Thesis (Ph. D.)--University of Chicago, Dept. of Anthropology, June 1999. / Includes bibliographical references. Also available on the Internet.

Thesis (Ph.D.)--Aberdeen University, 2009. / Title from web page (viewed on Jan. 18, 2010). Includes bibliographical references.

No description available.

Thesis (M.Sc.)--Memorial University of Newfoundland, 2005. / Restricted until May 2006. Bibliography: leaves 184-194.

The North Sakhalin Basin is a polyphase Neogene basin situated on an active strike-slip plate boundary between the Amur and Okhotsk microplates.  This basin contains a sedimentary record of the Amur River, as well as the tectonic processes which have resulted in the formation and deformation of the basin.  I use a multi-disciplinary approach, involving heavy mineral analysis, seismic interpretation and geomorphic observations and analyses, to constrain the evolution of the landscape, sedimentary basins and fluvial systems at this active continental margin. Detrital mineralogy and integrated sediment accumulation rates indicate that the drainage basin of the Amur River has been relatively stable since the Early Miocene, with no evidence for continental-scale drainage capture during this time.  Instead, sediment delivery to the basin has responded to a number of tectonic and climatic processes, most notably the onset of Northern Hemisphere glaciation in the Pliocene and uplift and erosion of the North Sakhalin Basin in the Late Neogene.  By contrast, the Colorado River, which also has a delta on an active strike-slip margin, has been profoundly affected by tectonic processes at the continental margin, resulting in major drainage re-organisation in the Late Neogene. Sediment delivery to the North Sakhalin Basin has been strongly affected by tectonic processes along the Sakhalin-Hokkaido Shear Zone.  The basin underwent a phase of transtension during the Early Miocene (>15 Ma), followed by continued strike-slip offset during the Middle-Late Miocene (15-6.3 Ma), and finally transpression during the Pliocene which is still ongoing today.  The diachronous, northeastward-propagating deformation and uplift of the North Sakhalin Basin (initiated between 6.3-3.6 Ma) is preserved in the geomorphic characteristics of fluvial networks, the first-appearance of recycled deltaic sediments and by onlapping reflector terminations on offshore anticlines.  The landscape of Sakhalin is transient, and continuing to deform in the present day.

Thesis (Ph. D.)--University of Oregon, 2003. / Typescript. Includes vita and abstract. Includes bibliographical references (leaves 689-733). Also available for download via the World Wide Web; free to University of Oregon users.

Thesis (M.A.)--Oregon State University, 2007. / Printout. Includes bibliographical references (leaves 78-82). Also available via the World Wide Web.

For several centuries following their introduction into the British Isles by the Normans, rabbits were farmed on man-made warrens. The right to hunt rabbits during the medieval period was restricted to the highest strata of society and warrens, and rabbit products, carried connotations of wealth and exclusivity. During the post-medieval period, as rabbits became less expensive, their exclusivity declined and access to the species increased across a wider spread of the population. Consequently, later warrens tended to be purely commercial ventures that in places lingered as a form of animal husbandry up until the early twentieth century. Evidence of these warrens is particularly common across England and Wales and typically, although not exclusively, takes the form of pillow mounds, earthworks created to encourage rabbits to burrow. Despite their longevity and high numbers, warrens remain relatively little studied. This thesis investigates surviving warren architecture within south-west England, incorporating archaeological data into a GIS in order to identify the locational, morphological and typological trends of the region’s warrens. It also assesses associations between warrens and other classes of archaeology, notably elite residences and parks, large ecclesiastical institutions and prehistoric earthworks. Doing so allows for a better understanding of warrens’ roles within their immediate environs and of their relationships with other aspects of the human landscape. This study also addresses natural geographical aspects of the landscape in order to determine the principal factors that influenced where warrens were installed. This study investigates documentary reference to warrens as many have not survived within the landscape. Medieval chancery rolls in particular allow for the creation of a national framework of warrening so that the South West can be compared and contrasted to other regions of medieval England. Documentary references, both medieval and post-medieval, to the South West’s warrens allow for the creation of a discrete regional history that defines the context for the establishment of the region’s warren architecture. This study assesses how rabbits were interpreted by medieval society and discusses symbolism, particularly the visual role played by warrens in advertising their owners’ wealth and any possible religious concepts associated with rabbits.

This thesis examines the effects the imposition of Anglo-Norman lordship, following the Anglo-Norman expansion into Wales in the eleventh and twelfth centuries, had upon the landscape of the Welsh border region. In order to achieve this aim this project makes extensive use of digital Geographical Information Systems (GIS) in order to produce a detailed county-wide study of the landscape of post-Conquest Monmouthshire as well as comprehensive case studies of individual Anglo-Norman lordships contained within the boundaries of the county. This thesis also aims to locate its findings within important current debates in historic archaeology about the effects of medieval lordship upon the landscape, on the roles of the physical environment and human agency in the forming of the historic landscape, on the wider role of castles as lordship centres, beyond simple military functionality.

This study investigates the territories of Neapolis and Nola in order to understand what role they played in the economy of their cities and in Campania. It further explores the difficult relationship between mankind and the fragile landscape of Vesuvius, how eruptions changed settlement patterns, exploitation strategies, and how people dealt with other smaller natural disasters that frequently occurred in that area. The thesis is organised in nine chapters, each describing a separate layer of the landscape. The introduction analyses the reasons for the apparent lack of data for the northern slopes of the volcano and further discusses the theoretical issues pertaining to the economy of the countryside. The history chapter lists the major facts of the histoire événementielle and their connection with the landscape’s longterm history. The third chapter studies the features of the static landscape and the exploitation of bedrock resources. Vesuvius is the subject of the fourth chapter, in which are discussed its shape and the eruptions' effects on the static landscape. Chapter five discusses the river Sebethus and how the intermingled action humans and nature created the marshes. Agriculture and animal breeding are analysed in chapter six, settlement patterns in chapter seven, trade in chapter eight. Through archival research and field survey it has been possible to plot 820 sites from ancient southern Campania, 263 of which from the territories of Neapolis and Nola. This evidence has been matched with environmental and archaeological datasets to provide estimates on agricultural produce and population, thus defining surplus and dependance for certain products. The results reveal a high compartmentalisation and degree of dependence of each micro-regional area on the others, for which one can deduce a high specialisation of each economic agent but not necessarily a high productivity for each of its units.