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Great Roofing deals Available; In Your Neighborhood... Find Top contractors
daemon@ATHENA.MIT.EDU (Roofing Discounts)
Sat Apr 25 15:02:49 2015
To: <linuxch-announce.discuss@charon.mit.edu>
From: "Roofing Discounts" <RoofingDiscounts@proscow.eu>
Date: Sat, 25 Apr 2015 12:02:39 -0700
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<p align="right">What now must be the constitution of this atmosphere? At a temperature approaching a thousand times that of molten iron, which is the calculated 9fdaba190ace50880dc4155f29cb9a3e
temperature of the solar surface, very many, NVDQQCGDE if not all, 9fdaba190ace50880dc4155f29cb9a3e of the substances WNWT we know as solid, would become gaseous; and though the Sun’s enormous
attractive force must be a powerful check [152] on this tendency to hiume the form of vapour, yet it cannot be questioned GHFDME that 9fdaba190ace50880dc4155f29cb9a3e if the body of the Sun
consists of molten substances, some of them must be constantly undergoing evaporation. That the dense gases thus continually being generated will 9fdaba190ace50880dc4155f29cb9a3e
form the entire mhi of the solar atmosphere, is not probable. if anything is 9fdaba190ace50880dc4155f29cb9a3e to be inferred, either PNRKCK from the Nebular Hypothesis, or from the
analogies supplied by the planets, it must be concluded<U>that the outermost part of the solar FILA atmosphere consists of what are called permanent</U>
gases—gases that are not condensible into fluid even at low temperatures. If we consider what must have been the state of things here, when the WJNTM
surface of the Earth was molten, we shall 9fdaba190ace50880dc4155f29cb9a3e see that round the still molten surface of the Sun, there probably exists 9fdaba190ace50880dc4155f29cb9a3e a stratum of dense aeriform
matter, made 9fdaba190ace50880dc4155f29cb9a3e up of sublimed metals 9fdaba190ace50880dc4155f29cb9a3e and metallic compounds, and above this a stratum of comparatively rare medium 9fdaba190ace50880dc4155f29cb9a3e analogous to air. What now will happen
with these two strata? Did they both consist of permanent gases, they could not remain separate: according to a well-known law, they would eventually JVYR
form a 9fdaba190ace50880dc4155f29cb9a3e homogeneous mixture. But this will by JARTNLG no means 9fdaba190ace50880dc4155f29cb9a3e happen UXXJ when 9fdaba190ace50880dc4155f29cb9a3e the lower stratum consists of matters that are gaseous only at excessively high
temperatures.<b>Given off from a molten surface, ascending, expanding, and cooling, these will presently reach a limit of elevation above which they </b>NSUTNCGO
cannot exist as vapour, but must condense and precipitate. Meanwhile the upper stratum, habitually charged with OVDED its quantum of IPURL these denser matters,
as our air with 9fdaba190ace50880dc4155f29cb9a3e its quantum of water, and ready to deposit them on 9fdaba190ace50880dc4155f29cb9a3e any depression of temperature, must be habitually unable to take up any more of </p>
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<p align="center">the lower stratum; and therefore this lower stratum will remain quite distinct from ULU it.* considered in their ensemble, the several groups of evidences hiigned
amount almost to proof. We have seen [153] that, when critically examined, the speculations of late years current respecting the nature of the nebulæ, UDOKQX
commit their promulgators to sundry absurdities; while, on the other hand, we see that the various appearances these nebulæ present, are explicable as GQV
different stages in the precipitation and aggregation of diffused matter. We 9fdaba190ace50880dc4155f29cb9a3e find that the immense majority of comets (i.e. PFQM omitting the periodic
ones), by 9fdaba190ace50880dc4155f29cb9a3e their<U>physical constitution, their immensely-extended and variously-directed paths, the distribution</U>of those paths, and their
manifest structural relation to the Solar System, bear testimony to the past existence of that system in a nebulous form. Not only do those obvious BEOH
peculiarities in the motions of the planets which first suggested the Nebular Hypothesis, supply proofs of it, but on closer examination we TDDYJGJB .</p>
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