The evolution of climateBrooks, C. E. P. (Charles Ernest Pelham)
Science
The evolution of climate
Brooks, C. E. P. (Charles Ernest Pelham)
Climatology; Paleoclimatology
The largest ruins of this type invariably lie near the main lines of
drainage. They consist of villages with houses of several storeys.
But digging down beneath these ruins we find (_c_) traces of an
older occupation, and ruins of a primitive type are also found on
the plateaus remote from any except small valleys. “They are usually
small, and are greatly ruined, and seem to belong to a time long
anterior to the main large ruins.” Huntington terms this type the
Hohokam; unfortunately this and the Pajaritan occupations cannot
be accurately dated, but it is reasonable to connect them with the
rainfall maxima shown by the trees, about the time of Christ, and in
A.D. 1000 to A.D. 1300.
A similar succession has been found in the neighbourhood of Mexico
City. The earliest trace of occupation is a crude “mountain pottery,”
in ordinary river sand and gravel. These deposits are succeeded by
finer sand with better pottery known as the “San Juan” type, above
which comes a culture layer with the remains of houses. This is
covered by a bed of “tepetate,” a white calcareous deposit frequently
found in dry regions where much water evaporates. The gravels suggest
the occasional heavy rains of arid countries. The San Juan pottery
extends throughout the “tepetate,” which probably corresponds to the
dry period of A.D. 400-1000 in California.
Historical records in Mexico date back to the coming of the Aztecs in
A.D. 1325. They show that in 1325 and again in 1446 the level of the
lake of Mexico was high, but towards the end of the fifteenth century
the water was much lower. In 1520 it was high again; in 1600 it was
low, but high from 1629 to 1634. From 1675 to 1755 was a long dry
period. On the whole the climate from 300 to 600 years ago seems to
have been moister than that of to-day.
Still further south in the Peninsula of Yucatan recent explorations
have yielded results of extreme interest. Yucatan lies within the
tropical rain-belt, and is covered by almost impenetrable forests.
The climate is enervating and unhealthy, and the present inhabitants
are greatly lacking in vigour. In the forest, however, have been
found the ruins of ninety-two towns, some of them of great size,
and all remarkable for the beauty as well as the solidity of their
architecture.
Public-domain text, read in full here on John Shaqi.
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