Hawaiian Volcano Observatory

Explosive eruptions produce multiple hazards

Hawaiian volcanoes have produced explosive eruptions ranging in size and vigor from relatively small lava fountains to large eruptions.

Explosive eruption column from Halema‘uma‘u Crater 11:15 a.m. May 1...

Explosive eruption column from Halema‘uma‘u Crater 11:15 a.m. May 18, 1924 - one of many in a series of similar events during May 11-27. Photo from northwest rim of Kīlauea summit, present site of HVO. (Credit: Maehara, K. Public domain.)

Larger events can generate pyroclastic surges—hot, ground-hugging, and fast-moving currents of rocks and gas—and send a column of rocks, ash, and gas high into the atmosphere. During large explosive eruptions, wind disperses the finest rock particles (ash) and gases tens to hundreds of kilometers (miles) from an erupting vent and can result in heavy ash fall downwind. Volcanic ash can make breathing difficult and can cause buildings and structures to collapse (especially when the ash is wet), damage agricultural crops, and contaminate grass used for livestock feed. The downwind ash plume from such eruptions also poses a hazard to aircraft.

The USGS sponsored Volcanic Ashfall Impacts Working Group offers resources and guidance for ashfall preparedness and impact.

 

Lava fountain 450 m (1,475 ft) high from Kīlauea Pu‘u ‘Ō‘ō eruption, 1984. Smallest tephra in dark column behind fountain transported southeast tens of kilometers by prevailing trade winds.

 

Lava fountain 450 m (1,475 ft) high from Kīlauea Pu‘u ‘Ō‘ō eruption...

Lava fountain 450 m (1,475 ft) high from Kīlauea Pu‘u ‘Ō‘ō eruption, 1984. Smallest tephra in dark column behind fountain transported southeast tens of kilometers by prevailing trade winds. (Credit: Heliker, Chrisitna. Public domain.)

Lava fountains generate airborne lava fragments, with limited fallout on ground

 

The small-scale explosive activity of lava fountains shreds and blasts molten rock into the air, forming a variety of lava fragments that solidify as tephra and fall back to the ground. Most fragments land within a few hundred meters from the vent, typically forming a spatter cone or rampart. Finer windborne fragments, however, can be carried many tens of kilometers (miles) downwind of the vent.

For example, in 1984-1986 during the episodic lava fountains at Pu‘u ‘Ō‘ō, tephra reached the town of Nā‘ālehu about 63 km (39 mi) from the vent. The tephra that fell on inhabited areas was not harmful to most people, but it was a source of irritation to those with respiratory problems and an inconvenience to the many residents with rain-water-catchment systems. Following some of the lava fountain episodes, Hawai‘i County Civil Defense recommended that people disconnect and clean their rain-water-catchment systems to prevent the particles from washing into their water supply.

 

Tephra deposits as thick as 11 m (36 ft) at summit of Kīlauea Volcano, Hawai‘i, were erupted during an extended period that included many explosive eruptions between about 1500 and 1800.

 

Large explosive eruptions most hazardous activity at Kīlauea Volcano

Color photograph showing an exposure of tan to grey volcanic tephra deposits

Tephra deposits as thick as 11 m (36 ft) at summit of Kīlauea Volcano, Hawai‘i, were erupted during an extended period that included many explosive eruptions between about 1500 and 1800. (Public domain.)

 

Satellite image, Kīlauea Volcano summit, Hawai‘i. Dashed line shows area covered by pyroclastic surge erupted in 1790. Solid line shows areas that may be covered by similar, future caldera eruption.

 

Eruption of lava flows is the dominant style of activity at Kīlauea today, but layers of fragmented rocky deposits on the volcano record many explosive eruptions during the past 2,500 years. For example, between about 1500 and 1800, at least a dozen pyroclastic surges swept across the summit area. One surge erupted in 1790 killed a large number of Hawaiians traversing the summit area near the current location of HVO—these deposits can be found as far as 3.5 km (2.1 mi) beyond the summit caldera. Other explosive events resulted in ash fall at the summit and over broad areas far downwind.

Unlike lava fountains, large explosive eruptionseject tephra that consists mostly of broken rock from the sides of the vent and little magma (molten rock). The largest of these eruptions are known to have resulted in rocks about 3 cm (1 in) in diameter falling on the south shore of Kīlauea and beyond into the sea. Tephra in the eruption column reached high into the westerly jet stream wind currents and were blown downwind.

These large explosive eruptions occurred in clusters over centuries, during times when a deep calderaexisted at Kīlauea Volcano's summit and few lavaflows were erupted. 
 

Satellite image, Kīlauea Volcano summit, Hawai‘i. Dashed line shows...

Satellite image, Kīlauea Volcano summit, Hawai‘i. Dashed line shows area covered by pyroclastic surge erupted in 1790. Solid line shows areas that may be covered by similar, future caldera eruption. (Public domain.)

The long-term hazards will be severe when a repeat of similar explosive eruptions occur over a period of several centuries. The early part of the next explosive period will likely include a major collapse of the summit caldera that lasts days to weeks. Such a dramatic shift will be apparent to everyone, because there will be many large-magnitude earthquakes that accompany collapse of the next caldera. After caldera formation, Kīlauea will not likely erupt continuously. There will likely be periods of years to decades between explosive eruptions. The change from the current effusive activity to intermittent explosive activity will challenge nearly everyone on the Island of Hawai‘i, but there is no way to forecast when the next explosive period may begin.

 

Additional resources relating to explosive eruptions and tephra hazards

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