Province of Upper Canada Grant to the Honorable Peter Russell of the Township of Newark

Province of Upper Canada Grant to the Honorable Peter Russell of the Township of Newark. He is granted 150 acres in the Town of Newark in the County of Lincoln. This is registered in Liber B, folio 133. This was entered in the auditor’s office July 26, 1796. This document is held together with tape. The text is not affected, July 2, 1796.

Province of Upper Canada Grant (paper mounted on canvas) to the Honorable Peter Russell of the Township of Newark

Province of Upper Canada Grant (paper mounted on canvas) to the Honorable Peter Russell of the Township of Newark. He is granted 10 acres in the Township of Newark in the County of Lincoln. This document is mounted on canvas. This was entered in the auditor’s office Sept.29, 1797. Part of the paper document is missing but this does not affect the text, Sept. 1, 1797.

Province of Upper Canada Grant (vellum) to Joseph Mills of the township of Grimsby

Province of Upper Canada Grant (vellum) to Joseph Mills of the township of Grimsby, son of United Empire Loyalist John Mills, United Empire Loyalist. He was granted 200 acres in the 5th Concession in Windham in the County of Norfolk. This was registered in in Liber L, folio 387 on Feb. 14, 1803. The crown land seal is attached, but broken into small pieces, Nov. 25, 1802.

Province of Upper Canada Grant (vellum) to Christian Myers of the Township of Cornwall

Province of Upper Canada Grant (vellum) to Christian Myers of the Township of Cornwall, son of Michael Myers, United Empire Loyalist. He is granted 200 acres on Lot no. 18 in the 9th Concession in the Township of Mountain in the County of Dundas. This document is faded and part of the paper are missing or stained. Some of the text is affected. A small piece is missing from the crown land seal which is also faded. This was registered in Feb. 1803, Dec. 1, 1802

Province of Upper Canada Grant (vellum) to Peter McCollum of the Township of Grimsby

Province of Upper Canada Grant (vellum) to Peter McCollum of the Township of Grimsby, son of James McCollum, United Empire Loyalist. He was granted 200 acres in Lot no.12 in the 5th Concession in the Township of Scott in the County of Yorke. This was entered with the auditor on Nov. 17, 1809. There is a partial crown land seal attached to this document but it is broken, Nov. 16, 1809.

Province of Upper Canada Grant (vellum) to Thomas Fraser of the Township of Edwardsburgh granted 1 acre in Lot no.9 in the County of Stormont

Province of Upper Canada Grant (vellum) to Thomas Fraser of the Township of Edwardsburgh granted 1 acre in Lot no.9 in the County of Stormont. Signed by William Jarvis, Sir Isaac Brock, Prideaux Selby and John Macdonell. There are some holes in the document and there are small pieces missing on the right hand side. William Jarvis was the Provincial Secretary of the Lt. Governor of Upper Canada; Sir Isaac Brock. Jarvis was an officer in the Queen’s Rangers. He also served as Provincial Secretary of Upper Canada. A partial crown seal is attached, Mar. 26, 1812.

The Thorold Post, Thorold, Ontario, July 30, 1927

The Thorold Post, Thorold, Ontario, July 30, 1927.

The Thorold Post, Thorold, Ontario, June 30, 1927

The Thorold Post, Thorold, Ontario. This is a supplement to the paper commemorating the Canada’s Diamond Jubilee 1867-1927. The front page of the supplement is coloured, June 30, 1927.

1964-65 Board of Governors

The 1964-65 Board of Governors. Pictured here are those who attended the first meeting on December 8, 1964. From left to right - Front Row: E. E. Mitchelson, Niagara Falls. Mrs. J. J. Bench, St. Catharines. W. B. Gunning, Chippawa. Dr. J. A. Gibson, St. Catharines. D. G. Willmot, St. Catharines. J. M. Trott, Welland. C. B. Hill, St. Catharines. A. C. Rae, Fonthill. Back Row: E. S. Howard, Fort Erie. W. J. Freeman, Port Colborne. M. L. Swart, Thorold. C. F. Anderson, Port Colborne. W. S. Martin, Queenston. E. R. Davey, Niagara Falls. R. L. Hearn, Queenston. C. W. Morehead, Welland. S. J. Leishman, Thorold. F. H. Leslie, Chippawa. F. C. Cullimore, Chippawa. W. B. C. Burgoyne, St. Catharines. H. C. Blenkhorn, St. Catharines. M. A. Chown, St. Catharines. B. P. R. Newman, St. Catharines. R. S. Misener, St. Catharines. Missing: R. M. Schmon, Niagara on the Lake. E. J. Barbeau, St. Catharines. P. E. Roberts, Toronto. L. R. Williams, Welland.

Dr. Jack Miller

Professor J. Miller, left, of the Department of Chemistry, instructs Mr. E. Farnworth of Thorold, a second year Chemistry student and Summer Research Assistant, in the theory and practice of Nuclear Magnetic Resonance.

Historical Map

Note the land allocated for Brock University shaded in gray between Thorold and Grantham townships.

Walker Complex (April 2002)

The complex was comprised of the new Student/Community Health and Fitness Centre and the state-of-the-art health club called The Zone, in addition to encompassing the existing physical education facilities. Among the new facilities was a 23 000-square-foot gymnasium, which boasted four basketball courts and a 200-meter, three-lane elevated track. The building was named after Walker Industries Holdings, a Thorold firm that was the key donor to the project.

Sedimentology and stratigraphy of the Lower Silurian Grimsby formation, in subsurface, Lake Erie and Southwestern Ontario

Since the first offshore Lake Erie well was drilled in 1941, the Grimsby and Thorold formations of the Cataract Group have been economically important to the oil and gas industry of Ontario. The Cataract Group provides a significant amount of Ontario's gas production primarily from wells located on Lake Erie. The Grimsby - Thorold formations are the result of nearshore estuarine processes influenced by tides on a prograding shelf and are composed of subtidal channel complexes, discrete tidal channels, mud flats and non-marine deposits. Deposition was related to a regressive - transgressive cycle associated with eustatic sea level changes caused by the melting and resurgence of continental glaciation centred in Africa in the Late Ordovician/Early Silurian. Grimsby deposition began during a regression with the deposition of subtidal channel complexes incised into the marine deposits of the Cabot Head Formation. The presence of mud drapes and mud couplets suggest that these deposits were influenced by tides. These deposits dominate the lower half of the Grimsby. Deposition continued with a change from these subtidal channel complexes to laterally migrating, discrete, shallow tidal channels and mud flats. These were in turn overlain by the non-marine deposits of the Thorold Formation. Grimsby - Thorold deposition ended with a major transgression replacing siliciclastic deposition with primarily carbonate deposition. Sediment was sourced from the east and southeast and associated with a continuation of the Taconic Orogeny into the Early Silurian. The fluvial head of the estuary prograded from a shoreline that was located in western New York and western Pennsylvania running NNE-SSW and then turning NW-SE and paralleling the present day Lake Erie shoreline. iii The facies attributed to the Grimsby - Thorold formations can be ascribed to the three zones within the tripartite zonation suggested by Dalrymple et ale (1992) for estuaries, that is, a marine-dominated facies, a mixed energy facies, and a facies that is dominated by fluvial processes. Also, sediments within the Grimsby - Thorold are commonly fining upwards sequences which are common in estuarine settings whereas deltaic deposits are normally composed of coarsening upwards sequences in a vertical wedge shape with coarser material near the head. The only coarsening observed was in the Thorold Formation and attributed to non-marine deposition by palynological evidence. The presence of a lag deposit at the base of the sediments of the Grimsby Thorold formations suggests that they were incised into the Cabot Head Formation. Further, the thickness of Early Silurian sediments located between the top of the Queenston Formation, where Early Silurian sedimentation began, to the top of the Reynales - Irondequoit formation are constant whether the Grimsby - Thorold formations are present or not. Also, cross-sections using a sand body located in the Cabot Head Formation for correlation further imply that the Grimsby Formation has been incised into the previous deposits of the Cabot Head.

Beaverdams 1812-1814, 1912-1914

On cover: Beaverdams, 1812-14-1912-14.