Late Archaic |
The Late Archaic component consists primarily of one large, nearly 6-m diameter lens of burned rock with a shallow central basin. Resting on a stable surface and largely intact, this large buried feature had poorly defined margins of scattered burned rock and had been disturbed during backhoe trenching during Phase I. The feature is interpreted as an incipient, or early stage, burned rock cooking oven. Had this cooking spot been used over and over again, it might eventually have become a larger, more massive burned rock mound, or midden. Four small rock clusters identified within the boundaries of the oven feature represented the dump areas, where the Late Archaic cooks discarded burned rock that had become too small and fractured to retain sufficient heat for cooking. Plant remains from the feature included a few burned prickly pear seeds, a burned mesquite seed, burned walnut shell, and burned agave leaf fragments. Though sparse, these materials suggest the oven was used for the preparation of bulk plant foods that require lengthy cooking. This interpretation also is supported by lipid residues, or fatty acids, indicative of high-fat plants which were extracted from the burned rocks. Beyond the ill-defined boundaries of the large burned rock feature, the Late Archaic period occupation area was somewhat difficult to discern. Material immediately around and within the burned rock feature was relatively limited in quantity, but included sparse lithic debris (roughly 1800 pieces) from stone tool-making, a few mussel shell fragments, five other isolated burned rock clusters, some scattered burned rocks, and a small number of chipped-stone tools. Identified dart point styles associated with this burned rock include Frio, Marcos, Ensor, Castroville, and Edgewood. Although these types frequently are associated with bison hunting, bison bones were not present in this camp. The different projectile point types may indicate different groups of people with different backgrounds gathered to conduct bulk processing of a targeted plant food and resharpen or otherwise rejuvenate their chipped-stone tools. The component was radiocarbon dated by 11 accepted dates to a 600-year period between 1700 and 2310 B.P. Middle ArchaicThe Middle Archaic component was neither extensive nor well-defined, but was definitely present, indicating campers had used this site, perhaps only once, during the interval. Except for the compressed northern end of the deposit in Block A, this somewhat dispersed, wedge-like layer of material was separated from and below the Late Archaic materials, and was segregated above the older Early Archaic materials. The artifacts from this interval were vertically distributed over a 20 to 40 cm thick zone. Some 6,000 pieces were recovered, dominated by debtage, the waste flakes generated from the making of chipped-stone tools. Other materials included butchered deer bones, scattered burned rocks, and only 25 formal chipped-stone tools, among which were a number of Early Triangular projectile points. Two poorly organized burned rock clusters were identified and documented. The preservation of animal bone is rare in sites of this time period; thus the recovery of deer bone along with remains of rabbit, and possibly bison, though sparse, is significant. Had these bones not been burned, they likely would have decayed and disintegrated. Three radiocarbon dates—two on wood charcoal and one on a deer bone—directly date the Middle Archaic occupations to a 900-radiocarbon year period between 3910 and 4820 B.P. These three absolute dates are older than the Late Archaic materials above and younger than the Early Archaic materials below. Although the Middle Archaic is not well-known from other excavated sites, the material remains are not significantly different than those of other hunter-gatherer camps, except this group preferred unnotched projectile points. This is a key distinctive trait of this one group. Early ArchaicThe Early Archaic materials were situated within a roughly 30-cm thick zone, resting right on the much older river gravels. This position may indicate that the occupants camped directly on a gravel bar of the creek. With roughly 135,000 pieces, the component was extremely rich in artifacts. Materials varied in depth below the surface from a shallow 50 cm at the north end to a much deeper 120 cm in the southern end of Block A. Materials of this age are neither frequently encountered nor thoroughly investigated, and therefore are quite important. Some 170 dart points were recovered from this zone and classified as types Early Corner-Notched, Bandy, Martindale, Gower, Baker, and Merrell. These varied dart point types, along with a diverse array of stone tools (some1,300 pieces including bifaces, scrapers, drills, etc.), undoubtedly represent multiple, short-term camping events that have become mixed over time. Besides the chipped-stone tools and waste flakes, nine clusters of burned rocks were uncovered. These included two mostly intact hearths, two apparent dumps of burned rocks, and five general clusters of burned rocks. Bones, charcoal, and other organic materials were not preserved in this zone. Only a few scattered fragments of animal bones, a few burned prickly pear seeds, and a couple of wood charcoal pieces were recovered. Fifteen radiocarbon dates on animal bones, burned seeds, a snail shell, and plant particles yielded radiocarbon dates that document a minimum use period of 1,080-radiocarbon years from 5200 to 6280 B.P. Older events may be represented by these materials, but poor preservation may have destroyed the older organic material. A variety of data from this component indicates that the environment was somewhat cooler and wetter that other periods represented at the site as well as others in the region. During this time period, the Varga site and its surroundings may have provided a greater abundance of plants and animals, causing campers to return repeatedly to the area. Sampling and Laboratory AnalysesIn addition to chipped-stone tools and bone, a quantity of burned rock, soil samples, and other materials were collected from each of these occupation zones for specialized analyses. These technical studies, conducted on a wide variety of materials and samples, provide a wealth of insights into prehistoric activities at the Varga Site and are the subject of the following section: How Do We Know That?
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