The 2014 Oso landslide was the deadliest landslide in continental U.S. history.
The landslide occurred within an ~ 200 m-high hillslope of unconsolidated deposits.
Field reconnaissance revealed landslide zones with distinct geomorphic expression.
Observed landslide morphology provided insight into the failure as a multi-stage event.
LiDAR shaded relief images show striking evidence of multiple past landslides in the vicinity.