Tectonics Flashcards
The crust
Added to by sedimentation and dead sea creatures. As no metals are involved it is able to ‘float’ on the mantle.
Why is the core metal?
As the Earth cooled, denser materials like iron and nickel sank. It’s kept solid by the pressure of all the layers.
Description of constructive margin
-Core heats magma, rises to asthenosphere
-Cannot break through so moves parallel
-Plates are dragged apart
-Ridge push as plates are pushed up in the middle and their weight pushes them apart
-Slab pull where the other end of the plate is on a destructive margin
-Mid Atlantic ridge
Paleomagnetism
Study of magnetic rock to record history of the magnetic field
Continental drift (pangea) and evidence for
Alfred Wegner 1915
-Jigsaw fit
-Geology that seems to be the same across continents
-Fossil evidence
Crust characteristics
400 C
Less dense
Granite & basalt
Solid
Mantle characteristics
870 C
Less to medium density
Upper=olivine Lower=magnesium silicate
Liquid & solid
Outer core characteristics
4400-6100 C
Dense
Iron & sulphur
Liquid
Inner core
7000 C
Very dense
Iron & Nickel
Solid
Effusive
Runny
Description of destructive margin
-Oceanic plate is subducted (slab pull)
-Fold mountains, as plate concertinas
-Melted rock & gas in subduction zone
-Great pressure so magma rises to make volcanoes, these are explosive
-Many shallow and deep EQs with benioff zone going deep
-Nazca and SA plates
Description of continental collision margin
-Neither subducts so no volcanoes
-Crumple upwards to make fold mountains
-EQs mainly on boundary and are very violent, also intra-plate as plates deform
-The Alps (African and Eurasian)
Description of transform margin
-Plates move parallel
-No subduction so no volcanoes
-Many shallow EQs
-Elastic rebound
-San Andreas Fault
Elastic rebound
Plates get stuck at the margin so start to bend. Snap back to original shape in new locations.
Formation of island chains
-Hotspot in oceanic plate
-Outpouring of basalt makes land
-Plate moves so creates island in new spot
-Hawaii