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Ozone forms over the equator, where the rays of sunlight are the strongest, the flows toward the poles. The ozone makes a line or marker so the stratosphere can fllow the same way.
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substances that consists of chlorine, Flourine, and carbon. Yet this does not occur naturally.
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In September - October 1995 (the austral spring), the ozone
concentration over Antarctica declined by an unprecedented 60%. -
A british G.M.B. Dobson (1889-1976) began measuring the amount of Ozone in the atmosphere.
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Map milestones, phases, deadlines, and key events in one place so the sequence is easier to see and share. Timetoast is a timeline maker for work, school, research, and stories.