390 



W. D. Lang — The Selbornian of Charmouth. 



SECTION AT THE CUTTING, CHAEMOUTH. 



ft. ills. 

 450 



426 6 



425 S 



.As.K^ ^^Kw. - ^\i'i^s^. 



Scale, I foot = '076 inch. 



0;,oO -O- ■ 



l-'p;o.c7;o.o;o- 



•..■y.•.•■^).■■.■o;-.s•. 



•■:s".G-:0.'-OA 





X X 



Weathered remains of Chert beds, i.e. lower half , of zone oiPectett asper, 

 consisting of angular Cliert fragments, in a sandy matrix 



Very dark green, loamy, glauconitic sand, veined with purplish-black and 



pink-red iron oxide . . 

 Greenish-brown glauconitic sand, with occasional veins of purplish-black 



iron o.xide, and occasional obscure fossil remains . . 

 Reddish and brown glauconitic sand, crowded with fragmentary shells, 



chiefly Exogyra and Neithca, and bits of Chert 

 Same as bed ii. Greenish-brown glauconitic sand, with occasional veins of 



purplish-black iron oxide, and occasional obscure fossil remains 

 Whitish and yellow glauconitic sand, with fragmentary shells in Beekite, and 



casts in purple-black iron oxide, and specks of purple-black iron oxide 



Same as bed 8, with no or few fossils 



Broken ground 



Yellow and white glauconitic sand with occasional obscure fossil remains, 

 and a little iron oxide 



Darker yellow and white glauconitic sand, with occasional obscure fossil 

 remains 



Yellow and white glauconitic sand veined with black clay 



Reddish-yellow glauconitic sand 



Broken ground 



rii. 



\ 



4 o shown. 



West. "SS Roadway — Charmouth to Lyme. S^ East. 

 '^ To Lyme i| miles. To Charmouth jf mile. BS" 



