Cycles of Sedimentation vn the Hocene. 153 
ea 7; ul - 
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Brats 
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AUG _cf to: e: ae = 
4sD3LIHM Wd & ares aD = 5 E 
a Ga gare SUR a 
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OF ao :: eee 'O:: ® 
Of Sy ee ak 5 
2h aston on 2 
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7 HENGISTBURY 
LOWER 
HIGHCLIFFE SANDS OF SURVEY. 
BAGSHOT 
= 
these pass into coarse gravels, etc. In the extreme east, as at New- 
haven, the mottled clays give place to well-bedded clays crowded 
with estuarine shells (Woolwich Beds), and similar beds occur at 
Dieppe. At the base of the series there is a thin bed of greenish 
or brownish glauconitic sand, resting on an irregular surface of 
Chalk. Some small rolled green-coated flints occur at the base, as 
well as angular flints left after the sub-surface solution of the Chalk, 
and the bed is obviously marine. As Parent? has pointed out, it is 
1 Parent, “‘ Notes sur les Terrains Tertiaires du Pays de Caux’’: Ann. 
Soc. géol. Nord, vol. xxii, 1894, p. 9. 
