﻿Vol. 6 T .] THE OCCURRENCE OF RHiETIC ROCKS AT BERROW HILL. 425 



19. On the Occurrence of Rh^tic Rocks at Berrow Hill, near 

 Tewkesbuey. By Linsdall Richardson, F.G.S. (Read 

 May 24th, 1905.) 



Berrow Hill (184*8 feet above Ordnance-datum) is a small outlier 

 of Lower Liassic and Rhsetic deposits, distant about 2 miles in a 

 south-easterly direction from Chase-End Hill, the southern end of 

 the Malvern Range. It occurs in the centre of a basin-shaped 



Fig. 1. — Geological map of the country around Berrow, showing the 

 geographical distribution of the Keuper Sandstone and the 

 position of Berrow Hill. 



= Keuper Marls hwl = Keuper Sandstone I i = Rhsetic 



[Scale : 1 inch = 1 mile.] 



area formed by the Keuper Sandstone, which in this district comes 

 about 215 feet below the base of the Rhaetic. By means of this 

 sandstone- deposit, it is possible to trace with very great accuracy 

 the amount of fiexuring that these Keuper beds have undergone. 



