III

Of the _three_ general postulates or _a priori_ assumptions of this

curiously out-of-date mediæval science, namely, (1) Uniformity, (2) the

Cooling globe theory, and (3) the theory of the Successive Ages, the

first two have already been examined and found wanting by other

investigators, and have been allowed to lapse into a sort of honored

disuse, though their memory is still reverently cherished in all the

text-books of the science. The "Challenger" Expedition dissipated most

of the myths that had long been taught regarding the deep waters of the

ocean; and Professor Suess has disposed of the closely related myth

about the coasts of the continents being constantly on the seesaw up and

down. These two discoveries, with others that might be mentioned,

dispose of Lyell's theory of uniformity. Lord Kelvin and the other

physicists dissipated the idea of a molten interior of the earth. Hence,

because these other false hypotheses have already in a measure been

disposed of, as well as for the sake of brevity, I shall here discuss

only the _third_ of the prime postulates of the current system of

geology, namely the theory of Successive Ages. And when we have adjusted

this aspect of the science of geology to the facts of the rocks as made

known to us by modern discoveries, we shall find little in this science

out of harmony with the older view of a literal Creation as taught in

the Bible and as already confirmed by the other branches of science

which we have been examining.

There are _five_ leading arguments against the reality of these

successive ages. Four of them must be dismissed here by a brief summary

of the facts as we know them to-day, referring the reader to the

author's larger work, where detailed evidence is given for each. The

_fifth_ series of facts I shall give here in more detail, though of

course even this must be but an outline of what is given elsewhere.

1. In the earlier days of the theory of successive ages it was taught

that only certain kinds of fossils were to be found _at the bottom_ of

the series, or next to the Primitive or Archæan. This feature of the

theory was demanded by the supposed universal spread of one type of life

all around the globe in the earliest age. But it is now known that the

so-called "oldest" fossiliferous rocks occur only in detached patches

over the globe, while other or "younger" kinds are just as likely to be

found on the Primitive or next to the Archæan. Not only may any kind of

fossiliferous rocks occur next to the Archæan, but even the "youngest"

may be so metamorphosed and crystalline as to resemble exactly in this

respect the so-called "oldest" rocks. On the other hand some of the very

"oldest" rocks may, like the Cambrian strata around the Baltic and in

some parts of the United States, consist of "muds scarcely indurated and

sands still incoherent."[40]

[Footnote 40: J.A. Howe; Encyclopædia Britannica, Vol. II, p. 86.

Cambridge Edition.]

All this means that many facts regarding the _position_ of the strata as

well as regarding their _consolidation_ contradict the theory of

successive ages.

2. Many of the rivers of the world completely ignore the alleged varying

ages of the rocks in the different parts of their course, and treat them

all as if of the same age or as if they began sawing at them all at the

same time. This is true of the Rhine, the Meuse, and the Danube in

Europe, the Sutlej of India, and the upper part of the Colorado in

America, not to mention others. The old strand lines around all the

continents act in the very same way, ignoring the varying ages of the

rocks they happen to meet; as is also true of nearly all the great

faults or fissures which are of more than local extent. The ore veins of

the various minerals are about as likely to be found in Tertiary or

Mesozoic as in the Palæozoic. A very similar lesson is to be learned

from the fossils found lying exposed on the deep ocean bottom; for they

are about as likely to be Palæozoic or Mesozoic as Tertiary.

From these facts we conclude that practically all the great natural

chronometers of the earth seem to treat the fossiliferous rocks as if

they are _all of about the same age_, completely disregarding the

distinctions in age founded on the fossils.

3. According to the present chronological arrangement of the rocks, very

many genera, often whole tribes of animals, are found as fossils only in

the oldest rocks, and _have skipped all the others_, though found in

comparative abundance in our modern world. Very many others have skipped

from the Mesozoic down, while still others skip large _parts_ of the

series of successive ages.

These absurdities would all be avoided by acknowledging that the current

distinctions as to the ages of the fossils are purely artificial, and

that one fossil is intrinsically just as old or as young as another.

4. It is now known that any kind of "young" beds whatsoever, Mesozoic,

Tertiary, or even Pleistocene, may be found in such _perfect

conformability_ on some of the very oldest beds over wide stretches of

country that "the vast interval of time intervening is unrepresented

either by deposition or erosion"; while in some instances these

age-separated formations so closely resemble one another in structure

and in mineralogical make-up that, "were it not for fossil evidence, one

would naturally suppose that a single formation was being dealt with"

(McConnell); and these conditions are "not merely local, but persistent

over wide areas" (A. Geikie), so that the "numerous examples" (Suess) of

these conditions "may well be cause for astonishment" (Suess).

A still more astonishing thing from the standpoint of the current

theories is that these conformable relations of incongruous strata are

often _repeated over and over again in the same vertical section_, the

same kind of bed reappearing alternately with others of an entirely

different "age," that is, appearing "as if _regularly interbedded"_ (A.

Geikie) with them, in a manifestly undisturbed series of strata.

Here again we have a very formidable series of facts whose gravamen is

directed wholly against the artificial distinctions in age between the

different groups of fossils; and their argument is an eloquent plea that

the fossils are neither older nor younger but all of a similar age.

5. Our last fact demands a somewhat more extended consideration; but it

may be stated in advance briefly as follows:

In very numerous cases and over hundreds and even thousands of square

miles, the conformable conditions specified in the previous fact are

exactly reproduced _upside down_; that is, very "old" rocks occur with

just as much appearance of natural conformability on top of very "young"

rocks, the area in some instances covering many hundreds of square

miles, and in one particular instance in Montana and Alberta covering

about five or six thousand square miles of area.

The first notable example of this phenomenon was discovered at Glarus,

Switzerland, a good many years ago; since which time this locality has

become a classic in geological literature, and has called out many

ponderous monographs in German and French by such men as Heim, Schardt,

Lugeon, Rothpletz, and Bertrand. This example, which was first (1870)

called the Glarner Double Fold by Escher and Heim, is now universally

called a nearly flat-lying "thrust fault," in accordance with the

explanations since adopted of similar phenomena elsewhere. Without

obtruding unnecessary technicalities upon my non-professional readers, I

may quote the words of Albert Heim as to the conditions as now

recognized in these parts:

"These flat-lying faults, of which those at Glarus were the first to be

discovered, _are a universal_ _phenomenon_ in the Northern and Central

Alps."[41]

[Footnote 41: "Der Bau der Schweizeralpen," p. 17.]

The favorite method of explaining these conditions has slightly changed

within recent years, as already remarked. For whereas the classic

example at Glarus was at first spoken of as a double fold-in from both

sides toward the Sernf Valley, this is now universally spoken of as a

"thrust fault," with the rocks all pushed one way. Incidentally it may

be noted that this very fact that what was long regarded as two

completely overturned folds is now spoken of as one flat-lying thrust

fault, is _prima facie_ evidence that there is here _no physical proof_

of any real overturning of the strata, such as we do find on a very

small scale in true folded rocks. The latter can usually be measured in

yards, feet, or inches; while in this example at Glarus the area

involved would be measured in many miles, and in some very similar

examples to be presently mentioned from America the measurement could

best be made in degrees of latitude and longitude or in arcs of the

earth's circumference. In these larger examples it is manifestly

impossible that there should be any physical evidence sufficient to

indicate a huge earth movement of this character, especially when, as is

usually the case, both the upper and the lower strata are _quite

uninjured in appearance_. No; the fossils are here in the wrong order,

that is all. And so, to save the long established doctrines of a very

definite order of successive life-forms, this theory of a "thrust fault"

is offered as the best available explanation. As Dr. Albert Heim himself

once expressed it very naively in a letter to the present writer, that

the strata over these large areas are in a position manifestly at direct

disagreement with the received order of the fossils, "is a fact which

can be clearly seen,--only we know not yet how to explain it in a

mechanical way."

An example in the Highlands of Scotland was about the next to be

discovered. Here, as Dana says, "a mass of the oldest crystalline rocks,

many miles in length from north to south, was thrust at least ten miles

westward over younger rocks, part of the latter fossiliferous;" and he

further declares, "the thrust planes _look like planes of bedding, and

were long so considered._"[42]

Sir Archibald Geikie and others had at first described these beds as

naturally conformable; and when at length they were convinced that the

fossils would not permit this explanation, Geikie gives us some very

picturesque details as to how natural they look.

The thrust planes, he says, are with much difficulty distinguished "from

ordinary stratification planes, like which they have been plicated,

faulted, and denuded. Here and there, as a result of denudation, a

portion of one of them appears capping a hilltop. One almost refuses to

believe that the little outlier on the summit does not lie normally on

the rocks below it, but on a nearly horizontal fault by which it has

been moved into its place."

Of a similar example in Ross Shire he declares:

"Had these sections been planned for the purpose of deception, they

could not have been more skilfully devised, ... and no one coming first

to the ground would suspect that what appears to be a normal

stratigraphical sequence is not really so."[43]

[Footnote 42: "Manual," pp. 111, 534.]

[Footnote 43: _Nature_, November 13, 1884, pp. 29-35.]

Here again we have unequivocal testimony from the most competent of

observers that there is _no physical evidence whatever_ to lead any one

to say that a ponderous scale of the earth's crust was really pushed up

on top of other portions, as this makeshift theory of "thrust faults"

involves. The _fossils are here in the wrong order_, just as in the case

at Glarus; that is all. The facts seem to be a flat contradiction to the

theory of definite successive ages, and to save the theory this

explanation of a "thrust fault" is invented, though there is absolutely

no physical evidence of any disturbance of the strata.

Our next stopping place is in the Southern Appalachian Mountains of

eastern Tennessee and northern Georgia. Here we have the Carboniferous

strata dipping gently to the southeast, like an ordinary low monocline,

_under_ Cambrian or Lower Silurian, one of these so-called faults having

a reported length of 375 miles,[44] while in another instance the upper

strata are said to have been pushed about eleven miles in the direction

of the "thrust."[45] These conditions, we are told, "have provoked the

wonder of the most experienced geologists,"[46] because of the perfectly

natural appearance of the surfaces of the strata affected; or as this

same writer puts it, "The mechanical effort is great beyond

comprehension, but the effect upon the rocks is inappreciable," and "the

fault dip is often parallel to the bedding of the one or the other

series of strata."[47] Which means, in other words, that these "thrust

planes" _look just like ordinary planes of bedding between conformable

strata_.

[Footnote 44: Bailey Willis, Geol. Survey, Report, Vol. 13, p. 228.]

[Footnote 45: C.W. Hayes, _Bull. Geol. Soc_., Vol. 2, pp. 141-154.]

[Footnote 46: Willis, _op. cit_., p. 228.]

[Footnote 47: Willis, _op. cit_., p. 227.]

The Rocky Mountains furnish examples of many kinds of natural phenomena

on the very largest scale, and those of the sort here under

consideration are no exception to this rule. For here we have an immense

area east of the main divide, extending from the middle of Montana up to

the Yellowhead Pass in Alberta, or over 350 miles long, where the tops

of the mountains consist of jointed limestones or argillites of

Algonkian or pre-Cambrian "age," resting on soft Cretaceous shales.

Often the greater part of the mass of a range will consist of these

"older" and harder rocks, which by the erosion of the soft underlying

shales are left standing in picturesque, rectangular, cathedral-like

masses, easily recognizable as far off as they can be seen. And the

almost entire absence of trees or other vegetation helps one to trace

out the relationship of these formations over immense areas with little

or no difficulty.

In the latitude of the Bow River, near the Canadian Pacific main line,

there is a long narrow valley of these Cretaceous beds some sixty-five

miles long, called the Cascade Trough, with of course pre-Cambrian

mountains on each side. Somewhat further south there are two of these

Cretaceous valleys parallel to one another, and in some places _three_;

while just south of the fiftieth parallel of latitude, at Gould's Dome,

there are actually _five parallel ranges_ of these Palæozoic mountains,

_with four Cretaceous valleys in between_, one of these valleys, the

Crow's Nest Trough, being ninety-five miles long.

But we ought to take a nearer view of these wonderful conditions. A

convenient point of approach will be just east of Banff, Alberta, near

Kananaskis Station, where the Fairholme Mountain has been described by

R.G. McConnell of the Canadian Survey. The latter remarks with amazement

on the perfectly natural appearance of these Algonkian limestones

resting in seeming conformability on Cretaceous shales, and says that

the line of separation between them, called in the theory the "thrust

plane," resembles in all respects an ordinary stratification plane. I

quote his language:

"The angle of inclination of its plane to the horizon is _very low_, and

in consequence of this its outcrop follows a very sinuous line along the

base of the mountains, and _acts exactly like the line of contact of two

nearly horizontal formations_.

"The best places for examining this fault are at the gaps of the Bow and

of the south fork of Ghost River.... The fault plane here is nearly

horizontal, and the two formations, viewed from the valley, _appear to

succeed one another conformably."[48]

[Footnote 48: Annual Report, 1886, Part D, pp. 33, 34.]

This author adds the further interesting detail that the underlying

Cretaceous shales are "very soft," and "have suffered very little by the

sliding of the limestone over them."[49]

About a hundred miles further south, but still in Alberta, we have the

well-known Crow's Nest Mountain, a lone peak, which consists of these

same Algonkian limestones resting on a Cretaceous valley "in a nearly

horizontal attitude," as G.M. Dawson says, which "in its structure and

general appearance much resembles Chief Mountain,"[50] another detached

peak some fifty miles further south, just across the boundary line in

Montana.

Chief Mountain has been well described by Bailey Willis,[51] who

estimates that the Cretaceous beds underneath this mountain must be

3,500 feet thick; while the so-called "thrust plane is essentially

_parallel to the bedding_" of the upper series.[52]

"This apparently is true not only of the segments of thrust surface

beneath eastern Flattop, Yellow, and Chief Mountain, but also of the

more deeply buried portions which appear to dip with the Algonkian

strata into the syncline. While observation is not complete, it may be

assumed on a basis of fact that thrust surfaces and bedding are nearly

parallel over extensive areas."[53]

[Footnote 49: Report, 1886, Part D, p. 84.]

[Footnote 50: Report, 1885, Part B, p. 67.]

[Footnote 51: _Bull. Geol. Soc._, Vol. 13, pp. 305-352.]

[Footnote 52: _Id_., p. 336.]

[Footnote 53: _Id_., p. 336.]

Quite recently this region has been studied by Marius R. Campbell of the

Washington Survey Staff (Bulletin 600), while the part in Alberta has

been studied by Rollin T. Chamberlin of Chicago. Much of the vast area

involved is not yet well explored; but over it all, so far as it has

been fully examined, the same lithological and stratigraphical

structures reappear with the persistence of a repeating decimal. And

were it not for the exigencies of the theory of Successive Ages, this

whole region of some five or six thousand square miles would be

considered as only an ordinary example, on a rather large scale, of

undisturbed horizontal stratification cut up by erosion into mountains

of denudation, with of course occasional instances of minor local

disturbances here and there, as would be expected over an area of this

extent.

Richards and Mansfield in a recent paper describe the "Bannock

Overthrust," some 270 miles long, in Utah, Idaho, and Wyoming. The

Carnegie Research recently reported a similar phenomenon about 500 miles

long in northern China.

But it would be tiresome to follow these conditions around the world. We

have plenty of examples, and we have them described by the foremost of

living geologists. What we need to do now is to adopt a true scientific

attitude of mind, a mind freed from the hypnotizing influence of the

current theories, in order correctly to interpret the facts as we

already have them.

_How much of the earth's crust would we have to find_ in this upside

down order of the fossils, before we would be convinced that there must

be something hopelessly wrong with this theory of Successive Ages which

drives otherwise competent observers to throw away their common sense

and cling desperately to a fantastic theory in the very teeth of such

facts?

The science of geology as commonly taught is truly in a most astonishing

condition, and doubtless presents the most peculiar mixture of fact and

nonsense to be found in the whole range of our modern knowledge. In any

minute study of a particular set of rocks in a definite locality,

geology always follows facts and common sense; while in any general view

of the world as a whole, or in any correlation of the rocks of one

region with those of another region, it follows its absurd, unscientific

theories. But wherever it agrees with facts and common sense, it

contradicts these absurd theories; and wherever it agrees with these

theories, it contradicts facts and common sense. That most educated

people still believe its main thesis of _a definite age for each

particular kind of fossil_ is a sad but instructive example of the

effects of mental inertia.

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