r 



216 



ILLUSTRATIONS OF THE 



yft 



I k 



lat any of them hav 

 ide's Bay, in Pen 

 brokefbire, the primary and (econdary flrata ai 



hceii obfe 



At St B 



feen 



very near 



line I bel 



their jundi 

 is not vilibl 



b 



T 



the precife 



pits 



the fccondary ftrata, approach here within a few 

 hundred yards of the primary. The feccndary 

 llrata v;hich commence at this place, occupy both 



iides of 



Eriftol Channel, and meet the C 



fh fchiftus, which 



d 



I) 



fs the north of 





(hire to the qiiantock Hills, in a line th 



may be looked for on the fea-coaft, fome 

 between Watchett and Minehead. 



195. Befides the fca-coaft, the beds of 

 jtiay be expected to 

 fubje(5l. 



T 



h 



the 



afford information on this 



^ 



fiances I have mentioned, I 



ns from the inland 



oth 



country to be added. One of them is from the 



river Jed, a littl 



(^ 



Utt 



■_ 



y above Jedburgh, where 



the fecondary flrata are feen lying horizontally 

 on the primary, a fedion of both being made by 

 the bed of the river. The phenomena here are 

 very diftincT:, and ilrongly marked : Dv Huttcn 

 has defcribed and reprefented them in a plate *. 

 He has mentioned another jundion, not far from 

 this, wdiich he faw in the Tiviot. Both thefe 

 belong to the fame primary ridge with the Siccar 

 Point. 



195. I 



* 



Theory of the Earth, vol. i. p. 43c. j alfo plate 3. 



