The estuarine peaty shale still to be seen in the cliff section below the Martello tower at Clacton has a thickness of 10 or 12 feet, and seems to pass gradually into a dark clay which we find as the top layer of the shore deposit. On the shore below the Martello, and east of the stone groyne, the following layers were observed:—

1. Dark, stiff clay, without shells. To be seen only on the upper part of the shore, near the sea-wall. Further down, it. has been denuded. Thickness, c. 9 in. from shore sand.

2. A shelly layer, containing much Unıo littoralis: more sandy than the last. c. 3 in.

3. A dark layer with occasional shells. Lower limit variable. c. 4 in.

4. Blue loam: one of the most characteristic features of the deposit. Shells of Unio occur. Helix was also found. There is also in some parts much wood. Partly embedded in this layer most of the bones are found on the shore surface. Eastwards the layer grows less homogeneous and comes to rest directly on the London Clay. I am not sure what is the full thickness of this layer, but, where it is covered by others, I have dug 18 in. into it without reaching anything else. Accumulation of water and return of the tide prevented deeper trenching, but I think if we gave 2 feet as the total thickness we should not be far wrong.

5. A very thin layer, made up almost wholly of fragments of Unio.

6. Sand, shells, and broken flints. Thickness varies; 3 in. and 5 in. were measured in two trenches.

7. Stony layer. Flint pebbles, broken flints, some sand, some shells. Astragalus of deer, horn core (probably of deer), tibia of deer were found in trenching this layer.