PEESXWICH CRAG-BEDS OF STJFPOLK Ain) NOEFOIK. 



463 



In the next range of cliffs the further relation of the same beds to 

 the Elephant-bed of Norfolk is shown. The higher part of the cliff 

 at Kessingland is formed by the upper division of the Boulder-clay. 

 Beneath are beds of sand with subordinate seams of small flint- 

 gravel, which may be referred to the Boulder-clay series, though 

 the lower part may belong to the "Westleton beds. Beneath these 

 sands, and just on the same level as in the cliffs at Cove and Easton 

 Bavent (two and four miles south), the Chillesford Clay crops out 

 and ranges to near Pakefield. 



Pig. 33. — Oliff between Kessingland and Pakefield, about one mile 

 north of the former place. 



feet. 

 a. Loamy sand and gravel 4 to 6 



8. Boulder-clay (upper division) 



15 to 20 



7 7. Light-coloured sands, with some 

 seams of fine gravel and a few 

 fragments of shells 20 to 25 



^^gfe^^^B>^^^^^^^^ 5&45&4 (traces of). Flints and iron- 

 ^■^^ — ^"'^^^ '^'"' '~^ ~~ -*=-'^«^!= sand, with rootlets running 



down into 3 to 1 



^^ 3 3 Greenish clay (Chillesford Clay) 5 



The clay is here more compact, and in places contains a number 

 of worn fragments of flint. No shells are found in it *. 



The Forest- bed, together with the associated freshwater bed, now 

 becomes sufficiently well marked, as the following section shows : — 



Fig. 34. — Lower part of Cliff 1| mile south of PaTcefield. 



7. As in fig. 33. 



5. Elephant-bed, 1 foot. 



4. Forest-bed, to 6 feet. 

 3. Chillesford Clay. 



At this place a depression in the Chillesford Clay has been filled by 

 a local freshwater deposit (4) consisting of a dark carbonaceous and 



* Mr. Crowfoot informs me that he found a deer's bone in this clay. 



