Zusammenfassung der Ressource
Physical
Geography
- Restless Earth
- How do convection currents
cause plate movement
- 1. The core heats the
molton rock in the mantle
which creates a convection
current.
- 2. The heated rock
rises to the surface.
- 3. At the surface convection
currents move the tectonic plates
in the crust.
- 4.Molton rock cools and flows
back to the core.
- 3 main plate boundaries
Anmerkungen:
- Collison Plate boundries
- E.g: Indo Australian and Eurasion plates
- two continental plates collide and the two plates buckle
- Many Earthquakes
- Destructive
- when 2 plates colilde one flows under the other (subduction)
- e.g. Nazca Plate and South American Plate
- Earthquakes and volcanoes occour
- constructive
- Rising convection currents pull apart
- e.g. Eurasion and North American Plate
- forming volcanic ridges e.g. Mid-Atlantic RIdge
- conservative
- Two plates slide past one another
- e.g San Andreas Fault California
- Earthquakes
- Volcanic and earthquake hazards
- Earthquake in Kashimer 2005
- 75 000 dead
- 2.8 million homeless
- 75 000 injured
- property damage $440 million
- Earthquake in California, 1989
- up too 12 000 homeless
- 3757 injured
- property damage $10 million
- 63 dead
- volcanoes
- shield volcanoes
- found on constructive plate boundaries
- formed by long thin,runny lava which flows
a long way before it solidifies
- gentle sloping sides and a wide base
- contains baslaltic magma which is very hot with low
silica and gas content
- Erupts frequently but not violently
- composite volcanoes
- found on destructive plate boundraies
- formed by eruptions of viscous sticky lava and ash that don't flow far
- have steep slopping sides and narrow base
- made up layers of thick lava and ash
- contains andesitic magma which is less hot
but contains lots of silica and gas
- erupts frequently but not violently includes pyroclastic flow
- Managing earthquake and
volcanic hazards
- they are very difficult to predict
Anmerkungen:
- - when will they be
- where will it be exactly
- how big?
- What other impacts will there be
- how many people live there
- can we evacuate the people
- what can help predict earthquakes
Anmerkungen:
- - animals and birds fly away
- increase in gas emmisions
- increase in soil temperature
- volcano swelling
- increase in small earthquakes
- water ponds getting warmer
- lots needed after an earthquake e.g. volunteers, clean water
Anmerkungen:
- - trained volunteers to help clear up debris, injured and dead people
- clean water to prevent spread of disease
- food as often roads, farms, shops and towns have been effected
- radio communication because phones will often not work
- medical people to care for the injured
- a plan to evacuate the area if needed
- Case Study: Mount Pinatubo
Volcano 1991
- Social Effects
- 58 000 people were evacuate
from a 30km radius of the
volcano
- 874 deaths in total
- 300 killed from collapsing roofs
- 100 killed by layhars
- 1.2 million lost their homes
- people round the
volcano had to
migrate to shanty
towns in manila
- Economic Effects
- houses & bridges
destroyed and
needed replacing
- Manila airport had to be closed
- 1991 harvest destroyed
and 650 000 people lost
their jobs
- farmland destroyed by falling
ash & pumice unusable for
years
- Heavy rainfalll from Typhoon
Yunga causes buildings to
collapse
- Enviromental Effects
- Fast flowing volcanic mudflow
(Lahars) cause servere river bank
erosion undercut bridges etc.
- Volcanic ash blown in all directions
over hundreds of kms, smothering
fields and buildings
- Global cooling caused by ash in
the atmosphere of 0.5c
- Where?
- Island of Luzon in the
Phillipines
- SE Asia at the
destructive plate
boundry between
the Eurasion &
Philippine Plates
- Why?
- Result of Oceanic Philipine plate being
subducted under the lighter continental
Eurasion plate
- What?
- Composite Volcano exploded in
June 1991 creating Lahars &
massive ash & gas cloud
- Managing the hazard
- Prevention
- 75 000 people evacuated up to a 30km radius
- US Air Force helicopters helped evacuation
- Alert Systems put in place to warn of eruption
- Government Shelters
- Strategies for long term aid and disease control during evacutions
- Prediction
- 75 000 people were evacuated due to accurate predictions
- Set up a permanent monitoring points or use satellite images to look at volcano site for changes in land surfaces
- The US Geological Service helped to predict the disaster
- No monitoring till April when seisometers were put into place
- Prepatation
- Evacuation camps built for refugees
- Warning sign like gas and steam looked for
- Long & short term aid organised especially from the Red Cross and the US
- Storage of medical
supplies of food and
water in preparation
for disaster