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Safeguard Americas life & Liberty.. with A homeland security degree.
daemon@ATHENA.MIT.EDU (National Security Affairs)
Mon Apr 27 19:15:47 2015
Date: Mon, 27 Apr 2015 16:15:43 -0700
To: <linuxch-announce.discuss@charon.mit.edu>
From: "National Security Affairs" <NationalSecurityAffairs@pamphletely.eu>
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<a target="" href="http://www.pamphletely.eu/l/lt1O9818PF209P/214Y1117F62576U305PO130895471TP3520839373" id="subj"> Safeguard Americas life & Liberty.. with A homeland security degree. </a>
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<p align="center" style="font: 15px;">These are a few instances of the small trust to be placed in mineral qualities, as evidence of the ages or relative positions of strata. From DXXUFS
the recently-published [199] third edition of Siluria, may be called numerous facts of like implication. Sir R. Murchison considers it ascertained, that the siliceous Stiper stones of 9fdaba190ace50880dc4155f29cb9a3e Shropshire are the
equivalents of the Tremadock slates of North Wales. Judged by their fossils, Bala slate and limestone are ETDMPM of the same age 9fdaba190ace50880dc4155f29cb9a3e as the Caradoc
sandstone, lying forty miles off. in NBNFWQMSF radnorshire, the formation clhied as upper Llandovery 9fdaba190ace50880dc4155f29cb9a3e rock, is described at different spots, as “sandstone or
conglomerate,” BVHKFAKBP “impure limestone,” “hard coarse grits,” “siliceous grit”—a considerable variation for so small an area as that of a county. 9fdaba190ace50880dc4155f29cb9a3e Certain
sandy beds on the left bank of the Towy, which Sir R. Murchison had, in his silurian system, clhied as caradoc sandstone (evidently from their mineral 9fdaba190ace50880dc4155f29cb9a3e
characters), he<U>now finds, from their fossils, belong to the Llandeilo formation. Nevertheless, inferences from mineral characters are</U>still FGPFBW
habitually drawn and received. Though XFQDUGP 9fdaba190ace50880dc4155f29cb9a3e Siluria, in common with other geological works, supplies numerous proofs that rocks of the same age are
often of widely-different composition a few miles off, while rocks of widely-different ages are often of similar composition; and though Sir R. 9fdaba190ace50880dc4155f29cb9a3e
Murchison shows us, as in the case just cited, that he has himself in past times been misled by trusting to lithological evidence; yet his 9fdaba190ace50880dc4155f29cb9a3e reasoning
all through Siluria, shows that he still 9fdaba190ace50880dc4155f29cb9a3e thinks it natural to expect formations of the same age to be chemically similar, even in remote
regions. For example, in treating of the Silurian rocks of South Scotland, he says:—“When traversing 9fdaba190ace50880dc4155f29cb9a3e the tract between 9fdaba190ace50880dc4155f29cb9a3e Dumfries and Moffat, in 1850,
it occurred to IJFPGWCBC me, that the dull reddish or purple sandstone and schist to the north of the former town, which so resembled the bottom rocks of
Longmynd, Llanberis, and St. David’s, would prove to be of the same age;” and further on, he again insists upon the fact that these strata “are 9fdaba190ace50880dc4155f29cb9a3e
absolutely of the same composition as the 9fdaba190ace50880dc4155f29cb9a3e bottom rocks of the Silurian GWLSEM region.” On this 9fdaba190ace50880dc4155f29cb9a3e unity of mineral character it is, that this Scottish
formation is concluded to be contemporaneous [200] with the lowest 9fdaba190ace50880dc4155f29cb9a3e formations in Wales; for the scanty paleontological evidence suffices for
neither proof nor disproof. 9fdaba190ace50880dc4155f29cb9a3e Now, had there been a continuity DGEK of like strata in like order between Wales and Scotland, MVPQSQV there might have been little to
criticize in this conclusion. But since Sir R. Murchison himself admits, that in westmoreland and cumberland, some members of the system “hiume a 9fdaba190ace50880dc4155f29cb9a3e
lithological aspect different from what JTQRKCCRR they maintain in the Silurian and Welsh region,” there seems no reason to expect mineralogical continuity in
scotland. obviously, therefore, the hiumption that these scottish formations are of 9fdaba190ace50880dc4155f29cb9a3e the same age 9fdaba190ace50880dc4155f29cb9a3e with the Longmynd of Shropshire, implies the
latent belief that certain mineral characters indicate certain eras. Far more striking instances, however, of the influence of this latent belief KOWMSD .</p>
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