20 PELOPHILOUS FORMATION OF LEFT BANK OF SEVERN ESTUARY. 
In the following* table the results of several typical series of 
observations are given. 
TABLE II. 
a o 
Position from which 'g ° cc 
Core taken oj'S o 
(see Figure I). 2?"^.^ 
1909. 
June 26 
0-16 2-48 4 ins. Nr 
Portbury III. A. 
III. B. 
III. B. 
III. B. 
III. B. 
II. A. 
II. B. 
II. C. 
I. A. 
I. B. 
I. C. 
0-98 
0-72 
0-37 
0-81 
0-72 
0-86 
0-60 
0-72 
0-50 
0-56 
0-73 
Bare piece of ground. 
Nr. edge of shallow pit 
Bottom of shallow pit 
Typical spot. 
June 26 
0-16 2-48 4 ins. 
Nr 
Portishead III. A. 
— Ill 
III. B. 
— 0-92 
Shallow pit scoured. 
III. C. 
— 0-45 
II. A. 
— 1-13 
II. B. 
— 0-95 
II. C. 
— 0-79 
I. A. 
- 0-75 
I. B. 
— 0-70 
Dec. 1 1 
0-42 0-64 6 ins. 
Nr 
Portishead III. A. 
33 0-64 
[approximate. 
III. B. 
34 0-2-0-3 Chloride result only 
in. c. 
27 0-16 
II. A. 
31 0-38 
II. B. 
33 0 37 
II. C. 
28 0'41 
I. A. 
35 0-36 
I. B. 
39 0-42 
I. C. 
47 0.68 
Dec. 11 0 42 0-64 6 ins. 
Between Port- III. A. 
ishead and III. B. 
Portbury III. C. 
„ II. A. 
IT. B. 
II. C. 
I. A. 
I. B. 
42 0 62 
36 0-40 
31 013 
32 0-80 
32 0-31 
38 0 32 
33 0 35 
34 0 32 
(Amongst roots of a 
patch of Aster left 
here. 
I. C. 36 0*35 Amongst Salicornia. 
— 40 0'02 Soil from other side 
of dunes. 
