In brief
A 5.2‑scale earthquake hit a region 200 km north‑west of Port‑Ølry, Vanuatu, at 2242 GMT Saturday. The U.S. Geological Survey identified a shallow 10‑km depth and specific coordinates for the epicenter, and no harm was reported. The event underscores the seismic vigilance required in the region, though details on any aftershocks remain pending.
A 5.2‑magnitude earthquake struck an area 200 km northwest of Port‑Ølry, Vanuatu, on Saturday, at 2242 GMT, the U.S. Geological Survey reported in a statement released by Xinhua News Agency.
The U.S. Geological Survey said the quake’s epicenter was located at a depth of 10 km, initially determined to be at 13.87 degrees south latitude and 165.65 degrees east longitude.
Xinhua’s news release, published by the state‑run agency on 2026‑11‑01, noted that the seismic event produced no injuries or damage in the area where it occurred.
According to the U.S. Geological Survey, the magnitude was measured on the Richter scale, a common method for quantifying the energy released by an earthquake.
The agency’s bulletin also detailed the precise geographic coordinates of the epicenter, allowing seismologists and local authorities to understand the spatial context of the shaking.
Port‑Ølry, a location in Vanuatu, was mentioned as a reference point – the quake occurred roughly 200 km to its northwest, placing it off the main populated coastlines of the island nation.
Xinhua’s report stated that the U.S. Geological Survey’s assessment of the depth at 10 km indicated a shallow seismic source within the upper crust of the earth.
Shallow earthquakes, while limited in depth, can often cause stronger ground motion at the surface compared to deeper events of the same magnitude.
Despite the potential for stronger shaking, the area impacted by this 5.2‑magnitude event saw no reports of structural damage or human casualties.
The U.S. Geological Survey, the federal agency responsible for monitoring seismic activity worldwide, identified the event as a localized tectonic disturbance within the region.
U.S. Geological Survey officials also noted that the event’s impact assessment was based on contemporary seismic networks and instruments recording the tremor’s characteristics.
Because the news release cites only the U.S. Geological Survey’s initial determinations, details regarding any aftershocks, tremor duration, or potential long‑term effects remain unreported in the available source materials.