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Reducing the impacts of natural hazards – WJEC What makes communities more vulnerable?

Natural hazards create many dangerous scenarios for people and environments. Volcanic eruptions, earthquakes and tsunami are a constant threat. Reducing this threat is crucial.

Part of GeographyTectonic landscapes and hazards

What makes communities more vulnerable?

There are three major factors which can increase the threat to people:

  • physical factors - the of the event and the type of event
  • social factors - the number of people living in an area near to a hazard
  • economic factors - the vulnerability of people affected by an event - this is also linked to poverty

Vulnerability, in the context of hazards, means the ability of an individual or group of people to anticipate, cope with, resist and recover from the impact of a natural hazard, or man-made hazard.

Physical factors

To determine the magnitude of a volcanic event, scientists or volcanologists use a measure called the Volcanic Explosivity Index (VEI). This is a measure of the height and volume of the which is ejected from the volcano. Each point measured is ten times the magnitude of the one before it.

Graphic showing the Volcano Explosivity Index (VEI).
Figure caption,
The eruption at Yellowstone, USA, 600,000 years ago was ten times the magnitude of the eruption at Tambora in 1815

The moment magnitude scale (Mw) is used to measure earthquakes. It measures the distance moved by a fault multiplied by the force needed to move it. Each number on the scale is ten times more powerful than the preceding one.

Graphic of the moment magnitude scale.
Figure caption,
A magnitude ten earthquake is ten times more powerful than a magnitude nine. The earthquake in Chile in 1960 was the world’s most powerful earthquake

The type of tectonic hazard is also an important physical factor which can increase the threat posed by an eruption. Often, when a volcano erupts, lava flows and ash clouds form. The deadliest types of volcanic hazards are pyroclastic flows and .

At the Soufrière Hills on the island of Montserrat (between 1995-1997), a gigantic wall of super-heated pyroclastic flow sped down the side of the volcano at a speed of over 100 km/h, with temperatures exceeding 600°C.

A large cloud of volcanic material flowing down the side of a mountain.
Image caption,
A large mass of material collapses and flows downhill, a pyroclastic flow

Lahars are another deadly after-effect of a volcanic eruption. The mud flow can sweep away roads, bridges and buildings. Farmland and crops are destroyed, putting a great strain on food supplies in the area.