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

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argue that all these sites comm<strong>and</strong> extensive views into the lower<br />

ground <strong>of</strong> the San Francisco valley (1995: 357), this definitely is not<br />

true for the site at O Cruceiro, which moreover is located on the wrong<br />

spot on their map; it should be situated at least 300 m further east<br />

(Fig. 36). O Cruceiro is a most extensive <strong>and</strong> steeply south sloping<br />

outcrop area, where only one cup-<strong>and</strong>-three-rings was reported.<br />

Inspection <strong>of</strong> the site, however, revealed at least two more single<br />

cupules. From O Cruceiro, on top <strong>of</strong> a cliff <strong>and</strong> directly high above the<br />

beach, the other sites are definitely invisible, but there is a splendid<br />

view <strong>of</strong> the beach <strong>of</strong> San Francisco <strong>and</strong> the Louro peninsula with its<br />

distinct solitary hill. This resembles the situation at Mogor near<br />

Pontevedra, where a major cup-<strong>and</strong>ring<br />

site overlooks a most accessible<br />

s<strong>and</strong>y beach, but also many sites in<br />

Scotl<strong>and</strong> similarly overlook beaches or<br />

small bays suitable as l<strong>and</strong>ing places<br />

(Monreith <strong>and</strong> Garlieston in Galloway;<br />

Ardifur <strong>and</strong> Poltalloch in Argyll).<br />

<strong>The</strong> distribution pattern in these two<br />

valleys (Ia <strong>and</strong> Ib) indeed seems to<br />

indicate that prehistoric people<br />

approached the Muros peninsula from<br />

the south; possibly in two flows (Fig.<br />

48). <strong>The</strong> coastline north <strong>of</strong> Muros town<br />

is rather muddy <strong>and</strong> is rather<br />

inaccessible, especially at ebb. Several<br />

FIG. 48: ROUTES I – II. beaches on the Muros peninsula<br />

however, are most suitable as l<strong>and</strong>ing<br />

place, but probably because <strong>of</strong> the more sheltered character the<br />

beaches at Louro <strong>and</strong> especially San Francisco were favoured, whereas<br />

the more exposed beaches <strong>of</strong> Lariño <strong>and</strong> Carnota (Fig. 35) were<br />

ignored. <strong>The</strong>re is for instance, no rock art in the valley NE <strong>of</strong> the<br />

beach at Lariño. Bradley, Criado & Fábregas moreover argue (1995:<br />

354) that “if the rock carvings really formed part <strong>of</strong> a territorial<br />

system, we might expect them to be located around particular<br />

resources”. As the valley NE <strong>of</strong> Lariño differs not much in character<br />

from the valleys <strong>of</strong> Louro <strong>and</strong> San Francisco, it is more than strange<br />

that there is no rock art in this valley.<br />

Beyond the arc <strong>of</strong> rock art sites at San Francisco no circular<br />

petroglyphs have been recorded until one reaches the head <strong>of</strong> the<br />

valley. <strong>The</strong>re, a most prominent outcrop stack marks the site <strong>of</strong> the<br />

Laxa da Rodas, which bears one <strong>of</strong> the most interesting collection <strong>of</strong><br />

petroglyphs <strong>of</strong> the whole peninsula. Together with the cupmarked rocks<br />

newly reported by Bradley, Criado & Fábregas, it marks the pass<br />

M. <strong>van</strong> HOEK: 69 GEOGRAPHY

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