Bighorn Canyon Archeology: A Reply

Abstract

In a review of Bighorn Canyon Archeology (Husted 1969), Kehoe (1972) resorts to misrepresentation and insinuation in an attempt to discredit a differing point of view. The author reiterates his position and replies to Kehoe’s insinuation of unethical practice.     

The Meander Site (39Lm20L) In Fort Randall Reservoir,South Dakota

Abstract

The Meander Site (39LM20l) is located on the left bank of the White River in Lyman County, South Dakota, about eight miles above the junction of the White and Missouri rivers. Test excavations at the site were conducted in 1953 by Harold A. Hus cher of the Smithsonian Institution, River BasinSurveys. Though few in number, the artifacts recovered indicate the occupation belongs to the Chouteau Aspect. Ceramic analysis suggests the site was occupied at a time somewhat prior to the occupation of the Crazy Bull Site (Frantz 1962).     

The Sister’s Hill Site: A Hell Gap Site In North-Central Wyoming

Abstract

The cultural horizon at the Sister’s Hill Site has produced typical Hell Gap points and a small group of associated artifacts. The radiocarbon date of 9650 ± 250 B. C. is in agreement with late Agate Basin or early post Agate Basin sites in the High Plains. On the basis of the current data, Hell Gap points appear to have developed from Agate Basin styles and seem to be developmental to Alberta, Scottsbluff and Eden types.     

The Gillette Site (39ST23), Oahe Reservoir,South Dakota

Abstract

Fieldwork at the Gillette Site primarily cons is ted of the partial excavation ofthreecircular houses, across section of a fortification ditch, and the removal of a buriaL The latest occupation, Component A, is identified as a manifestation of the Stanley or Snake Butte focus, dating from about 1700 to 1800 A. D. Component B represents a circular house tradition probably belonging to an earlier period in the Coalescent Tradition than does Component A. The limited data from Component C implies a village occupation of an indeterminate cultural affiliation earlier than Component B.     

The Stricker Site

Abstract

The Stricker site is a multi-component habitation area in Big Bend Reservoir, South Dakota. Component A, the latest and most I imited occupation, represents the Dakota from the middle of the 19th century to the present. Component B represents the major occupation by people following the Coalescent Tradition in the form of the Extended Coalescent variant. Component C, a minor occupation, is representative of the Initial variant of the Middle Missouri Tradition. Most of the features and artifacts pertain to Component B. The analysis provides evidence for a transition from the Shannon phase into the Felicia phase     

Notes On Bison In Val Verde County,Texas: Additions To Dillehay

Abstract

Bison remains from deeply stratified deposits at the Castle Canyon Site, an area of southwestern Texas where bison remains are outstandingly rare, date about 1500 B.C.-A.D. 1000. The last bison known in the area died about 1885. It is suggested that environmental conditions in the area may not have changed, and that presence-absence periods might rather reflect changing conditions on the Central or Northern Plains. These data do not alter Dillehay’s conclusions, but present information not available to him.     

A Description of Certain Engraved ar Tif Acts From the utz Oneota Site

Abstract

Engraved objects of various types have been found at the Utz Oneota Site in Saline County, Missouri. A number of these artifacts are described and illustrated in this article, with comparative data from other localities. They indicate a line of cultural contact and/ or trade running northwest and southeast, along the Missouri-Mississippi River System.     

The Sister’s Hill Site And Its Bearing On The Wyoming Postglacial Alluvial Chronology

Abstract

Alluvial sediments exposed at the Sister’s Hill Site near Buffalo, Johnson County, Wyoming shed new light on the stratigraphy of the Ucros s and Kaycee formations and reveal that another stratigraphic unit occurs between these formations in some places. At the Sister’s Hill Site, Hell Gap artifacts occur in the lower part of the new unit and in association with a Carbon-14 date of 9650 B. P.     

Three Human Skeletons From The Pk Burial Sheridan County,Wyoming

Abstract

Fragmentary skeletal material from a burial found near the Big Horn Mountains of north-central Wyoming was determined to constitute the remains of three individuals. The few artifacts in association provide little basis for an assessment of cultural affiliation, however, cranial characteristics suggest a close relationship to previously studied Siouan populations.

In February, 1962 Mr. Donald C. Grey of Sheridan, Wyoming submitted skeletal material recovered from the PK Burial Site in Sheridan County, Wyoming to Dr. William M. Bass for identification. Assistance in the analysis of the material was given by Mr. Donald C. Lacy, a graduate studentinphysicalanthropology. According to Mr. Grey (personal communication February 14, 1962), the PK Burial Site was discovered during the summer of 19 59 by a University of Illinois geology student, a member of a summer field crew based at Sheridan College, Sheridan, Wyoming. He discovered a human skull (See Fig. 1: a, b, and c) exposed in the side of a small hilltop overlooking a rodeo corral on a ranch west of Sheridan. The site is located in the foothills of the Big Horn Mountains.     

T-W-DIamond,a Stone Ring Site in Northern Colorado

Abstract

The T-W-Diamond Site, 4LR200, is a large teepee ring village on the? edge of the High Plains in northern Colorado. Seventeen out of the 47 remaining stone ring areas were excavated or tested by the Colorado State University Archae-ological Field School in 1971. Artifacts, fire hearths and midden materials were scarce but indicated the domestic nature of the structures. Stone and ceramic artifacts indicate cultural affiliations with the Late Prehistoric period as reported at Birdshead Cave, and the Piney Creek sites in Wyoming; and at the Agate Bluff Rock Shelters, and the Dipper Gap site in northern Colorado. Carbon-14 dates of A. D. 1020±230 years and A.D. 1170±220 years support the time of the occupation. A third date of A.D. 400±340 seems improbably early. It is hypothesized that the village was occupied seasonally for a short time by a small group of people, perhaps of Shoshonean affiliation, exploiting a mixedbase subsistence economy.     

The Kobold Site, 24BH406: A Post-Althithermal Record of Buffalo-Jumping for The Northwestern Plains

Abstract

The Kobold Site, 24BH406, contained four components of which the oldest is believed to be an altithermal occupation, Buffalo jumping was not occurring at this time, The other three components produced evidence of buffalo jumping beginning with the early post-altithermal and ending just prior to historic times.     

Wickiup Cave

Abstract

Wickiup Cave, site 24BE601, is located in the Tendoy Mountains of southwestern Montana. The site consists of a log, brush, and rock wickiup built in a huge limestone cave. The wickiupand numerous artifacts found in the cave are attributed to historic Tukudika Shoshone occupation.     

Phillips Spring, 23HI216:

Abstract

The Phillips Spring Site is situated on a Holocene terrace of the Pomme de Terre River in northern Hickory County, Missouri. Eleven. radiocarbon dates provide a good chronologie framework for the four cultural components recognized at the site. There are three Archaic components which span the period 4280 to 1990 BP. The initial Archaic occupation coincides with the establishment of the present vegetation pattern in the area. A single Late Woodland assemblage, dating from 1410 to 1000 BP, is comparable in cultural content to components of the HighlandAspect.     

Low rate of infusional toxicity after expanded cord blood transplantation

Background aimsUmbilical cord blood (CB) is used with increasing frequency to restore hematopoiesis in patients with bone marrow transplant who lack a suitable human leukocyte antigen–matched donor. CB transplantation is limited by low cell doses and delays in neutrophil and platelet engraftment. CB progenitors expanded ex vivo before transplantation provide more rapid hematopoietic and immune reconstitution as well as less engraftment failure compared with unmanipulated CB. However, the safety of infusing double and ex vivo–expanded CB has not been systematically examined.MethodsWe reviewed the immediate adverse events (AE) associated with the infusion of CB occurring within 24 hours in 137 patients enrolled in clinical CB transplant trials at the MD Anderson Cancer Center from February 2004 to May 2010. All patients received an unmanipulated CB unit followed by infusion of a second unmanipulated CB unit or a second CB unit expanded ex vivo with the use of cytokines in a liquid culture system or in mesenchymal stromal cell co-cultures.ResultsA total of three grade 2 and two grade 3 infusion reactions occurred within 24 hours of CB transplantation. This resulted in an AE rate of 3.7%. The majority of AEs manifested as signs of hypertension. No association with patient age, sex, disease status, premedication, ABO compatibility or total infusion volume was observed. In summary, the incidence of infusion-related toxicities in patients who receive unmanipulated and ex vivo–expanded double CB transplantation is low.ConclusionsWe conclude that the infusion of unmanipulated followed by expanded CB products is a safe procedure associated with a low probability of inducing severe reactions.     

The Archaeology Of The Breeden Site

Abstract

The Breeden Site cultural sequence reenforcesthe general culture history already established for the Bad-Cheyenne Region and the more inclusive Middle Missouri Tradition. House remains and the bulk of the ceramic materials from the site indicate habitation of the area by peoples of the Initial Middle Missouri Variant and the PostContact Coalescent Variant.Component A at the Breeden Site and the Monroe and Anderson components at the Dodd Site exhibit a complex of diagnosticcultural traits significant enough to define a new phase - the Anderson Phase. A temporal span of approximately A.D. 950to 1250 is suggested for the phase. Component B of the Breeden Site, an early manifestation of the Post-Contract Coalescent Variant, is closely associated with components of the Felicia Phase and the putative Talking Crow Phase. Breeden Component B probably represents an upriver movement of Coalescent peoples from the Big Bend area, eventually being assimilated into the Arikara populations of the Bad River Phase within the Bad-Cheyenne Region.     

The Bentzen-Little Bald Mountain Site

Abstract

Excavation of a campsite and kill site area situated on a natural animal crossing or saddle between the North Fork of the Tongue River and Beaver Creek just south of Little Bald Mountain, Wyoming, at an elevation of 9,000 feet is described. Among the features found were two firepits containing burned rock, animal bones, and artifacts. The amount of artifacts and animal bones recovered suggested a long and/or intensive occupation, The bones included those of elk and mountain sheep, intermixed with teeth.     

Book Reviews

Book reviewed in this article:
ARCHEOLOGY: Kin Kletso: A Pueblo III Community in Chaco Canyon, New Mexico. G ordon V ivian and T om W. M athews .
ARCHEOLOGY: Tree-Ring Dating of the Archeological Sites in the Chaco Canyon Region, New Mexico. B ryant B annister .
ARCHEOLOGY: Contributions to Mesa Archaeology: II. Site 875, Mesa Verde National Park, Colorado. R obert H. L ister .
ARCHEOLOGY: The Archeological Survey of Wetherill Mesa: Mesa Verde National Park–Colorado. A lden C. H ayes .     

Investigation of the Swift Bird House (39DW233) in the Oahe Reservoir,South Dakota

Abstract

The Swift Bird House (39DW233) is a prehistoric structure of indeterminate characteristics. The associated artifacts are directed to a Northern Plains horticulture and hunting complex. A tenuous relationship to the Anoka Focus and a possible occupation date of about A. D. 1500 is suggested for the site     

Jackson Fall-Leaf: A Multi-Component Occupation Site Inc Northeasternc Oklahoma

Abstract

The Jackson Fall-Leaf site is a deeply buried multi-component occupation site located in the Little Caney River Valley of Northeastern Oklahoma. The site, situated in the Cross Timbers province on the southeastern periphery of the Southern Plains, contains cultural debris from the Woodland and Plains Village periods. Excavation produced a large quantity of chipped stone artifacts and allowed the delineation of an activity area within the site. Typological cross dating, in combination with intensive paleo-environmental research at the site and at other locales in the Copan area, indicates that the site dates from the period between A.D. 500 and A.D. 1300.     

Wedding of the Waters Cave, 48 HO 301, A Stratified Site in the Big Horn Basin of Northern Wyoming

Abstract

During the summer of 1959, the writer investigated several rock shelters at the mouth of the Wind River Canyon, about 3 miles south of Thermopolis, Wyoming. One of the rock shelters proved to be of archaeological value. A test trench revealed nearly 3 feet of stratified cultural deposits. The cultural materials fits well in the sequence for the Northwestern Plains, (Mulloy 1958: 204-223) and should be important in an area little known archaeologically.