3,499 research outputs found
Sean Rubin: Cook Prize 2025, Silver Medal Acceptance Speech
No full textAuthor and illustrator Sean Rubin gives an acceptance speech for The Iguanodon’s Horn (Clarion/HarperCollins)https://educate.bankstreet.edu/cook/1015/thumbnail.jp
Appropriations of Irish drama by modern Korean nationalist theatre : a focus on the influence of Sean O’Casey in a colonial context
No full textMy thesis explores how a translated author on the periphery of the host culture’s
translated repertoire can be at once subversive and innovative on the colonial scene,
using as an example the case of Sean O’Casey in colonial Korea. It explores the
importation of Irish drama in modern Korean theatre during the colonial period and
examines the appropriations of O’Casey’s plays by a central Korean playwright, Yu
Chi-jin, in creating his own plays. Under Japanese colonial rule in the early twentieth
century, intellectuals perceived the supreme task for the Korean people to be the
recovery of national sovereignty and independence. The modern Korean theatre
movement which rose among Korean intellectuals and dramatists during the colonial
period was to play a major part in this task. The ultimate goal of this movement was
to establish a modern national theatre promoting Korean culture and educating the
people, thereby recovering national independence. As their modernised dramatic
polysystem was still "young", Korean intellectuals and dramatists who were
involved in the theatre movement had to borrow dramatic models from other
countries. One of the models they chose was Irish playwrights, especially those who
were involved in the Irish dramatic movement. They published or staged the works
of W.B. Yeats, Lord Dunsany [Edward John Moreton Drax Plunkett], Augusta
Gregory, J.M. Synge, St. J. Ervine, T.C. Murray and Sean O'Casey. Although
O'Casey was considered an important dramatist in the Irish dramatic movement, he
was a playwright on the periphery in the list of translated Irish dramatists in Korea
due to the colonisers’ censorship. However, he remained as a subversive and
innovative playwright on the colonial scene by virtue of being appropriated by Yu
Chi-jin who used O’Casey’s plays as models when creating his own works. In
discussing the subject matter of my thesis, I use Even Zohar’s polysystems theory as
a starting point in looking at ideological issues surrounding translation and extend
the discussion to offer a postcolonial perspective. While most translation in a
colonial context was considered as "an expression of the cultural power of the
colonisers," my thesis shifts the focus to translation as an expression of the cultural
power of the colonised. I explore how the colonised uses another colonised culture to
subvert the colonisers’ power
Downgoing plate topography stopped rupture in the A.D. 2005 Sumatra earthquake
No full textEarthquakes in subduction zones rupture the plate boundary fault in discrete segments. One factor that may control this segmentation is topography on the downgoing plate, although it is controversial whether this is by weakening or strengthening of the fault. We use multichannel seismic and gravity data to map the top of the downgoing oceanic crust offshore central Sumatra, Indonesia. Our survey spans a complex segment boundary zone between the southern termination of the Mw = 8.7, A.D. 2005 Simeulue-Nias earthquake, and the northern termination of a major 1797 earthquake that was partly filled by an Mw = 7.7 event in 1935. We identify an isolated 3 km basement high at the northern edge of this zone, close to the 2005 slip termination. The high probably originated at the Wharton fossil ridge, and is almost aseismic in both local and global data sets, suggesting that while the region around it may be weakened by fracturing and fluids, the basement high locally strengthens the plate boundary, stopping rupture propagation
Interview with Canadian teacher and author Dr. Sean Steel
No full textRozhovor Dr. Zuzany Svobodové s kanadským učitelem a publicistou Dr. Seanem Steelem.Interview with Canadian teacher and author Dr. Sean Steel
Unlocking a global ocean mixing dataset: toward standardization of seismic-derived ocean mixing rates
No full textTurbulent mixing is vital for water transformation in the ocean and sustains the global thermohaline circulation. Despite decades of global observations using different platforms, our understanding of ocean turbulence is still limited. More observations are needed to better characterize the spatiotemporal distribution of mixing to reduce uncertainties in climate models. Marine seismic reflection surveys are an untapped data resource for high-resolution ocean turbulence observation. Turbulent mixing can be extracted from seismic data through horizontal internal wave slope spectra. However, to date, a standardized approach to prepare seismic data for this spectral analysis is still lacking, leading to insufficient consideration of the impact of noise on the resulting diffusivities. To address these issues, we perform a full-wavefield synthetic modeling and processing to reveal noise-induced overestimation of diffusivities. We further propose a widely applicable workflow and apply it to three field seismic surveys with increasing noise levels conducted in regions of different turbulence environments: ocean ridges, open ocean interior, and continental slope. The derived diffusivities are bench-marked against direct measurements around the region to show the fidelity of this seismic method. The extended observation records by seismic data across the Kauai Channel and away from the Mid-Atlantic Ridges reveal the importance of topography in modifying the propagation of internal tides and the distribution of turbulent mixing in both near and far fields. Our proposed workflow marks a key advancement toward standardization of seismic-derived ocean mixing rates and holds the potential to unlock massive marine seismic reflection datasets worldwide for ocean mixing characterization.</p
Basement and Regional Structure Along Strike of the Queen Charlotte Fault in the Context of Modern and Historical Earthquake Ruptures
No full textAbstract The Queen Charlotte fault (QCF) is a dextral transform system locate
An Abrupt Transition in the Mechanical Response of the Upper Crust to Transpression along the Queen Charlotte Fault
No full textThe Queen Charlotte Fault (QCF) is a major strike-slip fault that forms the boundary between the Pacific and North American plates from 51 degrees to 58 degrees N. Near 53.2 degrees N, the angle of oblique convergence predicted by the Mid-Ocean Ridge VELocity (MORVEL) interplate pole of rotation decreases from > 15 degrees in the south to < 15 degrees in the north. South of 53.2 degrees N, the convergent component of plate motion results in the formation of a 40 km wide terrace on the Pacific plate west of QCF and earthquakes with thrust mechanisms (including the 2012 Haida Gwaii earthquake sequence) are observed. North of 53.2 degrees N, in the primary rupture zone of the M 8.1 strike-slip earthquake of 1949, the linear terrace disappears, and topography of the continental slope west of the QCF is characterized by a complex pattern of ridges and basins that trend obliquely to the primary trace of the QCF. Deformation within the Pacific plate appears to occur primarily through strike-slip faulting with a minor thrust component on secondary synthetic faults. The orientations of these secondary faults, as determined from seismic reflection and bathymetric data, are consistent with the reactivation of faults originally formed as ridge-parallel normal faults and as thrust faults formed parallel to the QCF south of the bend at 53.2 degrees N and subsequently translated to the north. We suggest that an oblique convergence angle of 15 degrees represents a critical threshold separating distinct crustal responses to transpression. This result is consistent with theoretical and analog strain models of transpressive plate boundaries. The sharpness of this transition along the QCF, in contrast to purely continental transform boundaries, may be facilitated by the relatively simple structure of oceanic crust and the presence of pre-existing, optimally oriented faults in the young Pacific plate.National Science Foundation (NSF) EAR-9219870, EAR-9527011Institute for Geophysic
RV Sonne Cruise 198-2, 18 Jun-01 Aug 2008. Merak, Indonesia - Merak, Indonesia
No full textAll plate boundaries are divided into segments - pieces of fault that are distinct from one another, either separated by gaps or with different orientations. The maximum size of an earthquake on a fault system is controlled by the degree to which the propagating rupture can cross the boundaries between such segments. A large earthquake may rupture a whole segment of plate boundary, but a great earthquake usually ruptures more than one segment at once.Earthquakes offshore of Sumatra on December 26 2004 (MW=9.3) and March 28 2005 (MW=8.7) ruptured, respectively, 1200-1300 km and 300-400 km of the subduction boundary between the Indian-Australian plate and the Burman and Sumatra blocks. Rupture in the 2004 event started at the southern end of the fault segment, and propagated northwards. The observation that the slip did not propagate significantly southwards in December 2004, even though the magnitude of slip was high at the southern end of the rupture strongly suggests a barrier at that place. Maximum slip in the March 2005 earthquake occurred within ~100 km of the barrier between the 2004 and 2005 ruptures, confirming both the physical importance of the barrier, and the loading of the March 2005 rupture zone by the December 2004 earthquake. Cruise SO198-2, from Merak to Merak between 18 June and 01 August 2008 is the second of three cruises, funded by the Natural Environment Research Council (NERC), which will form a coherent set of geophysical observations in the source regions of the 2004 and 2005 great Sumatra earthquakes. This cruise collected seismic reflection (MCS) profiles at SB1 and SB2 with the following objectives:1. To image the geometry and nature of the downgoing slab from the trench to 30-40 km depth within the forearc2. To image faults within the over-riding plate responsible for the development of the accretionary wedge3. To provide a set of shots that will calibrate the array of ocean-bottom seismometers deployed on cruise SO198-1, and be recorded by the land seismometer array established by a different part of the consortium.Cruise SO198-2 also included nine days of ship time funded by the United States National Science Foundation to investigators from the University of Texas Institute for Geophysics (UTIG). This allied study targeted the subject of rupture pathways, with a focus was on how the earthquake rupture propagates updip through the accretionary prism to ultimately move the seafloor and create the tsunami.Approximately 5000km of multichannel seismic reflection data were collected during the cruise, as well as continuous recording of gravity, magnetics, Parasound and swath bathymetry data while in the permitted area
Recall this Book 60: Sean Hill on Bodies in Space and Time
No full textElizabeth is joined by Elizabeth Bradfield, poet, naturalist and professor of poetry at Brandeis, in a conversation with the poet Sean Hill, author of Blood Ties and Brown Liquor (2008) and Dangerous Goods (2014). Sean read his Musica Universalis in Fairbanks, (it appeared in the Alaska Quarterly Review) and then, like someone seated in an archive turning over the pages of aged and delicate documents, unfolded his ideas about birds, borders, houses and who was here before me
Sean of the South
No full textRecording of the radio show The North Avenue Lounge broadcast May 6, 2019 on WREK Atlanta, 91.1FMShannon speaks with prolific author, storyteller, blogger, and musician, Sean Dietrich, aka Sean of the South. Sean speaks about growing up as an underestimated kid, his early influencers, how community college change his life, and talks about writing process. In the final segments, Sean reads from his daily blog and we sample his podcast performances
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