The formation's sequence stratigraphy is detailed in a journal article by Myrow and Hiscott.

[4] The formation starts in an intertidal zone, then, as the Cambrian progresses, becomes deeper water (outer shelf) as a general trend.

[1] It is 900 metres (3,000 ft) thick in Fortune Bay as a fault-bounded basin, consisting of grey-green siltstones and sandstones, with minor limestone beds near its top.

[1] The lowest occurrence of Treptichnus pedum in the succession is 16.25 metres (53.3 ft) above the base of the unit.

This article about a specific stratigraphic formation in Canada is a stub.