VOLCANO WATCH: Scientists Detail Kilauea Magma Intrusion

# VOLCANO WATCH: Scientists Detail Kilauea Magma Intrusion

USGS: “Pu‘ukoa‘e, on the Southwest Rift Zone of Kīlauea, is prominent in this aerial photo taken on February 6, 2024. The slopes of Mauna Loa and the Nīnole Hills are visible in the background.” (USGS photo by H. Winslow)
Kīlauea is currently not erupting, and its USGS Volcano Alert level is still at ADVISORY. This is due to a decrease in seismic activity following the recent intrusion of magma into the area.

According to the latest Volcano Watch article by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates, last week, USGS Hawaiian Volcano Observatory (HVO) scientists closely monitored earthquakes and ground deformation in the region southwest of Kīlauea’s summit. The increased unrest led to the raising of the Alert Level/Aviation Color Code for Kīlauea to WATCH/ORANGE on January 31 as another intrusive event began beneath the surface.

Intrusions occur when magma breaks rock to create new pathways within the ground. As magma moves beneath the surface into its new space, the ground above it deforms to accommodate the new material. HVO detects intrusions through earthquake locations and changes in the ground surface known as deformation, which can be recorded using tiltmeters, GPS, and satellite-based methods.

Earthquake swarms south of Kīlauea caldera began over the weekend on January 27. This activity was not unexpected, as intermittent earthquake swarms have been occurring in the south caldera since October 2023, and there is a known body of magma in this area.

However, on January 31, earthquake activity significantly increased, with over 700 earthquakes detected throughout the day. The actual number of earthquakes was likely much greater, as many of the smallest earthquakes went undetected in the intense swarm of activity.

Around the same time, tiltmeters at Uēkahuna bluff (the summit of Kīlauea) and Sand Hill (southwest of the caldera) began to show changes to the ground surface. Starting just before 4:30 a.m. HST in the morning, the tiltmeters began to show highly variable directions and rates, indicative of crack growth that can precede either an eruption or intrusion. This prompted HVO to raise the Alert Level/Aviation Color Code for Kīlauea to WATCH/ORANGE at 4:41 a.m. HST.

The U.S. Geological Survey (USGS) map shows the location of the latest earthquake activity south of the Kīlauea caldera on February 2, 2024.

HVO seismologists were analyzing earthquake locations in real time, ready to collect data in the event of a new eruption. However, earthquake locations migrated farther to the southwest, along the Koaʻe fault system. By the evening, the tiltmeters showed a more consistent deflationary signal. These monitoring datasets indicated that magma had opened a new pathway and was moving from the storage system below Kīlauea summit to the southwest.

These observations were later confirmed with satellite-based InSAR data, showing deflation of the summit area as the region southwest uplifted and spread apart. In the center of the uplifted area, a narrow band of subsidence marks where the dike (a vertical sheet of magma) intruded, with a small section of ground dropping to accommodate lateral spreading.

USGS: “This map shows recent unrest at Kīlauea volcano. Yellow circles mark earthquake locations from January 31, 2024, through February 3, 2024, as recorded by HVO seismometers. Colored fringes denote areas of ground deformation over a one-day timeframe from 6 p.m. HST on January 31 through 6 p.m. HST on February 1, 2024. More fringes indicate more deformation. The complex patterns indicate overall deflation of the summit area as magma moved underground to the southwest, where the patterns show uplift and spreading (along with subsidence) due to intrusion of a dike (a vertical sheet of magma).”

By February 2, the numbers of earthquakes began to decrease, along with ground deformation rates. On the morning of February 3, HVO lowered the Alert Level/Aviation Color Code for Kīlauea back down to ADVISORY/WATCH.

While there have been several intrusions in the south caldera region of Kīlauea over the years, the recent intrusion extended farther southwest, towards Puʻukoaʻe and the Kamakaiʻa Hills on the Southwest Rift Zone of Kīlauea. This resulted in surface cracks forming in loose Keanakākoʻi tephra along the Maunaiki trail near Twin Pit Craters in the Kaʻū Desert of Hawai‘i Volcanoes National Park.

USGS: “An aerial view of the Twin Pit Craters near Maunaiki trail in the Kaʻū Desert of Hawaii Volcanoes National Park.” (USGS photo by K. Mulliken)

The south caldera area and Koa‘e fault system are informal names for specific geographic areas that we see on the surface of Kīlauea, but they extend into the subsurface. There is a well-known magma body beneath the south caldera region and the Koaʻe faults are structural features related to Kīlauea’s south flank. However, how these features are connected beneath the surface, to each other, and to the Southwest Rift Zone of Kīlauea is not well-understood.

Intrusions are a common process that volcanoes around the world experience, acting as a pressure-release valve for the magma reservoir. Although there hasn’t been an eruption at Kīlauea since September 2023, the recent intrusion shows that the volcano has been very active beneath the surface.

Author: OpenAI