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  2. Paleontology in New Mexico - Wikipedia

    en.wikipedia.org/wiki/Paleontology_in_New_Mexico

    The location of the state of New Mexico. Paleontology in New Mexico refers to paleontological research occurring within or conducted by people from the U.S. state of New Mexico. The fossil record of New Mexico is exceptionally complete and spans almost the entire stratigraphic column. [ 1] More than 3,300 different kinds of fossil organisms ...

  3. Western Interior Seaway - Wikipedia

    en.wikipedia.org/wiki/Western_Interior_Seaway

    The ancient sea, which existed from the early Late Cretaceous (100 Ma) to the earliest Paleocene (66 Ma), connected the Gulf of Mexico to the Arctic Ocean. The two land masses it created were Laramidia to the west and Appalachia to the east. At its largest extent, it was 2,500 feet (760 m) deep, 600 miles (970 km) wide and over 2,000 miles ...

  4. List of the prehistoric life of New Mexico - Wikipedia

    en.wikipedia.org/wiki/List_of_the_prehistoric...

    Life restoration of a herd of Mammuthus columbi, or Columbian mammoths. The extent of the fur depicted is hypothetical. Charles R. Knight (1909). Life restoration of a herd of Neohipparion. Robert Bruce Horsfall (1913). Restoration of a herd of alarmed Miocene-Pleistocene peccaries of the genus Platygonus.

  5. El Malpais National Monument - Wikipedia

    en.wikipedia.org/wiki/El_Malpais_National_Monument

    El Malpais National Monument and National Conservation Area. El Malpais National Monument is a National Monument located in western New Mexico, in the Southwestern United States. [3] The name El Malpais is from the Spanish term Malpaís, meaning badlands, due to the extremely barren and dramatic volcanic field that covers much of the park's area.

  6. Geology of New Mexico - Wikipedia

    en.wikipedia.org/wiki/Geology_of_New_Mexico

    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]

  7. Puye Cliff Dwellings - Wikipedia

    en.wikipedia.org/wiki/Puye_Cliff_Dwellings

    The Puye Cliff Dwellings are the ruins of an abandoned pueblo, located in Santa Clara Canyon on Santa Clara Pueblo Reservation land near Española, New Mexico.Established in the late 1200s or early 1300s and abandoned by about 1600, this is among the largest of the prehistoric Indian settlements on the Pajarito Plateau, showing a variety of architectural forms and building techniques.

  8. Sandia Mountains - Wikipedia

    en.wikipedia.org/wiki/Sandia_Mountains

    The Sandia Mountains are the most visited range in New Mexico. Numerous hiking trails exist on both sides of the range, such as the popular La Luz Trail and Crest Trail. Much of the west side of the range is included in the Sandia Mountain Wilderness; the trails on that side are steeper, and water is very scarce. Numerous picnic and recreation ...

  9. Capitan Formation - Wikipedia

    en.wikipedia.org/wiki/Capitan_Formation

    Capitan Reef in Guadalupe Mountains National Park. The Capitan Formation is a geologic formation found in western Texas and southeastern New Mexico. It is a fossilized reef dating to the Guadalupian Age of the Permian period . The formation underlies El Capitan in Guadalupe Mountains National Park, [ 1] and the formation and its associated ...