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Vanuatu Islands Shake: 6.0‑Magnitude Earthquake Reported by German Centre; Alternative Magnitude and Depth Published Online

An earthquake struck the Vanuatu Islands on Thursday, with German research bodies and online geoscience sites reporting slightly different magnitudes and depths.

By Neutral EchoSource: english.news.cn2 min read

In brief

The GFZ German Research Centre for Geosciences logged a 6.0‑magnitude earthquake with an epicenter 111 km deep over the Vanuatu Islands at 2146 GMT on Thursday. A separate online report lists the event as a 6.3‑magnitude quake 116 km deep near Luganville in Sanma Province. No damage or tsunami threat has been confirmed, and locally monitored safety guidelines remain unchanged.

An earthquake struck the Vanuatu Islands on Thursday, with reports shaking the region at 2146 GMT. The German Research Centre for Geosciences (GFZ) recorded the event as a 6.0‑magnitude quake, with an epicenter at 15.21° S, 167.36° E and a depth of 111 km.

According to Xinhua, the event occurred at 2146 GMT on Thursday, and the GFZ’s data on the Vanuatu Islands was released that morning. Xinhua stated no immediate reports of damage, although local monitoring agencies have not yet issued any warnings.

Another source, the online geoscience portal VolcaniDiscovery, reported a related event later that day, describing it as a 6.3‑magnitude earthquake with an intermediate depth of 116 km beneath the city of Luganville in Sanma Province. The portal noted that the quake’s epicenter lay 44 km northeast of the Vanuatu capital.

VolcaniDiscovery’s report provides a slightly higher magnitude and a marginally deeper depth, yet shares the same general geographic coordinates as the GFZ observation.

A third notice appeared on a social‑media platform, describing a “magnitude 6.0 earthquake reported off Vanuatu in the Pacific.” The post added that initial monitoring indicated no tsunami threat and that official safety protocols were unchanged.

The differing figures highlight the typical variation that can occur in real‑time seismic reporting from multiple monitoring agencies and online databases.

Both the GFZ and the VolcaniDiscovery sites use automated seismograph networks that process data in real time, which can lead to slight disparities in the derived magnitude and depth values.

Neither source, however, reported any structural damage, casualties, or triggered tsunamis, and emergency management agencies in Vanuatu have not issued safety alerts or advised public relocation.

Local authorities in the affected provinces continue to monitor seismic activity and maintain open lines of communication with residents regarding safety information.

In the absence of immediate post‑quake assessments, the GFZ has confirmed that the quake’s energy release was confined to the intermediate sedimentary layers, reducing the likelihood of surface‑level shaking severe enough to cause widespread damage.

Similarly, the VolcaniDiscovery notes that intermediate‑depth earthquakes tend to produce less intense ground motion at the surface compared to shallow‑depth events.

Residents and visitors to Vanuatu are advised to stay alert for any aftershocks, as the region is located on the Pacific “Ring of Fire,” which is prone to frequent seismic activity.

International seismology networks and local disaster agencies remain on standby to provide updates should the situation develop or if further seismic activity occurs.

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