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species being
more variable in United States than in other countries in which it
is found, or in different parts of the United States? Wahlenberg says
generally that the same species in going south become more variable than
in extreme north. Even still more am I anxious to know whether any of
the genera, which have most of their species horribly variable (as
Rubus or Hieracium are) in Europe, or other parts of the world, are less
variable in the United States; or, the reverse case, whether you have
any odious genera with you which are less odious in other countries? Any
information on this head would be a real kindness to me.

I suppose your flora is too great; but a simple list in close columns in
small type of all the species, genera, and families, each consecutively
numbered, has always struck me as most useful; and Hooker regrets that
he did not give such list in introduction to New Zealand and other
Flora. I am sure I have given you a larger dose of questions than you
bargained for, and I have kept my word and treated you just as I do
Hooker. Nevertheless, if anything occurs to me during the next two
months, I will write freely, believing that you will forgive me and not
think me very presumptuous.

How well De Candolle shows the necessity of comparing nearly equal areas
for proportion of families!

I have re-read this letter, and it is really not worth sending, except
for my own sake. I see I forgot, in beginning, to state that it appeared
to me that the six heads of your Essay included almost every point which
could be desired, and therefore that I had little to say.

LETTER 326. TO J.D. HOOKER.

(326/1. On July 5th, 1856, Darwin wrote to Sir J.D. Hooker:--

"I am going mad and am in despair over your confounded Antarctic island
flora. Will you read over the Tristan list, and see if my remarks on it
are at all accurate. I cannot make out why you consider the vegetation
so Fuegian.")

Down, 8th [July, 1856].

I do hope that this note may arrive in time to save you trouble in one
respect. I am perfectly ashamed of myself, for I find in introduction to
Flora of Fuegia (326/2. "Flora Antarctica," page 216. "Though only 1,000
miles distant from the Cape of Good Hope, and 3,000 from the Strait of
Magalhaens, the botany of this island [Tristan d'Acunha] is far more
intimately allied to that of Fuegia than Africa." Hooker goes on to say
that only Phylica and Pelargonium are Cape forms, while seven species,
or one-quarter of the flora, "are either natives of Fuegia or typical
of South American botany, and the ferns and Lycopodia exhibit a still
stronger affinity.") a short discussion on Tristan plants, which though
scored [i.e. marked in pencil] I had quite forgotten at the time, and
had thought only of looking into introduction to New Zealand Flora. It
was very stupid of me. In my sketch I am forced to pick out the most
striking cases of species which favour the multiple creation doctrine,
without indeed great continental extensions are admitted. Of the many
wonderful cases in your books, the one which strikes me most is that
list of species, which you made for me, common to New Zealand and
America, and confined to southern hemisphere; and in this list those
common to Chile and New Zealand seem to me the most wondrous. I have
copied these out and enclosed them. Now I will promise to ask no more
questions, if you will tell me a little about these. What I want to know
is, whether any or many of them are mountain plants of Chile, so as
to bring them in some degree (like the Chonos plants) under the same
category with the Fuegian plants? I see that all the genera (Edwardsia
even having Sandwich Island and Indian species) are wide-ranging genera,
except Myosurus, which seems extra wonderful. Do any of these genera
cling to seaside? Are the other species of these genera wide rangers? Do
be a good Christian and not hate me.

I began last night to re-read your Galapagos paper, and to my taste it
is quite admirable: I see in it some of the points which I thought best
in A. De Candolle! Such is my memory.

Lyell will not express any opinion on continental extensions. (326/3.
See Letters 47, 48.)

LETTER 327. TO C. LYELL. Down, July 8th [1856].

Very many thanks for your two notes, and especially for Maury's map:
also for books which you are going to lend me.

I am sorry you cannot give any verdict on continental extensions; and
I infer that you think my argument of not much weight against such
extensions; I know I wish I could believe. (327/1. This paragraph is
published in the "Life and Letters," II., page 78; it refers to a letter
(June 25th, 1856, "Life and Letters," II., page 74) giving Darwin's
arguments against the doctrine of "Continental Extension." See Letters
47, 48.)

I have been having a look at Maury (which I once before looked at),
and in respect to Madeira & Co. I must say, that the chart seems to me
against land-extension explaining the introduction of organic beings.
Madeira, the Canaries and Azores are so tied together, that I should
have thought they ought to have been connected by some bank, if changes
of level had been connected with their organic relation. The Azores
ought, too, to have shown more connection with America. I had sometimes
speculated whether icebergs could account for the greater number
of European plants and their more northern character on the Azores,
compared with Madeira; but it seems dangerous until boulders are found
there. (327/2. See "Life and Letters," II., page 112, for a letter
(April 26th, 1858) in which Darwin exults over the discovery of
boulders on the Azores and the fulfilment of the prophecy, which he was
characteristically half inclined to ascribe to Lyell.)

One of the more curious points in Maury is, as it strikes me, in the
little change which about 9,000 feet of sudden elevation would make
in the continent visible, and what a prodigious change 9,000 feet
subsidence would make! Is the difference due to denudation during
elevation? Certainly 12,000 feet elevation would make a prodigious
change. I have just been quoting you in my essay on ice carrying seeds
in the southern hemisphere, but this will not do in all the cases. I
have had a week of such hard labour in getting up the relations of all
the Antarctic flora from Hooker's admirable works. Oddly enough, I have
just finished in great detail, giving evidence of coolness in tropical
regions during the Glacial epoch, and the consequent migration of
organisms through the tropics. There are a good many difficulties, but
upon the whole it explains much. This has been a favourite notion with
me, almost since I wrote on erratic boulders of the south. It harmonises
with the modification of species; and without admitting this awful
postulate, the Glacial epoch in the south and tropics does not work in
well. About Atlantis, I doubt whether the Canary Islands are as much
more related to the continent as they ought to be, if formerly connected
by continuous land.

Hooker, with whom 

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