Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader — John Shaqi
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
=Observational geology _versus_ speculative philosophy.=—There appears
to be a more or less prevalent notion that the views which are held
by scientists in one generation are abandoned by those of the next;
and this is apt to lead to the belief that little is really known and
that much is largely guessed. Some ground there undoubtedly is for
such skepticism, though much of it may be accounted for by a general
failure among scientists, as well as others, to clearly differentiate
that which is essentially speculative from what is based broadly upon
observed facts. Even with extended observation, the possibility of
explaining the facts in more than one way is not excluded; but the
line is nevertheless a broad one which separates this entire field
of observation from what is essentially speculative philosophy. To
illustrate: the mechanics of the action which goes on within volcanic
craters is now fairly well understood as a result of many and extended
observations, and it is little likely that future generations of
geologists will discredit the main conclusions which have been reached.
The cause of the rise of the lava to the earth’s surface is, on the
other hand, much less clearly demonstrated, and the views which are
held express rather the differing opinions than any clear deductions
from observation. Again, and similarly, the physical history of the
great continental glaciers of the so-called “ice age” is far more
thoroughly known than that of any existing glacier of the same type;
but the cause of the climatic changes which brought on the glaciation
is still largely a matter for speculation.
In the present work, the attempt will be, so far as possible, to give
an exposition of geologic processes and the earth features which result
from them, with hints only at those ultimate causes which lie hidden in
the background.
=The scientific attitude and temper.=—The student of science should
make it his aim, not only clearly to separate in his studies the
proximate from the ultimate causes of observed phenomena, but he should
keep his mind always open for reaching individual conclusions. No
doctrines should be accepted finally upon faith merely, but subject
rather to his own reasoning processes. This should not be interpreted
to mean that concerning matters of which he knows little or nothing
he should not pay respect to the recognized authorities; but his
acceptance of any theory should be subject to review so soon as his
own horizon has been sufficiently enlarged. False theories could hardly
have endured so long in the past, had not too great respect been given
to authorities, and individual reasoning processes been held too long
in subjection.
Public-domain text, read in full here on John Shaqi.
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