Types of Volcanic Eruptions

Article by Jessica Ball

Volcanic Eruptions The most common type of volcanic eruption occurs when magma (the term for lava when it is below the Earth's surface) is released from a volcanic vent. Eruptions can be effusive, where lava flows like a thick, sticky liquid, or explosive, where fragmented lava explodes out of a vent. In explosive eruptions, the fragmented rock may be accompanied by ash and gases; in effusive eruptions, degassing is common but ash is usually not. Volcanologists classify eruptions into several different types. Some are named for particular volcanoes where the type of eruption is common; others concern the resulting shape of the eruptive products or the place where the eruptions occur. Here are some of the most common types of eruptions: Hawaiian Eruption In a Hawaiian eruption, fluid basaltic lava is thrown into the air in jets from a vent or line of vents (a fissure) at the summit or on the flank of a volcano. The jets can last for hours or even days, a phenomenon known as fire fountaining. The spatter created by bits of hot lava falling out of the fountain can melt together and form lava flows, or build hills called spatter cones. Lava flows may also come from vents at the same time as fountaining occurs, or during periods where fountaining has paused. Because these flows are very fluid, they can travel miles from their source before they cool and harden. Hawaiian eruptions get their names from the Kilauea volcano on the Big Island of Hawaii, which is famous for producing spectacular fire fountains. Two excellent examples of these are the 1969-1974 Mauna Ulu eruption on the volcano's flank, and the 1959 eruption of the Kilauea Iki Crater at the summit of Kilauea. In both of these eruptions, lava fountains reached heights of well over a thousand feet. Strombolian Eruption Strombolian eruptions are distinct bursts of fluid lava (usually basalt or basaltic andesite) from the mouth of a magma-filled summit conduit. The explosions usually occur every few minutes at regular or irregular intervals. The explosions of lava, which can reach heights of hundreds of meters, are caused by the bursting of large bubbles of gas, which travel upward in the magma-filled conduit until they reach the open air. This kind of eruption can create a variety of forms of eruptive products: spatter, or hardened globs of glassy lava; scoria, which are hardened chunks of bubbly lava; lava bombs, or chunks of lava a few cm to a few m in size; ash; and small lava flows (which form when hot spatter melts together and flows downslope). Products of an explosive eruption are often collectively called tephra. Strombolian eruptions are often associated with small lava lakes, which can build up in the conduits of volcanoes. They are one of the least violent of the explosive eruptions, although they can still be very dangerous if bombs or lava flows reach inhabited areas. Strombolian eruptions are named for the volcano that makes up the Italian island of Stromboli, which has several erupting summit vents. These eruptions are particularly spectacular at night, when the lava glows brightly. Vulcanian Eruption A Vulcanian eruption is a short, violent, relatively small explosion of viscous magma (usually andesite, dacite, or rhyolite). This type of eruption results from the fragmentation and explosion of a plug of lava in a volcanic conduit, or from the rupture of a lava dome (viscous lava that piles up over a vent). Vulcanian eruptions create powerful explosions in which material can travel faster than 350 meters per second (800 mph) and rise several kilometers into the air. They produce tephra, ash clouds, and pyroclastic density currents (clouds of hot ash, gas and rock that flow almost like fluids). Vulcanian eruptions may be repetitive and go on for days, months, or years, or they may precede even larger explosive eruptions. They are named for the Italian island of Vulcano, where a small volcano that experienced this type of explosive eruption was thought to be the vent above the forge of the Roman smith god Vulcan. Plinian Eruption The largest and most violent of all the types of volcanic eruptions are Plinian eruptions. They are caused by the fragmentation of gassy magma, and are usually associated with very viscous magmas (dacite and rhyolite). They release enormous amounts of energy and create eruption columns of gas and ash that can rise up to 50 km (35 miles) high at speeds of hundreds of meters per second. Ash from an eruption column can drift or be blown hundreds or thousands of miles away from the volcano. The eruption columns are usually shaped like a mushroom (similar to a nuclear explosion) or an Italian pine tree; Pliny the Younger, a Roman historian, made the comparison while viewing the 79 AD eruption of Mount Vesuvius, and Plinian eruptions are named for him. Plinian eruptions are extremely destructive, and can even obliterate the entire top of a mountain, as occurred at Mount St. Helens in 1980. They can produce falls of ash, scoria and lava bombs miles from the volcano, and pyroclastic density currents that raze forests, strip soil from bedrock and obliterate anything in their paths. These eruptions are often climactic, and a volcano with a magma chamber emptied by a large Plinian eruption may subsequently enter a period of inactivity. Lava Domes Lava domes form when very viscous, rubbly lava (usually andesite, dacite or rhyolite) is squeezed out of a vent without exploding. The lava piles up into a dome, which may grow by inflating from the inside or by squeezing out lobes of lava (something like toothpaste coming out of a tube). These lava lobes can be short and blobby, long and thin, or even form spikes that rise tens of meters into the air before they fall over. Lava domes may be rounded, pancake-shaped, or irregular piles of rock, depending on the type of lava they form from. Lava domes are not just passive piles of rock; they can sometimes collapse and form pyroclastic density currents, extrude lava flows, or experience small and large explosive eruptions (which may even destroy the domes!) A dome-building eruption may go on for months or years, but they are usually repetitive (meaning that a volcano will build and destroy several domes before the eruption ceases). Redoubt volcano in Alaska and Chaiten in Chile are currently active examples of this type of eruption, and Mount St. Helens in the state of Washington spent several years building several lava domes. Surtseyan Eruption Surtseyan eruptions are a kind of hydromagmatic eruption, where magma or lava interacts explosively with water. In most cases, Surtseyan eruptions occur when an undersea volcano has finally grown large enough to break the water's surface; because water expands when it turns to steam, water that comes into contact with hot lava explodes and creates plumes of ash, steam and scoria. Lavas created by a Surtseyan eruption tend to be basalt, since most oceanic volcanoes are basaltic. The classic example of a Surtseyan eruption was the volcanic island of Surtsey, which erupted off the south coast of Iceland between 1963 and 1965. Hydromagmatic activity built up several square kilometers of tephra over the first several months of the eruption; eventually, seawater could no longer reach the vent, and the eruption transitioned to Hawaiian and Strombolian styles. More recently, in March 2009, several vents of the volcanic island of Hunga Ha'apai near Tonga began to erupt. The onshore and offshore explosions created plumes of ash and steam that rose to more than 8 km (5 miles) altitude, and threw plumes of tephra hundreds of meters from the vents. What Determines Eruption Type The crystal and gas content and temperature of a magma help determine a volcano's eruption style.   -- Crystals in magma make it more viscous, so magma with a high crystal content is more likely to explode than flow.   -- Gases create explosions if they cannot easily escape from viscous magma, but they can also be released without explosions (or with only minor ones) from fluid magma.   -- High-temperature magmas usually erupt effusively, while low-temperature magmas cannot flow easily and are more likely to erupt explosively. About the Author Jessica Ball is a graduate student in the Department of Geology at the State University of New York at Buffalo. Her concentration is in volcanology, and she is currently researching lava dome collapses and pyroclastic flows. Jessica earned her Bachelor of Science degree from the College of William and Mary, and worked for a year at the American Geological Institute in the Education/Outreach Program. She also writes the Magma Cum Laude blog, and in what spare time she has left, she enjoys rock climbing and playing various stringed instruments. Find it on Geology.com

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Hawaiian Eruption Hawaiian eruption. In a Hawaiian eruption, fluid lava is ejected from a vent as fire fountains or lava flows. The 1969 eruption at Mauna Ulu, a vent of Kilauea Volcano in Hawaii, was a spectacular example of fire fountaining. Photo by D.A. Swanson, USGS, August 22, 1969. Enlarge Image Strombolian Eruption Strombolian eruption. Short bursts of glowing lava, created from the bursting of large gas bubbles at the summit vent of a volcano typify a Strombolian eruption. This photo, taken from the summit of Stromboli, a volcano in the Aeolian Islands, Italy, shows a classic example of this activity. Photo by Andrew Hague, Istockphoto.com. Vulcanian Eruption Vulcanian eruption. Relatively small but violent explosions of viscous lava create columns of ash and gas and occasional pyroclastic flows, as seen at this eruption of the Santiaguito volcanic dome complex in Guatemala. Photo by Jessica Ball, March 15, 2009. Plinian Eruption Plinain eruption. The largest and most violent of all explosive eruptions, Plinian eruptions send columns of pulverized rock, ash, and gases that rise miles into the atmosphere in a matter of minutes. Mount St. Helens in Washington State experienced a Plinian eruption following a major flank collapse in 1980. Photo by Austin Post, USGS, May 18, 1980. Enlarge Image Lava Dome Lava dome. Lava domes, such as this example in the crater of Mount St. Helens, are piles of viscous lava that are too cool and sticky to flow far. Domes grow and collapse in cycles, and often form at volcanoes that also experience Plinian eruptions. Photo by Lyn Topinka, USGS, August 12, 1985. Enlarge Image Surtseyan Eruption Surtseyan eruption. Lava erupting through water creates the dramatic plumes of scoria and billowing ash-and-gas clouds of a Surtseyan eruption. The type example of this eruption occurred at Surtsey, a volcanic island off the coast of Iceland. NOAA image of the 1963 eruption. Enlarge Image Volcanic Eruptions Resources Bardintzeff, J.-M. and McBirney, A.R., 2000, Volcanology: Massachusetts, Jones & Bartlett Publishers, 268 p. Schminke, H.-U., 2004, Volcanism: Berlin, Springer, 324 p. McNutt, S.R., Rymer, H., and Stix, J. (editor), 1999, Encyclopedia of Volcanoes: San Diego, CA Academic Press, 1456 p. Gates, A.E. and Ritchie, D., 2007, Encyclopedia of Earthquakes and Volcanoes, Third Edition: New York, NY, Checkmark Books, 346 p.

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Future Iceland Eruptions Could Be Deadly for Europe

What if one of the largest volcanic eruptions in recent history happened today? A new study suggests that a blast akin to one that devastated Iceland in the 1780s would waft noxious gases southeastward and kill tens of thousands of people in Europe. And in a modern world that is intimately connected by air traffic and international trade, economic activity across much of Europe, including the production and import of food, could plummet.

From June of 1783 until February of 1784, the Laki volcano in south-central Iceland erupted. Although the event didn’t produce large amounts of volcanic ash, it did spew an estimated 122 million metric tons of sulfur dioxide gas into the sky — a volume slightly higher than human industrial activity today produces in the course of a year, says Anja Schmidt, an atmospheric scientist at the University of Leeds in the United Kingdom.

Historical records suggest that in the 2 years after the Laki eruption, approximately 10,000 Icelanders died — about one-fifth of the population — along with nearly three-quarters of the island’s livestock. Parish records in England reveal that in the summer of 1783, when the event began, death rates were between 10 percent and 20 percent above normal. The Netherlands, Sweden, and Italy reported episodes of decreased visibility, respiratory difficulties, and increased mortality associated with the eruption. According to one study, an estimated 23,000 people died from exposure to the volcanic aerosols in Britain alone. But elsewhere in Europe, it’s difficult to separate deaths triggered by the air pollution from those caused by starvation or disease, which were prominent causes of death at the time.

To assess how such an eruption might affect the densely populated Europe of today, Schmidt and her colleagues plugged a few numbers into a computer simulation. They used weather models to estimate where sulfur dioxide emissions from an 8-month-long eruption that commenced in June would end up. They also estimated the resulting increases in the concentrations of airborne particles smaller than 2.5 micrometers across, the size of aerosols that are most easily drawn into human lungs and that cause cardiopulmonary distress. Then, they used modern medical data to estimate how many people those aerosols would kill.

In the first 3 months after the hypothetical eruption began, the average aerosol concentration over Europe would increase by 120 percent, the team reports online today in the Proceedings of the National Academy of Sciences. The number of days during the eruption in which aerosol concentrations exceed air-quality standards would rise to 74, when a normal period that length typically includes only 38. Not surprisingly, the air would become thickest with dangerous particles in areas downwind of the eruption, such as Iceland and northwestern Europe, where aerosol concentrations would more than triple. But aerosol concentrations in southern Europe would also increase dramatically, rising by 60 percent.

In the year after the hypothetical eruption commences, the increased air pollution swept from Iceland to Europe would cause massive amounts of heart and lung disease, killing an estimated 142,000 people. Fewer than half that number of Europeans die from seasonal flu each year.

At least four Laki-sized eruptions have occurred in Iceland in the past 1,150 years, Schmidt and her colleagues say. So the new figures are cause for concern.

The team “has done a good job of showing where volcanic aerosols would end up, and the human health response to such aerosols is well understood,” says Brian Toon, an atmospheric scientist at the University of Colorado, Boulder. “This is all very solid science.”

Icelandic volcanoes shut down European air traffic for more than a week in April 2010 and for several days in May of this year. But those eruptions are tiny compared with a Laki-sized eruption, which could ground airplanes for 6 months or more, says Alan Robock, an atmospheric scientist at Rutgers University in New Brunswick, New Jersey. Such an event would have a huge impact on crop yields and, by affecting shipping and air traffic, would also affect Europeans’ ability to import food, he notes. It could even have a dramatic effect on daily life, he says. “If there are sulfur dioxide clouds over Europe, people with respiratory problems can’t do much about it except stay indoors.”

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