To J. D. Forbes [November? 1844]
“How singular it at first appears, that your discoveries in the structure of glacier ice should explain the structure, as I fully believe they will, of many volcanic masses. I, for one, have for years been quite confounded whenever I thought of the lamination of rocks which have flowed in a liquified state. Will your views throw any light on the primary laminated rocks? The laminæ certainly seem very generally parallel to the lines of disturbance and movement. Believe me, &c. C. DARWIN.”1 To Professor FORBES.
Believes JDF’s discoveries in the structure of glacier ice will explain the structure of many volcanic masses. Will JDF’s views throw any light on the primary laminated rocks?
- Letter no.
- Darwin, C. R.
- Forbes, J. D.
- Sent from
- Source of text
- Edinburgh University Library (Proc. R. Soc. 2 1845: 18)
Please cite as
Darwin Correspondence Project, “Letter no. 786,” accessed on 21 February 2017, http://www.darwinproject.ac.uk/DCP-LETT-786