The National Geographic Magazine, Vol. I., No. 4, October, 1889Various
History
The National Geographic Magazine, Vol. I., No. 4, October, 1889
Various
Geography -- Periodicals
We find in California very marked and important effects following
irrigation. For instance, taking the great plains of Fresno, in the San
Joaquin valley: when irrigation commenced there twenty years ago, it
was 70 to 80 feet down to soil water--absolutely dry soil for nearly 80
feet--and it was the rule throughout the great plain, 20 miles in width
and 25 miles in length, that soil water was beyond the reach of the
suction pump; now, in places, water stands on the surface, rushes grow,
mosquitos breed, malarial fevers abound, and the people are crying for
drainage; and lands, whose owners paid from five to twenty dollars per
acre for the right to receive water, now need drainage, and irrigation
is considered unnecessary. The amount of water taken from King's river
which was, a few years ago, regarded as not more than sufficient for
one tenth of the land immediately commanded and that seemed to require
it, is now applied to a fourth of the whole area; so that if irrigation
keeps on, the time will come when the whole country will require
draining.
In a district, where water is applied by the broad method, I saw in
1877 enough water, by actual measurement of flow, put on 20 acres of
land to cover it 18 feet deep, in one season, could it all have been
retained upon it. It simply soaked into the ground, or flowed out under
the great plain. Taking cross sections of this country, north and south
and east and west, I found that where the depth to soil water had,
before irrigation, been about 80 feet, it was then 20, 30, 40 or 60 and
more feet down to it. The soil water stood under the plain in the form
of a mountain, the slope running down 40 to 50 feet in a few miles on
the west and north. On the south and southwest the surface of this
water-mountain was much more steep. In the Kern river country, we have
a somewhat similar phenomenon. Irrigation, in the upper portion of the
Kern delta, affects the water in the wells 6 or 8 miles away. As I
remember the effect is felt at the rate of about a mile a day, that is
to say, when water is used in irrigating the upper portion of the
delta, or of Kern island, as it is called, the wells commence to rise a
mile away in twenty-four hours, and five miles away in perhaps five
days.
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