18G0.] WOOD — RED CRAa. 551 



C furlongs N.N. W. of it, which are worthy of special visit ; the latter 

 shows continuous oblique bedding in a vertical section of 25 feet. They 

 seem to be beaches of the age of/, but may be of that of d"^. In the clay- 

 pit a piece of the upper bed of e' has been transported, dropped again, 

 and interbedded with/. 



21. That by Easton Bavent Cliffs. 



22. That by Coveliithe Cliff. N.B, There is a bed of loam, sometimes contorted, 



resting on a denuded surface of e' at the north end of Easton and south 

 end of Covehithe Cliff; but it seems to be post-glacial and to have no 

 connexion with^^. There is also a post-glacial gravel-capping to the 

 cliff, and a more recent sand in the valley-depression. Similar sections 

 to 21 and 22 occur in several brick-fields between Wangford and 

 Frostenden. 



23. That by Pakefield Cliff, if" comes up at the base of the cliff, but is better 



exposed at Corton Ciitf, 6 miles further north (and out of the line of 

 section), where it is at one part contorted, with gravels in the con- 

 tortions ; h is here thinner, varying from 25 to 35 feet. 



24. That by the Brick-field at Toft Monks, near Beccles, 5 furlongs N.N.W. of 



the 110th railway mile-post. N.B, The gravels capping e in the section 

 are not the bed /, but post-glacial. Post-glacial gravels also occur in a 

 pit immediately north of the kiln, sharply faulted down beside h. By 

 ascending from the Brick-field for a furlong, the beds up to and in- 

 cluding i are passed over. 



25. That by the Brick-field at Ingate, Beccles. 



26. That by numerous pits near Eockland Staith, and in Surlingham (6 miles 



east of Norwich). In one pit at Rockland Staith, g^ is faulted down 

 beside /. In a pit at Surlingham Wood the upper beds of e' are late- 

 rally squeezed up, the lower remaining horizontal. The upper beds of c' 

 are also much eroded by the shingle-beds of/ The sections in h and i 

 are on the top of the hill. 



27. That by the Bramerton Crag-pit. 



28. That by the hill descending to the Crag-pit. 



29. That by the pits behind Brundall Station, and beside the railway 4 fur- 



longs west of that Station. 



30. That by the Crag-pit at Thorpe, near Norwich. N.B. The Postwick-Grove 



Crag-pit adjoining includes from c?2' to e only. In the section in the pit 

 east of Postwick Church d?' , d?\ and (^^' seem absent, and e to rest on the 

 chalk, showing the rapid approach of the edge of the deposit. The same 

 is the case at Saxlingham, which is out of the line of section. At the pits 

 on Smockmill Common, Saxlingham, the shells are in a friable condition, 

 and e is sand ; but at the pits 3 furlongs W.N. W. and 5 furlongs S.W. 

 by W. respectively from the Baptist Meeting-house, Saxlingham, e is in 

 the condition of gravel with mammalian remains, e at these places 

 resting on the Chalk, e' caps e in all the pits at Saxlingham, although 

 its development is feeble. 



31. That by the Brick-earth -pit, 2 furlongs N.N.W. of the Thorpe Crag-pit, and 



the Brick-field one furlong further N.N.W. 



32. That by numerous chalk-quarries and brick-pits near Bishop's Bridge, 



Norwich, and on the Catton side of Mousehold Heath. N.B. The Heath 

 itself is capped by a very deep bed of post-glacial gravel. 



33. That by the Brick-fields at Plumstead Street, 6 miles north-east of Norwich. 



34. That by the Brick-pits \ mile north of Wroxham Bridge, by Horstead Marl- 



staith, and by the Lime- and Brick-kiln immediately north of Coltishall 

 village. N.B. It is only in this neighbourhood that the bed /has yielded 

 fossils. 



35. That by the heath-country between Westwick and North Walsham. 



36. That by two deep pits 6 furlongs south-east of North Walsham. 



37. That by the Brick-pits and Marl-pits in the valley of North Walsham. g'^ 



occurs here in the form of very chalky marl coming out in the bottom of 

 the valley. 



38. That by Edingthorpe Heath. 



VOL. XXir, PART I, 2 P 



