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January 31, 2022

The U.S. Geological Survey's Hawaiian Volcano Observatory (HVO) recorded a magnitude-4.0 earthquake located under the south part of the Island of Hawai‘i on Monday, January 31, at 1:55 a.m., HST.

HAWAIIAN VOLCANO OBSERVATORY INFORMATION STATEMENT

U.S. Geological Survey

Monday, January 31, 2022, 3:01 AM HST (Monday, January 31, 2022, 13:01 UTC)



HAWAIIAN VOLCANO OBSERVATORY INFORMATION STATEMENT



The U.S. Geological Survey's Hawaiian Volcano Observatory (HVO) recorded a magnitude-4.0 earthquake located under the south part of the Island of Hawai‘i on Monday, January 31, at 1:55 a.m., HST.



The earthquake was centered about 8 km (5 miles) east-northeast of Pāhala, at a depth of 32 km (20 miles). A map showing its location is posted on the HVO website at http://volcanoes.usgs.gov/hvo/earthquakes/. More details are available at the National Earthquake Information Center website at https://earthquake.usgs.gov/earthquakes/eventpage/hv72897042/.



Light shaking, with maximum Intensity of IV on the Modified Mercalli Intensity Scale, has been reported across parts of the Island of Hawai‘i. At that intensity, significant damage to buildings or structures is not expected. The USGS "Did you feel it?" service (http://earthquake.usgs.gov/dyfi/) received 48 felt reports within the first hour of the earthquake.



According to HVO seismologist Jefferson Chang, “This earthquake appears to be part of the seismic swarm under the Pāhala area, which has been going on for over a year. Out of over ten thousand earthquakes that were detected in the area over the past year, four have been magnitude-4 or greater.” HVO Scientist-in-Charge Ken Hon said, “The earthquake had no apparent effect on Kīlauea or Mauna Loa volcanoes. The eruption in Halema‘uma‘u at Kīlauea summit resumed yesterday evening and we do not see any detectable changes in that eruption as a result of these earthquakes.” HVO continues to monitor Hawaiian volcanoes for any changes.



Earthquakes beneath Kīlauea's lower Southwest Rift Zone are produced mostly at depths of 25-40 km (15-25 mi), beneath the town of Pāhala and extending about 10 km (6 mi) offshore. Earthquakes in this region have been observed at least as far back as the 1960s and are posited to be related to deep magma pathways under the island. For more information, see the “Volcano Watch” article, “Why do so many deep earthquakes happen around Pāhala?”: https://www.usgs.gov/news/volcano-watch-why-do-so-many-deep-earthquakes-happen-around-pahala.



For information on recent earthquakes in Hawaii and eruption updates, visit the USGS Hawaiian Volcano Observatory website https://www.usgs.gov/observatories/hvo.



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Subscribe to these messages: https://volcanoes.usgs.gov/vns2/



Summary of volcanic hazards from eruptions: https://www.usgs.gov/observatories/hvo/hazards



Recent earthquakes in Hawaiʻi (map and list): https://www.usgs.gov/observatories/hvo



Explanation of Volcano Alert Levels and Aviation Color Codes: https://www.usgs.gov/programs/VHP/volcanic-alert-levels-characterize-conditions-us-volcanoes



CONTACT INFORMATION:



askHVO@usgs.gov



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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