Plains Indian Studies - Smithsonian Institution Libraries
Plains Indian Studies - Smithsonian Institution Libraries
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