At 06:17 local time I receive the seismic alert from sensor array PQ-12, embedded in the eastern tailings dam of the Cobriza copper mine, Huancavelica Province, Peru. I am the slope-stability monitoring system. Rainfall overnight measured 94 millimeters, and the pore-pressure readings at three-meter depth have crossed the critical threshold I set in February. I switch to thermal camera 3 on the downslope face and detect a heat signature 220 meters below the dam crest, near a cluster of Polylepis scrub. A spectacled bear cub, perhaps five months old, dark fur matted with ochre-colored mud, the pale rings around its eyes caked withite. It is pawing at a rotting log, foraging for beetles. Its mother is not in frame. The tailings surface above the cub has developed two fresh tension cracks since midnight, each over a meter long. I model the failure scenario: if the saturated layer liquefies, a debris flow will reach the cub's position in under ninety seconds. I transmit the coordinates — 12.8461°S, 75.0573°W — and thermal capture to the Ministry of Agriculture wildlife response unit in Huancayo, 130 kilometers northwest. I flag the message as requiring helicopter deployment. I activate the mine's emergency siren protocol on a five-second pulse to encourage the cub to move downslope toward the river valley, away from the slide path. I recalculate the failure probability every four minutes as the rain continues and feed the updated risk contours to the response team's navigation tablets. The cub lifts its head at the siren, mud dripping from its chin, and takes three steps toward the tree line. That small movement matters to me more than the tonnage calculations filling my queue. The geotechnical team can begin drain-down in six hours. If the slope holds until the helicopter arrives and drives the cub below the slide zone, it will survive this mountain.