Yol. 57.] UPPER GPvEENSAND AND CHLORITIC MARL OF WILTSHIRE. Ill 



are embedded many brown-coated stones like the Cornstones of 

 Maiden Bradley, and like them varying in length from 1| or 

 2 inches across to such as are 4 or 5 inches long. Besides these 

 many phosphatic nodules and phosphatic casts of fossils occur, and 

 in places small patches of a more sandy material like that of the 

 bed below, so that the bed is crowded with inclusions. 



Eig. 3. — Section at Dead-Maid Quarry^ Mere. 





Vegetable soil 



Feet. 



Pale yellow chalky earth, apparently a wash 

 r of Chalk-debris filling a hollow 4 



^ Soft Chalk-Marl, graduating down into hard 

 rocky Chalk-Marl 4 



J Sandy glauconitic marl, with a few phosphatic 

 f fragments 5 



Hard glauconitic marl, with many fossils and 



I Hard glauconitic marl, witri many lossus ana 

 r phosphatic nodules at the base 2 



' Popple-bed,' brownish calcareous sand con- 

 taining many hard stony concretions 1 to 1| 



Hard calcareous glauconitic sandstone, with 

 >- some hard stony concretions; of irregular 



thickness, varying from 1 to 2 



^ "^ / ^ Fine sand, with irregular masses of chert 6 



About 20 



[Vertical scale : 1 inch = 4 feet.] 



