Page:Quarterly Journal of the Geological Society of London, vol. 27.djvu/399

 1871.] WHITAKER TERTIARY CLIFF-SECTIONS. 265 At one place the sand (3) seems to abut against the beds below, as if from a small fault. At Varengeville, beyond the next gap, is a bike section, the sand (8) and its included masses of sandstone being in great part white, and there are also sandy shell-beds. The Oldhaven sand is hidden by fallen masses from above. At the next hill the top part of the London Clay contains a bed of buff sand 2 feet thick. In Passy's work a mass of Calcaire Grossier (?) is figured (plate xix.) as resting unconformably on the beds below. I did not see it ; but it may have fallen into the sea since his time. Inland there is a tile -kiln in the London Clay. 2. Newhaven. The section here was, I believe, at its best when I saw it, the cliff having been then cut back to the highest ground ; and for this reason I venture to describe it to the Society, although it has already been described at least five times (three times in the Society's publications), and in all these cases by well-known observers, so that, of course, I shall incorporate their notes with my own. The shape of the outliers will be seen from the accompanying- map (fig. 1), which differs from that of the Geological Survey in separating the Tertiary beds into two masses, instead of joining the whole into one along the face of the cliff. I believe that the mass Fig. 1. — Geological Map of the Newhaven Outliers. From Sheet 5 of the Geological Survey Map (1864), with alterations (1866). Scale 1 inch to a mile. a. London Clay. b. Woolwich and Reading Beds. c. Chalk, d. Alluvium. X X Between these points the Chalk is capped by a wash of the Tertiary beds. of loam, sand, and flints that occurs along the top of the cliff be-