Complex C

Cultural Complex C occurs primarily between the depths of 50 to 72

inches below baseline. The definition is based on the occurrence of

a cluster of traits similar to those found in a previously defined

unmixed culture. A certain amount of the apparent overlap is due to

the telescoped nature of the stratigraphy, which aggravates the effects

of trampling and other disturbances. It is not possible on the basis

of the available evidence to determine the relationship of Complex C

to those traits which are not consistent with the culture. They may

represent traits adopted by the C people, or they could be remains of

intermittent occupation by other groups, (see above).

The closest affiliation of Complex C is to the lower level of the

McKean Site, (Mulloy, 1954a), Signal Butte I, and related sites. The

most significant typological similarities occur in the projectile point

categories. The most numerous type at the site is the shouldered,

concave based point, (24 examples), designated “Duncan” by Wheeler

(1952). “Duncan” points are very common at the McKean Site. Somewhat

less well represented at the LoDaisKa are the McKean lanceolate

types. Though the general similarity to the McKean type material is

undeniable, certain differences occur uniformly. Most noticeable is

the discrepancy in size, McKean specimens being consistently larger.

The largest LoDaisKa examples approximate the smaller or medium-sized

McKean points. The small LoDaisKa points are completely out of the

range of McKean specimens, but certain of them do resemble types from

Signal Butte I, (Strong, 1935). Such differences and similarities may

reflect distance and local stylistic variation, functions of the points

in different economies, or perhaps chronological difference.

A second trait which was found to be useful in defining Complex C

is the end scraper. Though common at all depths above 72 inches, it

is almost completely absent below and aids in segregation of the

complexes, especially C and D. Many such scrapers were found at McKean

and Signal Butte.

The third important trait of technological as well as typological

significance is the striking of prismatic flakes, presumably from

prepared cores. As in the case of projectile points, most of the

examples are smaller than those which occur at McKean. On the other

hand, they appear to be more regular with a greater percentage that

have trapezoidal sections and roughly parallel sides. Some of these

have been worked and utilized as gravers, cutting edges, and possibly

scrapers. In this respect they approach, though do not equal, the

classic northern prismatic flake assemblages. For example, they

approximate the lower part of the size range and the slightly rougher

section of the material from Anangula Island, (Laughlin and Marsh,

1954).

The vertical distribution of stone-filled hearths is not confined to

the limits of Complex C. However, those features may be related to

those at McKean where they are large and well-defined. Grinding stones

were also important at both sites.

[Illustration: FIGURE 76—Projectile points from Signal Butte

illustrated for comparison. A-C. Signal Butte I, presumably IA. D-F,

flake points, presumably IC. A-D, drawn from photostats courtesy of R.

Forbis, E-F by R. G. Forbis.]

Relations with Signal Butte I are most evident in the projectile point

category, especially in the size average. A communication received

from R. G. Forbis, to whom we are deeply indebted, indicates that the

modal weight of the Signal Butte McKean points is about .56 that of

those at the McKean Site. Further, the collections from Signal Butte

contain three flake points. One striking example of a flake point in

the shape of a “Duncan” was found at LoDaisKa, (Fig. 15, type A).

Other flake points of varying form (listed as xx) occur in Complex C

levels. Some of these are not dissimilar to that of Signal Butte I, but

Dr. Forbis feels that these may belong to a later phase than the McKean

points. The main differences lie in the relative scarcity or perhaps

absence of straight stemmed or “Duncan” types at Signal Butte I[9],

and the occurrence of flared stemmed varieties or “Hanna” points. The

former are numerous at LoDaisKa, the latter absent. There is a good

possibility that Signal Butte I should be divided into two or three

phases, with McKean points earliest, (Bliss, 1950b, and R. G. Forbis,

personal communication).

[9] American Journal of Science, Vol. 257, No. 1, Jan. ’59, p. 21

“Lamont Natural Radiocarbon Measurements V.” Dates are now available

for Signal Butte, Ia: L 385 B, 4550±220 years and Signal Butte Ic: L

385 D, 4170±250 years. However, they may suggest that there is little

time lapse between the cultures of Signal Butte I.

Relations to other known sites may also be noted. Not only the stemmed

and lanceolate points, but side-notched and certain corner-notched

types are found in Deadman Cave, Stansbury Island, and Danger Cave

(Smith, 1952; Jameson, 1958; Jennings, 1957). The total range, however,

differs considerably. There is also some similarity to materials of the

earlier levels of Birdshead Cave, (Bliss, 1950a).

The stemmed “Duncan” types have rather wide morphological similarities.

As far away as Texas, middle levels of certain sites yield similar

materials (Pearce, 1932, pp. 46-47). Pedernales points of the Edwards

Plateau Aspect are roughly comparable (Suhm, Krieger, Jelks, 1954, p.

468; Kelley, 1947, 1959). At the other extreme, Thomas Kehoe (1955)

reports finding “Duncan-like” points at the Billy Big Springs Site

in Montana. Lister (1953) has suggested that a generalized form of

indented-based, stemmed point is a horizon marker in the West and

Southwest.

A large number of the artifacts that occur with the above are of

little diagnostic value. However, some of them are probably associated

culturally and formed part of the total artifact inventory. These

include: leaf-shaped and triangular knives, end and side scrapers, and

discoidal and serrated forms, one expanding base drill, perforators,

a few small ovoid bifaces, utilized flakes, chopper/hammerstones, one

bone ornament, paint stones, headed and splintered awls, used bone

splinters, one bone knife, and one wood shaft.

Excavations at the LoDaisKa Site in the Denver, Colorado area · 第 149 / 158 题