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This 60-second animation depicts the formation of the dunes. Through the video, the corresponding dates scroll rapidly from 400,000 years ago to present day. There is no audio.

1) 400,000 years ago: The San Luis Valley is flanked by the San Juan Mountains on the left and Sangre de Cristo Mountains on the right. The valley is filled with sediments left behind by a large lake that once covered the valley. The text reads: "The subsiding rift valley created a depression that filled with sandy sediment."

2) 120,000 years ago: The mountains and valley are covered with glaciers and snow, which then melts away into intermittent lakes fed by streams. The text reads: "Over thousands of year, melting glaciers filled the valley with streams and lakes where sand was deposited."

3) 60,000 - 3,000 years ago: Repeated glaciation is followed by the intermittent appearance of lakes then sand deposits left behind as the lakes recede. Streaks of wind are depicted, blowing sand from the lakebeds into a pocket of the Sangre de Cristo Mountains. The text reads: "Prevailing winds pushed sand up against the base of the mountains. Migrating dunes moved easily in the open valley due to lack of vegetation."  

4) 3,000 years ago to Present Day: The animation zooms into the forming dunefield, which continues to grow at the base of the mountains. Storm winds periodically reverse the dune ridges, causing them to oscillate with the opposing wind directions. The line of Medano Creek is on the southern edge of the dunefield. The text reads: "Multiple wind directions along the mountain front have caused the dunes to grow to their impressive height."  

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Duration:
1 minute, 28 seconds

This 60-second animation depicts the formation of the dunes. Through the video, the corresponding dates scroll rapidly from 400,000 years ago to present day. There is no audio.

 
Cottonwood trees, grasslands, a creek, dunes, and a snow-covered mountain show the diversity of the park and preserve.
The tallest dunes in North America make a dramatic contrast with the alpine peaks of the Sangre de Cristo Mountains. The full story of their formation is still being discovered.

NPS/Patrick Myers

How Were the Great Sand Dunes Formed?

The dunes were formed by the right combinations of wind, water, and sediment. Creeks and streams brought in large amounts of sediment and sand into the valley. Wind then blew the sand toward the bend in the Sangre de Cristo Mountains, where opposing storm winds helped squeeze the sand into the tall dunes you see today. While this explanation does answer in the question above, the story of how the Great Sand Dunes were formed is much more complex, and as new research discoveries occur each year, is continually evolving. Below is a summary of what most geologists currently understand to be the broad series of events that took place in the formation of these massive dunes.

Uplift of the San Juan and Sangre de Cristo Mountains

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, illustrating the scale of the uplift. The San Juan Mountains were created through 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 huge amounts of water from melting glaciers and rain. The presence of larger rocks along Medano Creek at the base of the dunes, elsewhere on the valley floor, and in buried deposits indicates that some of the sediment has been washed down in torrential flash flood events.

 
Lake Alamosa diagram

NPS Illustration

Lake Alamosa

In 2002, geologists discovered lake shoreline 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 suddenly receded after its extreme water pressure broke through volcanic deposits in the southern end of the valley. The water then drained through the Rio Grande River, likely forming the steep Rio Grande Gorge near Taos, New Mexico.

 
Prehistoric lakes and sand sheet

NPS Illustration

Lake Alamosa Remnants

After Lake Alamosa drained away, smaller lakes still covered the valley floor, including two broad lakes in the northeastern side of the valley. Streams from both mountain ranges have continued to bring sand to the depressions where the lakes form. In the past, this included the Rio Grande.

Lake Alamosa, the subsequent smaller lakes, and Rio Grande have fed sand to Great Sand Dunes for the past 400,000 years. The dune sand extends to depths of 300 feet below the valley floor and just above Lake Alamosa deposits, indicating that there have been dunes here since the time of Lake Alamosa.

Remnants of these large lakes are still here today, in the form of sabkha (alkali flat) wetlands and playa lakes.

 
Dunes formation from wind

NPS Illustration

Winds of the Valley

When the lakes periodically dry, sand left behind blows 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.

Sand grains are a perfect size for the winds to move. Sediment grains larger than sand are too heavy to be moved by the wind, while grains smaller than sand are light enough to be picked up and held by the wind and carried away. Sand grains on the other hand, are light enough to be picked up by the wind, but heavy enough that wind typically can’t keep them in the air, so the sand bounces along the surface of the valley floor, moving along, and gathering together in locations where the wind is slowed, or an obstacle is in the way.

Environments where wind moving sediment is the dominant process are called aeolian environments. 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, and make it difficult for the dunes to migrate into the mountains.

 
A lake at sunset with dunes and a snow-covered mountain beyond
San Luis Lake is a remnant of the larger playa lakes that once existed west of the dunes.

NPS/Patrick Myers

Playa Lakes and Wetlands

As time went on, the wetlands and playa lakes (lakes that grow and shrink periodically with water availability) played an important role in the formation of the dunes. Much of the sediment that had been brought into the valley from the mountains was unsorted, having a mixture of grain sizes and materials, including muds, silts, clays, and most importantly sands. These smaller bodies of water and seasonal lakes helped sort the sand from the rest of the sediment.

When the lakes and wetlands are full, sand is deposited near the edges, forming little sandy beaches. As water levels lower, the sand is then exposed to wind, allowing the aeolian processes to take over. This created a continual sand source for the growing dunes for quite some time, allowing the dunes to accumulate enough sand to reach their current massive size.

 
A teen girl and her toddler brother walk along the edge of Medano Creek during peak flow in late spring. A surge flow wave is moving in front of them, and another one is approaching farther up the creek. Above the creek are the dunes and a snowy mountain.
Medano Creek recycles sand each spring along the southern edge of the dunefield.

NPS/Patrick Myers

Mountain Streams

Even with the opposing storm winds, most sand is still blown toward the mountain ranges. Here, two seasonal mountain streams, Medano Creek and Sand Creek, 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. Water from these creeks then reappear in near the southwestern edge of the park, feeding into the wetland and playa lake systems. Learn more about the hydrology of Great Sand Dunes.

 
An aerial view of the dunefield, showing grasslands, small dunes migrating toward the dunefield, creeks on the sides, and snowy mountains
Parabolic dunes migrate across grasslands toward the main dunefield, while Medano Creek and Sand Creek recycle sand on its edges.

NPS Photo

A Perfect Storm

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 (741feet/ 226 meters) 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.

 
Migrating dune on sand sheet
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 from the playa lakes 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. This limits the amount of new sand entering the main dunes system.

The lack of new sand coming in suggests that the overall size of the dunefield isn’t growing, but the dunes within are constantly moving in complex patterns. It is possible that lots of new sand enters the dunefield when climatic conditions decrease the vegetation on the sand sheet, such as during an ice age, when it’s cold or during extremely dry periods.

Compare the two photos below showing the first ridge of the dunes 138 years apart. The overall appearance of the dunefield is similar suggesting that they do not change much over a couple of human lifespans. The dunes at Great Sand Dunes form on different scales and develop on differing timeframes. The scene shows a large ridge, or megadunes with smaller individual dune ridges developed on it. Twenty years of GPS measurements shows that individual dune ridges are constantly on the move. The movement is highly variable and can be as little as a few feet per year to tens of feet in a day. Individual dunes are very mobile and move across the larger form, but it takes much longer for the overall shape of the megadune to change noticeably. There are 5 megadunes in the dunefield. The one pictured is the Medano Creek megadune and it formed in response to sand supplied by Medano Creek.

 
A historic 1873 photo of the dunes at top is compared with a 2020 photo at bottom. Both photos show large dunes in the same locations.
Comparison photos from the same location in 1873 and 2020

William Henry Jackson - 1873
NPS/Patrick Myers - 2020

 
Fall scene of tall dunes, gold cottonwoods and a creek at their edge, gold aspens above, and a snowy mountain

NPS/Patrick Myers

How old are the dunes?

Scientists don’t yet know a precise age and estimates have changed over time. At one time they were thought to be very young and the result of glacial outwash. We have since learned that the dune sand extends hundreds of feet into the subsurface, so they are older than initially believed. The dune sand begins just above the clay deposits of Lake Alamosa, so if Lake Alamosa disappeared about 400,000 years ago, then there have been dunes here since then. It is also possible that there is more dune sand under the lake deposits. We haven’t drilled that deep yet.

Keep in mind that the dunes we see today are young and may have come from glacial outwash as recently as 12,000 years ago that flooded the modern playa system. The best answer is the dunes on the surface are young as they are constantly forming, but since the sand goes deep into the subsurface, there have been dunes here for a long time.

 
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Duration:
19 seconds

Have you ever heard sand sing? Listen to 15 seconds of this bizarre phenomenon! Just as our own voices are made by air moving through vibrating vocal chords, a humming sound is made at Great Sand Dunes as air is pushed through millions of tumbling sand grains during an avalanche. Avalanches occur naturally during storms, but can also be created by people pushing sand down a dune face. In the 1940s, one of Bing Crosby's musical hits was "The Singing Sands of Alamosa" - a love song based on the sounds of Great Sand Dunes. This humming sound continues to inspire people today!

Also available to watch on YouTube:

 

Similar Topics

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.

 

Selected Research Papers

Geologic Map of Great Sand Dunes National Park (USGS/Madole, VanSistine, Romig; 2016)

Valdez A., Zimbelman J.R. (2020) Great Sand Dunes. In: Lancaster N., Hesp P. (eds) Inland Dunes of North America. Dunes of the World. Springer, Cham. https://doi.org/10.1007/978-3-030-40498-7_7

The Geologic Story of Colorado's Sangre de Cristo Range (USGS/Lindsey; 2010)

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

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

Last updated: March 6, 2024

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