76 
neighborhood, or were carried there, I am unable to say. 
To all appearance the only deposit superior to the glacial 
clay in the neighborhood is a thin crust of travertine lime- 
stone which lies directly on the boulder clay. 
(b) Corney Point Road.—A large erratic occurs near the 
main road from Warooka to Corney Point. Ft is situated on 
the north side within about twent yard of t road in 
is much greater. It is not a "gran nite roc ock” but a 
colored, granular, lóra biendiè schist, having a close re- 
coast at Corney Point. From the effects of weathering it 
has split into several pieces—the measurements given are in- 
tended to include the block as a whole. The occurrence of 
this transported stone in the position described, is intercst- 
img, as it marks the most westerly point that I was able to 
it 
lagoons that are Ra tueféd over the southern portions of 
a 
are pneri of ac features Bet. with my 
visit was on the north side of the ake, in Section No. 178 
tains a group of twelve large pieces of pink-colored granite, 
having but a slight elevation above the ordinary lev el The 
group measures ten feet by six feet, and was probably only 
one piece si sent but has split alone joint planes as the 
result of weathering. 
bout —€— yards to Pen westward of this erratic, other 
two huge granite blocks can be seen standing in the mud of 
