30 



POST-TERTIARY 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 







Hard stony clay 



. 69 







Sand with a few shells 



. 3 







Stony clay with boulders 



. 46 



6 



Mud and running sand 



. 11 







Hard clay, boulders, and broken rock 



. 27 







Millichin, two miles east of Garscadden. 



Sandy clay 



Brown clay and stones 



Mud . 



Sandy mud 



Sand and gravel with water 



Sandy clay and gravel 



Sand 



Mud . 



Sand 



Gravel . 



Brown sandy clay and stones 



Hard red gravel 



Light mud and sand 



Light clay and stones 



Light clay and whin block 



Fine sandy mud 



Brown clay, gravel, and stones 



Dark clay and stones 



170 



. 5 ft 



Oin 



. 17 







. 15 







. 31 







. 28 







. 17 







. 5 







. 6 







. 14 







. 30 







. 30 







. 4 



6 



. 1 



8 



. 6 



6 



. 26 







. 36 







. 14 



4 



. 68 







355 



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

 part i. 



