One, Ennan. Two, Gera. Three, Giro. Four, Gerack. Five, Miltingum. Six, Ennan Miltingum. Seven, Gera Miltingum. Eight, Amgrokim. Nine, Conizinkin. Ten, Mingitkim. Twelve, Mingitkim Gera Parole. Thirteen, Mingitkim Giro Parole. Fourteen, Mingitkim Gerack Parole. Fifteen, Kiddegitten. Sixteen, Kiddegitten Ennan Parole. Seventeen, Kiddegitten Gera Parole. Eighteen, Kiddegitten Giro Parole. Nineteen, Kiddegitten Gerack Parole. Twenty, Kalekin. Thirty, Kalekin Mingitkim Parole. Forty, Gerack Kalekim. Fifty, Miltingum Mingitkim Parole. Sixty, Gera Kalekim Mingitkim Parole. Seventy, Giro Kalekim Mingitkim Parole. Eighty, Gerack Kalekim. Ninety, Gerack Kalekim Mingitkim Parole. One Hundred, Miltingum Kalekin, 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.