Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
_Injury in the arid regions._—In the arid regions, where the rainfall
frequently comes in heavy downpours or “cloudbursts,” immense damage
to pasture lands has been brought about by overstocking, in Arizona
and New Mexico; involving the destruction of the natural cover of
vegetation and the loosening of the surface especially by sheep; after
which a heavy rainfall will carry off the surface soil, the muddy water
being gathered largely in the trails made by cattle going to water.
Thus gradually gullies are formed, which enlarging more and more become
ravines and cut up the pasture slopes into “bad lands,” useless equally
for pasture and for agriculture.[83] California, eastern Oregon and
Washington, and Montana, offer striking and lamentable examples of the
same destructive agencies.
[83] Open Range and Irrigation Farming. R. H Forbes, in Forester, Nos.
7, 9, 1902.
_Deforestation._—The deforestation of hill and mountain lands has, the
world over, led to similar results; causing not only the destruction
of pasture and agricultural lands, but also the conversion of streams,
flowing from springs and seepage all the year, into periodic torrents,
flooding the lowlands during rains by the rapid running-off of the
water from the bare and hard-baked mountain slopes, and then running
dry within a short time, so as not even to afford drinking water to
pasturing cattle in summer. Thus for half a century the unsolved
problem of the “correction of the waters of the Jura mountains” was
before the Swiss and French governments; and the great and costly
public work involving re-forestation, deflection of torrents and
filling-in of deep ravines and gullies, is not even yet nearly
completed. In Spain, which in the time of the Roman occupation was
largely a forest country with abundant rainfall, the same results are
seen, notably in the South, in the wide, and mostly dry, sandy beds
of streams once running deep and clear; and in the scarred hill-and
mountain-sides, and scant vegetation of low shrubs (“chaparral”) that
replace the once abundant tree growth, _e. g._, in Old and New Castile.
Unfortunately the lessons taught by the bitter experience of the old
world seem to require actual repetition in the new, before means of
prevention are even thought of.
Public-domain text, read in full here on John Shaqi.
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