Using Interferometric Synthetic Aperture Radar, we observe subsidence following the tunnel’s construction, which can be explained by significant water leakage encountered during the work. Three years later, an earthquake swarm occurred about 3 km from the tunnel, in an area without previous swarm activity. We build a catalog of the swarm and through analysis of its spatio‐temporal distribution propose that changes in pore pressure and stress, potentially linked to the leakage, may have played a role in triggering the swarm. Fault valving or pumping are possible mechanisms to explain the cascading nature of the earthquakes in the swarm.

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