glacial fan
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Author(s):  
J.E.T. Channell ◽  
M. Smelror ◽  
E. Jansen ◽  
S.M. Higgins ◽  
B. Lehman ◽  
...  
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1916 ◽  
Vol 3 (3) ◽  
pp. 111-117
Author(s):  
R. M. Deeley

At about 55 miles we reach the Hendon Lobe fan. At Dollis Hill the base of the fluvio-glacial beds lies at a height of about 200 feet, whilst their upper limit at Hendon is about 280 feet. On Finchley Hill to the north-east the Boulder-clay lies between the levels of 240 and 340 feet. This was a small lobe, and the fluvio-glacial fan may have sloped rapidly towards the fluvio-glacial gravels of the main stream. On the section, Fig. 2, the heights are shown without correction for slope towards the River Thames.



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