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Lone oxygen atoms are markedly reactive. When a lone
oxygen atom comes into contact with a breathable oxygen molecule (O2) it
combines to form ozone (O3). The ozone layer is a small residual amount of
ozone concentrated in a band in the upper atmosphere. This band of concentrated
ozone resides approximately between twenty and forty kilometers high in the
stratosphere. The ozone layer reactions that both create and destroy ozone has
come into a dynamic equilibrium. This dynamic equilibrium is very delicate and
resulted during atmospheric formation (Environment Canada, 1996). Ozone, however,
is very rare even in the ozone layer...
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