336 
Geology of Sydney. 
2. Glossopteris, abundant in the shales at Lith- 
gow. 
3. Remarkable weathering of granite immedi- 
ately around Bathurst. The rock is decom- 
posed in situ to a depth of 60 to 100 feet. 
4. Basalt, showing a streaming structure of its 
felspars, capping the Bald Hills. 
5. Junction of slate and granite, near New- 
bridge platform. 
6. Contorted slates on the road from George’s 
Plains to Cow Flat, and also in the hills about 
the old Copper Mines. 
7. Diabase, in a quarry near the R. C. Church, 
Blayney, and on the hills around the Annan- 
dale Copper Mine. 
8. Gabbro, around the township of Carcoar. 
9. Spheroidal weathering of granite, on the hill 
above Cowra. 
10. Fossil corals in the limestone at the lime- 
kilns, 18 miles north of Bathurst. 
11. Silurian fossils, abundant Grinoids, &c., at 
Cave Creek, near Orange. 
12. Fossil corals in limestones, at Molong. 
13. At Molong the limestones may be noted 
dipping west. Six miles to the west of 
Molong they have an easterly dip. 
14. Serpentine, near Lucknow mines, and also at 
Whitney Green. 
15. Basalt, andesite, and slate rocks. Orange — 
German s Hill Road. 
