This paleogeogrphical map suggests that in the Cambrian sediment accumulation in the vicinity of Ireland are part of the sedimentary fill that collected on a trailing margin that was part of the continental terrain that flanked the northern margin of Gondwana and later became Avalonia (after Chris Scotese).

Diagrams and maps of Paleozoic Geology of Hook Head, Co. Wexford, Ireland / ScoteseCamb Assembled by Chris Kendall after Blakey and Scotese 3/2/2006 Click on Galleries to return to USC Sequence Stratigraphy photo galleries or on USC Sequence Stratigraphy for Strata home page kendall@sc.edu