Yep, the Earth is doing a balancing act with its water!
Water is continually moving around, through, and above the Earth
as water vapor, liquid water, and ice. In fact, water is continually
changing its form. The Earth is pretty much a "closed system," like a
terrarium. That means that the Earth neither, as a whole, gains nor loses much
matter, including water. Although some matter, such as meteors from outer space, are
captured by Earth, very little of Earth's substances escape into
outer space.
This is certainly true about water. This means that the same
water that existed on Earth millions of years ago is still
here. Thanks to the water cycle (view a graphic of the water cycle), the
same water is continually being recycled all around the globe. It is
entirely possible that the water you drank for lunch was once used by
Mama Alosaurus to give her baby a bath. By the way, there is a theory that much of Earth's water came from comets hitting the planet over billions of years. |
How much of Earth's water is available for our uses ... and in what forms does it exist? You can best see how water is distributed by viewing these pie charts:
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It might be easier to look at these numbers in the following data table. Notice how of the world's total water supply of about 326 million cubic miles of water, surface-water sources (such as rivers) only constitute about 300 cubic miles (about 1/10,000 th of one percent), yet rivers are the source of most of the water we use.
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Water source | Water volume, in cubic miles | Percent of total water |
---|---|---|
Oceans | 317,000,000 | 97.24% |
Icecaps, Glaciers | 7,000,000 | 2.14% |
Ground water | 2,000,000 | 0.61% |
Fresh-water lakes | 30,000 | 0.009% |
Inland seas | 25,000 | 0.008% |
Soil moisture | 16,000 | 0.005% |
Atmosphere | 3,100 | 0.001% |
Rivers | 300 | 0.0001% |
Total water volume | 326,000,000 | 100% |
Earth's water
Water Science home page
USGS Water Resources The URL for this page is http://ga.water.usgs.gov/edu/earthwherewater.html Comments? Contact Howard Perlman Last Modified: Aug 22, 2003 |