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Idaho National Laboratory Cultural Resource Management Plan

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INL (Marler 2004; Reed et al. 1987a, 1987b).<br />

Birch Creek points were found in direct<br />

association with a series of 8000-year-old bison<br />

kills at the Wasden site and Owl Cave (Butler<br />

1978, 1986; Miller 1982) and at Bison Rockshelter<br />

and Veratic Rockshelter in the Birch Creek valley<br />

(Swanson 1972). Evidence from all locations,<br />

dated or not, suggest that the people who used<br />

these points were relying heavily on animal<br />

species such as bison and mountain sheep, which<br />

survived the transition from the Pleistocene to the<br />

Holocene epoch.<br />

Middle Prehistoric Period: 8000 to<br />

1300 B.P.<br />

The close of the early prehistoric period and<br />

the beginning of the middle prehistoric period was<br />

marked by a major change in projectile point<br />

structure and form, probably corresponding to a<br />

major shift in hunting technology. Large spear<br />

points characteristic of the earlier period were<br />

almost entirely replaced by smaller notched and<br />

stemmed forms. This transition probably<br />

represents the adoption of an atlatl (i.e., spear<br />

thrower) technology, which may have been more<br />

effective in exploiting newly evolved species that<br />

survived the Pleistocene-Holocene transition. The<br />

presence of ground stone in middle prehistoric<br />

contexts at some sites such as Wilson Butte Cave<br />

(Gruhn 1961) and the Birch Creek Rockshelters<br />

(Swanson 1972) also suggests that plant foods<br />

such as camas may have gained increased<br />

importance during this time. However, available<br />

evidence suggests that hunting remained a<br />

dominant economic endeavor. Thus, the middle<br />

prehistoric period on the eastern Snake River Plain<br />

was marked by some changes in lifestyle, but it<br />

did not represent a major break from the previous<br />

early prehistoric period.<br />

The environment during the middle prehistoric<br />

period was one of transition. A general warming<br />

trend continued, reaching a point of maximum<br />

warmth and dryness at approximately 3800 B.P.<br />

(Currey and James 1982), but available evidence<br />

seems to indicate that these conditions did not<br />

produce dramatic environmental changes in the<br />

area. Pleistocene Lake Terreton probably declined<br />

to its present seasonally marshy state, and the<br />

internal playas held little, if any, standing water.<br />

However, pollen profiles indicate that modern<br />

xeric (i.e., dry) vegetation was present throughout<br />

the interval (Davis and Bright 1983). This<br />

essentially modern habitat supported many<br />

animals that were of economic importance to<br />

human populations, including modern bison and<br />

antelope on the grasslands and mountain sheep,<br />

elk, and deer in the higher elevations.<br />

Middle prehistoric projectile point forms<br />

suggest that this was a time of some cultural<br />

reorganization and mobility. The archaeological<br />

record reflects this in a proliferation of point<br />

styles, which appear to have correlates in both the<br />

northwestern plains and the Great Basin. It appears<br />

that people from these surrounding areas were<br />

moving in and out of the eastern Snake River<br />

Plain, perhaps in response to deteriorating<br />

environmental conditions (Benedict 1979; Madsen<br />

1982).<br />

The diagnostic time markers of the initial<br />

portion of the middle prehistoric period are<br />

Bitterroot or Northern Side-Notched points<br />

(Greiser 1984; Gruhn 1961; Swanson 1972) and<br />

sporadic stemmed-indented base points that<br />

resemble the Pinto series of the Great Basin<br />

(Holmer 1986a). Both forms occur in prehistoric<br />

contexts ranging from 8000 to 6000 B.P. at sites<br />

such as the Birch Creek Rockshelters (Swanson<br />

1972) and further south at Weston Canyon<br />

Rockshelter (Miller 1972). At both of these sites,<br />

mountain sheep appear to have been the preferred<br />

prey in an economy that continued to be focused<br />

on the acquisition of game animals.<br />

Between approximately 6000 and 3500 B.P.,<br />

large side-notched points decreased in frequency,<br />

and around 5000 B.P., stemmed-indented base<br />

points became the dominant style of dart in the<br />

region. Large corner-notched varieties and new<br />

small lanceolate forms also made their first<br />

appearance around 4000 B.P., but did not become<br />

dominant until later (see Figure 11). Once again,<br />

mountain sheep and bison appear to have been the<br />

favored game.<br />

19

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