|
Ordovician and Silurian greywackes and shales.
Glacial till
Glacial drift
Shallow drift onto rock
Morainic deposits
Cryogenic deposits
Greyish brown in subsoil, sometimes reddish brown.
Sandy silt loam within topsoil but finer textures
e.g. clay loam at depth. Drift deposits are slightly coarser in texture. Slightly stony.
Permanent pasture, forestry and
recreation. |