Introduction to Tectonics and Folds Flashcards
Tectonics
The branch of geology which deals with the large scale structures of the Earth and the processes that have produced them
In plate tectonics which of the Earth’s layers are moving and in response to what
Lithosphere moves horizontally over the hotter, semi-plastic asthenosphere in response to gravity and friction
What are the three types of plate boundaries
- Divergent boundaries
- Transform boundaries
- Convergent boundaries
What happens at divergent boundaries and what are they characterised by
Plates move away from each other and they are characterised by mid-ocean ridges and continental rift zones
Process of ocean forming at divergent boundaries - beginning
the thick continental crust insulates the mantle causing partial melting of the mantle and the rise of more buoyant material which is the cause of continental breakup
Process of ocean forming at divergent boundaries - Stage 1
Stage 1: rising magma causes crustal upwarp which stretches and thins the crust leading to basaltic magma from the mantle erupting at the surface forming an incipient rift
Process of ocean forming at divergent boundaries - Stage 2
A rift develops leading to the continental crust breaking and basaltic lava fills the rift
Process of ocean forming at divergent boundaries - Stage 3
A narrow sea develops which is the beginnings of a new mid-ocean ridge. The oceanic crust is more developed and the continents are still relatively close
Process of ocean forming at divergent boundaries - Stage 4
An ocean basin is formed in the well developed mid-ocean ridge as the continents are widely separated
What happens at drivers
- ridge push at elevated ridge
- slab pull at trench - old, cold, dense lithosphere
- convection
What happens at transform boundaries and what are they characterised by
- plates move past each other
- characterised by large faults or faults along mid-ocean ridges
- intense seismic activity
What happens at convergent boundaries and what are they characterised by
- earth isn’t expanding so creation of lithosphere must be balanced by destruction
- subduction occurs as plates move towards each other and old lithosphere is consumed
- characterised by ocean trenches, volcanism, earthquakes and metamorphism
Oceanic - Oceanic subduction
- subduction zone where two plates of oceanic lithosphere converge
- one plate dives into mantle
- characterised by ocean trenches and volcanic island arcs
- Produces basalt (& andesite) (mafic)
Oceanic - Continental subduction
- subduction zone where one plate of oceanic lithosphere and one plate of continental lithosphere converge
- oceanic plate dives into mantle - more dense
- characterised by oceanic trenches, volcanic mountain range and metamorphism
- produces andesite (intermediate)
Continental - Continental subduction
- subduction zone where two plates of continental lithosphere converge
- continental lithosphere cannot be subducted - too thick, low density
- plate motion taken up by intense deformation
- characterised by mountain ranges, plateaus, intrusions and metamorphism
- produces granite (intrusions) and rhyolite