STRATA OF SHROPSHIRE AND DENBIGHSHIRE. 



19 















Mr. 



con- 



im- 



the 



and 

 the 

 ne. 













M 



w 

 El 



to 

 ■d 









4> 



Conglomerate-like gr 

 1 foot, supposed by 

 Binney to be the 

 glomerate which 

 mediately underlies 

 red marls. 



Blaek sand, 13 feet. 



Red Sandstone, 31 feet. 



Calamites, Siffillaria, 

 fossil wood lay in 

 debris of thissandsto 





d. pp. 19, 20. 











00 



1 



a 



s 

 « 

















ft. 

 42 

 20 



25 



10 

 soft , 



and 

 ratio 







ft a 





w 



a 



M 



pq 











Grits and metals 

 Red sandstone, and 



metal 



Hard siliceous rock ... 

 " The sandstones are 



reddish,and greenish 



sometimes conglome 



at the base." 



• A 



: d 

 : 00 







° 



pq 

 SB 



5 



l 







4. Aye 









"3 



0. 



a 



a 



K 



R«d sandstone 



Red sandston 



shales 







E. Hull, ' Geo 

 Country aro 

 p. 18. 



5i 





0? 



3 







of 

 5 



13 cT 





to 



to 



0) 







a 



4a 



t2 00 







■0 



H 



01 









'<-* 











M 









§ 

 00 



3 



. OD 







3 



W 









5 



a 



O 



u 





















burr 



gated 



jet. 







5 







■4-3 

 00 



d 



— 

 





d a> 





g 





CO 



i«a 





03.0) 



ii« 







j» 





4) <» 





fit- 



v. «e 

 oa >■ •— 1 





w 







P5 







M 



w 





w 



s 



:> 



ft 









Q 



a 

 



00 



d 



a 



00 



ttled marls 

 estones, 30 

 nney found 

 ils in the 



red Band- 

 he-grained 



90 feet. 

 - Schizodus 

 Turbo. 





nney, 'Geology 

 ountry around 

 p. 14; 'Geol. 

 gan,' p. 28. 





H 

 H 

 P 





00 



— - c 



pie and mo 

 ith thin lim 

 et. " Mr. Bi 

 ermian foss 

 mestones." 



onglomerate, 

 stones, soft, fi 

 and streaked, 

 ossils found - 

 Bakewellii and 





5 



a 



<N 





g«H 



O 



00 



. <3 





& Bi 

 the C 

 escot,' 

 ar. Wi 









f 55. 



a ? .-Phis 





s oPhO 









EO 



Ph 



O f=< 





w 





















i 











e shale 

 of lime 

 ick. 



ive of th 

 estone 

 and." 

 3d a par 

 an Lime 

 , Barrow 

 er place 



inney. 



s-Its 







> 

 > 



S* 









indst 



ar vei 



ve of 



1 Sa 



cen 



Hull 





E. Binney and E. H 

 1 Geology of the Coun 

 around Wigan,' p. 27. 



> 

 > 



3 

 w 



03 



pq 









Red and purp] 

 with thin layers 

 stone, 30 feet til 



" The representat 

 Magnesian Lira 

 the east of Eng 



"May have form 

 of the Magnesi 

 stones of Stank 

 mouth, and otli 

 in the north." 

 E. B 



a — s 00 







r-t 









Brown, .1 

 100 fee 



"The rej 

 Lower 

 stone 

 countie 















a* 

















•-So 

 1 * 



Hi 



• 8* 



O 



O o5 













<0 tD 















O 00 



T2 





g 



4> 0} 









B 





.0 >>d 



d an 

 ited 

 mest 



dsto 

 reen 

 ■ey 

 recci 









pq 





M 





CQ 











►o 





** 



eo 



<N* 















1—4 



























c 2 



