96 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. 



Well-section, Notting Dale, near Notting Hill. 



(Mr. R. W. Mylne.) 



Feet. 



Made ground 12 



Gravel 5 



London clay 154 



Mottled clay 35 



Pebbles and sand 38 



244 

 Chalk 12 



This point is made clearer by the following more careful section 

 near Westbourne Grove. 



Well-section, Westbourne Estate Waterworks. 

 PI. I. Diag. A, Loc. sect. 18. 



(Mr. R. W. Mylne.) 



Feet. 



T ^ ri r i. Yellow clay 29 



London Clay. |^ glue clay 188 



f/. Mottled clay 40 



Tir 1 • T. j\ e' Pebbles 2^ 



"•^""^'^^f «'*'^J rf. Green sand, pebbles, and clay 7 



ReadmgSenesA ^ s,„^ „„h «^^ii ^phhW % 



61 feet. 



Sand and small pebbles 3-|- 



b. Green sand 2^ 



a. Sand, pebbles, and clay 6 



Thanet Sands, \ b. Gv&y sdMdi 17 



18/ee^. \ a. FUnts 1 



297 



Chalk 15 



Having thus traced the Woolwich and Reading beds into juxta- 

 position with the Thanet Sands in this direction, we will now return 

 to our starting-point at Hungerford and follow the former along their 

 southern outcrop. 



At Highclere, near Newbury, the section at the brick-pit is as 

 under: — 



Highclere. 



Feet. 

 London clay 12 



I. Basement-bed. Large flint-pebbles in sand 1 



' e. Fine ochreous sand 10 



II. Woolwich d. Mottled ligbt red, yellow and grey brick-clay, the upper 



and Reading-l part sometimes being a red tile clay 25 



Series. c. Whitish sand 10 



, b. Iron-sandstone 1 



At Ewhurst the following section of a well near the church was 

 given me from recollection by the man who had made it a few years 

 previously*: — 



* There is apparently some mistake in these measurements, although I believe 

 the order of succession and the occurrence of lignite (b) to be correct. 



