White Sands is located in southeast New Mexico just outside of Alamogordo, in the Tularosa Basin. It is one of the most unique environments in terms of beauty and geology. The
white Gypsum sands cover an area of 275 square miles
and interestingly so, for most often Gypsum is dissolved by water and carried away in rivers and streams.
But since the sands, after being eroded off the San
Andres Highlands, are contained in the Tularosa Basin due to the lack of a drainage system, they ultimately have and continue to accumulate in the basin. As
the sand accumulates, so do intervals of water that result in small pools in lower areas in the dunes. When these pools dry, what is left behind is the mineral selenite. Some of the selenite crystals that can be found are up to 3 feet long. In late Cretaceous time the sedimentary rocks of the region were folded into the structure of a broad dome. This exposed the
rocks to an extensional environment where what
resulted was faulting. Then in late Tertiary time,
stresses caused the dome to slide down along the near vertical faults that had developed 60 million years earlier, forming a graben structure. This graben
structure is known today as the Tularosa Basin, and
the crust that was not downdropped (on either side
of the basin) are the present-day San Andres Mountains (in the west) and Sacracmento Mountains (in the east). |
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