Save
Busy. Please wait.
Log in with Clever
or

show password
Forgot Password?

Don't have an account?  Sign up 
Sign up using Clever
or

Username is available taken
show password


Make sure to remember your password. If you forget it there is no way for StudyStack to send you a reset link. You would need to create a new account.
Your email address is only used to allow you to reset your password. See our Privacy Policy and Terms of Service.


Already a StudyStack user? Log In

Reset Password
Enter the associated with your account, and we'll email you a link to reset your password.
focusNode
Didn't know it?
click below
 
Knew it?
click below
Don't Know
Remaining cards (0)
Know
0:00
Embed Code - If you would like this activity on your web page, copy the script below and paste it into your web page.

  Normal Size     Small Size show me how

tsunami answer

QuestionAnswer
an earthquake that occurs after a larger earthquake in the same area aftershock
the point beneath earths surface where rock break causing an earthquake focus
a type of sesmic waves that moves on the ground up and down or side to side s waves
a force that acts on rock to change its shape or volume stress
a type of fault were rocks on either side move past each other sideways with little up or down motion strike slip fault
stress that squeezes rock until it folds or brakes compression
a scale that rates earthquakes acording to their intesity and how much damage they cause mercali scale
a large wave produced by an earthquake on the ocean floor tsunami
Potential Tsunami Locations Subduction Zones
what are Subduction Zones an area where an oceanic plate is being forced down into the mantle by plate tectonic forces.
Convergent Plate Boundary occurs between two oceanic plates one of those plates will subduct beneath the other. Normally the older plate will subduct because of its higher density.
volcanic island formation pt 1 The subducting plate is heated as it is forced deeper into the mantle, and melts. Magma spots created as a result,magma is lower density than the rock material
Volcanic island formation pt.2 It ascends by melting and fracturing through the rock material.Magma chambers at the surface form a volcanic cone. early stages of this boundary the cones will be in deep ocean, later grow above sea level
example of Convergent Plate Boundary - Oceanic Japan, the Aleutian islands and the Eastern Caribbean islands of Martinique,St. Lucia and St. Vincent and the Grenadines are examples of islands formed through this type of plate boundary
Convergent Plate Boundary - Continental The two thick continental plates collide and both of them have a density that is much lower than the mantle, which prevents Subduction
Convergent Plate Boundary - Continental example The Himalaya Mountain, and The Appalachian Mountain Range,are the best active examples of this type of plate boundary
Created by: 15bgarcia
Popular Science sets

 

 



Voices

Use these flashcards to help memorize information. Look at the large card and try to recall what is on the other side. Then click the card to flip it. If you knew the answer, click the green Know box. Otherwise, click the red Don't know box.

When you've placed seven or more cards in the Don't know box, click "retry" to try those cards again.

If you've accidentally put the card in the wrong box, just click on the card to take it out of the box.

You can also use your keyboard to move the cards as follows:

If you are logged in to your account, this website will remember which cards you know and don't know so that they are in the same box the next time you log in.

When you need a break, try one of the other activities listed below the flashcards like Matching, Snowman, or Hungry Bug. Although it may feel like you're playing a game, your brain is still making more connections with the information to help you out.

To see how well you know the information, try the Quiz or Test activity.

Pass complete!
"Know" box contains:
Time elapsed:
Retries:
restart all cards