VOL. XIX. (3) EXCURSION— CHELTENHAM & CLEEVE HILL 195 
(T) 
P 
c 
If) 
in 
K-( 
P 
w 
p 
p 
p 
p 
w 
H 
HH 
P 
O 
O 
o 
►— t 
p 
w 
p 
H 
P 
W 
o 
p 
o 
o 
H 
<< 
P 
H 
P 
P 
P 
c/i 
O 
P 
u 
p 
p 
c/i 
cJ 
rv> 
rH 
< 
cJ 
in 
P 
P 
w 
t/3 
C 
m 
h-H 
1-^ 
d 
p 
O 
« 
P 
>< 
m 
During the elutriation it was clear that this grade consisted of very fine sand, mostly of diameter > %. These analyses conform to a type 
which is very different from that of any other British deposits I know. — P.G.H.B. 
