STORY MAKES HISTORY,THEORY MAKES STORY: DEVELOPING RÜSEN'S HISTORIK IN LOGICAL AND SEMIOTIC DIRECTIONS

This essay will argue that the traditional opposition between narrative and theory in historical sciences is dissolved if we conceive of narratives as theoretical devices for understanding events in time through special concepts that abridge typical sequences of events. I shall stress, in the context of the Historical Knowledge Epistemological Square (HKES) that emerged with the scientization of history, that history is always narrative, story has a theoretical ground of itself, and scientific histories address the need for a conceptual progression in ever‐improved narratives. This will lead to identification of three major theoretical levels in historical stories: naming, plotting (or emplotment), and formalizing. We revisit Jörn Rüsen's theory of history as the best starting point, and explore to what extent it could be developed by (i) taking a deeper look into narratological knowledge, and (ii) reanalyzing logically the conceptual strata in order to bridge the overrated Forschung/Darstellung (research/exposition) divide. The corollary: we should consider (scientific) historical writing as the last step of historical research, not as the next step after research is over. This thesis will drive us to a reconsideration of the German Historik regarding the problem of interpretation and exposition. Far from alienating history from science, narrative links history positively to anthropology and biology. The crossing of our triad name‐plot‐model with Rüsen's four theoretical levels (categories‐types‐concepts‐names) points to the feasibility of expanding Rüsen's Historik in logical and semiotic directions. Story makes history, theory makes story, and historical reason may proceed.     

THE TRANSITION TO A SOCIETY WITH A STATE IN THE SOUTH EAST OF THE IBERIAN PENINSULA (6th–4th CENTURY BC)

Summary. From the 6th century BC onwards the Iberian culture, with its strong and deep Mediterranean roots, developed along practically the whole of the east coast of Spain, in eastern Andalusia, and part of the Ebro valley, being most clearly defined between the 5th and 3rd centuries BC. An example in the South East of the Iberian Peninsula is one of those which most clearly displays its character.
This paper (a summary of my doctoral thesis, Madrid 1988) concentrates on the middle of the Segura basin, in what are known as the western and eastern districts of Murcia and the pre-coastal depression of Murcia. It is a region which has its own cultural and geographical identity, while offering a minimum of published data, sufficiently significant for bibliographical review, which makes it possible to maintain the historical hypothesis put forward.     

EVALUATION OF CONVENTIONAL AND ADAPTIVE PUSHOVER ANALYSIS II: COMPARATIVE RESULTS

In this paper, the methodology for evaluation of conventional and adaptive pushover analysis presented in a companion paper is applied to a set of eight different reinforced concrete buildings, covering various levels of irregularity in plan and elevation, structural ductility and directional effects. An extensive series of pushover analysis results, monitored on various levels is presented and compared to inelastic dynamic analysis under various strong motion records, using a new quantitative measure. It is concluded that advanced (adaptive) pushover analysis often gives results superior to those from conventional pushover. However, the consistency of the improvement is unreliable. It is also emphasised that global response parameter comparisons often give an incomplete and sometimes even misleading impression of the performance.     

Early medieval landscapes in north‐west Spain: local powers and communities,fifth–tenth centuries

There has been in the last few years a rapid expansion in the archaeology of early medieval societies in the north‐west of the Iberian Peninsula. A large part of this evidence remains unpublished or has been published incompletely. This article considers the historical landscapes of the north‐western Iberian Peninsula in the early medieval period as social constructions, starting with the identification of the systemic relationships between different archaeological entities. The dynamics and articulation of early medieval societies in the Cantabrian area and in the Duero and Tagus basins will be outlined by means of deconstructing their landscapes. To achieve this, a set of variables will be analysed in comparative terms from three regions selected as case studies: Madrid, the Duero basin and the Basque Country. With the aim of explaining these systems diachronically a division between the fifth–eighth and eighth–tenth centuries will be taken into consideration.     

THE TECHNOLOGICAL AND TYPOLOGICAL BEHAVIOUR OF A NEANDERTHAL GROUP FROM EL SIDRÓN CAVE (ASTURIAS,SPAIN)

This paper presents the first detailed analysis of the lithic industry from El Sidrón Cave. Previously we have published other works concerning Anthropology and Palaeogenetics. The lithic assemblage contains 415 artefacts coming from both unofficial and official excavations and is largely flake‐based. The raw material derives from the immediate cave environment, and is mostly chert, with quartzite in a lesser proportion. To date, 67 artefacts have been refitted, including some tools and cores. The spatial distribution of the refitted lithic artefacts confirms, on the one hand, the unity of the assemblage and, on the other, its secondary context.     

SEISMIC HAZARD ASSESSMENT IN FLORENCE CITY ITALY

A seismic hazard analysis of Florence city was performed in the frame of a project concerning the dynamic behaviour of cable-stayed bridges. Both a probabilistic approach and a methodology based on the use of a local macroseismic catalogue were applied. A local catalogue was expressly compiled for this purpose, to collect the macroseismic intensities actually observed at the site as a result of past earthquakes. This sort of catalogue is an independent tool to verify the assumptions of the probabilistic approach (seismic zoning, earthquake recurrence relation, attenuation model), though it can supply results in terms of macroseismic intensity only and reflects the effective seismic history at the site, without taking into account any variability. The Cornell' methodology was used to assess probabilistic hazard in terms of macroseismic intensity, peak ground acceleration, peak ground velocity, and pseudovelocity uniform response spectra. The local catalogue points out level VII of the Mercalli-Cancani-Sieberg scale (MCS) as the maximum intensity historically observed in Florence. The probabilistic approach leads to the consideration of intensity VIII MCS as the maximum credible for the city. The probabilistic analysis in terms of ground motion was performed using attenuation relations estimated for alluvium sites, since the geology of Florence area is represented by fluvial and lacustrine deposits of various thickness. Peak ground acceleration values with 90% non exceedence probability in 50 and 500 years are respectively 145 and 219 cm/s's for a shallow alluvium site, and 95 and 157 cm/s's for a deep alluvium site; the corresponding peak ground velocity values for sites located on alluvium are 6.41 and 11.76 cm/s. Uniform response spectra are provided for shallow and deep alluvium sites, according to frequency-dependent attenuation relations estimated from strong Italian earthquakes.     

RESTORING CONTINUITY: NOTES ON HISTORY AND FICTION

In 1935, as Europe witnessed the rise of fascism, Paul Valéry tried to identify the origins of the crisis in a lecture titled “Le bilan de l'intelligence.” Things were better, he claimed, when people were able to understand their present moment as the result of past events—that is, when “continuity reigned in the minds.” In this article, I discuss why that sense of continuity with the past is, in fact, indispensable for individuals and societies alike; using instances from great works of fiction, ranging from Don Quixote to the novels of Toni Morrison and Abdulrazak Gurnah, I suggest that fiction—the literary imagination of the historical past—might be uniquely adept at restoring continuity when it is broken.     

INFLUENCE OF THE UNCERTAINTY IN THE SOIL-ROCK SPECTRAL RATIOS IN THE DEFINITION OF UNIFORM HAZARD SPECTRA AT SURFACE LEVEL

Based on traditionally accepted hypothesis and verified by existing data, an expression is derived to calculate response spectrum at the ground surface if the response spectrum at the basement rock is known. The fundamental assumptions are with regards to the form of variation of the exceedance rates of spectral accelerations in the basement rock, and based also on the usual (lognormal) distribution forms of the uncertainties associated with the spectral amplification function. The resulting approach multiplies the mean of the amplification function in order to consider in a rigorous way its uncertainty.