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

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� CHAPTER 1.2.2 �<br />

THE LOCH TAY ROUTE<br />

PATTERNS OF DIVERGENCE<br />

� INTRODUCTION �<br />

This study area (Fig. 16) comprises a mountainous inl<strong>and</strong> region in the<br />

centre <strong>of</strong> Scotl<strong>and</strong> (Fig. 3), dominated by the river <strong>and</strong> Loch Tay which<br />

roughly stretches for 60 km between Crianlarich <strong>and</strong> Ballinluig.<br />

Included is the l<strong>and</strong> flanking this stretch up to 5 km on both sides. <strong>The</strong><br />

study area therefore measures roughly 600 km 2 , but the focus is on<br />

three smaller concentrations, indicated within frames on Fig. 16.<br />

map<br />

map map<br />

FIGURE 16: THE LOCH TAY STUDY AREA; SCOTLAND.<br />

In the previous chapter we have seen that the Kilmartin valley served<br />

as a major ritual key area <strong>and</strong> that patterns <strong>of</strong> convergence dominated<br />

the distribution <strong>of</strong> rock art sites <strong>and</strong> monuments. When prehistoric<br />

people travelled further inl<strong>and</strong> from the Kilmartin area, the use <strong>of</strong> two<br />

major lakes, Loch Awe <strong>and</strong> Loch Tay, caused a strong funnelling effect.<br />

This is reflected in the (sparse) distribution <strong>of</strong> rock art along this<br />

M. <strong>van</strong> HOEK: 34<br />

GEOGRAPHY

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