By Alan H. Gardiner

Historical Egyptian Onomastica via Sir Alan H. Gardiner

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Cit. 22). The rich iron ore deposits of Skye notwithstanding, there are few mineral resources of any value in Atlantic Scotland. The rarity of these mineral resources elsewhere in western Europe ensured the importance of contacts with Atlantic areas throughout the prehistoric period and undoubtedly stimulated the early development of maritime contacts between coastal communities. 2 Distribution of major metal deposits in the Atlantic zone. topography of the interior zone (Ruíz-Gálvez 1989: 103).

The coastline has been shaped by the enormous erosive forces of the sea etching out the younger, softer rocks over the millennia while leaving the older, more resilient rocks projecting out into the sea as jagged headlands. While erosion is a major factor in the current appearance of the Atlantic seaboard, the impact of rising sea levels (eustatic change) coupled with the localised warping and sinking of the coastline (isostatic change) over the last ten thousand years is responsible for the drowning of the lower reaches of river valleys throughout the zone, forming distinctive ria type coastlines with long winding indentations.

1983). Late Bronze Age During the Late Bronze Age there were significant environmental changes. Evidence for colder and wetter conditions is seen through the expansion of peat bogs in Atlantic areas. It is widely accepted that there was a 2°C drop in overall mean temperature in the first quarter of the first millennium BC (Cunliffe 1995a: 16). This would have substantially shortened the growing season and thus have a drastic effect on marginal, upland Atlantic communities. This set of circumstances is dramatically seen in the abandoned field systems and farmsteads, dating to the second and early first millennia BC, in Dartmoor.

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Ancient Egyptian Onomastica by Alan H. Gardiner


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