ANALYSE ET CARTOGRAPHIE DES DOMMAGES DU SÉISME SURVENU AU QUÉBEC LE 25 NOVEMBRE 1988

Dans le cadre d'un projet de recherche en cours portant sur l'évaluation de la vulnérabilité municipale aux catastrophes naturelles (Boivin 1990), un examen des dommages du séisme du 25 novembre 1988 a été mené afin de mieux documenter l'analyse du risque séismique au Québec. À partir de sources variées de rapports de dommages mais, plus spécifiquement, par l'étude des demandes liées au programme de dédommagement mis sur pied par le gouvernement du Québec, une analyse et une cartographie des dommages rapportés est fournie. Les résultats montrent que la majorité des dommages sont concentrés près de l'épicentre dans les régions du Saguenay/Lac Saint-Jean et de Québec. Les dégats répertoriés concernent principalement les ouvertures (portes et (enê tres) avec 11%, les murs intérieurs ou extérieurs (29%), l'apparition de fissures (72%), les fondations (44%) et les cheminées (29%). Au total, 1521 cas de dommages ont été rapportés et analysés dans ce projet de recherche.     

ROCK PHYSICS AND THE NEOLITHIC AXE TRADE IN GREAT BRITAIN*

This paper is concerned with the products of a number of Neolithic quarries in highland Britain. It investigates the claim that the scale of axe distribution was partly the result of social factors which resulted in these artefacts gaining an added value in areas remote from their sources. One case study considers the sequence of production in Cumbria, in relation to the tensile strength of the rock quarried in different parts of the region. It shows that these considerations had only a limited influence over the choice of stone source and the scale on which it was worked. A second study compares the tensile strength of the main raw materials used for making non-flint axes with the extent to which these sources were actually exploited. Again there is only a limited relationship between the two, suggesting that social factors may indeed have been important.     

RARE EARTH ELEMENT DISTRIBUTION PATTERNS IN SHETLAND STEATITE - CONSEQUENCES FOR ARTIFACT PROVENANCING STUDIES

An attempt has been made to relate steatite artifacts to the source of rock from which they were manufactured, using the distribution patterns of rare earth elements. Radiochemical- and instrumental-neutron activation analyses of Shetland steatites suggest that the use of rare earth elements in artifact provenancing may be unreliable. Concentrations of rare earth elements in many Shetland steatites are too low to be measured reliably by a cost effective method. The relative importance of primary igneous and secondary metasomatic processes in controlling steatite rare earth element geochemistry is discussed and geological arguments against the existence of unique rare earth ‘fingerprints’ for steatite are presented.