Hazardous Earth Flashcards
What are Plate Tectonics?
Plate tectonics is the scientific theory that Earth’s lithosphere comprises a number of large tectonic plates, which have been slowly moving since about 3.4 billion years ago.
Jigsaw fit
Some continents fit together like a geological jigsaw
puzzle. All the rocks were formed when the land was a single continent – Pangea.
What was the one big large mass called created by Alfred Wegner?
Pangaea
What is Continental drift?
The idea that continents are slowly shifting their positions
Convection currents
In the Mantle, Convection Currents were found to be slow yet extremely powerful
movements of volcanic rock in the mantle. The magma is heated to 50000C in the
mantle and rises to the crust where they cool and sink only to be heated again. The
process continues. This was powerful enough to move the earth’s plates.
Study of fossils
Similar fossils are found on different continents. This is evidence that these regions
were once very close or joined together. Such species could not have crossed
oceans, so they must have lived on the same land mass at some time in the past.
Where was the bones of the reptile Mesosaurus found?
The bones were forund in southern Africa and the southern part of South America.
Geological patterns
Similar pattern of rock
layers on different
continents is evidence that
the rocks were once close
together or joined.
Oceanic crust
plate that is made up of more dense rock. It sinks easily due to its
density and is constantly created at boundaries. It is ‘young/new
rock’ and forms our ocean bed.
Subduction zone
where one plate is forced downwards below another plate and
grinds past it causing huge amounts of friction and heat.
Destructive plate boundary
where two plates are moving towards each other, one of which is
continental crust and one is made of oceanic crust
Continental crust
this is a plate that is made up of less dense rock. Because it is less
dense it doesn’t sink. It is exceptionally old and makes up our land
surfaces.
Plate boundary
where two very large crustal plates meet on the earth’s surface.
Earthquakes and volcanoes happen here.
Fold mountains
are large mountain ranges formed by the collision and ‘folding’
of two plates as they plates continually push into one another.
Ocean trench
a particularly deep point of the ocean bed where the oceanic and
continental crust have dragged each other downwards.