Hursley village is situated on the chalk at the northern edge of the Palaeogene deposits of the Hampshire Basin; the chalk is largely overlain by head and 'clay with flints', insoluble material concentrated out of dissolved chalk.
A number of dry valleys converge from the north.
Immediately to the south of the village lies a belt of Palaeocene sandy clays of the Lambeth Group, sloping up to a ridge of Eocene clays and sandstones of the London Clay, Nursling and Whitecliff sands at Ladwell.
Hursley village is situated on the chalk at the northern edge of the Palaeogene deposits of the Hampshire Basin; the chalk is largely overlain by head and 'clay with flints', insoluble material concentrated out of dissolved chalk. A number of dry valleys converge from the north. Immediately to the south of the village lies a belt of Palaeocene sandy clays of the Lambeth Group, sloping up to a ridge of Eocene clays and sandstones of the London Clay, Nursling and Whitecliff sands at Ladwell.
Hursley