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Beacon Hill, Radnorshire - Royal Commission on the Ancient and ...

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RCAHM Wales Upl<strong>and</strong>s Initiative – <str<strong>on</strong>g>Beac<strong>on</strong></str<strong>on</strong>g> <str<strong>on</strong>g>Hill</str<strong>on</strong>g>Broad ClassNo. SitesIndustrial 45Water Supply <strong>and</strong> Drainage 11Agriculture <strong>and</strong> Subsistence 167Transport 144Religious, Ritual <strong>and</strong> Funerary 6Domestic 33Recreati<strong>on</strong>al 1Commemorative 1Civil 2M<strong>on</strong>ument by Form 9Unassigned 3Total 422Table 3: Sites grouped by Broad ClassBr<strong>on</strong>ze AgeThere are few prehistoric sites <strong>on</strong> <str<strong>on</strong>g>Beac<strong>on</strong></str<strong>on</strong>g> <str<strong>on</strong>g>Hill</str<strong>on</strong>g> comm<strong>on</strong>. No new Neolithic or Br<strong>on</strong>zeAge sites were discovered. The barrows c<strong>on</strong>form to a general pattern in <str<strong>on</strong>g>Radnorshire</str<strong>on</strong>g>whereby barrows occur east of <strong>the</strong> River Ith<strong>on</strong> <strong>and</strong> cairns occur fur<strong>the</strong>r west. A line offour round barrows (nprn 306147-306150) <strong>on</strong> <str<strong>on</strong>g>Beac<strong>on</strong></str<strong>on</strong>g> <str<strong>on</strong>g>Hill</str<strong>on</strong>g> is <strong>on</strong>e of <strong>on</strong>ly two suchgroups in <str<strong>on</strong>g>Radnorshire</str<strong>on</strong>g> (<strong>the</strong> o<strong>the</strong>r is at Cwm Difwg). Pairs of barrows, like those <strong>on</strong>Rhos Crug (nprn 306164, 306165), are more comm<strong>on</strong> (figure 2), examples of whichin <str<strong>on</strong>g>Radnorshire</str<strong>on</strong>g> are also at Cwm Bwch, Cefn Wylfre <strong>and</strong> Carneddau (J<strong>on</strong>es 2004, 164-65). On Rhos Crug <strong>the</strong>re is also an outlying barrow (nprn 306163, but outside <strong>the</strong>present survey area), which is <strong>on</strong> lower ground to <strong>the</strong> south east, bey<strong>on</strong>d a deepstream valley. This c<strong>on</strong>figurati<strong>on</strong> of an outlying barrow separated from <strong>the</strong> main pairby a natural obstacle, is also replicated at two o<strong>the</strong>r sites in <str<strong>on</strong>g>Radnorshire</str<strong>on</strong>g> (Dunn 1988,38).4

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