A spectacular outcrop of the Lower Miocene Inamura subaqueous landslide deposit at Kamiichi-machi, Toyama Prefecture, central Japan

Aerial video of the Inamura (稲村) outcrop and surrounding landscape. The lower Miocene Orido tuff member is exposed at the outcrop, which expands generally southward. Some of the alternating beds are thought to have slid along the seafloor at the time, dipping from north to south, independent of the present strike and dip direction. In this video, Toyama (富山) Plain, Toyama Bay and Noto (能登) Peninsula are seen from a distance in the northwest, with Hayatsuki (早月) River in the northeast.