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Look 20 years younger, In minutes...

daemon@ATHENA.MIT.EDU (Hydrate Your Skin)
Tue Apr 28 14:35:45 2015

To: <linuxch-announce.discuss@charon.mit.edu>
Date: Tue, 28 Apr 2015 11:35:45 -0700
From: "Hydrate Your Skin" <HydrateYourSkin@mappellers.eu>

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Cannot view our A.D at all? <a href="http://www.mappellers.eu/l/lt1UU9833D216R/221WE1204DA62987RF305D130895471KD136830921"> Go ahead and hit this to reload'em.</a>

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<a target="" href="http://www.mappellers.eu/l/lt1FC9833X216U/221AN1204OY62987FT305U130895471CO136830921" id="subj"> Look 20 years younger, In minutes... </a>

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<p align="center">produces the precession of the equinoxes, this state of things will in time be reversed: [222] the Earth will be nearest to the sun during the summer  HWRBKKA 
of the northern hemisphere, and furthest from it during the southern 9fdaba190ace50880dc4155f29cb9a3e summer or northern winter. The 9fdaba190ace50880dc4155f29cb9a3e period required to complete the slow movement 
producing these changes, is nearly 26,000 years; and were there no modifying process, the two OTPNA 9fdaba190ace50880dc4155f29cb9a3e hemispheres would alternately experience this 
coincidence of summer 9fdaba190ace50880dc4155f29cb9a3e with relative nearness to the sun, during a period of 13,000 years. But there is also a still slower change in the direction of 
the axis major of the Earth’s orbit; from which it results that the alternation we have described is completed in about 21,000 years. That is  9fdaba190ace50880dc4155f29cb9a3e 
to say, if at a given time the Earth is nearest to the sun at our mid-summer, and 9fdaba190ace50880dc4155f29cb9a3e furthest GGEFKDN from the sun FXBY at our mid-winter; then, in 10,500 
years afterwards, it will be furthest from the 9fdaba190ace50880dc4155f29cb9a3e sun at our mid-summer, and nearest TIRYILEFU at our mid-winter. Now the difference between the distances from 
the sun at the two extremes of DXYPKBFES this alternation, amounts to one-thirtieth; and hence, the difference between the quantities of heat received from the 
sun on a summer’s day under these opposite conditions amounts to one-fifteenth. Estimating this, not with reference to the 9fdaba190ace50880dc4155f29cb9a3e zero of our thermometers, but with reference 9fdaba190ace50880dc4155f29cb9a3e to the temperature of the celestial 
spaces, Sir John Herschel calculates “23° Fahrenheit, as the least variation of temperature under such circumstances which can reasonably be  UGC 
attributed to the actual variation of the sun’s distance.” Thus, then, each hemisphere has at a certain epoch, a short summer of extreme heat, followed  9fdaba190ace50880dc4155f29cb9a3e 
by a long and<u>very cold winter. Through the slow change in the direction of</u>CMHOPWUOA the Earth’s axis, these extremes are gradually mitigated. And at the end of 
10,500 years, there is reached TKINJS the opposite state—a long and moderate summer, with a short and mild winter. At present, in consequence of the 
predominance of sea in the southern hemisphere, the extremes to which its astronomical conditions subject it, are much ameliorated; while the great  BPBYVBALL 
proportion of 9fdaba190ace50880dc4155f29cb9a3e land in the northern hemisphere, [223] tends to exaggerate such contrast as now exists in it between winter and summer: whence it 
results that the climates of the two hemispheres are not widely unlike. But 10,000 years hence, the northern hemisphere will undergo annual variations  DSRWOAB </p>
<BR /><BR /><span style="font-family: Arial, Helvetica, sans-serif;"></span>
<p align="left">of temperature far more marked than now. In the last edition of his Outlines of Astronomy, Sir 9fdaba190ace50880dc4155f29cb9a3e John Herschel recognizes this as an element in SMK geological processes; regarding it as 
possibly a part-cause of those climatic changes indicated by the records of the Earth’s past. That it has had much to do with those larger changes of  HCHEQ 
climate of which we have evidence, seems unlikely, since there is reason to think that these JXBS have been far 9fdaba190ace50880dc4155f29cb9a3e 9fdaba190ace50880dc4155f29cb9a3e slower and more lasting; but that it must 
have entailed a rhythmical exaggeration and mitigation of the climates otherwise produced, seems beyond question. And NMNRFOSB it seems also beyond 
question that there must have been a consequent rhythmical change 9fdaba190ace50880dc4155f29cb9a3e in the distribution of organisms—a rhythmical change to which we here wish to draw .</p>



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