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  2. Point Lookout Sandstone - Wikipedia

    en.wikipedia.org/wiki/Point_Lookout_Sandstone

    The sandstone was first described by A. J. Collier for exposures in cliffs at Point Lookout, in Mesa Verde National Park, Montezuma County, Colorado, in the Paradox Basin, [6] and later described by Allen and Balk in 1954 as part of the Mesaverde Group in the San Juan Basin in New Mexico.

  3. Mesa Verde National Park - Wikipedia

    en.wikipedia.org/wiki/Mesa_Verde_National_Park

    Mesa Verde National Park is an area of federal exclusive jurisdiction. Because of this all law enforcement, emergency medical service, and wildland/structural fire duties are conducted by federal National Park Service Law Enforcement Rangers. The Mesa Verde National Park Post Office has the ZIP code 81330. [145] Access to park facilities vary ...

  4. Cliff House Sandstone - Wikipedia

    en.wikipedia.org/wiki/Cliff_House_Sandstone

    "Geology and fuel resources of the Upper Cretaceous rocks of the Barker Dome-Fruitland area, San Juan County, New Mexico". U.S. Geological Survey Oil and Gas Investigations Map. OM-144. doi:10.3133/om144. Hunt, ReBecca K.; Santucci, Vincent L.; Kenworthy, Jason (2006). "A preliminary inventory of fossil fish from National Park Service units".

  5. You can drive along 700 years of history at Mesa Verde ... - AOL

    www.aol.com/drive-along-700-years-history...

    Can you go inside Mesa Verde? Yes. From Oct. 23 through April 30, the park entrance fee is $20 per private vehicle. From May 1 through Oct. 22, that fee goes up to $30.

  6. Point Lookout (Colorado) - Wikipedia

    en.wikipedia.org/wiki/Point_Lookout_(Colorado)

    Point Lookout is an 8,427-foot (2,569 meter) elevation sandstone summit located in Mesa Verde National Park, in Montezuma County of southwest Colorado. [3] This prominent landmark is situated 2 miles (3.2 km) south of the park entrance, and 9.3 miles (15.0 km) east-southeast of the town of Cortez, and towers 1,600 feet above the surrounding terrain of Mancos Valley.

  7. Menefee Formation - Wikipedia

    en.wikipedia.org/wiki/Menefee_Formation

    The Menefee Formation consists of fluvial sandstone, shale, and coal.Based on ammonite biostratigraphy, the age of the Menefee Formation can be constrained to 84.2-79 million years (), based on the presence of Baculites perplexus in the overlying Cliff House Sandstone, and ammonites from the late Santonian in the underlying Point Lookout Sandstone.

  8. Hovenweep National Monument - Wikipedia

    en.wikipedia.org/wiki/Hovenweep_National_Monument

    Most of the pueblo building was conducted, about the same time as the Mesa Verde cliff dwellings, between 1230 and 1275 [3] [17] when there were about 2,500 residents. [9] The Hovenweep architecture and pottery was like that of Mesa Verde. [11] Pueblo III Era – 1150–1350 The Hovenweep inhabitants completed construction over a period of time.

  9. Cliff Palace - Wikipedia

    en.wikipedia.org/wiki/Cliff_Palace

    A large square tower is to the right and almost reaches the cave "roof". It was in ruins by the 1800s. The National Park Service carefully restored it to its approximate height and stature, making it one of the most memorable buildings in Cliff Palace. It is the tallest structure at Mesa Verde standing at 26 feet (7.9 m) tall, with four levels.

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