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Relevant bibliographies by topics / Ffestiniog, Vale of (Wales)

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Academic literature on the topic 'Ffestiniog, Vale of (Wales)'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "Ffestiniog, Vale of (Wales)"

1

Hawkins, T. R. W., and F. G. Jones. "Fold and cleavage development within cambrian metasediments of the vale of ffestiniog, North Wales." Geological Journal 16, no. 1 (2007): 65–84. http://dx.doi.org/10.1002/gj.3350160107.

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2

Gwyn, David. "The Landscape Archaeology of the Vale of Ffestiniog." Industrial Archaeology Review 27, no. 1 (2005): 129–36. http://dx.doi.org/10.1179/030907205x50478.

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3

LUCAS, PETER. "Jigsaw with pieces missing: Charles Darwin with John Price at Bodnant, the walking tour of 1826 and the expeditions of 1827." Archives of Natural History 29, no. 3 (2002): 359–69. http://dx.doi.org/10.3366/anh.2002.29.3.359.

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ABSTRACT: Darwin seems to have paid two visits to John Price, Welsh speaking school friend of both Darwin brothers, at his family's home, Bodnant in North Wales. In June 1826 with Nathan Hubbersty he stayed at Bodnant on the walking tour of North Wales which took them to Ffestiniog, Snowdon and other places. In July 1827, the fragmentary evidence strongly suggests, both Darwin brothers, Erasmus and Charles, stayed at Bodnant with expeditions to the Great Ormes Head, near Llandudno, and west across the Conwy river to the Carneddau range. The visits serve as a reminder of the wealth of topograph

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4

Bromley, Alan V. "A volcanic vent in the tremadocian rocks southeast of Blaenau ffestiniog, Merionethshire, North Wales." Geological Journal 6, no. 1 (2007): 7–12. http://dx.doi.org/10.1002/gj.3350060103.

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5

Cope, J. C. W., and A. W. A. Rushton. "Cambrian and early Tremadoc rocks of the Llangynog Inlier, Dyfed, South Wales." Geological Magazine 129, no. 5 (1992): 543–52. http://dx.doi.org/10.1017/s0016756800021701.

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AbstractUntil recently no Cambrian rocks were known in the Llangynog area. Detailed mapping has now revealed a succession of ?Lower and Upper Cambrian rocks overlain by Tremadoc rocks. The Allt y Shed Sandstones (new) rest unconformably on the Precambrian, but have yielded no diagnostic fossils and are tentatively assigned to the Comley Series. Succeeding with faulted or unconformable contact is an Upper Cambrian Merioneth Series succession which includes in ascending order: conglomerates, sandstones and siltstones with olenid trilobites and resembling the Treffgarne Bridge Beds of the Haverfo

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6

Young, T., F. Martin, W. T. Dean, and A. W. A. Rushton. "Cambrian stratigraphy of St Tudwal's Peninsula, Gwynedd, northwest Wales." Geological Magazine 131, no. 3 (1994): 335–60. http://dx.doi.org/10.1017/s0016756800011109.

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AbstractLithostratigraphic units of early to late Cambrian age established by T. C. Nicholas in 1915 in the St Tudwal's Peninsula are revised. They comprise, in ascending order: Hell's Mouth Formation (> 190 m); Trwyn y Fulfran Formation (37 m);Cilan Formation (400 m); Ceiriad Formation (40 m seen); Nant-y-big Formation (> 110 m seen); Maentwrog Formation (in part, 50 m seen, an estimated 250 m concealed); Ffestiniog Flags Formation (in part, c. 120m seen). The ‘calcareous grit’ at the top of Nicholas's Nant-pig Mudstones spans the unconformable boundary between the Nant-y-big and Maentw

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7

Williams, D. E. "St Paul's Footbridge, Ebbw Vale, Wales—landmark structure." Proceedings of the Institution of Civil Engineers - Bridge Engineering 159, no. 2 (2006): 77–81. http://dx.doi.org/10.1680/bren.2006.159.2.77.

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8

LUCAS, PETER. "“A most glorious country”: Charles Darwin and North Wales, especially his 1831 geological tour." Archives of Natural History 29, no. 1 (2002): 1–26. http://dx.doi.org/10.3366/anh.2002.29.1.1.

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Darwin's tour with Adam Sedgwick in 1831, the last of some 14 Welsh visits before the Beagle voyage, divides into three periods: a week, mostly with Sedgwick, from 5 August; a middle period ending by 20 August, when Sedgwick left Anglesey; and a final period during which Darwin spent some days in Barmouth, reaching Shrewsbury on 29 August. His activities are well documented, for the first period, through both men's geological notes and, for the last, in the journal of the Lowe brothers (showing Darwin reaching Barmouth from Ffestiniog on 23 August and parting from Robert Lowe on 29 August). Fo

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9

BROOKS, M., M. MILIORIZOS, and B. V. HILLIER. "Deep structure of the Vale of Glamorgan, South Wales, UK." Journal of the Geological Society 151, no. 6 (1994): 909–17. http://dx.doi.org/10.1144/gsjgs.151.6.0909.

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10

Simmons, J. E. L., R. T. Knox, and W. O. Moss. "The development of PTFE (polytetrafluoroethylene)-faced hydrodynamic thrust bearings for hydrogenerator application in the United Kingdom." Proceedings of the Institution of Mechanical Engineers, Part J: Journal of Engineering Tribology 212, no. 5 (1998): 345–52. http://dx.doi.org/10.1243/1350650981542155.

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Polytetrafluoroethylene (PTFE)-faced hydrodynamic thrust bearings have been used for many years in the former Soviet Union and in the People's Republic of China for large hydrogenerator applications. Although there has been some recent interest in other countries, few installations of this sort have previously been reported in Europe or the USA. This paper describes the state of the art and the development and laboratory testing of a prototype set of PTFE pads. Following these trials, a second larger set of thrust pads was designed for use in the pumped-storage hydroelectric power station at F

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