The National Geographic Magazine, Vol. I., No. 4, October, 1889Various
History
The National Geographic Magazine, Vol. I., No. 4, October, 1889
Various
Geography -- Periodicals
streams of California are of such a character that the work of the
farmers can avail nothing. There must be strong associations and large
capital. For this purpose special laws are required. On the Santa Aña,
in San Bernardino county, water has been easily diverted, and such is
the case with every stream in the interior valley of San Bernardino and
Los Angeles counties.
Capital for the first works was not required. The water was procured by
primitive methods and the works were simple. But in San Diego, an
entirely different condition of affairs prevailed. There the waters are
back in the mountains, twenty or twenty-five miles from the coast, and
the irrigable lands are close along the coast, or within ten or twelve
miles of it. To bring the water out of these mountains requires the
construction of ditches following the mountain sides for 20 to 35
miles. But simple ditches do not answer, because of the great quantity
of water lost from them. So the companies have resorted to fluming, and
even to lining the ditches with cement. Thus in San Diego, individual
effort is out of the question. Farther north again, in the great
interior valley, King's river is a stream where coöperative and
individual effort have been efficient, although it requires a greater
amount of capital there than in the southern interior valley. In the
southern interior valley, perhaps, $10,000 would often build a ditch
and divert all the water that the supply would furnish. On King's river
the works have cost from $15,000 to $80,000 each; on Kern river the
works have cost from $15,000 to $250,000 each; and on the Tuolumne they
will cost from $1,000,000 to $1,200,000 apiece. On Merced river, the
cost has been $800,000 for one work. Taking the streams from San
Joaquin river north, that come out of the Sierra Nevada, up to the
northern end of the valley where the Sacramento river enters it, every
important stream comes into the valley within a deep gorge. The beds of
several of the northern streams are so filled up with mining debris
that diversion from them would be comparatively easy, but in their
natural state there is not an important stream north of the San Joaquin
which could be utilized for irrigation by any other means than through
the agency of capital in large amount. On the west side of this great
valley the tillable strip is comparatively narrow. It is on the lee
side of the coast range of mountains. Precipitation is made first on
the seaward face of the Coast Range, and then crosses the valley,
dropping upon the inland face of the outer range very little more than
upon the valley itself, where the precipitation is only about 10
inches. So that we have no streams coming out of the Coast Range into
the southern part of the interior valley specially noteworthy as
irrigation feeders. But as we go northward the Coast Range becomes
wider, and the big mountain basin containing Clear Lake furnishes a
large supply of water to Cache Creek, probably enough for 10,000 acres.
Public-domain text, read in full here on John Shaqi.
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