SOIL ASSOCIATIONS -
 SOURHOPE

Soils Landcover Regional Landscapes Soils & Sustainability


DERIVATION:

Lavas of andesitic composition associated with sediments of Lower Old Red Sandstone age (also associated with granitic masses at Cheviot and in Argyll).

TYPES OF PARENT MATERIALS MAPPED:

Glacial till
Glacial drift
Shallow drift onto rock
Morainic deposits
Shattered rock in situ

COLOUR:

Reddish brown in subsoil.

TEXTURE:

Sandy silt loam or silt loam in till deposits but coarser textures (sandy loam) characterise drift and morainic parent materials.  Moderately to very stony depending on depth to rock.

DOMINANT LAND USE:

Arable, permanent grassland, forestry.



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LANDFORMS:

Hills, often steeply sloping with frequent outcrops of rock in some areas.
Also associated with valley sides on long gentle slopes.

SOIL CHEMISTRY:

High phosphorus in topsoils.

SOIL PHYSICAL PROPERTIES:

Potential rooting depth approximately 40 to 60cm depending on presence of rock or induration. 
Weak soil structure.

 SERIES NAME  SOIL TYPE  DRAINAGE  PARENT MATERIAL
 Atton  Noncalcareous gley (SW)  Poor Drift and till
 Balquhandy  Humus iron podzol  Free Till
 Bellshill  Brown forest soil with gleying  Imperfect Drift and till
 Cowie  Peaty podzol  Free below iron pan Drift, till and colluvium
 Edgerston  Peaty gley  Poor Drift and till
 Elsrickle  Brown forest soil with gleying  Imperfect Drift often stony
 Fearnoch  Peaty gley  Poor and very poor Stony colluvium
 Frandy  Humus iron podzol  Free Drift and till
 Gellyknowe  Brown forest soil with gleying  Imperfect Till
 Hungry Brae  Humus iron podzol  Free Stony drift
 Lawsuit  Peaty gley  Very poor Drift and till
 Sourhope  Brown forest soil  Free Drift, till and colluvium
 Sourskel  Skeletal soil  Variable Very shallow drift and residual

 
* Occurs only as component in soil complexes

 
Updated: 30 October 2009