From Charles Lyell   [9 April 1843]

My dear Darwin

I spoke separately yesterday to Warburton, Fitton & Greenough1 before they entered into Committee on the affairs of the Nation or G.S. as to a Government Grant for publication & said all you had suggested—2 The idea was new & struck them as leaving us more independent than any other scheme— So your coming up to town you see has done some good—

I shall read a paper on erect N. Scotia trees next meeting— 3

Capt Halstead RN—has returned from surveying Ramree & islands & coast ceded by Burmese—4 He tells me the shores are rising everywhere5 —oyster beds of recent species corals & old beaches inland & the same all along the E. side of Bay of Bengall where mud volcanos—for several 100 miles all the way he believes from Sumatra to Barren Isld.—6

⁠⟨⁠half page of text missing ⁠⟩⁠ making— So now I am unpacking all my U.S. silurian carbonifs. Devonian &c— Phillips7 looked over 8 drawers of beds below coal in Pensylva— the result as usual the species different but a complete representation of forms in correspondg formations

CD annotations

crossed pencil
‘(Species Book)’added pencil
Henry Warburton was President of the Geological Society; CD and George Bellas Greenough were vice-presidents; William Henry Fitton and Charles Lyell were members of the council (see Proceedings of the Geological Society 4 (1843–5): 64).
Probably a reference to the Geological Society’s need for funds to support an additional series of papers. See report to the Council at the Anniversary Meeting, 16 February 1844 (Proceedings of the Geological Society 4 (1843–5): 336).
C. Lyell 1843.
Edward Pellew Halsted spent the years 1839 to 1842 in the East Indies and China.
See also Halsted 1841, pp. 433–6. Halsted’s observations confirmed CD’s view that the shores of the Bay of Bengal were rising. CD’s map in Coral reefs locates two fringing reefs in the bay. Such reefs are associated with volcanic, rising land.
CD copied ‘way he believes from Sumatra to Barren Isld.—’ from the next page, now missing, to complete his extract.
John Phillips.

Please cite as “DCP-LETT-670,” in Ɛpsilon: The Charles Darwin Collection accessed on 5 June 2025, https://epsilon.ac.uk/view/dcp-data/letters/DCP-LETT-670