Assessment of hazard of erosion of shoreline bluffs requires an unders
tanding of the natural processes and human use in these high risk area
s. As an important component associated with erosion and natural evolu
tion of bluff shorelines, alongshore sediment transport is an essentia
l process in defining the hazard associated with bluff erosion. The ob
jective of this study is the integration of an understanding of alongs
hore sediment transport into a proposed management framework for cohes
ive bluff shorelines. A study of a ten kilometre area along the southe
astern Lake Huron shoreline, at the cottage community of Horizon View,
north of Goderich, Ontario examines the natural and human components
which have led to the development of bluff erosion hazards. Although d
ominant sediment transport is north to south alongshore, the pattern o
f wave refraction during south and southwest waves, suggests frequent
northward transport of material from the 30 meter high bluffs at the s
ite. Examination of beach sediments and bluff conditions support this
finding and indicate long term sediment supply and bluff instability.
Planning of future development at this location must appreciate the po
tential for continued bluff erosion and the study results suggest that
when combined with other factors such as wave energy, bluff morpholog
y, groundwater conditions, vegetation cover, land uses and impacts of
fluctuating lake levels, studies of alongshore sediment transport can
be a useful tool to assist in management of cohesive coastlines and un
derstanding the natural hazard of bluff erosion in developed coastal a
reas. A management framework for cohesive bluffs attempts to integrate
an understanding of natural processes with human uses and land use po
licies in order to identify, assess and select a preferred management
option reflecting this understanding.