Mynydd Llangatwg or Llangattock Mountain is a hill in the
Brecon Beacons National Park
The Brecon Beacons National Park ( cy, Parc Cenedlaethol Bannau Brycheiniog) is one of three national parks in Wales, and is centred on the Brecon Beacons range of hills in southern Wales. It includes the Black Mountain (range), Black Mountain ...
in the county of
Powys
Powys (; ) is a Local government in Wales#Principal areas, county and Preserved counties of Wales, preserved county in Wales. It is named after the Kingdom of Powys which was a Welsh succession of states, successor state, petty kingdom and princi ...
, south
Wales
Wales ( cy, Cymru ) is a Countries of the United Kingdom, country that is part of the United Kingdom. It is bordered by England to the Wales–England border, east, the Irish Sea to the north and west, the Celtic Sea to the south west and the ...
. It is named from the village of
Llangatwg
Cadoxton (or in full Cadoxton-juxta-Neath) ( cy, Llangatwg), is a village situated in Neath Port Talbot county borough, Wales. Cadoxton is located just outside the town of Neath and borders the villages of Cilfrew and Bryncoch. The village has 1, ...
(or '
Llangattock
Llangattock ( cy, Llangatwg) is a village, community and electoral ward in the Brecon Beacons National Park in Powys, Wales. It lies in the Usk Valley just across the river from the town of Crickhowell. The Monmouthshire and Brecon Canal passe ...
') which sits in the valley of the
River Usk
The River Usk (; cy, Afon Wysg) rises on the northern slopes of the Black Mountain (''y Mynydd Du''), Wales, in the westernmost part of the Brecon Beacons National Park. Initially forming the boundary between Carmarthenshire and Powys, it fl ...
to the north of it. It is essentially an undulating plateau rising in the west to a height of at and in the east to a height of at Hen Dy-aderyn / Twr Pen-cyrn. This spot is marked by a
trig point
A triangulation station, also known as a trigonometrical point, and sometimes informally as a trig, is a fixed surveying station, used in geodetic surveying and other surveying projects in its vicinity. The nomenclature varies regionally: they a ...
. The shallow pool of Pwll Gwy-rhoc sits in a broad depression towards the northern edge of the plateau whilst a smaller pool frequently occupies a large shakehole a few hundred metres to its west. The hill forms an impressive northern scarp overlooking the Usk valley and commonly referred to as the Llangattock Escarpment. Its southern margins are more subdued. Its eastern end is defined by the drops into the
Clydach Gorge
The Clydach Gorge (also known as Cwm Clydach) is a steep-sided valley in south-east Wales down which the River Clydach flows to the River Usk. It runs for from the vicinity of Brynmawr in Blaenau Gwent eastwards and northeastwards to Gilwern ...
. Beyond the
B4560 to the west the hill merges with
Mynydd Llangynidr
Mynydd Llangynidr is a mountain in the Brecon Beacons National Park largely in the county of Powys, south Wales. Its southern slopes extend into the northernmost parts of the county borough of Blaenau Gwent. It is named from the village of Llangyn ...
which has a similar character.
Particular features of note include 'The Lonely Shepherd', an isolated limestone pinnacle which stands at the eastern tip of the plateau, left there by quarryworkers who removed great quantities of the surrounding rock. A number of cairns are scattered across the hill, notably the sizeable pair which decorate the summit of Twr Pen-cyrn and which are thought to be of
Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts ...
age. Some freshwater ponds litter the mountain, including the “witches pool”. A more recent addition to the landscape was Cairn-Mound Reservoir which once impounded the headwaters of Nant yr Hafod on the southern slopes though
Welsh Water
Welsh may refer to:
Related to Wales
* Welsh, referring or related to Wales
* Welsh language, a Brittonic Celtic language spoken in Wales
* Welsh people
People
* Welsh (surname)
* Sometimes used as a synonym for the ancient Britons (Celtic peopl ...
abandoned this some years ago and its bed has revegetated, though the embankment remains. A couple of gas pipelines have been laid across the mountain and their courses can be traced variously by fences, vegetation changes and marker poles.
Geology
Mynydd Llangatwg is formed from a layer cake of
Palaeozoic Era
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon.
The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838
by combining the Greek words ''palaiós'' (, "old") and ' ...
sandstones and limestones which dip gently southwards into the
South Wales Coalfield
The South Wales Coalfield ( cy, Maes glo De Cymru) extends across Pembrokeshire, Carmarthenshire, Swansea, Neath Port Talbot, Bridgend, Rhondda Cynon Taf, Merthyr Tydfil, Caerphilly, Blaenau Gwent and Torfaen. It is rich in coal deposits, espec ...
basin. Imposing cliffs of
Carboniferous Limestone occur along the northern escarpment and this rock underlies the entire hill and hosts the extensive cave systems which lie beneath it, notably those of
Ogof y Daren Cilau
Ogof y Daren Cilau is one of several cave systems in the Llangattock escarpment near Crickhowell in south Powys, Wales. The cave was discovered in 1957 and is one of the longest cave systems in the country.
The cave
It is one of the longest syst ...
and
Ogof Agen Allwedd
Ogof Agen Allwedd or Agen Allwedd, is, at , one of the longest cave systems in Wales, and the longest cave system on the Llangattock escarpment.
History
The cave was first investigated by Brian Price and party in 1949 and 1950, but it was not un ...
. These two systems are amongst the longest in Britain. The plateau is formed from coarse sandstones ('gritstones') also dating from the
Carboniferous Period
The Carboniferous ( ) is a Period (geology), geologic period and System (stratigraphy), system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago (Myr, Mya), to the beginning of the Permian Period, ...
and which have foundered in many places as the underlying limestone has dissolved over millennia. The sandstone forming low secondary scarps above the main northern and eastern escarpments is the frequently
conglomeratic Twrch Sandstone
The Marros Group is the name given to a suite of rocks of Namurian age laid down during the Carboniferous Period in South Wales. These rocks were formerly known as the Millstone Grit Series but are now distinguished from the similar but geographi ...
often still referred to by its earlier name, the Basal Grit. In contrast, the more poorly exposed sandstone forming the high ground of the centre of the hill is the lowermost
Westphalian age
Farewell Rock which marks the base of the
South Wales Coal Measures. Sections of the hill have a pock-marked appearance due to the dozens of
shakehole
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are locally also known as ''vrtače'' and shakeholes, and to openi ...
s in its surface arising from the presence of the limestone beneath the sandstone cover.
Quarries and tramways
The greater part of the length of the northern escarpment is scarred by limestone quarries which operated for much of the nineteenth century. The rock was removed by means of a series of
tramroads or
tramways which linked north via steep inclines to a wharf on the
Monmouthshire and Brecon Canal
The Monmouthshire and Brecon Canal ( cy, Camlas Sir Fynwy a Brycheiniog) is a small network of canals in South Wales. For most of its currently (2018) navigable length it runs through the Brecon Beacons National parks of England and Wales, Na ...
at
Llangattock
Llangattock ( cy, Llangatwg) is a village, community and electoral ward in the Brecon Beacons National Park in Powys, Wales. It lies in the Usk Valley just across the river from the town of Crickhowell. The Monmouthshire and Brecon Canal passe ...
and south to
Brynmawr
Brynmawr (; , ,) is a market town, community and electoral ward in Blaenau Gwent, Wales. The town, sometimes cited as the highest town in Wales, is situated at above sea level at the head of the South Wales Valleys. It grew with the devel ...
and the ironworks at
Nant-y-glo by two tramroads which contoured the eastern end of the hill. The upper tramway which dates from the start of the nineteenth century, runs south from Pant y Gilwern and Daren Disgwylfa and then west around the head of
Cwm Clydach. It is now a grassy footpath providing easy walking through otherwise rough terrain. The lower tramway was constructed in 1828-30 and has since been converted to a public road. Both tramroads had several branches to serve individual quarries along the escarpment. Both the Twrch Sandstone and Farewell Rock have been quarried on a small scale in the past alongside the B4560 Beaufort Road with larger quarries in the latter once operating near the hill's southwestern corner.
Access
The
B4560 road
B roads are numbered routes in Great Britain of lesser importance than A roads. See the article Great Britain road numbering scheme
The Great Britain road numbering scheme is a numbering scheme used to classify and identify all roads in Gr ...
from Garnllydan to
Llangynidr
Llangynidr is a village, community and electoral ward in Powys, Wales, about west of Crickhowell and south-east of Brecon. The River Usk flows through the village as does the Monmouthshire and Brecon Canal. It is in the historic county of B ...
cuts across the high moorland and offers the easiest access to the hill and to Mynydd Llangynidr to its west. Almost the entire hill is designated as
urban common and was mapped as open country under the provisions of the
Countryside and Rights of Way Act 2000 and therefore freely available for walkers to roam at will. There are few defined paths though a public footpath crosses from north to south passing just east of the top known as Twr Pen-cyrn. The former tramways mentioned above also provide easy level access around the margins of the hill.
References
External links
Images of Mynydd Llangatwg from Geograph website
{{coord, 51.8236, -3.1667, type:mountain_region:GB, display=title
Mountains and hills of Powys
Brecon Beacons