﻿Vol. 64.1 THE FOSSILIFEEOTJS SILTJRIAISr EOCKS OF TOKTWOETF. 513 



II. Description of the Exposures. 

 (1) The Llandovery Beds. 



The Llandovery rocks crop out along an area generally from 1 to 

 2 miles wide, which follows the general trend of the Carboni- 

 ferous Limestone rim of the Bristol CoalJBeld, and stretches in a 

 north-westerly direction from Charfield Green to the neighbourhood 

 of Woodford and Middlemill, and then, after an interval occupied 



Fig. 1. — Geological map of the Tortworth Inlier and the immediate neigJibourJiood, 



Scale: i mile =i inch. 



Trap. 



[Heavy black lines indicate faults.] 



by Wenlock rocks, from Palfield to a point in Eastwood Park 

 south-east of the House. The continuity of the outcrop to the 

 north of Charfield Green is broken for a space by the overlap of 

 the Trias, and the exposures in the south-western part of the area 

 are exceptionally poor and scanty. The best exposures occur in 



