St. Catharines and District Labour Council fonds, 1957-1986

The St. Catharines and District Labour Council was founded in May 1957 by unionized workers from St. Catharines, Thorold, Merritton, Port Dalhousie and Grimsby. They sought to improve the social and economic welfare of workers; promote the organization of workers into unions for their mutual benefit, regardless of race, creed, colour, or national origin; encourage the sale of union-made goods and services; promote worker education; provide workers with a voice in politics; and safeguard the democratic nature of the labour movement. The Council, affiliated with both the Canadian Labour Congress and the Ontario Federation of Labour, was instrumental in assisting local workers with their labour disputes, including Canadian Pulp and Paper workers at Abitibi Provincial Paper in Thorold [1975-76], and Gallaher Paper [1999], workers at the St. Catharines Eaton’s store [1985], as well as smaller disputes such as that between the part-time secretarial staff and the Welland County Roman Catholic Separate School Board [1972] and workers of the Skyway Lumber Company [1972]. The Council also assisted the community at large by offering a Community Counseling Service [1971-1976] to help citizens with issues concerning various government agencies, social services and Acts, such as the Vacation Pay Act, Landlord and Tenant Act, Employment Standards Act, unemployment insurance claims and workman’s compensation claims. Other projects that the Council organized included an annual Education Institute [1958-1965] and the annual publication of Labour Review, a summary of the Council’s past year. The Labour Council continued to operate until 2010, when several local Labour Councils merged to form the Niagara Regional Labour Council.

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.

Morrey's Farmers and Business Directory, Containing the Following Valuable Information: The Name, with the Post Office Address, Lot and Concession, of each Farmer; also whether a Freeholder or a Tenant (1884/85)

The Union Publishing Co.'s farmers' and business directory for the counties of Haldimand, Lincoln, Welland & Wentworth.

Marriage Certificate - Hamilton K. Woodruff and Julia C. Cleveland

The marriage certificate of Mr. Hamilton K. Woodruff of St. Catharines and Miss Julia C. Cleveland of Erie, Pennsylvania. This is certificate no. 5221 signed by James C. Wilson. This is accompanied by 2 envelopes; one envelope is from Henry L. Rea, clerk of courts, Erie Pennsylvania to Mr. H. K. Woodruff, the other envelope just says "marriage certificate Mrs. H. K. Woodruff", Nov. 21, 1894.

Letter with the letterhead “H.H. Warner and Co.” of Rochester, N.Y. from the H.H. Warner Co

Letter with the letterhead “H.H. Warner and Co.” of Rochester, N.Y. from the H.H. Warner Co. The writer asks why Mr. Woodruff did not stop there on his way home from Pennsylvania regarding his shooting share at Point Mouillee [a game area in Monroe County, Michigan]. This letter is accompanied by an envelope, May 19, 1886.