being entombed. 
In 
situated about twenty-five miles north of CoteSt — 
locality in Wentworth occurs on Lake Louisa, about sixteen miles 
of the first Grenville specimens, from which — 
the same distance north of west, the lines — 
measuring these distances running across several py U- 
e We 
in 
gray limestone, which has somewhat the aspect of a conglomerate, 
specimens have been i 
by Giimbel in his illustrations of the forms met with by himm 4 
Bavaria. * * * 
sin the county of 
. Reddish and flesh-colored granitic oni 
j TA granitic gneiss : 
Sais Se Fosn flesh-colored gneiss, ainstimnse hornblendic; mean of seve 10,400 
' ements 
: manee magne 
nee graphite ; sometimes very thin, but in other places atta 
. estim * 
om an ascending section of the L oe 
Hastings, Ontario, by Mr. H. G. Ven me 
i. ge 
Laurentiat 
__, 2,000 
--- 
weweeern 
dad 
-- 
: mpegs?" 
sian, includes in Elzivir a 0 . 
bone aw 
e 
ated as averaging -..-------------" 
“ : th dark micaceous schists, chloritic and epiO™” 4 999 
rocks, including beds of Magnetite ; average oo T 
ms % granular magnesian limestone, aan and 930 
’ e 
interstratified with dio 
small beds of impure steati 
rites, 
and near the base with siliceou yes 
te aaa 
is metalliferous, holding disseminated copper is of 
This limestone 
blende, mispickel, and 
. 
