Geology. 321 
worked by man, but this we may dismiss on the same ground as 
* 
Another case brought forward from abroad but recently, has 
found much favor here as there.} Around the Lake of Zurich 
recently two Swiss professors have proclaimed that they have 
obtained proofs incontestable that man was there, and wove a 
. ‘ hese fra 
pointed sticks, sharpened across the grain, not tapering naturally, 
and a cross set of binding withes, all now pressed and changed, 
but by such characters referred to work o I e 
s, however, ¢ , and, 
— speak with caution, showing only how I think the thing 
might : 
idespread beds of loam and sand, and gravel, cover the 
lower levels of East Anglia; and, probably ranging over a vast 
period, have been collectively described as “ middle-glacial,” for 
these, because in great part made up of the older beds, are like 
es Bourgeois, Congr. Inter. d’Anthrop., 1867, p. 67. : 
t Riitimeyer, Archiv. fiir Anthropologie, 1875; Heer, Primmval World of 
Switzerland. 
¢ Mem. Geol. Surv. Geology of Fenland. 
