622 Transactions. 
stream has worn, consisting of concretionary sands, well bedded, with 
layers of harder and softer material interstratified with sandy shales ; some 
of the harder layers contain numerous sharks’ teeth. These beds strike 
N. 10° W., and dip to the west at angles of 15°. They are succeeded by 
—— BENMORE COAL AREA 
B Direction- S.E.to N.W. Length- about Ye Mile 
$ — Section | 
© Along Creek near W.E.end of Area 
\ 1 H : 
\ fob M te 
\ N 2 v) v v 
35° \ as 
> S ^] 
zs \ N 
S.E. e. e ee NW. 
— Section2 —— 
Across middle of Area 
SE. e. d. aris N.W. 
— LGrevwacke 2.Coat-MeasureES — 
: Rhyolite conglomerate 
. Coal seams with Clays & Sands 
‚ Sands with Gypsum & Sulphur 
. Greensands ; 
. Sands whitish &ye llowishk brown 
оазе еа 
faulted against the greywacke, which has been pushed over the sands from 
the south-east. The fault-plane hades at an angle of 40?, and apparently 
runs north-east and south-west. The surface of the sand is indurated an 
much slickensided. It is impossible to determine the amount of the throw 
from the exposures, 
