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August 16, 2022

The earthquake swarm in the Manuʻa islands of American Samoa continues, with a source closer to Taʻū island than Vailuluʻu seamount.

U.S. Geological Survey
Monday, August 15, 2022, 6:17 PM HST (Tuesday, August 16, 2022, 04:17 UTC)

TA'U ISLAND (VNUM #244001)
14°13'48" S 169°27'14" W, Summit Elevation 3054 ft (931 m)
Current Volcano Alert Level: UNASSIGNED
Current Aviation Color Code: UNASSIGNED


No significant changes over the past 24 hours. The earthquake swarm in the Manuʻa islands of American Samoa continues, with a source closer to Taʻū island than Vailuluʻu seamount. A microseismometer (earthquake-detecting device) installed in Fitiʻuta village on Taʻū island on August 13 is recording approximately 30-60 earthquakes per hour; most events are too small to be felt. Estimated magnitudes of the largest earthquakes, including the felt events, are between magnitude 2 and 3.

Observations and Reports

  • There were no significant changes overnight and conditions remain the same as reported on Sunday, August 14, 2022.
  • Residents of the Manuʻa group of islands in American Samoa continue to feel earthquakes. Residents reported that earthquakes began about 3 weeks ago and this fits with a felt earthquake report from July 26th.  
  • The largest events recorded over the past 24 hours appear to be between magnitude 2 and 3. Approximately 30-60 earthquakes are occurring per hour, but most are too small to be felt. 
  • Reports suggest that the earthquakes vary in intensity, but are generally short, sharp jolts. The earthquakes are more likely to be felt by people indoors at rest and along the coast, where buildings sit on sediment that amplifies shaking. These factors are probably responsible for the variability in reporting.
  • Based on the analysis of earthquake data from a microseismometer installed on Taʻū island and felt reports, the source of these earthquakes is likely closer to Taʻū island rather than to Vailuluʻu. 
  • Scientists plan to install additional instruments to monitor earthquakes and other activity in the coming week.


The earthquake activity reported to date suggests a local source close to Taʻū island.

Due to limited earthquake monitoring equipment, the exact location of these earthquakes is currently unknown. A newly installed microseismometer in Fitiʻuta village on Taʻū island suggests that this activity is likely occurring closer to Taʻū island than the nearby submarine volcano Vailuluʻu.

We also received several hours of data on Sunday, August 14, from a seismometer placed in Olosega village on Ofu-Olosega islands. The earthquakes detected from this station were about twice as far away from their source as those detected in Fitiʻuta village on Taʻū island. While we cannot determine precise locations of the earthquakes yet, they seem closest to Taʻū island.

Not all earthquake swarms on volcanoes result in eruptions. Current low-level earthquake activity may continue and vary in intensity for days to months or longer without an eruption. It is also possible that the swarm is an early precursor to an eventual eruption. At this time, we cannot determine which of these possibilities is more likely. A large explosive eruption similar to the Tonga eruption earlier this year is extremely unlikely.

Scientists are also investigating reports of other activity provided by local residents. We value and appreciate these observations as residents have the experience to recognize significant changes in their environment and provide significant contributions to our understanding of activity.

Reports of exposed coral along the coast in the Manuʻa islands were investigated on August 12 and have been correlated with a King Tide that affected American Samoa. King Tides are more extreme than normal tides and thus may expose areas along the coast that are not exposed during a typical tide. However, USGS and other scientists will continue to investigate this event to confirm its origin.

Several residents of Taʻū reported booming noises on August 10; last night a resident of Olosega village reported a boom at the same time they felt an earthquake. Booming noises could have a number of natural and man-made sources including rockfalls, ground cracking, volcanic noise, and human caused events. USGS HVO scientists will be deploying infra-sound microphones in the coming weeks to capture and analyze noises in the region.


Experts at the Pago Pago National Weather Service Office (NWS), USGS Volcano Hazards Program, NOAA Pacific Tsunami Warning Center, NOAA-IOC International Tsunami Information Center, and USGS National Earthquake Information Center are working together with the American Samoa EOC to understand the source of these earthquakes better. The Samoa Meteorological Service is also reporting increased seismicity south or east of Tutuila Island.

Dr. Natalia Deligne of the US Geological Survey Hawaiian Volcano Observatory (HVO) arrived on August 11 in Pago Pago and is consulting with local authorities on the situation. Yesterday, August 14, she traveled to the Ofu-Olosega islands with local authorities to meet with residents and an install earthquake-monitoring instrument with the assistance of NWS staff. Today, Dr. Deligne is traveling back to Tutuila island.

On August 13, the USGS Hawaiian Volcano Observatory installed a microseismometer to monitor earthquake activity in Fitiʻuta village on Taʻū island. This instrument stopped recording data this morning, August 15, and HVO/NWS staff are trouble-shooting. On August 14th, Natalia Deligne traveled to Ofu-Olosega islands with other authorities to talk with residents and install a second microseismometer. The seismometer was installed in Olosega village and is transmitting data intermittently.  Staff are trouble shooting the instrument.  

USGS HVO staff member Dr. Drew Downs is traveling to Pago Pago on Monday, August 15, with additional microseismometers and other volcano-monitoring tools.

Additional HVO personnel and permanent seismometers for earthquake detection are expected to arrive in American Samoa later this week. These will allow HVO scientists to better locate where the earthquakes are occurring and identify the souce of the earthquakes.  

Dr. Charles McCreery, Director of the Pacific Tsunami Warning Center, will arrive Monday, August 15, to advise about tsunami concerns.


American Samoa’s volcanoes are monitored for earthquakes by a microseismometer in Fitiʻuta on Taʻū island (RS DataView BETA ( and a more distant global seismic station in Apia, Samoa (Station AFI USGS TELEMETRY DATA). The sparse monitoring stations may not allow for advanced warning of new activity. The USGS, NWS, PTWC, and other agencies are working together to improve this network so earthquake locations and magnitudes can be more precisely determined. USGS HVO scientists plan to install additional earthquake monitoring instruments in the coming weeks.

Remote sensing satellite data is also being used to monitor American Samoa for events potentially related to volcanic activity, such as thermal anomalies, volcanic plumes, or volcanic gases. This monitoring is being done by USGS Alaskan Volcano Observatory (AVO) scientists and the Wellington Volcano Ash Advisory Center (VAAC).

Residents can assist these monitoring efforts by noting and reporting accurate times that they feel earthquake shaking, hear unusual noises, or see changes that might be volcanically related to either the National Weather Service Office ( or American Samoa EOC in Pago Pago (684-699-3800). Questions for USGS HVO scientists can be sent to


Taʻū is a shield volcano with rift zones to the northeast and northwest. Ofu and Olosega are two islands formed from two shield volcanoes. In 1866, as a submarine eruption formed a cone between Taʻū and Ofu-Olosega islands. Vailuluʻu is a submarine volcano with a summit about 2000 feet (600 m) below the ocean surface. It is located about 25 miles (40 km) to the east of Taʻū island and has erupted multiple times over the past 50 years.

Volcanoes in American Samoa are similar to those in Hawaii. If activity escalates to an eruption, it will most likely include slow-moving lava flows or low-level explosions of lava that are localized to a small area. This can still be disruptive for residents of the Manuʻa islands.  A very large eruption like Hunga Tonga–Hunga Ha'apai in Tonga earlier this year is extremely unlikely as it is a different type of volcano. Volcanoes in Tonga erupt much more explosively than ones in American Samoa and Hawaii. 


It is unclear if this unrest will escalate to a volcanic eruption. An eruption could pose significant hazards to residents of American Samoa; these hazards include volcanic gases, low-level explosions of lava localized to a small area, lava flows, earthquake shaking, and tsunami.

Information about these hazards, which are similar to those in Hawaii, can be found at this HVO website:

A submarine volcanic eruption or landslide can generate a tsunami. The Pacific Tsunami Warning Center will issue a warning if they detect earthquake activity that is likely to cause a tsunami. However, volcanic eruptions do not usually generate large enough earthquakes to warrant a tsunami warning. If there is a tsunami from a nearby volcanic eruption, residents of the Manuʻa islands and elsewhere in American Samoa are more likely to experience natural warning signs before receiving an official tsunami warning.

If you are at the coast, heed the natural tsunami warning signs. If you feel a strong or long-duration earthquake, see a sudden rise or fall of the ocean, hear a loud roar from the ocean, or see a large aerial plume from an eruption, a tsunami may follow, and you should immediately move to higher ground.

Here is information on what you can do to protect yourself and your family if you see a tsunami or receive a warning:

Additional information will be provided as it becomes available.

More information

Tsunami information

How you can help scientists

Contact if you have information or observations to share, such as times and types of earthquake shaking, steaming ground, discolored or steaming water, unusual changes to the ground surface, ocean, or new large areas of dead vegetation or wildlife. These are most useful if you include time and location of the observation plus a photo or video with scale, if possible, that shows what you see. A person, boat, house, or tree can provide scale. Only take a photo or video if it is safe to do so.

Stay informed

The U.S. Geological Survey (USGS) Hawaiian Volcano Observatory will be sharing information about unrest in American Samoa via the USGS Volcano Notification Service (VNS) in addition to the existing website. This free service sends notices via email about volcanic activity in the US.

Subscribe to the VNS at For emails about American Samoa unrest, select Ofu-Olosega, Ta’u Island, and Tutuila Island from the list of available volcanoes. Alternatively, select “Hawaiian Volcano Observatory - Add All Volcanoes” from the list of available volcano observatories to receive notices about volcanoes in Hawaii and American Samoa.

For more information about the different types of VNS notifications, please see:

If you have questions, please contact:

Taʻū Island website:

Volcanoes in American Samoa website:

Subscribe to these messages:
Summary of volcanic hazards from eruptions:
Recent earthquakes in Hawaiʻi (map and list):
Explanation of Volcano Alert Levels and Aviation Color Codes:


The Hawaiian Volcano Observatory is one of five volcano observatories within the U.S. Geological Survey and is responsible for monitoring volcanoes and earthquakes in Hawaiʻi.

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