Soil Associations

0541u ELLERBECK

Soil and site characteristics

Very stony well drained loamy soils locally on hummocky ground. Some similar but less stony soils.

Geology

Glaciofluvial drift

Cropping and Land Use

Stock rearing on permanent grassland in moist lowlands; some cereals, sugar beet and potatoes in drier lowlands.

Component soil series

Subgroup	Series name	Percentage	WRB 2006 link
5.41	ELLERBECK	40%	Dystric Episkeletic Cambisols
5.41	HALL	30%	Eutric Endoskeletic Cambisols
6.11	BASCHURCH	20%	Episkeletic Entic Podzols

Covers 267 km² in England and Wales

Soilscapes Classification

6	Freely draining slightly acid loamy soils

0541u ELLERBECK

Detailed Description

This association of dominantly free draining soils is developed on very stony glaciofluvial or river terrace drift in Northern England, the Midlands and Wales. It contains loamy-gravelly Ellerbeck and Baschurch soils and also the less stony, coarse loamy Hall series, which overlies gravel at between 40 and 80 cm depth. The terrain is undulating or hummocky on lower valley sides or bottoms, or almost level on outwash fans. The Ellerbeck series has a brown, slightly or moderately stony surface horizon changing abruptly at plough depth to a dull, very stony sandy loam or clay loam which overlies gravel containing little fine earth. The Baschurch series is similar but the subsoil is enriched with translocated iron and aluminium. The porous nature of all these soils allows roots to penetrate easily.

These soils cover 161 km², in the Tyne valley, the Eden valley near Penrith, Teesdale, some Lake District valleys and the North York Moors. In wetter western districts there is a larger proportion of podzolic soils than elsewhere, the Ellerbeck series, typical brown earths, giving way to typical brown podzolic soils of the Baschurch series. Stoniness and texture vary, and where the drift becomes less stony and deeper over the gravels, Ellerbeck soils are replaced first by the Hall series, typical brown earths, and then by the Wick series. Sandy and sandy-gravelly soils, represented by the Newport and Netherby series respectively, are also present in places. The stones are hard sandstone, greywacke or igneous rock. Low-lying places contain the seasonally waterlogged loamy-gravelly Greengill series. Small areas of alluvium, with the Eversley series, also occur. On the North York Moors, the gravelly Rushwick series is present.

Soil Water Regime

The principal soils are well drained (Wetness Class I) and permeable. Excess winter rainwater quickly soaks in and there is little surface run-off. Profile available water, which is variable and affected by stoniness, is less than 100 mm in Ellerbeck and Baschurch soils, and less than 150 mm in the Hall series. Except in the Lake District and Pennines, the soils are slightly to moderately droughty for grass, depending on the potential moisture deficit.

Cropping and Land Use

This is easily worked land suitable for cultivation except where the climate is too wet or the slope too steep. Land use varies from livestock production and dairying, in wetter districts, to some arable in the drier districts. Natural fertility is poor and the stony topsoil can severely wear farm implements and create difficulty with cultivations and harvesting. The chief restriction to grass growth is the small amount of available soil water, but in the wetter western districts this is ameliorated by the climate. The soils are resistant to poaching and can carry large numbers of stock. Where wet soils are extensive this association is especially valuable in winter, as the land may be used by stock with little damage to either soil structure or the grass sward. The soils are very suitable for slurry acceptance, except where very stony at the surface or where the ground slopes steeply. The association is under trees near Hexham, Northumberland where larch, Douglas fir and beech, ash and sycamore are the principal species planted.

0541u ELLERBECK

Distribution Map

Note that the yellow shading represents a buffer to highlight the location of very small areas of the association.

Keys to component soil series

Northern Region

All information Copyright, Cranfield University © 2024

Citation: To use information from this web resource in your work, please cite this as follows:
Cranfield University 2024. The Soils Guide. Available: www.landis.org.uk. Cranfield University, UK. Last accessed 08/12/2024