Samples of beach gravels were obtained from foreshore cusp deposits at
Portmore Beach, near Malin Head, Republic of Ireland. Axial dimension
s (A, B and C) were measured, and the maximum projection sphericity wa
s derived, for each of 4360 clasts. Each sample was also categorized a
ccording to depositional subenvironment. Principal components analysis
and cluster analysis were used to identify potential facies zonation.
Results indicate that reworking of the foreshore by incident and edge
waves resulted in clast size and shape segregation both parallel and
perpendicular to the beach. Patterns of zonation were distinctly diffe
rent from those described in earlier facies descriptions, showing a co
mplex set of foreshore facies. The distribution of these facies was co
ntrolled primarily by location within beach cusp systems. Primary and
secondary facies demonstrate alongshore variability of a magnitude com
parable to across shore differences. The results have important implic
ations for palaeoenvironmental reconstruction, morphosedimentary descr
iption and research sampling design, and provide the basis for a conce
ptual model of gravel beach cusp facies.