Scenic Design of James and the Giant Peach

The purpose of this thesis is to provide research, supporting paperwork, production photographs and other materials that document the scenic design process for James and the Giant Peach at Adventure Theatre MTC. This thesis contains the following: concept statement, scenic research images collected to express location, and the emotional/ intellectual/ psychological landscapes for the production, preliminary sketches, photographs of the ¼” scale model, drafting plates and supporting paint elevations to communicate the design, prop list and accompanying research, archival production photographs to document the completed design, and finally periodical reviews of the show.

Troilus and Cressida - A Scenic Design

The purpose of this thesis is to provide research, supporting paperwork, production photographs, and other materials that document the scenic design process for the production of William Shakespeare’s Troilus & Cressida by the University of Maryland – College Park, School of Theater, Dance, and Performance Studies. This thesis contains the following: scenic research images collected to express period, location, and emotional/intellectual landscapes to the production team; preliminary sketches; photographs of the ¼” scale model; a full set of drafting plates and paint elevations used to communicate the design to the technical director and paint charge; a unit list naming each scenic element; a props list and research book to detail each hand prop, furniture piece and consumable to the prop master; and, lastly, archival production photographs to document the completed design.

Intimate Apparel: A Lighting Design

The purpose of this thesis is to provide research, supporting paperwork and production photographs that document the lighting design for the University of Maryland - College Park, School of Theatre, Dance, and Performance Studies’ production of Intimate Apparel, by Lynn Nottage. This thesis contains the following: a design concept statement, research images collected to develop and visually communicate ideas about color, texture, intensity, form, composition and mood to the production team; preliminary and final organization of desired equipment to execute the lighting design; a full set of drafting plates and supplementary paperwork used to communicate the organization and placement of lighting equipment to the master electrician; and magic sheets and cue lists used as organizational tools for the lighting designer during the tech process. Archival production photographs are included as documentation of the completed design.

CONSTRAINTS ON THE LITHOSPHERIC STRUCTURE OF MID OCEAN RIDGES FROM OCEANIC CORE COMPLEX MORPHOLOGY

The Mid-oceanic ridge system is a feature unique to Earth. It is one of the fundamental components of plate tectonics and reflects interior processes of mantle convection within the Earth. The thermal structure beneath the mid-ocean ridges has been the subject of several modeling studies. It is expected that the elastic thickness of the lithosphere is larger near the transform faults that bound mid-ocean ridge segments. Oceanic core complexes (OCCs), which are generally thought to result from long-lived fault slip and elastic flexure, have a shape that is sensitive to elastic thickness. By modeling the shape of OCCs emplaced along a ridge segment, it is possible to constraint elastic thickness and therefore the thermal structure of the plate and how it varies along-axis. This thesis builds upon previous studies that utilize thin plate flexure to reproduce the shape of OCCs. I compare OCC shape to a suite of models in which elastic thickness, fault dip, fault heave, crustal thickness, and axial infill are systematically varied. Using a grid search, I constrain the parameters that best reproduce the bathymetry and/or the slope of ten candidate OCCs identified along the 12°—15°N segment of the Mid-Atlantic Ridge. The lithospheric elastic thicknesses that explains these OCCs is thinner than previous investigators suggested and the fault planes dip more shallowly in the subsurface, although at an angle compatible with Anderson’s theory of faulting. No relationships between model parameters and an oceanic core complexes location within a segment are identified with the exception that the OCCs located less than 20km from a transform fault have slightly larger elastic thickness than OCCs in the middle of the ridge segment.