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Sandia Cave : ウィキペディア英語版
Sandia Cave

Sandia Cave is an archaeological site near Bernalillo, New Mexico, within Cibola National Forest, that is open to the public. It is rather difficult to reach, as it is located high up on the steep wall of Las Huertas Canyon on the north end of the Sandia Mountains.〔(【引用サイトリンク】url=http://www.showcaves.com/english/usa/caves/Sandia.html )
A statement of its significance in 1961 read:
A recent condition report is:
It was declared a National Historic Landmark in 1961.〔〔Note: A National Register of Historic Places Inventory-Nomination document should be available upon request from the National Park Service for this site, but it appears not to be available on-line from the (NPS Focus search site ).〕
==History==
Archaeologists argued about claims associated with this site for decades, making it difficult to determine its importance.〔Preston, Douglas. 1995. The mystery of Sandia Cave. New Yorker 71:66-72.〕 The site was excavated in the 1930s and 1940s by Frank Hibben while at the University of New Mexico〔Hibben, F. C. 1937. Association of man with Pleistocene mammals in the Sandia Mountains, New Mexico. American Antiquity 2:260-263.〕〔Hibben, F. C. 1941. Evidences of early occupation in Sandia Cave, New Mexico, and other sites in the Sandia-Manzano region. With appendix on correlation of the deposits of Sandia Cave, New Mexico, with the glacial chronology. Smithsonian Miscellaneous Collections 99(23).〕
Both Folsom and Sandia hunting points were recovered, with the hitherto unknown Sandia points interpreted by Hibben as being much older than any other evidence of man in North America. Faunal remains included extinct, Pleistocene mammals.〔 Later study of stratigraphy and radiometric dates corrected serious earlier misinterpretations, leaving "Sandia Man" as definitely younger than earlier claimed.〔Haynes, C. V., Jr., and G. A. Agogino. 1986. Geochronology of Sandia Cave. Smithsonian Contributions to Anthropology 32:1-32.〕
Faunal remains recovered by Hibben and others include such extinct forms as mammoth, mastodon, sloth, horses, and camels, as well as many mammal and bird species that survived the end of the Pleistocene, making this one of the most important Pleistocene paleontological sites in northern New Mexico.〔http://www.utep.edu/leb/pleistNM/sites/sandiacave.htm〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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