What is a volcano?
A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. This molten rock is known as magma.
When it erupts, huge amounts of very hot gas, boulders, ash and molten rock can burst out. This is thrown into the air, often pouring down the side of the mountain.
When the molten rock pours down the mountain it creates lava or pyroclastic flows. Any buildings or structures surrounding the area of a volcano when it erupts will be destroyed or damaged.
As well as flows of incredibly hot liquid mud and rock, homes are most commonly destroyed by hot ash falling like rain on everything below.
Did you know?
Why and how do volcanoes erupt?
How does a volcano erupt?
A volcano eruption happens when magma below the surface rises to the top of the mountain, causing gas and bubbles to appear. Pressure from this gas can build so much that a volcano explodes.
How often do volcano eruptions happen?
According to David Pyle, Professor of Earth Sciences at Oxford University, there are about 1,500 volcanoes around the world that are known to have erupted at some point in the past 10,000 years.
Most of these volcanoes could erupt again at some time in the future. In any year, about 60 to 80 volcanoes erupt. Mostly these will be small eruptions.
Where do volcano eruptions happen?
The majority of volcano eruptions occur along the Pacific Rim, in what is known as the ‘Ring of Fire’. The Ring of Fire is a path along the Pacific Ocean characterized by active volcanoes and frequent earthquakes. 75% of all volcanoes are located along the Ring of Fire.
Most volcanoes are found in lines along the edges of the Earth's tectonic plates.
In some places, for example in South America, Alaska and eastern Russia, volcanoes form tall mountains that are spaced 40 to 50 kilometres apart and line up parallel to the edge of the continent.
In other places, such as the West Indies, some Pacific islands and parts of Indonesia, volcanoes form islands.
The effects of living by volcanoes
More than half a billion people around the world live in the direct vicinity of a volcano. Despite the known dangers, people still choose to live in such a high-risk location. But the question is, why?
Thanks to a phenomenon known as ‘upside risk’, the opportunities of living in such a place may offset the known risks.
For farmers, one of the benefits of living near a volcano is the fertile agricultural ground, enhanced by the volcanic ash.
This also applies to areas that were covered by volcanic mudflows.
But there are also interesting social reasons for choosing to live in such a high-risk area, with volcanoes shaping the cultural identity of the communities surrounding them.
The risks of living by a volcano
Although there are benefits to living close to a volcano, the families who do, are mostly at risk of being affected.
Dr Zoe Mildon, a leading expert in the field of Earth Sciences and a lecturer at the University of Plymouth, explains the health dangers caused by deadly volcanic eruptions. According to Dr Mildon:
- There is the potential for lahars to develop, which are formed by volcanic ash mixing with water, which can engulf villages and cut off communities.
- Volcanic gases, if present in high enough concentrations can be poisonous.
- Inhaling volcanic ash can cause extensive damage to lungs, as volcanic ash particles are very tiny and very sharp.
Apart from the obvious health risks, homes and infrastructure are extremely vulnerable when volcanoes erupt. People might lose their home to the disaster, leaving them in urgent need of shelter.
How does ShelterBox respond to a volcano eruption?
ShelterBox is always on alert to respond to a volcano eruption, just like any other disaster.
However, extra care needs to be taken when responding to volcano eruptions, due to the dangers and challenges around this type of disaster. We need to make sure the environment is safe for our Response Teams to operate in.
We might send our Response Teams out with additional safety equipment, such as respiratory protection, as the air quality can be affected by volcano eruptions.
As soon as we know the operating environment is safe, we would aim to have a ShelterBox Response Team on the ground.
PLANNING FOR THE DISASTER
We asked our Operations team some questions about how to plan for a volcanic eruption and how ShelterBox prepares for such a disaster.
How do scientists and volcanologists monitor volcanoes?
Many of the world's most active volcanoes are monitored with instruments designed to detect early warning signs: webcams, to detect visual changes around the volcano, or in the volcanic vent; seismometers, to detect earthquakes; and spectrometers to measure changes in gas composition.
Many volcanoes can also be monitored from space, using radar and other instruments to measure changes in the shape of the volcano as pressure builds up below; or to measure changes in volcanic heat and gas.
What are the challenges of responding to a volcanic eruption?
In the aftermath of a volcano eruption, communities often face huge difficulties as the volcano can still be active and monitored. There is sometimes still a lot of seismic activity after a volcano eruption, so communities cannot return to certain areas until it is shown all clear.
Watch the video below to find out what were the challenges faced in Guatemala, after the eruption of the Fuego volcano.
Responding to Fuego volcano in Guatemala
We responded in Guatemala in 2018, after Fuego volcano erupted.
The challenges for local communities were huge, with some families unable to return home. A major road between communities had been cut by the volcanic flow, which made the challenges even greater.
The authorities were also planning a no-build zone in areas at risk of future eruptions, so for some families. This meant that they would never be able to return to their previous locations.
ShelterBox supported families in Guatemala with small tents that were used as safe spaces to give families some privacy and preserve dignity.
Many thanks to Dr Zoe Mildon, a leading expert in the field of Earth Sciences and a lecturer at the University of Plymouth and to David Pyle, Professor of Earth Sciences at Oxford University.
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