tectonic hazards Flashcards
describe the continental drift theory:
- proposed by Alfred Wegener
- suggested the continents were not always in the same position as they’re in today.
- at one point in time, all the continents were joined together as one large mass of land.
- there are similar patterns of rocks and fossils on both sides of the Atlantic, suggesting that they were once joined.
- includes fossil remains of land mammals which wouldn’t have been able to swim across from one side to the other.
what are tectonic hazards?
threats caused by the movement of tectonic plates that have the potential to cause damage to life, property, or the environment. examples include volcanoes and earthquakes.
describe the global distribution of earthquakes:
earthquakes usually occur at plate margins due to enormous pressure build-up. however, there are anomalies that don’t occur on plate margins, and these are caused by human activity e.g. underground mining.
describe the global distribution of volcanoes:
the majority of volcanoes run along plate margins. e.g. pacific ring of fire, mid-atlantic ridge.
how are volcanoes generally formed?
hot, molten rock (magma) rises to the surface at constructive and destructive plate margins, forming volcanoes.
- they can also form in ‘hot-spots’, where the crust is thin enough for magma to break through it.
describe the difference between oceanic and continental crust:
oceanic crust:
- dense
- thin (5-10km)
- younger
- can be destroyed
continental crust:
- less dense
- thick (20-200km)
- older
- cannot be destroyed
describe convection currents:
the Earth’s core is hot and this heats the mantle. the heated magma rises as it is less dense. as it rises, it cools and becomes denser again.
this creates a circular movement within the mantle (convection currents). the plates sit atop the mantle and the convection currents drag the plates along.
describe ridge push and slab pull:
ridge push:
- mid-ocean ridges are higher than the rest of the ocean floor so gravity causes the ridge to force the plate down
slab pull:
- tectonic plates are heavy. when a plate begins to subduct (sink), gravity means that it’ll pull the rest of the plate down with it.
> it’s always the oceanic plate that’s subducted beneath the continental plate.
why are earthquakes hazardous?
- the ground shakes, causing buildings to collapse
- water and gas pipes are damaged, causing fires and floods
why are volcanoes hazardous?
- ash clouds disrupt air travel and can make it difficult and dangerous for planes to fly
- ash can also cover farmland, covering and damaging the crops underneath
- heavy ash can also, in some cases, cause buildings to collapse
what occurs at a constructive plate margin?
plates move apart. new crust is formed as magma rises to the surface. the process’s friction causes earthquakes, but the end result is typically broad and flat shield volcanoes, as the magma is hot and fluid, and flows a long way before cooling.
what occurs at a destructive plate margin?
plates move towards each other. the denser oceanic plate subducts (sinks) beneath the less dense continental plate. gravity pulls the oceanic plate into the mantle. friction between the two plates causes earthquakes. the end result is a steep-sided, composite volcano, that’s violent and explosive.
what occurs at a conservative plate margin?
the plates are moving past each other (usually one is going at a different speed to the other). friction between the plates causes earthquakes. there are no volcanoes because there is no magma.
what occurs at a collision plate margin? (linked to destructive plate margins)
two continental plates meeting doesn’t result in subduction. instead, the two plates collide, the crust is crumpled and uplifted, and results in mountains. these processes cause earthquakes, but no volcanoes as there is no magma.
why do people choose to live on plate margins? what are the benefits?
- better building designs can withstand earthquakes, so people feel less at risk.
- volcanoes can bring benefits e.g. fertile soils, rocks for building, rich mineral deposits, hot water.
- more effective monitoring of volcanoes and earthquakes can allow people to receive warnings and evacuate before events happen.