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Appendix I. Cultural Resource Regional Ethnohistory I-30 subperiod extends into and through the subsequent Middle Archaic (Neusius and Gross 2007). During the Middle Archaic, an increase in the amount of local obsidian in archaeological sites is thought to indicate a decrease in mobility during this period. In southwestern Great Basin the Gypsum Period developed in a climate that was moister, leading to the filling of some desert lakes and extensive marshlands. This was a time of intensive occupation in the Mojave Desert and diversification of subsistence activities. The area east of Barstow in the Mojave Desert has yielded important archaeological sites that have provided data leading to greater understanding of this period. Split-twig figurines are an interesting artifact found in northern Arizona, Nevada, Utah, and California. Made of split twigs, the figurines are of stylized quadrupeds thought to be used in hunting rituals. Rock art depicting quadrupeds and found in the same regions are also thought to be a part of such rituals. The Coso Range is well known for such depictions (Neusius and Gross 2007). As noted above, the Black Rock subperiod continued from the Early Archaic through the Late Archaic in eastern Great basin. The bow and arrow was introduced in this region during the Middle Archaic years of this period. By the end of this period the region had returned to more moist conditions (Neusius and Gross 2007). Once the Late Archaic commenced the climate had returned to more arid conditions. In southwestern Great Basin the Saratoga Springs (1500 – 800 BP) and Shoshonean Periods (800 BP – contact) developed. The Saratoga Springs Period is similar to the earlier Gypsum Period, but with smaller projectile points. Thisisthoughttoindicatetheintroductionofthebowandarrowinthe region. Various parts of the southwestern Great Basin exhibit influences from their neighboring culture regions during this time. One of the more notable interactions occurred in southern Nevada and southeastern California with the Southwestern Anasazi. Influence of the Anasazi is seen in pottery of the Mojave Desert. Evidence of their physical presence in the region between 1300 and 1100 BP has been found at the turquoise mines of Halloran Spring which were then used by the Hakataya of the Southwest and then the Southern Paiute of the Great Basin (Neusius and Gross 2007). The Shoshonean Period is marked by the introduction of Desert Side Notched points and brownware pottery. This would be concurrent with the end of the Anasazi occupation of southern Nevada. Trade with coastal people becomes evident. Many Antelope Valley and upper Mojave River village sites appear to have been positioned along trade routes and played a major role in the movement of goods. The Shoshonean Period also marks the spread of Numic speakers out of the southwestern Great Basin. However, there is debate as to whether the Late Archaic Shoshoneans are the same as the Numic-speakers that occupied almost all of the Great Basin at the time of European contact. Draft PEIS for Geothermal Leasing in the Western US May 2008PDF Image | STATE OF THE TRIBAL LANDS FOR GEOTHERMAL RESOURCES
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