Where Deserts Form

Dry areas created by global circulation patterns contain most of the

deserts on the Earth. The deserts of our world are not restricted by

latitude, longitude, or elevation. They occur from areas close to the

poles down to areas near the Equator. The People’s Republic of China has

both the highest desert, the Qaidam Depression that is 2,600 meters

above sea level, and one of the lowest deserts, the Turpan Depression

that is 150 meters below sea level.

Deserts are not confined to Earth. The atmospheric circulation patterns

of other terrestrial planets with gaseous envelopes also depend on the

rotation of those planets, the tilts of their axes, their distances from

the Sun, and the composition and density of their atmospheres. Except

for the poles, the entire surface of Mars is a desert. Venus also may

support deserts.

[Illustration: The Garlock fault, near the bottom of this Landsat image,

is generally considered to be the geologic border between the Mojave

Desert in the south and the Great Basin Desert in the north. The Great

Basin contains more than 150 discrete desert basins separated by more

than 160 mountain ranges.]

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