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DENBI

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Originally appearing in Volume V08, Page 18 of the 1911 Encyclopedia Britannica.
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DENBI }ISHIRE (Dinbych), a See also:

county of N. See also:Wales, bounded N. by the Irish See also:Sea, N.E. by See also:Flint and See also:Cheshire, S.E. by Flint and See also:Shropshire, S. by See also:Montgomery and See also:Merioneth, and W. by See also:Carnarvon. See also:Area, 662 sq. m. On the N. See also:coast, within the Denbighshire See also:borders and between Old Colwyn and Llandulas, is a See also:wedge of See also:land included in See also:Carnarvonshire, owing to a See also:change in the course of the Conwy stream. (Thus, also, See also:Llandudno is partly in the See also:Bangor, and partly in the St See also:Asaph, See also:diocese.) The See also:surface of Denbighshire is irregular, and physically diversified, In the N.W. are the See also: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 (See also:Lat. See also:Hospitium) and Llangwm range, between See also:Denbigh and Merioneth. From this See also:watershed flow the Elwy, Aled, Clywedog, Merddwr and Alwen, tributaries of the Clwyd, Conwy and See also:Dee (Dyfrdwy). Some of the valleys contrast agreeably with the bleak hills, e.g. those of the Clwyd and Elwy. The portion lying between See also:Ruabon (Rhiwabon) hills and the Dee is agricultural and See also:rich in minerals; the Berwyn to See also:Offa's Dyke (Wdl (See also:ea) is See also:wild and barren, except the Tanat valley, Llansilin and Ceiriog. One feeder of the Tanat forms the Pistyll Rhaiadr (See also:waterspout fall), another rises in Llyncaws (See also:cheese See also:pool) under Mod Sych (dry See also:bare-See also:hill), the highest point in the county. Aled and Alwen are both lakes and streams.

See also:

Geology.—The geology of the county is full of See also:interest, as it develops all the See also:principal strata that intervenes between the Ordovician and the Triassic See also:series. In the Ordovician See also:district, which extends from the See also:southern boundary to the Ceiriog, the LIandeilo formation of the eastern slopes of the Berwyn and the See also:Bala beds of shelly See also:sandstone are traversed See also:east and See also:west by bands of intrusive felspathic See also:porphyry and ashes. The same formation occurs just within the county border at Cerrig-y-Druidion, Langum, Bettys-ycoed and in the See also:Fairy Glen. Northwards from the Ceiriog to the See also:limestone fringe at Llandrillo the See also:Wenlock shale of the See also:Silurian covers the entire See also:mass of the Hiraethog and Ciwydian hills, but verging on its western slopes into the Denbighshire grit, which may be traced southward in a continuous See also:line from the mouth of the See also:Conway as far as Llanddewi Ystrad Enni in See also:Radnorshire, near Pentre-Voelas and Conway they are abundantly fossiliferous. On its eastern slope a narrow broken See also:band of the Old Red, cr what may be a conglomeratic See also:basement See also:bed of the Carboniferous Limestone 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 See also:fault, and there forks into two divisions that terminate respectively in the See also:Great See also:Orme's See also: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 See also:division it is itself overlaid by the Millstone Grit of Ruabon and Minera, and by a See also:long reach of the See also:Coal See also:Measures which near See also:Wrexham are 41 m, in breadth. Eastward of these a broad See also:strip of the red marly beds succeeds, formerly considered to be See also:Permian but now regarded as belonging to the Coal Measures, and yet again between this and the Dee the ground is occupied—as in the Vale of Clwyd—by the New Red rocks. As in the other See also:northern counties of Wales, the whole of the See also:lower ground is covered more or less thickly with glacial See also:drift. On the western See also:side of the Vale of Clwyd, at Cefn and Plas Heaton, the caves, which are a See also:common feature in such limestone districts, have yielded the remains of the See also:rhinoceros, See also:mammoth, See also:hippopotamus and other See also:extinct mammals. Coal is See also:mined from the Coal Measures, and from the limestone below, See also:lead with See also:silver and See also:zinc ores have been obtained. Valuable fireclays and terra-See also:cotta marls are also taken from the Coal Measures about Wrexham.

The uplands being uncongenial for See also:

corn, ponies, See also:sheep and See also:black See also:cattle are reared, for fattening in the Midlands of See also:England and See also:sale in See also:London. Oats and turnips, rather than See also:wheat, See also: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 & See also:North-Western railway (See also:Holyhead line), with the Conway and Clwyd valleys branches, together with the lines connecting Denbigh with Ruabon (Rhiwabon), via See also:Ruthin and See also:Corwen, Wrexham with Connah's See also:Quay (Great Central) and Rhosllanerchrhugog with Glyn Ceiriog (for the Great Western and Great Central See also:railways) have opened up the county. Down the valley of See also:Llangollen also runs the Holyhead road from London, well built and passing through See also:fine scenery. At Nantglyn paving flags are raised, at Rhiwfelen (near Llangollen) slabs and slates, and See also:good slates are also obtained at Glyn Ceiriog. There is plenty of limestone, with See also:china See also: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 See also:brick and pottery See also:clay.

The Ceiriog valley has a See also:

dynamite factory. Llangollen and Llansantffraid (St Bridgit's) have woollen manufactures. The area of the See also:ancient county is 423,499 acres, with a See also:population in Igor of 129,942. The area of the administrative county is 426,084 acres. The See also:chief towns are: Wrexham, a See also:mining centre and N. Wales military centre, with a fine See also:church; Denbigh; Ruthin, where assizes are held (here are a See also:grammar school, a See also:warden and a 13th-See also:century See also:castle rebuilt); Llangollen and Llanrwst; and See also:Holt, with an old ruined castle. The Denbigh district of See also:parliamentary boroughs is formed of: Denbigh (pop. 6483), Holt (1059), Ruthin (2643), and Wrexham (14,966). The county has two parliamentary divisions. The See also:urban districts are: Abergele and Pensarn (2083), Colwyn See also:Bay and Colwyn (8689), Llangollen (3303), and Llanrwst (2645). Denbighshire is in the N. Wales See also:circuit, assizes being held at Ruthin.

Denbigh and Wrexham boroughs have See also:

separate commissions of the See also:peace, but no separate See also:quarter-session courts. The ancient county, which is in the diocese of St Asaph, contains seventy-five ecclesiastical parishes and districts and See also:part of a See also:parish. The county was formed, by an See also:act of See also: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 (See also:lord) of Dinas See also:Bran. Cefn (Elwy Valley) limestone caves hold the prehistoric hippopotamus, See also:elephant, rhinoceros, See also:lion, See also:hyena, See also:bear, See also:reindeer, &c.; Plas Heaton See also:cave, the See also:glutton; See also:Pont Newydd, felstone tools and a polished stone See also:axe (like that of Rhosdigre); Carnedd Tyddyn Bleiddian, " platycnemic (See also:skeleton) men of Denbighshire" (like those of Perthi Chwareu). Clawdd Coch has traces of the See also:Romans; so also Penygaer and Penbarras. See also:Roman roads ran from See also:Deva (See also:Chester) to Segontium (Carnarvon) and from Deva to See also:Mons Heriri (Tomen y mur). To their See also:period belong the inscribed Gwytherin and Pentrefoelas (near Bettws-y-coed) stones. The See also:Valle Crucis " Eliseg's See also:pillar " tells of Brochmael and the Cairlegion (Chester) struggle against )Ethelfrith's invading Northumbrians, A.D. 613, while Offa's See also:dike goes back to the Mercian advance. Near and parallel to Offa's is the shorter and mysterious See also:Watt's dike. Chirk is the only Denbighshire castle comparatively untouched by See also:time and still occupied. Ruthin has cloisters; Wrexham, the Brynffynnon " nunnery "; and at both are collegiate churches.

Llanrwst, Gresford and Derwen boast See also:

rood lofts and screens; See also:Whitchurch and Llanrwst, portrait See also:brasses and monuments; Derwen, a See also:churchyard See also:cross; Gresford and Llanrhaiadr (Dyffryn Clwyd), stained See also:glass. Near Abergele, known for its sea See also:baths, is the ogof (or cave), traditionally the See also:refuge of See also:Richard II. and the See also:scene of his See also:capture by See also:Bolingbroke in 1399. See J. See also:Williams, Denbigh (1856), and T. F. Tout, Welsh Shires.

End of Article: DENBI

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