Thesis (Ph. D.)--Ohio State University, 2004. / Title from first page of PDF file. Document formatted into pages; contains xv, 170 p.; also includes graphics. Includes bibliographical references (p. 130-139).

Thesis (M.A.)--Ohio State University, 1940. / Includes bibliographical references (leaves 54-56). Available online via OhioLINK's ETD Center

Thesis (M.S.) -- Ohio State University, 2005. / Includes bibliographical references (leaves 110-118). Available online via OhioLINK's ETD Center

Thesis (M.S.)--University of Wisconsin--Madison, 1966. / eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.

Texte remanié de: Diss.--Universität Stuttgart, 1995. / Notes bibliogr. Bibliogr. p. 375-406. Résumés en polonais et en anglais. Index.

Texte remanié de: Diss.--Universität Münster, 1997. / Bibliogr. p. 402-432. Index.

Made available in DSpace on 2014-06-12T16:27:57Z (GMT). No. of bitstreams: 2 arquivo1918_1.pdf: 8599430 bytes, checksum: 5ff7691e1a400f323890fbfcc3e58c35 (MD5) license.txt: 1748 bytes, checksum: 8a4605be74aa9ea9d79846c1fba20a33 (MD5) Previous issue date: 2009 / John Waters é um diretor americano que começou a fazer filmes underground na década de sessenta. A partir de Pink Flamingos, Waters tornou-se conhecido por cenas tidas como bizarras. Protagonizadas, entre outros, pelo ator Harris Glen Milstead, mais conhecido como Divine. Um dos grandes fatores de reconhecimento para o autor foram as exibições no circuito cinematográfico Midnight Movie, dedicado à mostra de filmes que, por seu teor escatológico, não seriam bem aceitos em cinemas convencionais. Essas sessões, assim como a exploração de roteiros anti-convencionais em sua obra, geraram em torno de si um público ávido pelo consumo de filmes voltados a uma estética não canônica, o que reverbera até os dias atuais. A seguinte análise, leva em conta elementos presentes na primeira fase de John Waters (década de setenta até meados da década de 80), abordando temas como o grotesco, o feio e o camp. Na segunda parte nos propomos a analisar alguns aspectos dos Midnight Movie em busca de elementos de gosto, que formariam uma subcultura onde seus membros apresentariam em comum a preferência pelo nãocanônico. Depois nos ativemos a uma análise estética, confrontando características do cinema clássico com as teorias estudadas. Por fim, tentamos confrontar as duas premissas com base no teórico Michel Foucault, buscando descobrir a coerência entre o conceito de transgressão e o material analisado

The Summit Camp, now abandoned, is located seven miles north of the town of Greenwood in south-central British Columbia. Mineral deposits in skarn zones of the camp were mined for their copper, gold, and silver values. The oldest rocks in the Summit Camp are the contorted grey cherts of the Knob Hill Formation of Paleozoic (?) age. The Knob Hill Formation is overlain nonconformably by the Paleozoic Attwood Series, made up of the shales of the basal Rawhide Formation; the limestones, chert breccia, and limestone breccia of the Brooklyn Formation; and the pyroclastics, lavas, and greenstones of the Eholt Formation. The chert and limestone breccias of the Brooklyn Formation, interpreted by some earlier workers as the results of silicification and tectonic brecciation respectively, are considered to be of clastic sedimentary origin. There is a pronounced nonconformity between the Brooklyn and Eholt Formations. These sedimentary rocks were intruded in Mesozoic (?) time by the Emma Intrusive consisting of quartz diorite, diorite and minor gabbro. This event was followed by the emplacement of the Lion Creek Intrusive, which consists of quartz diorite and syenite. In Oligocene time the arkoses of the Kettle River Formation were deposited in fresh-water basins in the area. Earlier rocks were intruded by Miocene (?) phonolite and pulaskite, that also gave rise to flows of similar composition. Miocene (?) basic dikes are the latest rocks of the area. Mineral deposits of the camp contain magnetite, pyrite, pyrrhotite, chalcopyrite and tetrahedrite in a gangue of skarn minerals. Skarn has formed from Brooklyn limestone as a result of the addition of heat and large amounts of Si, Al, and Fe⁺⁺⁺ from the Lion Creek Intrusive. The intrusive assimilated large amounts of Ca and CO₂ in the process. Skarn zones are controlled by proximity to the Lion Creek stock, or by a contact of limestone with other rocks, or by the presence of channelways such as faults or permeable beds. Metallic minerals were introduced into the skarn zones along fractures and foliation planes with falling temperature. Epithermal precious metal veins that occur close to the Mesozoic (?) intrusives of the Boundary District are not found in limestone. It is believed that these veins were emplaced during a late stage in the cooling of the plutonic rocks. The earlier, higher temperature release of metals into the skarn deposits may be the result of the assimilation of CO₂ that locally prevented the solidification of the shell of the consolidated intrusive body. The mineralizing fluids responsible for the epithermal veins were trapped within the shell and released at a late stage by fracturing due to cooling. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate

The problem of this study was to make a critical evaluation of the qualifications and duties of counselors in girls' selected private summer camps in Texas, New Mexico, and Colorado for the following purposes: 1. To determine the duties and qualifications of camp counselors; 2. To determine criteria for qualifications and duties of camp counselors; 3. To determine the opinions of camp directors regarding the duties and qualifications of counselors; 4. To determine the extent to which counselors available for these areas meet the qualifications outlined by camp directors; 5. To determine the needs of the camps for counselors from the viewpoint of the directors of camps; 6. To determine the duties and needs indicated by the directors as far as training is concerned; 7. To determine recommendations for pre-service training in physical education departments for future counselors.

No description available.