4i 4 Salisbury . — The Soils of Blakeney Point : A Study of Soil 
(X. 4 6 and X. 4 6a) show a lower carbonate content than the main bank, 
but the single sample from the high elbow of VII shows a slightly higher 
*Z- 
•z- 
/ 
/ 
/ 
/ 
/ 
/ 
/ Organic 
/ 
/. 
/ 
/ 
/ 
>r 
\ 
Carbonates 
“X- 
G&J E D C B 
Text-fig. 4. Graph showing the relation between organic content and carbonates in dunes of 
. varying ages as indicated by the letters a to J (cf. map, Text-fig. 1). 
content than the other parts of the bank. Taking all the banks into 
consideration, however, there is a general tendency for the lowest values to 
be found towards the higher levels at the distal end, which supports the view 
that leaching is the main factor involved. 
