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d to the knowledge of it that we already possess, I did not think it advisable to delay for such a purpose, and therefore as soon as we were underweigh steered for the mainland and continued to run northerly along the shore at the distance of six miles from it. At noon our latitude was 31 degrees 37 minutes 32 seconds. The coast is formed by sandy hillocks, or dunes, of from one hundred to one hundred and fifty feet high, here and there sprinkled with shrubs, but in many parts quite bare: behind this frontier a second range of hills was occasionally seen on which the trees appeared to be of moderate size: the shore is rocky for two miles off and in many parts the sea broke. At half-past three o'clock we were abreast of a low, sandy projection, supposed to be Captain Baudin's Cape Leschenault. The appearance of the coast to the northward on this cape differed from what we passed in the morning, in that the coast hillocks are more bare of vegetation; there appeared to be several ridges behind the coast dunes, but they were all equally unproductive of vegetation. Lancelin Island was not distinctly made out but the two small rocky lumps on the bare sandhills that M. De Freycinet mentions, were seen and thought to be very remarkable. At seven o'clock, having reached in my plan the latitude 31 degrees 0 minutes 30 seconds, and longitude 115 degrees 0 minutes 0 seconds, we hauled off shore for the night. January 16. And at six o'clock a.m. stood towards the land again. At half-past ten o'clock we were so near to it as to see the beach: at noon the latitude was observed to be 30 degrees 52 minutes 13 seconds, its longitude being 114 degrees 56 minutes 45 seconds, at which time we were on the parallel of the two rocky lumps seen the last evening. Hence we steered north on a parallel direction with the coast and ran forty-five miles, passing the different projections of the beach at the distance of four or five miles, and sounding in between nineteen and twenty-five fathoms. At four o'clock we were abreast of a bare sandy point which appeared to be the north head of Jurien Bay, in which two rocky islets were seen, fronted by reefs, on which the sea in many parts was breaking violently. To the southward of the point the coast hills are rather high and principally formed of very white sand, bearing a strong resemblance, from the absence of vegetables, to hills covered with snow. Here and there however a few shrubs partially conc
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