Rev. R. Ashington Bullen—MHolian Deposits at Etel. 7 
together with what is probably Lydian Stone: but these rocks must 
form the subject of a second part of this paper. This raised beach 
aon N 
Wet 
PL 
Kem, 
2 SZ 
Gs y Etel : 
Sp Raised 
Beach 
c.de} § 
: OG Ay S: 
Le Chaudronmer YS/ -p 
Barre \ & ae 
ao fe Echelle metrique. 
aN) 
: | 500 
a 
- : “e, 1000 2000 6000 4000 5000 melres 
Fie. 1. Diagram of Etel, estuarine area, rivers omitted. [N.B. for Lottois read 
Lorrois. ] 
is overlain by from 33 to 4 feet of very dark brown, vegetable, peaty- 
looking mould, irregularly and sparsely scattered in the lower half 
of which are similar raised-beach pebbles (Text-fig. 2). Untor- 
tunately, the rest of the Raised Beach on the other side of the road 
has been quarried away, but the section that remains above the solid 
granulite contains a few scattered pebbles. No local granulitic pebbles 
occur in the Raised Beach, although some angular granulitic fragments 
do occur in the ‘overburden’ of mould. After careful examination 
no marine shells, fragmentary or otherwise, were to be seen in the 
Raised Beach. The absence of local stone in the Raised Beach itself 
is noteworthy. The raised beaches of this region must have been 
