This project examines the Southern California and Inland Empire banking environment during the period from 1992 to 1997. It includes an analysis of Washington Mutual's market strategy, and financial strategy for entering this fiercely competitive environment. Washington Mutual's competitive advantages and weaknesses will be analyzed to understand its approach to capturing strong market presence.

No description available.

This dissertation critically examines the entrenched Western classical music paradigm in K-12 and higher education music programs and its impact on Black, Indigenous, and People of Color (BIPOC) students. Utilizing Critical Race Theory (CRT) (Delgado & Stefanic, 2017) and Culturally Relevant Pedagogy (CRP) (Ladson-Billings, 2022), the study explores how this dominance leads to epistemological and ontological imprisonment, marginalizing non-Western musical traditions and perpetuating cultural hegemony and systemic racism. Through qualitative peer research interviews with BIPOC university music education students, faculty members including the curriculum director, the research uncovers significant themes, including normalizing and cultural hegemony of Western classical music, the pressure to conform, resistance to pedagogical shifts, and structural barriers to implementing culturally sustaining pedagogies. Additionally, it highlights the duality and dialectical tension educators and students face navigating the dominant Western paradigm while striving to integrate diverse musical epistemologies. The dissertation passionately advocates for new possibilities in practice through transformative approaches to music education that honor students’ cultural backgrounds and challenge dominant narratives. The text suggests the need for changes in the curriculum, policies, and inclusive educational practices to better represent the diverse cultural backgrounds of all students. It offers practical recommendations for educators and institutions to create a fairer and

隨著社會與科技發展，電影教育之規劃也持續改變，特別是數位科技的浪潮衝擊下，電影教育的變化也隨之加劇。本研究之目的即在探討美國電影教育如何受到電影產業對、社會及科技的影響。本文以University of Southern California, New York University, University of California-Los Angeles, and Syracuse University 這四個學校為主要研究對象，針對其自1960年代迄今的電影教育規劃、學位授與設計、和課程結構進行整理分析，以試圖理解電影教育與產業、社會與科技變化之關係，並透過文獻研究與專家深訪，加以驗證。此研究發現電影教育機構透過新課程的開設、學程提供及學位授與規定的調整等等方式，反應產業、社會、科技的變化。雖然電影創造的本質並未改變，但其本質及概念仍持續影響學校電影課程的外貌。 / American film education system is changing, particularly in light of the digital technology boom. Just how American film education has evolved with regards to the market, social, and technical influences is the objective of this research. Four schools--University of Southern California, New York University, University of California-Los Angeles, Syracuse University--and their undergraduate and graduate curricula from 1960s to present are examined. Qualitative explanations are supported by interviews with administrators and instructors. The study finds that technological developments play an important role in the evolution of American film education by engendering the creation of new courses, programs, departments, and degrees. Yet, the fundamentals of filmmaking have not changed, and schools’ origin and philosophy remain influential factors in shaping the film curriculum.

No description available.

The purpose of this study is to determine the effects of school-wide positive behavior interventions and supports (SWPBIS) on student academic performance and other outcomes. The participants in the study are eight middle schools from an urban Southern California school district that were mandated to implement SWPBIS in 2005.

The purpose of the study is to develop a foundation of knowledge that could improve the current policies and procedures with regards to their implementation within the mental health services provided by the Children's Bureau.

The Inland Empire offers many advantages for business. This project documents how the Inland Empire is a suitable area to start and grow a business due to its reasonable space and labor costs, educated work force, infrastructure advantages and easy accessibility to freeways, ports, railroads and airports.

Indiana University-Purdue University Indianapolis (IUPUI) / Differential exhumation within the eastern Transverse Ranges of southern California has revealed a tilted crustal section that provides a unique view into the architecture of the Mesozoic arc. At the base of this crustal section is a group of well-exposed sheeted plutons. Well-developed, gentle to moderately dipping magmatic and solid-state fabrics within these plutons are regionally consistent, margin-parallel, discordant to internal sheeting and layering, and are generally parallel to equivalent host rock structures and fabrics. In some plutons, magmatic foliations define regional fold structures, thus recording regional contraction during chamber construction. Collectively, field mapping and fabric analyses within these sheeted plutons show that the observed fabric patterns are better explained by regional deformation rather than internal magma chamber processes. This interpretation is in direct contrast to previous mapping in the region. The host rocks also record complex processes during sheeted pluton emplacement. Deflection of host rock foliations and structures into parallelism with pluton contacts suggest that downward ductile flow played a role in making space for these plutons. However, evidence of regional faulting and shearing is not observed, suggesting that they did not play a significant role. Although there is considerable microstructural variability within each pluton, the observed microstructures are generally consistent with a transition from magmatic to submagmatic/ high-temperature solid-state deformation. Magmatic microstructures are defined by euhedral to subhedral plagioclase, hornblende, and biotite that do not show significant internal crystal-plastic deformation. Evidence for high-temperature solid-state deformation includes high-temperature grain boundary migration in quartz, plagaioclase, potassium feldspar, and hornblende; chessboard extinction in quartz; and ductile bending in plagioclase and hornblende. Microstructural observations also indicate that mafic and intermediate compositions record stronger magmatic fabrics than felsic compositions. Based on the structural and microstructural observations presented in this study, I interpret that these sheeted plutons were emplaced into an active continental arc setting that was undergoing regional contraction. The strong magmatic fabrics and high-temperature solid-state overprinting is likely a consequence of regional deformation during crystallization. The weak fabrics within upper crustal plutons relative to the strong fabrics within the mid-crustal plutons suggest that deformation was largely localized to the more compositionally heterogeneous mid-crustal portions of the arc structure.

Indiana University-Purdue University Indianapolis (IUPUI) / The objectives of this study are, generally, to analyze and understand internal processes that produce melts in an oceanic-continental subduction setting; and, specifically, to understand the assembly of a Cretaceous magmatic arc pluton (Palms pluton), including the timing of melt emplacement(s) and melt evolution from the source. SiO2 concentrations vary from ~ 69-76 % by weight. Whole rock trace element concentrations vary up to 7 times. Zircon analysis shows a minimum age difference in the pluton of 3 my, if considering the uncertainties of the oldest and youngest samples. According to the model made from the HEAT program, this is approximately six times longer than the estimated crystallization time of one batch of melt with the same physical properties as the Palms pluton. Two distinct sources, perceived from chemical analysis of premagmatic zircons, are found throughout the pluton. REE compositional patterns show a hybridization of Proterozoic and Mesozoic sources in some, but not all, Palms pluton granites. This data suggests that the pluton formed from multiple intrusions and the Proterozoic source remained relatively consistent throughout the pluton’s assembly with few additions of younger Mesozoic source material.