The potential interconnections between human settlement systems, subsistence practices, and rapid, high-magnitude transformation of the physical landscape (e.g., earthquakes, volcanic eruptions, and landslides) is an important issue of discussion in archaeology. This paper critically examines the argument that prehistoric abandonment of Classic Lillooet pithouse villages of south-central British Columbia, Canada, at approximately 1200-1000 B.P., was linked to one or more catastrophic landslides at Texas Creek that blocked the Fraser River, destroyed salmon resources, and caused the abandonment of this area. Examination of the location and depositional condition of several excavated archaeological sites within the Fraser Valley, as well as reflection on the expected environmental and cultural responses to a catastrophic landslide, challenge previous interpretations of the existence, location, and magnitude of such a landslide event, and indicate that archaeologists need to reconsider deterministic environmental explanations for the abandonment of pithouse villages in the interior of British Columbia.