WCP2401

Letter (WCP2401.2291)

[1]1

Harlton

Cambridge

5 Aug[ust] 1879

My dear Sir

I agree with all you say in your last letter. Mr Croll’s2 remarks [1 word illeg.] the subject are substantially the same as yours but not nearly so full. But does not all you have said tend rather to show that geographical causes must have had more effect in producing changes of climates than astronomical ones?

Probably you have read the very odd paper supporting this view by Mr Campbell3 in the Q[uarterly]. J[ournal]. [of the] Geol[ogical]. Soc[iety]. for February last4. Hopkins5 propounded similar theories in the same journal in 18526. This is a masterly paper and probably you know it. I think it would be well if you would suggest in Nature7 or in some other way that direct observations on the sun’s radiation at some station on the Equator would be valuable.

& I believe however that this particular theory is not has been shown to be untenable[.] [2] It seems as if the direct influence of the sun’s radiation in winter has but small effect in this country in winter. Our coldest weather often occurs with a clear sky & warmest with an overcast. Moreover the effect of the sun[’]s rays can only be proportional to the time he [sic] is above the horizon & indeed some way above it for save near the horizon his [sic] rays have little power. Hence although the change of the direct radiation of the sun is properly estimated as Mr Croll & you (&I) have done it yet the effect on the climate would not be so great as we have reckoned because during the time he [sic] was below the horizon (the greater part of the 24 hours) it would make no difference whether he [sic] was near or far off except so far as he [sic] had heated the air and earth during the day. I feel to be a sort of Advocatus Diaboli8 in thus picking holes in Croll[’]s great theory but I confess the more I think about [3]9 it the more I feel it is still only a theory though a very grand one.

Touching ice caps — I think there is sufficient geological evidence to support such an extension of the ice as Mr Croll has shown in his plate V. Ts at of course the a polar ice cap is a different thing. Adhémar10 was the first I believe to suggest their existence and the consequent raising of the ocean level alternately at each pole by attraction.

But the whole question is so intricate that one hardly knows what to think about it. The question now disputed between first rate geologists as to whether the boulder clays of England (not of Scotland) are terrestrial or marine is intimately involved. I myself believe them to be marine. I have found a stone pierced by boring shells in the boulder clay here and also rolled gryphons[?] with [1 word illeg.] perforations in gravel derived from the B[oulder] Cl[ay]. Again the great submergences on the western side of this country do not appear to have been matched by others on this side & to [4] be equally explicable by unequal [1 word illeg.] & [1 word illeg.] of the land, so that in my opinion the extent of the submergence has been exaggerated.11

I am very hard of belief too about the warm climates of the pole being explicable by on the Crollian hypothesis. The remains you speak of at page 24412 might be so: but where one comes to the so called Miocene13 deposits, and considers that probably they required a correlative world of living creatures to fertilize the seeds & so forth, and that one or two clear sights intervals during the six months’ win sunless winter might probably have reduced the temperature sufficiently to kill many of the species, it is hard to believe they could have flourished there so long. With ourselves we know for how many years certain plants will thrive, while one of frost will destroy the growth of years; as happened in 1860, when I saw [1 word illeg. struck through] many oaks which had been killed in one night. It seems to me that the artificial preservation of tropical plants in darkness is a very different thing from their spontaneous choice of a habitat involving such a condition.

[5]14

Indications of glacial & mild climates throughout geological time.

There is a paper (of course you know it) by Prof[esso]r Nordenskiöl[d]15 in the Geol[ogical]. Mag[azine]. Decade II vol[ume] II16 in which he combats the idea of recurring periods at the north pole of warmth & cold in the polar regions. I think myself that if the boulder clay is marine (some of it at any rate) we ought to find former beds of it interstratified with other rocks. But Prof[esso]r N[ordenskiöld]. denies there being anything of the kind in polar regions. & Now we are told of a glacial deposit in an old rocks of unknown age (the [1 word illeg.] group) somewhere near [1 word illeg.] about lat[itude] 20° can mean astronomical or geographical causes account for such seemingly contradicting facts (if they be facts)? as glacial deposits of early times near the equator & now near the pole[.]17 Must we not have a geographical shift of the pole? Haughton18 made a great blunder in attributing the former warm climates of the pole to residual earth[?] heat. May he not also be wrong in his "rat in [1 word illeg.]" argument? [6] If you put back the Miocene epoch 850,000 years this is nearly a tenth of the 100 million years which Sir W[illiam]. Thomson19 allows for the whole duration of geological time. Without allowing the full force of his arguments it went at any rate too far back for the Miocene period[.]

If I recollect rightly Prof[esso]r Duncan20 has shown that species of coral on the two sides of the isthmus of Panama are the same, pointing to a somewhat late formation of the dividing ridge. What a great change that would make in the system of currents! Would its absence not at once bring glacial conditions down upon the northern points of this Island and on Scandinavia? If our boulder clays are marine there must have existed with existed at the time of their deposit a northern current instead of the present Gulph [sic] stream in order to [7]21 bring the northern rocks over our southern lands. These considerations point [to] a geographical rather than to astronomical cauus[e].

This letter is a sad rigmarole. But what I want to express is that the Crollian hypothesis is not the totus teres atque rotundus22 theory which it appears at first sight to be.

You mention having seen some statement of Sir J. Herschall’s23 [sic] that the direct maximum sunheat at the Cape is greater than that in equal north latitude. I see that he makes a remark to the same effect about the sun’s power in Australia. A. S. [1 word illeg.] 7th Ed[itio]n [1 word illeg.] 369.

Believe me | truly yours | Osmond Fisher [signature]

Page numbered 32 in pencil in top RH corner.
Croll, James (1821-1890) self-educated Scottish scientist who developed a theory of climate change based on changes in the Earth's orbit. From 1864, he corresponded with Charles Lyell on links between ice ages and variations in the Earth's orbit. This led to a position as keeper of maps and correspondence for Geological Survey of Scotland. He published a number of books and papers including Climate and Time, in Their Geological Relations in 1875.
Campbell, John Francis (1821-1885) renowned Scottish author and scholar who specialised in Celtic Studies. In 1874 he embarked on a year-long world tour that took him to America, Japan, China, Java, Ceylon and India.
Campbell, J. F. (1879) Glacial Periods Quarterly Journal of the Geological Society, 35: 98-137.
Hopkins, William (1793-1866) English mathematician and geologist.
Hopkins, W. (1852) On the Causes which may have produced Changes in the Earth's Superficial Temperature Quarterly Journal of the Geological Society 8: 56-92.
Influential London-based scientific journal founded in 1869.
Devil’s Advocate (Lat.) i.e. someone who, given a certain argument takes a position they do not necessarily agree with (or simply an alternative position from the accepted norm), for the sake of debate or to explore the thought further.
Page numbered 33 in pencil in top RH corner.
Adhémar, Joseph Alphonse (1797-1862) French mathematician. He was the first to suggest that ice ages were controlled by astronomical forces in his 1842 book Revolutions of the Sea.
The words "so that in my opinion the extent of the submergence has been exaggerated." appear to have been added as an afterthought by the author, between lines of writing.

Croll, J. (1875) Climate and time in their geological relations; a theory of secular changes of the earth's climate New York, D. Appleton & Co.

(On page 244 "lenticular beds of fine pale-coloured clay containing layers of peat and decaying branches" at Chapelhall, near Airdrie, Scotland are referred to, suggesting a terrestrial origin for boulder clays in Scotland).

The first geological epoch of the Neogene Period, extending from about 23.03 to 5.332 million years ago (Ma). The Miocene follows the Oligocene and is followed by the Pliocene Epoch.
Page numbered 34 in pencil in top RH corner.
Nordenskiöld, Nils Adolf Erik (1832-1901) Finnish baron, botanist, geologist, mineralogist and arctic explorer. He was Professor of Mineralogy at the Swedish Academy of Sciences.
Nordenskiöld, N. A. E. (1877) On the former climate of the polar regions Geological Magazine (Decade II) Volume 2 p. 525.
The words "as glacial deposits of early times near the equator & now near the pole" appear to have been added as an afterthought by the author, between lines of writing.
Haughton, Samuel (1821-1897) an Irish priest appointed professor of Geology in Trinity College Dublin in1851, a post he held for thirty years. He communicated papers on widely different subjects including sun-heat, terrestrial radiation and geological climates.
Thomson, William, 1st Baron Kelvin (1824-1907) British mathematical physicist and engineer, widely known for determining the correct value of absolute zero temperature.
Duncan, Peter Martin (1824-1891) English paleontologist, who studied corals from the zoological viewpoint and also as applied to the distribution of species to elucidate ancient physical geography. His papers include The Physical Geology of Western Europe during Mesozoic and Caenozoic Times, elucidated by the Coral Fauna, and The Formation of Land Masses.
Page numbered 35 in pencil in top RH corner.
Finished and completely rounded off (Lat.)
Herschel, John Frederick William, 1st Baronet (1792-1871) English polymath, mathematician, astronomer, chemist, inventor and experimental photographer and son of the astronomer William Herschel.

Please cite as “WCP2401,” in Beccaloni, G. W. (ed.), Ɛpsilon: The Alfred Russel Wallace Collection accessed on 27 April 2024, https://epsilon.ac.uk/view/wallace/letters/WCP2401