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The article presents abstracts of geographical research papers. In the research paper "A Geographical Study of Nova Scotia," researcher R.H. Whitebeek discusses the geographic conditions of Nova Scotia. Lying nearer Europe and possessing many excellent harbors and peopled by immigrants from the best European stocks, the province of Nova Scotia in Canada has now, after 300 years, fewer people than the city of Boston, Massachusetts. Its total manufacturing output is less than that of single companies in New England, and the province has shared but slightly in Canada's economic growth.

Minority groups differ from one another, among other things, in the extent to which they are integrated into or apart from the societies to which they belong. The extent of this integration or apartness is reflected in the various ways in which the minorities differ from the rest of the population, such as in the effect of economic class upon voting. No minority group is ever completely integrated into its society, for complete integration is tantamount to the extinction of group identity. No minority group is ever completely apart, for the term "minority" implies the existence of a majority with which the minority forms a common society. The dimension of integration-apartness is related to but not identical with the dimension of assimilation. Assimilation refers to the replacement or modification of group characteristics as a consequence of out-group contacts. Integration refers to the extent a minority actually forms a part of the body politic of its society. Thus, German "non-Aryan" Christians were fully assimilated but, in the Third Reich, certainly not integrated into the German society. In general, the term "integration" is applicable at various levels of analysis. We talk of the integration of individuals into groupings, the integration of these groupings into further units, and the integration of these into larger units in turn. In the case of our study, individuals are more or less integrated into their respective minority groups, and these in turn are more or less integrated into their respective societies. We are concerned in this paper with developing a measure for the degree of integration of minority groups into their societies. The basic proposition of this paper is: The more apart a minority group is from its society, the more will it differ from that society as a whole in the effect of economic class upon voting. An analysis of the voting of two minorities in Central Europe illustrates the above proposition. This is followed by comments on minority group voting in the United States and Canada. [ABSTRACT FROM AUTHOR]

Facies relationships in Pleistocene braided outwash deposits in southern Ontario demonstrate the presence of a large braid bar with adjacent side channel. The core of the bar is up to 6 m high, and consists of crudely horizontally stratified gravels. Downstream from the core is the bar front facies, consisting of large gravelly foresets up to 4 m high, rounded off in many places by reactivation surfaces. Upstream from the core is the bar stoss side facies consisting of several sets (individually up to 35 cm thick) of tabular cross-bedding, arranged in coarsening-upward sequences. The stoss side-core-bar front relationships are continuously exposed in one 400 m long quarry face which is cut almost parallel to the palacoflow direction. A transverse quarry face shows the side channel facies, which consists if trough cross-bedded sands. Gravel layers can be seen to finger from the main gravelly bar into the sandy side channel, but they do not reach the base of the channel. This surprising relationship indicates that gravel moved only in the topographically higher parts of the system. After deposition in the side channel, and growth upstream and downstream from the bar core, the entire system aggraded. Crudely horizontally stratified, and imbricaled gravel sheets were laid down as a bar top facies. Grain size analyses indicate strongly bimodal distributions, implying that much of the sand in the spaces between pebbles and boulders filtered in after the gravel had been deposited. This interpretation is strengthened by velocity calculations—mean velocities in excess of 300 cm/s would be needed to roll the gravel as bed load, but at such a velocity, a large amount of sand would be transported entirely in suspension. In a final section of the paper, our results are combined with other work on braided systems in an attempt to formulate a more general facies model. [ABSTRACT FROM AUTHOR]

The article focuses on the program for the annual meeting of the Phycological Society of America. The meeting will be held at the University of Alberta, Edmonton, Alberta, in Canada, from June 20-24, 1971. The chairmen of the program will be Harold C. Bold and Louis Druehl. All sessions of the program at which contributed papers, lectures and the symposium are presented are scheduled as joint sessions of the Phycological Society of America, the Phycological Section of the Canadian Botanical Association and the Phycological Section of the Botanical Society of America.

In this paper harmonic analysis is employed to investigate regional variations of the annual march of precipitation over Canada. In order to examine the regional variations of the annual march of precipitation, the researcher is confronted with the problem of presenting variations of space as well as time. A method of objectively describing and mapping these space-time characteristics of precipitation is that of harmonic analysis. Before proceeding to examine the area distribution of the two major variance components, the annual and semiannual, it is useful to establish the distribution of the total variance and also the relationship of the two major components to the total variance and to one another.

The article reports on the National Conference on the Blind Pre-school Child, which being sponsored by the American Foundation for the Blind on March 13 to 15, 1947 at the Russell Sage Foundation hall in the U.S. It provides information on the number of participants attending the conference from various states and foreign countries including Canada, Brazil, and South Africa. The conference received research papers, which being arranged by Berthold Lowenfeld, director of education for the foundation.

Discusses highlights of the convention on educational psychology to be held in Quebec, Montreal from August 27-31, 1973. Information on the work done by educational psychologist Benjamin S. Bloom in the field of mastery achievement; Progress report on the first year of National Institute of Education by the institute's director Thomas K. Glennan; Details on a paper session devoted to the topic of teacher behavior and evaluation.

The paper focuses on the article written by the author on C.U.A. rate-making procedure, which is biased against high risk categories because of the double-counting which results from treating dependent risk classes as if they were independent. An analyst has presented some data on industry loss ratios, which seem to deny the author's conclusion when applied to the specific case of driving record classes. The data does not refute the author's conclusion that C.U.A. rates are biased upwards for high risk classes, but it does seem to deny the C.U.A. assumption that persons should be classified as high risks simply because they have had an accident in one of the previous three years.

The article presents information on the "Sixth International Conference on Oral Biology" to be held at Toronto, Ontario, from June 3-5, 1974. The theme of the conference will be "Pharmacology and Therapeutics." Interested scientists are invited to submit specific titles and abstracts of papers to be considered for presentation at the conference. Primary consideration will be given to research utilizing a multidiscipline approach and having a wide appeal to scientists in oral biology. Titles should clearly define the topic; a single page abstract must include a summary of materials, research methodology, results and conclusions.