Plate margins Flashcards
Seismicity
the frequency, intensity, and distribution of earthquakes in a given area
volcanicity
the process through which gasses and molton rock are either extruded on the earth’s surface or intruded into the earths crust
Constructive plate boundary
- Plates moving apart
- eg Mid-Atlantic ridge
Mid-Atlantic ridge
- 7000km long
- Iceland lies on it, observe volcanoes and high temperature waters
Features found at a constructive plate boundary
- MOR
- Rift valley e.g African Rift valley
- Oceans form in them eg Red Sea
- Continental crust, thinned by erosion, cools contracts and sinks beneath the sea eg Atlantic ocean
Destructive plate boundary
Two plates colliding
Oceanic- oceanic convergence example
Japan, Mt. Fuji
- slower plate carried downwards
- basaltic oceanic plat melts
- Melted minerals separate and rise
- magma erupts at the surface
- Volcanic islands created
- Metamorphasised rocks create island
Oceanic- continental convergence example
The Andes, Nazca sub ducts under S. American
- same process
- more explosive volcanoes as silicic magma creates rhyolitic volcanoes
- large batholiths also form due to melted continental crust
- Fold mountains form due to compression of continental crust
- High mountains with deep roots created
Continental-continental convergence example
Himalayas, India sub ducts under Asian
-shallow and intermediate earthquakes created
-subduction stopped due to no difference in density, plates crumpled together
-Fold mountains created instead
Subduction zone sank beneath collision zone without first feeding volcano
-Granite batholiths created as base of continental crust melted due to its thickness
Conservatize plate boundary
Two plates slide laterally past each other
eg San Andreas Fault
-No subduction
-Shallow focus earthquakes
-Creeping movement of plates
-1906 last big earthquake (8.6 on richter scale) (700 killed)
San Andreas Fault
- 1300km long
- 5cm movement annually
- East pacific plate moves North West
- North American plate moves West North West
Fissures
lines of weakness in plates which allow magma to rise
Where do the most explosive volcanoes occur
Convergent boundaries due to the greatest pressure
Types of Lava
Basalt, Andesite, Dacite, Rhyolite
- Decreasing mobility
- Increasing viscosity
- Increasing silica content
- Decreasing eruption temperature
Volcano classification
- Fissure
- Shield
- Composite
- Acid or Dome
- Caldera