The Evening Journal, St. Catharines, Ontario, May 8, 1883

The Evening Journal, St. Catharines, Ontario, May 8, 1883.

The Evening Journal, St. Catharines, Ontario, August 16, 1900

The Evening Journal, St. Catharines, Ontario, August 6, 1900.

The St. Catharines Standard supplement, November 28, 1974

The St. Catharines Standard supplement featuring a Tribute to the Father of Transportation, the Honorable William Hamilton Merritt, November 28, 1974.

The Prince’s Visit to St. Catharines Broadside, 1860

Broadside advertising the appearance of the Prince of Wales, Albert Edward, who was Queen Victoria’s eldest son. He was to become Edward VII. The visit took place on Tuesday, the 18th of September in 1860. The broadside measures 20 cm. x 17.5 cm. The Royal Coat of Arms is featured on the top. Different typefaces are used throughout the broadside. The Broadside reads: "The Prince's Visit to St. Catharines. His Royal Highness will be at St. Catharines on Tuesday, the 18th Sept. 1860. The Committee of Management express the earnest hope that the Inhabitants of the Counties of Lincoln & Welland Generally, will manifest their Loyalty by joining in an enthusiastic demonstration to the Prince. Come Early to get Seats! As the accommodation in the Amphitheatre will be limited. A Grand Procession Of Firemen and other Public Bodies will be formed, accompanied by Bands of Music. A Royal Salute Will be fired by the St. Catharines Volunteer Artillery Company; and British Cheers will be given by the assembled assembled thousands. A General Illumination in the Evening! God Save The Queen! C.P. Camp, Sec'y to Committee. St. Catharines, September 15, 1860."

Plan of the Grand Central Hotel

Pre 1913 plan showing the Grand Central Hotel and Santorium Co. Ltd. on St. Paul Street, St. Catharines, Ont.

Campbell for Mayor

Alderman John S. Campbell expresses interest in becoming mayor of St. Catharines. Surce: The Star-Journal (St. Catharines, Ont.), Tuesday, November 27, 1906

Anomalous carbonate preservation in the abyssal North Pacific, ODP sites 882 and 1179: planktonic foraminiferal analysis, climate change and palaeogeomagnetism /

Thesis (M.Sc.)--Brock University, 2004.

Structural studies in the Southern Province, South of Sudbury, Ontario

Rocks correlated with the Hough Lake and Quirke Lake Groups of the Huronian Supergroup form part of a northeasterly trending corridor that separates 1750 Ma granitic intrusive rocks of the Chief Lake batholith from the 1850 Ma mafic intrusive rocks of the Sudbury Igneous Complex. This corridor is dissected by two major structural features; the Murray Fault Zone (MFZ) and the Long Lake Fault (LLF). Detailed structural mapping and microstructural analysis indicates that the LLF, which has juxtaposed Huronian rocks of different deformation style and metamorphism grade, was a more significant plane of dislocation than the MFZ. The sense of displacement along the LLF is high angle reverse in which rocks to the southeast have been raised relative to those in the northwest. South of the LLF Huronian rocks underwent ductile defonnation at amphibolite facies conditions. The strain was constrictional, defined by a triaxial strain ellipsoid in which X > Y > z. Calculations of a regional k value were approximately 1.3. Penetrative ductile defonnation resulted in the development of a preferred crystallographic orientation in quartz as well as the elongation of quartz grains to fonn a regional southeast-northwest trending, subvertical lineation. Similar lithologies north of the LLF underwent dominantly brittle deformation under greenschist facies conditions. Deformation north of the LLF is characterized by the thrusting of structural blocks to form angular discordances in bedding orientation which were previously interpreted as folds. Ductile deformation occurred between 1750 and 1238 Ma and is correlated with a regional period of south over north reverse faulting that effected much of the southern Sudbury region. Post dating the reverse faulting event was a period of sedimentation as a conglomerate unit was deposited on vertically bedded Huronian rocks. Rocks in the study area were intruded by both mafic and felsic dykes. The 1238 Ma mafic dykes appear to have been offset during a period of dextral strike slip displacement along the major fault'). Indirect evidence indicates that this event occurred after the thrusting at 950 to 1100 Ma associated with the Grenvillian Orogeny.

The genetics of glucosamine resistance in yeast /

Thesis (M. Sc.) - Brock University, 1975.

Improving grade eight students' spelling performance with a triad strategy approach

Thesis (M.Ed.)-- Brock University, 1996.

Is technology a threat to education? : the contribution of George Parkin Grant

Thesis (M.Ed.)-- Brock University, 1995.

On the Ewald method and the quartic Helmholtz free energy of an anharmonic metallic crystal

Thesis (M. Sc.) - Brock University, 1978.

Sentence combining and thinking : a study of adult ESL learners

Thesis (M.Ed.)--Brock University, 2003.

The effectiveness of explicit strategy instruction on the top level structure of a text

Thesis (M.Ed.)-- Brock University, 1995.

Canada seventy years ago : or, Prince Edward's visit to Niagara /

Verse.