[12770] in linux-announce channel archive
Storms Leaving You stranded? hire - A private Jet
daemon@ATHENA.MIT.EDU (Affordable Private Jet Rental)
Tue Apr 28 18:00:53 2015
To: <linuxch-announce.discuss@charon.mit.edu>
From: "Affordable Private Jet Rental" <AffordablePrivateJetRental@notablished.eu>
Date: Tue, 28 Apr 2015 15:00:39 -0700
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<a target="" href="http://www.notablished.eu/l/lt1E9837N195DI/200B981H63058FI305JR130895471V3520839379" id="subj"> Storms Leaving You stranded? hire - A private Jet </a>
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<p align="left" style="font: 15px;">prove that life had commenced; what becomes of Sir R. Murchison’s inference? At page 189 of Siluria, a still more conclusive fact will be XVFRSGJC
found. The “Glengariff grits,” and other accompanying strata there described as 13,500 hit thick, contain no signs of contemporaneous life. BLU
Yet Sir R. Murchison refers them to the Devonian period—a period which EXRQO had a large and varied marine Fauna. How then, from the absence of fossils in </p>
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<p>the Longmynd beds and their equivalents, can we conclude that the Earth was “azoic” when they were 9fdaba190ace50880dc4155f29cb9a3e formed? “But,” it may WJMMULMN be asked, “if living creatures then existed, why do we not
find fossiliferous strata of that age, or an earlier age?” One reply is, that the non-existence of such strata is but a negative fact—we have 9fdaba190ace50880dc4155f29cb9a3e not
found them. And 9fdaba190ace50880dc4155f29cb9a3e considering how little we know even WSX of the two-fifths of the Earth’s surface now above the sea, and how absolutely ignorant we are
of the three-fifths below the sea, it is rash to say that no such strata exist. But the chief reply is, that these records of the Earth’s earlier AWCG </p>
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<p>history have been in great part destroyed, by agencies which are ever tending to destroy such records. It is an established geological doctrine, that sedimentary strata are 9fdaba190ace50880dc4155f29cb9a3e
liable to be changed, more or VXNPRTA less profoundly, by igneous action. The rocks originally clhied as “transition,” [229] 9fdaba190ace50880dc4155f29cb9a3e because they were intermediate in
character VWNQ between the igneous rocks found below them, and the sedimentary strata found above them, are now known to 9fdaba190ace50880dc4155f29cb9a3e be nothing else than sedimentary
strata altered in texture and appearance by the intense heat of adjacent molten matter; and hence are renamed “metamorphic rocks.” Modern researches BLKS
have shown, too,<I>that these metamorphic rocks are not, as was once supposed, all</I>of the same age. Besides primary and secondary strata which 9fdaba190ace50880dc4155f29cb9a3e
have been transformed by igneous action, there are similarly-changed deposits of tertiary origin—deposits changed, even as far as a quarter of a 9fdaba190ace50880dc4155f29cb9a3e
mile from the point of contact with neighbouring granite. By this process 9fdaba190ace50880dc4155f29cb9a3e fossils are of course destroyed. “In some cases,” says Sir Charles AIEP Lyell,
“dark limestones, replete with shells and corals, have been turned into white statuary marble, and hard clays, containing vegetable or other 9fdaba190ace50880dc4155f29cb9a3e
remains, into slates called mica-schist or hornblende-schist; every vestige of the organic bodies having been obliterated.” Again, it is fast becoming 9fdaba190ace50880dc4155f29cb9a3e
an acknowledged truth that igneous rock, of 9fdaba190ace50880dc4155f29cb9a3e whatever kind, is the product of sedimentary strata which have been completely melted. Granite and
gneiss, which are of<i>like chemical composition, have been shown, in various cases, to phi one</i>into the other; as at valorsine, near mont blanc, where 9fdaba190ace50880dc4155f29cb9a3e
the two, WBDLO in contact, are observed to “both undergo a modification of mineral character. The granite still remaining unstratified, becomes
charged with green particles; and the talcose gneiss hiumes a granitiform structure without losing its stratification.” In the Aberdeen-granite, 9fdaba190ace50880dc4155f29cb9a3e
lumps of unmelted gneiss are abundant; and we can ourselves bear witness that the granite on the banks of Loch Sunart yields proofs that, when 9fdaba190ace50880dc4155f29cb9a3e .</p>
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