David Davies was born in July 1857, the youngest of ten children.
His father died when David was just seven years of age, and at the age of ten, he began working at a candle factory at Caedraw. When the factory closed, David returned to school for a short time before gaining employment at another candle factory in Victoria Street. When he was 18 he began working at the Plymouth Works Rolling Mills, and after their closure, he found employment at the Ifor Works Rolling Mills.
In 1878 he became a conductor on the London and Northwest Railway omnibuses which connected the train passengers with the Brecon and Merthyr Railway at Dowlais Central Station. When the Morlais Tunnel opened in June 1879, the buses were no longer required, so he became a porter and later signalman. He married Mary in 1881 and moved to Pant, and the couple had six children – Annie, Albert, William, Arthur, Frank and Bryn, Albert losing his life in the First World War.
A man deeply involved in local politics, fighting for an improved living standard for others, he organised a large demonstration at Cyfarthfa Park, asking for 2,000 new houses to be built. He was also a J.P., served on the Board of Guardians for nine years, was one of the founders of the Dowlais Co-operative Society (later becoming its chairman), and he was also a founder member of the Dowlais Railwaymen’s Coal Club, which had its own wagons, and by cutting out the middle-man, saved the profits for its members.
In 1919, he was the official candidate (Dowlais Ward) for the Merthyr Trades Council and Labour Party. Points of his campaign were:-
Free medical and nursing care for infants.
Clean, plentiful, cheap milk; managed by the people for the people and thus eliminating private profit.
Free meals for hungry children.
Free medical treatment for the needy and sick.
He was elected mayor in 1925-26.
David died in 1940, his principal aim in life having been to leave the town of his birth a better place than he found it.
It was not until September 1968 that I first became acquainted with ‘The Stinky’, the name given to the Morlais Brook by past generations of children and adults who lived along its banks.
Not being a Merthyr boy I was really unaware of its existence, let alone details of its course and history. Where I lived in Troedyrhiw we had the River Taf across the fields of Bill Jones’ farm and our only brook was an old Hill’s Plymouth Collieries’ watercourse which drained numerous disused mountainside coal levels. Despite its origins, the water was clear and clean, drinkable, dammed in the summer holidays, paddled and bathed in. When bored or just at a loose end we raced empty Bondman tobacco tins along its course, running to keep up with the flow and ensure that our own particular tin wasn’t held up by a fallen branch or trapped in an inconvenient eddy. On first encounter I couldn’t imagine any of those activities taking place along ‘The Stinky’ and my initial observations confirmed that its local name was not in any way exaggerated. Indeed, the name appropriately characterised some of its more sinister and less praiseworthy qualities.
The stretch I first got to know was, what a student of physical geography would term, the stream’s ‘Old Age’, that is the portion towards the end of its life. Indeed, one might say at its very death, for union with the parent Taf was imminent and in 1968 the confluence of the two was observable, not as now concealed beneath a highway and pedestrian pathway. To the south of the stream were some of the streets and courtways of the town, many of which were derelict and already marked as candidates for slum clearance. Within two or three years these would be swept away. Rising up from its northern bank was the huge tip of waste produced over a century earlier by the Penydarren Ironworks, its industrial waste concealed for the most part by surprisingly lush vegetation. The British Tip, as it was sometimes known, took its name from the British and Foreign Bible Society, founders of the academy which graced its summit. On its plateau top was a once grand construction, a building of a century’s age but which in many respects had seen better times. Abermorlais, the school’s official name, was most appropriate, as it proclaimed its location, at the union of Taf and Nant Morlais. Unfortunately, there was to be seen no evidence in the stream here of a course well run, more confirmation of ill use, where Sixties’ waste and detritus continued to be added to over a century’s massive abuse. A sad end indeed to what no doubt had once been in pre-industrial times a clear and unspoilt mountain stream.
A map from the 1860s showing the Morlais Brook (flowing East to West) entering the Taff (flowing North to South). Abermorlais School is shown overlooking the scene.
Perhaps though, to gain a more comprehensive appreciation of the stream’s course, it is probably better to follow the guidance of another Thomas, and “begin at the beginning”.
Nant Morlais forms from numerous small tributaries on the slopes of Twynau Gwynion and Cefnyr Ystrad on the 560 metre contour above Pantysgallog and Dowlais. In a distance of seven and a half kilometres it descends 440 metres to its confluence with the Taf. It’s not easy walking country with the gently dipping beds of Millstone grit overlying the Carboniferous Limestone. The surface is rough with ankle breaking rocks and many sink holes to topple into. Among many, but by far the largest of these is Pwll Morlais, a deep and supreme example of what happens where the underlying Limestone has been eroded and the grit collapses into the void. Depending on the season this can be a steep sided, empty peat banked hole or after heavy rain, full to overflowing with a brew of brown froth. The song of the skylark can be enjoyed here on a fine summer day but it is also a solitary place, disconcerting or eerie even, when mist or low cloud descends and the lone walker is surprised by the frantic cry of a disturbed snipe.
Pwll Morlais. Photo Clive Thomas
On a clear day the view to the south is the trough of the Taf Valley. Always viewed into the sun so never really clear, with only silhouettes, shadows and reflections to give a hint of detail. One wonders how different it would have looked when all of the works below would have been at their height?
From Pwll Morlais, the stream is called Tor-Gwyn by the Ordnance Survey, until its junction with another parallel tributary, and thereafter it becomes Nant Morlais proper. The stream’s descent is gentle to begin with over the hard resistant gritstone. It is along this stretch that there is much evidence of the importance placed on the brook as a source of water power for the rapidly growing Dowlais Works during the early part of the nineteenth century. There are still the remains of sluices and numerous places where the course has been altered, or feeders led its water off to be stored in numerous hillside reservoirs.
Sluice where water was diverted from the stream into the Pitwellt Pond. Photo Clive Thomas
Where one of these diversions fed the extensive but now dry Pitwellt Pond above Pengarnddu, the Brook leaves the Millstone Grit and begins to cut a deep gorge into the softer Coal Measure rocks. From here there is more urgency in its flow, its course becomes narrower and more confined. At several locations it caused railway builders of the past to pause and consider the inconvenience of its course which would necessitate the construction of embankments and small bridges. The line which took limestone to the ironworks at Rhymney crossed hereabouts, as did the Brecon and Merthyr Railway on its way north over the Beacons and the London and North Western on its descent into Merthyr Tydfil via the ‘Miler’ or Morlais Tunnel.
The stream cuts down into some of the softer beds of the Coal Measures. Photo Clive Thomas
More significantly however, it is within this section of the stream that geologists have been able to discover some of the secrets of the South Wales Coalfield and probably many hundreds of school pupils, university students, and local amateur geologists will have benefitted from the instruction of teachers like Ron Gethin, Tom Sharpe or John Perkins. Like myself on many occasions I am sure, they have stumbled down its steep banks into the course of the stream below Blaen Morlais Farm in search of Gastriocerassubcranatum or Gastriocerascancellatum . Not valuable minerals these, but the important fossils which would indicate the location of one or other of the marine bands which were significant in determining the sequence of sedimentation of the rocks generally, and the coal seams in particular.
By the second half of the 19th century, Merthyr was served by several railway companies, one of which was the Brecon and Merthyr Tydfil Junction Railway (B&M) which, as its name implies, ran from Brecon to Merthyr.
A 1905 map showing the Railways around Merthyr and Dowlais
As early as 1836, Sir John Josiah Guest, of the Dowlais Ironworks, had written of his proposal to construct a railway linking Dowlais to the valley of the River Usk, and possibly also running into Brecon. The line would have pretty nearly covered the same route as was eventually adopted by the B&M. A similar proposal suggested a line running up the Taf Fawr valley over the Brecon Beacons via Storey Arms and thence to Brecon.
The Brecon and Merthyr Railway Company was established by a Bill of 1859, financially supported by several prominent Brecon citizens, and the complete route from Brecon to Merthyr Tydfil was authorised the following year. The first section to open was a 6.75 miles (10.86 km) section between Brecon and Talybont-on-Usk in 1863, which reused a section of a horse-drawn tram line. The Beacons Tunnel at Torpantau opened in 1868. Officially named the Torpantau Tunnel, at 1313 feet above mean sea level, it is the highest railway tunnel in Britain.
The system eventually came to comprise two sections of lines:
The Southern section, effectively the consumed Rumney Railway, which linked Bassaleg (where there were connections with the GWR and the London and North Western Railway) and the ironworks town of Rhymney, near the head of the Rhymney Valley.
The Northern section linked Deri Junction by means of running powers over a section of the Rhymney Railway in the Bargoed Rhymney Valley to Pant, Pontsticill and Brecon via a tunnel through the Brecon Beacons. From the tunnel the line descended towards Talybont-on-Usk on a continuous 1-in-38 gradient known as the “Seven-Mile Bank”. For southbound trains this presented the steepest continuous ascent on the British railway network.
Initially, the only connection to Merthyr Tydfil was by means of a horse-drawn bus from Pant, but by 1868, a connection with Merthyr at Rhydycar Junction had been established by sharing lines with Vale of Neath, London and North Western and Taff Vale railways. This involved the building of nearly seven miles of single line from Pontsticill to Merthyr, with an almost continuous descent of 1 in 45-50, two complete reversals of direction, and the construction of two viaducts to carry the line over the Taf Fechan at Pontsarn, and the Taf Fawr at Cefn Coed.
North of the Pontsarn viaduct, a connection was made with the LNWR’s Merthyr Extension line at Morlais Tunnel Junction from where the latter’s double track entered the 1034 yard Morlais Tunnel and beyond routed along the double line to Dowlais High Street and thence to Tredegar, Brynmawr and Abergavenny. The sections from Merthyr to Pontsticill and Bargoed through to Brecon were laid as single lines with passing loops and usually locomotive watering facilities at principal stations. For those single lines, tokens were issued to drivers from signal boxes at such locations and being essential for safe working over single lines.
The line was eventually amalgamated with the Great Western Railway in 1923, and by 1958, the line was running three services each way on weekdays, increasing to four on Saturdays, taking around 2½ hours to run from Brecon to Newport. Although surviving nationalisation, the service had run at a substantial loss for most of its lifetime, and was an obvious candidate for closure. Passenger services were closed from Pontsticill Junction to Merthyr Tydfil in November 1961, with the remainder of services stopping at the end of the 1962. The line was closed completely after the withdrawal of goods services in 1964.
Towards the end of the 1970s, a private company, the Brecon Mountain Railway, began to build a narrow-gauge steam-hauled tourist line on the existing 5.5-mile (8.9 km) trackbed from Pant through Pontsticill to Dol-y-gaer. The initial section of 1.75 miles (2.82 km) from Pant to Pontsticill first opened in June 1980. After more than 30 years of hard work and extra-funding, passenger services finally extended to Torpantau in April 2014, bringing the BMR to a total of approximately 5 miles in length.
For more about the Brecon Mountain Railway, please follow the link below:
David Davies was born in July 1857, the youngest of ten children.
