Settlement Pattern Change in the Morea (Peloponnisos), c.A.D. 1700–1830

Abstract

The historiography of the Ottoman period (Tourkokratia) in what is now the state of Greece contains many untested propositions about both the nature and the consequences of Turkish rule (Hatzidimitriou 1982). Amongst these is the notion that during the Ottoman occupation the Christian population – or at least a sizeable proportion of it – was driven into the mountains. Our paper sets out to test the hypothesis – for such it is – using readily available published information on the settlements of the Morea (Peloponnisos) dating from c.1700 and c.1830. First, though, we specify the hypothesis and indicate the types of evidence which appear to give it support.     

Potassium-argon ages of schist honestones from the viking age sites at Kaupang (Norway), Aggersborg (Denmark), Hedeby (West Germany) and Wolin (Poland), and their archaeological implications

Viking age honestones from four large sites in northern Europe have been made from two different types of quartz-muscovite schist: one dark grey, very fine-grained schist, and a light grey, fine-grained schist. In order to determine the provenance of these schist hones, KAr ages have been determined on 16 selected representative hones. The dark grey schist hones yield Caledonian ages of 403–446 Ma. and consideration of petrographic evidence leads to the conclusion that the hones were quarried in the Caledonian area (presumably) of Western Norway. The light grey schist hones are Precambrian, with KAr ages of 931–946 Ma, and are presumed to originate from Telemark, South Norway. The amount and homogeneity of these honestone groups from different parts of the Viking world indicates the existence of large quarries, and demonstrates that production and trade were more wide-ranging than had hitherto been assumed.