SOIL ASSOCIATIONS -
 ETTRICK

Soils Landcover Regional Landscapes Soils & Sustainability


DERIVATION:

Ordovician and Silurian greywackes and shales.

TYPES OF PARENT MATERIALS MAPPED:

Glacial till
Glacial drift
Shallow drift onto rock
Morainic deposits
Cryogenic deposits

COLOUR:

Greyish brown in subsoil, sometimes reddish brown.

TEXTURE:

Sandy silt loam within topsoil but finer textures 
e.g. clay loam at depth. Drift deposits are slightly coarser in texture. Slightly stony.

DOMINANT LAND USE:

Permanent pasture, forestry and recreation.



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LANDFORMS:

Highly variable, drumlins and undulating terrain within lowland areas, hill or valley sides, with gentle 
or moderate slopes and upland hill summits.

SOIL CHEMISTRY:

Moderate acidity (pH around 5 under semi-natural conditions and low to moderate percentage base saturation and phosphorus within the subsoil. Low available cobalt and copper in some soils.

SOIL PHYSICAL PROPERTIES:

Potential rooting depth up to 50cm unless restricted by presence of rock or induration. Weak to moderate structural development within subsoil.

 
 SERIES NAME  SOIL TYPE   DRAINAGE  PARENT MATERIAL
 Alemoor  Peaty gley (SW)  Poor  Till
 Altimeg  Brown forest soil with gleying  Imperfect  Drift
 Auchrae  Peaty podzol  Imperfect below
 iron pan
 Drift
 Dochroyle  Peaty gley (SW)  Poor and very poor  Drift
 Dod  Peaty podzol  Free below iron pan  Drift
 Dunscore  Brown forest soil  Free  Morainic deposits
 Ettrick  Noncalcareous gley  Poor  Till
 Ettriskel  Skeletal soil   Variable  Very shallow drift
 and residual
 Flemington  Brown forest soil  Free  Drift with partially
 sorted upper layers
 Hardlee  Peaty gley (SW)  Poor and very poor  Clayey till
 Kedslie  Brown forest soil with gleying
 and noncalcareous gley
 Imperfect  Clayey till
 Linhope  Brown forest soil  Free  Drift and colluvium
 Littleshalloch  Noncalcareous gley  Poor  Drift
 Merrick  Subalpine podzol  Free  Cryogenic
 Minchmoor  Humus iron podzol  Free  Drift
 Peden  Noncalcareous gley (SW)  Very poor  Till
 
Updated: 30 October 2009