Hawaiian Volcano Observatory


Kīlauea and other active Hawaiian volcanoes are ideal natural laboratories for researching how volcanoes work, because they are easy to access and have frequent eruptions and earthquakes. 

HVO geologist on rim of Halema‘uma‘u Crater downloading camera imag...

HVO geologist downloads images collected with infrared cameras set up on the rim of Halema‘uma‘u Crater. The cameras are aimed at an erupting lava lake to conduct a thermal survey of the lake's surface. (Public domain.)

Hawaii offers exceptional natural laboratories for scientists to monitor and study active volcanoes.

For more than 100 years, Hawaiian Volcano Observatory (HVO) scientists have developed new volcano-monitoring instruments and networks to record and document activity at Hawaiian volcanoes. Scientists use this monitoring data to better understand eruptions and earthquakes and to issue notifications of hazardous activity, which helps reduce impacts on communities. HVO also hosts scientists from around the world to help develop new monitoring methods and improve understanding of the dangerous consequences of earthquakes, tsunamis, and eruptions.

Monitoring networks provide data for research and public notifications.

HVO's monitoring networks consist of more than 100 field stations with instruments that record and measure earthquakes, ground movement, volcanic gases, sound waves, lava advancement, magma volume below ground, and visual changes in eruptive activity. These field stations continuously transmit data by radio signal to the observatory, where it is recorded, processed by specialized computer programs, and analyzed by scientists.

In addition to ground-based sensors, satellite data are used to detect changes in ground elevation and surface temperature, which can indicate lava or other eruptive activity. Sudden shifts in data are detected automatically, and HVO scientists are notified immediately for closer inspection and response. If monitoring data indicate significant changes in a volcano's activity, scientists issue public notifications.

HVO technicians working on seismic station at summit of Kīlauea Vol...

HVO technicians install a solar-powered seismic station near the summit of Kīlauea Volcano to monitor earthquake activity. The seismic data is transmitted via radio signal directly to the observatory, where the data is initially analyzed by automatic computer programs and then examined in greater detail by a seismologist. Mauna Loa Volcano in background. (Credit: Babb, Janet. Public domain.)

HVO is responsible for monitoring and reporting earthquakes in Hawaii.

HVO, unique among U.S. volcano observatories, has the USGS responsibility to record and report on the thousands of earthquakes that occur every year in Hawaii, mostly beneath the Island of Hawai‘i. The HVO seismic-monitoring network is part of the USGS Advanced National Seismic System (ANSS).

Most earthquakes in Hawaii are directly related to the movement, storage, and eruption of magma at the active volcanoes. These volcanic earthquakes are usually small—typically less than magnitude 4—and pose only a limited hazard. Much larger earthquakes can occur in structurally weak areas within and at the base of Hawaiian volcanoes. These large events, such as the 1975 Kalapana (magnitude 7.7) and 2006 Kīholo Bay (magnitude 6.7), are widely felt and have the potential to cause extensive damage throughout the Hawaiian Islands.

Tracking active lava flows allows scientists to provide warnings.

Geologist collecting sample of molten lava from 2011 Kamoamoa erupt...

HVO geologist carries a freshly quenched lava sample from the 2011 Kamoamoa fissure eruption on Kīlauea Volcano. Molten lava is quickly placed in a bucket of water to "freeze" the growth of minerals for chemical and microscopic analyses. (Public domain.)

Today, lava flows are the dominant style of activity of Hawaiian volcanoes, and tracking their advancement is a core HVO monitoring responsibility. Geologists document the movement and evolution of active flows under different conditions to better understand how lava advances and to provide warnings for people downslope from erupting vents.

Lava flows from the 1983–2018 Puʻuʻōʻō eruption on Kīlauea Volcano's East Rift Zone were monitored closely to determine their ever-changing eruption rates, locations, inundation areas, advance rates, and emplacement styles. Scientists also study the formation and evolution of lava tubes, which insulate the molten lava within them, allowing flows to travel greater distances.

Key methods for monitoring active lava flows include ground-based and aerial observations and mapping, webcam imagery, satellite-based data and images, and collecting lava samples for temperature, chemical, and mineral analyses.

Volcanic gases provide a record of magma movement and pose unique hazards.

The first volcanic gas measurements in the world were carried out at Kīlauea Volcano more than 100 years ago, and HVO's record of gas monitoring and innovation continues today. Measuring the composition of different volcanic gases and their changing emission rates is essential for characterizing the state of active volcanoes in Hawaii, because different gases are released as magma accumulates and rises beneath the surface. HVO began regular measurements of sulfur dioxide gas emissions at Kīlauea in 1979, and new methods for measuring these emissions are tested and used by HVO and other scientists in Hawaii. This gas monitoring is key to assessing volcanic air pollution (known locally as vog), which affects widespread areas downwind.

HVO geochemist measuring gas compositions during 2011 Kamoamoa erup...

HVO gas geochemist uses a Fourier transform infrared (FTIR) spectrometer to measure volcanic gas compositions emitted during the 2011 Kamoamoa fissure eruption on the East Rift Zone of Kīlauea Volcano. The instrument measures the infrared energy from the hot lava fissure as it passes through, and is absorbed by, the volcanic plume along an open atmospheric path. Individual gas species, including sulfur dioxide, carbon dioxide, water vapor, hydrogen chloride and others, absorb light energy and can be quantified within different wavelength regions of the energy spectrum. (Public domain.)