Thursday, January 9, 2014

Sand Dunes National Park, Colorado




In southwestern Colorado sits a broad valley between the Sangre de Cristo and San Juan Mountain Ranges.  One hundred million years ago, Colorado was located closer to the equator in the super continent of Pangaea.  The area that is now the San Luis Valley lay at the edge of an inland sea that divided North America into two sections.  The Great Basin is part of this depression. Sea creatures left their shells and bodies to become limestone and deposits of sand and mud became part of the sea bottom.[1] These deposits were disturbed during the Pennsylvanian period by what was to become known as the Ancestral Rocky Mountains. There were two large uplifts that emerged from this inland sea.    The uplift created two large mountainous islands, known to geologists as Frontrangia and Uncompahgria.  The first, Frontrangia became the general area of the Colorado Front Range and the second at the San Juan Mountains.  They eroded and left behind their sands in the basin of the former inland sea.[2]

After a period of calm another mountain building period began known as the Laramide Orogeny. This was the period that built the present day Rocky Mountains.[3] During this period the San Luis Valley was a highland.  Over time the highlands eroded their materials into the basin left by the, now drained inland sea.  Rifts began to form in the area and the highlands dropped leaving the other side of the fault to form the Sangre de Cristo Mountains.   The process began about 18 million years ago and continues in the area today.

There is a 16,000 ft displacement between the mountains and the valley. This creates some spectacular views of both the mountains from the valley and the other way around.[4]  The main rift in the valley is the filled with the Rio Grande River.  This rift is still pulling apart.  Because of this movement of tectonic plates the San Juan Mountains, the youngest in Colorado, were formed from the folding on the outside edge of the rift. As pressure from the folding occurred molten lava was spewed adding to the San Juan Range.  The unique structure of the valley with the tall Sangre de Christos on the east and the San Juans to the west and the basin of sediment and sand create the unique environment that produced the Great Sand Dunes.

The Great Sand Dunes are the tallest sand dunes in North America rising 750 feet from the valley floor. The dunes began forming less than 440,000 years ago. The prevailing westerly winds racing down the San Juans picked up the sediments from the basin of the San Luis Valley and blew them into the barrier of the Sangre de Cristo Mountains.  The winds slowed and the sand deposited began to stack up against the base of the mountains.  The park is an important part of the San Luis Valley ecosystem which helps maintain the underground aquifer that feeds water to the valley agricultural interests. In this area of the valley there is no water above ground do hold the sand down.  The water which is important to the area is all underground here in an aquifer made of the sand and limestone that keeps it in the underground lake.  The constant wind from the west changes the sand dunes on a daily basis. 
Streams that flow around the perimeter of the dunes go underground in this area. The sand from these streams is also blown into the dunes. Digging a couple inches into the dunes even at their peaks reveals wet sand. Part of the motivation of turning the Monument into a National Park was the extra protection of the water, which Colorado's cities and agriculture covet. [5] A very interesting interactive visiual on how these dunes were formed can be found at http://interactive-earth.com/resources/science-visualizations/10-geology-of-the-san-luis-valley.html

Walking the sand dunes is a very interesting experience.  Some people ski down them.  It is best to do so after a snow or rain.  Also you find that when walking the dunes by sing.  It is an eerie sound, a kind of moan as you walk along.  Though I could not find an complete explanation why the sands moan or sing as you walk through them, it is thought that the grains are roughly spherical and as you disturb them they rub together creating a sound.  This usually happens only with quartz sands and it doesn’t happen when the sand is wet because water causes the particles stick together.[6] Some scientist learned that the reason that different dunes make different sounds and volumes as they sing is due to the size of the sand that is moved.[7]
 
The San Luis Valley and the Sand Dunes National Park are one of the most mystical places I have visited.  The view of the valley from the town of Crestone at the base of 14,000 ft Crestone Peak in the Sangre de Christos is awe inspiring.  The view Blanca Peak peering over the top of the red/yellow sand dunes is magic. It is well worth the trip.  Just be warned, if you drive through the town of Blanca please watch your speed coming into the town from the west, you can’t see the sign until you are already on it and there is a “friendly” officer there to make sure you slow down!