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Earth Science

Earth Science revision

TermDefinition
earths four layers crust, mantle, outer core, inner core
2 types of crust oceanic and continental
oceanic crust thickness 5km to 10km
continental crust thickness 30km to 50km
the deeper you go into earth the more pressure there is
pangaea the name of the original landmass on earth
convection currents when warm molecules rise and cool molecules sink
the mechanism for crust movement convection currents in the mantle
divergent boundary plates move away from each other
convergent boundary plates move towards each other
transform boundary plates slide past each other
oceanic crust density more dense
continental crust density less dense
subduction when one plate gets pushed underneath another plate
features at subduction zones oceanic trenches and volcanoes
continental vs oceanic plate the oceanic plate gets pushed under the continental plate
oceanic vs oceanic plate the denser oceanic plate will be subducted under the other oceanic plate
continental vs continental plate earths crust crumples together and pushes upwards
subduction zone example Mariana Trench
convergent boundary example the Himalayas
oceanic divergent boundaries as the magma rises between the spreading plate it cools and creates more crust
features at oceanic divergent boundaries mid ocean ridges and underwater mountains
seafloor spreading divergent plates creating new sea floor
mid Atlantic ridge the largest mountain range in the world and is formed by divergent plate boundaries
features at divergent boundaries earthquakes, fault lines, rift valleys
divergent boundary example the red sea
transform boundary example the San Andreas fault
plate movement causes volcanoes to form and erupt, earthquakes, tsunamis
Alfred Wegener he proposed that originally all the continents were once connected to each other
continental drift evidence continents fitting together like a puzzle, same fossils and plants found on different continents, mountain ranges with identical age and structure on different continents, ancient climates
Marie Tharp she discovered and mapped the mid ocean ridge and matched this with the vast majority of earthquakes
first 2 continents of Pangaea Laurasia and Gondwana
Why Australia has unique plants and animals Gondwana separated from Laurasia 200 million years ago, causing the plants and animals to develop independently
the ring of fire a string of volcanoes and earthquake sites around the edges of the pacific ocean
earths magnetic field created by the movement of earths molten iron and nickel core
magnetic stripping when magnetic poles flip so does the alignment of magnetite particles in the sea floor
magma molten rock below earths surface
lava molten rock above earths surface
Created by: justineforrest
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