Folsom is also reasonably well dated on the Southern High Plains, with radiocarbon dates fromBlackwater Locality No. 1 and Lubbock Lake indicating an age range between 10,800 and 10,200 rcy BP(Holliday 1997:182). For the Plains and Southwest as a whole, the range is slightly larger, ca. 10,950 to10,250 rcy BP (Haynes 1993, Haynes et al. 1992) with the oldest Folsom dates overlapping the youngestClovis dates.Dating of the unfluted point styles is less secure, and Holliday (1997:185–186) identifies three significantchronological issues:• the dating of Midland and its relationship to Folsom,• the age of Plainview and its relationship to Folsom, and• the age and typological relationships among Plainview and the other unfluted point series.Midland points are relatively small, thin lanceolate points with a concave base and straight to slightlyconvex lateral edges. Both faces exhibit flat, regular scars from lateral thinning parallel or sub-parallel tothe fine marginal retouch, but remnants of the ventral surface of the flake perform are commonly evident.The basal concavity is generally less pronounced than Folsom, but some specimens exhibit the deep basalconcavity and attenuated ears that are characteristic of the Folsom fluting process. A few examples alsohave a basal nubbin that on Folsom preforms serves as the striking platform for fluting. On average, thepoints are smaller and thinner than Plainview and, except for the absence of fluting, they resemble Folsomin size and overall form.Midland points are not well dated. The solid carbon dates from the Midland (Scharbauer) type site appearunreliable (Wendorf and Krieger 1959), although a reanalysis of the site stratigraphy by Holliday andMeltzer (1996) suggests that the Midland points associated with the human remains may be younger than10,000 rcy BP. Judge (n.d.:35) lists two radiocarbon dates, 10,000±200 rcy BP (A-499) and 10,600±500rcy BP (A-504), as being associated with the Midland level at the Hell Gap site in southeastern Wyoming.These are two of four radiocarbon dates obtained from the lower portion of geological Unit E (Haynes1993:Figure 8; Irwin-Williams et al. 1973:Figure 3), but their relationship to the Midland materials isuncertain. As described in the preliminary report of the excavations, a small Goshen camp and a Folsomcamp were found at the base of geological Unit E in Locality 1. “Although vertical separation betweenthe two occupations was slight, their horizontal distribution was distinct. … Very slightly above theFolsom remains were a few artifacts assignable to the Midland Complex” (Irwin-Williams et al. 1973:44).Given the minimal separation of the three components and the large standard errors for the radiocarbondates, Haynes (1993:Table 1) rejects A-499 as unreliable and combines the other three dates to obtain anaverage age of 10,290±500 rcy BP for an undifferentiated Goshen-Folsom-Midland level. Based on theavailable evidence, then, Midland points can be tentatively dated between 10,300 and 10,000 rcy BP, butthey may have appeared earlier and persisted later.Despite the dearth of chronological evidence, there is general acceptance that the date range for Midlandpoints overlaps that of Folsom points. Apart from the overall similarity of the two point styles, Midlandand Folsom points have been found eroding from the same eolian unit at sites on the Llano Estacado,most notably at Midland and Shifting Sands (Amick 1995:2425; Holliday 1997:187). Further, althoughthe Folsom archetype is fluted on both faces, the artifacts recovered from Folsom components at anumber of sites also include points fluted only on one side, as well as “pseudo-fluted” and unfluted forms.It therefore seems likely that Midland is not a distinct point type but an unfluted variant of Folsom(Amick 1995; Frison 1991:51; Hofman 1992). Although Judge (1970) has demonstrated that themanufacturing trajectories of the two point styles are distinct, the primary difference is that the basalthinning of Folsom points is accomplished by fluting, whereas Midland point bases are thinned by lateralflaking. Since controlled lateral thinning is also characteristic of Folsom point performs, the Midlandmanufacturing trajectory can be viewed as an attenuated version of the Folsom trajectory. That someMidland points have characteristics associated with the Folsom fluting technique further suggests that thetwo trajectories may be part of a single technological tradition.4-4
Plainview are lanceolate points with slightly convex lateral edges, a lenticular cross-section, and aconcave base. Lateral flake scars are roughly parallel to collateral, and the proximal half to two-thirds ofthe lateral edges are moderately to strongly abraded (Knudson 1973:40–41). Final basal thinning isusually accomplished by the removal of multiple small vertical flakes (Turner and Hester 1993:175).Based on measurements of the Plainview and Ryan’s Cache collections (Hartwell 1995:Table 3; Knudson1973; Table D-1), Plainview points are generally larger than Midland points, although there is a slightoverlap. Mean length is 57 mm with a standard deviation of 9 mm; mean width is 23.4 mm with astandard deviation of 2.6 mm; and mean thickness is 6 mm with a standard deviation of 1.5 mm.Judge (n.d.:37) argues that two other named point types, Meserve and Milnesand, are variants ofPlainview. Milnesand points have a straight or slightly convex base, but exhibit the same basal thinningattributes and extensive abrading of the lateral edges as Plainview. They have been found in goodarchaeological context only at the Milnesand and Williamson site, and both of those sites also yieldedPlainview points (Holliday 1997:193). The only difference between Plainview and Meserve points is thatthe latter has a triangular blade with unifacially beveling (Turner and Hester 1993:154). Since beveling isa common technique used to sharpen projectile points, Meserve appear to be reworked Plainview points.Goshen points in the northwestern Plains are also morphologically similar to Plainview, but the two typesmay date to different periods. Goshen was reportedly found stratigraphically below Folsom at Hell Gap(Irwin-Williams et al. 1973). The Clovis-age AMS dates for Goshen at the Mill Iron Site (Frison 1996:8)are consistent with that placement, although the possibility that the radiocarbon dates were contaminatedby coal deposits cannot be totally discounted. In contrast, Plainview in the Southern High Plains occurstratigraphically above Folsom at Lubbock Lake, Lake Theo, and probably at Blackwater Locality No. 1.Radiocarbon dates associated with Plainview cluster at 10,000 rcy BP with a range of 10,300 rcy BP orolder at Bonfire Shelter to 9200 rcy BP or younger at Ryan (Holliday 1997:189–190).Two constricted base points, Agate Basin and later Hell Gap, follow Folsom in the northern Plains.Agate Basin points are long (average 7.5 cm), narrow points with a thick cross-section and slightlyconvex lateral edges that taper to a narrow base (Judge n.d.:41). Hell Gap points are similar but haveslight shoulders and a wider blade. Both styles typically have collateral flaking. Hofman (1989:40–41)reports that Agate Basin and Hell Gap points are relatively common in the southern Plains. Only AgateBasin points have been found in a stratigraphic context, however. Agate Basin points appearscontemporaneous with late Folsom in the spring conduit deposits at Blackwater Locality No. 1 (Haynesand Agogino 1966:819), and other Agate Basin material was recovered from lower Unit E, whichprobably dates to about 10,000 years BP (Hester 1972:59). Points morphologically similar to Agate Basinare also dated to about 10,000 BP at Lubbock Lake (Holliday 1997:192). Constricted base pointstherefore seem to have roughly the same date range in the Southern Plains as in the northwestern Plains;that is, 10,500–9500 rcy BP for Agate Basin and 10,000–9500 rcy BP for Hell Gap (Frison 1991:24–27).Thus there is considerable overlap with Plainview.A variety of unfluted points were recovered from an extensive bison bone bed located stratigraphicallyabove the Folsom and Agate Basin material at Blackwater Locality No. 1. Sellards (1952:72–74) calledthis assemblage the Portales Complex, and he described the projectile points as similar to Eden,Scottsbluff, San Jon, and Plainview. San Jon was defined by Roberts (1942) based on a single lanceolatepoint recovered from the San Jon site. The basal portion of the point has collateral flaking, a square base,and basal and lateral grinding. The tip is heavily reworked (Hill et al. 1995:382). Eden and Scottsbluffare diagnostic of the widespread Cody Complex. Cody Complex points are long, narrow points withstraight lateral edges and short stem indented by lateral flaking (Judge n.d.:48). Thinning and shaping ofthe points is achieved through regular, usually comedial, pressure flaking that produces a prominentmedial ridge and gives the points a characteristic diamond-shaped cross-section (Bradley 1993:260).Eden points are very narrow with barely perceptible shoulders. In some instances, the stem is formedentirely by abrading. Scottsbluff points have a wider blade and more pronounced shoulders.4-5
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National Register criteria, and dat
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• What data sets are needed to ad
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Fields, may be downloaded from the
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Development of Southeastern New Mex
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Table of Contents ContinuedRadiocar
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List of Tables ContinuedTable 3.13T
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CHAPTER 2PHYSIOGRAPHY, GEOARCHAEOLO
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The Llano Estacado Section or South
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Table 2.1 Selected Geologic Referen
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Portales ValleyThe Portales Valley
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The thickness of surficial deposits
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Alluvial Flats. Denudation of bedro
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Table 2.3 Physiographic Regions and
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Table 2.4Expected Average Condition
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Site densities were calculated for
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Figure 2.6. Area surveyed in square
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15. Based on the strong direct rela
- Page 38 and 39: REFERENCES CITEDAltschul, J. H., Se
- Page 40 and 41: 2005 Surficial Geologic Map of New
- Page 42 and 43: PREVIOUS TYPOLOGIESA number of typo
- Page 44 and 45: Expectation for quarry sites and to
- Page 46 and 47: As shown in Table 3.2, artifact sca
- Page 48 and 49: Table 3.3 Rank ordering of feature
- Page 50 and 51: Figure 3.2features.Histogram showin
- Page 52 and 53: Table 3.5Expanded Component Types (
- Page 54 and 55: 11. cave - a natural hollow or open
- Page 56 and 57: Ring Midden - a general donut-shape
- Page 58 and 59: Table 3.7Occurrences of Surface and
- Page 60 and 61: Our next concern was therefore the
- Page 62 and 63: SITETYPE/GEOARCH LANO SUBSISTENCE R
- Page 64 and 65: SITETYPE/GEOARCH LANO EFFORT AREA E
- Page 66 and 67: ecause we don’t know how many sit
- Page 68 and 69: Table 3.10 Proportional Area, Surve
- Page 70 and 71: Table 3.11 Distribution of Paleoind
- Page 72 and 73: Figure 3.53-32
- Page 74 and 75: Figure 3.63-34
- Page 76 and 77: Figure 3.73-36
- Page 78 and 79: Not surprisingly, the distribution
- Page 80 and 81: Table 3.15 Distribution of Unknown
- Page 82 and 83: Pielou, E. C.1969 An Introduction t
- Page 84 and 85: Wiseman, Regge N.1996 Corn Camp and
- Page 86 and 87: and projectile point chronologies c
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- Page 92 and 93: described by some authors in the lo
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- Page 96 and 97: CeramicIn contrast to the Archaic,
- Page 98 and 99: this feature type were observed. On
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- Page 102 and 103: • Did agricultural groups eventua
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- Page 106 and 107: the Apaches. Based on their locatio
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- Page 110 and 111: For Sebastian and Larralde, the que
- Page 112 and 113: Bohrer’s interpretation of the Fr
- Page 114 and 115: As Sebastian and Larralde recognize
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- Page 118 and 119: small game. Some rodents may also h
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Acquisition of the horse would have
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In using modern environmental data
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Table 4.1 Priority General Question
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Chronology and Culture History Subs
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Table 4.3. General question posed u
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1983 In Pursuit of the Past. Thames
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Gamble, C. S. and W. A. Boismier (e
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1997 Analysis of Paleoindian Bonbed
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1999 Comments on the Prehistory of
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Shelley, Phillip H.1994 A Geoarchae
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2000 Crosby Draw and River Camp: Co
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NMCRIS data indicate that survey co
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Addressing the Research QuestionsTh
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There are two major shortcomings to
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Artifact assemblages need to be des
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As with the selection of sites, the
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Architectural Sites(Single Residenc
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Based on the discussion of regional
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If Unit 1 deposits are exposed, the
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few artifacts are recovered and the
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2. Large artifacts should be tagged
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h. Subfloor tests will be dug to de
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. 1 x 1 m grids and/or backhoe tren
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Geophysical Remote SensingGeophysic
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1987 Man the Hunted: Determinants o
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CHRONOLOGICAL SAMPLINGGeneral Guide
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a. Conversions of Radiocarbon Years
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f. Samples should not be exposed to
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LITHIC ARTIFACT ANALYSISThe goals o
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24Manuport,tabular25 GroundstoneNon
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Use wear codes, terms and descripti
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B. Mano1. Type2. Material type3. Or
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References CitedAcklen, John C., Ma
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PROPOSED LITHIC MATERIAL CODE SHEET
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108 light gray with profuse red (26
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CERAMIC ANALYSISThe goals of the ce
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Jornada Red TooledJornada Corrugate
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Santa Fe Black-on-whiteGalisteo Bla
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VI. Whole Vessels1. Vessel height2.
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Data NeedsA. Usage of more sophisti
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5. The determination to wash the fa
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ARCHEOBOTANICAL STUDIES(from Dean 2
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V. Sample Size and NumberA. A recom
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B. Data return is dependent upon pr
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Or submit the vessel for a pollen w
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# FlotationSamples Flotation Sample
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might include “quids”, sandals,