122 



N .W.,likea sea cliff, and ^ f ^ *° ^^ of the rockg of all that 

 has « the «~— £££ rJlt: showing that a» upheaval 



^position. This observation^ ^^ ~ n^TtTSioh we snail 

 of the elevation of mountain ranges in different countries, 

 have briefly to refer further on. 



It would be entering into too wide a field to give in any ^detail, an a. 

 coun t of the sun-ounding Syrian strata but it may *«£££?££l 



«ri the lone ridge of Wenlock and Aymestrey limestone; and nearer still, 

 a ^Z:lX^^^^ members of the Caradoc group 



So far the geology in this direction is tolerably clear and well defined, 



„holeth. .uccrior, i. .<■ repilar {hat ths.re.ion a „„ e hout 



intoto ,hat ,.h,»e o. th. ^X^'tht t' o«^rSi, U£» 



to a very great extent ceases. * andTrice 



can be disentangled. 



As an instance of this great complication I would mention a portion 

 f the Onny Valley. About Horderly you will find the Caradoc succeeded 

 InlyX tlfcLbrian, and this again brought into iuxtaposit on ^ the 

 tl Tool strata, which you remember is a more ^recent formats than 



Caradoc. 



°L „,ual »ea»> .. aoocnting f« •»* • «- - *» » '° "J ^^ 



