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Over-lain by a red bed of the Gercus Fm, the Beciraman represents a marine offlap corresponding to continental beds related to extensive uplifts to the north and east.
The sand percentage within the Agbada Formation varies from 30 to 70%, which results from the large number of depositional offlap cycles.
Drag is also increased significantly by whorl offlap (Chamberlain, 1976).
This drop in sea level within Hudson Bay and James Bay will lead to an offlap of water and an outward migration of shorelines.