|
Sagebrush bark sandal from Catlow Cave, radiocarbon dated to 9,300 years old |
In 1938 archaeologist Luther Cressman (from the University of Oregon) excavated at Fort Rock
Cave, located in a small volcanic butte approximately half a mile west of the Fort Rock volcanic crater in
central Oregon. The Fort Rock Basin is the most northwesterly sub-basin of the
Great Basin, Western North America's vast intermontane desert.
Cressman found dozens of sandals below a layer of volcanic ash, subsequently determined to come from the eruption of the Mt. Mazama volcano 7500 years ago. Named for the site where they were first found, Fort Rock-style sandals have since been reported from ancient deposits in several Northern Great Basin caves.
Sagebrush bark sandals from Fort Rock Cave, similar to specimens radiocarbon dated from 10,500-9,300 years old. |
Fort Rock sandals are stylistically distinct. They are twined (pairs of weft
fibers twisted around warps), and have a flat, close-twined sole, usually with
five rope warps. Twining proceeded from the heel to the toe, where the warps
were subdivided into finer warps and turned back toward the heel. These fine
warps were then open-twined (with spaces between the weft rows) to make a toe
flap. Cressman surmised that a tie rope attached to one edge of the sole
wrapped around the ankle and fastened to the opposite edge.
Most dated Fort Rock-style sandals are from Fort Rock Cave, but directly
dated sandals of this type are also known from Cougar Mountain and Catlow
Caves. Directly dated Fort Rock style sandals range in age from at least 10,500
BP to 9200 BP (based on dendrocalibrated radiocarbon ages). For more
information, refer to Connolly and Cannon 1999.
Table 1. Directly dated Fort Rock-style sandals, northern Great Basin.
14C Age |
Lab No. |
Age Range (cal BP, 1 sigma) |
Dated Material |
Site |
Reference(s) |
9188±480* |
C-428a |
10,920-9650 BP |
sagebrush bark |
Fort Rock Cave |
Arnold and Libby 1951 |
8916±540* |
C-428b |
10,440-9380 BP |
sagebrush bark |
Fort Rock Cave |
Cressman 1951; Bedwell and Cressman 1971 |
8308±43 |
AA-30056 |
9380-9240 BP |
sagebrush bark |
Catlow Cave |
Connolly and Cannon 1999 |
8510±250 |
UCLA-112 |
9840-9240 BP |
tule |
Cougar Mtn. Cave |
Ferguson and Libby 1962; Connolly 1994 |
8500±140 |
I-1917 |
9530-9380 BP |
sagebrush bark |
Fort Rock Cave |
Bedwell and Cressman 1971 |
9215±140 |
AA-9249 |
10,360-10,020 BP |
sagebrush bark |
Fort Rock Cave? |
Connolly and Cannon 1999 |
8715±105 |
AA-9250 |
9870-9520 BP |
sagebrush bark |
Fort Rock Cave? |
Connolly and Cannon 1999 |
Note: *The commonly cited
9053±350 age for the "Fort Rock sandal" is actually an average of
these two dates, run on "several pairs of woven rope sandals" (Arnold
and Libby 1951:117). The weighted average of these two ages produces an age range
of 10,390-9650 cal BP.
Russian page translation by Alisa Bagrii alisa.bagrii@everycloudtech.com
References
·
Arnold, J. R. and W. F.
Libby
1951 Radiocarbon Dates. Science 113(2927):111-120.
·
Bedwell, Stephen F. and
Luther S. Cressman
1971 Fort Rock Report: Prehistory and Environment of the Pluvial Fort Rock Lake
Area of South-Central Oregon. In Great Basin Anthropological Conference
1970: Selected Papers, edited by C. Melvin Aikens, pp. 1-25. University of
Oregon Anthropological Papers 1. Eugene
·
Connolly, Thomas J. and
William J. Cannon
1999 Comments on "America's Oldest Basketry." Radiocarbon 41(3):309-313.
·
Cressman, Luther S.
1951 Western Prehistory in the Light of Carbon 14 Dating. Southwestern
Journal of Anthropology 7(3):289-313.
·
Cressman, Luther S.
1942 Archaeological Researches in the Northern Great Basin. Carnegie
Institution of Washingon Publication 538. Washington, D. C.
·
Ferguson, G. J. and W.
F. Libby
1962 UCLA Radiocarbon Dates. Radiocarbon 4:109-114.
Page design/contact: Tom Connolly