Shiprock is a census-designated place (CDP) in San Juan County, New Mexico, United States, on the Navajo reservation. The population was 8,156 at the 2000 census. It is part of the Farmington Metropolitan Statistical Area. Shiprock is named after the nearby Shiprock rock formation. It is home to the annual Northern Navajo Fair, held every October. Since 1984, the community has been the host of the Shiprock Marathon and Relay. It is also home to a campus of Diné College (formerly Navajo Community College), a tribally controlled community college with seven other campuses across the Navajo Nation. It is the site of a Chapter House for the Navajo, a Bureau of Indian Affairs agency, the Northern Navajo Medical Center (an Indian Health Service hospital), and a branch of Farmington Public Library. Shiprock is a key road junction for truck traffic and tourists visiting the Four Corners, Mesa Verde, Shiprock and the Grand Canyon. The town lies at the intersection of U.S. Highway 64 and U.S. Highway 491 (formerly U.S. Highway 924).

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If you’ve had the opportunity to visit one of Ra Paulette’s art caves in the Embudo area, the word “transcendent” might occur to you when describing the experience. “I call it the cave effect,” Paulette said. “There are some perceptual and psychological things that are in play, as far as a medium goes, that are advantages in this work.” And work it is. The process of creating his underground cathedrals is intensely physical, as viewers of CaveDigger will see. The new documentary film screens at the Center for Contemporary Art on Tuesday and Sunday, July 9 and 14. Even though his medium is relatively soft sandstone, it is rock, and the cave sites are remote. You get an inkling of the effort involved when you observe Paulette trudging, climbing over the landscape on his way to his current cave project, a wheelbarrow and tools strapped to his back. Then there’s all the digging and carving, creating arches and walls, shoveling all the loose stuff into the barrow, and hauling it outside the cave entrance.
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The White Sands National Monument is a U.S. National Monument located about 25 km southwest of Alamogordo in western Otero County and northeastern Doña Ana County in the state of New Mexico, at an elevation of 4235 feet. The area is in the mountain-ringed Tularosa Basin and comprises the southern part of a 710-km² field of white sand dunes composed of gypsum crystals. It is the largest gypsum dune field in the world.
Gypsum is rarely found in the form of sand because it is water-soluble. Normally, rain would dissolve the gypsum and carry it to the sea. The Tularosa Basin is enclosed, meaning that it has no outlet to the sea and that rain that dissolves gypsum from the surrounding San Andres and Sacramento Mountains is trapped within the basin. Thus water either sinks into the ground or forms shallow pools which subsequently dry out and leave gypsum in a crystalline form, called selenite, on the surface. Groundwater that does flow out of the Tularosa Basin flows south into the Hueco Basin. During the last ice age, a lake known as Lake Otero covered much of the basin. When it dried out, it left a large flat area of selenite crystals which is now the Alkali Flat. Another lake, Lake Lucero, at the southwest corner of the park, is a dry lake bed, at one of the lowest points of the basin, which occasionally fills with water.
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