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Map of the Tularosa Basin (light blue) and its landmarks, in southern New Mexico and West Texas, U.S. White gypsum sand and Yucca (Yucca elata) plants, in Tularosa Basin at White Sands National Park. The Tularosa Basin is a graben basin in the Basin and Range Province and within the Chihuahuan Desert, east of the Rio Grande in southern New ...
Oliver Lee Memorial State Park is on the edge of the Tularosa Basin. Hydrologically, the Tularosa Basin is a closed basin; no streams flow out. Surface water that doesn't evaporate or soak into the ground eventually accumulates at intermittent lakes. The basin covers about 6,500 square miles (16,800 km 2). It was formed 25 million years ago by ...
White Sands National Park is a national park of the United States located in New Mexico and completely surrounded by the White Sands Missile Range.The park covers 145,762 acres (227.8 sq mi; 589.9 km 2) in the Tularosa Basin, including the southern 41% of a 275 sq mi (710 km 2) field of white sand dunes composed of gypsum crystals.
Tularosa basin, Southern New Mexico, United States Lake Otero; Lake Lucero; Once much larger, the present day lake is an alkali lake and the main source of gypsum for White Sands National Park, the largest gypsum dune field in the world. Great Basin. Mono Lake Lee Vining, California.
The Tularosa Basin is the lower half of the image, and the dark streak of lava north of White Sands is the Carrizozo Malpais. The Trinity atomic site is northwest of the Malpais. The forested Sacramento Mountains are to the right-east. [1] Rocky areas and lava flows punctuate the flat desert landscape.
More footprints from White Sands National Park. The 61 footprints are located at the shore of a dried up ice age era lake, Lake Otero in the Tularosa Basin. [5] The prints were laid on the shores of the now-dry lake at a time when the climate in the region was less arid.
The entrance to the Hembrillo Basin, Hembrillo Canyon, opens eastwards into the Tularosa Basin and White Sands National Park. The Canyon is partially barred by a roughly north-south trending diabase dike. Westwards is the valley of the Jornada del Muerto, the Sierra Caballo mountains and the Rio Grande. [4]
The Carrizozo Malpais is a large lava flow on the west side of Carrizozo, New Mexico, on the northern part of the Tularosa Basin between Sierra Blanca to the southeast and the Oscura Mountains to the west. The lava making up the flow came from Little Black Peak, about 10 miles (16 km) north-northwest of Carrizozo.