CHAPTER IV

FACT NUMBER TWO

If we had ample evidence that a certain man was personally acquainted

with Julius Caesar, that they were born in the same town, went to school

together, served in the same wars, and later carried on an extensive

mutual correspondence, would we not conclude that they must have lived

in the same age of the world's history? I confess that the conclusion

seems quite unavoidable. Who would dream that eighteen centuries or more

had separated the two lives, and that while one was an old Roman the

other was an American of the latter nineteenth century?

Some such a puzzle as this is presented in geology under the general

subject of =conformability=. Let me define this term.

Strata laid down by water are in the first place in a horizontal

position. Some subsequent force may have disturbed them, so that we may

now find them standing up on edge like books in a library. But all human

experience goes to show that they were not deposited in this position.

Some disturbing cause must have taken hold of them since they were laid

down, for the water in which they were made must have spread them out

smooth and horizontal, each subsequent layer or stratum fitting "like a

glove" on the preceding. Thus when we find two successive layers

agreeing with one another in their planes of bedding, with every

indication that the lower one was not disturbed in any way before the

upper one was spread out upon it, the two are said to be =conformable=.

But if the lower bed has evidently been upturned or disturbed before the

other was laid down, or if its surface has even been partly eroded or

washed away by the water, the strata are said to be =unconformable=, or

they show =unconformability= in bedding.

Of course, in all this we are dealing only with =relative= time. When we

find one bed or stratum lying above another in their natural position,

the lower one is of course the older of the two; but whether laid down

ten minutes earlier, or ten million years earlier, how are we to

determine? Ignoring the matter of the fossils they contain, must we not

own that, though there is no way of telling just how much longer the

lower one was deposited before the next succeeding, yet if the two are

conformable to one another, and the bottom one shows no evidence of

disturbance or erosion before the other was fitted upon it, the strong

presumption would seem to be that no great length of time could have

elapsed between the laying down of the two layers. To say that we have

here a geological example similar to that of a modern American having

been personally acquainted with Julius Caesar, would seem to be quite

"inexplicable," as Herbert Spencer used to say.

But if the life succession theory be true, we have just such a conundrum

in our Fact Number Two, which is that =any formation whatever may rest

conformably upon any other "older" formation=.

The lower may be Devonian, Silurian, or Cambrian, and the upper one

Cretaceous or Tertiary, and thus according to the theory millions on

millions of years must have elapsed after the first, and before the

following bed was laid down, but the conformability is perfect, and the

beds have all the appearance of having followed in quick succession.

Sometimes, too, though less frequently, these age-separated formations

are lithologically the same, and can only be separated by their fossils!

But before going into the minute description of any of these cases, we

must notice some general statements. Thus as long ago as the date of the

publication of "The Origin of Species," Darwin, in speaking of the

"Imperfection of the Geological Record," could speak of "The many cases

on record of a formation conformably covered, after an immense interval

of time, by another and later formation, without the underlying bed

having suffered in the interval by any wear and tear."[20]

Also Geikie,[21] in speaking of how "fossil evidence may be made to

prove the existence of gaps which are not otherwise apparent," says that

"It is not so easy to give a satisfactory account of those which occur

where the strata are strictly conformable, and where no evidence can be

observed of any considerable change of physical conditions at the time

of deposit. A group of quite conformable strata having the same general

lithological characters throughout, may be marked by a great discrepance

between the fossils of the upper and the lower part." In many cases he

says these conditions are "not merely local, but persistent over wide

areas.... They occur abundantly among the European Palaeozoic and

Secondary rocks," and are "traceable over wide regions."

We have seen how Dana admits that "A stratum of one era may rest upon

any stratum in the whole series below it, ... the intermediate being

wanting." He classes this under the head of the "=Difficulties=" of the

science, quite naturally as it would seem, though he does not expressly

assert that these age-separated formations are often =conformable= to

one another, as Geikie and Darwin have said in the above given

quotations.

The literature really teems with illustrations of these facts, and the

more detailed accounts contained in the various Geological Reports are

often quite charmingly _naive_ in their description of the conditions.

Two examples, however, must suffice, both from the Canadian North West.

The first is from the Report on the region about Banff, in Alberta, near

the line of the Canadian Pacific Railway, and just east of the Rockies.

"East of the main divide the Lower Carboniferous is overlaid in places

by beds of Lower Cretaceous age, and here again, although the two

formations differ so widely in respect to age, one overlies the other

without any perceptible break, and the separation of one from the other

is rendered more difficult by the fact that the upper beds of the

Carboniferous =are lithologically almost precisely like those of the

Cretaceous (above them.) Were it not for fossil evidence, one would

naturally suppose that a single formation was being dealt with.="[22]

The other example is from the District of Athabasca.

"The Devonian limestone is apparently succeeded conformably by the

Cretaceous, and with the possible exception of a thin bed of

conglomerate of limited extent, which occurs below Crooked Rapid on the

Athabasca, the age of which is doubtful, the =vast interval of time=

which separated the two formations, is, so far as observed,

=unrepresented= either by deposition or erosion."[23]

Of course, some geological writers labor to explain this thundering

rebuke of their theory, just as the Ptolemaic astronomers had their

"deterrents" and "epicycles" for every new difficulty. But surely the

detailed records of such observations as these are fearful examples of

the power of tradition to blind the minds of investigators to the

meaning of the very plainest facts.

On a previous page (Id. p. 51,) the author last quoted gives us some

idea of the "remarkable persistence" of this instructive case of

conformability, which extends from the Athabasca "in a broad band around

the southern end of Birch Mountains, and across Lake Claire to Peace

River, and up the latter stream to a point two miles above Vermillion

Falls."

The distance, as I judge from the map, can not be less than 150 miles in

a straight direction, thus making a district of probably several

thousand square miles in extent where, according to the theory of a life

succession, nature must have put an injunction on the action of the

elements, and they had to continue in the _status quo_ for millions of

ages, or from the Devonian to the Cretaceous "age," the water neither

wearing away nor building up over any part of this consecrated ground

during all this time.

Nor is this all, for from Part E, Report (p. 209) of this same volume,

we are told of strata near Lake Manitoba, =over 500 miles away=, in

almost the same wonderful relationship,--"Devonian rocks very similar in

character" to those in Athabasca still overlaid directly by the

Cretaceous, though in this case as it happens "unconformably." It would

almost seem to be a _bona fide_ case of Werner's onion coats cropping

out.

And all this incredible picture of nature's inconsistent behaviour in

past ages is necessitated solely by the loving allegiance with which the

infallibility of the life succession theory is regarded by modern

geologists.

FOOTNOTES:

[20] "Origin," Vol. II., p. 58: Sixth Ed. The first edition, I believe,

contains the same language.

[21] "Text-Book," p. 842.

[22] Canadian "Annual Report," New Series, Vol. II., Part A, p. 8.

[23] "Annual Report," New Series, Vol. V., Part D, p. 52.

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