From newcastlecitybreaks.com
Barnard Castle is named after the men that built the stone castle and founded the town. In 1125 Bernard de Balliol succeeded to the lands first given to Guy de Balliol in 1095. The original timber castle was rebuilt in stone and expanded by Bernard and his younger son, Bernard de Balliol II. The large castle is built high on rocky cliffs above the River Tees, and is divided into four wards all walled in stone. The inner ward is protected by a deep ditch cut into the rock and within this ward are the remains of the most important castle buildings including the Round Tower and the Great Hall.
In 1216 Hugh de Balliol helped King John defend the North against a revolt by Northumbrian barons who were supported by Alexander I, King of Scotland. In July Barnard was besieged by Alexander's forces. Little is known about this siege although it appears to have been unsuccessful, and it claimed the life of Alexander's brother-in-law, Eustace de Vesci, killed by a crossbow bolt fired from the castle. Hugh died in 1228, and was succeeded by his son, John de Balliol. John gained land and titles in Scotland through his marriage to Devorguilla of Galloway, and this allowed his son, John de Balliol II, to become a contender for the vacant Scottish throne in 1292. A council of Scottish and English lords, convened by King Edward I, chose John as the new king. He swore loyalty to Edward, but once in power rejected the authority of the English king. In 1296 Edward marched to Scotland and John surrendered his right to the Scottish throne and was imprisoned in the Tower of London. All of his English estates were confiscated, although he was later allowed to retire to his family estates in Picardy.
The castle was not well maintained by subsequent owners, including the Beauchamps and Nevills, who regarded it more as a source of revenue. In 1569, during the 'Rising of the North', in which rebels planned to depose the protestant Elizabeth I and replace her with the catholic, Mary, Queen of Scots, Barnard was besieged by 5000 rebels. Sir George Bowes was unable to stop his men from leaving the castle and was forced to surrender. Following this siege the castle continued to fall into ruin. In 1630 it was sold to Sir Henry Vane who used the castle as a source of materials for extensive improvements he was making to his main residence at Raby Castle.
Durham, a maritime county in the north-east of England, bounded on the N by Northumberland, on the E by the German Ocean, on the S by Yorkshire, and on the W by Westmorland and Cumberland. Its boundary line along the north is chiefly the rivers Derwent and Tyne, along the south the river Tees. Its outline is somewhat triangular, one side extending east-north-eastward, another southward, another west-north-westward. Its greatest length from east to west is about 45 miles, its greatest breadth from north to south about 35 miles, its circuit about 140 miles, its area 647,281 acres. The surface for the most part is either mountainous, hilly, or undulated. The western angle is crossed by the chain of uplands known as the backbone of England, and presents a bleak, moorish, and barren appearance. The tract next to that angle is traversed by ribs from the backbone— lateral and lower ranges of hill spreading in various directions, and it shares much in the sterility of the extreme west, yet has strips of good land and fine scenery along the courses of the principal streams. The central tracts are pleasantly varied with hill and dale, and include some beautiful and fertile valleys. The eastern tract is more champaign, yet abounds in swells, vales, and dells, and embosoms many a picturesque spot. The coast or seaboard is generally bare and tame—much of it destitute of any Interesting feature— other parts redeemed from dreary monotony mainly by the outbreak of ravines and glens, and It presents no considerable headland except the bold and nearly insulated one at the town of Hartlepool. The main streams are the Tyne, the Wear, and the Tees; the chief tributary streams are the Derwent to the Tyne, and the Skerne to the Tees; and the secondary or minor affluents are the Urpeth, the Browney, the Sleekburn, the Gaunless, the Bedburn, and many brooks or becks. Magnesian limestone forms the coast from South Shields to Hartlepool, new red sandstone extends thence southward to the Tees, and westward up the lower part of the Tees valley; a coal formation connected with the coalfields of Northumberland and Yorkshire occupies a space of about 25 miles by 10 in the central and northern parts of the county, and constitutes the most important coal-field in the British Islands; and millstone grit, shale, sandstone, and carboniferous limestone severally or variously occur in the west. Dykes of basalt or greenstone cross the coal measures and extend to the sea, and these in many parts have charred the contiguous coal into cinder, and effected much change on sulphur and other minerals. The limestone is 70 feet thick near Sunderland, and fully 400 feet deep at Hartlepool, and it serves to be quarried, to be calcined, for polishing as marble, and yields galena and a few fossils. The coal presents no fewer than about 40 beds from 3 to 10 feet thick, and is worked in one place near Painswick to a depth of 1800 feet.
The chief mineral product of Durham is coal, of which it is normally the largest producer of any single county in the kingdom. Perhaps the most striking proof of this was given in 1892, when, notwithstanding the miners' strike, which practically brought work to a stand for some months, the production was 23,834,000 tons, valued at £7,398,480. The production of coke from Durham coal is a large industry. Salt is produced to the extent of 180,000 tons per annum, and pig-iron manufactured in this county with Northumberland exceeds 600,000 tons, though the quantity of iron ore mined is only some 3500 tons. Another mineral product is lead ore, of which the output exceeds 6000 tons.
A stiff loam, very fertile, extends from the mouth of the Tees toward Hartlepool; a poor thin clay extends thence along the coast to within a few miles of Sunderland; a loamy or a rich clay lies along much of the sides of many of the streams; a dry friable loam, sometimes shallow and poor, sometimes deep and rich, covers many of the hills across the whole county west of Bishop-Auckland and north of Barnard Castle; and other soils, ranging through all sorts of clay, loam, sand, and gravel, on to sheer, thin, moorish peat, occupy other parts
