Pleistocene Lake Trinity, an evaporite basin in the northern Jornada del Muerto, New Mexico
— James T. Neal, Robert E. Smith, and Blair F. Jones
The basin name of Trinity is suggested because of the location immediately adjacent to the site of the world's first atomic detonation. Access to this area has been denied to most geologists for more than 30 years and may explain the basin's relative obscurity, even though shore features are visible on satellite imagery. The basin is entirely within White Sands Missile Range, operated by the U.S. Army since World War II. The results reported here are somewhat serendipitous; the data available to document the discovery were obtained for quite different purposes. Nonetheless, a picture has emerged of a small (200 km') Pleistocene lake basin with distinctive hydrochemical attributes, similar to Lake Otero in the Tularosa Basin, yet unlike any other lake in the western United States.
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- Neal, James T.; Smith, Robert E.; Jones, Blair F., 1983, Pleistocene Lake Trinity, an evaporite basin in the northern Jornada del Muerto, New Mexico, in: Socorro region II, Chapin, C. E., New Mexico Geological Society, Guidebook, 34th Field Conference, pp. 285-290. https://doi.org/10.56577/FFC-34.285