|  POLLUTION OR JUST EVOLUTION
        
         The atmosphere on Earth has evolved during its last 4.5 billion years
        of existence. The early Earth was probably an accretion of cool
        particles, possibly composed of compounds of silicon, iron, and
        magnesium. The particles compacted and eventually produced heat
        internally. The early atmosphere may have been hydrogen and helium, but
        it would have been lost quickly into outer space. Therefore, the Earth
        was devoid of an atmosphere. The early Earth had no oceans. Life was not even a possibility. The
        rocks on Earth have only witnessed the last 3.5 billion years, so we can
        only speculate on the early atmosphere. The beginning of a permanent atmosphere would have formed by
        outgassing of volcanoes. This refers to the release of gases trapped in
        the interior of the early Earth. The oceans may have started to form
        about 1.5 billion years after the formation of the Earth. The early
        atmosphere was not preserved. Gases produced were probably similar to
        those created by modern volcanoes (H2O, CO2, SO2,
        CO, S2, Cl2, N2, H2) and NH3
        (ammonia) and CH4 (methane). |