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

Geologic Time

TermDefinition
Molds and casts Acids eat away the skeleton or shell and leave an impression in the rock. If the mold fills with minerals, it becomes a cast.
Tracks and trails Imprints are left in the mud, which later hardens. Dinosaur tracks are fairly common,
Carbonization Oils leave the plant and the remaining matter becomes a layer of carbo. In other cases nitrogen, hydrogen, and oxygen are distilled from the plant. Most common method of fossilizing plants.
Petrifaction Minerals in the plant cells crystalize; minerals enter openings or cavities in shells or bones. Common with plants.
Replacement Object buried in mud has its molecules replaced by minerals. It is rare.
Recrystallization Mineral aragorite in shells turns to calaite. Preserves the general shape of the animal.
Soft tissue preservation Mummification, frozen in ice. Fossils are relatively young and do not last long.
Traps Whole organismslocked in tar pits, asphalt, amber, ect.
Fossils Are the imprints or remains of organisms that were once alive. They provide evidence for the Geologic Time Scale.
Cenozoic Quaternary, teriary, halocane, pleistocane, pliocene, miocene, oligocene, eocene, palocene
Mesozoic Cretaceous, Jurassic, Triassic
Palezoic Permian, Carboniferous, Devonian, Silurian, Ordovician, Cambrian
Proterozoic Archaeon, Hadean, Precambrian
Eon The largest group; divided by the Cambrian Boundary (about 550 millions of years ago) when the variety of life forms exploded; billions of years long.
Era Mass extinctions mark the boundaries between the eras; hundreds of millions of years long.
Period Blocks of time when a unique rock series was laid down; tens of millions years long.
Epoch Divisions of the most recent periods; sereral million years long.
Humans Eon: Phanerozoic, Era: Cenozoic, Period: Quaternary, Epoch: Holocene, Years Ago: 11,000-Present
Rise of Mammals Eon: Phanerozoic, Era: Cenozoic, Period: Tertiary, Epoch: Paleocene, Years Ago: 65-54
Birds Eon: Phanerozoic, Era: Mesozoic, Period: Jurassic, Years Ago: 208-146
Created by: kelseylyall
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