Thesis (M.M.E.)--Boston University / A comparison of the vocal music program of Fairfield High School with other Connecticut high schools was necessary because, it was felt by the author and the school authorities, that the existing program was not up to the standards desired by the State Department of Education. The high school level was chosen because it was at this level, that the author was chiefly concerned. When the study was begun Fairfield High School was a Class B school, but before the investigation was completed, the enrollment of this high school had increased, so that the number of pupils was over one thousand, thus making it a Class A school. For this reason both types of schools were included in the survey. A few of the Class C schools were sent questionnaires, because of their nearness to the Fairfield location. Another reason for selecting high school level was because it was there that opportunities in various phases of vocal music education should be offered to the gifted student. Some definite problems existed in this school, so that it was felt by the author, that too many of these students were not getting all the advantages of a full music program. Poor planning and scheduling of classes, the failure to recognize music as an equal with other subjects in the curriculum, the lack of pupil participation in music activities in the school, as well as in the state, and lack of proper housing of the music department, were all problems that contributed to the failure of providing acequate opportunity for students gifted in music [TRUNCATED]

No description available.

Thesis (Ph. D.)--Catholic University of America, 1941. / Includes bibliographical references (p. 307-312) and index.

The study area encompasses 1100 km('2) in northwestern Connecticut and adjacent Massachusetts. It contains three lithologic-topographic belts: a crystalline upland, a marble lowland, and a phyllitic upland; each having two tills, the youngest of Woodfordian age. The youngest or "upper" till has ablation, resedimented (diamicton), meltout and basal facies. The older or "lower" till has oxidized and unoxidized zones. Tills and till facies of each belt can be discriminated by grain size and clast weathering characteristics. Abundance isopleths of upper till heavy minerals and exotic clasts indicate strong topographic control of basal ice movement and possible glaciotectonic thrusting. Field relationships and upper till compositional changes in the crystalline belt suggest this sequence: (1) erosion of the bed, (2) lodgment of till, (3) erosion of the bed and reincorporation of previously deposited till, and (4) ice stagnation. Entrained subglacial material locally was frozen during (3).

Thesis (Ph. D.)--Columbia University. / Also available in digital form on the Internet Archive Web site.

Thesis (M.S.)--Central Connecticut State University, 1999. / Thesis advisor: Dr Stuart R. Bennett. " ... in partial fulfillment of the requirements for the Master of Science Technology Education degree (Plan C)."

Thesis (M.S.)--Central Connecticut State University, 1998. / Thesis advisors: Dr. John E. Harmon and Dr. Richard Benfield. " ... in partial fulfillment of the requirements for the degree of Master of Science in Geography." Includes bibliographical references (leaves [101-107]).

Thesis (Ph. D.)--Columbia University.

Thesis (M.A.)--University of Wisconsin--Madison, 1965. / eContent provider-neutral record in process. Description based on print version record. Bibliographical essay: l. [106]-112.

Thesis (M.S.) -- Central Connecticut State University, 2010. / Thesis advisor: Dr. Damon Mitchell "... in partial fulfillment of the requirements for the degree of Master of Science in Criminal Justice." Includes bibliographical references (leaves 33-35). Also available via the World Wide Web.