The seismic doublet that struck Venezuela on June 24, 2026, involved two powerful earthquakes occurring in rapid succession, with magnitudes of 7.2 and 7.5 Mw. This phenomenon, characterized by similar magnitudes and close timing, resulted in significant destruction due to its shallow depth and the geological context of the region. Experts suggest that the first quake likely triggered the second, illustrating the complex interactions of tectonic plates in this seismically active area.