shacking
Liquefaction
Aftershocks
Tsunamis
Liquefaction
Can trigger landslides or avalanches and destroy buildings and bridges. It can also topple utility poles and fracture gase and water mains. Loose soil shakes more violently than rock.
occurs when earthquakes violet shaking suddenly turns loose soft soil into liquid mud. Happens most where the soil is full of moisture. The ground will give way and buildings will sink and pull apart.
an earthquake that occurs after a larger earthquake in the same area. The can strike hours, days or even months later.
The water that is displaced by an earthquake on the ocean floor. The height of the wave is small in the ocean but as the wave approaches shallow water the wave grows into a mountain of water.
an earthquake that occurs after a larger earthquake in the same area. The can strike hours, days or even months later.
Shaking
Aftershocks
Liquefaction
Tsunamis
Aftershocks
Can trigger landslides or avalances and destroy buildings and bridges. It can also topple utility poles and fracture gase and water mains. Loose soil shakes more violently than rock.
occurs when earthquakes violet shaking suddenly turns loose soft soil into liquid mud. Happens most where the soil is full of moisture. The ground will give way and buildings will sink and pull apart.
an earthquake that occurs after a larger earthquake in the same area. The can strike hours, days or even months later.
The water that is displaced by an earthquake on the ocean floor. The height of the wave is small in the ocean but as the wave approaches shallow water the wave grows into a mountain of water.
Tsunamis
The water that is displaced by an earthquake on the ocean floor. The height of the wave is small in the ocean but as the wave approaches shallow water the wave grows into a mountain of water.
an earthquake that occurs after a larger earthquake in the same area. The can strike hours, days or even months later.
occurs when earthquakes violet shaking suddenly turns loose soft soil into liquid mud. Happens most where the soil is full of moisture. The ground will give way and buildings will sink and pull apart.
Can trigger landslides or avalances and destroy buildings and bridges. It can also topple utility poles and fracture gase and water mains. Loose soil shakes more violently than rock.
The water that is displaced by an earthquake on the ocean floor. The height of the wave is small in the ocean but as the wave approaches shallow water the wave grows into a mountain of water.
Aftershock
Tsunami
Liquefaction
Shaking
Tension...
pushes rock together
stretches rock
can cause masses of rock to slip
Compression...
pushes rock together
stretches rock
can cause masses of rock to slip
Shearing...
pushes rock together
stretches rock
can cause masses of rock to slip
A force that acts on an area of rock to change its shape or volume is...
stress.
tension.
compresion.
shearing.
normal fault
Tension in the Earth's crust pulls rock apart causing...
normal faults.
reverse faults.
footwalls.
strike-slip faults.
The block of rock that lies above is called the...
hanging wall
footwall
The rock that lies below is the...
hanging wall
footwall
In a reverse fault the blocks move...
in the same direction.
in the opposite direction.
In a strike-slip fault, the rocks on either side of the fault slip past each other sideways, with little up or down motion.
This is accurate!
This is seriously wrong.
Seismic waves carry energy from an earthquake away from the focus, through Earth's interior and across the surface.
This is accurate!
This is seriously wrong.
Seismic waves carry energy from an earthquake toward from the focus, through Earth's interior and and into the sky.
This is accurate!
This is seriously wrong.
Surface waves move more slowly than P waves and S waves, but they can cause more severe ground movements.
This is accurate!
This is seriously wrong.
Surface waves move faster than P waves and S waves, but they can cause more severe ground movements.
This is accurate!
This is seriously wrong.
Geologists use seismic waves to locate an earthquake's epicenter.
That is accurate!
This is seriously wrong.
The best way to protect yourself during an earthquake is to drop, cover, and
hold
pray
roll
run
fly
A base-isolated building is designed to reduce the amount of energy that reaches the building during an earthquake.
That is accurate!
This is seriously wrong.
type of stress that pulls the crust and stretches rock so that it gets thinner in the middle
Tension
Compression
Shearing
How many faults are there?
1
2
3
4
5
Which ones are faults?
Normal Fault
Big Fault
Reverse Fault
Opposite Fault
Strike-Slip Fault
Faults occur along plate boundaries.
True
False
Faults occur along..
Plate Boundaries.
Holes in the ground.
Shaking.
Grand Canyon.
What does a seismograph measure?
seismic waves
earthquakes
P waves
S waves
Surface Waves
Why do faults form?
continuous movement of the plate boundaries
paper plates keep moving
earthquakes
people keep drilling holes in the ground
What kind of fault is the San Andreas fault?
Reverse Fault
Normal Fault
Strike-Slip Fault
Which Scale uses Roman Numerals I - XII?
Mercalli Scale
Richter Scale
Moment Magnitude Scale
Which scale measures the magnitude of an earthquake?
Mercalli Scale
Richter Scale
Moment Magnitude Scale
Which scale estimates the total energy released by an earthquake. This scale can be used to measure all sizes of earthquakes both near and far.
Mercalli Scale
Richter Scale
Moment Magnitude Scale
