Thesis (Ph. D.)--University of Washington, 2002. / Vita. Includes bibliographical references (p. 144-159).

Thesis (Ph. D.)--University of Oregon, 2002. / Typescript. Includes vita and abstract. Includes bibliographical references (leaves 131-137). Also available for download via the World Wide Web; free to University of Oregon users.

Hacienda San José de Cerro Gordo is a working hacienda 30 miles outside of Mexico City. The hacienda encompasses a large rancho (farming) area, mostly covered by prickly pear cacti and the central, gated compound, which includes the exquisite, 19th century casco (the main house of the hacienda), historic wall structures, and modern worker housing. The casco was built in the late 19th century (exact dates unknown). The hacienda is situated in an agrarian desert landscape, between the foothills of Cerro Gordo to the north and the pyramids of Teotihuacán in the distance to the south. The grand house has been completely uninhabited for forty years, the lack of maintenance leading to its dilapidation with each passing year. This Master's Report is in the format of a "feasibility study" which outlines the current conditions of the hacienda, explores the challenges it faces, options for its revitalization, and ultimately, to act as a resource for similar projects. The following research question is addressed: what are the best options for the stabilization and revitalization for Hacienda San José de Cerro Gordo, who are the actual and possible players in plan of action, what are the options for funding and what is the most feasible program for the hacienda? / text

Bogotá is a city that has seen rapid change in the recent years. By the 1990’s the city’s public space was in crisis and its elements were being used in inappropriate ways; some were even been illegally privatized. Inside the city’s multiple ills, a politically driven set of changes began to happen. By the turn of the millennium an urban renaissance of the city originated. Multiple public spaces, libraries, schools, and new transportation systems were built and implemented by different city Mayors. At present, after the initial thrill and polemics developed during the construction of the new public spaces, some of the major changes have settled. This situation makes it a good moment to develop an analysis of the performance of these public spaces today, in order to understand how they have evolved along with Bogotano’s during these years. The Plaza de San Victorino located in the downtown area of the city was one of the major renovation projects that the city underwent around the year 2000. Its analysis is representative of the evolution of Bogota’s public spaces during these years. This MDS makes an assessment from the point of view of the users of the Plaza de San Victorino. By making a Post-occupancy evaluation of this recently constructed public space using participant observations, mappings and surveys, this MDS generates a set of design recommendations for the Plaza and a design proposal for its improvement. / text

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Detailed mapping of Carboniferous rocks westward from areas mapped by Bogardus and Oden shows that rock units within the Marble Falls formation are traceable across "Cavern Ridge" a "barrier" invented by Plummer and referred to by others. The Ives breccia, Chappel limestone, Barnett formation, and Lower member of the Marble Falls formation formed as a transgressive depositional sequence. A thin zone of bypassing separates the Barnett and Marble Falls, but a hiatus between them in the Hall area cannot be demonstrated. A small-scale disconformity exists between the Lower and Middle members of the Marble Falls. Local faulting during deposition of the Marble Falls produced the Gibbons conglomerate, influenced the accumulation of Middle Marble Falls shale, and elevated the "Hall Uplift." Some lithosomes in the Upper member of the Marble Falls pinch out near the "Hall Uplift." Sandstone and mudstone of the Strawn formation abut against the carbonate mass of the Marble Falls to the north, but whether a period of erosion intervened between the deposition of the two is not known. Analysis of seven species of corals, twenty-three of brachiopods, two of pelecypods, five of gastropods, two of cephalopods, two of trilobites, and fourteen of conodonts suggests that the Chappel, Barnett, and Marble Falls faunal assemblages most closely resemble those of the Chouteau formation, Caney formation, and Morrow group respectively. In the Hall area no part of the Marble Falls should be correlated with the Atoka series. / text

published_or_final_version / abstract / toc / History / Doctoral / Doctor of Philosophy

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