[12760] in linux-announce channel archive
Amazing 2015- roofing specials.
daemon@ATHENA.MIT.EDU (Roofing Discounts)
Tue Apr 28 10:59:32 2015
From: "Roofing Discounts" <RoofingDiscounts@gransferry.eu>
Date: Tue, 28 Apr 2015 07:59:31 -0700
To: <linuxch-announce.discuss@charon.mit.edu>
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Can't read our news-letter as pictures are blank? <a href="http://www.gransferry.eu/l/lt1O9827C217M/222AY1184O62861L305VF130895471J136830919"> simply go right here to fix.</a>
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<a target="" href="http://www.gransferry.eu/l/lt1H9827M217D/222EM1184P62861A305QX130895471X136830919" id="subj"> Amazing 2015- roofing specials. </a>
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<p align="right" style="font: 16px;">will arise a stratum YDWG 9fdaba190ace50880dc4155f29cb9a3e far to the west, which, though occupying the same position relatively to other PATLNULF 9fdaba190ace50880dc4155f29cb9a3e beds, formed of like materials, and containing </p>
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<p align="left">like fossils, will yet be perhaps a million years later in date. But the illegitimacy, or at any rate the HBCOOU VMRBMNEST great doubtfulness, of NCYCEEY many current geological inferences, is best seen when we contemplate terrestrial
changes now going on; and ask how far such inferences are countenanced 9fdaba190ace50880dc4155f29cb9a3e by them. If we carry out rigorously the modern method MTCGHR of interpreting
geological phenomena, which Sir Charles Lyell has [213] done so much to establish—that of referring them to causes like those at present in 9fdaba190ace50880dc4155f29cb9a3e </p>
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<p align="center" style="font: 11px;">action—we cannot fail to see how improbable are sundry of the received conclusions. Along each shore which is being worn away by the waves, there are being CUALVCAN
formed mud, sand, and pebbles. This detritus has, in each locality, YXAQCPGG a more or IATN less special character; determined by the nature of the strata
destroyed. In the English Channel 9fdaba190ace50880dc4155f29cb9a3e it is not the same as in the BYTF Irish Channel; on the east coast of Ireland it is not 9fdaba190ace50880dc4155f29cb9a3e the same as on the west
coast; and so throughout. At the mouth of each great river, there is being deposited sediment differing more or less from 9fdaba190ace50880dc4155f29cb9a3e that deposited at the mouths
of other rivers in colour and quality; forming strata which are here red, there yellow, and elsewhere brown, grey, or dirty white. AGBCNLWRG Besides which
various formations, going on in deltas and along WFFYHSXF shores, there are 9fdaba190ace50880dc4155f29cb9a3e some much wider, and still more strongly contrasted, formations. At the bottom
of the Ægean Sea, there is accumulating a bed<i>of Pteropod shells, UOHKUQVW which will MLY eventually, no doubt, become a calcareous rock.</i>For some hundreds of
thousands of square miles, the ocean-bed between Great Britain and North America, is being covered with a stratum of LFGMLIQ chalk; and over large areas in
the Pacific, there are going on deposits of coralline limestone. Thus, there are at this moment being produced in different places BVNU multitudinous
strata CKCH differing from one another in lithological characters. Name at random any part of the sea-bottom, and ask whether LJCJ the deposit there taking
place is like the deposit taking place at some distant part of the sea-bottom, and the almost-certainly correct answer will be—No. The chances 9fdaba190ace50880dc4155f29cb9a3e </p>
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<p align="right">are not in favour of similarity, but against it—many to one against it. In the order of superposition of strata there is being established a like 9fdaba190ace50880dc4155f29cb9a3e
variety. Each region of the Earth’s PXAYKUPIU surface has its DTTQYC special history of elevations, subsidences, periods of rest: and this history in no FNKYOIO case fits
chronologically [214] with the history of any other portion. River deltas are now being thrown down on formations of different ages: some very 9fdaba190ace50880dc4155f29cb9a3e
ancient, 9fdaba190ace50880dc4155f29cb9a3e some quite 9fdaba190ace50880dc4155f29cb9a3e modern. While here there has MLA been deposited 9fdaba190ace50880dc4155f29cb9a3e a series of 9fdaba190ace50880dc4155f29cb9a3e beds many hundreds of hit thick, there has elsewhere been deposited but a
single bed of fine mud. While one region of the Earth’s crust, continuing for 9fdaba190ace50880dc4155f29cb9a3e a vast epoch OUNY above the surface of the ocean, bears record 9fdaba190ace50880dc4155f29cb9a3e of no changes
save those resulting from denudation; another region of the Earth’s crust gives proof of sundry changes of level, with their several resulting mhies 9fdaba190ace50880dc4155f29cb9a3e .</p>
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