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ts where the soil is suitable for gardening purposes, thus ensuring a supply of vegetables during the greater part, perhaps the whole of the year. (*Footnote. A sample of this ironstone picked up from the surface has furnished materials for the following remarks, for which I am indebted to the politeness of Warrington W. Smyth, Esquire, of the Museum of Practical Geology. On examining the specimens which you presented to our Museum, I see that they consist for the most part of the red or anhydrous peroxide of iron--similar in chemical character to the celebrated haematite ore of Ulverstone and Whitehaven. It is, however, less rich in iron than would be inferred from its outward appearance, since the pebbles on being broken, exhibit interiorly a loose and cellular structure, where grains of quartz and plates of mica are interspersed with the ore, and of course reduce its specific gravity and value. Such an ore, if occurring in great quantity, and at no great distance from abundant fuel and from a supply of limestone for flux, may prove to be very valuable; but I should fear that your suggestion of employing the coral and shells of the coast, for the last-mentioned purpose, might impair the quality of an iron thus produced, for the phosphoric acid present in them would give one of the constituents most troublesome to the iron-master, who wishes to produce a strong and tough iron.) SAIL FROM CAPE YORK. On November 2nd we sailed from Cape York on our way to Port Essington and Sydney, but owing to the prevalence of light airs, chiefly from the eastward, and calms, we did not reach Booby Island until the 4th, having passed out of Torres Strait by the Prince of Wales Channel. The Bramble was left to perform some work in Endeavour Strait* and elsewhere along the Inner Passage, and after its completion to make the best of her way to Sydney down the eastern coast of Australia against the trade-wind, before successfully accomplished by only two other vessels besides herself. Of course a considerable degree of interest has been excited by this intended procedure, as the two vessels start under pretty equal circumstances to reach the same place by two very different routes, of the merits of one of which comparatively little is known. (*Footnote. Since the survey of Endeavour Strait in 1844 by Lieutenant Yule in the Bramble (then attached to the Fly under Captain F.P. Blackwood) several sunken rocks have been discovered,
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