By Stanley Williamson
"An clever and well-informed documentary narrative of the catastrophe and the authentic inquiry."—The monetary background Review
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Extra resources for Gresford: The Anatomy of a Disaster
The 1840s in North Wales were a watershed in more ways than one,4 for by the time an economic revival had taken place the main current of industrial development had, like the channel of the Dee, shifted its course. The iron industry had largely moved away to areas such as the Black Country and South Wales, where better communications oﬀered easier access to larger markets. Fortunately for North Wales its untapped coal resources included the proﬁtable Main Seam which was well suited for gas manufacture and household purposes and for which local outlets could be found; it is no coincidence that towns in Denbighshire and Flintshire pioneered developments such as the use of gas for street lighting.
But whatever dreams and ambitions the success of Wilkinson and his associates may have prompted the North Wales coalﬁeld was clearly destined never to play a major role in the national economy. In 1892 a correspondent to a local newspaper pointed out that North Wales contributed a mere one-and-a-half per cent of the output of all British coalﬁelds. It is against this perspective that the events of the succeeding half-century must be viewed. By the 1840s the ruthless exploitation of the more easily accessible deposits on the western upland of the coalﬁeld had exhausted them, and technical problems, chieﬂy ﬂooding, had brought production at other pits to a halt.
CHAPTER 3 The Coalﬁeld The North Wales coalﬁeld extends in a shallow arc from the Point of Ayr, at the north-western tip of the Dee estuary, southward through Clwyd (formerly Flintshire and Denbighshire), and ends a mile or so inside the boundary of Shropshire, near Oswestry. It is about 45 miles long and 9 miles across at its widest point. The geological strata in this corner of Wales dip steeply eastward, producing a sharp and dramatic landscape, as limestone outcrops north of Llangollen give way to the rounded sandstone mountains which present their long eastern slopes to the Dee Valley and the rich pasture-lands of Cheshire.