Mexico -- Commerce; Mexico -- Economic conditions; Mexico -- Politics and government -- 1910-1946
Such _barrancas_ and valleys do not, of themselves, indicate either
great natural water power or navigable streams. There are wonderful
water power possibilities in Mexico, to be sure, which come from two
factors, the sheer drops which give ideal power sites with tremendous
heads of water, and the heavy torrential rainy season. But the streams
themselves do not carry sufficient water the year round to justify any
plant, and tremendous reservoir development is vital to any power plant
design. Such reservoirs have been built in various parts of Mexico,
but at appalling expense, such as only great financial interests can
swing--only foreign capital or the government has been able to handle
them. There is an added and unexpected element of difficulty--the
porousness of much of the soil of Mexico. The mountains, indeed, are of
igneous rocks, but underneath the valleys is often soft limestone, and
more often still, under those places where a great impounding of water
might be made with a relatively low and inexpensive dam, is the soft,
porous alluvial and volcanic-ash land with which the valleys have been
filled up.
This porous soil and limestone are factors bearing on the absence of
navigable streams. Even in the lowlands the streams run underground in
Mexico, and while they can be tapped by shallow wells, they deprive
Mexico almost entirely of the advantages of river transportation. Even
the Rio Grande, on the northern border, is useless for navigation most
of the year. The Panuco, at whose mouth is located the great oil center
of Tampico, is navigable only a short distance above that port. The
broad, rich coastal plain along the Gulf of Mexico is watered by tiny
streams, all of which, excepting the partially navigable Papaloapam,
are useless for steamers and even for launches most of the year. Not
until we reach the Isthmus of Tehuantepec do we find a river worth
considering for transportation. The Coatzacoalcos, at whose mouth
on the Gulf of Mexico is Puerto Mexico (the eastern terminus of the
Tehuantepec National Railway), furnishes a highway which made possible
the relatively great development of American tropical plantations
during the years of peace under Diaz. Its mouth was then the port of
loading for great ships, but only by continual dredging was it kept
open, and to-day the port is abandoned except for light-draft coasting
ships. Further south, emptying into the Gulf at Frontera, is the
magnificent system of which the Grijalva and the Usumacinta are the
chief streams. Here indeed have plied and in the future will ply great
river steamers, for upon the banks of the Usumacinta, at least, are
rich oil fields and the fairest farming land in all tropical Mexico.
Both the Grijalva and the Usumacinta are magnificent streams, and
the latter is comparable, in its majestic volume, to the Mississippi
itself. Only the bar at Frontera keeps them from being navigable to
ocean steamers. For a brief period under President Madero this bar
Public-domain text, read in full here on John Shaqi.
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