1 49 [Lesley. 
1871.] 
The ore is good. The outcrop runs along the top of a hill, about one 
hundred feet above the bottom of the Haw River Valley, and can be 
tunnelled into at that depth. There are apparent variations in the 
Fras. 18, 14, 15, 16. 
Seoteh, (lola ef Hoe anpforsunes ofbre ae hie Cnwke ben 
feet abave the 
Haw Rivet 
ees fi 200 300 40 $00 _fo2 yds. 
Faglb, Pes. Bh. miles in airline from Bemaja d tation, PRR. 
Ore-pit ok b, grepili,e,  d, eC; 
mearts and Mein beds \ Eyer 
a ri wath clay ee 
red wary pol, ashen 
Hew uthrles Herkinrses Geearme. dot. Ore. 
Ac ome pet @, Mare was ae ila. sol te 
S wel fi ad Hum Lhe Ve choy “ very Soff ‘i Vid 
ore, Dr the cutzrop , Hr whole appearereg G ana ontggt toms, paleatila we 
does matcme ‘dead 4 ore pers nene Lbs 
Uti Bommanrds : ‘ 
years ago Trabtisone dren Mavs 
7 Gthe’mett. A tus Hace 
dip, some of the outcrops seeming to be vertical, whereas the principal 
part of the mining has already shown a distinct dip towards the south- 
east and south. In pit fof the chart, the dip seems to be scarcely 40°, 
