Dalton Holme

The well at Dalton Holme is drilled into the Cretaceous-aged Burnham Chalk Formation, through a thin drift cover, to the north-west of Hull in Yorkshire. Our records of the water level in this well date back to 1889. The well is 1.5 m wide — almost big enough to lie down in!

BGS Enquiries can help you to access groundwater level data for this well.

TopograpLocation of Dalton Holme. BGS © UKRI.hic map with hillshade of the area around Dalton Holme. BGS © UKRI.
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Location of Dalton Holme. BGS © UKRI.

Hydrograph

Dalton Holme hydrograph, 1950 to 2002. BGS © UKRI.
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Dalton Holme hydrograph, 1950 to 2002. BGS © UKRI.

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Information about the well

Hydrogeological setting

Dalton Holme
Wellmaster ID SE94/5
NGR 4965 4453
Datum 34.5 m AOD
Monitoring details
Type Groundwater level
Aquifer Chalk
Confinement Confined
Depth 28.5 m
Record
Monitored by  EA North East
Records commence 1889
Records end Active

This well measures water level in the Chalk Group to the north-west of Hull.

Geological map of the area around Dalton Holme. BGS © UKRI.
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Geological map of the area around Dalton Holme. BGS © UKRI.

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Well or borehole construction

The original 1.5 m-diameter shaft on the site is thought to have been dug in 1876 to 28.5 m depth. A 460 mm bore was drilled through the base of the shaft in 1946 and plain lining (depth unknown) was inserted.

The well was constructed for a domestic water supply and is regularly pumped.

A borehole was drilled 10 m from the well in 1990.

Hydrograph response

The hydrograph has a broadly sinusoidal appearance, with an absolute recorded range of 14.8 m, although annuual fluctuations are typically around 7 m. The groundwater levels at Dalton Holme respond relatively slowly to rainfall, perhaps influenced by the drift cover.

The minimum recorded level is 9.64 m AOD, on 14 February 1992, and the maximum recorded water level is 23.82 m AOD on 30 March 1947. There does appear to be some constraint in both minima and maxima. As the well neither dries up nor overflows, this implies some regional stratigraphical control on levels.

Data issues

Weekly levels were measured from 1889. A chart recorder was fitted in 1977 and continuous digital recording started in 1986.

References


Finch, J, Marsh, T, and McKenzie, A A. 2007. A preliminary risk assessment of the potential for groundwater flooding during the winter of 2007/8 — an update. (Wallingford, UK: NERC/Centre for Ecology and Hydrology-British Geological Survey.)

Monkhouse, R A. 1992. Long-term hydrograph of groundwater levels in the Dalton Holme Estate well in the Chalk of Yorkshire. (Keyworth, Nottingham: British Geological Survey.)

Topographic map with hillshade of the area around Dalton Holme. BGS © UKRI.
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Topographical map with hillshade of the area around Dalton Holme. BGS © UKRI.

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Acknowledgements

At a national level, groundwater level monitoring data is collected and managed by the Environment Agency (England), the Scottish Environmental Protection Agency, Natural Resources Wales and the Department of the Environment (Northern Ireland).

Access the data they collect and curate, which includes many monitoring sites beyond those highlighted on these pages: 

Contact

Please contact BGS Enquiries for further information.