In 1982 Noel Fojut published a paper entitled ‘Towards a
geography of Shetland brochs’ in which he constructed a model of settlement
location in relation to the physical environment. He calculated that the
average distance to nearest neighbour was 2.787 kilometres (giving a figure of
around 7 sq. km. for the average area of a broch territory). The result of
mapping the brochs using this calculated average (fig.1) shows that, on the
large scale, the brochs are far from being regularly spaced. The density is
greatest at the southern end of the archipelago and so I have redrawn the map
(fig.2) to show just this area and assuming that each broch territory is a
square 1.5km x 1.5km. This seems to fit the data reasonably well, bearing in
mind that the broch wouldn’t always be at the centre of its territory.
Fig.1 Shetland broch territories, Fig.2 South Shetland broch territories
assuming a diameter of 2.787km assuming a diameter 1.5km
Mapping the Caithness brochs using a figure of 1.5km for the diameter of the territory gives an interesting result (fig.3). There is evidently more clustering in this region, which may an indication of family or clan groupings that farmed the land in partnership. Another (strong) possibility is that not all of the brochs were in use at the same time.
Fig.3 Caithness broch territories, using a figure of 1.5km for the territory diameter
Fojut suggests two possibilities for the observed
distribution in Shetland:
a)
brochs were located with regard to the siting of their
neighbours
b)
brochs were located with regard to the physical environment
It has been remarked at various times that brochs form
invisible chains across the landscape, presumably to allow rapid visual
communication, for example in case of surprise attack. This concept arose when
brochs were still thought of as Celtic watchtowers against Viking invasion.
Fojut clearly demonstrates that such lines of communication do not exist in
Shetland and goes on to say that brochs seem to be sited so that they have a
good view of the immediate surroundings, with less regard paid to distant
prospects.
So we can assume that, in the majority of cases, brochs were
located with regard to the physical environment. Environmental quality depends
on a number of factors such as soil quality, water supply and availability of
building material. Proximity to the coast may also have been a factor in some
regions. Fojut’s conclusion was that soil quality was the most influential
factor, suggesting that it was only thriving agricultural communities that had
the necessary wherewithal to erect these monuments. The rest of the population
had to make do with their existing huts and duns.
There is a high degree of preference for coastal locations
in Shetland, but this may be due simply to the lack of good agricultural land
further inland. Broch density is just as high in parts of central Caithness as
it is on the coast. Where brochs are located on the coast, they are often in
cliff-top locations, without direct access to the sea.
We have seen that most broch communities existed in close
proximity to agricultural land, but what of the location of the broch within
that community? In many cases the site chosen was an elevated one, often on the
side of a valley, and possibly at the border between the arable land and the
rough pasture. It is likely that such a site would have been closer to suitable
building material than one situated down in the valley. Defensibility was also
important. Of 75 Shetland brochs, Fojut found that only 4 were not on good
defensive sites.
What of the population associated with each broch? Fojut has
calculated that for each of the twelve most southerly Shetland brochs, the
associated land could have produced enough grain to feed a population well in excess
of one hundred. Of course if much of the land was given over to grazing, the
productivity would have been much less. Those communities with access to the
sea would in general have needed less land than their inland neighbours. In
general the rule seems to have been ‘a little arable, plenty of grazing and
access to the shore’.
Reference
Noel Fojut, 'Towards a geography of Shetland brochs', Glasgow Archaeological Journal, 9 (1982) 38-59
How do you feel this fits in with the distribution of Skye brochs? Difficult to know which were good areas land - much of what looks like very rough pasture today was cultivated less than 100 years ago.
ReplyDeleteLooking just at brochs, rather than Duns, promontory enclosures and other similar structures - here is a list of distance from the sea, in km, extracted from Anne Macsween's "The Brochs, Duns and Promontory Enclosures of Skye" (1985)
Broch name Distance from the Sea
Boreraig, Dunvegan -
Fiadhairt -
Flashader 0.4
Kingsburgh 0.4
Ard an t'Sabhail 0.8
Borrafiach 0.8
Colbost 0.8
Flodigarry 0.8
Garsin 0.8
Gearymore 0.8
Greanan 0.8
Beag, Struan 1.2
Edinbain 1.2
Hallin 1.2
Osdale 1.2
Raisaburgh 1.2
Sleadale 1.2
Glen Heysdal 2
Suledale 2.4
Arkaig 4.4
Borve, Snizort 5.6
I see no reason why Fojut's findings shouldn't apply to Skye, but I think that the prosperity of our broch builders had a lot to do with access to sheltered sea lochs (Dunvegan, Bracadale, Greshornish, Snizort).
ReplyDeleteNeed to find out a bit more about climate change - I gather climate deteriorated after the bronze age - became wetter - which might make some difference in which was good land and which was less good for cultivation. This in turn could make people more territorial - keener to keep hold of the best land and make sure no-one lese grabbed any. So far haven't found much evidence for the climate change - just the odd comment.
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