DE RANGE : UNDERGROUND WATERS IN LINCOLNSHIRE. 45 
Well near Rawcliffe Station. Per Dr. Parsons, 1876. 
From surface. Thickness. 
Ft. In. Ft. In. 
3 0 1. Black Sand ... ... ... ... 3 0 
8 0 2. Brown Coarse Sand ... ... ... 5 0 
16 0 3. Mottled Brown Clay ... ... ... 8 0 
4. Red Sand 
These soft red sands and loose sandstones would appear to be 
referable to the Keuper Sandstone, and are the representatives of the 
Cheshire Frodsham Beds, which have been observed eastwards by 
Mr. Aveline, F.G.S., and myself as far as Ashbourne in Derbyshire. 
Trial Boring for Water at New Bridge, near Snaith, in ancient 
course of the River Don, made in 1876 by the Goole Local Board, 
From Mr. Tudor, Surveyor, Goole. 
From surface. 
Thickness. 
Ft. 
In. 
Ft. 
In. 
46 
0 
Brown Warp, Peat, and Loam 
. 46 
0 
51 
0 
Gravel, with magnesian limestone fragments 
5 
0 
56 
0 
Coarse Reddish-brown Sand (decomposed rock ? 
) ,5 
0 
57 
0 
Light Green Marl .. 
1 
0 
80 
0 
Red Marly Sandstone 
23 
0 
87 
0 
Coarse Red Sandstone 
7 
0 
130 
0 
Bed Marly Sand ... 
. 43 
0 
133 
0 
Red Sand, with green marl ... 
. 3 
0 
170 
0 
Red Marly Sand ... 
. 37 
0 
173 
0 
Blue Marl 
. 3 
0 
175 
0 
Red Marl 
2 
0 
263 
0 
Red Marly Sand ... 
. 88 
0 
265 
0 
Variegated Marl ... 
2 
0 
309 
0 
Red Marly Sand 
. 44 
0 
329 
0 
Coarse Red Sand ... 
. 20 
0 
377 
0 
Red Marly Sand ... 
. 48 
0 
379 
0 
Variegated Marl ... 
2 
0 
403 
0 
Red Marly Sand ... 
. 24 
0 
404 
0 
Variegated Marl ... 
1 
0 
500 
0 
Red Marly Sand .. 
. 96 
0 
500 0 
