Master of Science

thesisInterest in the problem of "Attitudes Toward Intercollegiate Football" has been stimulated by the many controversial articles published in newspapers and magazines, and from various discussions broadcast over radio net-works. Especially has thi3 problem boon evident in the last few years, due to the cheating and "fix" scandals in the mid-west and e a 3t. Y^hat has caused these scandals? /re we overemphasizing football? Are we forgetting the true reasons for having football? Are the reasons for having football becoming strictly commercial? Recently a group of college presidents was called upon to establish a new code to control Intercollegiate athletic programs. In view of these considerations it is desirable to determine the present attitudes of various groups of people toward Intercollegiate football

The nature of the relationship existing between instructors' grades, Ohio State University psychological examination scores, and the graduate record examination scores of the 1949 graduating class at Boston University General College

Thesis (Ed.M.)--Boston Universit

Fly-fishing in Maine lakes : or, Camp-life in the wilderness.

https://scholars.unh.edu/angling/1003/thumbnail.jp

The effect of community status upon the differential achievement of school children

Thesis (Ed.D.)--Boston University

Freighter Off St. Kitts

Photograph taken by Salt Lake Tribune staf

A gravity and magnetic study of the Crooked Creek cryptoexplosion structure, Crawford County, Missouri

The pre-Pennsylvanian structure at Crooked Creek consists of a complex, vertically faulted ring of Cambrian and Ordovician sediments with a central uplifted core. The center of the structure is strongly deformed and contains shatter cones, brecciation, and other signs of extreme shock. A magnetic low over the center of the structure suggests that igneous material was not involved in the formation of the structure, and this is corroborated by core analysis. Gravity data indicates several small gravity lows, possibly associated with areas of brecciation, circling the flanks of the structure. As in the magnetic data, there is no indication that the feature extends to depth. The lack of a corresponding magnetic anomaly rules out a volcanic origin for the structure. The limited erosion of the area, the statistical orientation of the shatter cones, and the lack of deformation at depth, point to an explosive source near the original surface of the region. The only known way for a shock intensive explosion to occur near the surface without involving basement material is from the impact of a meteorite or comet --Abstract, page ii