Unit 2 Lesson 2 Flashcards
Relative dating
Determining whether an object or event is older or younger than other objects or events
Law of superposition
States that younger rocks lie above older rock if the layers have not been disturbed
Tilting
Happens when Earth’s forces move rock layers up or down unevenly.
The layers become slanted
Folding
The bending of rocks that can happen when rock layers are squeezed together
Fault
Intrusion
A break or crack in earth’s crust where rocks can move
Igneous rock that forms when magma is injected into rock then cools and becomes hard
Unconformity
A break in the geologic record that is made when rock layers are eroded or when sediment is not deposited for a long period of time
Fossils
The traces or remains of an organism that lived long ago most commonly preserved in sedimentary rock
Geologic column
An ordered arrangement of rock layers that is based on the relative ages of the rocks with the oldest rocks at the bottom of the column
Law of Original Horizontality
Sedimentary rock layers are deposited horizontally. If they are tilted, folded, or broken it happened later
Law of Cross-Cutting
If an igneous intrusion or a fault cuts through existing rock, the intrusion/fault is younger than the rock