The Premier (Transvaal) Diamond Mine is situated at the village of Cullinan, approximately 20 miles E.N.E. of Pretoria, the administrative capital of the Union of South Africa. It lies at an elevation of 4,722 feet above sea level. A paved highway connects Cullinan with Pretoria, and a spur-line, runs from the village to the Pretoria-Lourenco Marques railway. [...]

A great many geologists have visited the area and other regions where the Cobalt rocks are exposed. Although nearly all have expressed opinions on the geological problems concerned with the series, very few comprehensive reports have been published and these do not show complete agreement. [...]

The mine is located 6 miles east of the Town of Malartic, and is about 300 miles northwest of Montreal. A belt of altered peridotite about 2,500' wide trends southeasterly across the property. An embayment of talc-chlorite rock branches from the Cadillac fault, which forms the north contact of the peridotite, into the peridotite belt in a southeasterly direction. [...]

This thesis is a description of the geology of 125 square miles in south central Newfoundland. The area is a portion of a concession held by the Newfoundland and Labrador Exploration Company, for whom the survey was undertaken. It was mapped by the author and assistants during the summer of 1954. [...]

The subject matter of this thesis comprises a geological study of the map area of Dungannon and Mayo townships in southeastern Ontario plus detailed studies of special features of the geology of the map area. [...]

Stress-strain concepts and terminology are discussed, and definitions of basic terms given. The concepts of failure in the fields of Engineering, Soil Mechanics, and Geology are reviewed from a geological viewpoint. The conditions of rupture are discussed. Becker's (1893) paper is critically analyzed in the Appendix, and his principal conclusions are shown to be fallacious. [...]

The material used in this paper was obtained while carrying out mapping for the Quebec Department of Mines during the summer of 1957. The map area is underlain by gneisses and Labrador "Trough" type rocks. [...]

No geological map has been published of the Aillik-Makkovik area, as previous work was not done in sufficient detail to make correlation possible with the rest of the North American Pre-Cambrain, or for that matter, between different sections of the Labrador coast. The correlation of rocks at different sections of the coast is particularly complicated by the imperfect knowledge of the relative age of the tectonic movements of the bedrock. [...]

Following the discovery of copper-nickel mineralization in 1951 at St. Fabien de Panet, Montmagny County, about 50 miles east of Quebec City, the Quebec Department of Mines initiated a program of geological mapping in this area. In 1952, the author assisted Dr. J. Beland in the mapping of the St. Magloire area where the copper-nickel mineralization was discovered. [...]

p.4 missing - error in pagination / The Little Manicouagan Lake map-area lies within the co-ordinated: 51°30' N. and 51°55' N., and 67°20' W. and 67°53' W. The actual boundaries of the mapped area are not coincident with these co-ordinates since no attempt has been made at mapping a geographic unit; rather, the limits are provided by the outcrop areas investigated and therefore are largely confined to a narrow strip of readily available outcrops along the shores of the lake and the walls of the pass to the south. [...]