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1 References  





2 Further reading  





3 External links  














Ventana Cave






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Coordinates: 32°21N 112°14W / 32.350°N 112.233°W / 32.350; -112.233
 

From Wikipedia, the free encyclopedia
 


Ventana Cave

U.S. National Register of Historic Places

U.S. National Historic Landmark

Ventana Cave
Ventana Cave is located in Arizona
Ventana Cave

Ventana Cave is located in the United States
Ventana Cave

LocationPima County, Arizona, United States
Nearest citySanta Rosa, Arizona
Coordinates32°21′N 112°14′W / 32.350°N 112.233°W / 32.350; -112.233
NRHP reference No.66000189
Significant dates
Added to NRHPOctober 15, 1966[1]
Designated NHLJanuary 20, 1964[2]

Ventana Cave (O'odham: Nakaijegel) is an archaeological site in southern Arizona. It is located on the Tohono O'odham Indian Reservation. The cave was excavated under the direction of Emil Haury by teams led by Julian Hayden in 1942, and in 1941 by a team led by Wilfrid C Bailey, one of Emil Haury's graduate students.[3] The deepest artifacts from Ventana Cave were recovered from a layer of volcanic debris that also contained Pleistocene horse, Burden's pronghorn, tapir, sloth, and other extinct and modern species. A projectile point from the volcanic debris layer was compared to the Folsom Tradition and later to the Clovis culture, but the assemblage was peculiar enough to warrant a separate name – the Ventana Complex. Radiocarbon dates from the volcanic debris layer indicated an age of about 11,300 BP.[4]

Bruce Huckell and C. Vance Haynes restudied the Ventana Cave stratigraphy and artifact assemblage in 1992-1994. New radiocarbon dates and reanalysis of the artifacts indicates that the volcanic debris layer was laid down between 10,500-8,800 BP. Huckel and Haynes hypothesized that vertical turbation (postdepositional disturbance) is responsible for Haury's original interpretation that these extinct fauna were killed with stone tools. "This turbation may have led to the incorporation of bones of extinct fauna from an underlying conglomerate deposit rich in horse remains, creating the impression of their association with artifacts". Huckel and Haynes believe the Ventana Complex is post-Clovis, and not closely related.[5]

Ventana Cave was declared a National Historic Landmark in 1964.[2]

References

[edit]
  1. ^ "National Register Information System". National Register of Historic Places. National Park Service. January 23, 2007.
  • ^ a b "Ventana Cave". National Historic Landmark summary listing. National Park Service. Retrieved September 27, 2007.
  • ^ Haury, Emil (1943). "The Stratigraphy of Ventana Cave, Arizona". American Antiquity. 8 (3): 218–223. doi:10.2307/275901. JSTOR 275901.
  • ^ Emil Haury at Ventana Cave, Department of Anthropology, University of Arizona
  • ^ Bruce B. Huckell and C. Vance Haynes, Jr., 2003, The Ventana Complex: New Dates and New Ideas on Its Place in Early Holocene Western Prehistory, American Antiquity, Vol. 68, No. 2 (Apr., 2003), pp. 353-371 Abstract
  • Further reading

    [edit]
    [edit]
    Retrieved from "https://en.wikipedia.org/w/index.php?title=Ventana_Cave&oldid=1169591098"

    Categories: 
    Archaeological sites on the National Register of Historic Places in Arizona
    Caves of Arizona
    National Historic Landmarks in Arizona
    Cenozoic paleontological sites of North America
    Landforms of Pima County, Arizona
    History of Pima County, Arizona
    Paleontology in Arizona
    National Register of Historic Places in Pima County, Arizona
    Fossil parks in the United States
    Tohono O'odham Nation
    Hidden categories: 
    Pages using gadget WikiMiniAtlas
    Articles using NRISref without a reference number
    Articles with short description
    Short description is different from Wikidata
    Use mdy dates from August 2023
    Coordinates on Wikidata
    Articles containing O'odham-language text
    Articles with J9U identifiers
    Articles with LCCN identifiers
     



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