Mount Merapi is a volcano located on the island of Java, Indonesia, in a densely populated area. The Mount Merapi eruption in 2010 began on 25 October 2010 when the volcano began erupting with a Volcanic Explosivity Index (VEI) of 4. Several more eruptions continued up until 30 November 2010. Mount Merapi’s explosive eruptions released ash plumes, lahars, pyroclastic flows, and sulphur dioxide. As a result, over 300,000 people had to evacuate and over 300 people lost their lives.
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Jetzt kostenlos anmeldenMount Merapi is a volcano located on the island of Java, Indonesia, in a densely populated area. The Mount Merapi eruption in 2010 began on 25 October 2010 when the volcano began erupting with a Volcanic Explosivity Index (VEI) of 4. Several more eruptions continued up until 30 November 2010. Mount Merapi’s explosive eruptions released ash plumes, lahars, pyroclastic flows, and sulphur dioxide. As a result, over 300,000 people had to evacuate and over 300 people lost their lives.
Mount Merapi is located in central Java, Indonesia, South East Asia. Java is bordered by the Indian Ocean and the Java Sea.
The Mount Merapi eruption in 2010 was caused by the subduction of the Indo-Australian plate underneath the Eurasian plate. The volcano lies on a destructive plate margin at a subduction zone, which is part of the Pacific Ring of Fire. The Mount Merapi eruption happened when the denser plate edge, the Indo-Australian plate, sunk (subducted) beneath the less dense plate edge, the Eurasian plate. When this happens, the denser plate’s movement causes an increase in the temperature and pressure, which ultimately leads to the release of water from the rocks. This results in a decrease in the melting point of the rock above and magma rising to the surface, causing eruptions.
As with earthquakes, volcanoes happen when tectonic plates move at fault lines. We have two explanations, one on Earthquakes and one on Volcanoes, for you to check out!
The 2010 Mount Merapi eruption had numerous devastating effects on the environment, economy, and people. Let’s take a look at these impacts in more detail.
The ash plumes, lahars, pyroclastic flows, and sulphur dioxide released from Mount Merapi caused various short-term and long-term environmental problems, such as the destruction of ecosystems and housing and an increase in the greenhouse effect.
The ash plumes from the 2010 Mount Merapi eruption reached altitudes of 18km and fell up to 30km away from the peak of the volcano. The layer of ash on the ground was 2-4cm thick and damaged 200 hectares of forest. In the long term, the volcanic ash in the atmosphere can increase the greenhouse effect by reflecting sunlight onto the earth.
A positive long-term effect of the release of ash plumes is the fertilization of soil, which can benefit the farmers in the affected area.
Multiple explosions with lahars and pyroclastic flows occurred between 26 October and 30 November. Cangkringan and Kemalang were the most affected areas, where rice fields, farms, infrastructure, rivers, and soil were damaged. Significant damage was even observed two years later.
At higher altitudes, sulphur dioxide reacts with the environment and can cause acid rain and cooling of the climate by reflecting the sunlight. A sulphur dioxide cloud 12,000-15,000m above the Indian Ocean was observed on 9 November 2010 by the Volcanic Ash Advisory Center in Darwin, Australia. However, this was not enough to create an observable difference in global temperature.
In 1991, Mount Pinatubo released so much sulphur dioxide that it had a minor impact on the global temperature.
The social impacts of the Mount Merapi eruption in 2010 included the loss of lives, homes, livelihood, forced evacuation, and increased physical and psychological health problems.
Many of those who evacuated stayed in refugee camps where the public toilets were unhygienic. Additionally, the sulphur dioxide released from the eruption caused irritation to human skin, eyes, and respiratory tracts. Many people at the refugee shelters suffered from headaches, acute respiratory infection, and high blood pressure.
A lot of the refugees were farmers who lost their livelihoods because the ash from the volcanic eruption caused damage to crops. This also made people fearful of food shortages. Many were forced to become miners and sell sand from the eruption or take up other jobs initiated by the government, such as cleaning up the volcanic ash. However, some suffered from psychological trauma from the eruption, which made it more difficult for them to work.
A survey was conducted two years after the disaster to determine the psychological distress of those affected in Cangkringan and Pakem. It demonstrated that those living in the Cangkringan district experienced the most distress in relation to the environmental impact of the eruption.
The total economic impact from the Mount Merapi eruption in 2010 was estimated at £450 million. This was mainly due to the impact on farming, tourism, and manufacturing.
As we mentioned above, many farmers lost their livelihoods due to the ash from the eruption. There was significant damage to rice, fruits, and vegetables, and as a result, the economic loss from agriculture was estimated at £13 million.
As you can imagine, the eruption had a big impact on tourism. Compared to the previous year, the number of tourists in 2010 dropped by approximately 30 percent for domestic tourists and 70 percent for international tourists. Certain flights that travelled through the ash clouds also experienced engine failure. Around 2500 flights were cancelled for safety reasons.
Although tourism has increased since the eruption, it has been impacted by a decreased level of trust and security.
If you’re interested, you can read up on British Airways Flight 009. The plane, a Boeing 747-200, flew through a cloud of volcanic ash and experienced engine failure in all four engines!
Mount Merapi is an active volcano, meaning the people of Java have experienced several eruptions over the years. So, what mitigation (preventative) strategies existed before the 2010 Mount Merapi eruption, and what changed after the eruption? Let’s have a look.
The main mitigation strategies aimed at reducing the potential impact of volcanic eruptions have largely relied on monitoring and warning.
A mechanical seismograph was installed 9km from Mount Merapi in 1924. A tiltmeter (a device that measures small variations in the vertical level) is also used to monitor any changes in the volcano. Observations at the beginning of 2010, such as earthquakes and changes in the dome, suggested that the volcano was going to erupt.
Police and the military were prepared to provide trucks and buses ordering people to leave. Temporary shelters were also ready for evacuees.
Many communities rely on their traditional warning signs of volcanic eruptions. This includes ash plumes, the movement of monkeys and other animals down the volcano, minor earthquakes, and lightning storms from the ash. Many people also rely on their spiritual connection to the volcano, so if they don’t see these signs, they are not likely to listen to advice to evacuate based on scientific monitoring.
A significant reason for the consequences of the Mount Merapi eruption in 2010 is the forgotten danger of living next to the volcano. Previously, many people would ignore the smoke coming from the volcano. Civilians have now become more reactive, and the government and non-governmental organizations have also implemented strategies to limit the future consequences of eruptions.
People have now become more aware of the potential dangers of living near a volcano and pay more attention to possible eruptions. Training has also been given to communities for more organised evacuation.
The government relocated 2500 families to safer areas. However, some people are still hesitant to move due to limited education, the requirement to adapt to new jobs, and not being directly affected by the eruptions in 2010.
Many people have now been given handheld radios, which can give them updated information about the volcano. Representatives are also given information by the government monitoring centres, which speeds up the spreading of information. This is an improvement from the previous methods, which were slow and involved various sources of information.
Roads and bridges have been improved for a smoother evacuation process.
Here are some interesting facts about Mount Merapi:
Mount Merapi erupted in 2010 by releasing ash plumes, lahar, pyroclastic flows, and sulphur dioxide. The 2010 eruptions were the most explosive eruptions within the previous 100 years.
The Mount Merapi eruption in 2010 was caused by the subduction of the Indo-Australian plate underneath the Eurasian plate. The volcano lies on a destructive plate margin at a subduction zone, which is part of the Pacific Ring of Fire. The Mount Merapi eruption happened when the denser plate edge, the Indo-Australian plate, sunk (subducted) beneath the less dense plate edge, the Eurasian plate. When this happens, the denser plate’s movement causes an increase in the temperature and pressure, which ultimately leads to the release of water from the rocks. This results in a decrease in the melting point of the rock above and magma rising to the surface, causing eruptions.
Mount Merapi has been erupting since the sixteenth century. Since 1548, the volcano has had 68 historic eruptions.
Mount Merapi tends to erupt every five to ten years.
The Mount Merapi eruption in 2010 was caused by the subduction of the Indo-Australian plate underneath the Eurasian plate. The volcano lies on a destructive plate margin at a subduction zone, which is part of the Pacific Ring of Fire.
When in 2010 did Mount Merapi begin and stop erupting?
Mount Merapi began erupting on 25 October 2010 and lasted until 30 November 2010.
What was the Volcanic Explosivity Index of the Mount Merapi eruption in 2010?
Mount Merapi erupted in 2010 with a Volcanic Explosivity Index (VEI) of 4.
Where is Mount Merapi located?
The volcano is located on the island of Java, Indonesia. It lies on the destructive plate margin between the Indo-Australian plate and the Eurasian plate.
What did the eruptions release?
The eruptions released ash plumes, lahar, pyroclastic flows, and sulphur dioxide.
What caused the Mount Merapi eruption in 2010?
The Mount Merapi eruption in 2010 was caused by the subduction of the Indo-Australian plate underneath the Eurasian plate. The volcano lies on a destructive plate margin at a subduction zone, which is part of the Pacific Ring of Fire. The Mount Merapi eruption happened when the denser plate edge, the Indo-Australian plate, sunk (i.e., subducted) beneath the less dense plate edge, the Eurasian plate. When this happens, the denser plate’s movement causes an increase in the temperature and pressure, which ultimately leads to the release of water from the rocks. This results in a decrease in the melting point of the rock above and magma rising to the surface, causing eruptions.
What were the environmental impacts caused by ash plumes?
Ash plumes had the following environmental impacts:
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