Volcano Watch: What causes the collapse/explosion events at Kilauea’s summit?

  • Graphic created by BRIAN SHIRO A generalized graphic of how a collapse/explosion event sequence can occur. The upper graphic represents a cross-section of the crater filled with rock rubble and the lower graphic is an example of a typical number of earthquakes observed during a particular phase of the collapse/explosion cycle. Initially, the piston is supported by the magma reservoir. It is stable and there is very low seismicity. Second, as magma drains, stress on the faults increases and there is an earthquake swarm on the caldera ring faults. Third, the piston collapses down from its own weight. A large collapse earthquake occurs and a plume can result.

  • Photos by INGRID JOHANSON Aerial images of Halema‘uma‘u crater from May 27 and June 18. Note how the crater has enlarged during a three-week period, as shown in the June 18 photo. Also visible are cracks on the crater floor because of ongoing subsidence at the summit.

At the summit of Kilauea Volcano, Halema‘uma‘u has changed dramatically since early May.

As the crater walls and inner caldera slump inward, the depth of Halema‘uma‘u has more than tripled and the diameter has more than doubled. Before May, about 10 earthquakes per day were typical at the summit. As of late June, there are about 600 earthquakes located in the same region on a daily basis. Many of these earthquakes are strong enough to be felt, and some can be damaging. These earthquakes are understandably causing concern, especially in Volcano Village and surrounding subdivisions.

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What is causing these earthquakes?

The short answer is that the rigid rock of the caldera floor is responding to the steady withdrawal of magma from a shallow reservoir beneath the summit. As magma drains into the East Rift Zone (traveling about 40 km (26 mi) underground to erupt from fissures in the Leilani Estates subdivision), it slowly pulls away support of the rock above it. Small earthquakes occur as the crater floor sags. The collapse/explosion event is triggered when the caldera floor no longer can support its own weight and drops downward. Large collapses can produce an explosion and ash plume that rises above the crater.

An example of this is the most recent event that occurred at 4:49 a.m. June 28. An ash-poor plume rose about 300 m (1,000 ft) above the ground and drifted to the southwest. The energy released by the event was equivalent to a magnitutude-5.3 earthquake. Since May 16, we have observed intervals between collapse/explosion events as short at eight hours and as long as 64 hours. The average is about 28 hours, which is why they seem to happen on an almost daily basis.

Analyses of data from tiltmeters, GPS stations, seismometers, gas measurements, satellite and visual observations are ongoing, and several hypotheses could explain the processes occurring at the summit.

A leading concept is that incremental collapses beneath the caldera act as a piston dropping on top of a depressurized magmatic system. This collapse process culminates in a large earthquake that might be strong enough to be felt by residents in the area. It also can produce an explosion in which gas drives ash into the atmosphere.

After a large collapse/explosion event, the stress on the faults around Halema‘uma‘u is temporarily reduced, resulting in fewer earthquakes. Several hours later, as magma continues to drain out of the summit, stress increases on the faults around Halema‘uma‘u and earthquake rates increase and grow to a constant level that continues for several hours before the next collapse/explosion event.

The collapse/explosion events generate plumes that have become progressively more ash-poor and now rise only a few thousand feet above the crater. This is in contrast to the eruptive sequence from May 16-26, when the vent within Halema‘uma‘u crater was open so ash plumes could rise into the air during each collapse/explosion event, like the event May 17 that sent an ash plume to 30,000 feet.

But by May 29, rock rubble from the crater rim and walls had filled the vent and a portion of the conduit that comprises the shallow magma reservoir might have partially collapsed, blocking the path for most of the ash to escape.

Since June 21, nearby residents have reported feeling stronger, more intense shaking from the collapse/explosion events. Why do they feel stronger when the location and magnitude are about the same? It is possible that another partial collapse of the shallow magma reservoir occurred, also changing subsurface geometry. This changed the character of the seismic waves, which now have more high frequencies (shorter wavelengths) that people might feel more intensely.

An analogy is a home theater or car stereo. Imagine you have it set at a constant volume (like the consistent earthquake magnitude) but then change the dials to increase the treble while lowering the bass slightly. The total energy is the same, but it’s just being expressed in different frequencies. This is why, through time, people might be reporting they are feeling these events more widely and intensely.

One of the most frequently asked questions is when will this end?

The response is not so straightforward.

The summit continues to subside as magma moves from the shallow reservoir beneath the Kilauea summit into the lower East Rift Zone.

As this process continues, Halema‘uma‘u will continue to respond with collapse/explosion events.

If you feel strong shaking, remember to drop, cover and hold on until it stops.

Be sure to quake-proof your home, school and business. Look here for tips: https://www.shakeout.org/hawaii/resources.

Also, help the USGS by reporting at https://earthquake.usgs.gov/dyfi if you feel an earthquake.

Volcano activity updates

On Kilauea Volcano’s lower East Rift Zone, lava from the fissure 8 spatter cone continues to flow in an established channel to the Kapoho coastline. Minor overflows from the channel occur periodically, but are short-lived and do not extend beyond the current flow field. At the coast, the northern margin of the flow field is oozing lava at several points in the area of Kapoho Beach Lots. The lava channel has crusted over about 0.8 km (0.5 mi) inland of the ocean entry. Lava enters the sea over a broad area on the northern side of the entry area. Residents in the lower Puna District of Hawaii Island should remain informed and heed Hawaii County Civil Defense closures, warnings and messages (www.hawaiicounty.gov/active-alerts). At Kilauea’s summit, at 4:49 a.m. June 28, after approximately 26 hours of elevated seismicity, a collapse explosion occurred at the summit, producing an ash-poor steam plume that rose about 1,000 ft above the ground surface. The energy released by the event was equivalent to a magnitude-5.3 earthquake. Inward slumping of the rim and walls of Halema‘uma‘u continues in response to ongoing subsidence at the summit.

At Mauna Loa, HVO seismic and deformation monitoring networks have been recording near background levels of seismicity and ground motion for at least the past six months. These observations indicate the volcano is no longer at an elevated level of activity. Accordingly, HVO dropped the Mauna Loa alert level to “Normal” and the aviation color code to “Green.” HVO continues to monitor the volcano closely and will report any significant changes.

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Visit the HVO website (http://hvo.wr.usgs.gov) for past Volcano Watch articles, Kilauea daily eruption updates and other volcano status reports, current volcano photos, recent earthquakes and more; email questions to askHVO@usgs.gov.

Volcano Watch (http://hvo.wr.usgs.gov/volcanowatch/) is a weekly article and activity update written by U.S. Geological Survey`s Hawaiian Volcano Observatory scientists and colleagues.

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