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Miners would have slept in these quarters for the whole of the working week and would only have returned to their homes further down the dale, at weekends. Other important relics of Lead mining in the region can be found in the Weardale side valley of the Rookhope Burn. Here we may trace the course and remains of the two mile long Rookhope Chimney. This was a massive stone flue which carried dangerous toxic fumes across the moors away from the lead smelter at Lintzgarth near Rookhope village. A great stone arch can be seen nearby, which once supported the chimney, it resembles a ruined stone bridge that leads to nowhere and crosses nothing at all. While the eastern part of County Durham was part of the Great Northern coalfield, the dales in the western part of the county were once just as important for their lead. Since Roman times, this lead had been exploited in Weardale and the northern Pennines and perhaps it is worth noting that Hadrian's Wall divides the northern fringe of the North Pennine lead field, from the less mineral rich Northumbrian hills to the north. From the thirteenth century lead mining in the Durham dales was encouraged by the Prince Bishops who profited from the mining of the ore. The heyday of lead mining in the region was not however until the late eighteenth to mid nineteenth centuries, when the North Pennine lead field was arguably the most important in the world. The North Pennine lead field was bordered in the east by the Durham coalfield, in the south by the Stainmore Gap and in the north by the Tyne Gap. The main valleys of this area were Teesdale, South Tynedale, the Allendales, Derwentdale and at the centre, Weardale, collectively they were known as the `Lead Dales'.
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