124 



J. GTTNN ON THE FOREST-BED SERIES AT 



This I have seen here on one spot (a mere patch of a few yards 

 length) which has escaped denudation. It is well developed, with 

 blackened earth and large stools and stems of trees ; but I did 

 not find any mammalian remains in it ; and Mr. Thomson, of Pake- 

 Pig. 1.— Section of Cliff at Kessingland and Pakefiekh 



(h. 



Surface soil 



1. Upper Boulder-clay ... 



2. Middle Drift 







3. Chillesford Clay and J 

 Sand 1 



4. 



Norwich Crag (fluvio- i 

 marine) * 



Eootlet-bed and Unio- J 

 bed (freshwater) I 



Forest-bed with stools 

 of trees 



Soil of the forest-bed 

 (Elephant-bed and 

 Blue Clay ; estua- 

 rine). 



mm 



►Bouldered rocks, chiefly 

 oolitic. 



Cetacean 

 shells. 



bones, marine 



Freshwater & marine shells. 

 Mammalian remains (rare). 

 Freshwater shells abundant 



in black ZTm'o-bed. 

 Present beach level. 



(Elephas antiquus, Rhino- 

 ceros etruscus, Trogon- 

 therium Cuvieri. 



) Elephas meridionalis, Rhi- 

 noceros megarhinus 

 (rare). Cetacean re- 

 mains (common). 



field, whom I employed to collect specimens, says that he never 

 found any except in No. 7, in which they abound for about three 

 quarters of a mile. I mention this to show from what bed the spe- 

 cimens exhibited are taken, and not to affirm that they are confined 

 to No. 7, because a fine molar of Elephas antiquus has been ob- 



