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Maarten van Hoek The Geography of Cup-and-Ring ... - StoneWatch

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Another discrepancy between Hordal<strong>and</strong> <strong>and</strong> Sweden is that rocks with<br />

such deep <strong>and</strong> large cupules seem to be rare in the Bohuslän area <strong>of</strong><br />

Sweden, but relatively common in Norway, Denmark <strong>and</strong> northern<br />

Germany <strong>and</strong> indeed elsewhere in Europe.<br />

* 1.5.3.1 THE ROCK ART OF THE ETNE DISTRICT *<br />

� INTRODUCTION �<br />

This is a most interesting area, not only for its abundance <strong>of</strong> rock art,<br />

but also for the special topography. <strong>The</strong> district is notably situated in<br />

a transition zone between the lower coastal area <strong>and</strong> the rugged upl<strong>and</strong><br />

plateaux <strong>and</strong> mountains, parts <strong>of</strong> which still are covered with snow <strong>and</strong><br />

glaciers today. This division is reflected in the area itself. <strong>The</strong> west<br />

part <strong>of</strong> the Etne study area comprises more rolling high hills <strong>and</strong> low<br />

mountains, whereas the east part has higher <strong>and</strong> steep sided mountains,<br />

still partly snow covered in the summer. <strong>The</strong> western zone is marine,<br />

although it is located more than 40 km from the open ocean. <strong>The</strong><br />

eastern zone is lacustrine, although there is a pass from Lake Stordal<br />

connecting with the sea at the Åkrafjorden. <strong>The</strong> river Nord, running<br />

from Lake Stordal <strong>and</strong> emptying itself into the fjord near Etne,<br />

connects the two zones (Fig. 104).<br />

map<br />

map<br />

FIG. 104: THE ETNE DISTRICT, HORDALAND, NORWAY.<br />

M. <strong>van</strong> HOEK: 131<br />

GEOGRAPHY

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