River Nidd
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River Nidd
The River Nidd is a tributary of the River Ouse in the English county of North Yorkshire. In its first few miles it is dammed three times to create Angram Reservoir, Scar House Reservoir and Gouthwaite Reservoir, which attract a total of around 150,000 visitors a year. The Nidd can overflow the reservoirs, flooding the caves in the valley. In such cases the river overflows into the normally dry river bed past Lofthouse through to Gouthwaite Reservoir. The Yorkshire Dales Rivers TrusYDRThas a remit to conserve the ecological condition of the River Nidd from its headwaters to the Humber estuary. The upper river valley, Nidderdale, was designated as an Area of Outstanding Natural Beauty in 1994. Course The Nidd rises in Nidderdale at Nidd Head Spring on the slopes of Great Whernside in the Yorkshire Dales. It flows east into Angram and Scar House reservoirs before turning south just downstream of Newhouses. In dry conditions the river disappears underground into the sinkhole kn ...
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Nidd Gorge
Nidd Gorge makes up a section of the River Nidd in North Yorkshire, England, in which the river enters a deep ravine with sheer, tree covered valley sides. The river as a whole flows from its source near Great Whernside in Nidderdale (part of the Yorkshire Dales), to its confluence with the River Ouse near Nun Monkton. Nidd Gorge makes up approximately of the entire length of the river, and stretches from the now defunct Nidd viaduct at Bilton in Harrogate to Grimbald Bridge, just south of Knaresborough. Background The gorge was cut out of the soft sandstone during the last Ice Age. Humans were first active in this area around 5,000 years ago, but the extensive woodland has only been there since the early 17th century. During the 18th century and the advent of the industrial revolution, mills began to operate along this stretch of the river, using the force of the water to drive the machinery. Scotton Flax mill was erected in 1798 and run by the company Eteson Dearlov ...
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