Interior of Chapman College Chapel, Orange, California

Interior of Chapman College Chapel, Orange, California. The wooden-shingled church, constructed in 1909 for the congregation of Trinity Episcopal Church, is located on the northeast corner of East Maple Avenue and North Grand Street. Chapman College (now Chapman University) purchased the church for their chapel when the congregation moved to a new church on Canal Street.

Interior of Chapman College Chapel, Orange, California

Interior of Chapman College Chapel, Orange, California. Bill Carpenter, Chaplain. The wooden-shingled church, constructed in 1909 for the congregation of Trinity Episcopal Church, is located on the northeast corner of East Maple Avenue and North Grand Street. Chapman College (now Chapman University) purchased the church for their chapel when the congregation moved to a new church on Canal Street.

Chapman College Chapel interior, Orange, California

Small group meeting inside the Chapman College Chapel, Orange, California. The wooden-shingled church, constructed in 1909 for the congregation of Trinity Episcopal Church, is located on the northeast corner of East Maple Avenue and North Grand Street. Chapman College (now Chapman University) purchased the church for their chapel when the congregation moved to a new church on Canal Street.

Wedding, Chapman College Chapel interior, Orange, California

Wedding, Chapman College Chapel interior, Orange, California. The wooden-shingled church, constructed in 1909 for the congregation of Trinity Episcopal Church, is located on the northeast corner of East Maple Avenue and North Grand Street. Chapman College (now Chapman University) purchased the church for their chapel when the congregation moved to a new church on Canal Street.

Interior of Founders' Hall, Chapman College, Orange, California

Founders' Hall [now Roosevelt Hall], Chapman College, Orange, California. Life trustee James Roosevelt’s name graces this historical building, which was originally named Founders’ Hall, until its rededication in 1994. This building completed in 1928 (2 floors, 12,280 sq.ft.) is listed in the National Registry for Historical Buildings and houses the Center for Academic Success, Department of Languages, Division of Social Sciences and the Writing Center. Originally constructed to serve as the Art & Cafeteria Building for Orange Union High School, it was acquired by Chapman in 1954.

Interior of Founders' Hall, Chapman College, Orange, California

Desk and waiting area in Founders' Hall [now Roosevelt Hall], Chapman College, Orange, California. Life trustee James Roosevelt’s name graces this historical building, which was originally named Founders’ Hall, until its rededication in 1994. This building completed in 1928 (2 floors, 12,280 sq.ft.) is listed in the National Registry for Historical Buildings and houses the Center for Academic Success, Department of Languages, Division of Social Sciences and the Writing Center. Originally constructed to serve as the Art & Cafeteria Building for Orange Union High School, it was acquired by Chapman in 1954.

Interior of Founders' Hall, Chapman College, Orange, California

Inside Founders' Hall [now Roosevelt Hall], Chapman College, Orange, California. Life trustee James Roosevelt’s name graces this historical building, which was originally named Founders’ Hall, until its rededication in 1994. This building completed in 1928 (2 floors, 12,280 sq.ft.) is listed in the National Registry for Historical Buildings and houses the Center for Academic Success, Department of Languages, Division of Social Sciences and the Writing Center. Originally constructed to serve as the Art & Cafeteria Building for Orange Union High School, it was acquired by Chapman in 1954.

Interior of Founders' Hall, Chapman College, Orange, California

Inside Founders' Hall [now Roosevelt Hall], Chapman College, Orange, California. Life trustee James Roosevelt’s name graces this historical building, which was originally named Founders’ Hall, until its rededication in 1994. This building completed in 1928 (2 floors, 12,280 sq.ft.) is listed in the National Registry for Historical Buildings and houses the Center for Academic Success, Department of Languages, Division of Social Sciences and the Writing Center. Originally constructed to serve as the Art & Cafeteria Building for Orange Union High School, it was acquired by Chapman in 1954.

Interior of Founders' Hall, Chapman College, Orange, California

Lounge area inside Founders' Hall [now Roosevelt Hall], Chapman College, Orange, California. Life trustee James Roosevelt’s name graces this historical building, which was originally named Founders’ Hall, until its rededication in 1994. This building completed in 1928 (2 floors, 12,280 sq.ft.) is listed in the National Registry for Historical Buildings and houses the Center for Academic Success, Department of Languages, Division of Social Sciences and the Writing Center. Originally constructed to serve as the Art & Cafeteria Building for Orange Union High School, it was acquired by Chapman in 1954.

Structural analysis of interior layered deposits in north and south Coprates Chasma, Mars

Interior layered deposits within an embayment in the northern as well as near the southern wall of Coprates Chasma in the Valles Marineris, Mars are studied using HRSC, CTX, HiRISE and CRISM data. In the northern embayment, layered deposits outcrop in three separate locations (a western deposit, a central deposit and an eastern deposit). The central layered deposit in the north has a stratigraphic thickness of 2 km. The western layered deposit abuts against the chasma wall appearing to have a relatively un-eroded depositional surface. The eastern deposit is near a landslide scar which appears to have exposed basement layering showing downward displacement. This northern embayment is suggested to have been an ancestral basin. The triangular edged deposit near the southern wall of Coprates Chasma has an elongated mound protruding from the central edge and is suggested to be the outer limits of a fault block which is back rotated 6° south. The rotation may be the result of the Valles Marineris opening.

DEFORMATION OF INTERIOR LAYERED DEPOSITS (ILD) AND THEIR ASSOCIATED LANDFORMS IN WEST CANDOR CHASMA, MARS: IMPLICATIONS FOR THE TIMING OF ILD DEPOSITION

On Mars, interior layered deposits (ILD) provide evidence that water was once stable at the surface of the planet and present in large quantities. In West Candor Chasma, the ILD and their associated landforms record the depositional history of the chasma, and the deformation of those deposits provide insight into the stresses acting on them and the chasma as a whole. The post ILD structural history of West Candor is interpreted by analyzing the spatial relationships and orientation trends of structural features within the ILD. Therecording of stresses through brittle deformation of ILDs implies that the ILD had been lithified before the stress was imposed. Based on the prominent orientation trends of deformation features, the orientation of the stress regime acting upon the ILD appears to be linked to the regime that initially created the chasma-forming faults. An additional minor stress orientation was also revealed and may be related to large structures outside west Candor Chasma. The late depositional history of Ceti Mensa is herein investigated by examining the attributes and spatial relationship between unique corrugated, linear formations (CLF). The CLFs appear to be aeolian in origin but display clear indications of brittle deformation, indicating they have been Iithified. Evidence of lithification and the mineral composition of the surrounding material support the interpretation of circulating water in the area.

Capacity to Attend to the Needs of Persons with Dual Diagnoses in the Criminal Justice System: Views of Mental Health and Criminal Justice Professionals

Currently, individuals with intellectual disabilities are overrepresented within the Criminal Justice System (Griffiths, Taillon-Wasmond & Smith, 2002). A primary problem within the Criminal Justice System is the lack of distinction between mental illness and intellectual disabilities within the Criminal Code. Due to this lack of distinction and the overall lack of identification procedures in the Criminal Justice System, individuals with disabilities will often not receive proper accommodations to enable them to play an equitable role in the justice system. There is increasing evidence that persons with intellectual disabilities are more likely than others to have their rights violated, not use court supports and accommodations as much as they should, and be subject to miscarriages of justice (Marinos, 2010). In this study, interviews were conducted with mental health (n=8) and criminal justice professionals (n=8) about how individuals with dual diagnosis are received in the Criminal Justice System. It was found that criminal justice professionals lack significant knowledge about dual diagnosis, including effective identification and therefore appropriate supports and accommodations. Justice professionals in particular were relatively ill-prepared in dealing effectively with this population. One finding to highlight is that there is misunderstanding between mental health professionals and justice professionals about who ought to take responsibility and accountability for this population.

Ribbed moraines and subglacial geomorphological signatures of interior-sector palaeo-ice sheet dynamics

Transverse, subglacial bedforms (ribbed moraines) occur frequently in southern Keewatin, Nunavut, Canada, where they record a complex glacial history, including shifting centers of ice dispersal and fluctuating basal thermal regimes. Comprehensive mapping and quantitative morphometric analysis of the subglacial bedform archive in this sector reveals that ribbed moraines are spatially clustered by size and assume a broad range of visually distinct forms. Results suggest that end-member morphologies are consistent with a dichotomous polygenetic origin, and that a continuum of forms emerged through subsequent reshaping processes of variable intensity and duration. Translocation of mobile, immobile and quasi-mobile beds throughout the last glacial cycle conditioned the development of a subglacial deforming bed mosaic, and is likely responsible for the patchy zonation of palimpsest and inherited landscape signatures within this former core region of the Laurentide Ice Sheet. Comparison against field evidence collected from central Norway suggests that bedforming processes can be locally mediated by pre-existing topography.

STRUCTURAL ANALYSIS, LAYER THICKNESS MEASUREMENTS AND MINERALOGICAL INVESTIGATION OF THE LARGE INTERIOR LAYERED DEPOSIT WITHIN GANGES CHASMA, VALLES MARINERIS, MARS

The interior layered deposit (ILD) in Ganges Chasma, Valles Marineris, is a 4.25 km high mound that extends approximately 110 km from west to east. The deposition, deformation, and erosion history of the Ganges ILD records aids in identifying the processes that formed and shaped the Chasma. To interpret structural and geomorphic processes acting on the ILD, multiple layer attitudes and layer thickness transects were conducted on the Ganges ILD. Mineralogical data was analyzed to determine correlations between materials and landforms. Layer thickness measurements indicate that the majority of layers are between 0.5 m and 4 m throughout the ILD. Three major benches dominate the Ganges ILD. Layer thicknesses increase at the ILD benches, suggesting that the benches are formed from the gradual thickening of layers. This indicates that the benches are depositional features draping over basement topography. Layer attitudes indicate overall shallow dips generally confined to a North-South direction that locally appear to follow bench topography. Layering is disrupted on a scale of 40 m to 150 m in 12 separate locations throughout the ILD. In all locations, underlying layering is disturbed by overlying folded layers in a trough-like geometry. These features are interpreted to have formed as submarine channels in a lacustrine setting, subsequently infilled by sediments. Subsequently, the channels were eroded to the present topography, resulting in the thin, curved layering observed. Data cannot conclusively support one ILD formation hypothesis, but does indicate that the Ganges ILD postdates Chasma formation. The presence of water altered minerals, consistently thin layering, and layer orientations provide strong evidence that the ILD formed in a lacustrine setting.