Wealth of the World's Waste Places and OceaniaGilson, Jewett C. (Jewett Castello)
Science
Wealth of the World's Waste Places and Oceania
Gilson, Jewett C. (Jewett Castello)
Oceania -- Economic conditions; Waste lands
It may with truth be called naked because it is only partly clothed with
vegetation; moreover, such vegetation as exists is scanty and confined
chiefly to the river valleys and their slopes. In the interior are large
desert areas covered with lava and shifting sand. This desolate expanse
is frequently diversified by extensive jokulls, or elevated ice-fields,
one of which occupies four thousand square miles.
Strange as it may seem, the winters in the inhabited sections are not so
severe as those of New England, owing to the modifying influence of the
warm southwesterly wind and the mild temperature of the surrounding
waters. The summers are cool, owing to the nearness of the arctic
ice-fields. In the interior on the table-land one is apt to encounter
snowstorms even in August.
The only wild animal is the fox, of which there are two varieties, the
white and the blue. These animals probably drifted on the ice from
Greenland. They are hunted not only for their skins but also because
they attack the sheep.
The domestic animals are horses, cattle, sheep, dogs, and cats. The
horses and cattle are small. The ewes, instead of the cows, are milked.
Iceland ponies are famous for their hardiness and are sure-footed. Large
numbers of them are exported to England for service in the coal-mines.
There they are condemned to hard labor for life in the dark galleries.
Iceland ranks second among the geyser regions of the world, Yellowstone
Park being first. The boiling springs and geysers are not confined to
one locality but are scattered widely over the island. The most
prominent are east of Reykjavik.
According to its area probably no other part of the world except the
island of Java has so many volcanoes. More than one hundred craters and
cinder cones have been counted, many of which have been active within
the historical period of the island. The most destructive volcanic
eruption took place in June, 1783. The spring had opened auspiciously;
the cattle, sheep, and horses were cropping the juicy young grass; and
the air was balmier than usual. In the latter part of May a bluish smoke
accompanied by earthquakes began to spread over the land. As time passed
the earthquake shocks increased in violence. The surface of the earth
heaved like the ground swell of the ocean after a storm; the atmosphere
became filled with choking vapors and blinding smoke; the sun was
darkened and the low rumbling sounds became heavy peals of thunder.
Presently two mighty streams of lava, one of which was fifteen miles
wide and one hundred feet deep, came pouring down the sides of Skaptar
Jokull. The lava floods filled up the valleys, quenched rivers, and
spread destruction over the adjacent country. The intense heat blasted
the vegetation far and wide. Nine thousand people and fifty thousand
head of live stock were the result of the death harvest.
[Illustration: North Cape, Iceland]
Public-domain text, read in full here on John Shaqi.
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