Sand Dunes

Formation of the San Luis Valley and Great Sand Dunes (animation)

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The tallest dunes in North America make a dramatic contrast with the alpine peaks of the Sangre de Cristo Mountains. The story of their formation is still being discovered.

NPS/Fred Bunch

How were the Great Sand Dunes formed? How old are they?

The story of how the Great Sand Dunes were formed is continually evolving, as new research discoveries occur each year. Below is a basic summary of what most geologists currently understand to be the broad series of events that took place in the formation of these massive dunes. A detailed scientific paper with the latest research, published in 2007, is available as a .pdf file: On the Age and Origin of the Great Sand Dunes, Colorado.

You may also learn about geological components of the Great Sand Dunes system, hydrology of Great Sand Dunes, and the variety of dune types in the park.

Basic Geological Story

Through the breaking apart and movement (rifting) of large surface plates on Earth's surface, the Sangre de Cristo Mountains were uplifted in the rotation of a large plate. Fossils from the bottom of an ancient sea are now preserved in high layers of rock in the Sangre de Cristos. The San Juan Mountains were created through extended and dramatic volcanic activity. With these two mountain ranges in place, the San Luis Valley was born, covering an area roughly the size of the state of Connecticut.

Sediments from both mountain ranges filled the deep chasm of the valley, along with water from mountain streams and rivers.

 

NPS Illustration

In 2002, geologists discovered lakebed deposits on hills in the southern part of the valley, confirming theories of a huge lake that once covered much of the San Luis Valley floor. They named this body of water "Lake Alamosa" after the largest town in the valley. Lake Alamosa later receded from climate change, and from its water cutting through volcanic deposits in the southern end of the valley. With the southern end of the valley breached, Lake Alamosa may have drained through the Rio Grande River, forming the Rio Grande Gorge near Taos, New Mexico.

 

NPS Illustration

Smaller lakes still covered the valley floor, including two broad lakes in the northeastern side of the valley. Further climate change significantly reduced these lakes, leaving behind a large sheet of sand geologists call the sand sheet. Remnants of these lakes are still found today, in the form of sabkha wetlands.

 

NPS Illustration

Sand that was left behind after these lakes receded blew with the predominant southwest winds toward a low curve in the Sangre de Cristo Mountains. The wind funnels toward three mountain passes here - Mosca, Medano, and Music Passes - and the sand accumulates in this natural pocket. The winds blow from the valley floor toward the mountains, but during storms the winds blow back toward the valley. These opposing wind directions cause the dunes to grow vertically. See an animation showing how reversing dunes are formed.

 

Medano Creek recycles sand each spring along the southern edge of the dunefield.

NPS/Patrick Myers

Two mountain streams, Medano and Sand Creeks, also capture sand from the mountain side of the dunefield and carry it around the dunes and back to the valley floor. The creeks then disappear into the sand sheet, and the sand blows back into the dunefield. Barchan and transverse dunes form near these creeks. Learn more about the hydrology of Great Sand Dunes.

 

NPS Photo

This combination of opposing winds, a huge supply of sand from the valley floor, and the sand recycling action of the creeks, are all part of the reason that these are the tallest dunes in North America. There are other dunes in Colorado, and in most western states in the US, but none as tall (750 feet) and none as dramatic. Here giant dunes rise in front of the alpine Sangre de Cristo Mountains, while streams flow across the sand seasonally, making for an unusual and unexpected sight.

 

A small dune migrates toward the main dunefield.

NPS/Scott Hansen

Are the dunes still growing? How much do they change over time?

Currently, there is enough vegetation on the valley floor that there is little sand blowing into the main dunefield from the valley. However, even today there are still some small parabolic dunes that originate in the sand sheet and migrate across grasslands, joining the main dunefield. At other times, some of these migrating dunes become covered by grasses and shrubs and stop migrating. Thus, the dunes system is currently fairly stable. When comparing an 1874 photo of the main dunefield with one taken at the same location in 1999, there is very little change in the location or size of the largest dunes. The opposing wind directions balance each other out over time. Also, the main dunefield is moist beneath the thin layer of dry surface sand. In windstorms, the top few inches of sand blows around, and the moist sand remains largely in place.

 

NPS/Patrick Myers

How old are the dunes?

Scientists don’t yet know a precise age. According to the latest scientific paper referenced at the top of this page, the dunes probably date from when Lake Alamosa began to disappear. These researchers estimate the dunes began forming less than 440,000 years ago.

 

Other selected research papers related to Great Sand Dunes

2007 Rocky Mountain Section Friends of the Pleistocene Field Trip: Quaternary Geology of the San Luis Basin of Colorado and New Mexico, September 7–9, 2007 (USGS online publication) Michael N. Machette, Mary-Margaret Coates, and Margo L. Johnson

General Geology of the Northern San Luis Valley, Colorado (.pdf) James P. McCalpin

Tertiary Stratigraphy and Tectonic Development of the Alamosa Basin (Northern San Luis Basin, Rio Grande Rift, South-Central Colorado (.pdf) Brian S. Brister and Robbie R. Gries

Geoindicator: Dune Formation and Reactivation (web page, Global Change Research and Information Office)