The Late Cretaceous deposits in the railway cut at Hockai (Hautes Fagnes, NE Belgium) consist of an Early Campanian basal conglomerate, overlain by glauconitic sand and residual loam with black, cavernous flint of Late Campanian age, and a residual sandy loam with grey flint of Late Maastrichtian age. Early Maastrichtian deposits seem to be absent. Moreover, future study should determine whether of not a lithostratigraphic equivalent of the Santonian Aachen Formation occurs in this section.
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