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2009-08-24_REVISION - C1982056 (4)
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2009-08-24_REVISION - C1982056 (4)
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Entry Properties
Last modified
8/24/2016 3:55:01 PM
Creation date
8/25/2009 1:24:41 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Revision
Doc Date
8/24/2009
Doc Name
Sage Creek Subsidence Project Cultural Resources Inventory
From
MAC Metcalf Archaeological Consultants, Inc
To
BLM
Type & Sequence
PR8
Email Name
JHB
Media Type
D
Archive
No
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Overall, the Yampa valley data set has done little to resolve this poorly described cultural period, <br />but data are accumulating from recent work. <br />Aspen Tradition. The Aspen Tradition/Uinta Phase is characterized by a substantial <br />increase in the number and visibility of archaeological components across the region. The period <br />begins about 1950 BP and ends at 650 BP. Full-scale adoption of the bow-and-arrow, use of small <br />corner-notched points, the introduction of some locally made gray and brown ware ceramics, <br />frequent use of pit features, and evidence of resource use intensification in the form of seed and root <br />processing technologies are all characteristics of the cultural period (Metcalf 1987; Smith 1988; <br />Thompson and Pastor 1995; Reed and Metcalf 1999). This pattern shows up in Sage Creek area, <br />specifically at Red Army (Pool 1997) and in a number of surface sites. Small basin houses are <br />recognized in some sites in the region, and the period is regarded as the final fluorescence of the <br />Western Wyoming Adaptation Type (McNees 1999). While the number of excavated components <br />is relatively higher than for the Archaic Era region-wide, Aspen Tradition components are less <br />numerous than in the Archaic Era in the Yampa valley. Drying about 1000 BP may have strained <br />the Aspen Tradition but perhaps not severely enough to change the cultural adaptation. Certainly <br />the drop in the number of dated occupations after about 700 BP strongly reflects a change in <br />adaptation. <br />Antero Phase. The Antero Phase (650 BP - 300 BP), is marked by the replacement of small <br />corner-notched points by side and tri-notched forms (Desert Side-Notched), by the introduction of <br />Ute Uncompahgre brown or Shoshone Intermountain pottery, by increased mobility, and less <br />reliance on storage (Reed and Metcalf 1999:153). Considerably fewer pit features are apparent in <br />the record and there is a shift in land-use patterns from open basin dunal environments in favor of <br />wooded uplands and wet drainages. Within the cultural period, the transition to the Protohistoric <br />Era is signaled by the introduction of a small amount of European trade goods. <br />Evidence for intensive use of the interior basins and sand dune environments decreases in <br />this period. In the Unita Basin Lateral data there is a distinct trend for Desert Side-Notched points <br />to be found in upland locations where juniper or pinon juniper dominates, or at sites immediately <br />along wet drainages. This shift in preferred site locations supports the notion that a major shift in <br />settlement/subsistence took place between the Aspen Tradition and the Antero Phase. In the <br />American Southwest, widespread abandonment of settled villages and emigration of Puebloan <br />peoples occurred at this time period (e.g., Lipe et al. 1999). A similar shift in adaptive patterns is <br />seen in the Northern Colorado River Basin and Wyoming Basin, manifested by the replacement of <br />a basin-oriented processing-intensive pattern, by a more mobile, upland-oriented pattern. <br />Canalla Phase. The'Canalla Phase/Protohistoric Period is essentially a continuation of the <br />latest prehistoric period with the addition of trade goods. Sites of this age have not been investigated <br />in or near the Sage Creek area. <br />Current Research Directions. Current research in the Yampa valley area is focused on <br />exploring models integrating data on climate change with an expanding data base about the cultural <br />sequences (e.g. Reed et al. 2005; Metcalf 2005). For example, how did major and minor climatic <br />shifts effect prehistoric adaptations and use patterns? Did abrupt climatic shifts raise periodic <br />millennial-scale havoc with local subsistence systems forcing measurable adaptive shifts? Within <br />the region, there appears to have been five broad cultural adaptations characterized as Nomadic Big <br />7
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