Enquiry Question 1: Why are some locations more at risk from tectonic hazards? Flashcards
Seismic hazards
Earthquakes/tremors and associates events
Volcanic hazards
Associated with eruption events
Intra-plate earthquakes
earthquakes that occur away from plate boundaries (middle or interior of tectonic plates)
Volcano
A vent or fissure in the Earth’s surface through which magma and gases are expelled
Divergent plate boundary
constructive plate movement - found at mid-ocean ridges (mostly submarine), linked to shallow focus, low magnitude earthquakes.
Convergent plate boundary
destructive plate movement - subduction or colliding plates linked to seismic and volcanic activity.
Conservative plate boundary
Horizontal plate movement, linked to shallow focus seismic activity.
SiMa
Oceanic crust comprising of silica and magnesium
SiAl
Continental crust comprising of silica and aluminum
Constructive plate movement
Tectonics plates move apart to create new lithosphere
Destructive plate movement
Tectonic plates move towards each other and either subduction, or a collision, occurs
Conservative plate movement
Tectonic plates slide past each other, either in opposite directions or in the same direction but at differing speeds (e.g. San Andreas fault)
Hot spot
Weakness in the lithosphere, which is fed by a mantle plume, resulting in volcanic activity (e.g. Kilauea)
Mantle Plume
heated lower mantle rock that rises toward the lithosphere because it is less dense than surrounding mantle rock
Theory of Plate Tectonics
Earth’s lithosphere is divided into plates, and are moving due to convection currents in the mantle, slab pull, ridge push and subduction. Evidence of this has been shown through palaeomagnetism, geological and climatological evidence
Mantle Convection
radioactive decay in the earth’s core emits heat which in turns heats the mantle. Magma, when heated, becomes less dense, and consequently rises towards the lithosphere. (along the geothermal gradient) At the surface, the magma begins to cool and begins to sink back towards the core, creating a current in the mantle.
Asthenosphere
The solid, plastic layer of the mantle beneath the lithosphere; made of mantle rock that flows very slowly, which allows tectonic plates to move on top of it
Palaeomagnetism
The study of past changes in the Earth’s magnetic field (determined from rocks, sediment or archaeological records)
Sea floor spreading
the process by which new oceanic lithosphere forms as magma rises toward the surface (due to constructive plate movement at divergent plate boundaries) and solidifies
Subduction
Where the thinner, more dense tectonic plate (usually oceanic crust - SiMa) descends beneath the opposing plate due to convergent plate movement.
Slab Pull
the process that results when a dense oceanic plate sinks beneath a less dense plate along a subduction zone, pulling the rest of the plate that trails behind it
Ridge Push
a mechanism that may contribute to plate motion; it involves the oceanic lithosphere sliding down the oceanic ridge under the pull of gravity
Benioff Zone
a narrow zone of deep earthquake foci at a subduction zone
Moho discontinuity
boundary between the Earth’s crust and the mantle