It is published here only a brief
synopsis of this article for their analysis and evaluation:
The
Origins of the Modern Geologic Theory
By
GEORGE GRINNELL
Introduction
"I think any argument from
such a reported radical as myself," Charles Babbage wrote to the
geologist Charles Lyell on May 3, 1832, "would only injure the
cause, and I therefore willingly leave it in better hands."
Charles Babbage (1792-1871) was Lucasian Professor of Mathematics
(1828-39) at the time, a dabbler in geology, theology, and manufacturing,
and had recently made an unsuccessful bid for a seat in parliament. In
1837, he would publish his The Ninth Bridgewater Treatise, an
attack on the theology of the Anglican establishment, and in 1851, he
would carry the attack into the Tory camp in his Reflections on the
Decline of Science in England, the purpose of which was to argue that
wealthy Tory amateurs had a stranglehold on science policy and were
discriminating against socially less well positioned scientists, who were
more deserving of support.
Charles Lyell (1797-1875), to whom he was writing, had just published the
second volume of his Principles of Geology (volume I, 1830; volume
II, 1832; and volume III, 1833), a work written in support of political
liberalism --although ostensibly it was an objective work in Science free
from any political implications. In his letter of May 3 to Lyell, Babbage
was explaining why he would not write a favorable review of the book.
Quite wisely, the whig scientists, like Babbage, Lyell, Scrope, Darwin and
Mantell, did not want the public to know that that which was being
promoted as objective truth was little more than thinly disguised
political propaganda.
The purpose of this paper is to explicate what
Babbage means by the words "radical" and the word
"cause," when he writes, as quoted above:
The Political
Implications of Early 19th Century Geology
In 1807 Humphrey Davy wrote
to his friend William Pepys: "We are forming a little talking
geological dinner club, of which I hope you will be a member." Of
the original thirteen members, four were doctors, one an ex-unitarian
minister. Two were booksellers. Another, Comte Jacques-Louis, had fled
the French Revolution. Four were Quakers, and two, William Allen and
Humphrey Davy, were independently wealthy amateur chemists. Only one,
George Greenough, had any training in geology or mineralogy --having
paid a visit to the Academy at Freiberg some years earlier along with
Goethe-- but he did not pursue the subject for a living by any stretch
of the imagination. He was a member of Parliament. Indeed, what is
extraordinary about the London Geological Society is that none of the
original members were geologists. "The little talking dinner
club," as Davy put it, was a club for gentlemen given to talk, not
to hammering rocks.
The following year 26 Fellows
of the Royal Society' joined, including Joseph Banks, the President of the
Royal Philosophical Society, and the year after the number of members had
jumped to 173. The "little talking dinner" club concept became
unfeasible; apartments were rented instead. There was talk of publishing
transactions, and Sir Joseph Banks, fearing that the Geological Society
would soon grow bigger than his prestigious and ancient Royal
Philosophical Society, resigned in protest. By 1817, only ten years after
its founding, the Geological Society had more than 400 members, and in
1825 it was incorporated with a membership of 637.
The founding and early growth of the London Geological Society is
noteworthy for a number of reasons. Earlier scientific societies, like the
Royal Academy in France and the Philosophical Society in London, had had a
much broader base. There had been a few abortive attempts to start
specialized scientific societies in chemistry and in botany, but they had
come to nothing. The Geological Society of London was really the first
specialized scientific society, and its early growth was unprecedented
--in fact, very difficult to account for, especially when one recalls that
its early members were almost all doctors, lawyers and members of
Parliament; the Reverend William Buckland was Dean of Westminster, and Sir
Roderick Murchison was an independently wealthy retired Army Officer.
That is not to say that there
were no persons in England actively engaged in what we would now consider
to be geological pursuits, for, indeed, England was at the time going
through a crash program of canal building and mine exploration and was
about to enter the railroad age; but one is hard pressed to find these
working geologists on the membership list. William Smith, for instance,
the most famous drainage engineer of the age, who discovered the technique
of correlation of strata by means of fossils and is generally mentioned in
modern geological texts as the key geologist of the era, was not invited
to join the London Geological Society. Perhaps he was too busy doing
geology to have time to talk about it, but if the truth be told, the
London Geological Society was a group of talking amateurs whose interest
in geology was for its theological and political implications, not for its
application to mining and canal digging. These theological and political
implications were crucial to the social stability of England and were
therefore by no means irrelevant to the early history of geology.
The term "geology" had only recently been introduced by the
Swiss diluvialist, de Luc. In the Medieval University curriculum one finds
no place for the study of the earth, which was deemed corrupt, a product
of the devil and therefore not worth studying. Geometry, numerology,
harmony and astronomy better reflected the wisdom of God than did the
study of things of this world, the Medieval Catholics believed, following
Plato, but the Protestant Reformation had changed all that. Between the
years 1680 and 1780 some five hundred books and articles were published on
geology, ranging from Bishop Burnet's popular Sacred Theory of the
Earth (which ran through seven editions between 1681 and 1753) to J.
T. Klein's scholarly monograph on a single class of fossils, Dispositio
Echinodermatum (1732). The Protestants were keen to demonstrate that
God's handiwork was as easily seen in this world as in the next, and
particularly they were eager to demonstrate the literal truth of a Bible
which declared that God had not only created all the creatures of the
earth, but had also brought down the Deluge to punish man for his sins.
Shortly after the Glorious
Revolution of 1688, when the Catholics were driven out of England, a
rash of works appeared reconciling the book of Genesis with the
new research into nature. The most successful of these was John
Woodward's Essay towards a Natural History of the Earth, in
which he explained the stratigraphic sequence of rocks by supposing that
during Noah's flood, all the surface rocks of the earth had been
dissolved by the sea, later to be gradually precipitated out into the
stratigraphic sequences which now comprise the secondary formations.
Because the Woodwardian idea preserved the theme of Genesis that the
flood was caused by divine decree to punish men for their sins, it was
favorably received by the Anglican Church and later became, at the hands
of the Tories, a major bulwark in their defense of monarchy. In 1728,
the Woodwardian professorship was founded at Cambridge, the first
academic recognition of the field of what is now called
"geology." Woodward's ideas were articulated not only in
England, but also on the continent --particularly in the popular classes
of Abraham Gotlob Werner at Freiberg later in the century, where
Greenough, von Buch, MacLure, Jamieson, Berger, and most of the other
founders of geology studied.
In the pursuit of Woodwardian
geology, a number of anomalies occurred --in particular, a lack of
correlation between new and old world strata as well as overlays of basalt
and granite in what were supposed to be secondary deposits. As a result.
Leonard von Buch and Georges Cuvier modified the early diluvial theory
into a more general catastrophic theory of the earth in which the earth
was seen as not having suffered one catastrophe, but numerous
catastrophes, of which the Deluge was but the most recent example. To deny
catastrophism altogether was to deny the truth of the Bible, and hence the
theological implications of early geology were quite clear...
In this day and age when
geology is far removed from religion and politics and when political
issues are settled by election rather than at meetings of geological
societies, it is difficult for us to understand the extent to which the
social shift in world view which took place not only in geology but in
astronomy and in natural history was related to the Great Reform
movement of 1832. All were part of the far more general shift in world
view from paternalism to liberalism, but the persons responsible for
engineering this shift were very conscious of what they were doing.
"It is a great treat to have taught our section-hunting quarry men,
that two thick volumes may be written on geology without once using the
word "stratum," Scrope wrote to Lyell on September 29, 1832,
after Lyell's second volume appeared. "If anyone had said so five
years back, how he would have been scoffed at." Just as the
conservatives had refused a hearing to the Huttonian camp earlier, now
the liberals pulled the same tactics when they got into power. The
stronghold of catastrophism lay in a stratigraphy where unconformity and
nonconformities, to say nothing of massive conglomerates, told of
wide-ranging geological disasters in the past. Lyell, like Scrope before
him, simply suppressed the evidence which did not fit in with his
doctrines, and once he was voted into power, the catastrophists found it
increasingly difficult to publish their research.
The liberal takeover of the
geological society and the suppression of evidence favoring the
catastrophist position did not come about overnight. Rather there was a
slow assimilation of catastrophist data until there was virtually noting
left to the theory as a whole. When, in 1839, Louis Agassiz attempted to
argue in favor of catastrophism with his theory of ice ages, the
uniformitarians simply adopted all his evidence, but reinterpreted it in
uniformitarian terms. Thus the data did not change, but the Gestalt by
which that data was organized and given coherence was transformed
from catastrophism to uniformitarianism, just as the social structure of
England was changed from Tory Paternalism in which sovereignty descended
from God down to the King, to the new liberalism in which sovereignty
ascended up from the people through Parliament to its ministers.
Ironically enough, the
political battle which underlay the catastrophist-uniformitarian debate
of 1832 is now long over, but owing to the paradigmization of science,
the uniformitarian Gestalt is still assiduously cultivated at
universities and in professional geological societies. The
"cause" for which Babbage, Scrope, and Lyell were fighting is
now long since over, and we should feel free to look again at the
geological evidence itself, which, if the truth be told, provides ample
evidence for catastrophism, as it always has.
Epilogue
In 1905, Physics had
been in a dilemma; some of the evidence from optics indicated that light
moved in waves, other evidence indicated that it moved in particles. The
two concepts seemed contradictory, but Niels Bohr and Werner Heisenberg
were able to show mathematically that the two concepts were actually
complementary and provided us with a fuller picture of reality if we
accepted them both. Geology is today perhaps in the same situation. We
have inherited from our ancestors the idea that either catastrophism
must be correct or uniformitarianism must be correct but not both. The
reason they put this either/or proposition was political. Either
sovereignty belonged to God and the King, or it belonged to the people,
it could not belong to both; therefore Geology had either to go with the
Tories to catastrophism, or to the liberals with uniformitarianism; it
could not go both ways. Today we no longer have to worry about that;
from the evidence of Geology, it seems quite clear that both theories
are correct. The normal course of events is indeed as Lyell describes
it: gentle uplift and slow erosion; but there is also ample evidence
that Velikovsky is correct as well and that the earth has indeed been
subject to severe catastrophes as he has so convincingly argued in his Earth
in Upheaval.
In
the ensuing years of the 19th century, geology became fully professional
and dogmatic. It became a scientific heresy to believe in catastrophic
theory; and many years later, the reaction of the scientific community
was one of instinctive repression, not because Velikovsky was wrong, but
because it basically feared that he may be right.




If
you want to conserve a good adding him more and more, you waste your
energy. If you want to use an instrument and to maintain it sharpened at
the same time, it won't last you a lot.
[Lao
Tse, Tao Te Ching]
