Topic 1: Tectonic Processes and Hazards Flashcards
(34 cards)
natural hazard
a naturally occurring process or event that has the potential to affect people
natural disaster
a major natural hazard that causes significant social, environmental and economic damage
when a natural hazard strikes a vulnerable population that can’t cope using its own resources
vulnerability
the ability to anticipate, cope with, resist and recover from a natural hazard
greater scale natural hazard = more vulnerable population = greater disaster
plate-tectonic theory: mantle convection
- less accepted argument
- heat produced by decay of radioactive elements in Earth’s core
- heats lower mantle, creating convection currents (of hot, liquid magma)
- currents move in circles in asthenosphere, causing plates to move
plate-tectonic theory: slab pull
- newly formed oceanic crust at mid-ocean ridges becomes denser and thicker as it cools
- sinks into mantle under its own weight, pulling rest of plate further down with it
plate-tectonic theory: subduction
- two oceanic plates (or oceanic/continental) move towards each other
- one slides under the other into mantle
- melts in a subduction zone
plate-tectonic theory: seafloor spreading
- huge mid-ocean ridges form in the middle of oceans when hot magma is forced up from the asthenosphere and hardens
- forms new oceanic crust
- new crust pushes plates apart
structure of the Earth
core:
inner core →
outer core →
mantle:
lower mantle →
upper mantle →
crust:
lithosphere
crust + upper mantle
palaeomagnetism
the study of past changes in the Earth’s magnetic field (determined from rocks, sediment, or archaeological records)
evidence for seafloor spreading
- studies of palaeomagnetism in the 1950s
- Earth’s magnetic fields change direction (north and south poles swap) approx. every 400,000 years
- when lava cools and becomes rock, minerals in the rock line up with Earth’s magnetic direction (polarity) at the time
- same pattern of magnetic direction found on either side of mid-ocean ridges
- therefore new rock is being formed at the same time on both sides
asthenosphere
part of the mantle below the lithosphere, where the rock is semi-molten
asthenosphere
part of the mantle below the lithosphere, where the rock is semi-molten
Benioff zone
the area where friction is created between colliding tectonic plates, resulting in intermediate and deep earthquakes
convection currents
hot, liquid magma currents moving in the asthenosphere
crustal fracturing
when energy released during an earthquake causes the Earth’s crust to crack
epicentre
the point on the Earth’s surface directly above the focus of an earthquake
focus
the point inside the Earth’s crust from which the pressure is released when an earthquake occurs
hazard-management cycle
a theoretical model of hazard management as a continuous four-stage cycle involving mitigation, preparation, response and recovery
hot spot
points within the middle of a tectonic plate where plumes of hot magma rise and erupt
intra-plate earthquakes
earthquakes which occur far from plate margins
intra-plate earthquakes
earthquakes which occur far from plate margins
L waves
the slowest seismic waves, which focus all their energy on the Earth’s surface
liquefaction
when the violent shaking during an earthquake causes surface rocks to lose strength and become more liquid than solid