THIE ALCHAmOLOGY OF SITE. Ker-74 aB Francis A. Riddell DTI TOD UCTION In JianualJr, 1949, an historic Yokluts cemeteriy located approxima"tely twelve miles duo west of Delano, Kern County, Califoriia in T25SA:23E, lyin in t ervitory cla-imed aboriginally by the `uoiol, wras destr~red by lanc; levelin-. The present dlesiannation for this site is Ker-74, its aboriginal. name is tnilaion. The author, as Assitant Archaeologist of the University of' Califorrnia Archaeological Survey made a study of this site both in the field and in the museumr as part of his regular duties. The cemetery is situated on a natural sandy knoll on the edge of a former slough, and only a few -miles southeast of the former shore--line of Tulare Lake. Approxi-.,;ate1y 1.5 miles southiwest o; Ker-74 is an historic village that was occupied in Octpber, 1854,- thiS iS designated by Gifford and Schenck as their Site 28. 4 It is riot known that a habitation site existed on one of the other rises necr Ker-74. If so, th,.en Ker-74 can be assumed to be the cemetery for such a villag;e; if not, Gifford and Sch-no Ik's Site 28 m:ay possibly be the source for the burials in Ker-74L. Since fragmentary freshwater AMussel shell was evidenced in the earth spread out in the leveling operation it raicht be guessed t'hat there was a habitation site in conjunction writh, or in close proxinity to Ker-74. The artifacts, however, strongly indicate burial association rather than an unassoci;ated occurrence in a midden oe,?osit. Th-e .natrix, as far as coul be ascertainiece, was a fine sancd silt with little or no indicati'rn of charcoal or ash. The site -ras on or near the 22"' co-ntour< elevation which -places it a few f'eet higher th'-an tihe surrount'in, flat terain. Because of its elevation, --et nea;2ess to a slough, Ker-74 vic-2s a natural location for a village aUnd/or a ce-eteryr Present at t,;rhe cdestirn"ct4on o -tle cem-tetery were several local peop-le who wIre intcroafted iln L nreservin, as much -ateriel as oossible f rol.l destruc.-tion by tlhe land-Lc' leveling mach'lines. ItJ was from these persoas thnat I was able to obtain i:?iiZioriation on buria13 amu' artif WORK IN SHI1L The follovring is a list of shells octcuring in Ker-74 as artifacts:21 Olivella biplicata Marine clamishell (sp, ?) MyVtilus californianus Tivela stultorum Hinnites multirugoosus Norrisia norrisii Haliotis cracherodii Haliotis (californiensis ?) Shells occurring in the site but not as artifacts are given in the following J.ist:2s2 Donax sp. Mytilus sp. Marine clamshell (sp. ?) Callistoma (costatum ?) Tegula funebralis Anodonta (freshwater mussel) Planorbidae (freshwater snail) Anadara trilineata (Conrad)23 Clamshell: The species of clamn used for some of the bead specimens is not rli.ina le. Some o.f the specimeLns, limeverr, have been identified )a estultorumad it, cn be assuedthat the unidentified specimens areprtbiy t.e SThe Clamshell beads fall roughly into four categories: a) large thick discs, b) small discs, c) slender turbes, d) long, rectangular (flat in cross-section) forms. - T~p clamshell beads fall into the followuing types as given by Gifford: AVLa, AV2b, Vla, VlaI, VIbI, VUP and Vlg. The latter two types are an extension of Gifford's typoloey. Type AVla: This is a solid rectm gular bar that may be an incipieiorm of Type AV2b; this type is represented by one specimen, 1-103137.. l r e AV2b: These are cylindrical tubes and rectangular or -ateralyTatend tubea. This type is represented by the following specimens:t 1-103150, two specirmens; 1-116081, two specimens; 1-103120, three specimens; 1-103137, one specimeri. Vla: This type is an undecorated disc less than 2.O min. in diameter and often as small as 3*0 . in diameter,. This type is represented by the following: 1-103137, one specimen; 1-103136, about one hundred specimens N a .-l/ p as. - ( a ~ 2' to')I ( A C,. d. I II I I I II I I - ----f I I I ti N I-- --- li -, - r - I---. - 1? ---' 4. I I I e d I I (1) cell 'I/ . I11> k42 II! I W -- II ITo I " v i 1 1 ]I , a II , ii of so I I em I 'if, I0 h i . h' l V A FIGURE 1 EDGE INCISED CLA$SHELL'flISC BEADS (l/i) , - 14 " ueeVVlaIa This, toot is an undecorated disc less than 25*0 mm. in diameter,. ae ifference being that it is from an identifiable species# This type ranges in thickness from 7.0 MM. to 2*0 myi and is of Tivela stultorum* The following speciAens represent this type 1-*103127#TM i ; 1-116094, one specimen; 1.103129, one specimen; 1-116094, sixty-two specimens; 1-103140, one specimens Type VlbI: These are disc beads with a diameter over 25.0 mm. The ?olTeXinFEsocimens are from 8.0 mm. to 12.0 mm. thick: 1-103118, four specimens, undecorated. Vif: Beads of this type are discs under 25.0 mn. in diameter with incidecges (FiP la-d)* Wede125 also shows this bead type, as do .ifford and. Schenck.t6 This bead type is represented by these specimens: 1-103118, one specimen; 1-103140, three specimens. Traces of asphaltum in the incised lines indicate that the incisions were filled at one time with this material to make the design stand out. e Vlgt These disc beads are over 2'.0 mm. in diameter and have incesed77geso The specimens recovered from Ker-74 average about 10*0 mm. in thickness. Two of these specimens are in the UCMA, 1-103140; the others are il the Cornelison Collection (Figg. l.e-h ). Traces of asphaltum occur in some of the incised lines,. Haliotis Shell: Abalone shell ornaments from this site, though "a L.,t o g mmerically small are rather diverse typologically. Gifford's typology is used in describing the following ornament types. The majority of the ornaments are made from an unidentified species of Haliotis; it is unidentifiable simply because in the process of manufacture the ornament loses its distinguishing features4 Haliotis cracherodii is one of the identified species, the other is probably H cali lorniensis,. 1'_p J2aIT is represented by one specimen, 1-103141, and has a drian- e o. cin. The diameter of the perforation is 8.0 mm; the specimen is only 1,0 mm. thick (Fig. 2).. T KlaIV., a spec:imen in the Dorsey Collection, occurred in Burial . Th approxi.Late diameter of the s-pecimen is 2,.7 cmi. This specimen is a disc with one central porfocrxtion (Pi> 2 ). AnothLer specimen of uhis type is 1-118992; thou-gh only one-#alf of the specimen was recovered it was measurable and found to have a diameter of 1.9 cm.. and is lw.5 mm. thick. There were no location data with this specimen. T K2aIII is a disc with one peripheral perforation and is from a species oLf red backed abalone (Fige 2),. The single specimen of this type, however, is broken slightly Gong one edge and may actually have had a second perforation, thus making it Type K6aII.. This specimen,. which has no location, has a diameter of 3,5 cm, and is 3*0 mm. thick. e K5aTI, a single specimen, 1-J16060, is a disc with opposing periphera rations, The diameter is 2.-0 cm and is ]..f5 mm& thick, The perforations appear to have been conically drilled (Fi&. 2).. There is no location information for this specimen - 15-. Type K5bII is represented by three specimens; 1-116057, 1-116059 anc.'. 1 -i507 I these specimens have two opposed peripheral perforations ant pcripheral ixicising,(Fig. 2) . The diameter of the first specimen iq approximattely 2.5 cra though it is not completely circular; it is 1.5 i-I . thick. The second specimen is 2.,3 cm-w in diameter and 2.0 mn. thick* Thhis specimnen has asphaltum filling one perforation. The third specimen has a diameter of 2,3 cm. and a thickness of 2.5 mm, The perforations for the most part appear to lbe biconically drilled fAr all three specimens. There is no location for any of these specimens* rpe SoKaI is represented by two specimens, 1-103126, that have been tnade- arom Haliotis cracherodii shells, (Pigs 2) These ornaments are discs with acent peripheral perforations.. Since the perforations had becn damaagcd or broken out during recovery it is not possible to determine definitely if the perforations were biconically or conically drilledi Due to their relative thickness it may be safely assumed that the former process was followed. Both of these large ornaments are in glood condition and quite well matched, One has a diameter of 9.3 cm. and a thickness of 5.0 mm. The second spepimen is slightly larger with a diameter of 10.0 cm. and a thickness of 5.0 mm., also. These ornaments were in association with a burial that was estimated to have beean about 4 or 5 feet below the surface, no other data were obtained for this burial. T e K6aIII is a disc withl two adjacent peripheral perforations, but diffrinfom the preceding tyorpe in that the species of Haliotis is unidentified (Firrp 2) There are two specimens of this type. Specimen l-1Q3137, wivhich occurred with Burial 4;, is 2.5 cim'. in diameter and 2.5 m=. thick. This specimii-en has as5phalt~urn adhering to its surface. Spec'men 1-116061 is approximately 3.5 cm. in dianeter and 2.0 Am thick; this specimcn has no krnown location from the site* Type K8a is a disc with three peripheral perforations, two adjacen(t a one opposed (Fig. 3). This type is represented by specim.ien 1-116066 -which has a Diameter of 3.6 cm. and a thickness of 2.5 mm.. All three perforations appear to be conically drilledi This specimen has no location recorded for it. A second specimen of this type, occurring in Burial 4, is in the Dorsey Collection and is about the same size as the previous described specimen. Type K8bIII, like the previous type, is a disc with three peripheral pZTrThtions., two adjacent and one opposed. The difference, however, is that this type is incised on the edge of one face (Fjiig 3 ). This type is represented by .specimen 1-116056 which has a diameter of 2.6 cn. and a thickness of 3.0 mm. Alltthroe holes are conically drilled and two have traces of asphaltum in them. No location was obtained for this specimen. T Kl3aII is a disc with two opposed peripheral perforations and one mediaforation (Fig.. '3>4 Specimen 1-103128, the sole representative -of this type., is 2.o c0 . in diameter and 1.0 mm. thick. This particular specimen may actually have had edge incising when made. If this were true the specimen would rightly be classed as Type K13bII. Since the specimen has been worn considerably and has a patination or atain it is difficult to ascertain its original surface features. - 16 - tw K2a, an extension of Gifford's t~ypology, is a disc with two adjacent peripheral and tvwo adjacent medial perforations as well as edge incising on one face (Fig. 3 )t Specimen 1-103128, with no known location data, is the only specimen of this type. The diameter of this specimen is 2.9 cm, and it is 15 mm. thick* Type Q2afV is a more or less rectangular ornament with a single p~orforatho-i atonle end (Fig. 3 ). This type is represented by two specimens, 1-116089 and 1-118990. The first specimen is 1.1 cm. long, 6,0 mm. wide and 1.0 mm. thick; the second specimen is 2.2 cm, hong, 8,0 mm. wide and 205 mm. thick. These specimens have no location data recorded for them. m Q4aII, a roughly rectangular ornament, is represented by a sing1e, s p cE ns 1-116062. This types has two peripheral perforations on onc side (Fig. 3 ). Tae dimensions of this single ornament arc 3.5 cm. x 397 cm. having a thickr,'ss of 2., mm. There is no location rdcorded for this ariracct, Type Q7aTII is a trapezoidal ornament with two opposed peripheral perforations; tho cornors are rounded (Iij. 3 @. A sinlc specimen, 1-103121, is the reprcsentative for this iype. No location was obtained for this specimen. The maxilmum dimen'sions for this artifact are 2.1 cm. x 1J9 cm. The surface of this specimen has exfoliated so that the present thickness is but 1,O mn, T QllaII is a trapezoidal ornament with three peripheral holes, two at one endFnd one at the other (Jig. 3 ), This type, too, is rerprcsented by. but one specimen; no. 1-103121 and has no location given for it, Tlhis specimaien has a maximum estimated length of 2.7 cmt .(the single hole is broken out). Its maximum wi-dth is 1.2 cm, and it is 240 mm, thick* Typo Sla, a rectangular, unperforated Haliotis ornament, is represeted Wvtwo specimens imbedded in asphaltum n specimen 1-103142, a raptorial bird skcull (Fig. 3 )9 Type SlaI is represented by four specimens set in a rectangular asphalt tube- T'he ornaments are rectangular and unperforated and have edge incising. The specimens to which these ornaments adhere are in the Cornelison Collection. Type S2atII is represented by the recovery of two ornaments of this typerom the chest region of Burial 8* These specimcns, 1-116087 and 1-116088, are rectangular pieces with a single perforation at one end (Fig. 4). Type S6aIII is a rectangular ornamenznt with two central perforations and is rresntHe by a single spccimon fron Burial 4. This specimen (Fig. 4) is in the Dorsey Collection* The approximatc dimensions of this specimen are 3.5 cm. x 1*8 cm. Tpe S7aII is represents y one specimen which, like the specimens n1f3 Sla, is set in asphalt in the skull of a raptorial birds The ornament is rectangular with a perforation at each end (Fig. 3). - I7 - Type Slia is a rectangular ornaxfient with three peripheral holes, two at one endarid the other hole at the opposite end (Fig., 3). The only spcclfcn of this type is 1-103123 and has no location recorded for it. It is 4.0 cm. long, 1.4 cm. wide and 2.Q mm. thick, Type S15b, a rectangular ornament with peripheral incising on one face arcT` Xp-Thration in each corner, is representcd by one specimen which is in the Cornclison Collection (Fig. 4) 'the approximate dimensions for this specimen are 2.8 cm,. x 3*.5 cm. T S21, a rectangular ornament, has two perforations in the colners of oneld as well as two medial perforations.. The medial perforations tend to be separate rather than centrally located.. One of the medial perforations of the single specimen 1-116067, has a Type X4 Glivella bead insert held in position by asphalt (Fig.. 4 )G. The other seial perforation has a trace of asphaltum in it so it may be assumed that it, too, had an insert, The, length of this ornament is 5.0 cm. while its maximum width is 3,2 cm. It is 3.0 mm. thick; there is no location for this ornament. Type U2aIII is a triangular type of ornament with a single per- foration {Fi ) Two specimens,, 1-118999 and 1-103137, are the only specimens of this type. The former has no location though the latter is i' from Burial 4. The larger specimen, 1-118999, is. 3.0 cm, long, has a maximum width of 1.4 cm. and is 1.5 mm. thick. The other spccimcn is 1.6 cm. long (an estimate ..ince one corner is broken), 8.0 mm. wide (high) and 1.0 mm, thick. TYpe AP2aII is represenl.ted by five whole specimens and numerous fragmens'rlig. 4) The largest specimen is in the Cornolison Collections All whole specimens have the single perforation at one ends These ornaments are made from the inner rim of the Halaiotis shell. UCMA numbers for the specimens of this type are as follow1T6069, 1-116070, '1-116071 and 1-116087. Thu UCLA specimens have approximate dimensions as follows; 3t5 cm. long, 8-40 mm. wide arid 2-4.0 mm. thick. Thc Corn-elison spocimen is ca. 10.0 case long, 1.5 cm. wide and 4.0e mm thick. There 4s no location for this last speqLmn. Type AQla is a trough shaped ornament somewhat like the previous type. SpcUiicns 1-116088 and 1-116072 are the only two specimens of this type.(Fig. 3). These specimens average 3.5 cm. in length, 1.2 cia. in width and..about 2.0 mm, in thickness& A Haliotis ornamcnt type not given in Gifford' s typolofsr is represntT103139, This specimen is an ovoid ornament 4.0 cm, long, 3.0 cm. wide and 2-3.0 mm*, thick (Fig, 38). This specimen is an. ovoid ring with a perforated lug on one side suitable for suspension, It was associated with Burial 7. Another Haliotis ornament not given in Gifford's typology is represented nagle specimen from Burial 7. The specimen, 1-103139, is a lisc with a large central perforation and with 8 projecting perforated peripheral lugs with a notch or scmiPcircle at their extremities (Fig. 34. The maximum diameter is 3.1 cm. and the diameter of the central pprforation is 14.3 cm* The specimen has a thickness somewhat greater than 10 mm* 00 J2aIV KLaIV KEaII KbII K6aI FIGURE 2 K2aIII K6aItt IHALIOTIS SHELL -D.RNAi:ELtES (1/1). K13aII K8bIII K8a co o Hc LI 0 Q2aIV K20a QhaII 00 Q7aIII0 QllaII l Bo 11 AQla Sla SlaI *. * T# . t- i FI{tT~t 3 HALIOTIS SHELL OI-VA' } .ENAITS (1/1) . Ad 00 0 S2aIII 0 S)$b 36aI11 S21 U2aIII AP2aII U2aIII LI .AP2aIIH S Sla S7aII Slal . .- .I FIGURiE 4 HALIOTIS SHELL OTIRTAULTS (1/1). - 18 - Olivella shells Six types of Olivella beads were recovered from Ker-7428 One whole unmodified Olivella bipl4cata also was -ound, This specimen, 1-103137, was apparnocethe beach as it still has small grains of gravel stuck inside, the shell, It also still retains its purple, brown and white colorings This specimen occurred with Burial 49 The Olivella specimens are given below by type with museum numbers, descrRipton, location and quaitity, Tp C23c, an extension of Giffordts itypology,. is a whole Oliveliplicata shell with the spire ground off and the side in which the natural orifice is located abraded (excluding the orifice) to form a rather large perforation, When beads of this type are strung they form a braid rather than a linear string; the alternating of the beads form two rows on the one string rather than a single rows specimens of this type include the followings 1-103130, two specimens; 1-116053, one specimen; I#}l16084' two specimens 1-118995, threo spceimens; none of thee specimens had their locations 'ocordedq The single specimen l-116090 came from Burial 9. All beads of this type have two perforations, one at the spire and one laterally. T F5b is an Qliclla bilcata shell with the spire ground off1 thus hav3ns i;inglo rrad, ollowig specimens are of this typeO 1103114t three specimens (small) from Burial 5; 1-X03122, one specimen; 1-103124, 18 specimens (small, probably not adtlt shells); 1-103132, throo specimens; 1-103133, 7 specinens; 1-2,16083, 6 specimens; 1-116091, five specimens from Burial 9- i1.18996, 13 specimens, two with asphaltum; l118997, '29 specimens (small), one writh slight lateral abrasion about tho orifice. Type Glb is a cup-1ikd bead made from the spire of an Olivella shell wT aTace of the suture on tho exterior of the beadeip of the spire is ground off giving it 4 single- perforationq The single specimen, l-U603, has no location, .Typ X2b is a disc or oval- bcad from a section of the wall of an Olive~ll bTpicata shell with a trace of the inner whorl at cne end,* Specimens of this type include 1-103113, 32 specimens from Burial 5;' lo-lO3115, four specimens; 1-103125, 37 specimens; and 1-103131, two specimens, There was no location obtained for the latter three groups of beads, This bead type has a single central perforation. ypeX3bZ is a circular or oval bead from Olivella bpilicata shell wtrnt shelf-liko trace of inner whorl, ThE 'ca a i from the body whorl and has an even thicktess but a variable diameter, They have but a single central perforation, The following arc specimchs of this typos 1-103136 three specitcn from Burial 4; 1-116093, 25 specimens from Burial 9; -lll8994, one speci-mon, and 1-118996, four specimens. The last two groups had no location data concerning their recovery, Typc X4 is a small, round, concave-convex bead cut from the thick cnamel of tparictal callus of the Olivclla biplicatep This type has a single central perforation, Specimo is. type ~ aro as follows: - 19 1-116053, three specimens, two with asphaltum; 1-11608Q, six specimens; neither of these two groups of beads have any location* Occurring with Burial 9 are 1-116093, two specimcns and 1-116096, 18 specimens. Fiftoen specimcns, 1-118998, have no location data& WORK IN STEATITE Only a few specimens of steatite were recovered from this sites All of the specimens, however, appeared to have been made from the fine ? rained compact material having the grayish rather than a greenish tone. Wedel 9 suggests that this material may have come from near Lindsay,. Tulare County. Walker30 had previously reported on this quarry and Latta31 states that the local Yokuts Indians in the Lindsay area traded steatite to other Yokuts groups. The coarsely crystalline s eatite usually greenish in color that occurred at Buena Vista Lake was not represented in the artifacts of steatite from Ker-74* The specimens made of steatite found at this site are as followsW one arrowshaft straightener, one tubular bead, onersmall disc bead, one labret or lip plug and a rimn sherd of a vessel. Arrowshaft straightener: The single specimen, 1-103112 (Figs 5bc), was apparently OUT the local collectors in several fragments, probably having been broken at interment. Unfortunately the location and association for this artifact were not obtained. The specimen is a large and an unusually well formed piece with incised decoration on the upper surfaces of both ends, Themaximum length of the specimen is 12,0 cm., the maximum width is 6.7 cm. and the maximum thickness is 6.1 cm. The maximum width of the groove is 2.0 cm. which is the same as the maximum depth of the groove. The groove is quite well polished from uses The outside, though not as highly polished, has been smoothed as evidenced by the striations from the abrading tools Beadsi Specimen 1-103144 is a perforated steatite tube that might be classed as sub-rectangular rather than circular in cross- section. This artifact was found in the skull cavity of Burial l1 The dimensions are.3*3 Qm. long by 1.6 cim in diameters The perforation is approximately 9.0 mm. in diameters This bead is well polished and has a groove at either end of the perforation indicating that through lang continued suspension from a cord through the perforation a single groove or notch was worn on the inside rims at each ends The interior or "bore" of the perforation is quite polished though rings formed at the time of the drilling can still be discerned# From the diameter of the perforation and the occurrence of the rins on the interior it seems quite likely that this specimen was perforated with a stone drilL. A small disc bead, 1-116101, was recovered from Burial 9- The specimen is 6.o0 mmnin diameter and 2*0 mm* thick. It has a single central perforation- a* I I b* I i I I I I I I I I I I I I I I I k I C.. FIGURE S ALABASTER CHARMSTONTE (upper); STEATITE ,ARROWSHAFT STRAkIGHTENER (lower) (1/1). - 20 Lip plug: A single lip plug or labret, 1-103145, was recovered from th-eace region of Burial l1 The diameter of that portion outside of the lip of the wearer is 17 cm&kwhile the section that is "buttoned" into the lip is 144 cm. in diameters The specimen is 8.0 mm. thick and is moderately well finished (p1. lrn) Vessel rim sherd: A- rim fragment of a steatite vessel, 1-103116, occurreIei7hT No location was obtained for this specimen.' This artifact evidently came from a vessel that had been cracked and an attempt. had been made to mend the pot by drilling holes in the walls of the vessels One of the holes is biconically drilled while the other is conically drilled.- Along the edge near one hole arc several notches that may have served to hold the binding that held the vessel together4 Both the exterior and the interior are only moderately well finished4 . The fragment is too small to determine the shape of the entire vessel.' "Crack sewing", the method of repairing broken vessels of steatite by drilling holes on both sides of the crack or break and sewing the tff pieces together is noted in the Santa Barbara coast region by Rosers and from the southern San J oqquin Valley by Gifford and Schenck .- WORK IN CHIPPED STONE Chipped stone of any sort was exceedingly rare in Ker-7h if it can be assumed that the pieces recovered are a representative percentage. Pro~ectile pointss In Burial 4 there were found the tips of two obsidI rojeM.points, Because of their fragmentary condition no type could be assigned them, The lack of any quantity of chipped stone artifacts may be due to the recency of the burials' With the advent of the white man's trade goods the chipping of stone tools. became unimportant, These artifacts are in the Dorsey Collection. Flake araperat Two groups of artifacts that are nothing more than rathertBiiiiTflIes of obsidian 1used as scrapers, and occasionally knives, were associated with burials. One group of twelve specimens,.. 1-103111, consists of thin obsidian flakes of various irregular shapes, These specimens came from Burial 6 on the right side near the ribs, Only one specimen showed any signs at all of secondary flaking; however, nearly all edges showed varying degrees of "use retouch", i.d,* the edges were fractured through use. The second group consists of two specimens of the same type as described above , These specimens, 1-103137, were associated with Burial 4, the burial from which the projectile point fragments wore recovered*. Several other pieces of obsidian occurred with this burial., also, but are not in the UCMA collections. All of the above flake scraper specimens from the two burials average approximately 2,5 c4 'in diameter and about 4..O nu thick, They all appear to have been made from a translucent grey obsidian. 21 The Yokuts from the Tulare Lake rcgion were reported to have supplied other Yolcuts groups vrith obsidian, If this were true it is possible that the lake people got their obsidian from the Coast Range region to the west. However, since the Yokuts supplied obsidian to the Chumash and other peoples on the coast it seems the most of the obsidian used by the Yokuts came from Inyo County. Quartz crystal: No. 1-103119 is a portion of a quartz crystal that has boon fractured by percussion, The measurements of this specimen are 2.1 cm* x 1.9 cm. x l,3cm. No secondary flaking appears on this artifact.. Traces of red ocher appear on its surface on mne end. Quartz ;cryrstals have also Men noted >y Gifford and Schenck as coming from the Tulare Lake region. Walker3 recovered a crystal from a burial at a depth of 40 inches; there is no location data for 1-103119 described above. WFORK IN GROUND STONE Charmnstone: Cnly one artifact that might be termed a charmstone was mcv id rom Ker-74; it is nove in the Cornelison Collection. This specimen was associated with the burial from which the chirch medallions were recovered. The charmstone is of alabaster and is 12'8 cm. long, 6.3 cmo wide and weighs 632 grams. The average width of. the longitudinal groove is 6,00mm., the average depth of the groove is 2.3 mm. There has been a slight battering at both ends but not enough to make.it seem that the regular function of the specimen was as a hammer (Fig. 5a)* Mortars: One mortar, 1-103147, recovered from Ker-74 had apparently been br0inYy the land leveling machinery. Since all of the pieces had been saved, however, the mortar has been reconstructed, Maximum diameter ,a, Maxim= height ..... Sides *.. .; Cavity: Diameter. *. .. . Depth *,......... Lip . Rim ..a......... Bottoni:- Shape*... **9*es*eo Thick~ne s's. .* Finished , . .. ...... hlatcrial r.,,.',,99J Condition ..,... 23.0 cm. 17.8 cm* Convex 18.0 cm. 14.5 cm. Rounded and thin. Ca. 10.0 mm. wid9, wear and breakage. is undulating due to Flat or slightly convex. Ca. 3.0 mm. Pecked all over. Sandstone Complete exeapt for several fragments lost when specimecn was broken by land leveling machinery., This specimen had been much used though was not worn out, - There were slight tracos of red ocher on a portion of the walls of the cavity. There was no location for this piecea, - 22 - A second mortar, 1-103146a, is also made of sandstone and had been slightly damaged when scraped out of the site. Maximum diamotcr*e*-v 31.0 cm, Maximum height *#he.* 23.6 cm.. Sides a Convex-vertical. Cavity: Diameter *........ Car 25'5 cm* Depth . , .. ..Ca4 15#8 cms Lip * ,* .v..te . r Rounded Rim , Flat and cao 1.5 cm.* wide., Bottom: Shape . Conirex to flats Thickness *. C a go 8 cm= Finished * All over. Material *c, .,. Sandstones Condition eowavve-s.ows Good except for about a quarter of the rim which was chipped off before burial and a portion of the remaining rim which was broken by the scraper during the leveling of the sites Thc inside lip of this mortar is worn to form a facet at an angle to the walls of the cavity. There was no information concerning the location of this specimen When removed from the sites Pestles: A pestle, 1-103146b, probably associated with mortar 1-1031467,]isflattish or near ovoid in cross-section and tapers to the proximal end., The material is a granitic stone that has been rather well shaped and polished, Its length is 30.8 cme and it has ca.. 8.0 cm. for a maximum width. As with the above mortar, 1-103146a, there were no location data obtained for this specimens Another pestle recovered from this site is in the Dorsey Collection, It is ca. 20,,0 cm* long, round in cross-section and has rounded endss. The proximal end has a smaller end diameter than: the distal end,. thus giving the pestle a taper. This specimen is well formcd and in good condition. There were no location data obtained for this piece. DIATOMACEOUS ROCK SLABS Two rather unique specimens occurred with Burials 1 and 2e. These specimens wore slabs of diatomaccous rock that had been modified by scraping, smoothing and paintings, The larger slab, 1-103134, was found lying on edge on the right side of Burial 1 near the lower anm* This piece is 35.4 cm*. long, 13.0 cm-, wide at one end and lO6 cm*. wide at the other; it is from 215 to 3) cm, thick.> The surface on one side had been solidly painted with red ocher and then vertical and horizontal lines were scratched on the surface leaving the red paint on in irregular squares. On the reverse side there is at one end a pattern of incised lines (p1. la,b). Another- spccimen similar to the one dscribed above is 1-1031356. This artifact was also laid on its edge but in the vicinity of the upper right lug of Burial 2. This piece is 32,0 cm. long,.l0.0. cm.wide at onc end and 7.G0 cm. side at the other;- it is approxdnately 10*0. m. thick. This piece ias beon entirely stained -with red ocher and has #js black lines extending from one end toward the middle (pl.oc). The Yokuts obtained diatomaceous earth for white paint from the Coast mountains. 39 The material for the above described specimens may have come from this same area., FOSSIL MATERIAL A fragment of a sea shell tentatively idontifiodhO as Anadara trilineata (Conrad) came from Kcr-74 though no location was obtained ? tsThis shellfish was rare and doubtful before the Miocene but abundant from the Pliocene to Recent. This form occurs in the Kettleman Hills oil field in the Pecten and Trachycardium Zones of the Etchegoin formation which is Plioceno in ages. Latta sang that oddities or rare curios had a high trade value to the. Yokutst. If this specimon came from the) Kettleman Hills it is possible that it was picked up by someone on a trading mission to the coast. DAT1IIG Of major importance in establishing dates for Kcr-74 are the brass military buttons and the glass trade beads. I would here like to express mny appreciation for the invaluable assistance given me by Lr. Clement '. Mekighan concerning trade beads and by Mr. Arnold 1. Pilling concerning the military buttons. On the basis of common bead types which occur. in Kor-74 and other sites, the following sites are considered to show a historic connection with Ker-74. These sites were subject to some of the same, trade influences and are presumabJy of the same age,. at least in part* h,; North Shore Kern Lake.,.Kern County., 2. Shasta no. 20. 3* Yoi-13 (Mustang Site).,. 4.X Niios, Alameda C ounty. 5.. Winters Site no.. 3, Sacramento County. 6. Santa Rosa Island Site. no. 24. 7:* Santa Cruz Island Site no. 138.. 8.} Goleta Site no4-l., 9.- Fts-Vaincauvor, Oregon (Hudsonfs Bay )C o). - 24-- Thus, Ker-74 has soimC of the samc typos of glass beads as do sites on the Channel Islands which were presumably subject to Spanish influences. On tho other hand, there is an ovcriap of bead types with Sha-20 -and Yol-13, both of which appear to postdate the 1849 gold rush to California. It is with the first three sites given above, however, that Ker-74 has the greatest number of types of glass trade beads in common. From these apparent connections it would secm that the site was under Spanish trade influences dating back to circa 1810, and that in the later period, 1830 to circa 1860, the same site was receiving trade goods from Amcrican or Hudson's Day Company sourcesb The apparent connection between Ft. Vancouver and Ker..74 is worthy of note as the former was a Hudson-' s Bay trading post. Meighan's trade bead typology4i indicates that Burial 7 dates from 1810-1830. Burial 4 is dated between 1830-1860 as indicated by the association with brass military buttons of knowvn date.* Burial 9 falls into the post 1830 period and is thercfore contemporary with Burial 4# Nine typos of Class beads occurred with P.urial 9, of these nine types five were in common with Burial 4 and two wore in mamnon with Burial 7,. Of those latter two types one f?Om, Type 99, is common to all three burials. Meighan, howcvcr, has found 'hat this bead type, the only one common to all three burials, is quite widespread and apparently not very diagnostic for use in datingd The burial associated With the church medallions quite obviously post-dated the date of 1830 given on the medallionsv. Complete data concerning this burial would have been of prime importance in obtaining valuable information on glass trade beads. The glass beads accompanying the medallions weru considered of slight importance by the finder and consequently were not saved, No date has been assigned to the green glass liquor bottle that was removed fronm a burial; virtually no data were obtained for this burial. This bottle could have come equally well from Spanish sources or from the American period. CONClUSIONS -Of the numerous burials scraped out of Keor74 by heavy land leveling machinery only enough data were obtained from nine to allow burial rccord forms to be made out.. -Out of the nine burials there wore three burials with Caucasian manufactured material associated with the,. It was from those three burials that comparisons and cross-dating with other sites in California and Oregon was at all feasiblo. Despite the lack of proper information concerning these three burials they proved to be invaluable in aiding in the dating and general study of glass trade beads found in California. Caucasian trade articles occurred with both flexed and with c;:tended burials. Both flexed and extended burials, also, were associated with aboriginal material-without any trace of trade material. Depth infor-Mationi concerning the burials scoms to be of little value since relative depths arc unkownom Extended burials occurring at a grcater depth than flexed burials might be interpreted as meaning that with the introduction of thewhite man's shovel the Indians were able to dig deeper gravens The. extended burial itself probably is duo to Christian influ;ncc; hoi.vrevor, a conservative element continued to bury the dead in a flexed position even after contact. Numcrous questions present themselves concerning this Yokuts Indian cemetery that cannot be adequately answLred due to the lack of suffticient detailed information. Additional information, very carefully collected, may at somotimoe in the future be obtained that will be of considerable scientific aid to those interested in the protohistoric and historic periods of the aboriginal groups living in the southern portion of the San Joaquin Valley. Until additional information is made available, however, Ker-74 may well be considered to be a recent Yokuts cemtexry with the majority of the burials dating from about the end of the 18th Ccntury to about Civil War times9 Francis A. Riddell Departmont of Anthropology University of California c a b m n I PLATE I -Specimens from Ker- 74 - 26 - ' NOTES 1 Gayton, 1948, p. 8, map 2*. 2 Kern County site location records of the University of California Archaeological Surveys 3 Gifford and Sclhenck, 1926, p .29 (Coffee survey notes village).. 4 Ibid- 5 Heizer and Mills, MS, 1949. 6 Kroeber, 1925, pl. 72.; 19 , p. .- 7 Q'ifford and Schenck, 1926, pp. 49, 101-105; pis. 2, 7-10. 8 Wedel, 1941, pp. 36,109, 110, 116-120, 122, 124-127. 9 VWIalkerx, 1947, pp.. 6, 28*. 10 Latta, 1949,:p. 173., 11 Meighan, MS, 1950. 12 Walker, 1947, p. 39*. 13 Ibid, p. 36, third string from the left, middle of string.; 14 Gifford, 1947. For type description of all beads and ornaments see respective sections following. 15 Gayton, 1.948 pp. .232, 276. 16 Gifford and Schenck, 1926. pp. 50, 64; pl. 13. 17.Wedel, .1941. p.38. 18 Sample, 1950, p. .20. 19 Identificaticxi by Sheilagh Thompson., graduate student in the Department of Anthropology, University of Californiaa. 20 Walker, 1947. 21-22 Identification by Prof. E.W. Gifford, Director of UC1Ao..* 23 See section FOSSIL MATERIALo 24 Gifford. 1947. 25 Wedel, 1941, pl. 27 Ic and n... 26 Gifford and Schenckt 1926, p1.. 15 a-p.. 27 - 27 Gifford, 1947. 28 Gifford, 1947. 29 '11redel, 1941, pe 53. 30 Walker, 19350 31 Latta, 1949, pp. 65, 69. 3Z Wedel, locN cit. 33 Rogers, 1929, pl. 68. 34 Gifford and Schenck, 1926, pp. 74-75. 35 Sample, 1950, pp. 20-21. 36 Gifford and Schenck, 1926, p. 392. 37 Walker, 1947, Table 1, p. 10, 38 See section Medallions. 39 Sample, 1950, p. 20. 40 This identification was made by Henry T. +lerlyn, graduate student in Paleontology at the University of California, Berkeley. 41 Latta, 1949, p. 65. 42 Meighan, YiS, 1950. 43 Pilling., MS, 1950. * 28 * BIBLIOGRAPHY Gayton, A. He 1948. Yokuts and Western Mono Ethnography, University of California Anthropological Records Volt 10, No, l* Gifford, E.W, 1947# California Shell Artifacts, University of California Anthropological Records, Vol. 9, No. 1, and W. E, Schenck 1926. Archaeology of the Southern San Joaquin Valley, California. University of Caljfornia Publications in American Archaeology and Ethnology, Volt 23, No, age Heizer, R. F. and J. E. Mills 1950. The people of the liountain: the History of Tsurai Village in Trinidad Bay, 1775-1916, us, ffoueh, Walter 1889* Fire-Laking A4paratus in the U.S. National 1aiuseum# House risc. Documents, Vol. 15 Keen, As Myra 1937, An abridged Check List and Bibliography of West North American Marine Lollusca Stanford University Press, Kroeber, A. L. 1925. Handbook of the California Indiansa Bureau of American Ethnology, Bulletin 78. Latta, FF. 1949* Handbook of the Yokuts IndLans, Bear State Books, Oildale, California. kMeighan, CW* 19504 Occurrence and Distribution of Glass Trade Beads in California, M?* Filling -Ao R* 1950. Notes on Several Figured Metal Buttons From California MS#. Rogers, P.B. 1929. Prehistoric Man of the Santa Barbara Coast. Santa Barbara M)seum of Natural IHistory, Santa Barbara, Califonlia* Sample, L, L, 1950, Trade and Trails in Aboriginal California# University of California Archaeological Survey, Report Not 8,, Walker, E&?, 1947. Excavation of a Yokuts Indian Cemetery, Kern County Historical Society, Bakersfield,. Californian, Wttedel, W.R, 1941. Archaeological Investigations at Buena Vista Lake, Kern County, California* Bureau of American Ethnology, Bullstin 130.