A03-1014 "Chiripascapa" [A03-1014 - A03-1057]

Chiripascapa was recorded as three sites due to variability in the artifact distributions and the differences in topography. Due to downslope movement in the steep talus zone in one portion of the site, and deflation in the lower site complex, the Archaic Foragers component of this site complex will be described as one group.

ArchID	SiteID	FileType	Description	Area (m2)
1014	1014	Site_a	"Chiripascapa"	24,550,334
1023	1014	Lithic_a	Medium Dens, 100 Obs	38,785
1024	1014	Lithic_a	Medium Dens, 89 Obs	124,943
1025	1025	Site_a	"Chiripascapa2"	27,927,630
1026	1025	Lithic_a	High Dens, 100 Obs	2,470,331
1038	1025	Lithic_a	High Dens, 30 Obs	1,086,213
1041	1025	Ceram_a	Painted LIP	186
1043	1025	Lithic_a	Medium Dens, 100 Obs	9,484,728
1045	1025	Struct_a	Wall Bases Only, Cave	128
1052	1025	Lithic_a	Medium Dens, 100 Obs	888,906
1049	1049	Site_a	"Chiripascapa3", Rock shelter	3,657,074

Table 6-26. Loci in Chiripascapa

Description

The upper part of Chiripascapa consists of one medium sized rock shelter and three small rock shelters at the base of an east-north-east facing portion of the Huarancante volcanic breccia lava flow escarpment. Below the rock shelters a sloping talus field (a 25° slope), littered with lithics as well as ceramics, leads to a small intermittent stream 20 vertical meters below the rock shelter. On the banks of this stream is a scatter of lithics and ceramics from a variety of time periods that extend downstream for approximately 300 m. The south bank of the stream has a modern estancia (Pausa) and a large corral below the associated buildings, seriously disturbing any artifact scatters on the south bank. The north bank of the stream is also disturbed. Large scars from bulldozers scraped off the topsoil in certain areas. The resident at the Pausa estancia explained that during the 1970s highway improvement for the Majes Project the road crews caused these impacts as they were looking for gravel sources in that area. Just north of this site complex is a large, active gravel pit.

Figure 6-18. A03-1050 consists of four rock shelters: A, B, C, and D.

Figure 6-19. Chiripascapa [A03-1014], Archaic Foragers occupation.

A03-1050 - Four rock shelters of Chiripascapa

These rock shelters appear to be well situated with respect to the surrounding geography. The shelters face east-north-east and so despite being in a dark and slightly damp corner of the lava toe they catch the morning and midday sun. It is worth noting that the estanciadepicted in the center of the map appears to be deliberately built with the same aspect. The rock shelter is relatively well-hidden because it lies about 50m up a side quebrada and therefore goes unnoticed unless you climb the quebrada. Despite the concealed position, this location actually offers a partial view of the most important resource in the zone: the bofedal one km to the north-east. It would also be possible to monitor travel through the Ventanas del Colca access to the upper Colca from this hidden location. The stream below the shelters was dry at the end of the dry season, but probably flows most of the year.

Due to low GPS reception in the rock shelter area the four rock shelters were mapped as a single Struct-L line "A03-1050" and differentiated as A, B, C, and D. Only one shelter, the one designated as A03-1050B, had the characteristics of a residential shelter. The dimensions of this shelter are as follows. Height:2m, Depth:6.5m, Width:7m. Due to the overhanging roof formed from the lava flow, a considerable area is dry outside of the walls of the cave. This area shows signs of having been improved as a patio and the "patio" area extends the depth of the dry zone by another 12.5m. The rock shelter 1050A was large but wet, and 1050C and 1050D were very small but dry.

Below the rock shelters a talus slope extends approximately 20 vertical meters to the stream. A variety of lithics and ceramics were identified on this slope, though only one projectile point was diagnostic to a period that falls in the Archaic Foragers timespan. This point [A03-1051] was a Middle Archaic andesite point and it had a transverse snap and missing its haft element, suggesting that it was broken in use.

Features and Artifacts

The stream enters the open, sandy soils of the pampa and on either bank of the stream, though primarily on the north bank, projectile points from throughout the Archaic sequence were found. Preservation is relatively poor on this section of the pampa. In addition to the bulldozer impacts mentioned above, the soils appear deflated and this partly explains the high density of projectile points, from virtually every time period, found in this area. It seems possible that the entire site scatter was formerly more aggregated on the western part of this map, and with riverine transport the artifacts have been scattered over the pampa.

ArchID	Artif. #	Material	Form	Type	Temporal
1015	1	Obsidian	Proj Point Broken	1a	Early Archaic
1016	1	Obsidian	Proj Point	2c	Middle Archaic
1017	1	Volcanics	Proj Point Broken	4d	Late Archaic
1018	1	Volcanics	Proj Point	4d	Late Archaic
1019	1	Volcanics	Proj Point	3d	Archaic
1021	1	Volcanics	Proj Point Broken	2c	Middle Archaic
1023	1	Obsidian	Proj Point	2c	Middle Archaic
1024	4	Volcanics	Proj Point	4d	Late Archaic
1024	5	Volcanics	Proj Point Broken	4d	Late Archaic
1026	3	Obsidian	Proj Point	1b	Early Archaic
1031	1	Obsidian	Proj Point	4f	Late-Term. Archaic
1034	1	Chert	Proj Point	1b	Early Archaic
1035	1	Obsidian	Preform	2c	Middle Archaic
1036	1	Obsidian	Preform	2c	Middle Archaic
1037	1	Obsidian	Proj Point	1a	Early Archaic
1044	1	Obsidian	Preform	2c	Middle Archaic
1044	2	Obsidian	Proj Point	1a	Early Archaic
1048	1	Volcanics	Proj Point	4d	Late Archaic
1051	1	Volcanics	Proj Point Broken	3b	Middle Archaic
1057	1	Volcanics	Proj Point Broken	4f	Late-Term. Archaic

Table 6-27. Diagnostic Series 1 through 4 projectile points from Chiripascapa [A03-1014].

The temporal distribution of projectile points from Chiripascapa shows that virtually every time period is well represented. One distinction worth noting is that obsidian is used almost exclusively in the later time period, while about 50% of the projectile points (by count) are made from obsidian in the early time periods presented by Series 1 - 4 points.

Projectile Points	Obsidian	Volcanics	Chalcedony	Chert
Series 1 - 4	10 (48%)	9 (43%)	1 (5%)	1 (5%)
Series 5	24 (96%)	1 (4%)	0	0
Total	34	10	1	1

Table 6-28. Representative proportions of material types by projectile point styles.

The medium and high density lithic loci along the creek banks are difficult to temporally isolate because there are later period diagnostics, including twenty-six Series 5 projectile points and ceramics dating from the Middle Horizon, LIP, and Inka periods found in the A03-1038 lithic locus. Most of the flakes observed at this site were obsidian and chert. A small concentration of andesite flakes on the south bank of the stream in locus A03-1038 was observed, despite the fact that all andesite projectile points came from the north bank of the stream.

Material Type	Obsidian	Volcanics	Chalcedony	Chert	Quartzite
No.	88 (62%)	32 (23%)	5 (4%)	15 (11%)	1 (0.7%)
Mean Wt (g)	5.05	18.28	16.7	10.91	11.5
% by Sum Wt	34.5%	45.6%	6.7%	12.3%	0.9%

Table 6-29. All lithic artifacts from Chiripascapa.

The surface materials included bifaces, cores, and flakes of all local material types except quartzite, which was rare at the site. Based on the mean flake size and the percentage of the total contribution by weight, fine-grained volcanics appear the most local to the area. Isolating any one of the lithic concentrations to a particular time period is difficult, but when viewed collectively including the point scatters in A03-1014 and A03-1025, and the rock shelters in A03-1049, the site complex is one of the oldest residential areas in the larger study area. The rock shelter A03-1050B and the built up patio has a high probability of containing a stratified intact deposit that extends into the earlier parts of the Archaic.

A03-900 "Huañatira"

Huañatira is a horseshoe-shaped valley with escarpments of lava flows of volcanic breccia on three sides and a small rise in the center where a single toe of lava extends down lower towards the pampa. The result is a sheltered, circular valley with a sloping ramp that climbs towards the top of the lava flow to the east of the valley. The Huañatira valley provides a moderately sheltered area with good views of the surrounding pampa, and it is defensive because it provides means of escaping to the higher lava flow terrain without being observed by pedestrians approaching from the pampa.

Figure6-20. Huañatira [A03-900] and vicinity, Archaic Foragers occupation.

Description

The area has evidence of occupation from virtually every time period from the Early Archaic to the modern period. A maintained estancia is found just to the west of the study area shown in Figure 6-20, and a small driveway is shown on the map accessing the area from the east. A worn trail departs the estancia to the west; a travel route that probably dates to the pastoral period if not earlier. Projectile points were found scattered around the valley that date to all periods, however most of the large scale archaeological features in this area appear to be from the pastoralist period. The circular or oval features shown as structural loci (not labeled on Figure 6-20) are most likely of pastoralist origin. A rock shelter offering partial protection was found in the center of site 900 overlooking the pampa [A03-903]. This immediate valley area belongs to a very small local watershed, and during the dry season there was no apparent surface water. This small watershed prevented a great deal of surface runoff; a factor has probably helped to maintain artifact positions in their original contexts in this local valley more than at other sites from the survey.

ArchID	File Type		ArchID (cont.)	File Type
817	site_a		940	lithic_a
820	site_p		941	lithic_p
821	lithic_a		942	lithic_p
822	site_p		943	lithic_p
823	site_p		944	lithic_p
824	site_p		945	lithic_p
825	site_p		946	lithic_p
826	site_p		947	lithic_p
827	site_p		948	site_p
828	lithic_a		949	lithic_p
830	struct_p		951	lithic_p
831	site_p		953	lithic_p
900	site_a		954	lithic_p
902	lithic_a		956	site_a
903	struct_l		957	struct_l
904	lithic_a		958	struct_a
905	lithic_p		960	lithic_p
906	site_p		961	lithic_p
907	site_p		962	lithic_p
938	site_a		963	lithic_p
939	lithic_a		964	lithic_p

Table 6-30. Non-consecutive ArchID numbers at Huañatira [A03-900], an Archaic Foragers site.

A03-957 - Rock shelter

This is a relatively large rock shelter overlooking the pampa and the valley of Huañatira. Contrary to most residential rock shelters in the region, this shelter faces south-east and it is therefore not exposed to the warming sun and was probably a shelter that was cool in temperature nearly all year reducing its potential as a residential structure in the altiplano. The shelter offers a relatively large amount of residential space inside the dripline; the rock shelter is 7m deep from the dripline, 12m wide, and over 3m high. Virtually all of the interior space of the shelter is clear of rubble and useable for residential activities. Four projectile points from the Early, Middle, and Late Archaic Periods were found associated with this shelter. A recessed tomb dominates this shelter today, but given the size of the feature and the pattern of cave burial during the Late Intermediate Period, the mortuary feature in this shelter is interpreted as a LIP cist tomb. These features are described in the Late Prehispanic - Block 2 discussion (Figure 6-76), close to the end of this chapter.

Figure 6-21. Rock shelter of Huañatira with circular mortuary feature visible inside. One meter scale showing on tape resting on rock along dripline (see also Figure 6-76).

Features and Artifacts

Some cases of disturbed artifact provenience are obvious, such as the three projectile points in a wash at the base of the valley shown as the three points on the eastern edge of Figure 6-20. Also the points below the Huañatira rock shelter on the north end ofthis site were found in the colluvial zone below the shelter and were apparently displaced.

ArchID	Index#	Material	Form	Type	Temporal
820	1	Obsidian	Proj Point	3b	Middle Archaic
822	1	Volcanics	Proj Point	2c	Middle Archaic
941	1	Obsidian	Proj Point	1a	Early Archaic
942	1	Chert	Proj Point Broken	3b	Middle Archaic
943	1	Obsidian	Proj Point	4f	Late - Terminal Archaic
944	1	Obsidian	Proj Point	3b	Middle Archaic
945	1	Obsidian	Proj Point	1b	Early Archaic
949	1	Obsidian	Proj Point	2a	Early-Middle Archaic
951	1	Quartzite	Proj Point	3b	Middle Archaic
953	1	Obsidian	Proj Point	2c	Middle Archaic
954	1	Obsidian	Proj Point	4f	Late - Terminal Archaic
956	2	Volcanics	Proj Point Broken	1b	Early Archaic
956	3	Obsidian	Proj Point Broken	1b	Early Archaic
958	1	Volcanics	Proj Point Broken	3b	Middle Archaic
960	1	Volcanics	Proj Point	4d	Late Archaic
963	1	Volcanics	Proj Point Broken	4d	Late Archaic
964	1	Volcanics	Proj Point	4d	Late Archaic

Table 6-31. Diagnostic Series 1 through 4 projectile points from Huañatira [A03-900].

Artifact proportions are consistent with other Archaic Foragers sites in the area, with approximately 50 of the projectile points and 65 of all collected lithic artifacts being of obsidian. A number of bifaces and flakes were found at this site, primarily of fine-grained volcanic stone and obsidian, and one obsidian core.

Material Type	Obsidian	Volcanics	Chalcedony	Chert	Quartzite
No.	50 (64%)	14 (18%)	3 (4%)	9 (12%)	2 (3%)
Mean Wt (g)	4.97	99.8	31.4	49.5	111.1
% by Sum Wt	10.4%	57.8%	4.2%	17.6%	9.9%

Table 6-32. All lithic artifacts from Huañatira.

As with other residential areas in Block 2, it is difficult to differentiate the Archaic Foragers component in this area of heavy reoccupation. The area contains a large rock shelter and it provides a measure of shelter on the border of the pampa, as do the other shelters in the area. Several Late Archaic projectile points are dark fine-grained volcanic rock, akin to the Late Archaic (4d) points found at that Chiripascapa [a03-1014] a short distance to the north.

Method

The criteria used here for sites isolating through the dominance of particular material types are as follows for both lab analysis Lithics_I and Lithics_II. First, the lab results by SiteID (or isolated ArchID), showing count and percent, were shown in a table against material type in Arcmap. This table was joined to the All_ArchID_Centroids point geometry [link to Processing in Ch 5] so that lab results for lithic material types were aggregated by site or isolate. These features were then filtered by constructing a query where the artifact count for a geographical feature had to be greater than 5 so that relative percentages were meaningful. Finally, the index symbolized inFigure 6-22 is the Lithics_I lab results (the most comprehensive table) where Percentage of Non-obsidian lithic artifacts is greater than or equal to 50%.

Results

The use of non-obsidian materials such as chert, chalcedony, and especially fine-grained volcanic materials, dropped precipitously during the Terminal Archaic at sites in Block 2. While all lithic material types persist in use during the pastoral period, the herd management tasks of butchery and shearing appear to have been largely conducted using obsidian. Reviewing the percentages of sites with strong evidence of a pastoralist occupation (only Series 5 projectile points, a corral, water, and grazing opportunies) these sites commonly have between 20% - 40% non-obsidian flaked stone. Thus, the distinction between pastoralist and forager components based on material type is not firm, but the distributional pattern is reinforced by non-series 5 projectile point distributions, and this evidence is shown together in Figure 6-22.

Six sites have been identified with a relatively robust Archaic Foragers component in Block 2 and the environmental characteristics of these six sites will be compared with all locational characteristics of B2 sites in order to look for patterning among the environmental criteria of Archaic Foragers sites. These six sites include the following A03- 396, 884, 894, 900, 1014, 1049 and while diagnostics from the Archaic Foragers period were widely encountered throughout the region, these sites are selected as representantive for the larger Archaic Foragers time period and life way based on inference. Clearly the boundaries of the "site" are probably not coterminous with the Archaic Foragers component of these sites, nevertheless these measures serve as a general indicator of changes in the environment context of settlement through time.

	Selectedm	Selecteds	All B2 Sitesm	All B2 Sitess	All B2 Sitesm - Selectm
Altitude (masl)	4382.6	12.69	4393.2	25.7	-10.6
Slope (degrees)	7.86	8	8.33	6.34	-0.47
Aspect (degrees)	146.5	96.4	138.4	58.23	8.1
Visibility/Exposure	33.6	13.1	40.1	25.53	-6.5
Dist. to Bofedal (m)	497.3	212.2	307.5	261.5	189.8

Table 6-33.Environmental characteristics of selected Archaic Foragers sites in Block 2.

The high standard deviation values in the Table 6-33 "Selected sites" underscores the variability and inconsistency in these estimates. This comparison shows that the Archaic Foragers sites tend to be more sheltered/lower visibility than the pastoralist sites. As was previously noted, the Archaic Foragers sites are often adjacent to overlooks but the sites often do not occupy the high exposure area specifically. Archaic Foragers sites are considerably further than average from bofedales. This strong tendency in the data is probably accentuated by the intensification and maintenance of pastoral resources that has occurred in recent years. That is to say, as pastoralism is today the principal economy activity in the area, bofedales and attendant pastoral facilities have been well-maintained in the recent past, which is the criteria from which bofedales were selected from the ASTER satellite imagery for this measure. A further issue with respect to distance to water is the fact that many of the potential forager sites are adjacent to small streams that were probably seasonal and appear as dry in the modern dry-season ASTER imagery.

A03-1000 "Kakapunku" [A03-1000 - A03-1013]

The site of Kakapunku [A03-1000] (a.k.a. C'oponeta) is located on the south side of the Río Llapa on a north facing bluff just upstream of the confluence of the Río Llapa and the Río Pulpera. This site consists of three rock shelters spaced about 15m apart along the base of a 10m high irregular cliff band that lies approximately 30m up the hill and south of the high-water line on the Río Llapa. There is a colluvial ramp below the rock shelters and on a terrace below that ramp lie number of lithic loci and some ceramics. The rock shelters are generally north facing so that they are oriented to the mid-day sun and the shelters are warm and well-lit.

ArchID	SiteID	FileType	Description	Area (m2)
1000	1000	Site_a	"Kakapunku"	3400.0
1004	1000	Lithic_a	High Dens, ~70 Obs	1771.3
1010	1000	Lithic_a	High Dens, ~70 Obs	76.7
1013	1000	Lithic_a	Medium Dens, ~70 Obs	148.6

Table 6-35. Loci in Kakapunku [A03-1000].

ArchID	Description	Height	Depth	Width	Width Entrance
A03-1001	Mortuary, looted. MNI=7	1.6	3.2	5.2	1.9
A03-1002	Domestic, warm rock shelter	4	3.5	6	5.1
A03-1003	Mortuary, looted. MNI=14	1.6	~8	1.4	1

Table 6-36. Rock shelters at Kakapunku [A3-1000], dimensions in meters.

Figure 6-26. Site of Kakapunku [A03-1000].

A03-1001 -East rock shelter at Kakapunku

This is a looted mortuary context. The rock shelter is moderately difficult to access on a cliff face, and the entrance appears to have been formerly walled off. The original rock shelter height is difficult to determine because cist tombs in the floor of rock shelter have been excavated by looters. A number of complete crania and long-bones were present. The crania and long bones were examined in the field by Mirza del Castillo, a team member who is a physical anthropologist. From her in-field visual assessment she cautiously suggests that a number of the crania had female metric proportions, and that a number of the crania appeared to have hypoplasia of the bone marrow on the posterior edge of the parietal bones which is a possible indicator of anemia.

Figure 6-27. The entrance of A03-1001 with looted cist tomb visible inside the rock shelter.

A03-1002 - Center rock shelter at Kakapunku

This rock shelter is relatively shallow but other characteristics made it appear to be to be an inviting residential location for a small group of foragers or pastoralists. The shelter is dry inside the dripline, north facing, flat interior, defensible, a short distance from water, and immediately south of a terrace for open-air activities where loci a03-1004 through 1013 are located.

A03-1003 - West rock shelter at Kakapunku

This rock shelter is a lava tube sloping upwards into the cliff face. It appears to contain many disturbed interments. Undisturbed human remains perhaps exist here but they were not visible on the surface.

Discussion

Kakapunku is another case of a multicomponent site where discerning the Archaic component is difficult. Five projectile points were identified belonging to different Archaic Periods, and combined with the ceramics (described later), there is a some affiliation with virtually all time periods at this site.

ArchID	Index	Material Type	Form	Type	Temporal
1001	1	Obsidian	Proj Point	3a	Early-Middle Archaic
1002	1	Obsidian	Proj Point	2b	Latter part of Middle Archaic
1004	1	Obsidian	Biface	n/a
1004	2	Obsidian	Biface	n/a
1004	3	Obsidian	Proj Point Broken	5	Late
1005	1	Volcanics	Core	n/a
1007	1	Obsidian	Proj Point	3b	Middle Archaic
1008	1	Volcanics	Proj Point	4d	Late Archaic
1009	1	Obsidian	Preform	5a	Late
1010	1	Obsidian	Proj Point Broken	5d	Late

Table 6-37. Selected Lithics from Kakapunku [A03-1000].

On the terrace below the rock shelter [A03-1002] the largest concentration of artifacts were noted. Samples collected from the medium and high density lithic loci on the terrace are approximately 50% obsidian materials with the non-obsidian primarily consisting of aphanitic volcanic stone. The northern high density locus, A03-1010, is eroding down the cutbank caused by erosion and it is possible that this terrace was significantly larger but has been truncated by fluvial erosion of the terrace. In sum, Kakapunku appears to have served as a regular residential area with three relatively small rock shelters.

A03-985 "Quelkata"

This rock shelter lies just below the confluence of the Río Llapa and Río Pulpera along a sweeping bend in the river channel where the Río Llapa first approaches the Castillo de Callalli formation. This rock shelter is well situated and probably served as a residential base through most of prehistory, however surface collections by Jose-Antonio Chávez Chávez (1978) for his Bachelor's thesis revealed primarily preceramic occupation levels with late, Series 5 projectile points. By the time Chavez was able to systematically investigate the materials in the rock shelter it had been largely destroyed in 1976 by the road construction crews associated with the Majes Project (Chávez 1978: 3). The rock shelter was dynamited because it is unfortunately located precisely at a point of the Río Llapa where the project planned to build a bridge on the road to the Condoroma reservoir. What remains today of the rock shelter is a concavity in the tuff with a shelter dry zone measuring approximately 150m wide inside the dripline. Chávez systematically collected and analyzed projectile points from this rock shelter but, curiously, the artifactual evidence available shows an occupation sequence going only as far back as the Terminal Archaic.

Figure 6-28. Cueva de Quelkata was dynamited by Majes Project road crews in 1976. Two people are visible for scale inside the shelter to the left of center.

Figure 6-29. Quelkata in 1975 redrawn from Chavez (1978: 20). Red dotted line shows estimated border of the portion of the rock shelter that remains after the dynamiting for road widening.

Description

The rock shelter was significantly larger in the recent past. Chavez (1978: 20-21) estimates that the dry portion of the rock shelter was 7m deep, 50m wide, and 2.65m high at the mouth. The sheltered area amounted to a 365 m²area with the bulk of cultural debris concentrated in the south portion of the rock shelter. Chávez estimated that the stratigraphy included up to 3m of cultural material. During the 2003 season a great abundance of cultural material was not observed in the slopewash between the highway and the river, as one might expect if the highway were constructed on such quantities of cultural fill, but the area has been much disturbed in recent years.

Figure 6-30. Quickbird satellite image of Quelkata area in 2005. The shelter is under the tuff outcrops immediately to the left of the bridge. Data courtesy of Google / Digital Globe.

Quelkata is located at a major cross-roads in the local transportation network and it has probably been a significant landmark among people in the Upper Colca since the earliest human occupation of the region. The rock shelter mouth opens east-north-east and deposits still evident in the back of the rock shelter are approximately 5 vertical meters above the river and 2.5 meters above the modern highway. As the rock shelter is on a bend in the river the shelter appears to have been scoured out of the outcrop of welded tuff by the waters of the Río Llapa until the river channel was sufficiently incised that it not longer entered the rock shelter proper. Recently Noble (2003) collected a K-Ar sample from precisely this location and the resulting age of 20.7±0.6 million years indicates that the formation dates to the Early Miocene.

Geographical attributes of this location can be summarized as follows.

(1) Quelkata is a large, sheltered site close perennial to water source that probably provides year-round fishing opportunities.

(2) The east-north-east aspect results in warming by the morning sun.

(3) It is located at major intersection in local travel routes which suggests that many were familiar with the site, but also exposes the occupants to anyone traveling in this portion of the valley.

(4) Summits of the "Castillo de Callalli" tuff outcrops immediately above are defensible and appear to have been fortified during the LIP.

Figure 6-31. A 65cm column of cultural deposits still exists at the back of Quelkata at a height of approximately 1.8m above datum (at head height between the gravels and the tuff in photo).

Preservation of Quelkata

Road crews associated with the Majes Project dynamited the rock shelter in 1976 but this was not the first important disturbance in this high traffic area. Significant impacts on preservation at Quelkata are the following

(1) Although the rock shelter lies approximately 5 meters above the dry season water level of the Río Llapa, the rock shelter has probably been scoured repeatedly by high water in past millennia. Quelkata is located on the outer edge of river bend precisely at a channelized portion of the river where 1000 year or even 100 year floods potentially entered the rock shelter and disturbed the contents.

(2) As noted by Chávez (1978: 17) a road has long existed in this area due to the fact that it is a crossroads location and, as a channelized portion of the river, it probably has had bridges prior to the modern bridge construction. With the mining history in the Cailloma area, a road was likely constructed to connect this ore-rich province with the Sumbay railroad sometime in the early 20^thcentury. The dynamiting by the Majes crew was intended to widen the road at the bridge and the intersection, and it significantly impacted the rock shelter. However, the downslope colluvial outwash from the rock shelter, which are frequently deposits of great archaeological interest from a rock shelter, had long been disturbed by road construction and by fluvial erosion prior to the destruction by the Majes crew.

(3) The construction crews dynamited the site in 1976 and largely destroyed the southern portion of the rock shelter, the portion that Chávez (1978) describes as having the deepest deposits. There are still significant deposits at the back of the rock shelter, however. As part of the archaeological reconnaissance of the Llapa valley materials systematically surface collected from the rock shelter as will be described below.

(4) The intersection and bridge at Quelkata was a principal junction in the Arequipa highway network until 2002 when the highway connecting Arequipa with Juliaca was paved. Until the asphalting of the Arequipa-Juliaca highway virtually all of the highway traffic between Arequipa and Cusco passed directly in front of this rock shelter where one of the few restaurants and gas stations along the route was located. Thus, a relatively high number of travelers probably visited the rock shelter and its surroundings while waiting for transportation. Fortunately, the dynamiting of the shelter created a sheer 2 m wall so that a brief segment of 4^thclass rock climbing is required to enter the rock shelter, discouraging casual visitors.

There are still cultural deposits in a broad but thin and shallow section at the back of Quelkata. While much of the strata along the back of the rock shelter are disturbed sand and river gravels, a cultural level approximately 60cm deep is found across a swath approximately 40m wide at the back of the rock shelter.

Figure 6-32. Profile of extant deposits at Quelkata shown in terms of relative collection units.

Proveniencing

As GPS cannot function in rock shelters, a collection strategy was devised using a datum inside the rock shelter. First, the shelter area was mapped expediently using tape and compass from a semi-permanent datum established on large rock on the north end of the occupation area near the road cut. Artifacts were surface collected from Quelkata in four horizontal collection units that were given ArchID# 986, 987, 988, and 989 to conform to the horizontal collection strategy throughout the survey. The deposits in the back of the rock shelter occurred on natural shelves and the vertical provenience was retained by collecting these shelves from the top (level 1) to bottom (level 5). The lowest level, the shelter floor, appeared to contain a mixture of materials that had cascaded down from above.

Site Collection

In the 2003 fieldwork season 22 flakes and retouched flakes from the rock shelter were collected. These consisted primarily of chert, chalcedony, and andesite. Of the 22 flakes 10 (45%) were made from obsidian, but these obsidian artifacts amount to only 7% of the flaked stone artifacts by weight. A number of bones and goat horns were among the faunal materials collected from the upper levels of the rock shelter, above the rock ledge. It is possible that the horns were placed in this location to dry out.

Chávez Collection

In his Bachelor's thesis José-Antonio Chávez (1978: 52-70) describes and analyzes surface collections that he conducted shortly after the dynamiting of the cave. Chávez includes photographs and drawings of projectile points that appear to be primarily of Type 5B and 5D forms. Chávez reports that he collected 36 projectile points and that the largest group was the concave base form (n = 17) that are probably Type 5B or Type 5D, diagnostic to the Terminal Archaic through the Late Horizon. Of these concave base forms 15 of them were made from obsidian (88%) and the remaining two were chert. Pressure flaking was noted on 16 of the points (Table 6-38).

	Obsidian	Non-obsidian	Totals
Unmodified	434	150	584
Modified	121	57	178
Total	555	207	762
Percent	72.8%	27.1%	100%
P.Pt Base: Convex	7	1	8
P.Pt Base: Flat	8	0	8
P.Pt Base: Concave	15	2	17
Probable Concave Base	12	0	12
Cores	2	3	5
Flakes - cortical	4	12	16
Flakes - noncortical	141	93	234
"Blades"	57	40	97
"Choppers"		5	5

Table 6-38. Counts of Material types by Artifact Form from 1977 Quelkata surface collections (Chávez 1978: 50-72).

A relatively large proportion of the points are non-diagnostic using Klink and Aldenderfer's typology. Three points described as "convex base" appear to be type 3D, a style which persists throughout the Archaic. Chávez notes that a large percentage of the artifacts were made of obsidian, although the identification of the Chivay source, 20 km to the south-west and 1000 meters in elevation above Quelkata, would not occur for another 15 years. Chávez attributes the relatively large percentage of obsidian to the many very small flakes of obsidian that were included in his sample. Had his analysis included weight of artifacts, the relative presence of obsidian by weight would have been considerably lower than that of other material types. It is apparent that obsidian was being transported to Quelkata and worked at the rock shelter from one of the Chivay obsidian source exposures in the study region.

Another notable pattern in these data is the lack of non-obsidian projectile points. This pattern is consistent with the predominantly base-notched (and Series 5) nature of this assemblage. However, results from the 2003 fieldwork show that this is anomalous in the region, even for the Terminal Archaic and onwards.

Discussion

Several of the projectile points that were noted on the top level of the rock shelter (in unit A03-988-level I) during a preliminary visit to the shelter in 2001 were gone from the rock shelter by the fall of 2003. The points required more careful study, but unfortunately this did not occur, and it was hoped that the points would have been retrieved during the course of the 2003 fieldwork.

It is notable that, despite the apparent importance of Quelkata in the regional settlement pattern, there were relatively few Archaic projectile points found in this rock shelter. Based on the evidence from Chávez and the 2003 examination of the rock shelter, the only definitive projectile point styles encountered at Quelkata are from the Terminal Archaic and onward. One parsimonious explanation for the lack of earlier projectile point styles is that the location of this rock shelter, only 5 m above the dry season water line, was insufficient to prevent particularly intense flooding during the Terminal Archaic which removed evidence from earlier time periods. Given data encountered at the site, this description of the Quelkata rock shelter perhaps belongs in the Early Agropastoralist discussion rather than the Archaic Foragers section of this dissertation. However, due to the centrality of this rock shelter in the settlement pattern, the shelter was likely a prominent settlement throughout the prehispanic period and thus it was included here.

A02-3 "Mollepunco"

The rock shelter of Mollepunco (aka Mollepunku, Cueva de Pirita) is one of the principal tourist destinations in the Upper Colca area (Cardona Rosas 2002: 143-147;Hostnig 2003: 52;Linares Málaga 1992: 287, 290, 291, 298) and it probably receives visitation by about ten groups of tourists per week during the high season. Formerly known as "Pirita" the shelter was renamed "Mollepunco" by Eloy Lináres Malaga in 1984 (1990;1992). This dry rock shelter at the base of a partly welded tuff outcrop consists of two principal cavities and with flat floors and sloping ceilings, and a dry outdoor activity area. The principal cavity is 7m deep, 4m wide, and 5m tall. The shelter is approximately 100 vertical meters above the Pulpera valley floor and it is adjacent to a small perennial stream. The shelter features pictographs and petroglyphs of camelid, bird, and humanoid figures that Augusto Cardona (2002: 143-147) argues are significant because they show the transition from pictographs to petroglyph techniques, and the art is believed to have been executed by herders and is therefore no older than 3000 BCE. The art has been interpreted as dating to relatively late periods because plump camelid figures are often shown in herds, and one solitary camelid has what appears to be a rope around its neck. The shelter was excavated by Linares (1992) and despite the gate blocking the entrance of one sector, it appears that the shelter was significantly looted. An open burial chamber probably dating to the LIP is evident high in the southern end of the rock shelter.

Figure6-33. Cueva de Mollepunco (A02-3).

Figure 6-34. Petroglyph of camelid on wall of Mollepunco.

Lithic debris is predominantly chert but a significant portion of the flaked material is obsidian. Bone and LIP ceramics are also evident at the site, perhaps resulting, in part, from the looted burial. Given the heavily visited and previously collected nature of this site surface the 2003 Upper Colca project field crew did not attempt a systematic recording of surface artifacts.

A03-1074 "Pokallacta"

This is a small, sheltered site that has evidence of occupations in both the Archaic Foragers period and subsequent times. The site is immediately to the west of a steep tuff outcrop approximately 100m high. The site is in the shadow much of the day, but it is a sheltered location that is protected and yet offers large views of the river valley.

The rock shelters are fronted by a flat area that today is a corral. This flat activity area is mapped as two Structure Loci though they are essentially one terrace. The two loci delimit the artifact spill zone for each respective rock shelter and each structure locus was assigned the same ArchID number as the rock shelter above it.

ArchID	SiteID	FileType	Description	Area (m2)
1074	1074	Site_a	"Pokallacta"	4,342.7
1075	1074	Struct_a	Southwest shelter	63
1076	1074	Struct_a	Northeast shelter	45

Table 6-39. Loci in Pokallacta [A03-1074].

ArchID	Description	Height	Depth	Width	Height At Back
1075	Residential, pastoral	2.5	9	10	1.2
1076	Residential	2.2	6	5.3	0.9

Table 6-40. Rock shelters at Pokallacta [A3-1074], dimensions in meters.

ArchID	Index	Material Type	Form	Type	Temporal
1074	1	Obsidian	Proj Point Broken	5d	TA - LH
1074	2	Obsidian	Biface Broken	n/a
1074	3	Obsidian	Proj Point Broken	5a	Term Archaic
1074	4	Volcanics	Biface Broken	n/a
1075	1	Chalcedony	Proj Point	5	TA - LH
1076	1	Obsidian	Proj Point	5b	TA - MH
1078	1	Obsidian	Proj Point	2a	Early - Middle Archaic
1080	1	Obsidian	Proj Point	3d	Archaic

Table 6-41. Selected Lithics from Pokallacta [A03-1074].

The bifacially flaked items are largely obsidian but notably the bulk of the grab sample of unmodified flakes was of chert and chalcedony. This reflects the location of the site on the north side of the Río Llapa, and is consistent with a raw material use pattern observed elsewhere on the survey.

A03-1075

This rock shelter has a very thick dung cap and it is difficult to see the ground. The slanting roof and open west side provides a large but only partly sheltered area. It appears that a protective wall was constructed on the west side in the past.

A03-1076

This rock shelter is the more protective residential shelter of the two, offering a view of the river valley and the surrounding terraces.

A03-599 "Callalli 11"

This site is on the east edge of Callalli just beyond a quebrada. A relatively dense scatter of flaked stone and projectile points from two Archaic styles and two later (Type 5) styles were found here, but the artifacts were not sufficiently dense to merit mapping as a low density lithic locus. The site is heavily disturbed by the construction of two roads on either side of it: the modern Callalli access road to the north and a narrow, steep road accessing the soccer field to the west and south of the site.

Figure 6-35. View westward from "Callalli 11" across quebrada shows the eastern edge of Callalli.

This deflated terrace edge area contained flakes approximately one half chert and one half obsidian by count, and 1/4 of the obsidian was cortical. A ground andesite hammerstone weighing 294 g and stained with ochre was also found here. This open air site area offers partial shelter in the form of the quebrada and associated lower terraces that are now destroyed by road construction. The quebrada probably contained water for part of the year.

Figure 6-36. Callalli 11 [A03-599] on terrace on the east edge of the town ofCallalli.

A03-785 "Anccasuyo"

Another possible logistical site was found away from the principal river channel in the area of the colonial site of Anccasuyo. A single type 1A (Early Archaic) or 2C (Middle Archaic) projectile point of chalcedony, broken at both ends, was found here. The temporal assignment is ambiguous because of the broken base. This location is adjacent to a small tributary to the Río Llapa and where an outcrop of tuff creates a small pool that has been developed into a stock pond.

Figure 6-37. Chalcedony projectile point [A03-790] from Anccasuyo [A03-785].

There were two obsidian flakes here, and five non-obsidian flakes. While the Archaic evidence from this site is small, a single point (that could have been scavenged from elsewhere by the colonial occupants), if the context is intact it represents a kind of peripheral, hidden habitation that one might expect to complement the larger residential bases elsewhere in the valley.

A03-675 "Taukamayo" (A02-26)

This area meets the criteria for a possible short term camp or logistical camp during the Archaic Foragers period. A red chert foliate projectile point was found just outside of the principal site of Taukamayo, a site that will be discussed in detail below. The chert point is probably type 3D (incomplete scar coverage) and it is of a style that is only diagnostic to the preceramic period. This location is a bench terrace that is relatively exposed topographically but, as with site A03-599 Callalli-11 there are opportunities for shelter nearby. This site is classified here this as a possible logistical camp during the Archaic because the immediate occupation appears relatively small and exposed for a residential base, but the evidence is conflated with quantities of flaked stone and pottery from later occupations. The site is positioned at the base of a principal access trail to the high country to the south, and close to the biggest river confluence in the region. In other words, there is not a lot of evidence of long term occupation or diversity of activities during the pre-pastoralist period at this site, but the location appears to be positioned strategically with respect to local travel corridors and the monitoring of the river confluence, and the site thus appears to have more than merely a chert procurement location.

A03-806: Sullullumba

A good example of a river terrace provisioning site with evidence of multiple Archaic Period occupations is "Sullullumba" [A03-806]. This site was the only site with purely Archaic occupations in Block 3. It is located up the Colca river from the confluence at Sibayo, and is therefore one of the areas furthest in the study area from the Chivay obsidian source. The site is located on a pronounced terrace edge on the inside bank of a broad bend in the Colca river. Under modern conditions, the area is exposed both to valley winds and by the fact that it lies on the edge of a 40 m steep downslope to the annual high water mark in the river channel.

Figure 6-38. Map of the Sullullumba [A03-806], an Archaic Foragers site showing lithic loci on terrace edge 40m above the annual flood line. Image courtsey of Quickbird DG / Google.

Figure 6-39. Sullullumba [A03-806] along terrace edge above the upper Río Colca. Yellow notebook and scale bar are visible in the center-rear of photo.

ArchID	SiteID	FileType	Description	Area (m2)
806	806	Site_a	Sullullumba	366.6
807	806	Lithic_a	Medium Dens, 10 Obs	169.6
808	806	Lithic_a	High Dens, 10 Obs	21.3

Table 6-43. Loci at Sullullumba [A03-806].

Artifact analysis from Sullullumba

As one of the only single component Archaic Forager sites, seventy-four artifacts collections from this site were given thorough attention in lab analysis. The items below indicate the kind of lithic reduction that occurred on river terraces some distance from the Chivay source.

Obsidian

Obsidian material consisted of two types: clear and clear-banded flakes with no heterogeneities, and grey and black shaded obsidian with heterogeneities. Two broken projectile points and one broken biface were made from obsidian that is presumably of Chivay type material. A single flake of clear obsidian was found highly rotated and with 20% dorsal cortex, placing it at a mid-stage reduction. This obsidian flake was perhaps struck from the biface or the projectile point collected from this site.

Chert and Chalcedony

No pattern was discerned in the color of chert used at Sullullumba, but there was a relatively high percentage of chert and chalcedony in the surface assemblage. From the collection of 74 artifacts from the site, 50% were made of chert or chalcedony. Sixty-five percent of the chert showed signs of heat treating. Interestingly, about half of the chert flakes showed signs of rotation indicating that the potential of chert cores was maximized despite the probable availability of chert in the Colca river. None of the flakes, however, were bifacial thinning flakes and only six flakes had more than 20% cortex. No correlation was noted between (1) the flakes with high rotation index and (2) heat treatment or chert color. Thus, it appears that chert was being procured and preforms were being produced but the final, thinning stages of point production were not occurring at this site or these smaller flakes were not recovered from the surface context.

A number of interesting projectile points were collected here that include a type 4f (Terminal Archaic) point made from clear banded Ob1 obsidian that includes pressure flaking around the haft Figure 6-40. Another point is a likely type 3b (Middle Archaic) point made from red chert with several spines on the haft margin.

(a)

(b)

Figure 6-40. Projectile points from Sullullumba [A03-806]. These include (a) an obsidian Ob1 4F (Terminal Archaic) point [A03-809.1] and (b) and the base of a probable 3b (Middle Archaic) chert point with shoulder spines [A03-810.2].

Figure 6-41. The high density lithic locus A03-808 consisted of aphanytic volcanics and chert.

Complete flakes from this site show highly variable attributes that result from a complete reduction sequence having occurred in the area. A high density locus of flakes made of fine-grained volcanics, chert flakes, and chert heat-shatter [A03-808] perhaps result from a single knapping event. In sum, this site presents evidence of Archaic Period open-air activities a greater distance away from the influence of the Chivay source.

A03-32 "Ichocollo" site cluster in Block 6

Approximately 10 km down stream from Block 3 a cluster of open-air sites along a tributary to the Colca was encountered in a smaller survey area called block 6. This block contains a large fraction of diagnostic Archaic projectile points along with ceramics and projectile points dating to the later Prehispanic period. In the modern geography of the region Block 6 lies immediately above the portion of the Colca valley with intensive agriculture. The Río Challacone descends from the north-east flanks of the glaciated Nevado Mismi (5556 masl) on the north side of the Colca valley, while the Ichocollo drains the south side of Cerro Chungara (5286 masl), a peak that was probably glaciated on its southern flank approximately in the same period of time as the Chivay obsidian source area contained glaciers.

SiteID	FileType	Description	Area (m2)
22	Site_a	"Ichocollo 3"	400.1
29	Site_a	"Ichocollo 4"	36.4
32	Site_a	"Ichocollo 5"	527.5
44	Site_a	"Ichocollo 6"	729.9
61	Site_a	"Ichocollo 7"	1375.5

Table 6-44. Site sizes in Ichocollo [A03-32].

This glaciation may have provided steady water to residents along the eastern tributary stream named Ichocollo. Today, the western of the two, the Challacone drainage, appears to be the larger stream channel and is more scoured out (see geology map in Figure 4-15), a feature perhaps related to the geologically recent large mudslide visible in the geology map as "Ladera Tinday" with the Qr-desymbology.

Figure 6-42. Block 6 Challacone - Ichocollo overview map

Figure 6-43. Ichocollo complex along Quebrada Ichocollo.

Artifacts from Ichocollo complex

Several clusters of lithics and ceramics were identified and divided into sites in this confluence area between the two drainages. The greatest density of artifacts were found on the west bank of Quebrada Ichocollo between the two streams, in an area that is relatively low lying compared to other creek banks in the zone. The area was occupied in numerous episodes in prehistory, as is evident in the diagnostic artifacts that belong to styles spanning all time periods from the Early Archaic to the Inka period. There are a number of environmental characteristics that would suggest that this area would be reused frequently in prehistory. On a local scale, the position of these sites between the two creeks perhaps provided the residents with greater opportunities in both water sources and in lithic raw materials, as cobbles occur in the creek beds. In terms of the position of this survey block in the valley, as was noted previously, the Challacone drainage is at nearly 4000 masl but it is geographically only 3 km to the east of Tuti zone that includes the warmer reaches of the Colca valley below 3900 masl and the beginning of intensive agriculture in modern landuse patterns.

A number of chert and chalcedony nodules were observed in the Ichocollo streambed and the chert was predominantly red in color and was a consistent, homogeneous material with moderately good fracture characteristics. The predominantly red-orange chert nodules in the river are evident in material used for the bifacially flaked lithics found in this site cluster, and 30 of these bifacial tools showed signs of heat treating. Relatively few of the artifacts of any material type, including chert, contained exposed cortex. One chert core had 3 rotations, and chert flakes were predominantly in advanced stages of reduction. Obsidian was of both grey and clear varieties and 27% of the obsidian in the collections had heterogeneities.

Figure 6-44. Photo looking northwest across Ichocollo creek in the foreground, the site cluster that includes "Ichocollo" [A03-32], and Challacone creek below the structure in the background.

	Biface	Retouched Flake	Proj Pt	Core	Total
Obsidian	14	2	5		21
Volcanics	3	1	2		6
Chalcedony	1	1	3		5
Chert	10	5	1	1	17
Quartzite	3				3
Total	31	9	11	1	53

Table 6-45. Bifacially Flaked Lithics from Ichocollo by Material Type

	Length (mm)								Total
	15-20	20-25	25-30	30-35	35-40	40-45	45-50	>50
Obsidian	4	8	3	3	1		1		20
Volcanics		1		1		1			3
Chalcedony			1	2		1		1	5
Chert		1	1		3	3	2	5	15
Quartzite						2	1		3
Total	4	10	5	6	4	7	4	6	46

Table 6-46. Bifacial Lithics at Ichocollo showing Counts of Material Types by Length

An examination of lengths of bifacially-flaked artifacts from the Ichocollo area by material type shows that the immediately-available chert and chalcedony materials are found in bifaces in a range of sizes. Together with the lack of high rates of cortex, these data suggest that the Ichocollo site cluster is associated predominantly with middle-stage reduction. Potentially, decortication occurred in or near the stream bed, while middle and more advanced reduction occurred closer to the residential sites.