Founding Members

The founding members of the Niagara Peninsula Joint Committee On Higher Education. The two men on the right are Ivan Buchanan and Fred Campbell. The Committee later grew into the Board of Governors which was then renamed the Board of Trustees.

Founding Figures

Pictured here from left to right are: Premier John Robarts, Mrs. Grover Egertor of the Allanburg Women's Institute, the woman who first came up with the idea of forming a University in the Niagara Region, Mrs. Bearss, the former chairwoman of the Women's Institute when the project was proposed, and Dr. Arthur A. Schmon, chairman of the Founder's Committee. This photo was taken at a dinner in Niagara Falls in 1963 that marked the official launch of the Brock University Project.

Founding Plaque Programme

A programme for the 1969 ceremony unveiling the Founding Plaque.

Founding Plaque Unveiling

The plaque commemorating the history of Brock is unveiled outside Thistle Complex.

Founding Plaque Unveiling

Dr. Gibson speaks during the unveiling of a historical plaque at Brock.

Founding Plaque Unveiling

Pictured here from left to right are: Dr. Gibson, President of Brock University; James N. Allen, Chairman of the Niagara Parks Commision; MacKenzie Chown, Mayor; and Prof J. M. S. Careless co-chairman of the provinces archaelogical and historic sites board and professor at U of T.

Shell Christening

Members of the Brock University Rowing Club and their new $3000 shell, named Cete, meaning a group of Badgers. Tony Biernacki is pictured here pouring pond water onto the shell in a mock christening.

Sedimentology and taphonomy of storm-generated shell beds from the Verulam formation (Ordovician), Lakefield and Gamebridge quarries, Southern Ontario, Canada /

The Verulam Formation (Middle Ordovician) at the Lakefield Quarry and Gamebridge Quarry, southern Ontario, is comprised of five main lithofacies. These include shoal deposits consisting of Lithofacies 1, winnowed crinoidal grainstones and, shelf deposits consisting of: Lithofacies 2, wackestones, packstones, grainstones, and rudstones; Lithofacies 3, laminated calcisiltites; Lithofacies 4, nodular wackestones and mudstones; and, Lithofacies 5, laminated mudstones and shales. The distribution of the lithofacies was influenced by variations in storm frequency and intensity during a relative sea level fall. Predominant convex-up attitudes of concavo-convex shells within shell beds suggest syndepositional reworking during storm events. The bimodal orientations of shell axes on the upper surfaces of the shell beds indicates deposition under wave-generated currents. The sedimentary features and shell orientations indicate that the shell beds were deposited during storm events and not by the gradual accumulation of shelly material. Cluster and principal component analysis of relative abundance data of the taxa in the shell beds, interbedded nodular wackestones and mudstones, and laminated mudstones and shales, indicates one biofacies comprised of three main assemblages: a strophomenid (Sowerbyelladominated) assemblage, a transitional mixed strophomenid-atrypid assemblage and an atrypid (Zygospira-dominatQd) assemblage. The occurrence of the strophomenid, the strophomenid-atrypid and atrypid assemblages were controlled by storm-driven allogenic taphonomic feedback.