78 NOTES ON SUME MINERAL LOCALITIES IN 
In oe Creek (N.E.), with tin ore, titanic noone and water- 
worn quartz crystals; colours, blue, green. opaque, 
semi-transparent, common ; go ood-coloured ampaieitn stones, rare. 
At Rocky River (N.E.), it alluvial drifts, with gold, titanic iron, 
and “gn small, much worn ; colours, blue or brown. 
= he in ‘Faglehawk oe Doctor s Creek, with diamond, 
spinel, gold, magnetic iron sand, and waterworn tourmalines, semi- 
transparent, saat sometimes trangparent colours, blue, red, 
brown, green, yellow ; generally small in 
At Oban (N.E.), rare, but occasionally sind in comparatively 
large pieces, always much rubbed. 
Parti-coloured stones are often met with in the befure-mentioned 
localities ; some specimens are from blue to green, others from blue 
or green, in part, to colourless. Some varieties exhibit rays from 
to circumference. 
Following are the weights in grains troy and the sp. g. of four 
stones from New England :— 
Locality. bn procteg Sp.G. 
No. 1. Severn River se 683 4°151 
No. 2 - 103 4°120 
No, 3. - 194 3-959 
No. 4. Oban 257 4-015 
No. 1. Colour, blue, semi-transparen 
No. 2. ae pale , transparent ; ata flawed, worn on 
e 
No. 3. Blue, opaque ; slightly worn on edges. 
No. 4. Blue, opaque ; very much rubbed and rounded. 
All the above specimens, except No. 4, have been broken in 
such a manner as to pre sbhee the original crystalline form from 
being recognized. No. 4 is apparently a portion of a prism in 
which cleavage has taken seats at right angles * the longer axis. 
BeErYt. 
Near Emmaville (N. E.), i in Carr’s claim. Gulf Berar in 
vee = feldspathic rock ; prisms small, rarely more than +4 
In aie Creek (Emmaville, N.E.), haga in worn prisms and 
with tin ore, small ; colour, pale gre 
ished pieces ; blue and aad corundum is 
unded po 
alo? Salt in Alas a drifts with the beryls, 
i ia Eis 
es 
