Cette recherche porte sur l'étude de la relation entre les changements environnementaux et culturels dans le Bas-Arctique. Une approche multidisciplinaire en géographie physique et géographie culturelle a été adoptée afin de comprendre le contexte dans lequel le site archéologique IbGk-3, situé sur l'île Drayton au sud d'Inukjuak, a été occupé. Le site est composé de vestiges de maisons semi-souterraines. Le paysage de l'île, dont plusieurs témoins du passage des glaciers sont visibles, est en constant changement, entre autres en raison du relèvement isostatique et du retrait marin qui y est associé. Les conditions environnementales clémentes d'il y a 960 ans cal. BP auront permis l'entourbement de certaines terrasses. Le choix de l'emplacement du site aurait été influencé par la disponibilité des ressources animales et des matériaux de construction des maisons tels le bois et la tourbe, mais également par la géomorphologie du site. Le savoir traditionnel inuit a permis entre autres de proposer un modèle d'aménagement intérieur des maisons semi-souterraines lequel est formé d'un tunnel d'entrée, d'une zone de couchage surélevée et d'un côté spécifique pour préparer la nourriture.

In the sixteenth century, the cartographic revolution was rapidly changing the experience of everyday life in England. Modes of thinking and inhabiting space (such as astronomy, trigonometry, surveying, and cartography) were advanced and refined, and in England, the map went from rarity to ubiquity in less than seventy years. Navigating Time explores how literary strategies changed in response to this rapid shift in the technology of spatial representation. I consider four epics, the epic being the early modern genre most overtly invested in matters of empire (and thus, in matters of space and history). Building on the insights of the spatial turn in the humanities, I argue that the epic offers a radical critique of the technological innovations of the cartographic revolution and the menace those innovations posed. Alongside this critique, the early modern epic outlined a new poetics centered on navigation. Epics by Holinshed, Spenser, Drayton, and Milton sought to encompass the representational possibilities of the map, but also to highlight and exceed the map's narrative insufficiency. Holinshed's Chronicles reforms the topography of the city, converting its streets and alleys into historical texts and presenting historiography and mapping as competing interpretive frameworks for urban space. The Faerie Queene redefines genre as the conduct of bodies in space, making it thus impossible to fix Faeryland as a mappable terrain, and asserting the continuous interpretation required by allegory against the compression imposed by the map. Drayton's Poly-Olbion seems at first to be a verbal map of Britain, but the poem quietly insists on the power of literature not to mimic but rather to supplant the world it describes, becoming the terrain a map can only represent. Finally, Milton's Paradise Lost creates a form of navigating without a destination, by transforming history into a geographic expanse that cannot be mapped, only wandered.

Diss. Uppsala : Univ., 2003.

Honors Project--Smith College, Northampton, Mass., 2009. / Includes bibliographical references (p. 101-106).

No description available.

This dissertation explores how the mythological heroines from Ovid‘s Heroides and Metamorphoses were cataloged, conflated, reconceived, and recontextualized in vernacular literature; in so doing, it joins considerations of voice, authority, and gender with reflections on Tudor technologies of textual reproduction and ideas about the book. In the late medieval and Renaissance eras, Ovid‘s poetry stimulated the imaginations of authors ranging from Geoffrey Chaucer and John Gower to Isabella Whitney, William Shakespeare, and Michael Drayton. Ovid‘s characteristic bookishness—his interest in textual revision and his thematization of the physicality and malleability of art in its physical environments—was not lost upon these postclassical interpreters who engaged with his polysemous cast of female characters. His numerous English protégés replicated and expanded Ovid‘s metatextual concerns by reading and rewriting his metamorphic poetry in light of the metaphors through which they understood both established networks of scribal dissemination and emergent modes of printed book production. My study of Greco-Roman tradition and English bibliofictions (or fictive representations of books, their life cycles, and the communication circuits in which they operate) melds literary analysis with the theoretical concerns of book history by focusing on intersections and interactions between physical, metaphorical, and imaginary books. I posit the Tudor book as a site of complex cultural and literary negotiations between real and inscribed, historical and fictional readers, editors, commentators, and authors, and, as my discussion unfolds, I combine bibliographical, historical, and literary perspectives as a means to understanding both the reception of Ovidian poetry in English literature and Ovid‘s place in the history of books. This dissertation thus contributes to a growing body of book history criticism while also modeling a bibliographically enriched approach to the study of late medieval and Renaissance intertextuality.

This dissertation explores how the mythological heroines from Ovid‘s Heroides and Metamorphoses were cataloged, conflated, reconceived, and recontextualized in vernacular literature; in so doing, it joins considerations of voice, authority, and gender with reflections on Tudor technologies of textual reproduction and ideas about the book. In the late medieval and Renaissance eras, Ovid‘s poetry stimulated the imaginations of authors ranging from Geoffrey Chaucer and John Gower to Isabella Whitney, William Shakespeare, and Michael Drayton. Ovid‘s characteristic bookishness—his interest in textual revision and his thematization of the physicality and malleability of art in its physical environments—was not lost upon these postclassical interpreters who engaged with his polysemous cast of female characters. His numerous English protégés replicated and expanded Ovid‘s metatextual concerns by reading and rewriting his metamorphic poetry in light of the metaphors through which they understood both established networks of scribal dissemination and emergent modes of printed book production. My study of Greco-Roman tradition and English bibliofictions (or fictive representations of books, their life cycles, and the communication circuits in which they operate) melds literary analysis with the theoretical concerns of book history by focusing on intersections and interactions between physical, metaphorical, and imaginary books. I posit the Tudor book as a site of complex cultural and literary negotiations between real and inscribed, historical and fictional readers, editors, commentators, and authors, and, as my discussion unfolds, I combine bibliographical, historical, and literary perspectives as a means to understanding both the reception of Ovidian poetry in English literature and Ovid‘s place in the history of books. This dissertation thus contributes to a growing body of book history criticism while also modeling a bibliographically enriched approach to the study of late medieval and Renaissance intertextuality.

In this thesis, I constrain rupture scenarios of active crustal faults in the southern Strait of Georgia and Boundary Bay in order to assess their tsunamigenic potential. The NW-SE-trending Drayton Harbor, Birch Bay, and Sandy Point faults had been previously identified on the southern side of Boundary Bay from aeromagnetic, LiDAR, and paleoseismic data; all show evidence of abrupt vertical Holocene displacements. South of Boundary Bay, the E-W-trending Skipjack Island fault zone was recently mapped on the basis of multibeam sonar imagery and seismic reflection data, with evidence for Holocene offsets of the seafloor and subsurface sediments. In addition, the Fraser River Delta fault had been hypothesized on the basis of a line of pockmarks and fluid seeps. Since these faults have only been recently mapped and identified as active, there is little information available on their structure, rupture style, and past large earthquakes. This makes it difficult to constrain rupture models to predict how fault slip could displace the seafloor during a large earthquake, for input to tsunami models. I analyzed relocated earthquake hypocentres, earthquake mechanisms, bathymetry, topography, and aeromagnetic, seismic reflection, and magnetotelluric data, to constrain the location, strike, dip, and rupture width of each fault. Correlations between datasets enabled mapping of northwestward extensions of the Sandy Point and Birch Bay faults, as well as delineating the previously unmapped Fraser River Delta fault. These offshore faults appear to be associated with infilled basement valleys in the subsurface, perhaps due to differential glacial erosion of weakened fault zone material. The Drayton Harbor fault could not be definitively mapped across Boundary Bay, so was excluded from the rupture modelling. Rupture styles were constrained using a combination of earthquake mechanisms, stress orientations, other evidence of regional compression, and vertical paleoseismic offsets. Where possible, paleoseismic displacements in past earthquakes were used to constrain the amount of fault slip for scenario earthquakes; empirical relations between fault slip and fault length or area were used to estimate displacements for the Skipjack Island and Fraser River Delta faults. The Birch Bay, Sandy Point, Skipjack Island, and Fraser River Delta faults all pose a significant tsunami risk to communities surrounding the southern Strait of Georgia and Boundary Bay. Considering both the originally mapped and extended lengths, the Birch Bay and Sandy Point faults could rupture in reverse-faulting earthquakes up to Mw 6.7-7.4 and 6.8-7.5, respectively, with seafloor uplift up to 2-2.5 m triggering damaging tsunami waves (up to at least 2.5 m) that could arrive onshore with little to no warning after the shaking begins. Similarly, the Fraser River Delta fault could host reverse or dextral-reverse slip earthquakes up to Mw 7.0-7.6, with seafloor uplift of 0.6-3.5 m. Ruptures on the Skipjack Island fault would likely have a larger strike-slip component; earthquakes of Mw 6.9-7.3 produce modelled seafloor uplift of 0.5-1.9 m. These results suggest that large tsunamigenic earthquakes on crustal faults in the southern Strait of Georgia should be included in future seismic and tsunami hazard assessments on both sides of the international border. / Graduate

No description available.