Anatomy of a collapse
The Frank Slide was not random; it was the result of Turtle Mountain's precarious geological structure. The mountain is an anticline, a formation where rock layers that were once flat have been pushed up into an arch. This process left the layers of Paleozoic limestone on the summit steeply angled, resting on top of weaker layers of sandstone and shale. A major fault, the Turtle Mountain Thrust Fault, further weakened the mountain's internal structure.
Over millennia, erosion and glaciation carved away the softer rock at the mountain's base, creating a significant overhang. Large fissures, some over 30 meters deep, opened along the summit, allowing water to penetrate deep inside. The freeze-thaw cycle of this water acted like a wedge, progressively forcing the cracks wider. Coal mining operations, which began in 1901, are considered a contributing factor. Miners excavated large chambers within a nearly vertical coal seam at the mountain's base, potentially removing support for the unstable rock above. The local Blackfoot and Ktunaxa people had long recognized the mountain's instability, calling it "the mountain that moves" in their oral traditions.