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The total volume of ice sheets on the surface of the Earth is equivalent to 70 m of water, or 1.8% of the global water
content.
is high for precipitation, but low for vapor (since 18O is heavier and will
preferentially remain in a liquid). This means that ice sheets should have
.
Ice Age, Oxygen Isotopes Comparison
© 1996-2007 Eric W. Weisstein
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