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amining large quantities of driftwood both on the west coast and on the east coast of Greenland. I have, moreover, found pieces drifting in the sea off the east coast, and, like earlier travellers, have arrived at the conclusion that much the greater part of it can only have come from Siberia, while a smaller portion may possibly have come from America. For amongst it are to be found fir, Siberian larch, and other kinds of wood peculiar to the north, which could scarcely have come from any other quarter. Interesting in this respect are the discoveries that have been made on the east coast of Greenland by the second German Polar Expedition. Out of twenty-five pieces of driftwood, seventeen were Siberian larch, five Norwegian fir (probably Picea obovata), two a kind of alder (Alnus incana?), and one a poplar (Populus tremula? the common aspen), all of which are trees found in Siberia. "By way of supplement to these observations on the Greenland side, it may be mentioned that the Jeannette expedition frequently found Siberian driftwood (fir and birch) between the floes in the strong northerly current to the northward of the New Siberian Islands. "Fortunately for the Eskimo, such large quantities of this driftwood come every year to the coasts of Greenland that in my opinion one cannot but assume that they are conveyed thither by a constantly flowing current, especially as the wood never appears to have been very long in the sea--at all events, not without having been frozen in the ice. "That this driftwood passes south of Franz Josef Land and Spitzbergen is quite as unreasonable a theory as that the ice-floe with the relics from the Jeannette drifted by this route. In further disproof of this assumption it may be stated that Siberian driftwood is found north of Spitzbergen in the strong southerly current, against which Parry fought in vain. "It appears, therefore, that on these grounds also we cannot but admit the existence of a current flowing across, or in close proximity to, the Pole. "As an interesting fact in this connection, it may also be mentioned that the German botanist Grisebach has shown that the Greenland flora includes a series of Siberian vegetable forms that could scarcely have reached Greenland in any other way than by the help of such a current conveying the seeds. "On the drift-ice in Denmark Strait (between Iceland and Greenland) I have made observations which tend to the conclusion that t
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