50, known as' Tucker's.' "This ground, which is about 60 acres'in ; extent, has been tested in a most exhaustive manner, three faces having been opened and nine shafts sunk, exposing wash in some places 18ft deep, carrying tin ore in highly payable quantities. The right to an abundant supply of water has been Beoured. which water will be available for workfng the claim in the most extensive and remunerative manner on the 1 hydraulic system of sluicing. " The situation of the ground is all that could be desired for this mode of working, as in addi tion to its excellent situation with regard to fall from head race, there is also a good fall available for tailings. "The ore when dressed has only to be con veyed some two and a-half miles to Port Pet-a sub, a harbor available in all weather* for ships of the largest tonnage. In addition to its great value as an alluvial claim, there is every indi cation from the prospects already obtained that a rich lode will be found on the ground, which tg certain to be exposed as the ordinary work ing by sluicing is carried on. (Signed! J* A i ßbxnkzer Cokutfe. Mining Expert. Mr C. E. Riley, a Tasmanian Tin Miner, writes s— -**! have much pleasure as an expert in testi fying to the good and payable character of claim No. $0. the richness and depth of the wash, and the natural faculties for ground ttutelng on aa extensive scale, being such that With systematic working it ought to-pay a large -hyMend- v (Signed) "C.lTßrxire; ,' Peeasas, 20th July, 1889. Mr John Dwyer, also a Tasmanian Tin Miner, reports J— " To the Chairman, Tucker's Syndicate. " Dear Sir,-I beg to report that knowing well the position aad formatloo of claim No? 60,1 have no hesitation in saying that from the very -favorable indications snown during prospect. ins-, the greater part of which took plaoe under my own observation, the mine, if worked with ordinary economy, will pay good dividends from the stream tin alone, the working of which is almost sure to disclose the very rich lode that must exist in the vicinity; the presence of which it unmistakably shown by the rich tin impregnated stone found in tne present work ings amongst the alluvial tin, and which bears traces of little or no travelling. 