The lower range of plateaus, it will be seen, is far more frequently met
with through all parts of the earth than the higher, yet both combined
occupy a larger share of the surface of the globe. We can designate them
as sharply defined and broadly massive elevations, in contradistinction
to the long, narrow, and broken masses which have received the name of
mountain chains. The latter have too often been confounded with the
former and have received from geographers a treatment disproportionately
full in relation to their claims. The plateau has been until recently
an almost forgotten geographical element. Humboldt restored it to its
rightful place; by many hundreds of measurements he has accurately
settled its form, its effect on climate, on isothermal lines, on
agriculture, on the physical and moral life of nations, and even on the
course of human history.
In closing this attempt at a general consideration of plateaus, I must
confirm the reproach which Humboldt has cast upon most geographers of
this day for their abuse of the word plateau. And I must at the same
time admit that it is justly due to some parts of my own “Erdkunde,”
where I have considered the plateau systems of Central Asia and Africa.
When I wrote the pages of that work, thirty and more years ago, there
were no scientific measurements then made of those regions, and the
general ignorance led to a premature generalization, in which I used the
ascertained features of the New World as probably in analogy with the
unexplored center of the Old World. This use of really untrue analogies
was carried by others to great lengths, and choratographers went so far
as to depict the country according to the hypothesis of those who had
written at first hand, and after using all the lights then existing, but
who had never supposed that what they had indicated in general terms,
would be afterward made so definite and real to the public eye. Those
untrue statements of my own, I must leave however just as they are,
and rejoice that the great advance of science has led to the accurate
knowledge of the great plateaus of which the civilized world then knew
but little. One word more: I set the lower limit of plateaus of the
second grade at 500 feet, lower therefore than the great master in
Physical Geography set his.
Public-domain text, read in full here on John Shaqi.
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