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Henmore Brook

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Through England, Paleolithic and Middle Ages

In its upper reaches it is known as the Scow brook, much of which was inundated by the Carsington Water reservoir in 1991. It becomes the Henmore brook in the middle reaches, where there are three tributaries called the Parkside, Kniveton and Dayfield brooks.

The brook drains a catchment of mixed geology, which has an area of 46 square kilometres (18 square miles). It flows through the market town of Ashbourne, where flooding of the town centre by the brook has historically caused significant damage. The brook is designated as a Main river by the Environment Agency from the outflow at Carsington Water to the confluence with the River Dove.

Course

The source of the brook is at the base of Soldiers Knoll near Stainsborough Hall, from where it flows west until it reaches the upper end of Carsington Water near Hopton. It reappears at the outlet of the dam, and flows in a south-westerly direction past the villages of Hognaston, Atlow, and Sturston until it reaches the town of Ashbourne. Downstream of the town it passes the village of Clifton before reaching its confluence with the River Dove at Church Mayfield.

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