Brazil -- Description and travel; Geology -- Amazon River Valley
_April 9th._—Yesterday Mr. Agassiz lectured upon the traces of glaciers
as they exist in the northern hemisphere, and the signs of the same kind
to be sought for in Brazil. After a sketch of what has been done in
glacial investigation in Europe and the United States, showing the great
extension of ice over these regions in ancient times, he continued as
follows: “When the polar half of both hemispheres was covered by such an
ice shroud, the climate of the whole earth must have been different from
what it is now. The limits of the ancient glaciers give us some estimate
of this difference, though of course only an approximate one. A degree
of temperature in the annual average of any given locality corresponds
to a degree of latitude; that is, a degree of temperature is lost for
every degree of latitude as we travel northward, or gained for every
degree of latitude as we travel southward. In our times, the line at
which the average annual temperature is 32°, that is, at which glaciers
may be formed, is in latitude 60° or thereabouts, the latitude of
Greenland; while the height at which they may originate in latitude 45°
is about 6,000 feet. If it appear that the ancient southern limit of
glaciers is in latitude 36°, we must admit that in those days the
present climate of Greenland extended to that line. Such a change of
climate with reference to latitude must have been attended by a
corresponding change of climate with reference to altitude. Three
degrees of temperature correspond to about one thousand feet of
altitude. If, therefore, it is found that the ancient limit of glacier
action descends on the Andes, for instance, to 7,000 feet above the
level of the sea under the equator, the present line of perpetual snow
being at 15,000, it is safe to infer that in those days the climate was
some 24° or thereabouts below its present temperature. That is, the
temperature of the present snow line then prevailed at a height of 7,000
feet above the sea level, as the present average temperature of
Greenland then prevailed in latitude 36°. I am as confident that we
shall find these indications at about the limit I have pointed out as if
I had already seen them. I would even venture to prophesy that the first
moraines in the valley of the Marañon should be found where it bends
eastward above Jaen.”[9]
Public-domain text, read in full here on John Shaqi.
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