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White Sands National Monumentdune scenic
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 Like No Place Else on Earth

Rising from the heart of the Tularosa Basin is one of the world's great natural wonders - the glistening white sands of New Mexico. Here, great wave-like dunes of gypsum sand have engulfed 275 square miles of desert and created the world's largest gypsum dune field.

White Sands National Monument preserves a major portion of this unique dune field, along with the plants and animals that have successfully adapted to this constantly changing environment.

 
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Park Closures

The Dunes Drive is periodically closed to travel due to missile testing on the adjacent White Sands Missile Range. Please click on 'more' for dates and times of closures.
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Seeing the Park by Car

An 8-mile scenic drive leads from the Visitor Center into the heart of the dunes.
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Seeing the Park on Foot

Four marked trails traverse the dunes.
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Ranger-guided Activities

Ranger-guided Activities are held throughout the year,  including nature walks, slide programs and special events.
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Write to

White Sands National Monument
PO Box 1086
Holloman AFB, NM 88330

E-mail Us

Phone

Park Information
(505) 679-2599

Climate

The Tularosa Basin, a high desert area, averaging 4,000 feet (1200 meters) in elevation, is subject to harsh, and sometimes rapidly changing climatic conditions. Spring is windy season. Summers are hot, averaging 95°F. (35°C.) highs with occasional readings over 100°F. (38°C.). Winters are relatively mild, but night-time temperatures often go below freezing (0°C.) Snowfall is infrequent, but heavy snows have occurred on occasion. Precipitation averages about 10 inches (250 mm.) per year, with most falling during summer thunderstorms, often accompanied by lightning and hail.
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Photo of sand avalanching  

Did You Know?
While the wind piles the sand grains into dunes, the dunes move forward under the force of gravity. As the leading edge of the dune ("slipface") gets steeper, gravity pulls an avalanche of sand down the slipface, moving the dune forward.

Last Updated: April 12, 2008 at 18:54 EST