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ificent desolation about us. Even on the march, with loaded sledges and tugging dogs to engage attention, unconsciously one finds oneself with wits wool-gathering and eyes taking in the scene, and suddenly being brought back to the business of the hour by the fiend-like conduct of his team. There is an irresistible fascination about the regions of northern-most Grant Land that is impossible for me to describe. Having no poetry in my soul, and being somewhat hardened by years of experience in that inhospitable country, words proper to give you an idea of its unique beauty do not come to mind. Imagine gorgeous bleakness, beautiful blankness. It never seems broad, bright day, even in the middle of June, and the sky has the different effects of the varying hours of morning and evening twilight from the first to the last peep of day. Early in February, at noon, a thin band of light appears far to the southward, heralding the approach of the sun, and daily the twilight lengthens, until early in March, the sun, a flaming disk of fiery crimson, shows his distorted image above the horizon. This distorted shape is due to the mirage caused by the cold, just as heat-waves above the rails on a railroad-track distort the shape of objects beyond. The south sides of the lofty peaks have for days reflected the glory of the coming sun, and it does not require an artist to enjoy the unexampled splendor of the view. The snows covering the peaks show all of the colors, variations, and tones of the artist's palette, and more. Artists have gone with us into the Arctic and I have heard them rave over the wonderful beauties of the scene, and I have seen them at work trying to reproduce some of it, with good results but with nothing like the effect of the original. As Mr. Stokes said, "it is color run riot." To the northward, all is dark and the brighter stars of the heavens are still visible, but growing fainter daily with the strengthening of the sunlight. When the sun finally gets above the horizon and swings his daily circle, the color effects grow less and less, but then the sky and cloud-effects improve and the shadows in the mountains and clefts of the ice show forth their beauty, cold blues and grays; the bare patches of the land, rich browns; and the whiteness of the snow is dazzling. At midday, the optical impression given by one's shadow is of about nine o'clock in the morning, this due to the altitude of the sun, always giving
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