Tectonic plates and hazards Flashcards
(33 cards)
explain the distribution and cause of tectonic hazards
plate boundaries often move in different directions at different speeds creating a variations of plate boundaries which leads to variations in earthquake and volcanic activity
what is a divergent plate boundary
this is when the two plates move towards each other and one plate gets subducted which can cause earthquakes and volcanoes
eg: Nazca plate forced under south american plate
What is a convergent/collision plate boundary
this is when two plates move towards each other and collide forming mountains and tends to be continental rock eg: the himalayas
what is a constructive plate boundary
this is when the plates move apart from each other which can lead to creation of new crusts and when in the sea it can form new sea ridges
eg: pacific plate moving away from nazca plate
what is a conservative plate boundary
this is when two plates slide past each other and due to the friction this tends to form earthquakes eg: San andreas fault
what is convection
convection is when magma rises due to the heat and it being less dense causing denser and colder material to sink this tends to help volcanoes
what is mantle convection
heat produced by radioactive decay heats the lower mantle creating convection currents within the asthenosphere causing plate movements
explain sea floor spreading
judge mid ocean ridges formed (constructive) and magma is forced up and hardens forming new oceanic crust causing the sea floor to spread and push the tectonic plates apart
what is subduction
when two plates move towards each other one slides underneath the other causing a subduction zone
what is a slab pull
newly formed oceanic material at mid- ocean ridges become denser and thicker as it cools causing it to sink into the mantle pulling the plate down (helps subduction)
what are intra plate earthquakes
these occur in the middle (interior) of plates and their cause is most likely stresses from scientists faults becoming active again they have a random distribution
explain the distribution of hotspots
these can be found near the centre of some plates due to upwelling if the hot molten material form the core eg: hawaiian plate
or it can be caused by mantle plumes just under the crust heating the surface above it eg: cape verde islands
what is palaeomagnetism
this is a theory form the supercontinent pangaea and how you can find the same rock types at different coasts eg: south africa and south america and this is due to the magnetic field where either side of the plate the rocks ‘lock in’ forming the same pattern of rocks on either side
what are primary waves
primary waves arrive first and move through solid rock and fluids, they move in a push and pull motion
what are secondary waves
slower than P waves and only move through solid rock. They move in an up and down motion
what are Love waves
the only travel through the surface of the crust and are fast. They move from side to side
what are 3 secondary impacts of earthquakes (include examples)
tsunami- japan 2011 (powerpoint & 15,000)
landslides- movement of severe and rocks faking creating hazards such as road blockage kashmir 2005
liquification- sediments in ground become loose due to shaking. christchurch new z had a shallow earthquake 5.95 on which exaggerated liquification
primary factors from earthquakes
crustal factoring
ground shaking creating hazard
how are tsunamis formed
these tend to be formed when submarine earthquakes at subduction zones as a result of water column displacement
describe balsatic lava
hottest lava (1000-1200)
runny and thin
found at shield volcanoes & ocean hotspots
gentle eruptions
describe andestitic lava
around 800-1000
slow flowing however eruptions are moderately powerful
describe rhyolitic lava
coolest lava (650-800)
very high viscosity
has most violent eruptions
found at compositivo volcanoes/ super volcanoes
describe a shield volcano
found at hotspots or convergent boundary
erupt frequently but not that powerful
balsatic lava
describe a composite volcano
found at destructive plate boundary
erupt infrequently however are very powerful
andesitic/rhyolitic lava