Moderate mag. 5.7 earthquake - Coral Sea, 80 km southeast of Lata, Solomon Islands, on Monday, Dec 5, 2022 at 4:35 pm (GMT +11) -

A magnitude 5.7 earthquake near Lata, Santa Cruz Islands, Temotu Province, Solomon Islands, was reported only 16 minutes ago by the German Research Centre for Geosciences (GFZ), considered one of the key international agencies that monitor seismic activity worldwide. The earthquake occurred at an intermediate depth of 102 km beneath the epicenter in the afternoon on Monday, December 5th, 2022, at 4:35 pm local time. The exact magnitude, epicenter, and depth of the quake might be revised within the next few hours or minutes as seismologists review data and refine their calculations, or as other agencies issue their report.
Our monitoring service identified a second report from France's Réseau National de Surveillance Sismique (RéNaSS) which listed the quake at magnitude 5.6. Other agencies reporting the same quake include the citizen-seismograph network of RaspberryShake at magnitude 5.7, and the European-Mediterranean Seismological Centre (EMSC) at magnitude 5.6.
Based on the preliminary seismic data, the quake should not have caused any significant damage, but was probably felt by many people as light vibration in the area of the epicenter.
Weak shaking might have been felt in Lata (pop. 550) located 79 km from the epicenter.
VolcanoDiscovery will automatically update magnitude and depth if these change and follow up if other significant news about the quake become available. If you're in the area, please send us your experience through our reporting mechanism, either online or via our mobile app. This will help us provide more first-hand updates to anyone around the globe who wants to know more about this quake.

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Based on its magnitude, the fault that was active during the quake ruptured along a surface of approx. 50 km² (=19 sqare miles) as a first-order estimate. The length of the rupture zone thus was probably around 12 km (8 mi).
Aftershocks typically occur during the days and weeks following the quake at or near the same fault, at distances of up to approx. two times the length of the rupture zone.
The often broadly linear arrangement of aftershock epicenters encompasses the rupture zone of the main shock (check on the map below to verify).

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