- The document discusses the impacts of basaltic lava flows on the Owyhee River in Oregon, including morphological, hydrological, ecological, and regional landscape effects. - When lava flows entered the river canyon, it disrupted normal fluvial processes, blocking and diverting the river, forming lava dams and lakes. This thwarted the river's erosion and lowered the landscape more slowly. - Examples from the Owyhee River include the Saddle Butte and West Crater lava dams that formed lakes and deposited thick lacustrine sediments, demonstrating the long-term hydrological changes caused by intra-canyon volcanism.