文摘
This study aims to examine the temporal pattern of shoreline changes as indication of geomorphic phases. Selected individual transects from the compartmentalised sections of the St Ives and Padstow systems were shortlisted for examination. Here, four phases of geomorphic response were specifically identified in the St Ives/Hayle system and three phases in the Padstow/Camel system. Despite the exposure of the systems to the same regional climatic and environmental conditions, they responded differently over the historical time-scale. The only constant response in all the estuaries is landward recession of the low water shoreline. The lack of temporal conformity to changes across all the coastal systems, where rates and directions of change occur at different periods throughout the history considered, confirmed that other factors beyond climate change or climate forcing are responsible for site-specific response, adjustment and behaviour. These other factors are structural, such as the shape and orientation of the bedrock valley and embayment, or anthropogenic, such as the construction of training walls and establishment of some sections of the systems as Sites of Specific Scientific Interests (SSSIs).