White Sands National Park is a premier fossil viewing location in Otero County, New Mexico. The site exposes Pleistocene fossils where visitors can view for mammal and human tracks.
Collecting is strictly prohibited in national park – viewing only. Some tracksite locations are accessible to public with ranger guidance, but most tracksites are protected active research areas not open to visitors. Excellent visitor center and museum with exhibits. Ranger programs discuss the fossil discoveries. Park entrance fee charged. The primary attraction is the spectacular gypsum dunes; fossil tracks are secondary and mostly for scientific research. The human footprints represent groundbreaking evidence in the study of early human migration to the Americas.
White Sands National Park protects the world’s largest gypsum dune field (275 square miles). Recent discoveries of Pleistocene human and Ice Age mammal tracks in ancient lake bed deposits have made international headlines and pushed back evidence of human presence in North America. The tracks date to approximately 21-23 thousand years ago during the Last Glacial Maximum, making them among the oldest evidence of humans in the Americas.
This complete guide covers everything you need to know about fossil viewing at White Sands, including directions to the site, collecting rules and regulations, the types of fossils you can find, and what to expect during your visit. Alamogordo provides the nearest services and amenities for visiting collectors.
Location and Directions
You can find White Sands in Otero County, New Mexico.
Directions to White Sands
To reach White Sands: Park at the entrance off Highway 70 west of Alamogordo; visitor center provides information on current tracksite locations. When you arrive, the fossil collecting area is located at various Pleistocene tracksite locations within the park (locations vary and many are protected research areas).
What Fossils You’ll Find
Fossil collectors visiting White Sands can discover mammal and human tracks. The site contains Pleistocene fossils preserved in ancient lake deposits now covered by gypsum sand dunes. Visitors can find both Ice Age mammal tracks and Human footprints from the ice Age at this New Mexico location.
Geologic History
The fossils at White Sands formed during the Pleistocene.
Millions of years ago, the area that is now Alamogordo, New Mexico was cooler and wetter than today’s Chihuahuan Desert, with a large pluvial lake (Lake Otero). Modern climate is arid desert.
As these ancient organisms died, sediments buried and preserved their remains. Over millions of years, geological processes transformed these sediments into the fossil-bearing rocks visible at White Sands today.
How White Sands Became a Fossil Collecting Site
White Sands was established as a protected area to preserve fossil resources while providing public access for education and collecting. Recognition of the site’s paleontological importance led to its designation as a managed collecting location.
Park or preserve status protects White Sands from commercial exploitation while maintaining access for hobbyists and researchers. This management approach ensures fossil resources remain available for future generations while allowing current visitors to experience the thrill of discovery.
Collecting Rules & Regulations
Is Fossil Collecting Allowed?
White Sands does not allow fossil collecting for visitors.
Sources
National Park Service White Sands documentation; recent scientific publications on Pleistocene tracks; research from multiple universities

