A strong earthquake registered by the Icelandic Met Office (IMO) as M5.2 hit 4.9 km (3 miles) NE of the city of Grindavik at 10:25 UTC on March 12, 2020. The quake struck at a depth of 6.1 km (3.8 miles) and was felt in large areas of SW-Iceland.
More than 400 aftershocks followed through the rest of the day and into March 13, with magnitudes up to 3.4.
This is the largest earthquake detected on the Reykjanes peninsula since October 2013 when an earthquake of M5.2 occurred close to Reykjanestá.
It occurred in the northernmost part of the area associated with Mt. Thorbjorn land uplift.
"Although the land crisis actually ended in mid-February and earthquake activity decreased, there has nevertheless been enough tension in the area to cause this earthquake," said Kristín Jónsdóttir, group director of nature conservation at the Icelandic Meteorological Office.
"This was a tremendous tremor," said Hilmar Bragi Bárðarson, photographer for the local news website Víkurfréttir who was at home in Reykjanesbær when the large earthquake hit.
"I live on the fourth floor of a [five-story] apartment building, and the building swung, like you’d see in an American movie. It lasted a few seconds, but it felt like it would never end."
Uplift at Mt. Thorbjorn volcano is no longer being observed, which is likely due to the halt of magma inflow, IMO stated.
However, the uncertainty phase that the Civil Protections declared is still in force.
The earthquake swarm northeast of Grindavík is still ongoing but the activity has decreased since yesterday evening, the IMO reported at 09:30 UTC today.
The city of Grindavik and MT. Thorbjorn, Iceland. Image credit: Copernicus EU/Sentinel-2 (acquired February 22, 2020). Edit: TW
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March 20, 2020
"We evaluated the earthquake on March 12 to be M5.2, but now we have reassessed its magnitude at M4.6," Kristín Jónsdóttir, head of the Natural Hazard Monitoring Group at the Icelandic Met Office, said March 19.
"It can be complicated to estimate the size of larger earthquakes, but now several of us have studied the event and this is the result. This is partly because of strong wave reflections in the crust in Reykjanes Peninsula that complicate the data processing.
Featured image: The city of Grindavik and MT. Thorbjorn, Iceland. Image credit: Copernicus EU/Sentinel-2 (acquired February 22, 2020). Edit: TW
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