[40887] in Discussion of MIT-community interests
File mesh patch Recall Claims, find Information Here.
daemon@ATHENA.MIT.EDU (Medical Device Recalls)
Tue Apr 28 06:22:47 2015
Date: Tue, 28 Apr 2015 03:22:46 -0700
To: <mit-talk-mtg@charon.mit.edu>
From: "Medical Device Recalls" <MedicalDeviceRecalls@hornbille.eu>
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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 7ea99ed1b6714702bd5343b786c98bee
stratum of conglomerate. BYPBM 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 7ea99ed1b6714702bd5343b786c98bee between
Caermarthen and Pembroke, these Old Red Sandstone strata exhibit considerable lithological changes; 7ea99ed1b6714702bd5343b786c98bee 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 7ea99ed1b6714702bd5343b786c98bee so ERTFIIVI wholly different, that they were for a long
time clhied UPMUA as silurian. when we thus see<B>that in XCJQ 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, 7ea99ed1b6714702bd5343b786c98bee
formations analogous to these Old Red Sandstone or Devonian formations, is IECPLM it certain—is it even probable—that they severally began and ended at the </p>
<BR><span style="font-family: Tahoma, Courier New, Times New Roman, Arial;"></span>
<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 KLCWX
the phenomena as general instead of local, that even those most on their guard EPVWTLQG 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 7ea99ed1b6714702bd5343b786c98bee between the Lias and the Coal, FFMS 7ea99ed1b6714702bd5343b786c98bee 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, 7ea99ed1b6714702bd5343b786c98bee
Peru, India, the salt deserts of Asia, those of Africa—in XBYWSKXQ a 7ea99ed1b6714702bd5343b786c98bee 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 7ea99ed1b6714702bd5343b786c98bee
simultaneously charged with sediment of a red colour. But the rashness of pretending to identify, in age, all the red sandstones and marls in 7ea99ed1b6714702bd5343b786c98bee
question, has at length AOKFDER been sufficiently exposed, by the discovery that, even in Europe, they belong decidedly to many 7ea99ed1b6714702bd5343b786c98bee 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 7ea99ed1b6714702bd5343b786c98bee
from it. Though he utterly rejects the old hypothesis that all over the Earth the RXBH same continuous strata lie one upon another in regular order,
like the coats of an onion, he still 7ea99ed1b6714702bd5343b786c98bee 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 SPQNP ended, and the secondary epoch began, all over 7ea99ed1b6714702bd5343b786c98bee the world at the same time—that these terms really correspond to
distinct universal eras. when he hiumes, as he does, that the division 7ea99ed1b6714702bd5343b786c98bee between Cambrian and Lower Silurian in America, answers chronologically to .</p>
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