NO. 2 BIBLIOGRAPHY OF TIN HESS 127 



NEW SOUTH WALES (Continued) 



811. . Mines and mineral statistics of New South Wales. 



May 7, 1853, p. 71. 



In author's report to the Colonial Secretary, he drew attention for the first time to 

 the probable occurrence of extensive deposits of tin ore. He then stated that 

 " wolfram and oxide of tin with tourmaline, occur near Dundee and in Paradise 

 Creek, and it is probable that this ore of tin is plentifully distributed in the alluvial 

 of other tracts as I have found it amidst the spinelle, rubies, oriental emeralds, 

 sapphires, and other gems of the detritus from granite." 



812. . Researches in the Southern gold fields of New South Wales, 



1860. 



Tin, pp. 109, 12S. 



813. . Anniversary Address. 



Trans. Proc. Roy. Soc. New South Wales, for 1873 (1874), Sydney, pp. 1-39. 

 Address contains notes on tin in New South Wales. 



814. . Remarks on the sedimentary formations of New South Wales, 



etc. 



Edition 3, 1875, Sydney, pp. 61, vertical sections. 



Digest: Geol. Rec. for 1875, London, p. 148. 



Tin mines of New South Wales and Queensland occur in Devonian rocks. 



815. COGLAN, T. A. The wealth and progress of New South Wales for 1886- 



1887. 



Sydney, 1887, pp. 82-84. Ibid., for 1890-1891 (1891), pp. 84-86. Ibid., for 1894 (1896), 

 pp. 210-212. Ibid., for 1805-1896, Vol. 2, 1897, pp. 493-1023. 



816. CONDEB, HARTWELL. The occurrence of stannite in Australasia. 



Austr. Mg. Stand., Vol. 40, 1908, Sydney and Melbourne, p. 577. 



Gives a description of stannite and mentions localities in which it has been found. 

 States that it occurs in considerable quantity in the Conrad mines, New South Wales, 

 and the Oonah Mine (Zeehan) and at Heemskirk, Tasmania. In the Conrad mine 

 stannite occurs in a quartz vein cutting granite and is accompanied by argentiferous 

 galena, zinc blende, chalcopyrite and arsenical pyrites. Cassiterite occurs in the 

 granite, but rarely if ever in the vein. At Oonah stannite occurs with bismuthinite, 

 wolframite, galena, pyrite, and zinc blende in a vein between quartzite and graphitic 

 schist, and closely connected with galena deposits. Stannite at both places is argentif- 

 erous. Discusses difficulties of treatment. 



816a. COTTON, LEO A. The tin deposits of New England, New South Wales. 



Part 1, Proc. Linn. Soc. New South Wales, Vol. 34, 1910, Sydney, pp. 733-781, 

 pis. 59-62, figs. 13, geol. map. 



Describes the country rocks in detail, the distribution of the lodes, their direction 

 and causes of trend. The deposits are divided into eleven classes which do not appear 

 to be very distinctive. The veins under the different classes are described and com- 

 parisons made with occurrences in other countries. 



817. Cox, HERBERT S. Tin deposits of New South Wales. 



Journ. Proc. Roy. Soc. New South Wales, for 1886, Vol. 20, 1887, Sydney, pp. 93-112, 

 figs. 7. 



General description of both lode and alluvial deposits with geology of district. 

 Accompanying minerals are wolframite, copper pyrites, arsenical pyrites, fluorspar 

 (not in large quantities), tourmaline, fluorine bearing micas, and topaz; at Gulf mine, 

 near Bendemeer, beryl forms a rock in which cassiterite is impregnated. In the Inverell 

 district, diamonds, sapphires and zircons occur with stream tin. Cassiterite is 

 iridescent at Silverton. 



