The Siberian Overland Route from Peking to Petersburg,: Through the Deserts and Steppes of Mongolia, Tartary, &c.Michie, Alexander
History
The Siberian Overland Route from Peking to Petersburg,: Through the Deserts and Steppes of Mongolia, Tartary, &c.
Michie, Alexander
China -- Description and travel; Siberia (Russia) -- Description and travel
Our course lay obliquely across the lake, about W.S.W. towards
Listni-nijni at the head of the lower Angara. Had the weather been
less severe we should have been tempted to keep the deck, and enjoy
the sublime scenery with which we were surrounded. Both shores of
the lake are very mountainous, those on the south-eastern side being
highest, and covered with snow down to the water's edge. There was
very little snow on the western side, the snow showers up to that
time having been very slight and partial. The water of the lake,
away from land, is of a very deep blue, almost black. Its depths
have never been fathomed, probably from the want of proper tackle,
for I am not aware that any ocean-sounding apparatus has ever been
used on the Baikal. It has been said, I know not on what authority,
that "no bottom" has been found at three thousand fathoms; but much
that has been said of the Baikal is exaggerated, and I greatly doubt
whether such a depth has been satisfactorily established. I was
informed by a gentleman on the spot, personally acquainted with that
part of the country, that the deepest soundings yet obtained in the
lake were two hundred fathoms, and that beyond that depth nothing
was known. It is only in a few places where soundings have not been
taken.
The lake is over 300 miles in length, averaging about thirty in
breadth; it covers a surface of 11,000 square miles, and is 1300
feet above the sea level. It is fed by two considerable rivers, the
Little Angara on the north, and the Selenga on the east. It has only
one outlet, the Great Angara, on the west, which drains the waters
of the lake into the great river Yenisei, and that again into the
Frozen Ocean. It is estimated that the water so drained, out of
the lake does not amount to more than one-tenth of the quantity
poured into it. This estimate may be a little wide of the mark, but
there can be no doubt of the fact that the lake receives a large
surplus of water above what it gives out, which the quantity lost by
evaporation must be utterly inadequate to account for. The level of
the water fluctuates only a few feet between seasons.
Baikal is a Mongol name. In saintly Russia it is called the Holy
Sea, and among the peasant navigators it is considered high treason
to call it a lake.
Public-domain text, read in full here on John Shaqi.
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