Unit 14 Flashcards
Plate tectonics & earthquakes
•Continents seem fixed from human perspective. Until the mid-twentieth century, scientists believed Earth’s continents were rigid
Continental Drift
continents move on Earth’s surface; Alfred Wegener proposed this idea in 1912; Pangaea
Plate Tectonics
Theory behind motion of lithospheric plates; plates float on the ATHENOSPHERE
(get tectonic plates image form slides)
Convection
transfer of heat through a fluid; the asthenosphere bubbles up and encounters the crust which leads it to fracture the crust.
mid-oceanic ridges
formed by magma rising up from mantle
sea floor separates
new basaltic crust created
ocean trenches
sea floor comes together; older lithosphere descends into the asthenosphere where it is recycled
Plate Boundaries
the border between two plates
Divergent
moving away from each other; constructive; mid-oceanic ridge; youngest crust
Convergent
moving towards each other; destructive; collisions
oceanic-continental (destructive)
A) oceanic plates sink since it is more dense
B) forms oceanic trench and continental mountains (cascades &Andes)
C) earthquakes occur along margin
D) volcano formation along the plates (continental volcanic arc)
E) forms metamorphic rocks-blueschist
oceanic-oceanic (destructive)
A) subduction results in undersea trench formation
B) deep and shallow earthquakes
C) island volcanic arc
continental-continental
A) no subduction since two plates are highly buoyant
B) builds huge mountain ranges
C) volcanoes are rare
D) shallow earthquakes are relatively common
E) examples: Himalayan mountains
Transform (Stripe-slip)
slide against one another; neither creates nor destroys crust; commonly produce shallow earthquakes; San Andreas fault line (right lateral transform boundary)
Fault
a crack in the Earth’s surface