Tectonic Hazards Flashcards
Plate margin
the line between two or more different tectonic plates
Earthquake
the earth shaking due to seismic waves travelling through from an epicentre
Volcano
a mountain that has magma inside that could erupt
Shield volcano
a volcano that is much flatter than usual and usually has runnier lava. they are formed at constructive plate boundaries
Composite volcano
formed through subduction at a destructive plate margin, usually between oceanic and continental plates has thick lava and is steep
Tectonic plates
segments of the earth’s crust that slid around on top of the mantle
Core
the centre of the earth, split into the inner which is made from solid nickel and iron and the outer which is a liquid
Crust
the very tip of the earth, made from oceanic and continental plates
Mantle
thickest layer of the earth made from magma that is constantly moving, has a similar consistency to treacle
Convection current
the circular motion which is created when hot fluids rise then cool as they move along and then drop
Oceanic crust
thinner but heavier (more dense) than continental crust, 6-8km thick and made from basalt
Continental crust
thicker but lighter (less dense) than oceanic crust 30-50 km thick and made from granite
Hot spot
volcanic regions that are fed by underlying mantle which is hotter than the surroundings
Conservative margin
plates slide past each other and lock, the pressure builds up and suddenly they snap loose, shockwaves cause earthquakes on the surface
Constructive (transform) margin
two plates move apart, as this happens magma rises to fill the gap which causes volcanoes. on each side the crust has big cracks called faults where the magma can escape so the volcanoes are less powerful (shield)
Destructive margin (oceanic-continental)
an oceanic plate collides with a continental plate which forces the oceanic plate to be pushed under and melts, which releases energy sometimes creates earthquakes from the friction, volcanoes or fold mountains are formed
Collision/destructive margin (continental-continental)
they have the same density so are forced upwards very powerful and destructive earthquakes that can trigger landslides and fold mountains are created
Subduction
when the denser oceanic plate is pushed under the continental plate and melts into the mantle
primary effect
the impact that it has in the following few days initially
secondary effect
the more long term impacts that often last much longer
immediate response
the help that is given straight after an event has happened
long term response
systems that are put into place because of the event or things that continue to happen well after the incident has happened
monitering
watching the volcanoes or data collecting to know what is happening so that you can prepare for an event
prediction
using the data to estimate when an event might happen so people can be evacuated