A lot has changed during the past year on Kilauea Volcano. ADVERTISING A lot has changed during the past year on Kilauea Volcano. One year ago, the June 27 flow was threatening to cross Pahoa Village Road and, potentially, Highway
A lot has changed during the past year on Kilauea Volcano.
A lot has changed during the past year on Kilauea Volcano.
One year ago, the June 27 flow was threatening to cross Pahoa Village Road and, potentially, Highway 130. Lava destroyed one house Nov. 10, 2014, and was moving downslope toward many others.
Now, there is no imminent threat to Pahoa, and life in the lower Puna District largely has returned to normal.
So, what exactly happened to the Pu‘u ‘O‘o eruption during the past year?
In a word: disruption.
Pu‘u ‘O‘o has erupted nearly continuously for more than 32 years, but continuous does not imply steady. Instead, fluctuations in lava supply rate have been common, and these disruptions changed the vigor and reach of the flow field activity during the past year.
Let’s use a car as an analogy.
A drop in the lava supply rate is like easing your foot off the gas pedal. The lava flow, like the car, will slow down. If the lava supply rate drops enough, the flow can stall, similar to a car without enough gas.
An increase in the lava supply rate is analogous to pressing down on the car’s gas pedal. The lava flow, like the car, will speed up. But if the lava supply rate (or a car engine’s RPM) gets too high, their respective systems can rupture or fail.
Very high lava supply rates can trigger breakouts of lava from the tube system that rob lava from the flow front, causing it to stall — just as running an engine too high can trigger mechanical failure and cause the car to stop.
As with a car, a lava flow needs to operate within a certain “envelope” of efficiency to continue advancing. Lava activity outside this envelope — too little or too much — causes the flow front to stall. During the past year, major fluctuations in the lava supply rate have pushed the flow out of this envelope several times, disrupting the flow front advance.
A simple way to track lava supply rate is to look at Kilauea’s summit tilt.
Deflation of the summit magma reservoir normally is associated with a drop in lava supply rate, while inflation means an increase.
The day before Halloween 2014, a rapid drop in the lava supply rate occurred, causing the tip of the June 27 flow to stall about 155 m (170 yards) from Pahoa Village Road. About two weeks later, a major increase in lava supply rate triggered upslope breakouts from the tube, completely shutting off the flow front near Pahoa Village Road.
The lava supply rate remained steady enough for the next two months that a new lobe of lava advanced downslope once again, this time toward the Pahoa Marketplace, in late December. Fortunately, the lava supply rate was low and the flow front essentially stalled in January.
Another increase in lava supply rate triggered breakouts upslope of Pahoa in mid-March. As in November 2014, these upslope breakouts robbed supply from the flow front near Pahoa Marketplace, causing it to shut down.
Since March, surface flows have remained active, but haven’t strayed too far from Pu‘u ‘O‘o, staying within about 8 km (5 miles) of the vent. In fact, the farthest reach of Kilauea’s active breakouts has retreated slightly the past couple of months, and, as of this week, was 6.4 km (4 mi) northeast of Pu‘u ‘O‘o.
This is good news, of course.
But why haven’t the flows advanced very far during the past six months?
It most likely is because of a relatively low lava supply rate — or, in car terms, the gas pedal simply isn’t being pushed very hard at the moment.
With flows now closer to Pu‘u ‘O‘o and farther upslope from residential areas, there is no immediate threat to homes or roadways, as there was a year ago. But as we’ve seen throughout this eruption, lava supply rates fluctuate, and future increases in lava supply could restart slow advancement of the flow front toward communities.
Changes in lava flow activity can occur abruptly and with little warning, so the USGS Hawaiian Volcano Observatory continues to closely monitor the June 27 flow with on-site field visits, helicopter overflights, webcam imagery and satellite data.
Volcano activity updates
Kilauea continues to erupt at its summit and East Rift Zone.
The summit lava lake level varied between about 45 and 70 m (148–230 ft) below the vent rim within Halema‘uma‘u Crater. On the East Rift Zone, scattered lava flow activity remained within about 6.4 km (4 mi) of Pu‘u ‘O‘o.
Mauna Loa is not erupting. During the past week, earthquake rates continued to be elevated above background levels, though at a lower weekly rate than recorded in late summer.
Deformation data remain consistent with inflation of magma reservoirs within the volcano.
There were no earthquakes reported felt on the Island of Hawaii this past week.
Visit the HVO website (http://hvo.wr.usgs.gov) for past Volcano Watch articles, Kilauea daily eruption updates, Mauna Loa weekly updates, volcano photos, recent earthquakes info, and more; call for summary updates at 808-967-8862 (Kilauea) or 808-967-8866 (Mauna Loa); email questions to askHVO@usgs.gov.
Volcano Watch (http://hvo.wr.usgs.gov/volcanowatch/) is a weekly article and activity update written by scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory.
