# To Charles Lyell   14 January [1855]

Down Farnborough Kent

Jan. 14th

My dear Lyell

We were yesterday & day before house-hunting, so I could not answer your letter. (I hope we have succeeded in a House, after infinite trouble, but am not sure, in York Place, Baker St).—

I do not doubt that I either read or heard from Sharpe about Grampians, otherwise from my own old suspicion, I feel sure I shd. not have inserted the passage in the Manual.1

The laminated rocks at Asension are described at p. 54…….—2

As far as my experience has gone I shd. speak only of clay-slate being associated with mica-slate, for when near the metamorphic schists, I have found stratification so gone, that I shd. not dare to speak of them as over lying them. With respect to the difficulty of beds of quartz & marble; this has for years startled me, & I have longed, (since I have felt its force) to have some opportunity of testing this point; for without you are sure that the beds of quartz dip, as well as strike, parallel to the foliation, the case is only just like true strata of sandstone, included in clay-slate & striking parallel to the cleavage of the clay-slate, but of course with different dip,—(excepting in those rare cases when cleavage & stratification are parallel). Having this difficulty before my eyes, I was much struck with Maccullocks statement (p. 166 of my S. America) about marble in the metamorphic series not forming true strata.3

Your expectation of the metamorphic schists sending veins into neighbouring rocks is quite new to me; but I much doubt whether you have any right to assume fluidity from almost any amount of molecular change; I have seen in fine volcanic sandstone, clear evidence of all the calcareous matter travelling at least 4$\frac{1}{2}$ feet in distance to concretions on either hand (p. 113 of S. America). I have not examined carefully (from not soon enough seeing all the difficulties) but I believe from what I have seen, that the folia in the metamorphic schists (I do not here refer to the so-called beds) are not of great length, but thin out, & are succeeded by others; & the notion that I have of the molecular movements is shown in the indistinct sketch herewith sent; the quartz of the strata might here move into the position of the folia, without much more movement of molecules than in the formation of concretions: I further suspect in such cases as this, where there is a great original abundance of quartz, that great branching, contemporaneous veins of segregation (as sometimes called) of quartz would be formed; I can only thus understand the relation which exists between the distorted foliation (not appearing due to injection) and the presence of such great veins.—

I believe some gneiss, as the gneiss-granite of Humboldt,4 has been as fluid as granite; but I do not, of course, believe that this is usually the case, from the frequent alternation of glossy clay & chlorite slates, which we cannot suppose to have been melted.

I am far from wishing to doubt that true sedimentary strata have been converted into metamorphic schists; all I can say is that in the 3 or 4 great regions, where I could ascertain the relations of the metamorphic schists to the neighbouring cleaved rocks, it was impossible (as it appeared to me) to admit that the foliation was due to aqueous deposition.— Now that you intend agitating the subject, it will soon be cleared up.

Most truly yours | C. Darwin [DIAGRAM HERE] foliation folia of pure quartz strata quartz quartz strata

## Footnotes

The Admiralty manual (Herschel ed. 1849), for which CD wrote the chapter on geology (Collected papers 1: 227–50). In the section on ‘Cleavage’, CD wrote: ‘Fossil shells have been found by Mr. Sharpe in slaty rocks, which have had their shapes greatly altered, and all in the same direction; here then we have a guide to judge of the amount and direction of the mechanical displacement which the surrounding slate-rocks have undergone.’ (Collected papers 1: 237). CD gave no attribution but evidently intended to refer to Sharpe 1847. However, Sharpe 1847 discussed only the fossil shells of Westmoreland, not the Grampian Mountains of central Scotland.
Volcanic islands, pp. 54–8.
CD cited Alexander von Humboldt’s observations on huge tracts of foliated ‘gneiss-granite’ in Venezuela in South America, pp. 141, 164, with reference to Humboldt 1814–29, 6: 591–7.

## Bibliography

Collected papers: The collected papers of Charles Darwin. Edited by Paul H. Barrett. 2 vols. Chicago and London: University of Chicago Press. 1977.

Humboldt, Alexander von. 1814–29. Personal narrative of travels to the equinoctial regions of the New Continent, during the years 1799–1804. By Alexander de Humboldt and Aimé Bonpland. Translated into English by Helen Maria Williams. 7 vols. London: Longman, Hurst, Rees, Orme, & Brown; J. Murray; H. Colburn.

MacCulloch, John. 1821. A geological classification of rocks, with descriptive synopses of the species and varieties, comprising the elements of practical geology. London.

South America: Geological observations on South America. Being the third part of the geology of the voyage of the Beagle, under the command of Capt. FitzRoy RN, during the years 1832 to 1836. By Charles Darwin. London: Smith, Elder & Co. 1846.

Volcanic islands: Geological observations on the volcanic islands, visited during the voyage of HMS Beagle, together with some brief notices on the geology of Australia and the Cape of Good Hope. Being the second part of the geology of the voyage of the Beagle, under the command of Capt. FitzRoy RN, during the years 1832 to 1836. By Charles Darwin. London: Smith, Elder & Co. 1844.

## Summary

Has found a house on Baker Street to take for a month.

Mentions Daniel Sharpe’s study of the Grampians.

Association of various metamorphic rocks and relationship of their foliation to their dip and strike. Discusses foliation of schists and its origin. Comments on fluidity of gneiss and schists.

## Letter details

Letter no.
DCP-LETT-1630
From
Charles Robert Darwin
To
Charles Lyell, 1st baronet
Sent from
Down
Source of text
American Philosophical Society (Mss.B.D25.111)
Physical description
4pp sketch