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

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icecap first caused the l<strong>and</strong> to sink deeply into the earth <strong>and</strong><br />

simultaneously glaciers carved out deep troughs that extended even<br />

under sea level, simultaneously polishing the rocks. Especially at the<br />

Norwegian west coast this process created a distinctively indented<br />

shoreline characterised by the steepness <strong>of</strong> the valley walls, the great<br />

depth <strong>and</strong> the great inl<strong>and</strong> extent.<br />

Later, when the icecaps melted world wide, the sea level rose <strong>and</strong> such<br />

troughs became water filled <strong>and</strong> turned into the well known fjords,<br />

<strong>of</strong>ten providing splendid natural harbours. More importantly, also the<br />

l<strong>and</strong> rose to a higher level because <strong>of</strong> the isostatic uplift as a result <strong>of</strong><br />

the loss <strong>of</strong> weight consequent upon the melting <strong>of</strong> the icecap <strong>of</strong> the<br />

last Ice Age. It is estimated that in Sc<strong>and</strong>inavia this relative uplift<br />

amounts approximately 100 m (Coles 1990: 7). As a result, prehistoric<br />

coastlines are found at high altitudes nowadays.<br />

In general one can therefore state that the oldest rock art only occurs<br />

at higher level, whereas younger motifs are also found at much lower<br />

levels. <strong>The</strong> fact, however, that younger engravings can also be found on<br />

higher levels, presents a problem. Indeed, the general distinction in<br />

height proved to be not really helpful in particularly separating cup<strong>and</strong>-ring<br />

motifs chronologically from the Bronze Age iconic figures. In<br />

most cases cup-<strong>and</strong>-rings are too closely associated with the figures <strong>of</strong><br />

the Bronze Age. Especially in Bohuslän, Sweden, both types <strong>of</strong> rock art<br />

are <strong>of</strong>ten found intermingled at the same level.<br />

Still, there are indications that the Sc<strong>and</strong>inavian cup-<strong>and</strong>-ring motifs<br />

may be older than the Bronze Age. It notably is reasonable to suggest<br />

that Bronze Age rock art manufacturers were attracted to the<br />

previously executed cupules <strong>and</strong> cup-<strong>and</strong>-rings from the Neolithic<br />

period, even when lower surfaces were already available. <strong>The</strong> main<br />

question is now whether the surfaces used by the Bronze Age people<br />

were also available during the Neolithic. This proves to be the case in<br />

many situations. In Norway the major cup-<strong>and</strong>-ring sites near Etne all<br />

are located higher than 75 m, at a level certainly accessible for<br />

Neolithic people. But in Sweden the situation is more complex.<br />

An example may illustrate this. <strong>The</strong> engravings <strong>of</strong> the Vitlycke area,<br />

Bohuslän, are found roughly between the 15 m <strong>and</strong> the 35 m contours;<br />

the majority centred at about 25 – 30 m. <strong>The</strong> graph at Fig. 92 roughly<br />

shows when a certain altitude became dry l<strong>and</strong>, <strong>of</strong>fering two scenarios.<br />

It proves that all engravings lower than 35 m cannot be older than<br />

4300 BC in case <strong>of</strong> a rapid fall <strong>of</strong> the prehistoric sea level, <strong>and</strong> not<br />

older than 3000 BC in case <strong>of</strong> a slow fall. Even in the worst case<br />

scenario, the area between 25 m <strong>and</strong> 35 m was already available for<br />

engravings from 2400 BC <strong>and</strong> onwards; in the more favourable situation<br />

already by 3700 BC. This proves that at least late Neolithic people<br />

could have used the smooth granite outcrops on the prehistoric<br />

coastline <strong>of</strong> Bohuslän as canvasses for their rock art. Outcrop panels<br />

M. <strong>van</strong> HOEK: 120<br />

GEOGRAPHY

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