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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 have ...

  3. Paleobiota of the Chinle Formation - Wikipedia

    en.wikipedia.org/wiki/Paleobiota_of_the_Chinle...

    One of the most diverse floral communities is found near Fort Wingate, New Mexico. Paleobotanists have traditionally placed the Fort Wingate plant beds into the Monitor Butte Member , though more recently they are placed within the Bluewater Creek Formation , a subunit of the Chinle Formation first defined in 1989. [ 62 ]

  4. Nazca lines - Wikipedia

    en.wikipedia.org/wiki/Nazca_Lines

    The Nazca lines (/ ˈ n ɑː z k ə /, /-k ɑː / [1]) are a group of geoglyphs made in the soil of the Nazca Desert in southern Peru. [2] They were created between 500 BC and 500 AD by people making depressions or shallow incisions in the desert floor, removing pebbles and leaving different-colored dirt exposed. [ 3 ]

  5. Folsom site - Wikipedia

    en.wikipedia.org/wiki/Folsom_site

    Folsom site or Wild Horse Arroyo, designated by the Smithsonian trinomial 29CX1, is a major archaeological site about 8 miles (13 km) west of Folsom, New Mexico. It is the type site for the Folsom tradition, a Paleo-Indian cultural sequence dating to between 11000 BC and 10000 BC. The Folsom site was excavated in 1926 and found to have been a ...

  6. Bandelier National Monument - Wikipedia

    en.wikipedia.org/wiki/Bandelier_National_Monument

    Bandelier National Monument is a 33,677-acre (136 km 2) United States National Monument near Los Alamos in Sandoval and Los Alamos counties, New Mexico. The monument preserves the homes and territory of the Ancestral Puebloans of a later era in the Southwest. Most of the pueblo structures date to two eras, dating between AD 1150 and 1600.

  7. 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 ...

  8. Old Spanish Trail (trade route) - Wikipedia

    en.wikipedia.org/wiki/Old_Spanish_Trail_(trade...

    The Old Spanish Trail (Spanish: Viejo Sendero Español) is a historical trade route that connected the northern New Mexico settlements of (or near) Santa Fe, New Mexico with those of Los Angeles, California and southern California. Approximately 700 mi (1,100 km) long, the trail ran through areas of high mountains, arid deserts, and deep ...

  9. Jemez Mountains - Wikipedia

    en.wikipedia.org/wiki/Jemez_Mountains

    Topo map. USGS Polvadera Peak (1977) The Jemez Mountains (/ ˈheɪmɛz /, Tewa: Tsąmpiye'ip'įn, Navajo: Dził Łizhinii) are a group of mountains in Rio Arriba, Sandoval, and Los Alamos counties, New Mexico, United States. Numerous Puebloan Indian tribes have lived in the Jemez Mountains region for centuries before the Spanish arrived in New ...

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