Idaho National Laboratory Cultural Resource Management Plan
Idaho National Laboratory Cultural Resource Management Plan
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 />
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