2 ^8 [ pr0e - B.N.F.C. 



beautiful example of a narrow band of chalk caught up in a dyke 

 was observed. In the third quarry the exposure of chalk was 

 about 60 feet deep, the bands of flint were very pronounced and 

 regular, and on the floor of the quarry there were many fine 

 specimens of paramoudras, but they were not observed in situ. 

 Neither the Glauconitic Sands nor the Yellow Sandstones were 

 exposed in this quarry, but a good section of Chloritic Sands 

 passing upwards into Chloritic Chalk, surmounted by hard White 

 Chalk, was observed near the entrance, and fine specimens of all 

 the beds were secured. As the quarries are not now worked few 

 fossils were obtained. These included Belemnitella mucronata, 

 Terebratula carnea, and the cast of another brachiopod from 

 the chalk; Inoceramus crispi, and Echinocorys gibbus from the 

 Chloritic Chalk, and three specimens of Ventriculites from the 

 Chloritic Sands. 



