Chapter 13 - Drifting Continents: Plate Tectonics Flashcards
pangaea
supercontinent; previously-single large land mass
laurasia
landmass that would eventually become North America, Greenland, and Eurasia
gondwana
landmass that would eventually become South America, Australia, Africa, India, and Antarctica
continental drift
theory by Alfred Lothar Wegener proposing that continents move slowly across Earth’s surface
plate tectonics
theory describing the origin, movement, and recycling of lithospheric plates and the resulting landforms
subduction
a process in which oceanic lithosphere of one plate bends and dives into the mantle beneath another plate
plate boundaries
the place where lithospheric plates meet
active continental margin
follows a plate boundary
passive continental margin
has a broad sloping continental shelf and does not coincide with a plate boundary
ridge push
the process by which magma rising along a mid-ocean ridge lifts oceanic lithosphere and forms a slope
mantle drag
caused by convection within the asthenosphere
slab pull
the weight of the subducting portion of a plate accelerates plate movement by pulling the plate deeper into the mantle
divergent plate boundary
occurs where two plates move apart
convergent plate boundary
occurs where two plates move toward each other
transform plate boundary
occurs where one plate slips laterally past another