Maarten van Hoek The Geography of Cup-and-Ring ... - StoneWatch
Maarten van Hoek The Geography of Cup-and-Ring ... - StoneWatch
Maarten van Hoek The Geography of Cup-and-Ring ... - StoneWatch
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major route through the interior, as there is no rock art site which is<br />
found further away than two kilometres from the valley edges.<br />
Yet there are differences in the distribution <strong>of</strong> rock art, especially<br />
around the Loch Tay area. <strong>The</strong> most striking difference is that<br />
patterns <strong>of</strong> divergence emerge east <strong>of</strong> a certain point on the route.<br />
Although the drainage area <strong>of</strong> the river Tay further east <strong>and</strong> outside<br />
the study area has more than a hundred rock art sites, there are only<br />
very few sites actually lining the lower reaches <strong>of</strong> the river Tay; the<br />
rest is found widely scattered across relatively fertile <strong>and</strong> low-lying<br />
countryside <strong>and</strong> shows no distinct relation to features in the l<strong>and</strong>scape.<br />
* 1.2.2.1 CHANGING PATTERNS *<br />
In the study area, however, rock art is strictly confined to a limited<br />
area on both sides <strong>of</strong> the valleys involved. In the extreme west part <strong>of</strong><br />
the study area patterns <strong>of</strong> convergence are still present, although on a<br />
most modest scale. In this westerly area namely, the route to Loch Tay<br />
is joined by two other major routes from the south <strong>and</strong> each<br />
crossroads features a minor group <strong>of</strong> simple rock art, notably at<br />
Crianlarich <strong>and</strong> Mid Lix (Fig. 16).<br />
* 1.2.2.1.1 But further east there is a first attempt to diverge<br />
from the main route. From Killin (Fig. 16) a line <strong>of</strong> simple rock art sites<br />
enters the valley <strong>of</strong> the<br />
river Lochay. In this valley<br />
two distribution patterns<br />
emerge intermingled. Rock<br />
art is still marking a main<br />
axis <strong>of</strong> movement, but at the<br />
same time we see that minor<br />
concentrations are found<br />
running uphill for a short<br />
distance, <strong>of</strong>ten near minor<br />
streams, but without<br />
reaching the highest ground<br />
(compare with Bute).<br />
<strong>The</strong> major concentration,<br />
however, is found at<br />
Duncroisk on a relatively<br />
large floodplain. All sites<br />
FIGURE 17: DUNCROISK.<br />
again are located near<br />
streams <strong>and</strong> one decorated<br />
rock is even situated on an outcrop projecting into the river Lochay<br />
(marking a crossing place ?). It is significant that the major group <strong>and</strong><br />
the most complex art is concentrated on the valley floor, whereas<br />
simple art is found on the higher ground (the number <strong>of</strong> cup-<strong>and</strong>-rings<br />
between (), preceded by numbers <strong>of</strong> single cupules in Fig. 17).<br />
M. <strong>van</strong> HOEK: 35<br />
GEOGRAPHY