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| Saturday, 1 April, 2000, 14:44 GMT 15:44 UK Why volcanoes explode ![]() By BBC News Online's Dr Damian Carrington Volcanoes are the dramatic and deadly consequence of our restless planet cooling its fiery core. Through history, floods and earthquakes have resulted in more fatalities, but volcanoes continue to pose a terrifying threat. Scientists have become much better at predicting eruptions and how dangerous a volcano is. It turns out it all depends fundamentally on one thing - how sticky the magma is.
Their trademark is gushing torrents of red hot lava, flowing down the side of the mountain, like a river of fire. These are the less dangerous of the two types of volcano, because the path of the magma flow can easily be predicted. Boom and bust In contrast, when the magma rising up inside a volcano is sticky like treacle, the gas bubbles cannot escape, pressure builds and eventually the hot magma explodes and fragments. This type of eruption is much less predictable and therefore much more dangerous. The explosions at ancient Pompeii, Mount St Helens, Pinatubo, Montserrat and Mount Usu were of this type. Because the sticky magma is stronger, it can build taller volcanoes with steeper sides - the classic volcano shape - sometimes with catastrophic results. As magma pushes up, the whole side of a volcano can become unstable and fall off in a landslide. This is like smashing the top off a shaken champagne bottle, rather than teasing out the cork. Explosions of enormous power can result, blasting ash high into the atmosphere and sending clouds of burning gas and rock shooting down the sides of mountains. These "nuee ardentes" incinerate everything in their path. Predicting trouble The stickiness of the magma depends on how much silica it contains. The rocks that make up the continents are more silica-rich than the ocean floor. So, unfortunately, the sticky, explosive volcanoes are nearly always on land and often near human populations. The runny, less dangerous volcanoes tend to be safely tucked away under the seas or on oceanic islands. Overall, one in 10 people on Earth live within range of an active volcano. ![]() Burning ash flows can travel extremely fast The best method at present is to listen to the rumbles coming from inside a grumbling peak. As magma forces its way up, thousands of minor earthquakes are set off. The more of these there are the nearer the eruption. On Montserrat, the rhythm of the volcano is so well understood that the time of eruption can be predicted to within a few hours. Other methods of prediction include spotting changes in the composition of gases steaming from an active peak, the angle of the slopes and even the behaviour of local animals. Red for danger However, predicting volcanic eruptions is a dangerous business. In 1993, 10 volcanologists surveying the crater of a Colombian volcano were killed by an unexpected blast. Thankfully, much of the technology now deployed allows volcanologists to gauge the likelihood of an eruption from a safe distance. Satellites give real time temperature data and spectrometers "sniff" gas compositions from 20 km away. Remote sensing cannot completely replace in-situ measurements, but it has certainly already saved the lives of some of the scientists who brave the wrath of live volcanoes to protect others. |
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