The Voyage of the Vega round Asia and Europe, Volume I and Volume IINordenskiöld, A. E. (Adolf Erik)
History
The Voyage of the Vega round Asia and Europe, Volume I and Volume II
Nordenskiöld, A. E. (Adolf Erik)
Arctic regions -- Discovery and exploration; Northeast Passage; Vega (Ship)
[Illustration: HAIRSTAR FROM THE TAIMUR COAST. _Antedon Eschrichtii_,
J. MUeLLER. Three-fifths of the natural size. ]
Immediately after the _Vega_ lay-to, I therefore went down on the
ice in order to see whether here too some such metalliferous dust,
as I had before found north of Spitzbergen, was not to be found on
the surface of the ice. Nothing of the kind, however, was to be
seen. On the other hand, Lieutenant Nordquist observed small yellow
specks in the snow, which I asked him to collect and hand over for
investigation to Dr. Kjellman. For I supposed that the specks
consisted of diatom ooze. After examining them Dr. Kjellman however
declared that they did not consist of any organic substance, but of
crystallised grains of sand. I too now examined them more closely,
but unfortunately not until the morning after we had left the
ice-field, and then found that the supposed ooze consisted of pale
yellow crystals (not fragments of crystals) without mixture of
foreign matter. The quantity of crystals, which were obtained from
about three litres of snow, skimmed from the surface of the snow on
an area of at most 10 square metres, amounted to nearly 0.2 gram.
The crystals were found only near the surface of the snow, not in
the deeper layers. They were up to 1 mm. in diameter, had the
appearance shown in the accompanying woodcut, and appeared to belong
to the rhombic system, as they had one perfect cleavage and formed
striated prisms terminated at either end by truncated pyramids.
Unfortunately I could not make any actual measurements of them,
because after being kept for some time in the air they weathered to
a white non-crystalline powder. They lay, without being sensibly
dissolved, for a whole night in the water formed by the melting of
the snow. On being heated, too, they fell asunder into a tasteless
white powder. The white powder, that was formed by the weathering of
the crystals, was analysed after our return--21 months after the
discovery of the crystals--and was found to contain only carbonate
of lime.
[Illustration: FORM OF THE CRYSTALS. Found on the ice off the
Taimur coast. Magnified thirty to forty times. ]
Public-domain text, read in full here on John Shaqi.
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