Historic Flooding
in Calderdale
Why does Calderdale flood?
There are many different reasons that an area might flood but in Calderdale we are particularly at risk. Calderdale is prone to flooding due to its steep valleys, upland terrain, and fast-flowing watercourses, which cause rainwater to travel quickly into rivers such as the Calder and its tributaries. The area’s history of industrial and urban development along valley floors has reduced natural floodplains and increased surface runoff. Combined with intense and prolonged rainfall events these factors contribute to a high risk of both river and surface water flooding throughout the borough.
The Rochdale Canal runs close to the River Calder, so when the river level rises, the canal can be affected. Unlike rivers, canals aren’t built to handle large amounts of floodwater and were designed to stay separate from natural waterways. In severe floods, river water can spill over and overwhelm parts of the canal, like weirs and sluices. Find out more about the causes of flooding.
A long history of flooding
Flooding regularly occurs in Calderdale with records of flooding dating back to the early 1600’s. Areas that have experienced flooding include: Walsden, Ramsden Clough, Todmorden, Cornholme, Callis, Hebden Bridge, Cragg Vale, Mytholmroyd, Luddenden, Luddenden Foot, Sowerby Bridge, Copley, Elland, Wadsworth, Northowram, Halifax town centre, and Brighouse. Surface water flooding has also been an issue throughout the Calder Valley and is not confined to the main river valley.