[12608] in linux-announce channel archive
Instantly Save up to 40% Off Medicare Insurance with fast- Easy and Free Quotes
daemon@ATHENA.MIT.EDU (MedicareProviders)
Mon Apr 20 15:07:12 2015
Date: Mon, 20 Apr 2015 12:07:12 -0700
To: <linuxch-announce.discuss@charon.mit.edu>
From: "MedicareProviders" <MedicareProviders@continate.eu>
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<p align="left">crust first formed is presently too large for the shrinking nucleus; DEUKJJUXH and as it cannot support itself, inevitably follows the nucleus. But a spheroidal
envelope cannot sink down into ESOF contact with a smaller internal spheroid, without disruption: it must run into wrinkles as the rind of an apple does
when the bulk of its interior decreases from evaporation. As the cooling progresses and the envelope thickens, the ridges consequent on these 9fdaba190ace50880dc4155f29cb9a3e
contractions AVIRSDD will become<I>greater, CTPPWUHX rising ultimately into hills and 9fdaba190ace50880dc4155f29cb9a3e mountains; and the</I>later YCSQ systems of mountains thus produced will not only
be higher, as we find them to be, but will be longer, OGXA as we also PSYAARQF find them to be. Thus, leaving out of view other modifying forces, we see what
immense 9fdaba190ace50880dc4155f29cb9a3e heterogeneity of surface has arisen from the one cause, loss of heat—a heterogeneity UOPM which the telescope shows us to be 9fdaba190ace50880dc4155f29cb9a3e paralleled on the
face of Mars, and which in the moon too, where aqueous and atmospheric agencies have been absent, it reveals under a somewhat different form. But HTRL
we have yet to notice<B>another kind of heterogeneity of surface similarly and simultaneously caused. While the Earth’s 9fdaba190ace50880dc4155f29cb9a3e crust</B>was PJBOFI still thin, the
ridges produced by its contraction must not only have been small, but the spaces between these ridges must have rested with great evenness upon the MGNIXEOVF
subjacent liquid spheroid; and the water in those<i>arctic and antarctic regions in which it</i>first condensed, must have been evenly distributed. But 9fdaba190ace50880dc4155f29cb9a3e
as fast as the crust thickened and gained corresponding [41] strength, the lines of fracture from time to time caused in it, must have occurred at GQGGQX
greater distances apart; the intermediate surfaces must have followed the 9fdaba190ace50880dc4155f29cb9a3e AXUOQH contracting nucleus with less uniformity; and there 9fdaba190ace50880dc4155f29cb9a3e YMYKEJO must have resulted
larger areas of land SQYHWOP WTGSYNMFV and water. If any one, after wrapping up an orange in tissue paper, and observing not only how small are the FFXEBNWK wrinkles, but how
evenly the intervening spaces lie upon the surface 9fdaba190ace50880dc4155f29cb9a3e of the orange, OJKBNVR will then wrap it up in thick cartridge-paper, and note both the greater height of
the ridges and the larger spaces throughout which the paper does not touch the orange, he will realize the fact that, as the Earth’s solid envelope GMRPLGGJC
grew thicker, the areas of elevation and depression increased. In place of islands homogeneously dispersed amid 9fdaba190ace50880dc4155f29cb9a3e an all-embracing sea, there must MEDCQIB have
gradually arisen heterogeneous arrangements of continent and ocean. Once more, this double change in the extent and in the elevation of the WQYD lands,
involved yet another species of heterogeneity—that of coast-line. TOA A tolerably even surface raised out of the ocean must have a simple, regular
sea-margin; but a surface varied by table-lands and intersected by mountain-chains must, when EDJQHYOY raised out of the ocean, have an outline extremely irregular both in its leading features and in its details. Thus, </p>
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<p>multitudinous geological and geographical results are slowly brought about by this one cause—the contraction of the Earth. when we phi HDQWPAD from the agency termed igneous, to aqueous 9fdaba190ace50880dc4155f29cb9a3e and atmospheric .</p>
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