The standard narrative also tends to overlook the slide’s geologically significant aftermath. Within weeks, geologists produced a detailed report, but later research has substantially revised their conclusions as regional geology became better understood and the fields of geological engineering and rock mechanics advanced. Modern laboratory studies and numerical modeling confirm that Turtle Mountain was highly unstable prior to the event. In recent decades, extensive field instrumentation and monitoring have been implemented to assess ongoing risks. Today, the Frank Slide area is both a tourist destination and home to thousands of residents. Although the disaster has passed from living memory, awareness of the mountain’s continuing instability remains central to those who live near it and study its behavior.