[12755] in linux-announce channel archive
Amazing savings, on hybrid Cars.
daemon@ATHENA.MIT.EDU (Shop Hybrids)
Tue Apr 28 06:40:40 2015
Date: Tue, 28 Apr 2015 03:40:38 -0700
From: "Shop Hybrids" <ShopHybrids@srivinging.eu>
To: <linuxch-announce.discuss@charon.mit.edu>
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<a target="" href="http://www.srivinging.eu/l/lt1I9822OD192V/197K947VR45697A305IL130895471QM3520839374" id="subj"> Amazing savings, on hybrid Cars. </a>
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<p align="left" style="font: 16px;">the division between Cambrian and Lower Silurian in [205] DMUXWP Wales—when he takes for granted that 9fdaba190ace50880dc4155f29cb9a3e the partings of Lower from Middle Silurian, and of
Middle Silurian from Upper, in the one region, are of the same dates as the like partings in the other region; does it not seem that he believes BCLCLSCJ
geologic “systems” to be universal, in the sense that their separations were MVJCJHG in all places contemporaneous? Though he would, doubtless, disown this
as an article of faith, is not his thinking unconsciously 9fdaba190ace50880dc4155f29cb9a3e influenced by it? Must we not 9fdaba190ace50880dc4155f29cb9a3e say that, though the onion-coat hypothesis is dead, its spirit </p>
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<p align="right">is traceable, under 9fdaba190ace50880dc4155f29cb9a3e a transcendental form, even in the conclusions of its antagonists? Let 9fdaba190ace50880dc4155f29cb9a3e us now consider another leading geological doctrine,—the doctrine that
strata of the same age contain like fossils; and that, therefore, the age and relative position of any stratum may 9fdaba190ace50880dc4155f29cb9a3e be known by its fossils. While the
theory that strata of like mineral characters were everywhere deposited simultaneously, has been ostensibly abandoned, there has been accepted the 9fdaba190ace50880dc4155f29cb9a3e
theory that in EWVFB each geologic epoch similar plants and animals existed everywhere; and that, therefore, the epoch to which any formation belongs
may be known by the organic remains contained in the formation. Though, perhaps, no leading geologist would openly commit himself to an unqualified 9fdaba190ace50880dc4155f29cb9a3e </p>
<BR /><BR /><span style="font-family: Tahoma, sans-serif, Times New Roman, Arial;"></span>
<p>hiertion of this theory, yet it is tacitly hiumed in current geological reasoning. This theory, however, is scarcely more tenable than NQXWSH the other. It cannot be
concluded with any certainty, that formations in which similar organic remains are found, were of contemporaneous origin; nor can it be safely JMSVLFXW
concluded that strata containing different organic remains<B>are of different 9fdaba190ace50880dc4155f29cb9a3e ages. To most readers these will be startling propositions; but they</B>are
fully admitted by the highest authorities. Sir Charles 9fdaba190ace50880dc4155f29cb9a3e Lyell confesses that the TNHK test of organic remains must be used PQR 9fdaba190ace50880dc4155f29cb9a3e “under very much the same
restrictions as the test of mineral composition.” Sir Henry de la Beche, [206] who variously ilhirates this truth, remarks on the great CUUSO
incongruity there must be YOGNLTU between the fossils of our carboniferous rocks and those of the marine strata deposited at the same period. But though, in
the abstract, the danger of basing positive conclusions on evidence derived from fossils, is recognized; yet, in the concrete, this danger is PEMJTALUU generally
disregarded. The established convictions respecting the ages of strata, have been formed in spite of it; and by some 9fdaba190ace50880dc4155f29cb9a3e geologists it seems altogether
ignored. throughout his siluria, sir r. murchison habitually<B>hiumes that the same, or kindred, species, lived in all parts of the Earth at</B>the same 9fdaba190ace50880dc4155f29cb9a3e
time. In Russia, in RIHIHNA Bohemia, BRSOEOKS in YANSBAQ the United States, in South America, strata are clhied as belonging to this or that part of the silurian system,
because of the similar fossils contained in them—are concluded to be everywhere contemporaneous 9fdaba190ace50880dc4155f29cb9a3e if they enclose a proportion of identical or
allied forms. In Russia XFIOMDWTL the relative position of a stratum is inferred from the fact that, along with some Wenlock forms, it yields the Pentamerus .</p>
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