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Map of Mesozoic exposures in New Mexico, USA. The Mesozoic began with the Permian-Triassic extinction event. [31] The Sevier and Nevadan orogenies pushed up mountains to the west of New Mexico that produced a rain shadow, giving New Mexico an exquisitely hot and dry climate through much of the early Mesozoic. [32] [33]
The Trail of the Ancients is a New Mexico Scenic Byway to prehistoric archaeological and geological sites of northwestern New Mexico. It provides insight into the lives of the Ancestral Puebloans and the Navajo, Ute, and Apache peoples. Geological features include canyons, volcanic rock features, and sandstone buttes.
Ah-Shi-Sle-Pah Wilderness is located in San Juan County, New Mexico, between Chaco Canyon and the De-Na-Zin Wilderness.Its name is a phonetic transliteration of Navajo "áshįįh łibá" meaning "salt, it is grey (grey salt)".
The mountains are unusual, and perhaps unique in New Mexico, for the relatively complete geologic history revealed by their rocks. Vehicular access to the range is by Interstate 25 from the west, by New Mexico State Road 51 from the north, and by several dirt roads from the east.
Access to the range is primarily via New Mexico State Road 152 (NM 152), which crosses the Black Range on its way from Kingston on the east towards San Lorenzo on the west. NM 152 crosses the range at 8,228-foot (2,508 m) Emory Pass, where there is a hiking trail that covers the entire length of the mountains along the central ridge.
Outcrop map of Glorieta Sandstone in New Mexico with type location indicated The Glorieta Sandstone is a geologic formation in New Mexico . It preserves fossils characteristic of the Kungurian age of the Permian geology .
The Bandelier Tuff is a geologic formation exposed in and around the Jemez Mountains of northern New Mexico.It has a radiometric age of 1.85 to 1.25 million years, corresponding to the Pleistocene epoch.
Menefee Formation in a road cut through a hogback ridge near Cuba, New Mexico The Menefee Formation is an upper Santonian to lower Campanian geologic formation found in Colorado and New Mexico , United States.