Thesis (M.A.)--Ohio University, August, 2005. / Title from PDF t.p. Includes bibliographical references (p. 56-60)

The need and longing to connect to another is a fundamental desire of the human heart, enforcing a sense of movement toward social and personal security and, moreover, the future. Yet it is paradoxical that, where people are the most closely crowded together, feelings of alienation and loneliness are often the greatest. We live in times of busy isolation, on streets where we dont know our neighbours, in societies where our lives are lived behind closed doors. As the global village grows, our personal worlds shrink, both by circumstance and by choice. Our innate, gregarious nature faces its greatest challenge, or ultimate defeat.<p> The story of my hometown, New Waterford, is a substantial element in the story of my life as well as my art. The woodcuts and many of the paintings in the exhibition, Slag, are documentations of this place, its inhabitants and their way of life. It is a town with a unique character resulting from the circumstances surrounding its relationship to coalmininga town that is withering away now that the mines are gone. Other paintings in the exhibition depict people and spaces from other places that I have lived. Though the environments change, there are similarities in the pathos of the human subjects that remain constant. In my work, whether I am depicting the inhabitants of a hollowed out town or the solitary subway commuter, they are united as those things that have been lost or left behind in the name of progressthe leftovers and waste: the slag.

The need and longing to connect to another is a fundamental desire of the human heart, enforcing a sense of movement toward social and personal security and, moreover, the future. Yet it is paradoxical that, where people are the most closely crowded together, feelings of alienation and loneliness are often the greatest. We live in times of busy isolation, on streets where we dont know our neighbours, in societies where our lives are lived behind closed doors. As the global village grows, our personal worlds shrink, both by circumstance and by choice. Our innate, gregarious nature faces its greatest challenge, or ultimate defeat.<p> The story of my hometown, New Waterford, is a substantial element in the story of my life as well as my art. The woodcuts and many of the paintings in the exhibition, Slag, are documentations of this place, its inhabitants and their way of life. It is a town with a unique character resulting from the circumstances surrounding its relationship to coalmininga town that is withering away now that the mines are gone. Other paintings in the exhibition depict people and spaces from other places that I have lived. Though the environments change, there are similarities in the pathos of the human subjects that remain constant. In my work, whether I am depicting the inhabitants of a hollowed out town or the solitary subway commuter, they are united as those things that have been lost or left behind in the name of progressthe leftovers and waste: the slag.

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Over the course of the Civil War the small community of Waterford, Virginia maintained Unionist sentiments regardless of being a part of the Confederate States of America. These sentiments were rooted in loyalty to the United States, their ostracization from southern culture, and their Quaker faith. In particular, the women of this community became exceptionally vocal with their displeasure with the Confederacy. In the last year of the Civil War they made the deliberate choice to publicly assert their Unionist convictions with their newspaper The Waterford News. The experience of this community, particularly that of its female residents, was influenced by the variety of identities that they held. The women of Waterford were Quakers, female, southern, unionist and editors/producers of a newspaper. The community of Waterford, Virginia was placed in the margins of Southern society because of the cultural differences rooted in their Quaker faith. The Civil War created a chaotic historical moment where those on the margins of society experienced it differently than those around them. By examining their identities as newspaper producers, as citizens of different groups, and within their interpersonal relationships the reality of how war is lived is brought to light. All of these factors reveal how war is lived, and how lives are manipulated to fit within times of chaos. Motivation matters. / Master of Arts / Over the course of the Civil War the small community of Waterford, Virginia maintained loyalty to the United States rather than support the Confederate cause. These sentiments were rooted in patriotism to the United States, their exclusion from southern culture, and their Quaker faith. Women of this community were extremely vocal with their anger over Confederate occupation. In the last year of the Civil War they made the choice to publicly assert their convictions with their newspaper The Waterford News. The experience of this community, particularly that of its female residents, was influenced by the variety of identities that they held. The women of Waterford were Quakers, female, southern, unionist and editors/producers of a newspaper. The community of Waterford, Virginia was excluded from the rest of Virginian society because of their Quaker faith. The Civil War was a traumatic historical event where communities like Waterford experienced it differently than the majority around them. By studying the identities of these women as newspaper producers, as citizens of different groups, and within their interpersonal relationships the reality of how war is lived is revealed. All of these factors reveal how war is lived.

A dissertation submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of requirements for the degree of Master of Science. Johannesburg, 2014. / The Karasburg Basin is situated in southern Namibia and preserves a heterogeneous succession of Karoo Supergroup strata up to 1000m thick. The uppermost preserved succession in this basin is the Amibberg Formation which is 250m thick and consists of intervals of sandstone, siltstone and mudstone. This study uses facies analysis, sequence stratigraphy and petrography to determine the palaeogeography and provenance for the Amibberg Formation. This is then used to establish environmental variability across the Karasburg – Aranos – Main Karoo basins and to define an equivalent of the Amibberg Formation in the Main Karoo Basin. Detailed stratigraphic logging of five outcrop localities has led to the identification of seven distinct lithofacies and two dominant ichnofacies (Cruziana and Skolithos). These lithofacies include: 1) Massive, laminated and bioturbated mudstones interpreted as offshore deposits (OS); 2) Bioturbated siltstones and sandstones which are representative of offshore-transitional environments (OST); 3) Interbedded sandstones and siltstones also interpreted as offshore-transitional deposits (OST) and generated by river-fed hyperpycnal plumes; 4) Sharp based, massive sandstones interpreted as being deposited on the distal lower shoreface (dLSF); 5) Non-amalgamated hummocky cross-stratified (HCS) and wave rippled sandstones interpreted as distal lower shoreface deposits (dLSF); 6) Amalgamated HCS and wave rippled sandstones interpreted as proximal lower shoreface deposits (pLSF); and 7) Soft-sediment deformed (SSD) sandstones and siltstones occurring in close juxtaposition with dLSF and pLSF deposits. The vertical arrangement of these lithofacies shows a general coarsening and shallowing upward trend. Overall the rocks of the Amibberg Formation consist of wave-dominated shoreface deposits with significant influence by tidal processes. Petrographically, the sandstone samples fall into the class of quartz and feldspathic wackes and are sourced from craton interior provenances. Geochemical analysis of mudstones and nodules indicate high levels of microbial activity under predominantly oxic conditions during the deposition of the Amibberg Formation. Five poorly defined 4th order T-R cycles are observable within the strata of the Amibberg Formation. Large regressive intervals are capped by thin transgressive tracts and these cycles are interpreted to have formed due to eustatic processes. Overall, the Amibberg Formation represents a regressive shoreline. iii Based on the mean palaeocurrent vectors a NNE-SSW palaeoshoreline orientation is deduced and the shoreface must have occupied a palaeohigh on the northern side of the western Cargonian Highlands. This emergent highland acted as an extensive headland and assisted in the connectivity of the Karasburg and Aranos basins, with partial connectivity with the Main Karoo Basin during the Early Permian. Based on this study, the Amibberg Formation is considered an equivalent of the Waterford Formation in the Main Karoo Basin based on similar: stratigraphic position; thickness; sedimentary structures; trace fossil assemblages and stacking patterns.