997 resultados para Burke, Kenneth, 1897-1993


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Mode of access: Internet.

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El trabajo pretende brindar una aproximación crítica analítica a aquella propositiva histórica familiar dentro de la extensa literatura sobre los orígenes de la Guerra Fría. Reconociendo de antemano que el escenario de la Guerra Fría no fue necesariamente el efecto de una amenaza inminente.

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We use benthic foraminifers to reconstruct the Neogene paleobathymetric history of the Marion Plateau, Queensland Plateau, Townsville Trough, and Queensland Trough on the northeastern Australian margin (Ocean Drilling Program Leg 133). Western Queensland Plateau Site 811/825 (present depth, ~938 m) deepened from the neritic zone (0-200 m) to the upper bathyal zone (200-600 m) during the middle Miocene (~13-14 Ma), with further deepening into the middle bathyal zone (600-1000 m) occurring during the late Miocene (~7 Ma). A depth transect across the southern Queensland Plateau shows that deepening from the outer neritic zone (100-200 m) to the upper bathyal zone began during the latest Miocene (~6 Ma) at the deepest location (Site 813, present depth, 539.1 m), whereas the shallower Sites 812 and 814 (present depths, 461.6 and 520.4 m, respectively) deepened during the late Pliocene (~2.7 and ~2.9 Ma). At Marion Plateau Site 815 (present depth, 465.5 m), water depth increased during the late Miocene (~6.7 Ma) from the outer neritic to the upper bathyal zone. Nearby Site 816 (present water depth, 437.3 m) contains Pliocene upper bathyal assemblages that directly overlie middle Miocene shallow neritic deposits; the timing of the deepening is uncertain because of a late Miocene hiatus. On the northern slope of the Townsville Trough (Site 817, present depth, 1015.8 m), benthic foraminifers and sponge spicules indicate deepening from the lower upper bathyal (400-600 m) to the middle bathyal zone in the late Miocene (by ~6.8 Ma). Benthic foraminiferal faunas at nearby Site 818 (present water depth, 752.1 m) do not show evidence of paleobathymetric change; however, a late Pliocene (~2-3 Ma) increase in downslope transport may have been related to the drowning of the Queensland Plateau. Site 822 (present depth, 955.2 m), at the base of the Great Barrier Reef slope, deepened from the upper bathyal to the middle bathyal zone during the late Pliocene (by ~2.3 Ma). Queensland Trough Site 823 (present depth, 1638.4 m) deepened from the middle bathyal to the lower bathyal (1000-2000 m) zone during the late Miocene (~6.5 Ma). Benthic foraminiferal faunal changes at these Leg 133 sites indicate that rapid deepening occurred during the middle Miocene (~13-14 Ma), late Miocene (6-7 Ma), and late Pliocene (2-3 Ma) along the northeastern Australian margin.

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Top Row: Nick Watson, Kevin Sullivan, Ian Forsyth, Theo Molla

Middle Row: David Barnett, Matt Schroeder, Ryan Burt, Kenneth Kozloff, Michael Mahler, Don MacDonald

Front Row: head coach Ron Warhurst, Kris Eggle, Jay Schemanske, Mark Kwiatkowski, Jon Aubuchon

Not pictured: Jim Finlayson, Scott MacDonald, Andy Hayes, Robert Lee, Shawn MacKay, Daniel Shea, Chad Tibbetts

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Back Row: Nick Parsons, Kevin Sullivan, Ian Forsyth, Theo Molla

Middle Row: David Barnett, Matt Schroeder, Ryan Burt, Kenneth Kozloff, Michael Mahler, Don MacDonald

Front Row: head coach Ron Warhurst, Kris Eggle, Jay Schemanske, Mark Kwiatkowski, Jon Aubuchon

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The rhetoric of the pedagogic discourses of landscape architectural students and interior design students is described as part of a doctoral study undertaken to document practices and orientations prior to cross-disciplinary collaboration. We draw on the theoretical framework of Basil Bernstein, an educational sociologist, and the rhetorical method of Kenneth Burke, a literary dramatist, to study the grammars of ‘landscape’ representation employed within these disciplinary examples. We investigate how prepared final year students are for working in a cross-disciplinary manner. The discursive interactions of their work, as illustrated by four examples of drawn images and written text, are described. Our findings suggest that we need to concern ourselves aspects of our pedagogic discourse that brings uniqueness and value to our disciplines ,as well as that shared discourses between disciplines.

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This brief paper outlines some of the early work undertaken in Indigenous postgraduate activism in Australia. In particular, the work undertaken in the lead up to the 'Project into the Barriers which Indigenous Students must Overcome in Postgraduate Studies'.

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Louis Nowra wrote 'Radiance' especially for the three actors who performed it in the play’s premier season at Belvoir Street Theatre in September 1993. And the Currency Press playscript / programme produced for that season foregrounds these three performers – Rachael Maza, Lydia Miller and Rhoda Roberts – in such a way that the usual distinction between dramatis personae and the actors who play them is considerably diminished. Both the blurb on the back cover and Nowra’s introduction emphasise this special relationship between text and actors, but it is the front cover shot which particularly reflects the conjunction between the two. Rather than depicting a scene from performance, or a ‘graphic’ suggesting something of the play’s thematic content, the front cover of Radiance features the three actors in a posed promotional shot. Arms joined warmly, lovingly, about each other’s waist, bodies turned away from but faces towards the camera, it is the actors we see, not their characters. It’s a very joyful image; they’re positively beaming. Radiant. They look as if they could really be the three half-sisters they portray, except that such moments of blithe sorority are just about non-existent in the play.