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Idaho National Laboratory Cultural Resource Management Plan

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Data Requirements: Especially important to answering this question would be sites that are covered<br />

by volcanic flows. Since the presence of these features would not be detectable during survey, this kind of<br />

site would only be encountered during construction activities. Most post-eruption sites are recorded<br />

during survey, and those with subsurface deposits can tell us much about the human use of the area.<br />

Problem Domain: Environment<br />

The reconstruction of the environment is critical for interpreting human behavior. Humans usually<br />

respond adequately to climatic changes by adjusting their subsistence organization and/or technology to<br />

suit their changing needs. We know much about global climatic patterns, but little about the local effects<br />

of the constantly changing moisture and temperature cycles. Research concerning environmental<br />

reconstruction can be conducted at both archaeological sites and other sites where the proper data are<br />

preserved. Cave sites (e.g., lava tubes) with long depositional sequences are especially important because<br />

they often contain the remains of rodents and other small animals that are sensitive to climatic change.<br />

Caves also often trap pollen grains from plants growing in the area and from those brought to the site by<br />

prehistoric inhabitants. A climatic sequence based on a 2000-year cycle has been proposed (Butler 1978)<br />

based on cycles of small mammals recovered during the excavation of Owl Cave at the Wasden Site<br />

located just south of INL. In many ways, it correlates well with interpreted world climatic cycles (Denton<br />

and Karlen 1973).<br />

Of particular interest is that projectile point styles always change during interstadials and persist<br />

through the following stadial. Theoretically, the carrying capacity of a desert area like INL should<br />

decrease during the interstadials, which were generally warmer and dryer, thus stressing the human<br />

populations who rely on the natural resources. However, our present understanding of the climatic cycle<br />

is poor at best, and if we are to make interpretations about the meaning of artifact style changes, as well as<br />

subsistence and demographic changes, we must pursue environmental data as it applies to the local<br />

situation. INL sites have a tremendous potential for contributing to this understanding.<br />

Research Topic: Pleistocene Environments. We know that numerous species of animals became<br />

extinct near the end of the Pleistocene. The changing environment must have had a dramatic effect on the<br />

lifeway of people inhabiting the upper Snake River Basin. It is not known whether the adjustments that<br />

people had to make were slow, involving very slight changes over multiple generations, or dramatic,<br />

necessitating a single generation of inhabitants to make significant shifts in the lifeway.<br />

Research Question—How quickly did the Pleistocene megafauna become extinct?<br />

Data Requirements: Pleistocene sites with buried cultural deposits.<br />

Research Topic: Holocene Environments. Since the end of the Pleistocene the Snake River Plain<br />

has probably been much like it is now. There were wetter and dryer periods, resulting in the increase and<br />

decrease of pluvial lakes that temporarily supported animal and human populations. The history of the<br />

pluvial lakes at INL would provide a scale by which to interpret much of the habitation there. Occupation<br />

when water was not available is likely to be of a very different kind than when water was plentiful.<br />

Research Question—What is the sequence of pluvial lake increase and decrease?<br />

Some information is already known about this history, but much of the detail has not been studied. If<br />

we are to understand the human occupation of the area, we must know more about this sequence.<br />

Data Requirements: Playa-edge sites, with or without cultural material, which contain datable<br />

deposits due to flooding and desiccation.<br />

Problem Domain: Technology and Material Culture<br />

Aboriginal technology evolved over the 12,000+ years of occupation of the upper Snake River Basin.<br />

This is best recorded in stone tool manufacturing because stone is not perishable and the remains of all<br />

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