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Encyclopedia Britannica - Main :: DEM-DIO |
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DENBI }ISHIRE (Dinbych), a county of N. Wales, bounded N. by the Irish Sea, N.E. by Flint and Cheshire, S.E. by Flint and Shropshire, S. by Montgomery and Merioneth, and W. by Carnarvon. Area, 662 sq. m. On the N. coast, within the Denbighshire borders and between Old Colwyn and Llandulas, is a wedge of land included in Carnarvonshire, owing to a change in the course of the Conwy stream. (Thus, also, Llandudno is partly in the Bangor, and partly in the St Asaph, diocese.) The surface of Denbighshire is irregular, and physically diversified, In the N.W. are the bleak Hiraethog (" longing ") hills, sloping W. to the Conwy and E. to the Clwyd. In the N. are Colwyn and Abergele bays, on the S. the Yspytty (Lat. Hospitium) and Llangwm range, between Denbigh and Merioneth. From this watershed flow the Elwy, Aled, Clywedog, Merddwr and Alwen, tributaries of the Clwyd, Conwy and Dee (Dyfrdwy). Some of the valleys contrast agreeably with the bleak hills, e.g. those of the Clwyd and Elwy. The portion lying between Ruabon (Rhiwabon) hills and the Dee is agricultural and rich in minerals; the Berwyn to Offa's Dyke (Wdl (ea) is wild and barren, except the Tanat valley, Llansilin and Ceiriog. One feeder of the Tanat forms the Pistyll Rhaiadr (waterspout fall), another rises in Llyncaws (cheese pool) under Mod Sych (dry bare-hill), the highest point in the county. Aled and Alwen are both lakes and streams. Geology.The geology of the county is full of interest
series . In the Ordovician district, which extends from the southern boundary to the Ceiriog, the LIandeilo formation of the eastern slopes of the Berwyn and the Bala
porphyry and ashes. The same formation occurs just within the county border at Cerrig-y-Druidion, Langum, Bettys-ycoed and in the Fairy Glen. Northwards from the Ceiriog to the limestone fringe at Llandrillo the Wenlock shale of the Silurian
series , crops up along the Vale of Clwyd and in Eglwyseg. Resting upon this the Carboniferous Limestone extends from Llanymynach, its extreme southern point, to the Cyrnybrain fault, and there forks into two divisions that terminate respectively in the Great Orme's Head and in Talargoch, and are separated from each other by the denuded shales of the Moel Famma range. In the Vale of Clwyd the limestone underlies the New Red Sandstone, and in the eastern division it is itself overlaid by the Millstone Grit of Ruabon and Minera, and by a long reach of the Coal Measures which near Wrexham are 41 m, in breadth. Eastward of these a broad strip of the red marly beds succeeds, formerly considered to be Permian but now regarded as belonging to the Coal Measures, and yet again between this and the Dee the ground is occupiedas in the Vale of Clwydby the New Red rocks. As in the other northern counties of Wales, the whole of the lower ground is covered more or less thickly with glacial drift. On the western side of the Vale of Clwyd, at Cefn and Plas Heaton, the caves, which are a common feature in such limestone districts, have yielded the remains of the rhinoceros, mammoth, hippopotamus and other extinct mammals.Coal is mined
The uplands being uncongenial for corn, ponies, sheep and black cattle are reared, for fattening in the Midlands of England and sale in London. Oats and turnips, rather than wheat, barley and potatoes, occupy the tilled land. The county is fairly wooded. There are several important farmers' clubs (the Denbighshire and Flintshire, the vale of Conway, the Cerrig y druidion, &c.). The London & North-Western railway (Holyhead line), with the Conway and Clwyd valleys branches, together with the lines connecting Denbigh with Ruabon (Rhiwabon), via Ruthin and Corwen, Wrexham with Connah's Quay (Great Central) and Rhosllanerchrhugog with Glyn Ceiriog (for the Great Western and Great Central railways) have opened up the county. Down the valley of Llangollen also runs the Holyhead road from London, well built and passing through fine scenery. At Nantglyn paving flags are raised, at Rhiwfelen (near Llangollen) slabs and slates, and good slates are also obtained at Glyn Ceiriog. There is plenty of limestone, with china stone at Brymbo. Cefn Rhiwabon yields sandstone (for hones) and millstone grit. Chirk, Ruabon and Brymbo have coal mines. The great Minera is the principal lead mine. There is much brick and pottery clay. The Ceiriog valley has a dynamite factory. Llangollen and Llansantffraid (St Bridgit's) have woollen manufactures. The area of the ancient county is 423,499 acres, with a population in Igor of 129,942. The area of the administrative county is 426,084 acres. The chief
The county was formed, by an act of Henry VIII,, out of the lordships of Denbigh, Ruthin (Rhuthyn), Rhos and Rhyfoniog, which are roughly the Perfeddwlad (midland) between Conway and Clwyd, and the lordships of Bromfield, Yale (Idl, open land) and Chirkland, the old possessions of Gruffydd ap Madoc, arglwydd (lord) of Dinas Bran. Cefn (Elwy Valley) limestone caves hold the prehistoric hippopotamus, elephant, rhinoceros, lion, hyena, bear , reindeer, &c.; Plas Heaton cave, the glutton; Pont Newydd, felstone tools and a polished stone axe (like that of Rhosdigre); Carnedd Tyddyn Bleiddian, " platycnemic (skeleton) men of Denbighshire" (like those of Perthi Chwareu). Clawdd Coch has traces of the Romans; so also Penygaer and Penbarras. Roman roads ran from Deva (Chester) to Segontium (Carnarvon) and from Deva to Mons Heriri (Tomen y mur). To their period belong the inscribed Gwytherin and Pentrefoelas (near Bettws-y-coed) stones. The Valle Crucis " Eliseg's pillar " tells of Brochmael and the Cairlegion (Chester) struggle against )Ethelfrith's invading Northumbrians, A.D. 613, while Offa's dike goes back to the Mercian advance. Near and parallel to Offa's is the shorter and mysterious Watt
refuge
See J. Williams, Denbigh (1856), and T. F. Tout, Welsh Shires. End of Article: DENBI If you wish, you can link directly to this article.
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