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

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1950 ± 110 BC (HAR-3071), dating it to the Early Bronze Age<br />

(Beckensall 1983: 176). As cupules are <strong>of</strong> all ages, this specific<br />

cupmarked stone may indeed contemporary to the henge (but also<br />

earlier or later, as the execution <strong>of</strong> the cupule was not dated), but this<br />

single example does not <strong>of</strong>fer any evidence that the whole body <strong>of</strong> rock<br />

art in this region is contemporary to the henges.<br />

<strong>The</strong>re are three things that only seemingly link the henges with the<br />

petroglyphs. Both features are circular <strong>of</strong> character; both occur<br />

roughly in the same area (although henges have a more westerly<br />

orientation) <strong>and</strong> thirdly, some <strong>of</strong> the petroglyph sites indeed overlook<br />

the basin. But it does not mean that the initial distribution <strong>of</strong> the rock<br />

art near the Milfield Basin is actually related to the henges in the<br />

area. We have already seen that most <strong>of</strong> the art overlooks the valley <strong>of</strong><br />

the Till in between the two s<strong>and</strong>stone ridges (Fig. 31) <strong>and</strong> not the<br />

Milfield Basin. It proves that the two features are geographically <strong>and</strong><br />

geomorphologic separated <strong>and</strong> therefore possibly culturally <strong>and</strong><br />

temporally as well.<br />

* 1.2.3.3.3.2 <strong>The</strong>re may be another explanation for the<br />

concentration <strong>of</strong> rock art near this basin. It is notably a fact that the<br />

Milfield Basin once was a large glacial lake because <strong>of</strong> a morainic dam<br />

near Etal (the approximate extent <strong>of</strong> the lake is shown in Fig. 34). <strong>The</strong><br />

exact date <strong>of</strong> the draining <strong>of</strong> the lake is not known, but it is possible<br />

that the people <strong>of</strong> the cupule (or later the cup-<strong>and</strong>-ring) manufacturers<br />

arrived in the area when the basin was still a lake or possibly a marsh.<br />

This recalls the situation at the Kilmartin valley (Chapter 1.2.1) where<br />

a marshy area is lined with rock art, but only at two <strong>of</strong> the three sides.<br />

A similar situation occurs at the Milfield Basin: there is no rock art on<br />

the south <strong>and</strong> west side <strong>of</strong> the basin. A possible explanation may be<br />

that exposed rock is rather scarce in these upl<strong>and</strong> areas. <strong>The</strong> presence<br />

<strong>of</strong> granites <strong>and</strong> lavas as types <strong>of</strong> stone too hard to carve, is hardly an<br />

argument, as most engravings in Galicia <strong>and</strong> the Canary Isles<br />

(PowerPoint SLIDES 1) are on granite <strong>and</strong> lavas respectively.<br />

Most <strong>of</strong> the circular art can safely be dated to the Neolithic <strong>and</strong><br />

possibly is older than the passage tomb art. Most henges in Britain<br />

date however from the Late Neolithic <strong>and</strong> Early Bronze Age <strong>and</strong><br />

contemporaneity with the art is therefore highly unlikely.<br />

* 1.2.3.3.3.3 I must conclude that the art focussed more on<br />

the valley <strong>of</strong> the Till <strong>and</strong> avoided the basin, rather than it is related to<br />

the monuments in the Milfield Basin. <strong>The</strong> art already had been<br />

executed <strong>and</strong> routes had already been established long before the<br />

henge monuments were laid out in the Milfield Basin.<br />

A similar conclusion was reached for the Kilmartin valley in Scotl<strong>and</strong>:<br />

also in that area monuments <strong>and</strong> rock art are not contemporary. This<br />

conclusion seems to be confirmed by the striking absence <strong>of</strong> open-air<br />

petroglyphs in the direct neighbourhood <strong>of</strong> other important<br />

M. <strong>van</strong> HOEK: 54 GEOGRAPHY

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