Point at which West Beck becomes the River Hull shown within the East Riding of Yorkshire
Location
Country
England
Physical characteristics
Length
15.3 miles (24.6 km)[1][2]
Basin size
90.5 square miles (234.3 km2)[1][2]
Basin features
River system
River Hull[3]
Tributaries
• left
Little Driffield Beck
• right
Gipsey Race Driffield Trout Stream Main Drain Skerne Beck
v
t
e
West Beck (River Hull)
Legend
Spring - Elmswell Beck
Mill Farm
Church Drive
Little Driffield Beck
Becomes Driffield Beck
A614
Spring
The Keld (pond)
Kings Mill
Overflow
Kings Mill Weir
Footbridge
Footbridge
Gipsey Race
Beverley Road
Footbridge
Driffield Trout Stream
Becomes West Beck (River Hull)
Yorkshire Coast Line railway
Bell Mills Plantation
Footbridge
Footbridge
Skerne Road
Bell Mills Weir
Bell Mills
Footbridge
Main Drain
Footbridge
Whinhill Weir
Trout Farm
Footbridge
Footbridge
Footbridge
Mill Farm
Main Street (Skerne Road)
Snakeholm Pastures Nature Reserve
Footbridge
Footbridge
Former trout farm
Field Drain
Skerne Wetlands Nature Reserve
Cleaves Farm Weir
Footbridge
Skerne Beck
Footbridge
Becomes Driffield Navigation (West Beck)
Corpslanding Bridge (limit of navigation)
River Hull (Emmotland)
Becomes River Hull (New Cut)
River Hull (New Cut - Navigable)
West Beck is the common name given to the upper section of the old River Hull, as it rises in the foothills of the Yorkshire Wolds. After reaching Frodingham Beck at Emmotland, it becomes called the River Hull. It is noteworthy for being the most northerly chalk stream in England. It provides fly fishing for wild brown trout and grayling.
^ ab"West Beck Upper". Catchment Data Explorer. Environment Agency. Retrieved 7 November 2016.
^ ab"West Beck Lower to River Hull". Catchment Data Explorer. Environment Agency. Retrieved 7 November 2016.
^"Get to know your rivers; the Hull Catchment" (PDF). environment data.org. Environment Agency. p. 3. Retrieved 8 November 2016.
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