Chapter 8: Dynamic Earth Flashcards
Plate tectonics
the theory concerning the movement of the continental plates
Mantle
thick layer inside the Earth, below the crust. Most of the mantle is solid rock, although the upper part is molten rock called magma.
Convection currents
circular movement that occurs when warmer, less dense fluid particles rise and cooler, denser fluid particles sink
Continental Crust
circular movement that occurs when warmer, less dense fluid particles rise and cooler, denser fluid particles sink
Oceanic Crust
one of the types of crust that makes up the Earth’s outer layer. Oceanic crust is thinner than continental crust and made up of dense, heavy rocks such as basalt.
Subduction
one of the types of crust that makes up the Earth’s outer layer. Oceanic crust is thinner than continental crust and made up of dense, heavy rocks such as basalt.
Destructive plate boundaries
a convergent boundary where two plates collide
Constructive plate boundaries
plate that creates new land from cooling magma
Ocean ridges
an area where the tectonic plates move apart, allowing magma from the mantle to rise, forming underwater volcanoes and creating new oceanic crust as it is cooled and solidified by sea water
Conservative plate boundaries
Solid crust is neither created nor destroyed at these boundaries. The San Andreas Fault is perhaps the best known example of a boundary between sliding plates.
Laurasia
one of the two smaller continents created when the supercontinent Pangaea broke apart about 200 million years ago
Gondwanaland
one of the two smaller continents created when the supercontinent Pangaea broke apart about 200 million years ago
Hotspots
regions in the crust where rocks in the upper mantle melt and magma surges upwards into the crust. Hotspots occur within plates. The active volcanoes in the Hawaiian Islands are caused by hotspots. The old volcanoes of Australia are also the result of hotspots.
Folding
buckling of rocks caused when rocks are under pressure from both sides
Anticlines
folds that bend upwards
Synclines
folds that bend downwards