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Arenig Fawr, Merioneth - Royal Commission on the Ancient and ...

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1.0 Introducti<strong>on</strong><br />

The <str<strong>on</strong>g>Arenig</str<strong>on</strong>g> <str<strong>on</strong>g>Fawr</str<strong>on</strong>g> upl<strong>and</strong>s archaeology survey area centres <strong>on</strong> <strong>on</strong>e of <strong>the</strong> highest peaks<br />

of sou<strong>the</strong>rn Snowd<strong>on</strong>ia, to <strong>the</strong> west of Llyn Tegid <strong>and</strong> south-west of Llyn Celyn, in <strong>the</strong><br />

communities of Llanycil <strong>and</strong> Llanuwchllyn (fig 1). The combined survey area was<br />

approximately 32.5 square kilometres.<br />

The l<strong>and</strong>scape is dramatic, characterised by a large natural lake <strong>and</strong> its craggy<br />

precipitous slopes, <strong>the</strong> steepest of which were excluded from <strong>the</strong> survey area. It is<br />

principally a moorl<strong>and</strong> l<strong>and</strong>scape of hea<strong>the</strong>r, bracken <strong>and</strong> grass <strong>on</strong> <strong>the</strong> slopes of <str<strong>on</strong>g>Arenig</str<strong>on</strong>g><br />

<str<strong>on</strong>g>Fawr</str<strong>on</strong>g>, Mynydd Nodol <strong>and</strong> Moel Llyfnant, <strong>the</strong> summits of which are 854m AOD, 539m<br />

AOD <strong>and</strong> 751m AOD respectively. Llyn <str<strong>on</strong>g>Arenig</str<strong>on</strong>g> <str<strong>on</strong>g>Fawr</str<strong>on</strong>g> is a natural lake <strong>on</strong> <strong>the</strong> sheltered<br />

east side of <strong>the</strong> <str<strong>on</strong>g>Arenig</str<strong>on</strong>g> <str<strong>on</strong>g>Fawr</str<strong>on</strong>g> ridge. The geology of <str<strong>on</strong>g>Arenig</str<strong>on</strong>g> <str<strong>on</strong>g>Fawr</str<strong>on</strong>g>, which is directly<br />

relevant to extractive industries, comprises volcanic rocks, mainly in <strong>the</strong> form of ashes<br />

<strong>and</strong> agglomerates derived from lava flows, overlain in places by Ordovician shales.<br />

Igneous intrusi<strong>on</strong>s, in <strong>the</strong> form of granite, are found <strong>on</strong> <strong>the</strong> north side of <str<strong>on</strong>g>Arenig</str<strong>on</strong>g> <str<strong>on</strong>g>Fawr</str<strong>on</strong>g>.<br />

A large proporti<strong>on</strong> of <strong>the</strong> survey area is comm<strong>on</strong> l<strong>and</strong> bel<strong>on</strong>ging to <strong>the</strong> Crown Estates,<br />

but has been fenced into large sheepwalks by <strong>the</strong> comm<strong>on</strong>ers. Those areas in private<br />

ownership are of similar moorl<strong>and</strong> character but, except for <strong>the</strong> steep ground <strong>on</strong> <strong>the</strong><br />

west flank of <str<strong>on</strong>g>Arenig</str<strong>on</strong>g> <str<strong>on</strong>g>Fawr</str<strong>on</strong>g> <strong>and</strong> <strong>the</strong> moorl<strong>and</strong> north-west of Moel Llyfnant, are enclosed<br />

with dryst<strong>on</strong>e walls. A detached area of comm<strong>on</strong> l<strong>and</strong> <strong>on</strong> <strong>the</strong> north-west side of Bala,<br />

known as Gwastadros, has <strong>the</strong> same moorl<strong>and</strong> vegetati<strong>on</strong>, with frequent boggy areas,<br />

but is lower, rising <strong>on</strong>ly to 360m AOD, <strong>and</strong> is not enclosed.<br />

With <strong>the</strong> excepti<strong>on</strong> of Gwastadros, <strong>the</strong> survey area is a Site of Special Scientific<br />

Interest, <strong>and</strong> falls within <strong>the</strong> Migneint-<str<strong>on</strong>g>Arenig</str<strong>on</strong>g>-Dduallt Special Protecti<strong>on</strong> Area for its<br />

ornithological interest, <strong>and</strong> is a Special Area of C<strong>on</strong>servati<strong>on</strong> <strong>on</strong> account of its<br />

important habitat types (blanket bog, dry heath, peat-stained lakes <strong>and</strong> pools). The<br />

whole of <strong>the</strong> survey area is within Snowd<strong>on</strong>ia Nati<strong>on</strong>al Park <strong>and</strong> <strong>the</strong> majority is<br />

designated as Access L<strong>and</strong>.<br />

The field survey was undertaken between May <strong>and</strong> October 2010 by Richard Hayman<br />

<strong>and</strong> Wendy Hort<strong>on</strong>, with grant in aid from RCAHM Wales under <strong>the</strong> Upl<strong>and</strong>s<br />

Archaeology Initiative.<br />

2.0 Methodology<br />

The project aimed to identify <strong>and</strong> record <strong>the</strong> resource through rapid, systematic field<br />

survey. Archaeological remains of all periods were c<strong>on</strong>sidered equally. RCAHM Wales<br />

undertook aerial photograph mapping of <strong>the</strong> area, which was c<strong>on</strong>sulted through <strong>the</strong><br />

fieldwork phase. The regi<strong>on</strong>al Historic Envir<strong>on</strong>ment Record was c<strong>on</strong>sulted prior to <strong>the</strong><br />

fieldwork, which yielded records of 26 archaeological sites) <strong>and</strong> RCAHM Wales<br />

provided digital copies of <strong>the</strong> county series Ordnance Survey maps at 6-inch <strong>and</strong> 25-<br />

inch scales. Ti<strong>the</strong> surveys were also c<strong>on</strong>sulted, but a search did not discover any useful<br />

estate maps covering <strong>the</strong> area that have not previously been discussed.<br />

The area was divided into transects 30m apart, except in areas where archaeological<br />

sites were sparse. These were divided into 50m transects. The locati<strong>on</strong> (NGR) of each<br />

1

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