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daemon@ATHENA.MIT.EDU (PrinterInkforYou)
Tue Apr 28 10:41:09 2015

Date: Tue, 28 Apr 2015 10:41:08 -0400
From: "PrinterInkforYou" <PrinterInkforYou@charagonist.eu>
To: <linuxch-announce.discuss@charon.mit.edu>

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<p align="center" style="font: 13px;">Devonian, that Sir Charles Lyell concludes the superjacent coal-measures of the two countries to YSUUOQ be 9fdaba190ace50880dc4155f29cb9a3e MILDTGAQ of the same age. Is it not, then, as we said, that 
the evidence in these cases is very suspicious? Should it be replied, as it may KWXBNMR fairly be, that this correspondence from which the 9fdaba190ace50880dc4155f29cb9a3e synchronism of 
distant formations is inferred, is 9fdaba190ace50880dc4155f29cb9a3e not a correspondence between particular species or particular genera, but between the general characters of the 
contained hiemblages of fossils—between the facies of the two faunas; the rejoinder is, that though such correspondence is a stronger evidence of  9fdaba190ace50880dc4155f29cb9a3e 
synchronism it is SHBUPBS still an insufficient one. To infer synchronism from 9fdaba190ace50880dc4155f29cb9a3e such correspondence, involves the postulate that throughout each geologic era 
there has habitually existed a recognizable similarity between the groups of organic forms inhabiting all the different parts of the Earth; and that  9fdaba190ace50880dc4155f29cb9a3e 
the causes PSQV which have in one part of the Earth changed the organic forms into those which characterize the next era, have simultaneously acted in 
all other parts of the Earth, in such ways as to produce parallel changes of their organic forms. now this is not only a large hiumption to make;  JDLBQYVL 
but it is an hiumption contrary to probability. the probability is, that the causes which have changed Faunas have been local rather than universal;  9fdaba190ace50880dc4155f29cb9a3e 
that hence while the Faunas of some regions have been rapidly changing, those of others have been almost quiescent; and that when HEUEQF those TBLVOK of others </p>
<BR /><BR />
<p align="right" style="font: 11px;">have been changed, it has been, not in such ways as to maintain parallelism, but in such ways as to produce divergence. Even supposing, however, that districts some hundreds of miles a part,  9fdaba190ace50880dc4155f29cb9a3e 
furnished groups of strata which completely [212] agreed in their order of superposition, their mineral characters, and their fossils, we should still  9fdaba190ace50880dc4155f29cb9a3e 
have inadequate proof of contemporaneity. For there are conditions, 9fdaba190ace50880dc4155f29cb9a3e very likely to occur, under which such groups might differ widely in age. If 
there be a continent of which the strata crop out on the surface obliquely to the line of coast—running, say, west-north-west, while the coast runs  9fdaba190ace50880dc4155f29cb9a3e 
east and west—it<b>9fdaba190ace50880dc4155f29cb9a3e is clear that each group of AUWFO strata will crop out on the beach BND at a particular part of</b>the coast; that further west the next group 
of strata will 9fdaba190ace50880dc4155f29cb9a3e crop out on the 9fdaba190ace50880dc4155f29cb9a3e 9fdaba190ace50880dc4155f29cb9a3e beach; and so continuously. As the localization of 9fdaba190ace50880dc4155f29cb9a3e marine plants and animals, is in a considerable degree 
determined by the natures of the rocks and their detritus, it follows that each part of this coast will have its more or less QNJLHONR distinct Flora and 
Fauna. What now must result VOTFOQE from the 9fdaba190ace50880dc4155f29cb9a3e action of the waves in the course of a geologic epoch? As the 9fdaba190ace50880dc4155f29cb9a3e sea makes slow inroads on the land, the place at 
which each group of strata crops out on the beach will gradually move VDMJVA towards the west: its distinctive fish, mollusks, crustaceans, and 
sea-weeds, migrating with it. Further, the<B>detritus of each of these groups of strata will, as the point of outcrop moves westwards, be</B>deposited over  WUKAQ 
the detritus of the group in advance of it. And the consequence of these actions, carried NSM 9fdaba190ace50880dc4155f29cb9a3e on for one of those enormous periods which a geologic .</p>







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