Abstract

It may seem a paradox, but it is nevertheless true, that more is known of the remote Palæolithic period than of the later Stone Age that ended about 4000 years ago. This applies to the Continent as well as to Britain, but Scandinavia is exceptional, and for our present purpose the best subject of investigation. The accepted view is that the three Baltic kingdoms were uninhabited in Quaternary times, and could only be approached by man after the last, or Baltic, glaciation had come to an end. There are certain facts inexplicable on that hypothesis, but all will agree that the Neolithic period in that area can be divided into early and late divisions; and so rich are the prehistoric remains and so advanced is this study, that the Scandinavian system can be used as a touch-stone by which to test the facts and theories of our own later Stone Age. I propose, therefore, on the present occasion to deal in some detail with the latest results of Scandinavian research, and then to proceed in order with the districts that face us across the North Sea and the Channel—North-west Germany, Holland, Belgium, and Northern France. It is hoped that such a survey will enable a more rigid classification to be made of the large amount of British material referred to the Neolithic period. In this country one has to rely mainly on form, but in Scandinavia that element is combined with others, such as habitation-sites, shell-mounds, and megalithic remains that furnish proof of the succession of forms, and open up the question of relations with Britain at that early date. If the claims already made on that head be valid, then comparisons become possible, and certain stages at least of the period in question can be arranged on scientific lines.

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