Plate tectonics Flashcards
Plate tectonics:
is a theory addressing the origin, movement, and recycling of lithospheric plates and the resulting landforms.
- Lithosphere is broken into 14 major and minor plates that move over Earth’s surface as mantle beneath them convects.
how do earthquakes occur?
As the plates move they buckle, bend, and warp into mountains, split into valleys, and break, causing earthquakes
Continental drift:
a theory that proposed continents move slowly across Earth’s surface.
- Proposed in 1912 by Alfred Wegener
how did Alfred wegener come up with continental drift theory?
he noticed jigsaw-puzzle fit between east coast of South America and west coast of Africa
and he used evidence from matching rock types on separated continents, deposits of glacial gravels, and fossils of organisms
Pangaea:
“whole land”; a supercontinent that formed 300 million years ago
- Transition from Pangaea to today’s continents occurred in two major steps: opening of Tethys sea and opening of Atlantic Ocean
- Pangaea split into Laurasia and Gondwana about 200 million years ago
Laurasia:
Laurasia: the landmasses that would become North America, Greenland, and Eurasia
Gondwana:
the landmasses that would become South America, Australia, Africa, India, and Antarctica
plate tectonics history
- After World War II, sonar provided new evidence that led to development of theory of plate tectonics
- In 1960, Hess formalized theory of seafloor spreading, which developed into broader theory of plate tectonics
can plates recycle?
yes.
e.g. a new lithosphere forms at mid-ocean ridges, and old lithosphere is recycled deep into the mantle through subduction.
subduction:
the process in which the oceanic lithosphere of one plate bends and dives into the mantle beneath another plate.
plate boundaries:
is the places where lithospheric plates meet
- Fourteen plates
- 7 primary and 7 secondary
- Largest plate is Pacific Plate
what are the 3 types of plate boundaries?
1) Divergent: Where two plates move apart.
2) Convergent: Where two plates move toward each other.
3)Transform: Where one plate slips laterally past another.
the continental margins
Active continental margin: typically consists of deep-sea trench and narrow continental shelf.
Passive continental margin: typically has broad, sloping continental shelf and does not coincide with plate boundary.
Only some plate boundaries follow outlines of continents
Ridge push:
kind of plate movement.
the process by which magma rising along a mid-ocean ridge lifts oceanic lithosphere and forms a slope
Mantle drag:
kind of plate movement.
movement of a plate caused by friction between moving asthenosphere and the lithosphere