The accumulation of material at the point of subduction
aseismic buildings
buildings designed to withstand or minimise destruction during an earthquake
ash
fine particles and dust ejected during an eruption, which can remain airborne as clouds or accumulate on the ground
continental crust
crust that forms the continents of the lithosphere, on average 35km thick
continental drift
the movement of tectonic plates, due to varying weights of crust. It was originally thought that convection currents caused the movement of the plates, but now Slab Pull is thought of as the primary driving force
convection currents
the circulation of magma within the mantle (asthenosphere). Magma is heated by radioactive processes in the core and cools at the surface, and so circulates between the two places
epicentre
the point on the surface, directly above the earthquake's origin
focus
the place in the crust where the pressure/seismic energy is released
hot spot volcano
volcanoes found away from the plate boundary, due to a magma plume closer to the surface eg Hawaii
jokulhaup
a sudden glacial flood caused by a glacier on top of or near a volcano melting due to the heat from the eruption
lahar
a flow of mud and debris
oceanic crust
crust, usually thinner than continental crust, that forms the sea floor. It is on average 7km thick
partial melting
elements within the lithosphere have different melting points, and so rock is partially melted, partially solid
pyroclastic flow
a mixture of gases and rock fragments, at high temperatures travelling at rapid speeds
seismic waves
the energy released during an earthquake, in the form of Primary, Secondary, Love and Rayleigh Waves
tsunami
initial vertical water displacement (often from a submarineearthquake) creates waves, with large destructive power
volcanic island arc
a series of volcanoes (often in the shape of an arc) that are formed consecutively, as a tectonic plate moves across a magma plume
seismic hazards
Generated when rock within 700km of the surface breaks under stress
magma plume
an area under the crust, the magma melts the crust causing it to come through
Degg’s model
this model shows that a hazard becomes a disaster if it affects a vulnerable population
hazard mitigation cycle
the sequence of governance of a natural hazard: prevention & mitigation, preparation, response and recovery
park’s model
a model describing the decline and recovery of a country over time, following a natural disaster
the pressure and release model (PAR)
The model suggests that disasters are the result of two factors: pressures and vulnerabilities. Pressures are the underlying root causes of disasters eg poverty and inequality. Vulnerabilities are the conditions or factors that make people and communities susceptible to disasters like weak infrastructure, lack of preparedness, and limited access to resources.
asthenosphere
the uppermantle layer of the earth. it is semi-molten and approximately 440km thick
lithosphere
outermost layer of earth (crust and some of upper mantle) around 100km
it moves very slowly all the time and is broken into tectonic plates
love waves
a surface earthquake wave with horizontal displacement
primary waves
an earthquake wave causing compression within the body of rock
rayleigh waves
a surface earthquake wave causing both horizontal and vertical displacement
secondary waves
an earthquake wave causing vertical displacement within the body of rock
slab pull
the force contributing to the movement of tectonic plates. slab pull is due to the weight of the plate
paleomagnetism
the alternatingpolarisation of new land created. As magma cools, the magnetic elements within will align with the earths magneticfield, which can alternate over thousands of years
mid-ocean ridge
parting oceanic plates at a constructive plate boundary create a ridge, with new land at the base of the oceanic valley
richter scale
a logarithmic measure of earthquakes intensity
subduction
oceanic plate is forced below continental plate, due to the oceanic plate being more dense than the continental plate
volcanic explosivity index (VEI)
a measure of the magnitude of volcano eruptions
wadati-benioff zone
a region of the subducting plate, most affected by pressure and friction, where most destructive margin earthquakes originate
moment magnitude scale
a measure of an earthquake’s energyreleased, considered the most accurate measure
sea floor spreading
molten magma is forced up from the asthenosphere and hardens, forms new oceanic crust, the old crust pushed apart
Plate tectonics
A theory that explains large scale movement of the lithosphere (based off evidence from sea floorspreading and paleomagnetism )