Events such as earthquakes and volcano eruptions that cause harm
Continental Drift
The idea proposed by Alfred Wegner that continents were together in mega continent Pangea, then drifted away that forms our planet now and will drift back together.
Evidence of Continental Drift
Study of fossils - similar fossils are found in different continents
Shape of continents - they fit together like a jigsaw
Pattern of rocks - similar patterns of rock layers on different continents
Continental crust
The older continental crust is mainly made from granite. It is the thicker of the two plates. This is a less dense than the oceanic crust, so therefore it does not sink.
Oceanic crust
The younger oceanic crust is mainly made from basalt. It is the thinner of the two plates. This is more dense than the continental crust and is frequently being destroyed.
Constructive plate boundaries
Two plates move apart, magma rises and fills the gap
Non violent shield volcanoes are formed
Causes earthquakes
Destructive plate boundaries (2 different types of crust)
Oceanic and Continental plates colide, oceanic plate sinks as it's more dense
Creates volcanoes and earthquakes
Destructive plate boundaries (same type of crust)
no plates sink, land is pushed up creating mountain ranges
creates earthquakes
no volcanoes
Conservative plate boundaries
the plates slide past one another
different direction or same direction but one faster
friction between the two creates earthquakes
Earthquakes
A suddent movement in the Earth's crust. The sudden release of energy that causes a sesmic wave. They usually occours at margins.
Richter scale
each step up the scale has 30 times more energy released than the previous one
special equipment needed to measure the strength of vibrations
measure the amount of energy released (magnitude)
humans can't feel magnitude 1 - 2 on the scale
over 5 is a major earthquake
no upper limit
Mercalli scale
measured by eye witness and photographic evidence
measure the effects and damage caused by an earthquake
uses a scale of 1 - 12
not effective in areaas which have no buildings or infrastructure
Dangers of areas of tectonic hazards:
eruption: plyroclastic flow, ash clouds
damage to environment
damage of homes
impacts to livelihoods
deaths & injuries
air pollution
Reasons why people live near tectonic hazards
soil are extremely fertile
living there for generations
good climate
good views/landscape
cheap land
unaware of dangers
tourism - positive economic impacts
religous reasons
used to the risks
Monitoring and prediction: Volcanoes
signs of volcanic activities - eg. gas, smoke
remote sensing - detect heat
tilt meter - shows deforms in volcano
Protection: Volcanoes
embankments & explosives to redirect lava to minimise damage
Planning: Volcanoes
exclusion zones - moving people away from volcanoes
sending warnings and information to the public
Monitoring and prediction: Earthquakes
most likely after long periods without any plate movements
seismograph can measure small foreshocks before the main quake
animals often act strangely before one
Protection: Earthquakes
all new buildings must comply with strict earthquake planning regulations
frequent safety checks
existing buildings, roads and bridges should be strengthened
Planning: Earthquakes
prepare disaster plans and carry out regular practices - earthquake drills
train emergancy services such as police, fire and ambulance crews
organise and prepare hospitals and evacuation centres in safe areas
educate people about what to expect and what will happen
Tsunami
A large sea wave triggered by a sudden displacement of ocean water caused by volcanic eruptions, earthquakes, meteorites etc.