The Chautauquan, Vol. 05, March 1885Chautauqua Literary and Scientific Circle
Science
The Chautauquan, Vol. 05, March 1885
Chautauqua Literary and Scientific Circle
Chautauqua Institution -- Periodicals; Chautauqua Literary and Scientific Circle -- Periodicals
Mexico is a country reaching from the Gulf on its eastern coast to the
Pacific Ocean, almost 2,000 miles, with a breadth varying from 140 to
750 miles. The whole territory of Montezuma, at the time of the Spanish
conquest, was not less than 1,600,000 square miles, more than one half
of which has been obtained by the United States by purchase, enforced
treaties, or otherwise. The plains on the coast are low, marshy, and in
the summer and autumn malarial diseases are very prevalent. Strangers
can visit the place with safety only about four months in the year, when
severe northern gales cool the heated atmosphere and dissipate the seeds
of disease.
There are 6,000 miles of coast line, but, considering its extent, it does
not furnish many good harbors.
The main body of the land is an elevated plateau, traversed by chains
of mountains, some of which are of extraordinary height. The eastern
Cordillera, or chain, that runs nearly north from the initial point has
an elevation of 6,000 feet, the western nearly 10,000. Traversing the
longitudinal range, there are several cross ranges containing some of
the highest volcanoes on the continent. They are all quiescent now, and
none of them have been active during the present century. There are not
many lakes, and none that are very large. The basins of some, though of
sufficient extent, are so arid, and evaporation is carried on so rapidly
that the water in them has, at times, quite disappeared. Neither are the
rivers of much importance as thoroughfares. The Rio Grande, forming the
boundary between Mexico and Texas, is the longest (1,500 miles), but
navigable only for a short distance. Those in the mountain region are
impetuous torrents, larger near their source than afterward, as they lose
more by absorption, in passing through arid portions of the table-lands,
than they gain by drainage, except in the rainy season. After plowing
deep furrows, and cutting out immense ravines among the foot hills of the
mountains, some are partly exhausted, drawn into reservoirs and canals
constructed for purposes of irrigation, and spread out into sluggish
bayous, of no great depth, before they reach the sea. The lack of
navigable streams has been seriously felt.
Public-domain text, read in full here on John Shaqi.
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