30 



POST-TEUTIARY ENTOMOSTRACA. 



and the New Park) appears to have been broken under circumstances which led to the 

 intercalation of numerous beds of sand, gravel, and clay. Two bores may be quoted as 

 examples •} 



Blairhardie, No. 4 Pit. 



Surface soil .... 



. 4 ft. 



6 in. 



Blue clay 



. 9 



0 



Hard stony clay . 



. 69 



0 



Sand with a few shells 



. 3 



0 



Stony clay with boulders 



. 46 



6 



Mud and running sand 



. 11 



0 



Hard clay, boulders, and broken rock 



. 27 



0 





170 



0 



Milliddn, two miles east of Garscadden. 







Sandy clay . . . 



. 5 ft. 



0 in. 



Brown clay and stones 



. 17 



0 



Mud ..... 



. 15 



0 



Sandy mud 



. 31 



0 



Sand and gravel with water . 



. 28 



0 



Sandy clay and gravel 



. 17 



0 



Sand ..... 



5 



0 



Mud ..... 



6 



0 



Sand . . . 



. 14 



0 



Gravel ..... 



. 30 



0 



Brown sandy clay and stones . 



. 30 



0 



Hard red gravel .... 



. 4 



6 



Light mud and sand 



1 



8 



Light clay and stones 



. 6 



6 



Light clay and whin block 



. 26 



0 



Fine sandy mud . . . 



. 36 



0 



Brown clay, gravel, and stones 



. 14 



4 



Dark clay and stones 



. 68 



0 





355 



0 



' A series of bores is given in detail by Mr. Binnie in ' Trans. Geol. See. of Glasgow,' p. 133, vol. iii, 

 part i. 



