The Andalusian region has been the scene of numerous telluric movements throughout the centuries, some of them with catastrophic consequences. These events have not only transformed the landscape but have also forged the identity of its communities, which have learned to coexist with seismic activity.

One of the most significant episodes was the great Lisbon earthquake of November 1, 1755. This tremor, originating in the Atlantic, generated a devastating tsunami that violently struck the coasts of Huelva and Cádiz. In the capital of Cádiz, popular tradition recounts the intervention of the Virgen de la Palma to contain the waters, an event that spurred the birth of modern seismology and the creation of new settlements like Isla Cristina.

The province of Granada has historically been one of the areas most affected by seismic activity. The Arenas del Rey earthquake in 1884 is remembered as one of the most tragic, with approximately 900 fatalities. Decades later, on April 20, 1956, the towns of Albolote and Atarfe suffered a new earthquake that left twelve dead and hundreds injured, deeply affecting a generation of Granadans.

The seismic chronology of Andalusia is extensive, with records of significant tremors such as that of April 11, 1431, which destroyed Atarfe, that of Carmona on April 5, 1504, with 32 victims, or that of Almería on November 9, 1518, which caused 165 deaths and the destruction of Vera. More recently, on February 28, 1969, a 7.8-magnitude earthquake with an epicenter off Cape St. Vincent was strongly felt throughout the region, causing collapses and fatalities in Huelva.

These historical events underscore the importance of preparation and awareness in an area with geological activity. Knowing the past allows for the design of a safer future, where architecture and civil protection work to mitigate risks and protect the population. Resilience and solidarity among Andalusian provinces are key to facing the unpredictability of nature.