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A snippet of information on maps of Glamorgan - the following is from the Glamorgan section of Ogilby's strip-map "The Road from London to St David's" first published in 1675. In South Wales during the 19th century the rapid development of heavy industries & coal mining created centres of dense populations where voluntary efforts to provide education in many areas proved inadequate & ineffective.
Place names & notable buildings can be seen on this section from Aberavon to Cowbridge (A48). The characteristic feature of the industrial evolution of South Wales during the first half of the 19th century was the growth & expansion of the ferrous and non-ferrous metallurgical industries.
This is the remains of a type of primitive, shorter, parallel-sided windmill (similar to ones across the channel in Somerset). The establishment of colliery schools in South Wales followed very closely the various phases of development of coal mining.
In addition to authorities given, the comparison of the Norman names in Cal. preserved in France (Rolls Series) & Fabricius' Danske Minder i Norman-diet. For the most part above 300 feet contour-line, it forms part of an elevated limestone region which is defined on the north & east by the Rivers Kenfig and Ogmore and which to the south & west drops gradually to the sandhills of Merthyr Mawr, Newton and Kenfig.
Johannes Ascelina, 1267, p.687, Kenfig, which may be Askell suffix -in; but as there is a Norman Ascelin, Bjorkman (N. Before 1870, when the chief repsonsibility for the organisation & promotion of elementary education in England & Wales was in the hands of Voluntary Societies, large numbers of schools were also promoted or erected by proprietors of individual "works" and by large industrial companies.
The hollow in the rock was lined with blocks of limestone of various sizes to enclose an area roughly 4ft by 2ft 7in. Over the capstone had been piled up, without arrangement or method, a heap of stones of various sizes; but it was noticed that these stones did not extend downwards over the sides of the capstone into the hollow which contained the grave. The disturbance of one of the forearm bones of the right arm, which rested on the spinal column, clearly showed that the earth contained in the grave had entered after the decay of the body.
in maximum dimensions, the floor of which had been prepared for the body by a layer of oolitic limestone flakes. The removal of the capstone showed the grave to be full of comparatively clean tightly packed soil which revealed no trace on its surface of the remains it contained. The cist was too roughly built to be thoroughly earth-tight.