Mexico, Aztec, Spanish and Republican, Vol. 2 of 2: A Historical, Geographical, Political, Statistical and Social Account of that Country from the Period of the Invasion by the Spaniards to the Present Time.Mayer, Brantz
History
Mexico, Aztec, Spanish and Republican, Vol. 2 of 2: A Historical, Geographical, Political, Statistical and Social Account of that Country from the Period of the Invasion by the Spaniards to the Present Time.
AGRICULTURE--DRY AND RAINY SEASONS.--IRRIGATION--YIELD OF CORN
LANDS.--COLONIAL RESTRICTIONS.--COLONIAL DEPENDENCE--BAD
INTERCOMMUNICATION--ARRIEROS.--CORN LANDS--DIFFERENT KINDS OF CORN
IN MEXICO--MODE OF CULTIVATION--PRODUCTION--VARIOUS USES OF
CORN.--BANANA--MAINOC--RICE.--THE OLIVE--VINE--CHILE
PEPPER--TOMATO--FRIJOL--MAGUEY.--MAGUEY ESTATES.--MAKING
PULQUE.--ALOES--CACTI.
Sun, seasons, temperature, soils and moisture are the chief elements of
agricultural success or failure, according as they are beneficially
harmonized or unfortunately disunited. In our geological and
geographical descriptions we have already indicated the rapid changes of
temperature in Mexico experienced by rising gradually from the sea shore
to the summit of the table land, and passing through the _tierras
calientes_, _templadas_ and _frias_. This is the origin of the variety
of Mexican productions and the reason why the pine and the palm are
encountered upon the same parallel of latitude; but the _fertility_ of
Mexico is very much governed by the moisture with which it is annually
favored, and for which it is obliged to rely chiefly on the clouds. The
Mexicans are not accustomed to separate the year as we do into the four
seasons of spring, summer, autumn and winter, for the variation of
temperature scarcely authorizes such marked distinctions of climate; yet
they divide the twelve months into two grand divisions of _El Estio_--or
the dry season, and _La Estacion de las aguas_, or the rainy season. The
latter commences about May and lasts usually four months, whilst the dry
season comprises the remainder of the year.
The curving shores of Mexico along the gulf and interior highlands
gather and hem in an immense body of vapor, which is carried on by the
trade winds and condensed against the cold and lofty inland mountain
peaks which rise above the limit of perpetual congealation. This occurs
during the dry season whilst the sun is at the south. But when the power
of that luminary increases as it advances northward, and until it has
long turned back again on its southern course, these vapors are
dissolved by the hot intertropical air and descend, almost daily, in
fertilizing showers. The
[Illustration: GROUP OF PLANTS.]
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