Volcanoes found away from the plate boundary, due to a magma plume closer to the surface
Ash
Fine particles and dust ejected during an eruption, which can remain airborne as clouds or accumulate on the ground
Degg’s Model
This model shows that a hazard becomes a disaster if it affects a vulnerable population
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
Asthenosphere
The upper mantle layer of the Earth. It is semi-molten and approximately 2000km wide
Hazard Mitigation Cycle
The sequence of governance of a natural hazard: monitoring & prediction, mitigation, preparedness
Epicentre
The point on the surface, directly above the earthquake's origin
Continental Crust
Crust that forms the continents of the lithosphere, on average 35km thick
Accretion Wedge is the accumulation of material at the point of subduction
Focus
The place in the crust where the pressure/seismic energy is released
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
Aseismic Buildings are designed to withstand or minimise destruction during an earthquake
Natural hazards
Hot Spot
Jokulhaup
Lahar
Oceanic Crust
Crust, usually thinner than continental crust, that forms the sea floor. It is on average 7km thick
Love Waves
A surface earthquake wave with horizontal displacement
A sudden glacial flood caused by a glacier on top of or near a volcano melting due to the heat from the eruption
Paleomagnetism
The alternating polarisation of new land created. As magma cools, the magnetic elements within will align with the Earth’s magnetic field, which can alternate over thousands of years
Volcanoes found away from the plate boundary due to a magma plume closer to the surface
A measure of an earthquake's energy released, considered the most accurate measure
Primary Waves
An earthquake wave causing compressions within the body of rock
Lithosphere
The upper crust of the Earth (average thickness = 100km)
PartialMelting
Elements within the lithosphere have different melting points, and so rock is partially melted, partially solid
Geological features
Mid-Ocean Ridge
Oceanic Crust
Pyroclastic Flow
A mixture of gases and rock fragments, at high temperatures and speeds, that flows down the slopes of a volcano during an eruption
A flow of mud and debris
Governance of a natural hazard
Monitoring & prediction
Mitigation
Preparedness
Park’s Model
A model describing the decline and recovery of a country over time, following a natural disaster
Parting oceanic plates at a constructive plate boundary creates a ridge, with new land at the base of the oceanic valley
Richter Scale is a logarithmic measure of earthquake’s intensity
Tsunami is caused by initial vertical water displacement (often from a submarine earthquake) creating waves with large destructive power
Types of seismic waves
Primary Waves
Secondary Waves
Love Waves
Rayleigh Waves
Volcanic Explosivity Index (VEI)
A measure of the magnitude of a volcano’s eruptions
Seismic Waves are the energy released during an earthquake, in the form of Primary, Secondary, Love and Rayleigh Waves
Subduction
Oceanic plate is forced below continental plate, due to the oceanic plate being more dense than the continental plate
Rayleigh Waves
A surface earthquake wave causing both horizontal and vertical displacement
Wadati-Benioff Zone
A region of the subducting plate, most affected by pressure and friction, where most destructive margin earthquakes originate
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
Slab Pull
The force contributing to the movement of tectonic plates.SlabPull is due to the weight of the plate
Secondary Waves
An earthquake wave causing vertical displacement within the body of rock