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

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water-filled basins on top initially attracted the petroglyph<br />

manufacturers (compare with the Pedra da Chula).<br />

<strong>The</strong> large outcrop stack also has a few simple cupules on a ledge at its<br />

NE, “overlooking” the complex engravings further NE. In Galicia single<br />

cupules <strong>of</strong>ten are found on rocks that are situated slightly higher than<br />

the complex engravings. This brings Bradley, Criado & Fabregas to<br />

suggest that “they (the cupules) may have been added to places that<br />

had an already established significance (1995: 358)”. This statement is<br />

rather obscure as it is not clear whether the authors meant that the<br />

significance had firstly been established by the natural basins or by<br />

the complex designs. In my opinion the complex design were added<br />

later, whereas the cupules already had enhanced the importance <strong>of</strong> the<br />

natural basins <strong>and</strong> the outcrop stack. It may also be important that the<br />

two most complex designs (one comprising a natural basin with a natural<br />

crack as radial groove: Fig. 47) are both surrounded by distinct small<br />

uniform cupules in an organised manner, but simultaneously are<br />

situated near a small cluster <strong>of</strong> r<strong>and</strong>om st<strong>and</strong>ard cupules <strong>of</strong> different<br />

sizes, generally considered by me to be older.<br />

* 1.3.1.4 CONCLUSIONS *<br />

Unfortunately Bradley, Criado & Fábregas only discussed two valley<br />

systems with rock art on the Muros peninsula (San Francisco <strong>and</strong><br />

Serres), whereas there actually are four valleys with petroglyphs. Two<br />

<strong>of</strong> the valleys start at the accessible beaches <strong>of</strong> San Francisco<br />

(marked Ia on Fig. 35) <strong>and</strong> Louro (Ib), the coastline <strong>of</strong> the latter<br />

valley probably extending much further inl<strong>and</strong> in prehistoric days. Both<br />

valleys connect via low passes with the sheltered valley at Laxes (II),<br />

(named Serres by Bradley, Criado & Fábregas 1995: 355) continuing<br />

north as the distinctly individually developed valley <strong>of</strong> Valdexería.<br />

All rock art sites are found surprisingly concentrated east <strong>of</strong> the high<br />

dividing ridge which extends from the north to the south at Monte<br />

Naraio. An exception is the site at Chans de Tras. It is the only site<br />

situated on top <strong>of</strong> the crest <strong>of</strong> the dividing ridge, but despite its high<br />

altitude it is invisible from all other sites. It is also the only site with<br />

wide views <strong>of</strong> both the Ria de Muros <strong>and</strong> the Atlantic Ocean <strong>and</strong> the<br />

only site with a view <strong>of</strong> the beautiful beaches at Carnota.<br />

At the extreme south end <strong>of</strong> the dividing ridge are the important<br />

groups <strong>of</strong> Naraio, situated among a large number <strong>of</strong> conspicuous outcrop<br />

formations. <strong>The</strong> rock art group at Monte Naraio 2 overlooks the ancient<br />

coastline <strong>and</strong> the probable l<strong>and</strong>ing site, whereas Monte Naraio 1 is more<br />

focussed on the interior, <strong>and</strong> its labyrinth shaped petroglyphs connect<br />

with a similar design at the Laxe do Carrizo, still further inl<strong>and</strong>.<br />

Most remarkable, the group <strong>of</strong> rock art sites at San Francisco is found<br />

in a distinct arc, parallel to the accessible beach, <strong>and</strong> they probably<br />

embrace the ancient l<strong>and</strong>ing place. Although Bradley, Criado & Fábregas<br />

M. <strong>van</strong> HOEK: 68 GEOGRAPHY

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