plate tectonics Flashcards
solid nickel and iron
about 1000km thick
inner core
liquid
iron
2000 km thick
outer core
iron-rich Rock
about 3000 km thick
semi-solid
top of mantle called the asthenosphere
mantle
Rock/ crust
maximum thickness is about 100 km
lithosphere
proposed by wegener
noticed shape of continents, mountain ranges animal distribution
continental drift
multiple super continents most recent all land Atlantic Ocean is getting bigger Pacific Ocean is getting smaller
Pangea
made of basalt
dense
oceanic plates
made of granite
less dense
continental plates
crust rests on the mantle
upper mantle is called the asthenosphere
convection currents
partially melted
moves slowly
moves crust
asthenosphere
compression of plates
converge
tension
pull apart
diverge
slide past eachother
transform
ocean plate is pushed under the crust
subduction
occurs when plates collide
boundary
island arc Japan
ocean-ocean subduction.
Andes mountain and volcanoes
ocean-continent subduction
Himalayas and Appalachians
continent- continent
rift zone
new crust is made
ocean-ocean
Rift Valley
continent-continent
new crust is made at the mid-ocean ridge
cooling rock “fossilize” the current magnetic field
seafloor spreading and paleomagnetism