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Plains Indian Studies - Smithsonian Institution Libraries

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NUMBER 30<br />

hunting and fishing camps is from A.D. 810±100<br />

to 1495±90. Further, the lodge floor area of the<br />

six Glen Elder houses excavated by Krause (Lippincott,<br />

1976:118a) averages 732 square feet (68<br />

m^) and ranges from 482 to 909 square feet (45<br />

to 84 m^), slightly more than twice the maximum<br />

size cited by Krause for isolated households (i.e.,<br />

144 to 225 square feet, or 13 to 21 m^) in floor<br />

area. The increased size brings the lodges more in<br />

line with the range of Central <strong>Plains</strong> lodges<br />

known from other areas, and corresponds to<br />

Wedel's (1970:18) comment regarding the exceptionally<br />

small lodges described by Krause in his<br />

model: "I have the impression that houses as<br />

small as those of the second Solomon River settlement<br />

type are not characteristic of the Nebraska<br />

Upper Republican communities as these<br />

are now known where large scale excavations<br />

have been carried out." As a result of his research,<br />

Lippincott (1978:87) concluded:<br />

A realistic interpretation of both radiocarbon and seriation<br />

information would be to split the occupation of the Solomon<br />

River locality into a period of relatively intense occupation<br />

from A.D. 800-850 through A.D. 1200-1250 and a period of<br />

drastic reduction of occupation density after 1200-1250.<br />

Systematic analysis of the Glen Elder materials<br />

by Lippincott clearly demonstrates that Krause's<br />

model was only loosely tied to the available data<br />

and that alternative interpretations are equally<br />

viable. Nevertheless, several of the hypotheses<br />

proposed by Krause and incorporated into subsequent<br />

models provide the basis for additional<br />

research. All of the examined models assume<br />

continuous occupation of a locality for a substantial<br />

time period, usually 400 years (A.D. 900-<br />

1300). This span of occupation is established from<br />

a few radiocarbon dates. A shift in occupation<br />

from large lodges in hamlets to small isolated<br />

lodges or some variation is also a common theme<br />

of the models. Generally, all of the proposed<br />

models have been handicapped by the paucity of<br />

available radiocarbon dates from the localities.<br />

For example, when Roper (1976) prepared her<br />

radiocarbon study for the Central <strong>Plains</strong>, only 33<br />

dates were available for the entire Nebraska<br />

phase.<br />

Forty-one radiocarbon dates have been ob­<br />

185<br />

tained for the Glenwood locality, and these dates<br />

provide the basis for several observations regarding<br />

radiocarbon samples, time, span of occupation,<br />

and the relationships of large and small<br />

lodges in Glenwood.<br />

The Glenwood Temporal Sequence<br />

In developing their model of the Glenwood<br />

settlement sequence, Anderson and Zimmerman<br />

(1976) estimated a span of occupation based upon<br />

10 radiocarbon dates ranging from A.D. 430±100<br />

to 1280±70. Six of the samples were paired and<br />

represented three lodges. Gross intralodge differences<br />

between radiocarbon dates seriously compromised<br />

the reliability of these paired samples<br />

as accurate temporal indicators. For example, two<br />

dates from 13ML119, a Pony Creek lodge, were<br />

both early (A.D. 885±105 and 920±130) and consistent.<br />

But the dates from 13ML121, a Keg Creek<br />

house, were A.D. 870±95 and 1260±100, a difference<br />

of 390 years, and two samples from<br />

13ML124 were dated A.D. 430± 100 and 1215±95.<br />

The inability to obtain reasonable sample agreement<br />

within a lodge seriously compromised any<br />

estimate of span of occupation, and established a<br />

clear need for carefully controlled, multiple-lodge<br />

samples from the locality.<br />

As a direct result of the Highway-34 excavations<br />

and the continuing research of the author,<br />

31 additional radiocarbon dates were obtained<br />

from the Glenwood locality. An initial requirement<br />

of three radiocarbon dates per lodge was<br />

established. Samples were selected from wall<br />

posts, and the charcoal was identified to genus or<br />

species by Dr. Dwight Bensend, Iowa State University.<br />

Every attempt was made to control possible<br />

sources of error, from the field collecting<br />

stage through laboratory processing. The first set<br />

of three dates from lodge 13ML130 was processed<br />

commercially and sample agreement was encouraging.<br />

The remainder of the samples was processed<br />

at the Center for Climatic Research, University<br />

of Wisconsin, Madison.<br />

The initial selection of charcoal from the bottom<br />

of lodge wall posts served three purposes.<br />

First, the relatively small diameter of the post

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