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Mixed acid and basic metamorphic and igneous rocks, locally from intermediate metamorphic and igneous rocks e.g.hornblende-schist,
biotite-gneiss and diorite.
Glacial till
Glacial drift
Shallow drift on rock in situ
Deeply weathered rock
Morainic material
Cryogenic deposits
Dark yellowish brown to yellowish brown.
Highly variable, the till has a sandy loam to sandy clay loam texture
on free-draining sites but sandy silt loam to clay loam in sites with poor drainage. Drift deposits on the upper hill slopes and summitsis stonier and coarser in texture. Moraine deposits are generally a
stony, gravelly loamy sand. Moderately stony within subsoil.
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