f 
for or ag&t mt the result to be considered! otherwise his opinion 
j 
nay be like that of the ordinary antiquity enthusiast quite worth* 
less* Especially he should knot? that to allot? it to be stated on 
hia authority that a given specimen name as an original inclusion 
front a particular stratum, the age cf trMch he mines, %s to take 
ttie risk of tolling the world defi nitely that Imerlea -as occupied 
forty thbn'sand years, roro or lose, before BMXt hvvied on its scores* 
,* . ' 
V. 
I V ■ ' 
••Tf in a question t?hetiter ary single find of o So*o&Xle4 palebllihie 
' 4 , ' 
~ " ‘ A, 
specimen ha? conferred to the above requirements. 
X O ' 
'■•..«■ ■ . < 
o ' ■ , found even re* 
<r s ’ * 
inotely associated with the deposits belonging to or assumed to he 
of glacial time were classes as paleolithic* Today it is tho re* 
sponslbility of every student of the question of beer loan occupation 
to diligently in^nluvphother a Hi him d , t ©2*&1 or csaeouSj 
• '=*•■*-- l * <t ~ • > • f hi, 
SO far collected, either ij ni.x, Uqqentim, 
i 
or Peru, conforms fully to the.requirements of science* 
1 single instance illustrating a dangerous pitfall of tills 
early 
^dio^ecvlorers of the Delaware diver Vaiioy 
research nay be cited* 
