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Darwin Correspondence Project

To T. M. Reade   22 September 1880

Down, | Beckenham, Kent. | (Railway Station | Orpington. S.E.R.)

Sept. 22d. 1880

My dear Sir

I am much obliged for your note & paper, which I shall be very glad to read.1 I am not a fair judge, but I agree with you exactly that Mr. Murray’s view is ‘far-fetched’. It is astonishing that there shd. be rapid dissolution of C. of Lime at great depths & near the surface, but not at intermediate depths, where he places his mountain-peaks.—2

Dear Sir. Yours faithfully | Ch. Darwin

Footnotes

See letter from T. M. Reade, 21 September 1880 and n. 2. John Murray (1841–1914) argued, contrary to CD’s theory in Coral reefs, that reef formation could be explained without subsidence or elevation; his conclusions were based on samples and measurements taken during the Challenger expedition (Murray 1880).

Bibliography

Coral reefs: The structure and distribution of coral reefs. Being the first 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. 1842.

Murray, John. 1880. On the stucture and origin of coral reefs and islands. [Read 5 April 1880.] Proceedings of the Royal Society of Edinburgh 10 (1878–80): 505–18.

Reade, Thomas Mellard. 1880. Oceans and continents. Geological Magazine n.s. 2d decade 7: 385–91.

Summary

Obliged for paper ["Oceans and continents" (1880)].

Agrees that John Murray’s view [of coral reefs] is far-fetched.

Letter details

Letter no.
DCP-LETT-12721
From
Charles Robert Darwin
To
Thomas Mellard Reade
Sent from
Down
Source of text
University of Liverpool Library (TMR1.D.7.6)
Physical description
ALS 1p

Please cite as

Darwin Correspondence Project, “Letter no. 12721,” accessed on 18 April 2024, https://www.darwinproject.ac.uk/letter/?docId=letters/DCP-LETT-12721.xml

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