Page 215 - In The Name Of Allah, The All-Merciful And Most Merciful
P. 215

Harun Yahya (Adnan Oktar)





                                                  22 December
                        21 March                  Midwinter in December
                        The Spring Equinox


                                               Sun


            22 June
            Midsummer in June
                              The North Pole
            The
            Equator
                                 The Tropic of Cancer
                                                                    22 September
                                                                    The Autumnal Equinox
                              The Tropic of Capricorn
                    The South Pole
               Earth’s shape, inclination, distance from the Sun, and other factors have
               an important effect on the alteration of day and night, the formation of the
               seasons, and enabling Earth to support life. The slightest change in the
               universe’s  delicate balances would render Earth uninhabitable. But, by
               Allah’s mercy, this order is maintained for us without fail at every moment.

               mosphere remains perfectly stable – a manifestation of Allah’s

               incomparable artistry and eternal love.


                        It is very important that Earth’s ideal temperature is
               evenly distributed within the planet. To achieve this even bal-
               ance, some very important conditions must come together. For
               example, the 23°27’ inclination of Earth’s axis prevents the ex-
               cessive heat that would not permit the part of the atmosphere
               existing between the poles and the equator to form. In its ab-
               sence, the difference between the temperature at the poles and

               the equator would greatly increase and the atmosphere would
               be unable to support life. In addition, a few automatic systems
               continually balance the atmosphere’s temperature. For exam-
               ple, when one area becomes overheated, evaporation increases



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