The Discovery of America Vol. 1 (of 2): with some account of Ancient America and the Spanish ConquestFiske, John
History
The Discovery of America Vol. 1 (of 2): with some account of Ancient America and the Spanish Conquest
Fiske, John
America -- Discovery and exploration; Latin America -- History
In such vessels, well stocked with food and weapons, the Northmen were
accustomed to spend many weeks together on the sea, now and then
touching land. In such vessels they made their way to Algiers and
Constantinople, to the White Sea, to Baffin's Bay. It is not, therefore,
their voyage to Greenland that seems strange, but it is their success in
founding a colony which could last for more than four centuries in that
inhospitable climate. The question is sometimes asked whether the
climate of Greenland may not have undergone some change within the last
thousand years.[195] If there has been any change, it must have been
very slight; such as, perhaps, a small variation in the flow of ocean
currents might occasion. I am inclined to believe that there may have
been such a change, from the testimony of Ivar Bardsen, steward of the
Gardar bishopric in the latter half of the fourteenth century, or about
halfway between the time of Eric the Red and our own time. According to
Bardsen there had long been a downward drifting of ice from the north
and a consequent accumulation of bergs and floes upon the eastern coast
of Greenland, insomuch that the customary route formerly followed by
ships coming from Iceland was no longer safe, and a more southerly route
had been generally adopted.[196] This slow southward extension of the
polar ice-sheet upon the east of Greenland seems still to be going on at
the present day.[197] It is therefore not at all improbable, but on the
contrary quite probable, that a thousand years ago the mean annual
temperature of the tip end of Greenland, at Cape Farewell, was a few
degrees higher than now.[198] But a slight difference of this sort
might have an important bearing upon the fortunes of a colony planted
there. For example, it would directly affect the extent of the hay crop.
Grass grows very well now in the neighbourhood of Julianeshaab. In
summer it is still a "green land," with good pasturage for cattle, but
there is difficulty in getting hay enough to last through the nine
months of winter. In 1855 "there were in Greenland 30 to 40 head of
horned cattle, about 100 goats, and 20 sheep;" but in the ancient
colony, with a population not exceeding 6,000 persons, "herds of cattle
were kept which even yielded produce for exportation to Europe."[199] So
strong a contrast seems to indicate a much more plentiful grass crop
than to-day, although some hay might perhaps have been imported from
Iceland in exchange for Greenland exports, which were chiefly whale oil,
eider-down, and skins of seals, foxes, and white bears.
Public-domain text, read in full here on John Shaqi.
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