Mynydd Llangynidr
| Mynydd Llangynidr | |||
| Brecknockshire | |||
|---|---|---|---|
 Mynydd Llangynidr lloking towards Pen y Fan and Corn Du | |||
| Range: | Brecon Beacons | ||
| Summit: | 1,831 ft SO123151 51°49’40"N, 3°16’22"W | ||
Mynydd Llangynidr is a mountain in southern Brecknockshire, within the Brecon Beacons National Park. It is named from the village of Llangynidr which sits in the valley of the River Usk to the north of it. It is essentially an undulating plateau rising in the west to a height of 557m at Garn Fawr at OS grid ref SO123151. A secondary high point is achieved at a point marked by a trig point at SO147159. To the north the hill overlooks the valleys of Dyffryn Crawnon and Cwm Claisfer, themselves tributary valleys of the Usk. The shallow upper valley (Cwm Carneilw) of the Ebbw River reaches into the plateau in the south-east whilst the upper reaches of the Sirhowy Valley and its tributary the Nant Trefil define its western margins. A further tributary, the Nant Milgatw, reaches in from the south whilst the sharp edge of Rassau Industrial Estate also defines a part of its southern margin. Passing east across the B4560, the hill merges with Llangattock Mountain which has a similar character.[1]
Geology
Mynydd Llangynidr is formed from a layer cake of Palaeozoic Era sandstones and limestones which dip gently southwards into the South Wales Coalfield basin. Broken cliffs of Carboniferous Limestone occur along the northern edges and this rock underlies the entire mountain. The plateau is formed from coarse sandstones ('gritstones') also dating from the Carboniferous Period and which have foundered in many places as the underlying limestone has dissolved over millennia. The larger part of the mountain has a pock-marked appearance due to the hundreds of shakeholes in its surface arising from the presence of the limestone beneath the sandstone cover. The frequently conglomeratic sandstones of the central and northern parts of the hill are the Twrch Sandstone, also often still referred to by its earlier name, the Basal Grit. The less frequently exposed sandstone of the southern part is the lowermost Westphalian age Farewell Rock which forms the base of the Coal Measures.
Caves
The most celebrated cave on Mynydd Llangynidr is Ogof Fawr or Chartist Cave (or sometimes 'Chartists Cave'), so named as it was reputed to be a hiding place for the Chartists, situated 500 yards to the east of the top of Garn Fawr. The Carno Adit is a major horizontal tunnel driven beneath the mountain from the south. It intersects a cave system and has provided useful additional information about the area's geological make-up.[2] Other caves include Ogof Cynnes ('warm cave') whose small entrance lies in an elongate shakehole at SN140154 [3] and Crescent Cave not far from Chartist Cave at SN129151.[4]
Conservation designation
The area was proposed for designation as a site of special scientific interest in August 2012 in respect of its karstic geomorphology. The SSSI citation makes reference to the doline field, describing the site as a part of 'the best British example of an interstratal karst'. The SSSI extends to 2,216 acres.[5] The designation process was completed in February 2013.
Quarrying
A couple of major limestone quarries intrude upon the mountain. There is an active quarry at Trefil whilst that at Blaen Onneu in the north-east has not been worked since the 1980s. There are also a few small quarries for limestone which predate the larger workings. Some small scale mining of ironstone was also carried out near the head of Cwm Carneilw before the middle of the nineteenth century. [6] There are a handful of small abandoned workings for sandstone in the Farewell Rock outcrop on the hill's eastern margin in the vicinity of the Beaufort Road.
Archaeology
There are numerous ancient cairns on this tract of moorland, the most notable of which are Garn Fawr ('big cairn') and Carn Caws ('cheese cairn'). Other prehistoric cairns and a stone row together with evidence of house platforms occur towards its northern edge.
Access
The mountain is mapped as open country and therefore freely available for walkers to roam at will. There are few defined paths though two public footpaths cross from north to south from Llangynidr towards Tredegar. The B4560 road from Garnllydan to Llangynidr cuts across the high moorland to the east of the mountain and offers the easiest access to both Mynydd Llangynidr and to Llangattock mountain to its east. To the west a minor road heads north from the A465 Heads of the Valleys Road through the small village of Trefil and continues north as a bridleway, also offering easy access to the hill.
Outside links
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("Wikimedia Commons" has material about Mynydd Llangynidr) |
References
- ↑ Ordnance Survey Explorer map OL13 'Brecon Beacons National Park: eastern area'
- ↑ British Geological Survey 1:50,000 map sheet 232 'Abergavenny' & accompanying memoir
- ↑ Cambrian Cave Registry entry
- ↑ Cambrian Cave Registry entry
- ↑ Site of Special Scientific Interest Citation, Countryside Council for Wales, 2012
- ↑ Cassini Historical Map Old Series 161 The Black Mountains facsimile Ordnance Survey 1" scale mapping from 1830's Cassini Publishing Ltd (2006)