Save
Upgrade to remove ads
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

Geology 1.0

Physical Geology Exam 3

QuestionAnswer
TYPES OF FOLDS TYPES OF FOLDS
Anticline Ant Hill
Syncline Sink Line
The oldest rock in a anticline is at the? center
The oldest rock in a syncline is at the? exteriour
EARTHQUAKES EARTHQUAKES
Hypocenter Foucus of an earthquake.
Soundwaves travle faster throught the ground.
TYPES OF FAULTS TYPES OF FAULTS
Normal fauls form during extension so.. the hanging wall moves down. (where the miner hangs his lantern)
Reverse faults form during compression so... the hanging wall moves up steeply.
Thrust faults form during compression so the hanging wall moves at a gentle slope.
Strike slip fault when one section of land slide past the other.Like a base joint on a chop saw.
TYPES OF EARTHQUAKE MOTION TYPES OF EARTHQUAKE MOTION
Compressional (P-Wave) Like a slinky toy.
Shear (S-Wave) Like cracking a whip.
Surface waves Like the waves of the sea.
INTERLUDE D INTERLUDE D
Outer core liquid iron
Inner core solid iron
SOUND TRAVELS FASTER THROUGH LIQUID IRON
CRUSTAL DEFORMATOIN CRUSTAL DEFORMATION
Undeformed cracked, but not bent of faulted
Deformed broken or folded
STRAIN STRAIN
Shear Strain Like pushing on the top of a deck of cards and moving
Tension Streching of the crust
Strike slip horosontal shear stress
Hydrodynamic Compression in all directions
Monoclines the funky bend in the earth that has a "V" and a plunging line
Dome: Oldest rocks in the? center
Basin: Yongest rocks in the? Center!!!!!!!!!!!!!!!
INTERLUDE E INTERLUDE E
How to... create a fossil
step one kill animal
step two put animal in enviroment with no Oxygen or Decay
step three Wait for minerals to be replace with SILICA
ALL DONE!!!! ALL DONE!!!
Paleontologyists they clssify fossils based on MORPHOLOGY
RELATIVE AGE OF FOSSILS RELATIVE AGE OF FOSSILS
ROCK BEDS HAVE DISTINCT ASSEMBLAGE OF FOSSILS
Assemblage is recognized world wide
fossil assemblage alows pale peoples to identify relative age
STUDY GEOLOGIC TIME SCALE OF FOSSILS STUDY GEOLOGIC TIME SCALE OF FOSSILS
CHAPTER 10 CHAPTER 10
Uniformitarianisim: the present is the key to the past
Sediments are deposited horizontally
the rocks on the top are the youngest. :P
Sediment are deposited in continuous sheets
features that cut through layers are yoounger
A layer containing pebbls is _____ than the adjacet layer. youger
Principle of fossil sucession certain fossils stay within their certin layers
SEQUENCE OF EVENTS SEQUENCE OF EVENTS
REMEMBER: plutons and dikes are younger than the layers.
UNCONFORMITIES UNCONFORMITIES
Angular Unconformity two rock beds collide at angles
NON Conformity Horizontialish conformity between two rock beds
Dates to know Dates to know
Uniformitarian Age of Earth 4.55 Billion Years old
Limits to radiometric dating Limits to ratiometric dating
Only certain minerals are radioactive
Igneous and metamorphic rocks are the best candidates
SED Rock not datable
Created by: mr.vonlipich
Popular Physical 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