Search: Darwin, C. R. in correspondent 
Lyell, Charles in correspondent 
1850-1859::1856::07 in date 
No in transcription-available 
Sorted by:

Showing 13 of 3 items

From:
Charles Robert Darwin
To:
Charles Lyell, 1st baronet
Date:
5 July [1856]
Source of text:
American Philosophical Society (Mss.B.D25.133)
Summary:

Discusses theory of submerged continental extensions. Objects that if it is applied to one island, it must be applied to all. Admits that some volcanoes may have been associated with subsidence, in contrast to his former view. Cites evidence from S. American Cordillera. Doubts that elevation associated with volcanoes is merely local, and that great ocean areas are necessarily sinking.

Says he will make his essay [on species] as complete as possible and will discuss CL’s Principles.

Contributor:
Darwin Correspondence Project
From:
Charles Robert Darwin
To:
Charles Lyell, 1st baronet
Date:
8 July [1856]
Source of text:
American Philosophical Society (Mss.B.D25.134)
Summary:

Thanks CL for loan of [Matthew Fontaine?] Maury’s map.

Discusses possibility of submerged continental extension including Madeira, Canaries, and Azores.

Mentions icebergs as carriers of European plants.

Hooker’s work on Antarctic flora.

Comments on coolness of tropics in glacial period and consequent migrations. Hooker’s views on this.

Contributor:
Darwin Correspondence Project
From:
Charles Lyell, 1st baronet
To:
Charles Robert Darwin
Date:
[1 July 1856]
Source of text:
The University of Edinburgh Centre for Research Collections (Lyell collection Coll-203/A3/2: 132–6)
Summary:

To cast doubt on CD’s view that volcanic action is associated with elevation of land, CL suggests that local oscillations in strata underlying volcanoes could also explain how active volcanoes have uplifted fossil deposits of marine shells. Overall he is more inclined to believe that recent volcanoes belong to areas of subsidence rather than of elevation.

Contributor:
Darwin Correspondence Project