Note 181 — Chapter XIV · THE OLD SOUTH-WESTERN SEA-COAST—SOMERFORD, CHEWTON GLEN, MILFORD, HURST CASTLE, LYMINGTON.

For the geology of High Cliff, Barton, and Hordle Cliffs, see chapter xx. There are not many fossils in either the grey sand or the green clay before you reach the “bunny.” Plenty, however, may be found in the top part of the bed immediately above, known as the “High Cliff Beds,” and which rise from the shore about a quarter of a mile to the east of the stream.