Podoconiosis in the Ethiopian Rift Valley - Role of beryllium and zirconium

A geogenic origin has been proposed in the aetiology of non-filarial elephantiasis of the feet and legs, recently renamed podoconiosis. Soil collected in an area of the Ethiopian Rift Valley, the borough of Ocholo, known for its high prevalence of podoconiosis (5.06%), has been submitted to mineral analysis. High values of sulphur (S), cerium (Ce), lanthanum (La) and neodymium (Nd), typical for basaltic bedrocks, were found. Of special interest were the values for zirconium (Zr) and beryllium (Be), 618 +/- 87 ppm and 4.6 +/- 0.5 ppm respectively, twice as high as those recorded for soils sampled in neighbouring areas where the prevalence of podoconiosis is low. To be noted also, a high content in vanadium, above 250 ppm, in half of the soil samples collected in this region. Year-long exposure of unprotected feet to Zr and Be, known for their ability to induce granuloma formation in the lymphoid tissue of man, and present in a clay rich in colloidal silica particle, highly abrasive to skin, is doubtlessly a factor involved in the development of lymph node sclerosis leading to elephantiasis.

Des céramiques aux hommes : étude céramique des premiers horizons fouillés sous la cathédrale Saint-Pierre de Genève (1er millénaire av. J.-C. - 40 apr. J.-C.)

Résumé Le travail présenté est basé sur l'analyse systématique des 145'157 fragments de céramique émanant de 2137 ensembles recueillis entre 1976 et 2003 lors de la fouille de la cathédrale Saint-Pierre. Datés entre le Ier millénaire av. J-C. et le XIXe siècle, ils témoignent de l'ampleur et de la richesse des activités menées au sein de ce site phare de la ville de Genève. Les particularités observées pour les six premiers horizons reconnus, qui couvrent une période comprise entre le Ier millénaire av. J.-C. et 40 apr. J.-C., liées aux structures a priori énigmatiques mises en évidence lors de la fouille, ont orienté le champ d'étude vers une compréhension fine du mobilier recueilli dans ces strates anciennes. Ainsi cadrée, l'étude s'est concentrée sur 237 complexes céramiques ayant livré 23'129 fragments. La corrélation stratigraphique menée sur les 8000 m2 de terrain fouillé a permis de porter l'analyse sur la répartition spatiale du corpus considéré. Développée également sur le plan diachronique, cette démarche a largement contribué à la définition des activités menées sur le site. Ainsi, la concentration de fragments de panses d'amphore et de vaisselle de table importée de Campanie au pied d'un tertre mis en évidence sous le choeur de la cathédrale a conduit à reconnaître l'existence d'un banquet funéraire témoignant de l'ensevelissement sous tumulus d'un aristocrate allobroge décédé entre 120 et 70 av. J.-C. Réparties sur la totalité de la surface occupée par la nef de la cathédrale et des rues la flanquant, les quelques 1024 coupes à boire de La Tène finale mises au jour ont quant à elles permis d'identifier les surfaces de gravier qu'elles scellaient comme une aire de rassemblement ayant abrité des banquets tenus périodiquement. Le maintien de ces activités rituelles et collectives jusqu'au milieu du Ier siècle de notre ère conclut l'analyse diachronique. La mise en perspective historique des données recueillies sur le terrain souligne l'importance de l'antique oppidum extremum des Allobroges, dont le sort fut en 58 av. J.-C. à l'origine de la Guerre des Gaules.

Stability analysis of the 2007 Chehalis lake landslide based on long-range terrestrial photogrammetry and airborne LIDAR data

On December 4th 2007, a 3-Mm3 landslide occurred along the northwestern shore of Chehalis Lake. The initiation zone is located at the intersection of the main valley slope and the northern sidewall of a prominent gully. The slope failure caused a displacement wave that ran up to 38 m on the opposite shore of the lake. The landslide is temporally associated with a rain-on-snow meteorological event which is thought to have triggered it. This paper describes the Chehalis Lake landslide and presents a comparison of discontinuity orientation datasets obtained using three techniques: field measurements, terrestrial photogrammetric 3D models and an airborne LiDAR digital elevation model to describe the orientation and characteristics of the five discontinuity sets present. The discontinuity orientation data are used to perform kinematic, surface wedge limit equilibrium and three-dimensional distinct element analyses. The kinematic and surface wedge analyses suggest that the location of the slope failure (intersection of the valley slope and a gully wall) has facilitated the development of the unstable rock mass which initiated as a planar sliding failure. Results from the three-dimensional distinct element analyses suggest that the presence, orientation and high persistence of a discontinuity set dipping obliquely to the slope were critical to the development of the landslide and led to a failure mechanism dominated by planar sliding. The three-dimensional distinct element modelling also suggests that the presence of a steeply dipping discontinuity set striking perpendicular to the slope and associated with a fault exerted a significant control on the volume and extent of the failed rock mass but not on the overall stability of the slope.

Spiritual Kinship, Political Mobilization and Social Cooperation: a Swiss Alpine valley in the Eighteenth and Nineteenth Centuries

In this chapter I will present some observations and results about Ritual Kinship and political mobilization of popular groups in an Alpine valley: the Val de Bagnes, in the Swiss canton of Valais, - a mountain valley, well known today thanks to the tourist station of Verbier - where we can rely on excellent sources about local families. This region presents a particular political situation, because the 11 major villages of the valley form only one commune, which includes the whole valley.¦There are two major reasons to choose the Val de Bagnes for our inquiry on kinship and social networks in a rural society:¦A. The existence of sharp political and social conflicts during the 18th and the 19th centuries;¦B. The existence of almost systematic genealogical data between 1700 and 1900. (Casanova, Gard, Perrenoud 2005-08)¦The 18th century was characterized by the struggle of an important part of the community of Bagnes against the feudal lord, the abbot of St-Maurice. The culminating point was a local upheaval in 1745 in Le Châble, during which the abbot was forced to sign several documents in accordance with the wishes of the rebels (Guzzi-Heeb 2007). In the 19th century feudal lordship was abolished, but now the struggle confronted a liberal-radical faction and the conservative majority in the commune.¦The starting point of my presentation focuses on this question: which role did spiritual kinship play in the political mobilization of popular groups and in the organization of competing factions? This question allows us to shed light on some utilizations and meanings of spiritual kinship in the local society. Was spiritual kinship a significant instrument for economic cooperation? Or was it a channel for privileged social contacts and transactions?