Tectonics Flashcards
What is a tectonic hazard?
A natural event formed by tectonic processes which has the potential to threaten both life and property.
What are the three types of plate boundary?
- Divergent
- Convergent
- Conservative
Example of divergent plates
North American and Eurasian
Example of convergent boundary
Nazca and South American
Example of conservative boundary
North American and Pacific
Features of a divergent boundary
- Shallow earthquakes
- Volcanic is the eruptions - effusive
- Rift valleys
- Runny basaltic lava
- Gassy eruptions
- Mid Ocean Ridge
- Transform faults
- Island volcanoes
Features of a convergent boundary
- Medium to deep earthquakes
- Fold mountains
- Ocean trenches
- Explosive volcanoes (oceanic to continental)
- Batholiths - a mass of intrusive igneous rock (continental to continental)
- Dangerous eruptions of viscous lava
- Pyroclastic flows
- Slab pull
Features of a conservative boundary
- Medium to shallow earthquakes
* Some show a pattern of earthquakes - transform faults
Why is the lava viscous at a convergent oceanic to continental boundary?
- Introduction of silica from millions of years of sediment and sand deposited onto the ocean bed.
- The partial melting of the continental crust.
What is the Benioff Zone?
Area of seismicity that relates to the slab pull of a plate as it subducts below another
Why is there no volcanic activity at a continent to continent convergence?
The lava is too viscous
Why is there no ocean trench at a continent to continent convergence?
There is almost no subduction due to buoyancy of the continental crust
What are intraplate earthquakes?
They occurs in the middle of tectonic plates where the pressure of the plate being squashed and forced to move builds up and is released through the cracks in the rocks associated with fault zones.
This results in an earthquake.
Example of intraplate earthquake
New Madrid between 1811-1812 4000 earthquakes were recorded.
1811 - 7.5
1812 - 7.3
1812 - 7.5
Earthquakes at the North American plate
Faults were left after North America split from Rodina.
When the plate is under strain as the plates move, the fault zone takes some of the brunt and releases strain energy in the form of earthquakes.
The crust
- The thinnest layer - 75km
- Relatively cold
- Solid but brittle
- Oceanic and continental
The lithosphere
Top layer of crust
The Asthenosphere
- Top layer of crust
* Where the convection currents are
What is rheid?
Molten/semi solid
The core
Mostly nickel and iron
The inner core
- Solid
* Under intense pressure
The outer core
- Liquid/molten
* 4000 - 6000 ‘C
The mantle
The largest section
The inner mantle
- Mostly non metals
- Solid because of high pressures
- 3000’C
The outer mantle
- Bottom layer is liquid rock - 1400-1300’C
* Upper layer is rheid - lower temperature
What is ridge push
Magma that rises pushes the plates apart.
It is a continuous process which is thought to have lead to sea floor spreading.
What is slab pull?
- Gravitational pull of subducted lithosphere is a driving force of plate movement
- Cold, dense lithosphere sinks at an ocean trench, pulling the rest of the plate with it
What is sea floor spreading?
When convection currents force the plates to move apart and material rises
Fissure eruptions
Evidence of active rifting on MOR.
The lava is basalt
What is palaeomagnetism?
- The earth traps any iron and lines itself with the north pole at that time
- Magnetic field reverses roughly 4 times every million years
- A striped pattern is left behind - white stripes showing the reversal
What is happening to the MOR?
- The crust either side of the MOR is moving apart
* Radiometrically date them to calculate the rate of spreading
What is magnitude?
The size or extent of an event.
Each unit releases about 32 times more energy.
Hotspot volcanoes
- Occur in the centre of plates
- The surface expression for a mantle plume in the centre of a plate
- E.g. Hawaii
What is a mantle plume?
Stationary area of high heat flow from the mantle, which rises from depth and produces magma that feeds a hot spot volcano.
Factors affecting magnitude
- Seismic gap
- Types of movement/boundary
- Depth of the focus
What is a seismic gap?
Time period since last earthquake
Earthquake waves
- Primary waves
- Secondary waves
- Love waves
Primary waves
- Arrive first
- Compression and extensional movement
- Travel within the Earth
Secondary waves
- Arrive second
- Up-down movement
- Travel within the earth
Love waves
- Arrive last
- Long waves
- Surface waves
- Most damaging waves
Secondary hazards of earthquakes
- Liquefaction
- Landslides
- Tsunamis
Liquefaction
- Waves cause water pressures to increase in sediment and grains to lose contact with each other
- Water saturated sediment temporarily loses strength and acts as a fluid
- The most vulnerable areas are bays or marshland that we’re pumped with material
Landslides
- Large mass of material moves downslope
- Can be triggered by liquefaction
- 87,000 killed in Kashmir in 2005
Tsunami
- Wave of water which is usually caused by an earthquake.
* Usually caused by a dislocation of a larger section of crust on the sea floor, causing displacement of water.
Primary hazards of volcanoes
- Lava flows
- Pyroclastic flows
- Ash flows
- Gas eruptions
Secondary hazards of volcanoes
- Lahars
* Jokulhaups
Lava
- Viscosity is determined by temperature and chemical composition
- Hotter, low-silica lava flows fastest