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Volcano Watch: How Measuring Gravity on Mauna Kea Helps us Monitor Mauna Loa

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Article by US Geological Survey Hawaiian Volcano Observatory scientists and affiliates.

Gravimeters, essentially extremely precise pendulums, can measure a change in the force of gravity to one-in-one billionth of the force you feel every day. This force varies based on the distance and the amount of mass between the instrument (or you) and the center of the Earth.

A gravimeter measuring the force of gravity on Mauna Kea. These measurements are used to calibrate the instruments so they can precisely monitor changes in gravity from magma accumulation at Mauna Loa (background). USGS photograph taken on December 10, 2020. Public domain.

It’s 5 a.m. and a somewhat sleepy scientist is getting ready to leave his home in Honomū and head to the USGS Hawaiian Volcano Observatory office on Kamehameha Avenue in Hilo. Yawning—and not quite fully caffeinated—he says goodbye to the dog following him around the kitchen who’s wondering why they’re up so early.

At the HVO office, he picks up two identical instruments the size of a shoebox—gravimeters—and loads them into a USGS four-wheel-drive vehicle. Today will be a long day driving from Hilo to the summit of Mauna Kea and back—twice.

But these days are necessary, and any day spent on the mountain is a good day, especially if the sky is clear and views stretch to the horizon. Between Hilo and the summit of Mauna Kea, the HVO scientist will stop approximately half a dozen times at a series of locations (benchmarks) established beginning in the 1960s. At these benchmarks, the two gravimeters will be used to measure the variation of the force in gravity.


Days like this one are not particularly eventful; they consist of driving from one measurement site to another and waiting for the gravimeters to stabilize at each new site. They’re filled with audiobooks, Hawaiʻi Public Radio and listening to the sounds of the wind. These are not the exciting days trekking on the floor of Kīlauea caldera or flying by helicopter to the summit of Mauna Loa.

Gravimeters, essentially extremely precise pendulums, can measure a change in the force of gravity to one-in-one billionth of the force you feel every day. This force varies based on the distance and the amount of mass between the instrument (or you) and the center of the Earth.

Just like atmospheric pressure, the force of gravity changes depending on your altitude. For example, the higher in elevation you go (like driving up a mountain), the farther away you are from the center of the Earth (and its mass), and the weaker the force of gravity. This elevation effect is the primary contribution to changes in gravity measured on Mauna Kea. The changes in gravity are not as noticeable as the change in the atmosphere (it’s hard to breathe at the summit), but the average person also weighs about one-third of a pound less—equivalent to the weight of an orange—at the summit of Mauna Kea than they do in Hilo! 

Since the 1970s, small changes in time-varying gravity (microgravity) have been measured on the active volcanoes Mauna Loa and Kīlauea to determine whether magma is accumulating in their magma reservoirs. This intruding magma often opens and fills cracks and/or empty spaces, causing a net increase in the volcano’s mass that can be measured with a gravimeter. Measuring the gravity is an independent way to confirm whether ongoing uplift, like that occurring at Mauna Loa since 2014, is from new magma intruding into the volcano.


The precision and sensitivity of the gravimeters makes them extremely delicate, and they require regular calibration. As the dominant effect we measure is from changes in elevation, our ability to measure volcanic changes on the high elevations of Mauna Loa (13,680 ft or 4,170 m) requires us to calibrate the instruments over similar elevations on Mauna Kea where there is currently no influence from volcanic activity (the last eruption was more than 4,500 years ago). Without Mauna Kea, we would have to send the gravimeters back to California to be calibrated, making them susceptible to damage on their long journey.

The opportunity to calibrate HVO gravimeters on Mauna Kea provides the ability to design a gravity monitoring program to help understand volcanic unrest at Mauna Loa. Along with ground deformation and seismicity, future gravity surveys could help detect how much magma is slowly being supplied to Mauna Loa’s shallow magma storage system. On the Island of Hawaiʻi, Mauna Kea and Mauna Loa have played important roles in the past; today, they are acting together to help inform us about future volcanic activity.

Volcano Activity Updates  

Lava activity is confined to Halemaʻumaʻu with lava erupting from a vent on the northwest side of the crater.  Laser rangefinder measurements this morning, April 22, indicate that the lava in the western (active) portion of the lake is 226 m (741 ft) deep, with the eastern portion of the lava lake solidified at the surface. The summit tiltmeters recorded minor change over the past 24 hours. Sulfur dioxide emission rates measured on April 14 were 950 t/d. Seismicity remains stable, with elevated tremor. 

Mauna Loa is not erupting and remains at Volcano Alert Level ADVISORY. This alert level does not mean that an eruption is imminent or that progression to an eruption from the current level of unrest is certain.


This past week, about 175 small-magnitude earthquakes were recorded below Mauna Loa; most of these occurred below the summit and upper-elevations at depths of less than 8 kilometers (about 5 miles). Global Positioning System (GPS) measurements continue to show a slightly extensional summit deformation pattern over the past week. Gas concentrations and fumarole temperatures at both the summit and at Sulphur Cone on the Southwest Rift Zone remain stable. Webcams show no changes to the landscape.

There were 3 events with 3 or more felt reports in the Hawaiian Islands during the past week: a M3.0 earthquake 1 km (0 mi) ENE of Pāhala at 36 km (22 mi) depth on April 21 at 2:09 a.m. HST, a M2.8 earthquake 6 km (3 mi) E of Pāhala at 35 km (21 mi) depth on April 20 at 11:08 a.m. HST, and a M3.2 earthquake 23 km (14 mi) E of Honaunau-Napoopoo at 3 km (2 mi) depth on April 16 at 7:46 p.m. HST.

HVO continues to closely monitor both Kīlauea’s ongoing eruption and Mauna Loa for any signs of increased activity.   

Volcano Watch is a weekly article and activity update written by USGS HVO scientists and affiliates. 

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