When Stories Travel

Adapting fiction into film is, as author Cristina Della Coletta asserts, a transformative encounter that takes place not just across media but across different cultures. In this book, Della Coletta explores what it means when the translation of fiction into film involves writers, directors, and audiences who belong to national, historical, and cultural formations different from that of the adapted work. In particular, Della Coletta examines narratives and films belonging to Italian, North American, French, and Argentine cultures. These include Luchino Visconti’s adaptation of James M. Cain’s The Postman Always Rings Twice, Federico Fellini’s version of Edgar Allan Poe’s story “Never Bet the Devil Your Head,” Alain Corneau’s film based on Antonio Tabucchi’s Notturno indiano, and Bernardo Bertolucci’s take on Jorge Luis Borges’s “Tema del traidor y del héroe.” In her framework for analyzing these cross-cultural film adaptations, Della Coletta borrows from the philosophical hermeneutics of Hans-Georg Gadamer and calls for a “hermeneutics of estrangement,” a practice of mediation and adaptation that defines cultures, nations, selfhoods, and their aesthetic achievements in terms of their transformative encounters. Stories travel to unexpected and interesting places when adapted into film by people of diverse cultures. While the intended meaning of the author may not be perfectly reproduced, it still holds, Della Coletta argues, an equally valid and important intellectual claim upon its interpreters. With a firm grasp on the latest developments in adaptation theory, Della Coletta invites scholars of media studies, cultural history, comparative literature, and adaptation studies to deepen their understanding of this critical encounter between texts, writers, readers, and cultural movements

Ereignis y Différance. Derrida, intérprete de Heidegger.

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Fabric and clay activity in soil water retention behaviour

Modelling the water retention behaviour requires proper understanding of all the processes which affect the amount of water stored in the pore network, depending on the soil state and the soil history. Traditionally, in many applications a single water content – suction curve is used. This approach limits the applicability of the retention data to practical cases, especially when fine grain soils are dealt with, when the deformability and activity of the clay fraction significantly affect the interaction with water. On the other side, water retention is being recognised more and more as a fundamental information in the description of the mechanical response of the soil, as it provides the key connection to the partial volumetric strains in a deformation process. With reference to the work performed at the Politecnico di Milano in the last years, a contribution on the understanding and modelling the coupled water retention- mechanical response in deformable soils is presented. The contribution aims to: (i) summarise the mechanisms which contribute to water retention; (ii) point out the role played by an evolving fabric and the fluid properties on water retention; and (iii) provide an overview on some of the consequences of evolving water retention properties on the mechanical behaviour

Derrida: un pensamiento del exilio

Aunque en sus escritos Derrida no utilice el término «exilio», la experiencia de un extrañamiento radical, esto es, de una alteridad insoslayable que cohabita internamente con toda supuesta identidad, no deja de recorrer de arriba abajo su vida y su pensamiento haciendo así de este un pensamiento afirmativo, abierto a lo por venir y capaz de pensar de otro modo lo político.Although in his writings Derrida does not use the term ‘exile’, the experience of a radical estrangement, that is, of an inescapable alterity which cohabits inside any supposed identity, permeates his life and thinking, thus making this latter a form of affirmative thinking, open to what is ‘to come’, and capable of giving a new slant to that which is political

Geological constraints for a conceptual evolutionary model of the slope deformations affecting Mt. Nuovo at Ischia (Italy)

ischia island was the scenario of several Holocene slope in- stability events occurred at different scales, from shallow mass movements, triggered by meteo-climatic forcing, up to massive rock slope failures such as large debris avalanches these last ones related to the volcano-tectonic dynamics of a resurgent caldera. the present study focuses on the gravitational deformation that in- volves Mt. nuovo, located in the western portion of Mt. epomeo resurgent block. a high-resolution engineering-geological model was reconstructed according to a multi-modelling approach sup- ported by field geo-structural evidences and constrained by pas- sive seismic investigations. it revealed a complex morpho-struc- tural setting and led to the identification of a multiple compound mechanism, involving a rock mass volume of about 190 million of cubic meters. the obtained geological model shows a partial structural control of the pre-existing tectonic pattern on slope deformation mechanisms, highlighting geometric and volumetric similarities between the Mt. nuovo ongoing deformation and an already oc- curred rock avalanche. the defined conceptual evolutionary mod- el allows to hypothesize the role of inner pressures constraining the shear zone initiation and propagation and making reliable a future scenario of generalized collapse. Starting from these new field and laboratory data, numerical models will be reconstructed in order to depict the evolution of the gravitational slope deformation, evaluate its sensitivity and constrain future evolutionary instability scenarios

Sartre y el problema de la superación de la metafísica.

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Carbon and oxygen stable isotope record of upper Kimmeridgian shallow-marine ramp carbonates (Iberian Basin, NE Spain): the imprint of different burial and tectonic histories

Bulk carbon and oxygen stable isotopes of ancient shallow-marine carbonates can record the effects of multiple palaeoenvironmental factors, but also the imprint of several post-depositional processes, which may alter the original marine isotopic composition. In this study, carbon and oxygen stable isotope analyses were performed on bulk carbonate, bivalve calcitic-shell (Trichites) and calcite vein samples from two stratigraphic sections (Tosos and Fuendetodos, present-day distance 15km), representing proximal inner- and distal mid-ramp environments, respectively, of the uppermost Kimmeridgian ramp facies deposited in the northern Iberian Basin (NE Spain). These successions underwent different diagenetic pathways that altered the primary marine isotopic composition in each section in different ways. Different burial histories, tectonic uplift and a variable exposure to meteoric diagenesis from the end of the Kimmeridgian to the Cenozoic (following Alpine tectonic uplift) are reflected in the different alteration patterns of the carbon and oxygen stable isotope signatures. A significant deviation to lower values in both δ13O and δ18O is recorded in those carbonates mostly exposed to meteoric diagenesis (distal mid-ramp Fuendetodos section), because of post-depositional tectonic uplift (telogenesis). On the other hand, the deposits mainly affected by burial diagenesis (proximal inner-ramp Tosos section) only record low δ18O with respect to expected values for pristine Kimmeridgian marine carbonates. The different burial and tectonic uplift histories of these deposits in each sector, due to their different tectonic evolution in this part of the basin, resulted in a variable degree of diagenetic resetting. However, in spite of the different diagenetic resetting reported of the carbon and oxygen stable isotope signatures in each section, these carbonates show similar cement types in termsof fabrics and cathodoluminescence properties. The diagenetic resetting reported for these carbonates prevents the use of the δ13O and δ18O records for addressing palaeoenvironmental interpretations, but instead highlights useful features regarding the variable diagenetic overprint of the studied shallow-marine carbonate successions concerning their specific post-depositional history