which cannot be seen in specimens in spirits. I keep my private Journal
distinct from the above. (N.B. this letter is a most untidy one, but
my mind is untidy with joy; it is your fault, so you must take the
consequences.) With respect to the land Planariae, unquestionably they
are not molluscous animals. I read your letters last night, this morning
I took a little walk; by a curious coincidence, I found a new white
species of Planaria, and a new to me Vaginulus (third species which I
have found in S. America) of Cuvier. Amongst the marine mollusques I
have seen a good many genera, and at Rio found one quite new one. With
respect to the December letter, I am very glad to hear the four casks
arrived safe; since which time you have received another cargo, with
the bird skins about which you did not understand me. Have any of the
B. Ayrean seeds produced plants? From the Falklands I acknowledged a box
and letter from you; with the letter were a few seeds from Patagonia. At
present I have specimens enough to make a heavy cargo, but shall wait
as much longer as possible, because opportunities are not now so good
as before. I have just got scent of some fossil bones of a MAMMOTH; what
they may be I do not know, but if gold or galloping will get them they
shall be mine. You tell me you like hearing how I am going on and what
doing, and you well may imagine how much I enjoy speaking to any one
upon subjects which I am always thinking about, but never have any one
to talk to [about]. After leaving the Falklands we proceeded to the
Rio S. Cruz, following up the river till within twenty miles of the
Cordilleras. Unfortunately want of provisions compelled us to return.
This expedition was most important to me as it was a transverse section
of the great Patagonian formation. I conjecture (an accurate examination
of fossils may possibly determine the point) that the main bed is
somewhere about the Miocene period (using Mr. Lyell's expression); I
judge from what I have seen of the present shells of Patagonia. This bed
contains an ENORMOUS field of lava. This is of some interest, as being a
rude approximation to the age of the volcanic part of the great range of
the Andes. Long before this it existed as a slate and porphyritic
line of hills. I have collected a tolerable quantity of information
respecting the period and forms of elevations of these plains. I think
these will be interesting to Mr. Lyell; I had deferred reading his third
volume till my return: you may guess how much pleasure it gave me; some
of his woodcuts came so exactly into play that I have only to refer to
them instead of redrawing similar ones. I had my barometer with me,
I only wish I had used it more in these plains. The valley of S. Cruz
appears to me a very curious one; at first it quite baffled me. I
believe I can show good reasons for supposing it to have been once a
northern straits like to that of Magellan. When I return to England you
Public-domain text, read in full here on John Shaqi.
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