image: Larry Bane Bay, with vertical cliffs exposing members from the Boheeshane Chalk to the Ballintoy Chalk; higher members of the Ulster White Limestone Formation are exposed landward of the prominent fault plane.
Larry Bane Bay, with vertical cliffs exposing members from the Boheeshane Chalk to the Ballintoy Chalk; higher members of the Ulster White Limestone Formation are exposed landward of the prominent fault plane.
 
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