R. Bakewell on the Falls of Niagara. 
3. near by is still there. The 
outline of the American Fall 
is represented by fig. 4. It 
is reduced from an extended 
Diickly wooded, (fig. 2, d,) 
which continues on fie edge 
of the chasm until we ap- 
few yards exhibit a zig- hd 
appearance on the precipice, and bare rock, as if the Fall Z 
once been there, and indicates a movement sideways as 
backwards. The ‘auacaitlinas of this wooded elevation ee 
Fall, ¢, suggests the high 
probability that it oo once 
surro y water, and as- 
sumed the ee which 
the precipice of the cave, (¢). 
The dotted lines represen 
the former river—the bed of 
which I did not trace back to 
its commencement, although 
I felt convinced in my own 
portunity escape. But it 
gives me pleasure to say that 
since the a was written 
I have unexpectedly con- 
versed with Mr. P, the very a oopadior of this 
princely domain, and it is his politeness to an entire stranger 
which enables me to speak ne ee more confidence ou this inter- 
esting point. I mentioned to him what my opinion was respect- 
ing a torrent having once poured over the precipice at the cave, 
