Abstract. Remote sensing techniques can be used to gain a more detailed understanding
of hazardous rock slopes along railway corridors that would otherwise be
inaccessible. Multiple datasets can be used to identify changes over time,
creating an inventory of events to produce magnitude–frequency relationships
for rockfalls sourced on the slope. This study presents a method for using
the remotely sensed data to develop inputs to rockfall simulations, including
rockfall source locations and slope material parameters, which can be used to
determine the likelihood of a rockfall impacting the railway tracks given its
source zone location and volume. The results of the simulations can be
related to the rockfall inventory to develop modified magnitude–frequency
curves presenting a more realistic estimate of the hazard. These methods were
developed using the RockyFor3D software and lidar and photogrammetry data
collected over several years at White Canyon, British Columbia, Canada,
where the Canadian National (CN) Rail main line runs along the base of the slope. Rockfalls
sourced closer to the tracks were more likely to be deposited on the track or
in the ditch, and of these, rockfalls between 0.1 and 10 m3 were
the most likely to be deposited. Smaller blocks did not travel far enough to
reach the bottom of the slope and larger blocks were deposited past the
tracks. Applying the results of the simulations to a database of over 2000
rockfall events, a modified magnitude–frequency can be created, allowing the
frequency of rockfalls deposited on the railway tracks or in ditches to be
determined. Suggestions are made for future development of the methods
including refinement of input parameters and extension to other modelling
packages.