Chapter 8-Dynamic Earth Flashcards
Continental drift
movement of the plates of the Earth’s crust in relation to each other
Pangaea
a super-continent that existed about 225 million years ago. All of the landmasses that existed at this time were joined together to form this super-continent.
Panthalassa
the vast sea surrounding the supercontinent of Pangaea
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 Current
circular movement that occurs when warmer, less dense fluid particles rise and cooler, denser fluid particles sink
Continental Crust
the plates of the Earth’s crust that make up the land
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
process in which two tectonic plates push against each other, and oceanic crust sinks below the less dense continental crust
Destructive Plate Boundry
a convergent boundary where two plates collide
Constructive plate
plate that creates new land from cooling magma
Seismic Waves
Seismic waves: waves of energy that travel through the Earth’s crust, caused by earthquakes
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
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
a localised place where an activity occurs
Folding
buckling of rocks caused when rocks are under pressure from both sides
Anticlines
Folds that bend upwards
Synclines
folds that bend downwards
Fault
a break in a rock structure causing a sliding movement of the rocks along the break
Rift valleys
a sunken area where two blocks of crust have dropped down between faults
Horst
a block of the Earth’s crust, with faults on either side, that has been pushed upwards by the forces below
Slip fault
a geological feature where movement along a fault is sideways—that is, where the blocks of crust slip horizontally past each other
Tremors
vibration on the Earth’s surface caused by an earthquake
Epicentre
the point on the Earth’s centre directly above the site where an earthquake originates
Focus
the point at which an earthquake begins