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l far over midnight. But through it all runs the same sensation of longing and emptiness, which must not be noted. Ah, but at times there is no holding it aloof, and the hands sink down without will or strength--so weary, so unutterably weary. "Ah! life's peace is said to be found by holy men in the desert. Here, indeed, there is desert enough; but peace--of that I know nothing. I suppose it is the holiness that is lacking. "Wednesday, July 18th. Went on excursion with Blessing in the forenoon to collect specimens of the brown snow and ice, and gather seaweed and diatoms in the water. The upper surface of the floes is nearly everywhere of a dirty brown color, or, at least, this sort of ice preponderates, while pure white floes, without any traces of a dirty brown on their surface, are rare. I imagined this brown color must be due to the organisms I found in the newly-frozen, brownish-red ice last autumn (October); but the specimens I took to-day consist, for the most part, of mineral dust mingled with diatoms and other ingredients of organic origin. [57] "Blessing collected several specimens on the upper surface of the ice earlier in the summer, and came to the same conclusions. I must look further into this, in order to see whether all this brown dust is of a mineral nature, and consequently originates from the land. [58] We found in the lanes quantities of algae like those we had often found previously. There were large accumulations of them in nearly every little channel. We could also see that a brown surface layer spread itself on the sides of the floes far down into the water. This is due to an alga that grows on the ice. There were also floating in the water a number of small viscid lumps, some white, some of a yellowish red color; and of these I collected several. Under the microscope they all appeared to consist of accumulations of diatoms, among which, moreover, were a number of larger cellular organisms of a very characteristic appearance. [59] All of these diatomous accumulations kept at a certain depth, about a yard below the surface of the water; in some of the small lanes they appeared in large masses. At the same depth the above-named alga seemed especially to flourish, while parts of it rose up to the surface. It was evident that these accumulations of diatoms and alga remained floating exactly at the depth where the upper stratum of fresh water rests on the sea-water. The water on the surface wa
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