KiATraj[BAL P §[i(£ira®Ri nawaiBinriiiJi© ®ir®ijiem strata aw® 
Shore- of Luke Ene, for//and CJuaitouimie, County- Lengthy one forih of a mile 
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PLATE YIII 
i. 
y t m,. tiiere is a ffiick. mass of day gray-el and fragments of Che, rock separating a,portion) 
of the strata, above, which, at, either extremity is broken, and intermingled, with dir drift. ' 
.11 JV. the same fhmomena are exhibited, as at It. and, extending a/ considerable, distance rigid and, left . The lover projecting 
mass 1.1..S. ts a shelf of rode extending nearly two thirds of the whole distance and is entirely undisturbed,. 
t deep cavernous opening/ znade by the action, of the. wou-'es 
ip seer/, near the termtiutition, of the section . 
//// a/txt are, found standuuy 
greatest possible, confusionr . 
worn, fragments of the rock -The Strata, above less ctistnfbedfhe surfac&\ till e.andf.the STrafare again, sgrouted andthe intervening s/utceiided, oitiedccy and 
' grooved and striated after the manner of Glacial furrows. / dagmmisofliieshalyrock,Siewiwle/mssfobM,&ct)!itorted,.TkeSlroita,abovearebroh;nlutiwtclis/Uar&i. 
vnsmnxiled between, /tie 
as before indicated . 
,/oou 
C. Gln.g and, gravel with,,fragments of the subjacent / d. Clay ittitih 
Stratified, rock, rntermirugled/ tn, great confusion,! ofdiose betim 
At K. there, is a, mass or ccay cuiia, fragments or rook, 
strata,, the surface, below smoothed, and, striated- 
or vritermui. 
a. Upgua Stracanf, yellowish loam, a-nd, graved, 
b. Second, Stratum, bluish, clay and, gravel. 
