The Verulam Formation belongs to the
Simcoe Group in South-central Ontario and to the
Trenton Group in
Southwestern Ontario. Within the Simcoe Group, it overlies the
Bobcaygeon Formation. Both the Bobcaygeon and Verulam Formations are composed of bioclastic
wackestones,
grainstones, and
packstones interbedded with
calcareous shales and
siltstones. The Verulam contains more shale than the underlying Bobcaygeon Formation. Several
hardgrounds have been documented in detail from the upper Bobcaygeon and lower Verulam. The paleoenvironments in which the Bobcaygeon and Verulam Formations were deposited have been interpreted as a proximal carbonate shelf that ranged in depth and proximity from
shoal to shallow shelf in the Bobcaygeon and from deep shelf to shoal or shallow shelf in the Verulam Formation. == Fossil content ==