Term
|
Definition
continents drifted to current location (from Pangaea) |
|
|
Term
who proposed the continental drift theory? |
|
Definition
proposed by Wegner in 1912 |
|
|
Term
what were the problems of the con. drift theory? |
|
Definition
he didn't have proof and he didn't have an explanation. |
|
|
Term
fossil clues of con. drift theory |
|
Definition
similar plant and animal fossils found on both sides of the Atlantic |
|
|
Term
climate of con. drift theory |
|
Definition
glacial evidence in warmer climates fossils of ferns in cold climates |
|
|
Term
climate clues of con. drift theory |
|
Definition
glacial evidence in warmer climates fossils of ferns in cold climates |
|
|
Term
rock clues of con. drift theory |
|
Definition
similar rock types found on both sides of the Atlantic Ocean |
|
|
Term
|
Definition
molten rock pushed thru at mid-Atlantic Ridge |
|
|
Term
seafloor spreading proposed by henry hess (1960's) |
|
Definition
proof newer rocks near mid-Atlantic Ridge magnetic clues in rocks |
|
|
Term
|
Definition
crustal sections (plates) move around on mantle |
|
|
Term
|
Definition
plates move by convection current |
|
|
Term
|
Definition
|
|
Term
|
Definition
|
|
Term
|
Definition
two continental (less dense) plates collide (ex. India and Asia) |
|
|
Term
|
Definition
denser oceanic plate goes under less dense continental plate (ex. California Coast) |
|
|
Term
|
Definition
|
|
Term
|
Definition
two oceanic plates move apart (ex.- mid-Atlantic ridge |
|
|
Term
|
Definition
two continental plates move apart (ex. - E. African rift valley) |
|
|
Term
|
Definition
plate slide by each other- ex. - San Andreas fault (California) |
|
|
Term
|
Definition
vibrations that rocks produce when they break |
|
|
Term
|
Definition
surface that rocks move along when they break |
|
|
Term
|
Definition
caused by rock above the fault moving downward in relation to he rock below the fault |
|
|
Term
|
Definition
compression forces squeeze rock above the fault up and over the rock below the fault |
|
|
Term
|
Definition
rocks on either side of the fault move past each other without much upward or downward motion |
|
|