44 resultados para Grimsby Mills

em Brock University, Canada


Relevância:

60.00% 60.00%

Publicador:

Resumo:

Letter to Messrs. Summer and Nelles of Grimsby from Thomas Street and Mr. Hamilton in which they state that W.S. Britton has purchased the Grimsby Mills that belonged to W. James Paterson, Jan. 17, 1848.

Relevância:

40.00% 40.00%

Publicador:

Resumo:

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.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

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.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Ontario Editorial Bureau (O.E.B.)

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Edward W. Bowslaugh (1843-1923) was the son of Jacob and Anna (Beamer) Bowslaugh. Edward Bowslaugh married Mary Southward, and the couple had six children, Edgar Morley, Edward Freeman, twins Alfred Malcolm and Alice Mary, Annie Olivia, John Jacob and Mabel Florence. Edward W. Bowslaugh was a farmer, contractor and owner of the Grimsby Planing Mills in Grimsby, Ont. and Bowslaugh’s Planing Mill in Kingsville, Ont. The mills manufactured door and sash trim and other wood related products. Some customers contracted the firm to provide wood products for cottages being built at Grimsby Park, the Methodist camp ground. Some time before 1885 Edward Bowslaugh and his family moved to Kingsville, Ont. to open up a new planing mill and door and sash manufactory. He later sold the Grimsby Planing Mills to Daniel Marsh. The diaries and account books include many names of workers as well as friends and family members residing in the Grimsby and Kingsville areas. James M. Bowslaugh (1841-1882) was the son of Jacob and Anna (Beamer) Bowslaugh. James married first Anna Catharine Merritt and after her death in 1875 he married Mary Gee in 1877. James and Anna had three children, Eliza, James Herbert, George Hiram, all died very young. James and Mary Gee had one son, Charles Leopold Kenneth Frederich Bowslaugh, b. 1881. James Bowslaugh was a farmer and lumberman, much like his younger brother Edward. James’ early diaries often note the activities of himself and his brother Edward. Both Edward and James were heavily involved in the Methodist church, teaching or leading Sunday school and attending prayer meetings. Alfred M. Bowslaugh b. 1873 was the son of Edward W. Bowslaugh and his wife Mary Southward. The school notebook is from his days as a student in Kingsville, Ont.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

A vignette of Grist and Flouring Mills, Clinton, Andrew Dean, Esq., Proprietor.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

A vignette of the Lincoln and Welland Canal Mills

Relevância:

20.00% 20.00%

Publicador:

Resumo:

A vignette of the Mansion House in Grimsby, Andrew Randall, Proprietor.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

A vignette of J. McDonagh's Saw and Plaining Mills, Welland Canal, Thorold.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Contains information about the campground, the hotel, church services and includes advertisements.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

An account with W.M. Forbes dated April 1st, 1875 and amounting to $21.38. There is a line at the bottom of the receipt that reads "I don't care about any money but my creditors seem hard up".

Relevância:

20.00% 20.00%

Publicador:

Resumo:

An Invoice for Mr. W. Cowan form Alex Hutchison, totalling $1000.00. The note at the bottom of the invoice reads "I have nothing to communicate as Mr. Parks is just writing you. Hoping you and your family are all well with respect I am dear Sir, Yours Truly Alex Hutchison"

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Letter (1 page, typed) to S.D. Woodruff which accompanied the Rothrock account papers. Signed by Herbert Mills, assistant treasurer of Jarvis-Conklin Mortgage Trust Company, Oct. 27, 1890.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

The Interlake Tissue Mills storage location was at the intersection of Glendale and Merritt Street in Merritton. In the 1850s, the Beaver Cotton Mills (later Merritton Cotton Mills) was built. It was a frame building that burned down in 1881. A sandstone structure replaced the previous building. In 1906, the cotton mill closed and in 1912, the Independent Rubber Company took over the building. The mill was doubled in size. The rubber company remained there for ten years and then the building remained vacant until 1935. Interlake Tissue Mills acquired the building for storage purposes. A fire razed the larger of the plant’s buildings on Memorial Day weekend in 1961. After the fire, Domtar used the smaller building for storage for a short time. This is currently the site of the Keg Restaurant.