HONOLULU, Hawaii – For the first time in nearly 40 years, scientists were able to analyze magma erupting from the largest active volcano on Earth.
Mauna Loa in Hawaii erupted for about 12 days starting on Nov. 27, 2022, giving scientists the first chance to learn about the inner workings of the volcano since 1984 – the last time Mauna Loa erupted.
What the scientists discovered
Researchers found that the composition of lavas from Mauna Loa’s 2022 eruption was largely similar to those of its other eruptions dating back to 1843.
Lava from the 2022 eruption, however, had slightly lower average magnesium oxide (MgO) content than those of prior eruptions.
The MgO content of lava allows scientists to gauge how hot that magma may have been when it erupted as lava. Based on the lower average MgO content of lava from the Mauna Loa 2022 eruption, the lava measured approximately 2,111 degrees Fahrenheit.
Composition of the lava also indicates where the lava may have originated under the Earth’s surface. According to the USGS, the lava came from a new intrusion of homogenous magma.
How the lava was analyzed
Their analysis involved a number of facets, such as data from the Hawaiian Volcano Observatory’s (HVO) monitoring instruments being recorded during the eruption and direct observations and measurements from HVO field crews.
Another facet involved the collection of molten and solidified lava samples almost every day of the eruption for near-real-time analysis in laboratories, according to the USGS.
The samples were analyzed by using multiple methods in a lab environment.
One method involved energy-dispersive X-ray (ED-XRF) analyses, which was done in near-real-time. USGS said these studies revealed the composition of the erupting magma and the magma’s subterranean origins.
Methods used after ED-XRF analyses were secondary electron micro-analysis (SEM) and electron probe micro-analysis (EPMA). SEM and EPMA gave scientists an opportunity to measure the compositions of minerals and glass on small scales.