sed Afognak, and made Wood
Island landing, where we were most hospitably received by the North
American Fur Company's people. Wood Island, about 1-1/2 miles from Kadiak,
is small and well covered with spruce. It has some two hundred people,
for the most part natives, and under Russian rule was used for a huge
ice-storing plant. Kadiak Island, 100 miles by 30, is thickly studded
with mountains, and extremely picturesque, with the white covering of
early spring, as we found it, or when green with heavy grass dotted with
wild flowers in July.
[Illustration: ST. PAUL, KADIAK ISLAND.]
The Kadiak group looks as if it might have fallen out of Cook Inlet, and
one of the native legends tells us that once the Kadiak Islands were so
near the Alaskan shore that a mammoth sea otter, while trying to swim
through the narrow straits, got wedged between the rocks, and his
tremendous struggles to free himself pushed the islands out into their
present position. The sea otter and bear have always been most
intimately connected with the lives of the Kadiakers, and have exercised
a more important influence on their characters than any of their
surroundings except the sea. It is no wonder, then, that the natives
endowed these animals with a strength and size which easily takes them
into the realm of mythology. The sea otter being nearly extinct, the
bear is now made to shoulder all the large stories, and, strong as he
is, this is no light burden.
The Kadiak coast line is roughly broken by deep bays, running inland
from a half mile to fifteen or twenty miles. Some are broad, others
narrow, but all are walled in by serrated, mountainous sides, much
resembling the fjords of Norway. The highest peaks are about 4,000
feet.
The portions of Kadiak Island uncovered by spruce and the barren lands
of the mainland, are not absolutely devoid of trees or bushes. Often
there is a considerable growth of cottonwood trees along the bottom
lands of the streams, and large patches of alder bushes are common, so
that when the leaves are well out, one's view of the bottoms and lower
hillsides is much obscured. The snowfall must be heavy on the upper
reaches of the mountains, as there are great white patches to be seen
well into the summer time. The climate is not what one would expect,
unless he should look at the map, and note the warm Kuro Siwo (Japan
current) sweeping along the southern Alaskan coast. Zero weather is
uncommon, and except for the great
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