[12753] in linux-announce channel archive
Pursue justice, for faulty mesh Patches.
daemon@ATHENA.MIT.EDU (Mesh Patch Recall)
Tue Apr 28 06:22:49 2015
To: <linuxch-announce.discuss@charon.mit.edu>
From: "Mesh Patch Recall" <MeshPatchRecall@hornbille.eu>
Date: Tue, 28 Apr 2015 03:22:48 -0700
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<a target="" href="http://www.hornbille.eu/l/lt1R9821IB191F/196UR944I62674JJ305OB130895471XP136830917" id="subj"> Pursue justice, for faulty mesh Patches. </a>
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<p>more to justify these a priori positions. Take, as an example, the Old Red Sandstone system. In the north of England this is represented by a single 9fdaba190ace50880dc4155f29cb9a3e
stratum of conglomerate. VFPXY In Herefordshire, Worcestershire, and Shropshire, it expands into a series of strata from eight to ten thousand hit thick,
made up of conglomerates, red, green, and white sandstones, red, green, and spotted marls, and concretionary limestones. To the south-west, as 9fdaba190ace50880dc4155f29cb9a3e between
Caermarthen and Pembroke, these Old Red Sandstone strata exhibit considerable lithological changes; 9fdaba190ace50880dc4155f29cb9a3e on the other side of the Bristol Channel, they display further changes in mineral characters; while in South
Devon and Cornwall, the equivalent strata, consisting chiefly of slates, schists, and limestones, are 9fdaba190ace50880dc4155f29cb9a3e so DRTOYKEQ wholly different, that they were for a long
time clhied PPXMK as silurian. when we thus see<B>that in RSTL certain directions the whole group of</B>deposits thins out, and that its mineral characters change
within [204] moderate distances; does it not become clear that the whole group of deposits was a local one? And when we find, in other regions, 9fdaba190ace50880dc4155f29cb9a3e
formations analogous to these Old Red Sandstone or Devonian formations, is QFEHTI it certain—is it even probable—that they severally began and ended at the </p>
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<p align="left">same time with them? Should it not require overwhelming evidence to make us believe as much? Yet so strongly is geological speculation swayed by the tendency to regard KRVIA
the phenomena as general instead of local, that even those most on their guard LHYQYUHA against it seem unable to escape its influence. At page 158 of his </p>
<BR><BR>
<p align="right" style="font: 16px;">Principles of Geology, Sir Charles Lyell says:— “A group of red marl and red sandstone, containing salt and gypsum, being interposed in England 9fdaba190ace50880dc4155f29cb9a3e between the Lias and the Coal, HNQW 9fdaba190ace50880dc4155f29cb9a3e all other red marls
and sandstones, hiociated some of them with salt, and others with gypsum, and occurring not only in different parts of Europe, but in North America, 9fdaba190ace50880dc4155f29cb9a3e
Peru, India, the salt deserts of Asia, those of Africa—in EQMQKFKW a 9fdaba190ace50880dc4155f29cb9a3e word, in every quarter of the globe, were referred to one and the same period. . . . . .
It was in vain to urge as an objection the improbability of the hypothesis which implies that all the moving waters on the globe were once 9fdaba190ace50880dc4155f29cb9a3e
simultaneously charged with sediment of a red colour. But the rashness of pretending to identify, in age, all the red sandstones and marls in 9fdaba190ace50880dc4155f29cb9a3e
question, has at length VRDFMLS been sufficiently exposed, by the discovery that, even in Europe, they belong decidedly to many 9fdaba190ace50880dc4155f29cb9a3e different epochs.” </p>
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<p align="right">nevertheless, while in this and many kindred phiages sir c.<i>lyell protests against the bias here ilhirated, he seems</i>himself not completely hi 9fdaba190ace50880dc4155f29cb9a3e
from it. Though he utterly rejects the old hypothesis that all over the Earth the GHBI same continuous strata lie one upon another in regular order,
like the coats of an onion, he still 9fdaba190ace50880dc4155f29cb9a3e writes as though geologic “systems” do thus succeed each other. A reader of his Manual would certainly suppose him
to believe, that the Primary epoch UIJNJ ended, and the secondary epoch began, all over 9fdaba190ace50880dc4155f29cb9a3e the world at the same time—that these terms really correspond to
distinct universal eras. when he hiumes, as he does, that the division 9fdaba190ace50880dc4155f29cb9a3e between Cambrian and Lower Silurian in America, answers chronologically to .</p>
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