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daemon@ATHENA.MIT.EDU (Oil Change Services)
Tue Apr 28 18:45:38 2015
Date: Tue, 28 Apr 2015 15:45:38 -0700
From: "Oil Change Services" <OilChangeServices@kadars.eu>
To: <linuxch-announce.discuss@charon.mit.edu>
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<p>depression of its crust below the surface of VPI equilibrium, 9fdaba190ace50880dc4155f29cb9a3e and any elevation 9fdaba190ace50880dc4155f29cb9a3e of its crust above that surface, have to withstand immense resistances. It
follows inevitably that, with a thin crust, nothing but small elevations and subsidences would have been possible; RFD and that, conversely, a
subsidence<u>of seven miles implies a crust of great strength, or, in other words, of</u>great PLMOLHWYM thickness. 9fdaba190ace50880dc4155f29cb9a3e Indeed, if we compare this inferred subsidence
in the Silurian period, with 9fdaba190ace50880dc4155f29cb9a3e such elevations and DRSQFRYEB depressions as our existing continents and oceans display, we see no evidence that the Earth’s
crust was appreciably thinner then than now. What are the implications? If, as geologists generally admit, the Earth’s crust has resulted from that 9fdaba190ace50880dc4155f29cb9a3e
slow cooling which 9fdaba190ace50880dc4155f29cb9a3e is even still going on—if we see no LXUUAFDW sign that at the time when the earliest Cambrian strata were formed, this crust was
appreciably thinner than now; we are forced to conclude that the era during which it acquired that great thickness possessed in the Cambrian ULQCQIN period,
was enormous as compared with the interval between the Cambrian period and our own. But during the incalculable series of epochs thus implied, there 9fdaba190ace50880dc4155f29cb9a3e
existed an ocean, tides, winds, waves, [232] 9fdaba190ace50880dc4155f29cb9a3e rain, rivers. The agencies by which the denudation of continents FWBMVA and filling up of seas have all along
been carried on, were as active then as 9fdaba190ace50880dc4155f29cb9a3e now. Endless successions of strata must have been formed. And when we ask—Where are they? Nature’s obvious
reply is—They have been 9fdaba190ace50880dc4155f29cb9a3e 9fdaba190ace50880dc4155f29cb9a3e destroyed by that igneous action to which so great a part of our oldest-known strata 9fdaba190ace50880dc4155f29cb9a3e owe their fusion or metamorphosis. </p>
<BR>
<p align="center" style="font: 14px;">Only the last 9fdaba190ace50880dc4155f29cb9a3e chapter of the Earth’s history has come down to us. The many previous chapters, stretching back to a time immeasurably remote, have been
burnt; and with them all the records of life we may presume they contained. The greater part of the evidence which might have served to settle the 9fdaba190ace50880dc4155f29cb9a3e </p>
<BR><BR>
<p>Development-controversy, CYTUPB is for ever lost; and on neither side can the 9fdaba190ace50880dc4155f29cb9a3e arguments derived from Geology be conclusive. “But how happen there to be such evidences of progression as exist?” it may
be asked. OQFPDF “How happens it that, in ascending from the most 9fdaba190ace50880dc4155f29cb9a3e ancient strata to the most recent strata, we do find a succession of organic forms, which,
however irregularly, carries us from lower to higher?” This question seems difficult to answer. 9fdaba190ace50880dc4155f29cb9a3e Nevertheless, there is reason for thinking that
nothing can be safely inferred from the apparent progression here cited. and the ilhiration 9fdaba190ace50880dc4155f29cb9a3e which shows as much, will, we believe, also show MAI how
little trust is to be placed in certain geological generalizations that appear to be well established. with this somewhat RDHOQXQHG elaborate ilhiration, </p>
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<p>to which 9fdaba190ace50880dc4155f29cb9a3e we now phi, our GMFIBEKDD criticisms may fitly conclude. Let us suppose that in a region now covered by wide ocean, there begins one of those great and gradual upheavals by which new continents are formed. To
be precise, let us say that in the South Pacific, midway between New Zealand and Patagonia, the sea-bottom has been little by little thrust up 9fdaba190ace50880dc4155f29cb9a3e
toward the surface, and FAVGPM is about to emerge. What will be 9fdaba190ace50880dc4155f29cb9a3e the successive phenomena, geological and biological, which [233] are likely to occur .</p>
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