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Neolithic and Bronze Age Landscapes of North Mayo: Report 2011

Neolithic and Bronze Age Landscapes of North Mayo: Report 2011

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Bungurra River drains the Knocknalower valley floor in a <strong>North</strong>west direction <strong>and</strong> then turns South<br />

to drain the lowl<strong>and</strong>s East <strong>of</strong> Faulagh hill, before flowing into the <strong>North</strong>east corner <strong>of</strong> Carrowmore<br />

Lake.<br />

Present day settlement <strong>and</strong> farml<strong>and</strong> totals 1650ha, or 31% <strong>of</strong> the area, while blanket bog covers<br />

3,635 ha (69%). The major block <strong>of</strong> present day settlement is on the lowl<strong>and</strong> along the West coast,<br />

the West slope <strong>of</strong> Gortmelia hill, the Owenduff valley floor <strong>and</strong> the lower Southwest slope <strong>of</strong><br />

Dooncarton hill. A continuous narrow b<strong>and</strong> <strong>of</strong> settlement stretches along the <strong>North</strong> <strong>and</strong> <strong>North</strong>east<br />

coast from Dooncarton townl<strong>and</strong>, through Barnaguillew, Carnhill <strong>and</strong> Pollatomish, to Aghoos.<br />

Elsewhere, the present day settlements are in the form <strong>of</strong> small, fairly fertile oasis within the<br />

bogl<strong>and</strong>. These isl<strong>and</strong>s include the l<strong>and</strong> adjacent to the Glenamoy River, close to Bellanaboy bridge,<br />

the lower South slope <strong>of</strong> Faulagh hill, the East slope <strong>of</strong> Knocknalower hill <strong>and</strong> a b<strong>and</strong> <strong>of</strong> l<strong>and</strong> that<br />

stretches from the <strong>North</strong>west corner <strong>of</strong> Carrwomore Lake to Barnatra.<br />

Turbary, or the practice <strong>of</strong> turf cutting, is generally practised in close proximity to the present<br />

settlements. This is most evident in the case <strong>of</strong> the West <strong>and</strong> Southwest slopes <strong>of</strong> Dooncarton hill<br />

<strong>and</strong> most <strong>of</strong> Gortmelia hill, which are close to the quite densely settled villages <strong>of</strong> Dooncarton,<br />

Graghil, Gortbrack, Inver <strong>and</strong> Gortmelia. These villages were even more densely settled in prefamine<br />

times. Elsewhere, turbary is normally practised on South <strong>and</strong> West hillslopes, to facilitate the<br />

drying <strong>of</strong> the turf <strong>and</strong> on bogl<strong>and</strong> that is in close proximity to roads. Completely cut-away tracts <strong>of</strong><br />

bogl<strong>and</strong> are present on the two previously mentioned hillslopes, on the slopes <strong>of</strong> Carrowmore hill,<br />

on the Southwest slope <strong>of</strong> Faulagh hill <strong>and</strong> on the South slope <strong>of</strong> Knocknalower hill. The major<br />

continuous tract <strong>of</strong> uncut bog covers the lowl<strong>and</strong> in the East <strong>of</strong> the study area, the summit <strong>and</strong><br />

<strong>North</strong> <strong>and</strong> East slopes <strong>of</strong> Faulagh hill, the Southeast spur <strong>of</strong> Faulagh hill <strong>and</strong> the lowl<strong>and</strong> between<br />

Faulagh <strong>and</strong> Pollatomish hills. An exception here is the turbary practised on the low-lying bog in<br />

Aghoos townl<strong>and</strong>. Part <strong>of</strong> the surface <strong>of</strong> the low-lying, eastern bog is now planted with coniferous<br />

forest. The other areas <strong>of</strong> uncut bog cover the summit <strong>and</strong> <strong>North</strong> slope <strong>of</strong> Knocknalower hill, large<br />

areas <strong>of</strong> the summit <strong>and</strong> South to Southeast slopes <strong>of</strong> Dooncarton hill, the upper slopes <strong>of</strong><br />

Pollatomish hill <strong>and</strong> the low-lying area between Gortmelia <strong>and</strong> Carrowmore hills.<br />

Evidence <strong>of</strong> prehistoric forest cover in the area is gained from the extensive remains <strong>of</strong> tree stumps,<br />

trunks <strong>and</strong> branches, predominantly <strong>of</strong> pine <strong>and</strong> birch, but with some oak, preserved in their levels<br />

<strong>of</strong> growth either in lower layers <strong>of</strong> the bog or under it. A b<strong>and</strong> <strong>of</strong> bog containing such remains covers<br />

125

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