The coastal environment is home to a range of landforms and landscapes that
include those at either end of the sensitivity scale. The soft coastal lan
dscapes of beaches, sand dunes, and mudflats represent fast-responding and
mobile geomorphic systems that are highly sensitive to environmental change
. On the other hand, coastal landscapes in areas of hard rock and inherited
Quaternary deposits represent relatively slow-responding systems that are,
in the main, thought to be relatively insensitive to change. This paper fo
cuses upon both groups of systems and demonstrates not only how soft coasts
respond to environmental stimuli over a variety of time scales bur also ho
w this inheritance shapes subsequent development. Using mainly Scottish sof
t coast examples, the changes associated with sensitive coastal landscapes
are assessed in terms of the past timing and magnitude of changes in both s
ea level and sediment economy. Declining abundance of coastal sediment has
initiated a process of internal re-organisation that, because of an inheren
t sensitivity to sea level change and low thresholds for the forcing of cha
nge, fundamentally restricts future management options. The paper also atte
mpts to show that hard rock coasts are also responsive to particular types
of event on short time scales and examples are discussed that modify the ac
cepted view of hard rock insensitivity to environmental change. (C) 2001 El
sevier Science B.V. All rights reserved.