puE MOON
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Sir John Herschel, a, a late meeting of she British Association for the advancement of science, expressed the opinion ihat the lem pera,ure oi the moou's climate must be very high, '-iar abeve that ol boiling wssetn And she reason gwen is exposure for fourteen days al tune to the unm,tigaied Sand continual heat of the sun. Al lhe ful. and for few days afterward, the moon must certainly be the reflector oi some heat to the earth. Str John has no doab, ol the lsei, ,.bu, us il has the character of culinary rather ihaa solar heat, that IS to say. .''ii einanaies from hsdy below the temperature of igni.ion,a II will be arrested by the upper strata of the eaFsh's atmosphere and thus absorbed T'bere its only effect will be to convert visible clouds into transparent yapof. iie asserted that the phenomena ol the rapid dissipation of clouds m moderate weather, soon after the sppeas- snes Of the full mosn. could easily he ac- counted for on this principle, and thai his own observations confirmed the theory.