On May 29, 2008, the area near Selfoss, Iceland, was shaken by a doublet earthquake that registered a combined magnitude of 6.1. This geological event was characterized by two significant shocks that were felt across the region, leading to injuries for at least 30 people. The tremors caused local authorities to activate emergency services and initiate response protocols to assist those affected. In addition to the injuries reported, the quakes inflicted structural damages on local buildings, prompting inspections and repairs in the days that followed.

Selfoss, located in the south of Iceland, is situated close to the Mid-Atlantic Ridge, a seismic hotspot due to the separation of the North American and Eurasian tectonic plates. This geological setting makes Iceland particularly susceptible to earthquakes, as well as volcanic eruptions. Following the quakes, scientists increased their monitoring of seismic activity in the region, eager to assess potential aftershocks or further geological instability. The earthquakes were among the notable seismic events of 2008, highlighting the dynamic nature of the Icelandic landscape.

Residents expressed their fears and experiences across various media outlets, recounting the sensation of the ground shaking and the immediate scramble for safety during the tremors. Many reported the psychological impact of the quakes, citing increased anxiety in the days following. The Icelandic government launched initiatives to support those affected and to raise awareness about earthquake preparedness among the population, emphasizing the importance of having safety measures in place given the country's geological conditions.