Top 5 Ways Volcanoes Kill
1. Pyroclastic Flows
A deadly mixture of volcanic gas, ash, and rock, a pyroclastic flow can rush down a volcano as fast as 100 miles per hour (160 km/h) and be as hot as 1,300 degrees Fahrenheit (700 degrees Celsius). The dense and superheated cloud generally obliterates buildings, incinerates obstacles, and kills any creature in its path.
Where it happened: In AD 79, Mount Vesuvius buried the town of Pompeii with ash and pumice. Several thousand Romans suffocated in a flowing cloud of red-hot ash and poisonous gas. The ash settled around their bodies and set as hard as concrete, so that 19th-century archaeologists could make strikingly lifelike plaster casts of bodies that had crumbled to dust 2,000 years before.
2. Lahars
These mudflows can be as dense as wet concrete but move like raging rivers. They slide down volcanic mountains with enough force to carry boulders at breakneck speed for miles. Obstacles in a lahar’s path are typically battered, broken, and buried in mud.
Where it happened: Twenty years ago, Nevado del Ruiz in Colombia blasted molten rock outward, which melted the mountain’s cap of ice and snow. A wall of water, mud, and ash raced down the mountain. Just before midnight on November 13, 1985, it buried the town of Armero, killing 23,000 people 45 miles (72 km) away.
3. Landslides
Avalanches are common on volcanoes, where loosely packed rock and ash may sit precariously on a mountain getting steeper by the minute. Seismic tremors trigger the slide, which can have deadly effects.
Where it happened: The worst volcanic disaster in Japan’s history happened in 1792, when one of the Unzen volcano’s many lava domes collapsed. A massive landslide ripped through Shimabara City. The debris then crashed into the sea and generated a tsunami that devastated the coast. In the end, as many as 15,000 people were dead.
4. Tsunamis
These cataclysmic waves are often called tidal waves, but that’s not really correct – they have nothing to do with tides. Tsunamis are formed by seismic phenomena such as earthquakes and volcanoes. By the time a tsunami approaches the shore, the wave that was hardly noticeable when it formed out at sea is huge.
Where it happened: When Krakatoa erupted in 1883, it created one of the most catastrophic disasters in history. The explosion on the Indonesian volcanic island was so great that the boom could be heard thousands of miles away. Ash shot 50 miles (80 km) into the air. So much material was expelled that most of the island collapsed into the sea, triggering a tsunami that smashed into coastal towns in Java and Sumatra and left more than 30,000 people dead.
5. Gas
Volcanoes belch gases from deep inside the Earth. Some of them just smell bad, but others kill. Sulfur dioxide and carbon dioxide are just two of the noxious gases that seep from vents in the Earth’s crust.
Where it happened: Volcanic activity in the African nation of Cameroon in 1986 caused a huge amount of carbon dioxide to spurt up through Lake Nyos and reach a deadly concentration. The suffocating cloud drifted over nearby villages and killed 1,700 people, most as they slept.
And After All That, You Starve
Even after the eruption, your problems aren’t over. The ash and poisonous gases can choke vegetation and spoil fresh water sources. The next thing you know, your crops have failed and your livestock are dying. An eruption that directly kills a thousand people might leave tens of thousands dead from famine and disease in the months that follow.
Where it happened: The Laki fissure in Iceland erupted for more than eight months in 1783 and 1784, oozing lava over 220 square miles (570 sq km). The gases stunted crops and grasses and killed most of the island’s domesticated animals. More than 9,300 people – one fifth of Iceland’s population – perished during the resulting famine.
