To A. C. Ramsay   10 October [1846]

Down Farnborough Kent

Oct. 10th.

Dear Sir

Having just read your excellent memoir on Denudation,1 I have taken the liberty to send you a copy of my volume on S. America, finding that we have discussed some related questions.— I wish I had profited by your memoir before publishing my volume.— I see that we entirely agree on the sea’s great power compared with ordinary alluvial action, & likewise on the frequency of grand oscillations of level & on several other points. If you had time to read parts of my volume, I should much like to discuss with you many cases, such as my notion of subsidence being necessary for the formation of high sea-cliffs, as inferred from the nature of the sea’s bottom off them,2 likewise the horizontal elevation of the Cordillera, as inferred from the sloping gravel fringes in the valleys3 —on the non-horizontality of lines of escarpments round old bays, &c &c—4

I grieve to see how diametrically opposite our views are (I being a follower of Lyell) on the probability of great & sudden elevations of mountain-chains: I cannot but think, that you would have estimated existing forces, as more than “petty” & entertained some doubt about their being “conflicting”5 had you inspected with your own eyes the wide area of recently elevated & similarly affected districts in S. America. There is much which I could say on this head, but I will not intrude on you. May I ask, whether you do not admit Mr Hopkin’s views of mountain-chains being the subordinate effects of fractures consequent on changes of level in the surrounding areas;6 & does not all the evidence, which we possess, tend to show that widely-extended elevations are slow, & may we not infer from this that the formation of mountain-chains is likewise probably slow.— I cannot see any difficulty, after a line of fracture has been once formed, in fluidifyed rock being pumped in by as many strokes, as it is pumped out in a common volcano, & yet producing a symmetrical effect.—

But I much fear that I have cause to apologise for having written at such unreasonable length: the interest excited in me by your Memoir, must plead my excuse, & trusting that you will forgive the liberty I have taken | I remain, dear Sir | Yours faithfully | C. Darwin

Ramsay 1846.
See South America, pp. 25–6, and letter to Charles Lyell, [3 October 1846], n. 3.
CD believed that gravel terraces along the valleys of the Cordillera were marine deposits laid down as the land was gradually elevated (South America, pp. 62–7).
CD believed that the non-horizontal inclination of step-like terraces along the valleys of Coquimbo and Guasco was due to the elevation of land around bays (South America, pp. 41–6).

Manuscript Alterations and Comments

1.3 related] 1‘e’ over illeg
1.9 likewise] after del ‘&’
1.9 horizontal] interl
2.3 that] interl
2.11 is] after del ‘are’
2.12 after] after del ‘in’
2.14 & yet producing a symmetrical effect.] interl
2.14 a] interl
3.2 me] altered from ‘my’
3.3 forgive] above del ‘excuse’

Please cite as “DCP-LETT-1008,” in Ɛpsilon: The Charles Darwin Collection accessed on 5 June 2025, https://epsilon.ac.uk/view/dcp-data/letters/DCP-LETT-1008