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Project Gutenberg #13089
The Making of Arguments
A guide to defining issues, gathering evidence, testing reasoning, adapting to an audience, organizing a case, and debating persuasively.
Project Gutenberg #13089
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Public domain in the United States
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Cover source
Local typographic cover created for The Missing Workbook from public-domain source metadata
Section 7 of 8
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Page 2 of 9
APPENDIX I
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the earth ,
Each in their kind !'
The earth obeyed ,
and ,
straight Opening her fertile womb ,
teemed at a birth .
Innumerous living creatures ,
perfect forms ,
Limbed and full-grown .
Out of the ground uprose ,
As from his lair ,
the wild beast ,
where he wons In forest wild ,
in thicket ,
brake ,
or den :
Among the trees in pairs they rose ,
they walked ;
The cattle in the fields and meadows green ;
Those rare and solitary ;
these in flocks Pasturing at once ,
and in broad herds upsprung .
The grassy clods now calved ;
now half appears The tawny lion ,
pawing to get free His hinder parts —
then springs ,
as broke from bonds ,
And rampant shakes his brinded mane ;
the ounce ,
The libbard ,
and the tiger ,
as the mole Rising ,
the crumbled earth above them threw In hillocks ;
the swift stag from underground Bore up his branching head ;
scarce from his mould Behemoth ,
biggest born of earth ,
upheaved His vastness ;
fleeced the flocks and bleating rose As plants ;
ambiguous between sea and land ,
The river-horse
and scaly crocodile .
At once came forth whatever creeps the ground ,
Insect or worm ."
There is no doubt as to the meaning of this statement ,
nor as to what a man of Milton's
genius expected would have been actually visible to an eyewitness of this mode of origination of living things .
The third hypothesis ,
or the hypothesis of evolution ,
supposes that ,
at any comparatively late period of past time ,
our imaginary spectator would meet with a state of things very similar to that which now obtains ;
but that the likeness of the past to the present would gradually become less and less ,
in proportion to the remoteness of his period of observation from the present day :
that the existing distribution of mountains and plains ,
of rivers and seas ,
would show itself to be the product of a slow process of natural change operating upon more and more widely different antecedent conditions of the mineral framework of the earth ;
until ,
at length ,
in place of that framework ,
he would behold only a vast nebulous mass ,
representing the constituents of the sun and of the planetary bodies .
Preceding the forms of life which now exist ,
our observer would see animals and plants not identical with them ,
but like them :
increasing their differences with their antiquity ,
and at the same time becoming simpler and simpler ;
until ,
finally ,
the world of life would present nothing but that undifferentiated protoplasmic matter which ,
so far as our present knowledge goes ,
is the common foundation of all vital activity .
The hypothesis of evolution supposes that in all this vast progression there would be no breach of continuity ,
no point at which we could say "
This is a natural process ,"
and "
This is not a natural process ";
but that the whole might be compared to that wonderful process of development which may be seen going on every day under our eyes ,
in virtue of which there arises ,
out of the semifluid ,
comparatively homogeneous substance which we call an egg ,
the complicated organization of one of the higher animals .
That ,
in a few words ,
is what is meant by the hypothesis of evolution .
I have already suggested that in dealing with these three hypotheses ,
in endeavoring to form a judgment as to which of them is the more worthy of belief ,
or whether none is worthy of belief —
in which case our condition of mind should be that suspension of judgment which is so difficult to all but trained intellects ,—
we should be indifferent to all a priori
considerations .
The question is a question of historical fact .
The universe has come into existence somehow or other ,
and the problem is ,
whether it came into existence in one fashion ,
or whether it came into existence in another ;
and ,
as an essential preliminary to further discussion ,
permit me to say two or three words as to the nature and the kinds of historical evidence .
The evidence as to the occurrence of any event in past time may be ranged under two heads ,
which ,
for convenience '
sake ,
I will speak of as testimonial evidence and as circumstantial evidence .
By testimonial evidence I mean human testimony ;
and by circumstantial evidence I mean evidence which is not human testimony .
Let me illustrate by a familiar example what I understand by these two kinds of evidence ,
and what is to be said respecting their value .
Suppose that a man tells you that he saw a person strike another and kill him ;
that is testimonial evidence of the fact of murder .
But it is possible to have circumstantial evidence of the fact of murder ;
that is to say ,
you may find a man dying with a wound upon his head having exactly the form and character of the wound which is made by an ax ,
and ,
with due care in taking surrounding circumstances into account ,
you may conclude with the utmost certainty that the man has been murdered ;
that his death is the consequence of a blow inflicted by another man with that implement .
We are very much in the habit of considering circumstantial evidence as of less value than testimonial evidence ,
and it may be that ,
where the circumstances are not perfectly clear and intelligible ,
it is a dangerous and unsafe kind of evidence ;
but it must not be forgotten that ,
in many cases ,
circumstantial evidence is quite as conclusive as testimonial evidence ,
and that ,
not unfrequently ,
it is a great deal weightier than testimonial evidence .
For example ,
take the case to which I referred just now .
The circumstantial evidence may be better and more convincing than the testimonial evidence ;
for it may be impossible ,
under the conditions that I have defined ,
to suppose that the man met his death from any cause but the violent blow of an ax wielded by another man .
The circumstantial evidence in favor of a murder having been committed ,
in that case ,
is as complete and as convincing as evidence can be .
It is evidence which is open to no doubt and to no falsification .
But the testimony of a witness is open to multitudinous doubts .
He may have been mistaken .
He may have been actuated by malice .
It has constantly happened that even an accurate man has declared that a thing has happened in this ,
that ,
or the other way ,
when a careful analysis of the circumstantial evidence has shown that it did not happen in that way ,
but in some other way .
We may now consider the evidence in favor of or against the three hypotheses .
Let me first direct your attention to what is to be said about the hypothesis of the eternity of the state of things in which we now live .
What will first strike you is ,
that it is a hypothesis which ,
whether true or false ,
is not capable of verification by any evidence .
For ,
in order to obtain either circumstantial or testimonial evidence sufficient to prove the eternity of duration of the present state of nature ,
you must have an eternity of witnesses or an infinity of circumstances ,
and neither of these is attainable .
It is utterly impossible that such evidence should be carried beyond a certain point of time ;
and all that could be said ,
at most ,
would be ,
that so far as the evidence could be traced ,
there was nothing to contradict the hypothesis .
But when you look ,
not to the testimonial evidence —
which ,
considering the relative insignificance of the antiquity of human records ,
might not be good for much in this case —
but to the circumstantial evidence ,
then you will find that this hypothesis is absolutely incompatible with such evidence as we have ;
which is of so plain and so simple a character that it is impossible in any way to escape from the conclusions which it forces upon us .
You are ,
doubtless ,
all aware that the outer substance of the earth ,
which alone is accessible to direct observation ,
is not of a homogeneous character ,
but that it is made up of a number of layers or strata ,
the titles of the principal groups of which are placed upon the accompanying diagram .68
Each of these groups represents a number of beds of sand ,
of stone ,
of clay ,
of slate ,
and of various other materials .
On careful examination ,
it is found that the materials of which each of these layers of more or less hard rock are composed are ,
for the most part ,
of the same nature as those which are at present being formed under known conditions on the surface of the earth .
For example ,
the chalk ,
which constitutes a great part of the Cretaceous
formation in some parts of the world ,
is practically identical in its physical and chemical characters with a substance which is now being formed at the bottom of the Atlantic Ocean ,
and covers an enormous area ;
other beds of rock are comparable with the sands which art ;
being formed upon seashores ,
packed together ,
and so on .
Thus ,
omitting rocks of igneous origin ,
it is demonstrable that all these beds of stone ,
of which a total of not less than seventy thousand feet is known ,
have been formed by natural agencies ,
either out of the waste and washing of the dry land ,
or else by the accumulation of the exuviae of plants and animals .
Many of these strata are full of such exuviae —
the so-called "
fossils ."
Remains of thousands of species of animals and plants ,
as perfectly recognizable as those of existing forms of life which you meet with in museums ,
or as the shells which you pick up upon the seabeach ,
have been embedded in the ancient sands ,
or muds ,
or limestones ,
just as they are being embedded now ,
in sandy ,
or clayey ,
or calcareous subaqueous deposits .
They furnish us with a record ,
the general nature of which cannot be misinterpreted ,
of the kinds of things that have lived upon thy surface of the earth during the time that is registered by this great thickness of stratified rocks .
But even a superficial study of these fossils shows us that the animals and plants which live at the present time have had only a temporary duration ;
for the remains of such modern forms of life are met with ,
for the most part ,
only in the uppermost or latest tertiaries ,
and their number rapidly diminishes in the lower deposits of that epoch .
In the older tertiaries ,
the places of existing animals and plants are taken by other forms ,
as numerous and diversified as those which live now in the same localities ,
but more or less different from them ;
in the Mesozoic
rocks ,
these are replaced by others yet more divergent from modern types ;
and in the Paleozoic formations the contrast is still more marked .
Thus the circumstantial evidence absolutely negatives the conception of the eternity of the present condition of things .
We can say with certainly that the present condition of things has existed for a comparatively short period ;
and that ,
so far as animal and vegetable nature are concerned ,
it has been preceded by a different condition .
We can pursue this evidence until we reach the lowest of the stratified rocks ,
in which we lose the indications of life altogether .
The hypothesis of the eternity of the present state of nature may therefore be put out of court .
We now come to what I will term Milton's
hypothesis —
the hypothesis that the present condition of things has endured for a comparatively short time ;
and ,
at the commencement of that time ,
came into existence within the course of six days .
I doubt not that it may have excited some surprise in your minds that I should have spoken of this as Milton's
hypothesis ,
rather than that I should have chosen the terms which are more customary ,
such as "
the doctrine of creation ,"
or the "
Biblical doctrine ,"
or "
the doctrine of Moses,"
all of which denominations ,
as applied to the hypothesis to which I have just referred ,
are certainly much more familiar to you than the title of the
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