It is quite probable that all, or nearly all, the tribes or settlements on the shores of the Arctic, both on the Asiatic and American sides, have a common language, though differing, as we found, in some words, and also in pronunciation. The language is that of the Esquimaux race.
Those with whom we lived, and other settlements or tribes on the Asiatic coast with whom we have had any acquaintance, from East Cape to the north as far as our wreck, have no written language. We could not learn from them that any one had ever attempted to instruct them, or reduce their language to some system, or that any teacher in religion had ever visited them. Without a written language, or books, or teachers, or oral instruction in some form, the certain results must invariably be, that from age to age, they will continue in the same condition of mental ignorance, moral blindness, and physical degradation.
It was the opinion of Mr. Abram Osborn, Jr., who became a proficient in the language of the natives, and could converse with them with ease and fluency, that it was simple, and he believed could be readily reduced to some systematic form. The method he resorted to, in order to acquire the language, was simply this: when he heard a native word, he would write it, according to its sound, upon a piece of copper, and place opposite to it its English definition. He made inquiries of the natives as to the meaning of their words, and what they called certain things. In this manner he became very familiar with all the terms and phrases which they used.
The following are a few specimens of native language. English words are placed in the first column, and the Esquimaux in the second.
ICEBERGS.
Some of the most remarkable phenomena seen in the Northern Ocean, and the manner of their formation, are icebergs. They are greatly feared by seamen, and a contact with them would be equivalent to striking a rock. They are formed far up in the polar region during the intense and protracted cold of winter; and in the change of the season in summer, though ice is always accumulating in high latitudes, they drift with the currents into lower latitudes, where they melt, and finally disappear. They are of varied dimensions, indicating by these facts somewhat the sources whence they come, and wearing every conceivable exterior form.
They are formed by the falling of snow over steep and high cliffs on the borders of the sea; "little by little the incrustations on the shore and cliffs increase to the size of mountains, and then, being torn away from their fastenings, either by the winds, or by their own weight, or by the action of the sea beating against their bases or undermining them, are swept into the ocean, where they continue to accumulate by the falling of snow and frozen water, and finally resemble great islands."
Large masses of ice, which take the form of bergs, are formed along the rocky-bound coast of the Arctic.
On the fall of the tide, after the ocean has been frozen over, the localities of the rocks and ledges are clearly observable. When the tide rises, the superincumbent mass is lifted up, and a new layer is formed underneath. This process goes on with the rise and fall of the tides and the accumulation of ice, until vast ridges, broken and dislocated, assuming every variety of appearance, are thus pressed up to a great height.