The 2008 Scania earthquake was the strongest recorded seismic event in one of Europe's least seismically active regions in modern history.
Key Facts
- Moment Magnitude
- 4.2–4.3 Mw
- Epicenter distance from Malmö
- 60 km east km
- Epicenter distance from Sjöbo
- 5 km southwest km
- Time of occurrence
- 06:20 CET (05:20 UTC)
- Earthquakes in region since 1375
- 14 recorded events
- Prior quakes detected 1970–2008
- 3 (each below 2.8 magnitude)
By the Numbers
Location
Cause → Event → Consequence
The Skåne region of southern Sweden is characterized by extremely low seismic activity, with only three minor earthquakes detected between 1970 and 2008 and only 14 events on record since 1375. The geological conditions that produced this earthquake were not elaborated upon in available sources, but the region's infrequent seismicity made the event notable.
On 16 December 2008 at 06:20 CET, an earthquake measuring 4.2–4.3 Mw struck approximately 5 km southwest of Sjöbo and 60 km east of Malmö in Scania, southern Sweden. Strong shaking was felt across a wide area spanning Skåne to Östergötland in Sweden, into eastern Denmark, and as far as northern Poland.
Roadways in both Sweden and Denmark were reported to have sustained cracks following the earthquake, though investigations could not confirm a direct causal link to the seismic event. No casualties were reported in available sources. The event drew attention to the rare occurrence of significant seismic activity in this otherwise geologically quiet corner of northern Europe.