10 Rev. R. Ashington Bullen—Aolian Deposits at Etel. 
The small pea-sized gravel underlying these lines of stones pre- 
dominates. It is noteworthy that the same sort of gravel occurs at 
Constantine Island, Cornwall, as a Raised Beach! underneath the 
blown-sand, and on which the prehistoric, probably Neolithic, oblong 
‘potter’s house’ (discovered by Mr. Harold Hellyar, of Harlyn) used 
to exist before it was ruthlessly destroyed in 1902. 
Li tet 
Seviére a 
Fic. 3. Diagram of the Riviére W’Etel below Etel and La Magoire. 
1, 2, 3, 4, successive terraces. yp, pond. Y,, granulite outcrops. t+ Tt, marine 
mollusca. <A, steep face of present beach. 
Sepia officinalis, Bittium reticulatum, M. edulis (Young), Cy. europea, Cardium 
edule, various Tapes, Donax vittatus: very abundant on lett bank from f to fF. 
The sea-front material, now acted on by the waves, consists of 
a coarse sea-sand which appears to be driven in from seaward. The 
small pea-gravel appears to be much older than this coarse sea-sand, 
and the question naturally arises whether the former is not rather to 
be correlated with the before-mentioned Raised Beach (xX ), close to the 
town of Htel, especially as it stands at nearly the same level above 
1 Prestwich, Q.J.G.S., vol. xlviil, p. 282. 
