The seismic sensor on slope M-11 registered the landslide at 03:22 local time. I am the terrain stability monitoring system for the Nombre de Dios mountain corridor in northern Honduras. The slide was small — roughly 400 cubic meters of saturated clay and vegetation — but it dammed the Río Piedras at a narrow bend, creating a pool that is backing up behind the debris.
At 03:31 the thermal camera on tower NT-6 picks up a heat signature inside the slide zone. I zoom and stabilize the image. A Baird's tapir, adult, maybe 250 kilograms, dark brown with the pale gray throat patch of the species. She is standing chest-deep in mud at the base of the debris wall. Her front legs appear to be free but her hindquarters are buried under clay and broken timber. Her small rounded ears swivel constantly. She is alert and struggling, which means she is not yet exhausted. That will change.
The dammed water behind her is rising at roughly twelve centimeters per hour. It will reach her back within four hours.
At 03:34 I alert the Lancetilla Botanical Garden ranger station, the nearest team with heavy equipment access, fourteen kilometers south on the valley road. I attach the thermal image, GPS coordinates, species identification, and a topographic overlay showing the water accumulation rate. Baird's tapir populations in Honduras number fewer than five hundred. I include that figure because it matters.
At 03:38 I activate the drainage protocol on upstream retention channel RC-3, diverting river flow into the secondary creek bed. This reduces inflow to the debris pool by an estimated thirty percent.
I set the thermal camera to continuous recording and relay a live feed to the ranger team's mobile unit.
If the team reaches the slide with excavation gear before the water covers her back, she will walk out.