TAtLS OF montmorbmcy, 363 
i.'V(| produced by the foaming currents, and the 
tl^^sscs of stone, form a scene wild and pictu- 
V^*'ted • • now taking a southern direction, is 
c N (j, _ '*1 its vplni'nv oni\ fnims a £>Tand Cascade inter- 
ly, —velocity, and for ms a grand cascade inter- 
rocks. A quarter of a mile lower down a 
produced. After exhibiting an agreeable 
Si'’’* its course, the river is precipitated, in an 
f'SfWcular direction, over a rock two hundred 
r'’"ihh Wherever it touches the rock it 
;jt>roj)^ll® clouds of rolling foam j and, beneath, where 
l'3s "'■th unintemipted gravitation, it forms nu- 
like wool or cotton, which are gradually 
'i' fte descent, until they are received into tlie 
clouds of rolling foam j and, beneath, where 
with ...... 
> Iik( 
the c 
‘nd al 
J nc °t this surprising fall ; the brightness and volu- 
course ; the swiftness of their movement 
effg abyss beneath. 
worn the summit of the cliff is awfully grand. 
The prodigious depth of the descent of 
: and the loud and hollow noise emitted 
tj'ut t[, ■' '•welling 
l'li *^*'tioti^ ^ttshing waters, forcibly combine to attract 
elling witli incessant agitation from the 
Sft ^ 
.‘lu ’'Utne impress the mind of the spectator 
cf grandeur and elevation. The clouds of 
i-.'Ai 
assume the prismatic colours, contri- 
‘Veti 
cf a 
the scene. They fly off from the fall in 
revolving sphere, emitting with velocity 
:t| ' ttitef-’ ®Pray, which spread in receding, until 
*^y ’^he neighbouring banks, or dissolv- 
of 
degfp, 
'f% ^''■ecivji’ resplendent beauty, to flow down the 
the summit of which is crowned with 
I ®ision of the stream, to the breadth of 
i feet, •''"‘I the various small cascades pro- 
,^t. T ^’^C'iualities of its rocky bed, on its way to 
^'^rence, display a very singular and pleastnj 
fall is one hundred feet ; and the 
'bounded by steep cliffs, forms an angle of 
When viewed from the beech, the 
