Henry Williams : The Glasbury Bellfounder, and the production and tuning of bells
- Authors: Lewis, Colin A
- Date: 2012
- Language: English
- Type: Book chapter
- Identifier: vital:6159 , http://hdl.handle.net/10962/d1004779 , Full text available to the end of Chapter 2
- Description: The production and tuning of church bells is described before attention is paid to Henry Williams, the Glasbury bellfounder who died in 1722, and his bells. The bells of TP, his apparent successor are also described. Henry Williams was probably a member of the Williams family of Gwernyfed and was born c 1635. His presumed family connections are described. Bells known to have been cast by Henry Williams between 1677 and 1719 are listed; their distribution depicted; and their qualities assessed. The inventory of Williams' possessions at the time of his death is presented and discussed. Bells cast by TP during a brief foray into bell founding, apparently 1738-40, are described and their qualities assessed. TP was probably Benjamin Tanner (T), the industrialist specialising in iron production who succeeded Williams at the Pipton forge (P) in Aberllynfi parish near Glasbury, or Tanner (T) and Samuel Prichard (P). Prichard was the grandson of Henry Williams and his sole executor. , A complete copy of this book is available at The Whiting Society of Ringers at: http://www.whitingsociety.org.uk
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Recognition and development of the Irish Draught horse
- Authors: Lewis, Colin A
- Date: 2005
- Language: English
- Type: Book chapter
- Identifier: vital:6728 , http://hdl.handle.net/10962/d1007163
- Description: The number of horses in Ireland had shown remarkable consistency from 1861 until just before 1951. Between the end of the Second World War and 1951 there was a rapid decrease in the number of working horses, and the rate of the decrease accelerated during the decade of the 1950s and the early 1960s. Throughout the 1960s popular emphasis was placed on mechanisation, as if there were no role for the horse as a working animal. Even the production of pleasure horses seems to have been initially regarded as of little value. The 1970s were a sad period for both light and heavy draught horses in County Cork, as in the rest of Ireland. With increased mechanisation, the market for heavy draught animals which had previously dominated transport in the city of Cork, came to an end. There was a great danger that the Irish Draught would soon become extinct, so the formation of the Irish Draught Horse Society in 1976 was of great importance for the development of the Irish Draught as a breed. In 1982 this society published the "Breed Standard and Guideline", the first time that an official standard had been published for an Irish Draught. Despite various schemes during the 1980s and 1990s designed to increase the number and improve the quality of the Irish Draught horse population, it is, at the beginning of the 21st Century, one of the world's endangered breeds.
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The glaciations of Wales and adjacent areas, Introduction and Chapter 8: The upper Wye and USK regions
- Authors: Lewis, Colin A , Thomas, G S P
- Date: 2005
- Language: English
- Type: Book chapter
- Identifier: vital:6727 , http://hdl.handle.net/10962/d1007160
- Description: [From the preface]: The landscapes of Wales and adjacent areas have been profoundly influenced by glaciation. Much attention has been paid to the origins of the Welsh landscape, and, especially, to its morphology. This book, like its predecessor, "The glaciations of Wales and adjoining regions", published in 1970, aims to encourage and guide further research into the glacial history of Wales and its borderlands. [From Chapter 8]: Mid-Wales was probably glaciated on at least two occasions during the Pleistocene. The glacial sediments and landforms discussed in this chapter appear to be of Late Devensian age. The scale of glaciation during the Late Devensian varied from ice-sheet to cirque glacier in size. During glaciation the mid-Wales ice-sheet shrank to become two major valley glaciers, those of the Wye and the Usk. The age of deglaciation, especially in the Wye drainage basin, is a matter for debate and much absolute dating is still needed.
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