I 
OF WBSTEEN EUROPE AND THE MEDITERRANEAN COASTS. 947 
that the agglomerate here overlying the marine sands (a littoral deposit) is newer 
than that of Buena Vista and Bosia. I do not, however, see sufficient reason for this 
conclusion, and would suggest another interpretation (see fig. 16). 
Fig. 15. — Section from near Windmill Sill Barracks to the sea near Monkey's Gave-road (Ramsay and 
Geikie). 
L. Limestone. 
Platform of marine erosion 160 feet above the sea. 
Platform of marine erosion 260 feet above the sea. 
s^. Caloareons sandstone, horizontally' bedded, marine. 
s^. Calcareous sandstone dipping a'way from cliffs, the 'weathered and rearranged 
upper surface of s'. 
a. Unfossiliferous limestone agglomerate (the later agglomerate). 
Presuming, therefore, that the surface breccia on both sides of the Bock is all of the 
same age, my reading of this section would be as under. 
Fig. 16.— Alternative reading of Section No. 15. 
{ «'.Coarse limestone detritus. 
a". Composed mainly of the debris of the marine sands, c, with fragments of lime¬ 
stone in its upper part, 
f. Marine sands = Raised Beach. 
I take it that during upheaval the first effect of the effluent waters has been to 
denude the marine sands c, forming, with the limestone debris from higher up the 
slopes, a finer mixed detrital bed, which should be connected with the breccia or 
Bubble-drift a, and not with c. 
In another section (their fig. 12), the agglomerate is again shown directly over- 
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