NEOCOMIAN. 147 



and 400 feet thick in the west of Surrey. It is 



full of band> of fresh-water limestone, formed of 



.-water shells, especially Paludina. 



In various localities in Sussex, particularly 



near Hastings, the footprints of Tguanodan have 



been found, and both there and at Cuckfield a 



multitude of bones occur. They include small 



iur of the gei is 4 im h taurus 



and an Ichthyosaur p estuarine, together 



with a .u r roii[) of terrestrial saurians, entirely dif- 



of the Isle of Wight. These 



remains include US, the / n Man- 



tc//i\ Suchosaurus and M veil as 



Many plants are met with 



on this horizon, including some tern-, like Sphe- 

 nopteriS) with the fronds well ; ed; and nu- 



merous Cycads. Fresh-water shells include the 

 • errestrial fauna is very im- 



pertV. tly known in comparison with that buried 

 in t: m, from 



which entr I other 



reptiles have been obtained. Along the northern 



out. v > co mi an strata, by Farringdon, 



•on and e, numerous remains have 



curred and other 



ians hk- 1 he W eald, and 



with them are remains of Cy< nus and 



Pines. On this outcrop the NeOCOmian Sand 



ly on the Kime: \', A mpthill 



(May, and Oxford ( t Sa ly and Woburn 



in Bedfordshire, showing that an unconformity 



urates tl omian strata from the Oolites 



in the middle of England. 



The Lower Greensand is a marine bed which 

 extends over the fresh-water series of the Weald. 

 But beyond the Wealden area the sands are 



