INDONESIA VOLCANO CASE STUDY
MOUNT MERAPI 2010
Mount Merapi is a strato volcano
4 on the VEI (Icleand 3)
Destructive plate boundary
Pyroclastic flows
SOCIAL IMPACTS
200,000 people were made homeless
Emergency shelters had to be moved
353 people were killed from the main eruption
ECONOMIC IMPACTS
Large number of livestock were killed
Ash falls forced the closure of airport for over a fortnight
Many roads closed due to lava flows
However
Bought in jobs from the tourism industry
Medical use of hot spa water and mud seen to improve health
POLITICAL IMPACTS
International aid was offered from organisations such as Red Cross
Govt making money available to farmers to help replace livestock
ENVIRONMENTAL IMPACTS
Sulphur dioxide emissions caused acid rain to fall over large part of region
Conservation area has been set up around volcano where it is unsafe to live
Geothermal energy (renewable source) using steam from hot rocks
Ash from volcano eventually led to more fertile soil in the area
INDONESIA FACTS:
Eurasian Plate, Pacific Plate and Indo-Australian Plate are three avtive tectonic plates that cause the subduction zones that form these volacanoes
The PROBLEM is that many local residents refure to leave their homes - can be related to their livelihood - farms which are their only source of income, can also be realted to animist belief-systems - volcano warning signs such as ash and thunder are considered to be acts of their angry ancestors and by praying to local gods local communities believe they will be protected from any danger
TYPES OF ERUPTIONS IN INDONESIA
LAVA FLOWS
Speed of lava flows vary from several meters to tens of km/hr before it cools and solidifies
PYROCLASTIC FLOWS
Most destructive and deadly event from eruptions
Mixture of volanic gases and fragmented rock
Flows at high speeds
Very high temperatures
TEPHRA FALLS
Term from rock fragments released into the air by eruptions
Large tephra usually falls not far from crater
Lapilli - smaller tephra tend to be found further away
Can have huge impacts on human health, environmental pollution, animals
LAHARS
Hydro-volcanic events during eruption
Large discharge flow, high sediment concentration
MAGMA
Earthquakes occur due to magma movement
Volcanic islands result from repeated fast placement of magmatic products in a limited area
TSUNAMIS
Produced by unavoidable disturbances in marine/lake environments
Can cause underwater earthquakes/landslides/volcanic eruptions/collapse of sea floor/bombs
Long history of volcano-triggeres tsunamis in Indonesia
Why does Indonesia have so many volcanoes?
There is a widespread subduction zone along the entire 300km length of the Indonesia archipelgo
Much of Indonesia is an island arc formed by subduction of the Indo-Australian plate beneath the Eurasian plate
Continental shelf of northern Australia is in collusion with Eurasian plate - plate movements produce high levels of seismicity and volcanicity