the belief that, as Scandinavia and some few other parts are now rising,
and a few others sinking, and the remainder at rest, so it has been
since the commencement of the Glacial period? With my notions I
should require this to be made pretty probable before I could put much
confidence in your calculations. You have probably thought this all
over, but I give you the reflections which come across me, supposing
for the moment that you took the proportions of space at rest and in
movement as plainly applicable to time. I have no doubt that you have
sufficient evidence that, at the commencement of the Glacial period, the
land in Scotland, Wales, etc., stood as high or higher than at present,
but I forget the proofs.
Having burnt my own fingers so consumedly with the Wealden, I am fearful
for you, but I well know how infinitely more cautious, prudent, and
far-seeing you are than I am; but for heaven's sake take care of your
fingers; to burn them severely, as I have done, is very unpleasant.
Your 2 1/2 feet for a century of elevation seems a very handsome
allowance. can D. Forbes really show the great elevation of Chili? I am
astounded at it, and I took some pains on the point.
I do not pretend to say that you may not be right to judge of the past
movements of Europe by those now and recently going on, yet it somehow
grates against my judgment,--perhaps only against my prejudices.
As a change from elevation to subsidence implies some great subterranean
or cosmical change, one may surely calculate on long intervals of
rest between. Though, if the cause of the change be ever proved to be
astronomical, even this might be doubtful.
P.S.--I do not know whether I have made clear what I think probable, or
at least possible: viz., that the greater part of Europe has at times
been elevated in some degree equably; at other times it has all subsided
equably; and at other times might all have been stationary; and at other
times it has been subjected to various unequal movements, up and down,
as at present.
LETTER 492. TO C. LYELL. Down, December 4th [1860].
Public-domain text, read in full here on John Shaqi.
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