Kīlauea’s inflation means we might see more lava soon…

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Last week we discussed the change in seismicity that has occurred at Kīlauea.

Kīlauea's inflation means we might see more lava soonà...

This map shows the pattern of displacements recorded by GPS stations across Kīlauea Volcano since the start of October. The length of each arrow is proportional to the velocity that the GPS station has moved. The red scale arrow in the lower left shows the length of an arrow that indicates 5 cm/yr (an arrow twice as long would therefore indicate 10 cm of motion per year, and so on). Circles at the ends of the arrows indicate measurement error; there is a high degree of certainty that the arrow ends within the circle. The overall deformation pattern is inflation, or swelling, of the volcano. Arrows pointing away from Kīlauea caldera and the east rift zone indicate swelling due to magma accumulation beneath the surface.

(Public domain.)

The increased number of earthquakes along the upper east rift zone has also been accompanied by inflation of the summit, Pu‘u ‘Ō‘ō, and parts of the east rift zone between the two locations. Inflation began in earnest at the start of October (about the same time as the increased earthquake activity) and was shown by GPS and tiltmeter data that monitor changes in the shape of the volcano (these data can be viewed at http://hvo.wr.usgs.gov/kilauea/update/deformation.php).

Fundamentally, the inflation is caused by a disparity in Kīlauea’s magma budget—that is, more magma enters the volcano than is erupted. This means that either the amount of magma supplied to the volcano has increased, the amount erupted has decreased, or both.

A similar disparity may have prompted Kīlauea’s March 2011 Kamoamoa fissure eruption. The start of inflation at the summit, Pu‘u ‘Ō‘ō, and parts of the east rift zone and rising summit lava level in Halema‘uma‘u, beginning in late 2010, were indications of more magma coming into the volcano than was being erupted (comparable to what is occurring now). The inflation rate increased until March 5, 2011, when the 4.5-day-long Kamoamoa fissure eruption occurred between Napau Crater and Pu‘u ‘Ō‘ō. The eruption disturbed the east-rift-zone plumbing system, and several months passed, during which eruptive events occurred in August and September 2011. Steady lava effusion returned to Pu‘u ‘Ō‘ō, but the eruption rate has still not returned to pre-2010 values.

The increased rate of inflation extending from the summit to Pu‘u ‘Ō‘ō in the past month has been accompanied by continued, but slow, advance of a narrow lava flow across the coastal plain. A possible increase in this activity, though hard to measure, may be evidence of a small increase in eruption rate despite the constriction in Pu‘u ‘Ō‘ō.

Not only was the 2011 Kamoamoa eruption preceded by inflation, but there was also a major increase in the number of earthquakes along the upper east rift zone, as well as a rise in the level of the lava lake at Kīlauea’s summit—similar to the activity that is occurring now. Given the parallels between 2011 and today, the question everyone is asking is: Are we on the path to a new eruptive event at Kīlauea?

If current activity continues, the answer is probably “yes.” Kīlauea cannot erupt all of the magma that is coming in to the volcano, resulting in a buildup of pressure. This pressure can only be relieved by a decrease in the magma supply coming into the volcano, an increase in the eruption rate at Pu‘u ‘Ō‘ō, or an intrusion into south Kīlauea Caldera or one of Kīlauea’s rift zones, which may (or may not) culminate in the opening of a new eruptive vent.

If a new vent opens, where might it be? Past patterns suggest that new activity will probably occur somewhere along the east rift zone between the summit and near Pu‘u ‘Ō‘ō. We continue to record a high level of seismic activity beneath the summit caldera and within the upper east rift zone centered beneath Koko‘olau (Ko‘oko‘olau) Crater. While this has been a typical seismic pattern over the past 50 years, historical eruptions have not occurred there but were located either uprift—west of Lua Manu and within the south summit caldera—or downrift, between Hi‘iaka Crater and Pu‘u ‘Ō‘ō. Since 1983, many new vents have formed in the vicinity of Pu‘u ‘Ō‘ō.

Eruptions along the southwest rift zone and the lower east rift zone (downrift of Pu‘u ‘Ō‘ō) are less common historically. That is not to say, however, that eruptions cannot or will not happen in those places. Indeed, future eruptions will eventually occur in all parts of Kīlauea’s rift zones and summit area—the reason why HVO maintains a robust monitoring network across the entire volcano.

Perhaps the best lesson of the current inflation, seismicity, and lava level rise is that it pays to be vigilant. Kīlauea is giving warning signs of a potential change in eruptive activity, allowing everyone to prepare for that eventuality. The scientists at HVO are currently busy making measurements and deploying additional instruments to best track the evolving activity, which will teach us more about how Kīlauea works.

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Volcano Activity Update

A lava lake within the Halema‘uma‘u Overlook vent produced night-time glow that was visible from the Jaggar Museum overlook and by HVO's Webcam during the past week. The lava lake reached a new high level last weekend, about 22 m (72 ft) below the floor of Halema‘uma‘u Crater on October 26. Cracking and booming noises, caused by thermal fracturing of the vent wall, continued to emanate sporadically from the vent.

On Kīlauea's east rift zone, surface lava flows are still accumulating at the base of the Pulama pali within the abandoned Royal Gardens subdivision. The flows reached within 1.3 km (about 0.8 mile) from the shoreline on October 29 and continued to advance slowly. Within the Pu‘u ‘Ō‘ō crater, the northeastern pit still holds a circulating lava lake. Occasional flows were erupted from a pit on the southern side of the crater floor.

No earthquakes were reported felt across the Island of Hawai‘i during the past week.