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Draft Environmental Impact Statement for Roca Honda Mine

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Chapter 3. Affected Environment and <strong>Environmental</strong> Consequences<br />

Prehistory<br />

The earliest identified human settlement in North America occurs during the Paleoindian period<br />

(10,500–5000 B.C.). Archaeological evidence from this period indicates a nomadic lifestyle with<br />

a subsistence strategy focused on big game hunting. Although Paleoindian groups likely utilized<br />

small game and plant foods in addition to big game, a substantial change in the subsistence<br />

strategy to these food sources marks the transition to the Archaic period (5000 B.C.–A.D. 400).<br />

People during this period were still mobile; however, mobility was more restricted in<br />

geographical extent and cyclical, usually tied to the seasons. Once productive resource<br />

procurement locations were identified, people returned to these locations on a seasonal basis.<br />

Most early (5500–3200 B.C.) and middle (3200–1800 B.C.) Archaic sites appear to be single-use<br />

hunting camps, though grinding tools are encountered at sites, indicating seed and nut processing.<br />

During the late Archaic (1800 B.C. – A.D. 400), major changes were initiated with the acceptance<br />

of horticulture (e.g., maize) into the subsistence strategy and a higher degree of sedentism. In<br />

general, this portion of the Archaic is characterized by a shift from hunting and gathering as the<br />

prime subsistence economy to horticulture, and a much higher site density is noted.<br />

As with most areas of the American Southwest, evidence of Paleoindian people in the region is<br />

sparse. Paleoindian cultural deposits have been found in the Puerco Valley east of Mt. Taylor.<br />

Within the region of the proposed project area, the frequency of Archaic sites increases through<br />

the middle and late Archaic. Evidence <strong>for</strong> Archaic occupation is most common at San Mateo<br />

Mesa (which includes the mine project area), La Jara Mesa, Lobo Canyon, and Grants Canyon<br />

(Benedict and Hudson 2008).<br />

General cultural developments associated with the Basketmaker III period (A.D. 400–800)<br />

include the appearance of settlements consisting of between 1 and 20 pithouse structures (semisubterranean<br />

dwellings), an everincreasing dependence on cultivated crops, and a continued<br />

practice of local plant food gathering and hunting. During the Pueblo I period (A.D. 800–950),<br />

aboveground masonry dwellings are introduced and the number of sites found in flood plains and<br />

along canyon floors, in proximity to agricultural fields, increases. Agricultural practices began to<br />

include unique methods to improve crop production, such as terracing, irrigation, and gridding.<br />

Settlements continued to increase in size and complexity during the Pueblo II (A.D. 950–1100).<br />

There is a trend toward centralization in larger villages, with associated outlying limited-task sites<br />

(such as field houses) where supporting activities were conducted. The increase in residential<br />

density was met with an increase in the importance of agriculture, with the development of<br />

complex systems <strong>for</strong> irrigation and water control, along with further development of terraced<br />

gardens and grid systems.<br />

Population in the region during the Basketmaker and Pueblo I periods continued to be low;<br />

however, settlement in the area increased during the Pueblo II period, particularly in the San<br />

Mateo Valley (near the mine project area). Evidence that this increase in population may be<br />

related to the rise of Chaco Canyon as a major cultural center includes the multiple Chaco-related<br />

outlier sites in the vicinity, including in El Rito Canyon and around the village of San Mateo. The<br />

relationship between the populations in Chaco Canyon and the Mt. Taylor area is firmly<br />

demonstrated by the presence of timber beams from Mt. Taylor in Chaco Canyon structures.<br />

Intensive use of the landscape in the San Mateo Valley is shown by the high density of Pueblo IIera<br />

habitation sites (Benedict and Hudson, 2008).<br />

The Pueblo III period (A.D. 1100–1300) shows a dramatic change from its predecessors, with<br />

movement of populations to areas with permanent water sources. The Pueblo IV period (A.D.<br />

302 DEIS <strong>for</strong> <strong>Roca</strong> <strong>Honda</strong> <strong>Mine</strong>, Cibola National Forest

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