In the past, HVO would occasionally post images of people collecting lava samples on our website. These photos usually featured a person (with little-exposed skin) holding a rock hammer, with a metal bucket nearby. The bucket contained water to “quench” the sample, solidifying the hot lava into a cold glass. Natural-fiber or heat-resistant gloves, and sometimes a face mask, protected the sample collector from heat radiating off the 2,100-degree lava. The hammer was used to scoop some of the molten material into the bucket, which would hiss and steam in reaction; more water would be added to cool down the sample so it could be placed in a cloth bag.
HVO carefully archives or curates these precious geological samples collected by current and past HVO geologists, collaborators, visiting scientists, and volunteers. Most of the HVO samples were collected from around the island of Hawaii over the past several decades as part of HVO’s mission to monitor eruptive activity (sampling active lava flows) or to characterize previous volcanic activity (sampling prehistoric lava flows on or beneath the surface). For samples collected within Hawaii Volcanoes National Park, HVO works closely with National Park Service archivists to ensure appropriate record keeping and tracking.
When a sample is collected, it’s important to document the sample’s “metadata.” This includes the name of the sample collector, coordinates marking the sample location, and the collection date. if the sample was taken from molten lava, it’s labeled as a “quenched” sample, and the time of sample collection is also noted.
As part of metadata, geologists generally describe the sample location (such as the Southwest Rift Zone of Kilauea) and characterize the sample itself (a gray-colored, discontinuous, fine ash, for example). Usually, the sample is given a unique identifier (ID), often a combination of numbers and letters, which is written on the sample bag. This ID connects the sample to its metadata, which is entered into a searchable database.
Much preparation and forethought go into sample collection, with prior project planning, permitting, and gaining permission from landowners. For every geologist, it’s important to ask: “What question(s) will this sample help me to answer?” Samples are collected sometimes because their specific chemistry or physical characteristics can reveal important information that helps scientists to understand the past, or on-going, or potential future volcanic activity and hazards.
For example, a sample of ash from the Ka‘u Desert indicates that ash was deposited in that location at some point in the past and could, therefore, be deposited there in the future. Particle size and chemical analyses of the ash can provide information about the eruption magnitude (size) and character (was the eruption driven by steam or magmatic gas?).
Such information improves understanding of the range of behaviors Hawaiian volcanoes exhibited in the past and could exhibit in the future. Likewise, rapid analyses of molten lava samples during the 2018 lower East Rift Zone eruption allowed HVO to detect changes in magma chemistry that foretold a change in eruptive behavior — the arrival of increasingly hot and fluid lava — and associated hazards.
Several sample collections are currently being curated at HVO. The youngest consists of lava and ejecta from Kilauea’s 2018 lower East Rift Zone eruption and summit-collapse events. Other collections include lava samples from historical eruptions of Kilauea (including products of Pu‘u ‘O‘o and ejecta collected downwind of Halema‘uma‘u when there was an active lava lake); geological samples that aided in creating the Geologic map of the island of Hawaii; and ash and other ejecta collected as part of research to understand older explosive events in Kilauea’s history. The Pu‘u ‘O‘o collection in particular is perhaps unique in the world for its completeness and longevity covering a single eruptive event and is thus extremely valuable.
Each sample collection and resulting analytical data informs HVO and the wider volcanological community a little more about the behavior and hazards of Hawaiian volcanoes. These collections will continue to be an important resource for researchers, especially because some samples are from areas that are no longer accessible, having been covered by more recent lava flows or within the area of Kilauea’s summit that collapsed in 2018.
Eventually, one of Hawaii’s volcanoes will erupt again, and HVO will have another sample collection to curate and care for, and to help us understand Hawaiian volcanoes and their hazards a little more.
Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.
Volcano Activity Updates
Kilauea Volcano is not erupting. The USGS Volcano Alert level remains at NORMAL. Kilauea updates are issued monthly.
Kilauea monitoring data over the past month showed no significant changes in seismicity, sulfur dioxide emission rates, or deformation. The water lake at the bottom of Halema‘uma‘u continued to slowly expand and deepen.
Mauna Loa is not erupting. The USGS Volcano Alert level remains at ADVISORY. This alert level does not mean that an eruption is imminent or that progression to an eruption is certain. Mauna Loa updates are issued weekly.
This past week, about 87 small-magnitude earthquakes were recorded beneath the upper elevations of Mauna Loa; the strongest was a magnitude-3.9 event on March 19 in the Ninole Hills area. Monitoring data showed that slow summit inflation continued and fumarole temperature and gas concentrations on the Southwest Rift Zone remain stable.
There were three events with three or more felt reports in the Hawaiian Islands during the past week. A magnitude-1.7 earthquake occurred at 6:53 a.m. March 19 about 2 miles west-southwest of Pahala; a magnitude-3.2 earthquake was recorded at 6:20 p.m. March 18 about 13 miles southwest of Leilani Estates; and a magnitude-3.2 earthquake was recorded 4 miles west of Volcano at 9:16 p.m. March 15.
