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