science vocab terms Flashcards
the relatively thin part of the earth’s crust which underlies the ocean basins. It is geologically young compared with the continental crust and consists of basaltic rock overlain by sediments.
oceanic crust
the relatively thick part of the earth’s crust that forms the large landmasses. It is generally older and more complex than the oceanic crust.
continental crust
is the section of the Earth’s interior that begins below the crust and ends above the transition zone. This boundary starts directly beneath the oceanic and continental crust.
upper mantle
known for his theory of continental drift, he was a meteorologist, geophysicist, and polar researcher.
Alfred Wegner
a supercontinent that included almost all landmasses on Earth. It broke up because of the convection currents that rolled over in the upper mantle causing plates to slowly move across Earth’s surface
Pangea
the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth’s seismic activity occurs at the boundaries of these plates.
plate techtonics
plates that move AWAY from each other causing mid ocean ridge
divergent
plates that move together causing mountains, volcanoes, or subduction zones from large trenches, and sometimes earthquakes
convergent
plates that slide past each other, when stuck it can cause Eathquakes
Transform
a large plume of hot mantle material rising from deep within the Earth
hot spot
process by which heat is transferred by movement of a heated fluid such as air or water.
convection currents
the formation of new areas of oceanic crust, which occurs through the upwelling of magma at midocean ridges and its subsequent outward movement on either side.
seafloor spreading
a lowland region that forms where Earth’s tectonic plates move apart, or rift. they are created by the process of seafloor spreading.
rift valley
the gradual movement of the continents across the earth’s surface through geological time.
continental drift
the upper layer of the earth’s mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur.
asthenosphere