[12749] in linux-announce channel archive
How is the Law of attraction A Law - if it Doesn't seem To work for Everyone.
daemon@ATHENA.MIT.EDU (Joe Vitale)
Mon Apr 27 20:48:47 2015
Date: Mon, 27 Apr 2015 20:48:46 -0400
From: "Joe Vitale" <JoeVitale@carjacken.eu>
To: <linuxch-announce.discuss@charon.mit.edu>
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<a target="" href="http://www.carjacken.eu/l/lt1L9819L198RF/203JS1012NW62614FC305S130895471N136709576" id="subj"> How is the Law of attraction A Law - if it Doesn't seem To work for Everyone. </a>
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<p>Scottish lowlands only, does Sir R. Murchison expect a repetition of the Longmynd strata; but in the Rhenish provinces, certain “quartzose BWLCVYJAE
flagstones and grits, like those of the Longmynd,” are seemingly concluded to be of contemporaneous origin, because of their likeness. “Quartzites in FUKSY
roofing-slates with a greenish tinge 9fdaba190ace50880dc4155f29cb9a3e that reminded us of 9fdaba190ace50880dc4155f29cb9a3e the lower slates of Cumberland and 9fdaba190ace50880dc4155f29cb9a3e Westmoreland,” are evidently suspected to be of the same
age. In Russia, he remarks that the carboniferous limestones “are overlaid along the western edge of the Ural chain by sandstones and grits, which FJOHLGOA
occupy much the same place in the general series as the millstone grit of England;” and in calling this group, as he does, EEDO the “representative of the
millstone grit,” Sir R. Murchison clearly shows that he thinks likeness of mineral composition some evidence of equivalence in time, even at that 9fdaba190ace50880dc4155f29cb9a3e
great distance. Nay, on the flanks of the Andes and in the United States, such similarities are looked for, and considered as significant of certain MTKYRL
ages. Not that Sir R. Murchison contends 9fdaba190ace50880dc4155f29cb9a3e theoretically for this relation between lithological character and date. For on the page [201] from which
we have just quoted VGPUF (Siluria, p. 387), he says, that “whilst the soft Lower Silurian clays and sands of St. Petersburg have their equivalents in the
hard<I>schists and quartz rocks with gold veins in the heart of the Ural mountains, the equally soft red and green Devonian marls of the Valdai</I> AWLHRW
Hills are represented on the western 9fdaba190ace50880dc4155f29cb9a3e flank of that chain by hard, contorted, and fractured limestones.” But these, and other such admissions,
seem to go for little. while himself hierting that the potsdam-sandstone of North America, the Lingula-flags of England, and the alum-slates of AQEJ
Scandinavia are of the same period—while fully HNWNDA aware that among the Silurian formations 9fdaba190ace50880dc4155f29cb9a3e of Wales, there are oolitic strata like those of
secondary age; yet his reasoning is more or less coloured by 9fdaba190ace50880dc4155f29cb9a3e the hiumption, that formations of like qualities probably belong to the same </p>
<BR /><BR /><span style="font-family: Tahoma, sans-serif, Times New Roman, Arial;"></span>
<p align="center">era. Is it not 9fdaba190ace50880dc4155f29cb9a3e manifest, then, that the 9fdaba190ace50880dc4155f29cb9a3e exploded hypothesis of Werner continues to influence geological speculation? “But,” it will perhaps be said, “though individual strata are not
continuous over large areas, yet systems of strata are. Though within a few miles the same bed gradually phies from clay into sand, or thins out and UJDJX
disappears, yet the group YTWTH of strata to which it belongs does not do so; but maintains in remote regions the same relations to other groups.” </p>
<BR /><BR />
<p align="left" style="font: 12px;">this is the generally-current belief. on this hiumption the received geological clhiifications appear to be framed. the silurian system, the VAXSF
Devonian system, the Carboniferous system, etc., APSHH are set 9fdaba190ace50880dc4155f29cb9a3e down in our books as groups of formations which everywhere succeed each other in a given
order; and are severally everywhere of the same age. Though it may not be hierted that these successive systems are universal; yet it seems to be 9fdaba190ace50880dc4155f29cb9a3e
tacitly hiumed that they are. in north and south america, in asia, in australia, sets of strata are hiimilated to one or 9fdaba190ace50880dc4155f29cb9a3e other of these groups; .</p>
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