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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 names are of 2 classes - those holding lands in the county & those marked "test," who witness local charters and are found in the documents amongst local names. This third stage in the development of the coalfield inaugurated a whole succession of new colliery schools, most of which were located in the two Rhondda Valleys whilst many others were established in other colliery districts. Major Rugg kindly provided the necessary labour and has since deposited the finds in the National Museum of Wales.

There are no names connected with the ecclesiastical foundations. Stormy Down, a wind-driven stretch of heath, overgrown largely with scrub & pitted and broken by old and new quarry workings, borders the main road between Bridgend & Pyle, some 1.5 miles from the latter place (see 1).

Small-scale maps of Glamorgan & South Wales were the strip-maps of main roads 1st evolved as a cartographic medium by John Ogilby in 1675 - these held sway well into the 18th century. Their prosperity depended essentially upon the availabilty & supply of cheap coal and most of the larger iron & copper works had their own collieries.

Ogilby used the scale of 1 inch to the mile which had immense consequences. But collieries in this category had no schools, since the colliers' children attended the iron or copperworks schools eg.

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.

It was not possible to place in contact with this portion a fragment of the frontal bone which was present.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.The coverstone, a large slab of Pennant sandstone, the source of which was probably not more than 2 miles away (I have to thank Dr. This earth was cleared out with some difficulty, care being taken to leave the skeleton as far as possible undisturbed. The earth in the grave contained a number of snail-shells. S., as belonging to two species; Cepaea hortensis (Muller) & Cepaea nemoralis (Linne).The skeleton was found to be one of large size, strongly flexed, and lying on the left side, with head to the north (see fig.3). Those preserved have been indentified by my colleague, Mr J. The flint was found behind the pelvis of the skeleton (at the point A in fig.3) but its position, near the surface of the soil filling the grave, makes it practically certain that the implement was not in direct association wit the skeleton. A flint "knife" of somewhat similar type is said to have been found with a Beaker burial in Riley's Tumulus, on Merthyr Mawr Warren (Arch.

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The site is depicted & annotated as "Old Windmill" on OS 25" County Series Map of 1877 with an apparently working windmill some 100m to the south where there are 2 buildings annotated "Windmill" - it's not clear if this is just the name given to the buildings or if there was indeed a working windmill there. During the 18th century, Sir Humphrey Mackworth's Charity School at Neath for his miners' children & Nevill's Free Schools at Llanelly during the early years of the 19th century wre the earliest.

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