THE NORTHERN DISTRICTS OF NEW SOUTH WALES. 79 
Following is a description of four of the largest stones observed 
from this localit ity :— 
No. 1. Colour, pale green ; exterior, rough ; len rounded 
weight in air, 759 grs.; sp. g. 2°673. 
No. 2. Portion of prism not much worn ; colour, green, rather 
pale; weight in air, 341 grs.; s 664. 
No. 3. Irregular fragment ; colour, green, pale ; weight in air, 
319 grs. ; sp. g. "2-703. 
No. 4. Green prism, much worn, j-in. in diameter, 1 in. long, 
transparent ; weight in air, 269 grs. ; sp. g. 2°690. 
Dramonp. 
In Zaglehawk and Doctor’s Creek, near Bingera, in drift formed 
by the decomposition of quartz conglomerates, associated with 
blue, green, red, and colourless corundum ; also, topaz, garnet, 
tourmaline, and quartz. All the associated minerals are more or 
less rubbed and worn. 
At and in the neighbourhood of Tingha (N.E.), small diamppile 
are occasionally obtained whilst washing for tin ore. larg 
misshapen octohedral stone was found, or said to have been ee 
in Cope’s Creek, at Tingha, some time in the year 1882. This 
stone, which is now in the possession of Mr. 8. W. ——! of 
glomerate, has become disintegrated, has spread out and 
enveloped the sides of the hillocks ; other portions, having 
carried further oe have filled up some of the small 
obtained, fou there appears to be as ato no phen firm as to 
senaaad ‘they have been really derived from these conglomerate 
rocks, or have only become associated with the disinte tegrated 
‘istetinds after the decomposition of the original rock. The con- 
a in question are found to be resting unconformably upon 
u pid nae upper evonian or lower carboni iferous 
r 
and underlaying the diamondiferous drift ; but have never had an 
opportunity to make a proper search in this locality for fossils. 
