This thesis presents the results of a study conducted to determine the math capabilities of mentally challenged students attending Reagan Junior High School in Wichita Falls, Texas. Survey results are used to determine needed curriculum changes.

Master of Landscape Architecture / Department of Landscape Architecture/Regional and Community Planning / Laurence A. Clement / Street musicians and performers attract people to public spaces. These performers, or ‘buskers’ as they are commonly referred, typically congregate along specific streets, parks, plazas, and transit stops in a city. The term pitch describes the place buskers perform. Pedestrian flow, visibility, and acoustics are just some of the factors that street performers consider when selecting a pitch. While performers resourcefully adapt to the challenges of different pitches, public spaces often do little to accommodate performers and their audiences. William Whyte observed how street performances facilitate social interactions between strangers and give character to cities and neighborhoods. Relative Pitch explores where performances occur and how they benefit public places. Case studies of popular busking locations establish a typology of squares, streets, and transit stops. Video clip analysis of street performances demonstrates the spatial relations between performer and audience. Dimensions and observations from these case studies provided insight and information for the application of the typology to proposed sites in Wichita, Kansas. Buskers adapt pitches relative to their physical environment. Point, linear, planar, and volumetric elements define and articulate temporary stages, audience space, and circulation paths during performances. Design proposals for the typology sites in Wichita illustrate how flexible performance spaces can be incorporated in squares, streets, and transit stops. This project looks at ways to activate public spaces by encouraging street performance.

Call number: LD2668 .T4 1965 D96 / Master of Science

Master of Science / Department of Geology / Matthew E. Brueseke / The Southern Oklahoma rift zone (SOA), which stretches from southern Oklahoma through the Texas panhandle and into Colorado and New Mexico, contains extensive bimodal mafic-silicic magmatism related to the opening of the Iapetus Ocean during the late Precambrian and early Cambrian. Within the SOA, the subsurface in and adjacent to the Arbuckle Mountains in southern Oklahoma contains thick packages of mafic to intermediate lava flows interlayered with thick, extensive rhyolite lava flows and lesser silicic intrusive bodies, which were first described during a 1982 drill test (Hamilton Brothers Turner Falls well) in the region. Well cuttings of these units were collected from that well and three others (Pan-Am Williams D-2, Pan-Am Jarman, Pan-Am Newberry). This study is focused on these mafic-intermediate lava flows, which represent an important stage in the evolution of the SOA and provide insights into the formation and tectonomagmatic evolution of the rift zone. The estimated 210,000 km[superscript]3 of mafic rocks in the SOA were extruded as a result of the break-up of Pannotia and the formation of the failed arm of a three-armed radial rift system. Samples analyzed from the wells plot as basalts to andesites on the TAS diagram of Le Bas et al (1986) and as subalkaline-alkaline basalts to andesite-trachyandesites on the Zr/TiO[subscript]2 vs. Nb/Y diagram of Winchester and Floyd (1977). They are dominantly tholeiitic on multiple discrimination diagrams including those of Miyashiro (1974) and Irvine and Baragar (1971). The lava flows contain traits common with EMI OIB coupled with upper crustal contamination, such as Zr/Nb values ranging from 8 to 10, Ba/Nb values ranging from 10 to 20, and K/Nb values ranging from 300 to 600. Chemostratigraphic comparisons between each well reveal up to five lava flow packages within the larger mafic-intermediate sequence, at least in the vicinity of the sampled wells. When compared with intrusive mafic rocks outcropped in the Wichita Mountains, the SOA lava flows display geochemical traits most similar to those of the Roosevelt Gabbros, suggesting a possible co-genetic relationship. Overall, the whole rock chemical characteristics coupled with comparisons with other large igneous provinces (Columbia River and Oregon Plateaus, East African Rift System) indicate that the SOA lava flows are the result of flood basalt volcanism.

Thesis (M.A.)--University of Wyoming, 2007. / Title from PDF title page (viewed on Oct. 23, 2008). Includes bibliographical references (p. 102-110).

Thesis (D.W.S.)--Institute for Worship Studies, 2003. / Abstract. Includes bibliographical references (leaves 205-208).

Project/Thesis (D. Min.)--Abilene Christian University, 2000. / Includes abstract and vita. Includes bibliographical references (leaves 102-105).

Thesis (D. Ed.)--Ball State University, 2009. / "November 2008." Title from PDF t.p. (viewed on Nov. 11, 2009). Includes bibliographical references (p. 201-216).

The purposes of this study are: (1) to make an investigation of the home-room programs of the junior high schools in Wichita Falls, Texas, to discover what social guidance, if any, is offered to students; (2) to set up criteria for evaluating a social guidance program in a junior high school; and (3) to evaluate the social guidance programs of the home rooms in the junior high schools in Wichita Falls, Texas, in terms of the criteria set up for evaluation.

The purpose of this study is to learn to what extent the point of view of patrons of Wichita Falls, Texas, has a background of progressivism or of essentialism and to what extent, if possible, the children are influenced in school by the point of view held by the parents; also which part of the school system -- general education, the curriculum, the child, or the administration -- has the most progressive approval of the parents.