Today’s Volcano Watch begins with a question: Can you guess when the next slow slip event will happen on Kilauea Volcano’s south flank? As a hint, the last one was in October 2015, and before then, events occurred in May 2012, February 2010 and June 2007. If this seems like a pattern, you’re right.
What is a “slow slip event” anyway?
Slow slip events are sometimes called “slow earthquakes” or “episodic slip events.” They happen when a fault begins sliding, just like in a regular earthquake, but so slowly that it takes several days to finish instead of several seconds.
At Kilauea, slow earthquakes occur on the nearly flat-lying decollement fault that underlies the volcano’s south flank at a depth of 6-8 km (4-5 mi). This is the same fault that was responsible for the magnitude-7.7 Kalapana earthquake in 1975.
However, slow earthquakes produce no seismic waves and, therefore, none of the damaging shaking of a regular earthquake.
Because of this, we actually look forward to them!
They help relieve a small amount of stress on the fault and give us a view into frictional properties of this hazardous fault beneath Kilauea.
Motion of Kilauea’s south flank is recorded by the USGS Hawaiian Volcano Observatory’s GPS monitoring network. These instruments show that the south flank moves steadily seaward about 6 cm (2.3 in) every year, which is attributed to a phenomenon called “fault creep.”
During a slow earthquake, the south flank surges seaward by an additional amount, usually about 3 cm (1.2 in). This additional motion occurs throughout the course of 2-3 days, and is about the same amount that would happen in a regular magnitude-6 earthquake.
Kilauea slow slip events tend to occur evenly in time; in particular, events after 2005 have occurred every 2.5 years, give or take three months. They also are caused by slip on the same section of the fault every time and tend to be about the same size.
In fact, Kilauea slow slip events are examples of so-called “characteristic” earthquakes — a series of several earthquakes of similar magnitude and location, which indicates that they are breaking the exact same part of the fault again and again. According to the “characteristic earthquake hypothesis,” this series should continue into the future, allowing scientists to forecast the time, location and size of a future earthquake.
The characteristic earthquake hypothesis was originally developed in hope that it could predict regular, and possibly damaging, earthquakes. This idea emerged from observations of a series of earthquakes that seemed to strike about every 22 years near the town of Parkfield, Calif.
After earthquakes in 1857, 1881, 1901, 1922, 1934 and 1966, all of which occurred as magnitude-6 events in the same part of the San Andreas Fault, scientists predicted the next earthquake would occur in 1988.
As it turned out, the next Parkfield earthquake did not occur until 2004, 16 years after the predicted date. However, even though the characteristic earthquake hypothesis wasn’t successful at predicting a regular earthquake, it has been useful for forecasting the occurrence of slow slip events around the world.
Locations where recurring, predictable slow slip events happen include the Cascadia Subduction Zone offshore of Washington and Oregon. This fault produces slow slip events equivalent to a magnitude-6.7 earthquake every 15 months. In Japan, on the subduction zone along the Nankai Trough, major slow slip events occur approximately every seven years and are equivalent to magnitude-7 earthquakes.
Because the most recent slow slip event on Kilauea happened in October 2015, and the events have a recurrence time of about 2.5 years, we can forecast that the next one might occur between now and August of this year. But remember, there won’t be any shaking or other effect that could be easily felt by individuals.
We’ll be keeping our eyes on HVO’s monitoring networks to know when the next slow slip event happens on Kilauea, and you’re also invited to keep an eye on HVO’s website for updated information (https://volcanoes.usgs.gov/hvo/).
Volcano activity updates
This past week, Kilauea Volcano’s summit lava lake level fluctuated with summit inflation and deflation, ranging about 31-39.5 m (102-130 ft) below the vent rim.
On the East Rift Zone, the 61g lava flow remained active downslope of Pu‘u ‘O‘o, with scattered breakouts on the pali and coastal plain, but no ocean entry. The 61g flows do not pose an immediate threat to nearby communities.
Mauna Loa Volcano is not erupting.
A few small-magnitude earthquakes occurred beneath the volcano, primarily on its west flank, at depths ranging 5-13 km (3-8 mi). Two small earthquakes also occurred near Mauna Loa’s summit at depths less than 5 km (3 mi).
GPS and InSAR measurements continue to show slow deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone. Rates of inflation in the past few months have decreased compared to rates of the past year. It is uncertain if these lower rates will persist or pick up again in the near future.
No significant changes in volcanic gas emissions were measured.
One earthquake with three or more felt reports occurred in Hawaii this past week: a magnitude-3.2 earthquake at 8:58 p.m. Feb. 20 that was 13 km (8 mi) southwest of Volcano and 30 km (19 mi) deep.
Visit HVO’s website (https://volcanoes.usgs.gov/hvo) for past Volcano Watch articles, Kilauea daily eruption updates, Mauna Loa weekly updates, volcano photos, maps, 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 (https://volcanoes.usgs.gov/hvo/hvo_volcano_watch.html) is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates. This week’s article is by HVO geophysicist Ingrid Johanson.