Tectonics enq 1 Flashcards
Four types of plate margins with examples
Destructive - Montserrat, Constructive - Mid Atlantic ridge, Conservative - San Andreas Fault, Collision - Himalyas.
What is Ridge Push and Slab Pull?
- As the lithosphere thickens with distance away from the MOR, it cools and the boundary becomes deeper and slopes away from the ridge due to gravity, this weight produces a downward force, so the asthenosphere ‘pushes’ the older part of plate in front of it.
- With distance the lithosphere becomes cooler and denser, after subduction the cool, dense lithosphere sinks into the mantle under its own weight, pulling the rest of the plate down with it.
What 5 factors is Plate tectonic theory driven by?
- Mantle Convection
heat rises from core as it rises it cools becoming denser before sinking back into core to be heated again - Slab Pull
- Seafloor Spreading/ Palaeomagnetism
as new crust is formed at MOR plates are pushed apart as convection currents are the crust apart them apart, magnetic orientation evidences this. - Subduction
the earth isn’t expanding despite new crust being created as it is being destroyed by subduction as the end plate sinks beneath the continental plate.
Evidence for Plate tectonic theory
Continental drift, Palaeontology, Palaeomagnetism, Climate Change, Geography and Geology.
Intra-plate Earthquakes and Volcanic Hotspots
EQ - near the middle of plates as a result of solid crust cracking as it travels over millions of years
VH - result of upwelling of magma (mantle plume) forming volcanic hotspots
Name three different types of volcanoes
Basaltic, Andestic, Rhyolitic
Basaltic Volcano properties
1200 degrees, Very hot iron rich and silica poor, low gas content, can erupt continuously and not very explosive
Andestic Volcano properties
800 degrees, Hot iron poor silica rich, increased gas content, sticky, can be very explosive
Rhyolitic Volcano properties
600 degrees, Cooler lava iron poor and silica rich, very high gas content = very combustible, devastating but erupt rarely
Name 4 volcano primary hazards
Lava flows, Pyroclastic flows, Ash fall, Gas eruptions
Name 2 volcano secondary hazards
Lahars and Jökulhlaup
Case study: Montserrat Volcano
- minor eruptions preceded swarm of eqs
- pyroclastic flows meant that people had to evacuate the capital
- the ash covered two thirds of island
- social environmental and economic damage
What are lava flows
Stress of molten rock that pour from an erupting vent. The speeds at which it moves depends on type of lava and its viscosity
What are Jökulhlaups
‘Glacial outburst floods’
They occur when volcanoes and glaciers interact, they can occur anywhere where water accumulates in a subglacial lake beneath the glacier filling a caldera (volcanic crater). The ice cap can push the water out of the caldera
Case study: Jökulhlaups at Eyjafjallajökull, Iceland
- erupted April 2010
- disrupted flights across Europe - global impact
- Further eruptions generated more jökulhlaups that inundated an Icelandic town resulting in its evacuation
Define pyroclastic flows
Dense, fast moving flow of solidified lava pieces, volcanic ash and hot gases can be extremely dangerous and result in flooding.
Define ash fall
A rain of airborne ash resulting from a volcanic eruption
Define Gas eruption
eruption of carbon and sulphur dioxide with can poison people and animals in extreme cases. Occurs at subduction zones
