A landscape of powers in Highland Papua,C. 1899-1918

The article proposes that anthropologists and historians attend to a 'landscape of powers' to understand the ways colonial and mission projects become actualised in on-going social relations. An expanding body of scholarship for the Melanesian region has focused on the way missionaries and colonial agents, as much as the diverse Melanesian peoples, attain power through rendering persons and places in specific forms. This is documented here for Fuyuge-speakers relations with colonial and mission projects during their early phase. Although the forms and consequences of power among each--Fuyuge, colonial, mission--is different, attention is devoted to the resultant and emerging patterns of these long-standing interactions and interventions. In particular, the article maintains that when such projects become locally actualised a landscape of powers is established. A landscape of powers is the multiply constituted arrangement of persons and places in an historical and ethnographically delineated context.     

Discerning geological and geographical sources of Belgian Upper Paleolithic fluorites by rare earth elements and Sr-isotopic geochemistry

Fragments of fluorite (CaF₂) have been found at five Belgian Upper Paleolithic sites (Spy, Chaleux, Trou Magritte, Trou du Frontal and Verlaine caves), primarily of Magdalenian age. These sites are located in a large geographical area. The aim of this study is to isolate one or more primary sources where the mineral could have been quarried prehistorically, and hence try to deduce if time and effort were put into obtaining it, or if it was simply a useful nearby raw material. In order to achieve this objective, isotopic ⁸⁷Sr/⁸⁶Sr and REE ratios are used. A total of four archaeological samples from the Chaleux, Spy and Trou Magritte sites along with geological samples were analyzed (new results and data from the literature), obtained from two distinct stratigraphical units in Belgium: the Givetian limestones (mainly from the Calestian Band), and the Dinantian limestones.