An earthquake measuring magnitude 4.8 has been detected near 17 km WSW of Lixoúri, Greece, occurring at 17:51 UTC on Saturday, September 12, 2026. Here is everything you need to know about what happened, what it means, and what to do.
The Basics
According to USGS data, this earthquake originated at a depth of 34.0 km beneath the surface. At a focal depth of 34.0 km, this is classified as a shallow earthquake (0–70 km). Shallow events are typically the most damaging: the seismic energy has less distance to travel before reaching the surface, resulting in stronger and more abrupt ground shaking at the epicentre.
A magnitude 4.8 earthquake is considered a moderate event. In practical terms, this means it is felt strongly by everyone; minor to moderate damage possible in vulnerable buildings.
Why Does This Area Get Earthquakes?
Greece and the broader Aegean region are among the most seismically active areas in Europe, positioned along the Hellenic Arc where the African Plate subducts beneath the Eurasian Plate.
Greece accounts for approximately 50% of all seismic energy released in Europe. The Ionian Islands, Crete, and the North Aegean are historically the most active zones, though significant earthquakes can and do occur across the entire country.
How Much Energy Is That, Really?
The magnitude scale can be deceptive to non-specialists because it looks like a simple number. In reality, it is logarithmic: each step up releases around 32 times more energy.
A magnitude 4.8 earthquake releases approximately approximately 30,000 tonnes of TNT — comparable to the Hiroshima atomic bomb of energy. For comparison, this exceeds the energy released by most conventional explosive events and is sufficient to shift tectonic stress in measurable ways across a wide region.
Moderate earthquakes are felt by virtually everyone near the epicentre. Strong shaking lasting 10–30 seconds can topple unsecured items, crack plaster, and cause poorly anchored objects to fall. Aftershocks are common following moderate events.
Should People Be Worried?
Significant damage can occur to vulnerable structures — particularly unreinforced masonry, old adobe buildings, and poorly maintained older construction. Well-engineered modern buildings are designed to withstand this level of shaking with minimal structural impact, though contents may shift and non-structural elements (ceilings, partitions) can be damaged.
Aftershocks are a normal part of the earthquake process and should be expected in the hours and days following any notable event. Most aftershocks are smaller than the main shock, but they can be significant — and structures weakened by the main event may be more vulnerable to subsequent shaking.
Staying Safe
Keep an earthquake emergency kit accessible at home. It should include at least 72 hours of water (4 litres per person per day), non-perishable food, a first aid kit, torch, battery-powered radio, copies of important documents, and essential medications. Reviewing and restocking this kit annually is strongly recommended.
Fasten heavy furniture — bookshelves, water heaters, cabinets — to walls using earthquake straps. Store breakable items on lower shelves and heavy items closest to the floor. These simple steps significantly reduce the risk of injury from falling objects.
The Greek Earthquake Planning and Protection Organisation (OASP/EPPO) provides guidance and resources for residents. Standard Drop, Cover, Hold On procedures apply, and coastal residents should move inland immediately after strong shaking.
For real-time updates on this earthquake and all seismic activity worldwide, visit our live earthquake map. You can also read our full earthquake safety guide for detailed preparedness advice.
Building Codes and Earthquake Resilience
One of the most effective tools against earthquake damage is modern building codes that specify how structures must be designed and constructed to withstand seismic forces. Countries with active fault zones have developed increasingly sophisticated seismic design standards over the past 50 years. However, the gap between modern code-compliant buildings and older existing structures remains a critical challenge in earthquake risk reduction worldwide. Building retrofit programmes and public awareness campaigns are key components of any national earthquake preparedness strategy.
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