The seismic doublet that struck Venezuela on June 24, 2026, involved two powerful earthquakes occurring in rapid succession, leading to unprecedented destruction. With magnitudes of 7.2 and 7.5, these quakes were closely linked, triggering each other due to changes in stress on nearby faults. The shallow depth and proximity of the epicenters contributed significantly to the severity of the disaster, marking it as one of the most significant seismic events in the region's history.