81 



it is met with, increasing in thickness on the high ground at 

 Collen Park, and is traceable on to Upleadon. 



Limbury Hill has on its summit, flat table land of about 10 

 acres in extent, in which gravel is worked, which shews the 

 following section — 



ft. in. 

 2 







=^5^^ 





•^.,. :e^ ^ 





'^ .'^. 



Northern Drift 



Dark Red Quart - 

 zose Saud. 



N.D. Syenite, 

 Lickey Quartz, 

 Granite, Carbon- 

 iferous Limestone, 

 one piece of Rolled 

 Chalk, Flint, and 

 small slabs of Si- 

 lurian Rock, con- 

 taining the follow- 

 ing Fossils : — 



d 



Heliolites 



Halysites catenularius 

 Cyathophyllum 

 Favosites alveolaris . . . 



Petrk, bina 



Chonetes lata 



Orthis elegantula 

 Atrypa reticularis ... 

 Phacops caudatus ... 

 Bhynchonella Wilsoni 



Wenlock Limestone. 



Caradoc 

 Upper Ludlow. 



Wenlock Limestone. 



This section also rests upon the New Eed Sandstone. 



Catsbury has some N.D, Gravel scattered over the surface, 

 but no sub-angular pieces of Silurian Eocks. 



At Maisemore the N.D. is very irregular, increases in thick- 

 ness towards the summit, and is in places composed mostly of 

 Quartzose Sand ; on the road to Woolridge, at Spring Hill, there 

 is a pit about 9 feet deep of nearly all fine Eed Quartzose Sand 

 with some layers of small N".D. Pebbles. 



At Woolridge I found one slab of Silurian Eock, with Atrypa 

 reticularis and Orthis elegantula in it. 



The table land of Foscombe and Corse is composed of Lias, 

 with hardly, however, any N.D,; and there is a little N.D. at 



