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

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illus<br />

FIGURE 39: PETROGLYPH SITES AT OS CAMPOS, BAYONA.<br />

cupule, situated just north <strong>and</strong> down-slope <strong>of</strong> the well known petroglyph<br />

rock comprising complex but very superficial designs (<strong>and</strong> only one<br />

clear cupule). <strong>The</strong>se observations prove how important the exact<br />

recording <strong>of</strong> each cupule is.<br />

Moreover, the major group <strong>of</strong> petroglyphs at Os Campos (Fig. 39) is<br />

located south <strong>of</strong> a rocky hillock, the Outeiro dos Lameiros, with a large<br />

collection <strong>of</strong> animal engravings on a vertical cliff face. This hillock<br />

blocks the view to the north, where the Ria de Bayona <strong>and</strong> its<br />

accessible beaches (the original l<strong>and</strong>ing place ? - compare with similar<br />

situations at Muros) would have been visible. Apart from later motifs,<br />

simple cupules dominate the centre <strong>of</strong> the group, marking the highest<br />

point <strong>of</strong> a small saddle or watershed in the hills, whereas complex<br />

carvings (Fig. 184) are found on lines stretching west <strong>and</strong> east from<br />

this central group. All over the hillslopes are extensive suitable<br />

outcrops, even extending down to the outskirts <strong>of</strong> the town <strong>of</strong> Bayona,<br />

<strong>of</strong>ten yielding far better views, but these outcrops have been ignored.<br />

<strong>The</strong> sheltered situation at Os Campos resembles the Barcelos group,<br />

SW <strong>of</strong> Bayona (Fig. 130), where two panels with complex engravings<br />

(one group vaguely resembling the “fingerprint” patterns from Gavr’inis<br />

in France) are clearly separated from a small group <strong>of</strong> cupmarked rocks<br />

to the north. Although the distance between the complex group <strong>and</strong> the<br />

simple engravings is only a few meters (Fig. 40), it is striking to see<br />

how prominent (but undecorated) boulders between the two groups<br />

completely block <strong>of</strong>f all views between the two groups. Moreover, the<br />

complex group is found on lower level <strong>and</strong>, like the Pedra da Chula, it is<br />

M. <strong>van</strong> HOEK: 61 GEOGRAPHY

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