:nia ,1 OKADAIEA SHELL MOUND AT HITACHI, BEING AN APPENDIX TO O MEMOIR VOL. I. PART I. OK THE SCIENCE D E P A K T M E N T TOKIO DAIGAKU. ("crn^iVEE.siT-2" OF tok:io.) BY I. IIJIMA, AND C. SASAKI, Students ok Bioi.ogv. PUBLISHED BY TUKIO DAIGAKU, TOKIO. 2543 (1883). t-:^ci ,.._per.TY OF - C3 OUSDAl- OKADAIEA SHELL MOUND AT HITACHI, BEING AN APPENDIX TO MEMOIR A^OL. I. PART L OF THE SCIENCE DEPAETMENT, TOKIO DAIGAKU. BY I. II.IIMA, AND C. SASAKI, Students of Bioi.oriv. PUBLISHED BY TOKIO DAIGAKU, TOKIO. 2542 (1882). J 3 mui PiiEFACE. Til till' summer of 1879, 1 visited tliy ]irovince of Ilitaclil wliiili is uwuly 30 ri distant from Tokio, in order to collect molhisca in the lake of Kasnmiofaiira. Along the coast, there exist numerons fossil remains of marine shells which show evidence that the lake had once heen washed hy the sea in past times. Bearing in mind this feature, I carefully examined the southern coast of tins lake for shell heaps, and was finally rewarded hy discovering three shell mounds on the top of a hill known as Okadaira ; and afterwards found still other mounds at several jilaces not fur from the one previously mentioned, viz. one at Kiliara, two at Ami'iinira, one at Shimadzu ; and on my return to Tokio, I again met with a single enormously large mound at Kitakatnmuia in Shimosa. In the winter of the same year in company with ]\Ir. lijima I again visited the same province in order to make still farther researches in regard to these mounds by the order of Mr. Kato President of Tokio Daigaku. On this occasion, we found a number of other mounds in the same ])rovince already mentioned before, but only one was completely examined, and that was the Okadaira mound which was the largest and richest in ancient remains. The contents of this paper are mainly confined to the contents of this mound, and one of our objects is to compare its features with those of the Omori Shell mounds, which have been well described and accurately figured by I'rof. Edw. S. Morse in the first memoir of Tokio Daigaku. Our thanks are jiarticularly due to the never failing advice of Prof. Edw. S. Morse. Our thatdis are also due to Mr. M. Nishi for the determination of the iiatiu-e of the stone implements and to Mr. II. Yoshida on chemical analysis, ami lastly we are much indebted to our two sincere friends Mr. 0. Taneda, and Mr. M. Kikuchi for their kind assistance in many ways. To the artists Mr. J. Nomura, Mr. M. Indo, and Mr. K. Wat^mabe, our thanks are specially due for the fidelity with which they have made the illustrations. I. IIJIMA. C. SASAKI. Tokio Japan 1st Sei)t. •2542(1882). OKADAIRA .SHELL MOUXD AT 1HTAC1 ]. II.IIMA AND C. SASAKI. GENERAL CHAUACTERS of THE OKADAIRA SHELL MOUND. The Okadaira sIjcU inouiul lies on tlie south western side of a liill called Okadaira, and tlie eastern and western sides of it are already cultivated tor plantations. A wliite appearance due to hroken shells which the ground possesses in tlie vicinity of this hill is due to the remains of former moui\ds which have been scattered and destroyed by the farmers. The length of this mound is estimated about eighteen ken (about 33 m.) in length, and sixteen ken (about 29 m.) in width, and its siuflice is thickly covered with a number of huge trees. Tlie soil covering the mound is aliout si.x inches in thickness. The height of this mound varies from a foot to seven feet. The thickness of the deposit which varies from si.x inches to three feet, is in its deepest parts about si.x feet. The mound itself is nearly half a ri from the lake of Kusmnigaura on the north-eastern side, and also half a ri distant from a branch of the same lake on the west. And furthermore it is distant about five ri (about 12.5 milesl from the sliore of the sea of Kashima (Pacific ocean) of Hitachi. The evidence that the lake was formerly washed by the ocean is shown by ancient historical records ol' Hitachi (Hitachi Fudoki)and also from the presc^nce of fossil remains of marine shells at various exposures along the coast. SPECIAL CHARACTERS OF THE OKADAIRA DEPOSIT. The Okadaira Mound does not show any remarkable difTerence in its features from those of the Omori mounds which are desci-ibed by Prof. Edw. S. Horse in the first memoir of the science department of the University of Tokio in 2539 (1879). As a general rule, objects iditained from such a deposit in both the American and European Continents agree in tlu'ir general aspect, but each deposit has its special characteristics. I'li'l'. .Mor.st- will! i« till- first (liscovt-rer of ;i iiiuiiiul nf this cliaractcr in the l''.iii|iiru ()t° Ja|Niu liius |i(>iiit<-(l nut tlie tollowiiig chiiriu;tt;rs in reganl to thu Oiiiori (l»'|Mitiit : -" Tlie (.)riiiiii (Ifpo.'-itf: arc; iilsci six-ciiilizeil. Firet : liy lli<; |irc8oiiwi of c'luirinoiiH i|U!iiititiL-.s of pottery of iiiaiiy iliffL-riiit shapes, and of an almost inlinite variety of ornamentation. Second : by great scarcity of stone impiementfi, and tlie alwence of arrow lieads, spear jwints and otlier pointed implements of stone. Niit a sinfjio arrow head, (lake or chip lias been found by the various parties who liavi! lieen thine in tlie interests of the University ; and the combined time sjient there, if reprcsenliid by a sinj^le individual, would eijnal over eighty days work of seven hoius eaeh." Thefe peculiarities exiictly agn-e wilh the Okadaini deposit. The objects thus far ibiinil in the Okadaira mound are enuinenited a.s follows : — PoiTKHY. 1 . ( 'iiiikiiij; ve.ss»'ls. 2. Hand vessels. ;5 I5..wls. 4. Tots, rj. Cups, 'i Fni'^meiits (if pDtlery pnssiMy ll^c•ll fnr sinkers. Stonk. 1. Axes. '_>. Celts. ."• Worketl pumice. 4. Stone with circular pit-like depressions. HoKN. 1. ll.iMille. 2. Prongs of deer's antlers. I5()Ni;. 1. Ob calcis of Deer. PO'lTKUY. Many earthern vessels, and fragments of [Kjtteries were collected in the Okadaira deposit of Hitachi. The ves.sels are mainly composed of rough materials, and some of their shapes are extraordinarily ciuious. The pottery is gr-nerajly thicker than thiit of the Umori dejiosit, and mostly ornamented with various designs, plain or unornamented jiottc^ry being comparatively rare. Knobs are generally of large size, and of diversified form. The dimension of the largest one is 200 nam. in height. (Fig. 1, PI. IV). This peculiarity in form has never l)een met with in other deposits, and in most casee. tlie knobs are large and thick, and perforated with from two to six holes which communic:\te internally. This remarkable conformation has not been met with in other jwrts of the emigre, and seems to be peculiar to this deposit. In some the knob is simply a slight projection from the rim. In othere it forms a twi.stt'd loop In other it either projects oiitward, or internally from the inner surface of the rim. Still further, some rims are conical or notched or undulating. The designs are various, but we may be able to cjjissify them generally as follows: — as Prof. Morse has described in the Omori Deposit, "The designs are indifinitely vivried ; generally areas partially or wholly enclosed by curved lines, the area within or without the lines being cord marked, tlie other area being smooth " (Omori Mounds Memoir p. 8). In others, the entire outer surface is cord marked though in some an area near the margin is left which is destitute of the cord marks. Others have deep pits or grooves incised, and in others still the surface is entirely destitute of the cord impressions, and others have a little area near the margin which is separated from the cord-marked area lielow. The cord marks which are impressed on the entire surface of potteries extend as far as their margin. In some cases, potteries are entirely destitute of cord marks. The margins of the potteries are generally smooth and even, but in some cases they are deeply inci.«ed forming a sort of knobbed or undulating appearance. The common ornamentation is either in curved, spiral, or parallel impres- sions or lines. In many ca.ses, lines cross each other regularly giving a reticulated appearance to the surface. The parallel lines are unevenly interrupted, or a numlKjr of parallel lines are interrupted by a zigzag line, or sometimes a number of zigzag lines are arranged one after the other in regular series. The entire absence of legs or knols for the support of the vessel shows in this respect a resemblance to the pottery of the Omori Deposits. The inner surface of rims is, in some cases, marked with two or more parallel grooves. (Fig. 12, PI. IX., Fig. 3, 9, PI. VIII). One hundred and eighty seven bases more or less broken were collected, of which four are marked with the matting impression, and si.x with irregular scratched lines, and the rest are .smooth. The largest Ixjttom thus fare.vamined is about fourteen centimetres in diameter. In a few vessels the base is slightly larger in diameter than the wall of the ves.sel arising from it. Of thousands of speciinens more or less broken, seventeen are sufficiently complete to recognize their entire shajKi. Some are bowl shaped, or cup-like or pot-like. Ten of the pots are bowl shaped of which one is marked with an exquisite ornamentation on the whole area of the bmly wall, leaving a smooth space near the lx)ttora. 1 he rim is provided with a single knob peribrates nuirkeil with ii circular iui|)ressi()n stand re,s|«'clively on each of its angles. The boily wall is smooth, except the upper part of it where two conl marked hands run side by side. (Fig. 7, 8, PI. I). Two cup-shaped pots liave thick walls, and both have smootii liases, and uneven rims. The one (Fig- 5, I'l. 1) is ornamented with incised lines foriniiig rude oval figures. The other (Fig. 1, PI II) is plain, and is somewhat cylindrical in form. Two pots which have a smooth Imttom bulge at the ujiijer part of the body wall, and have flaring rims. (Fig. 6, PI. I., Fig. G, PI. II). The most curious vessel which is nearly complete, measures 3(X) nun. in heiglit. The lower half of this vessel is cylindric.il in form, while the upper half abruptly enlarges in size. The rim is provided with tv\'o knobs, and is marked witli two grooves on the upix»r face. The unstable form of this jiot leads us to believe that it might have been used for cooking, the narrower and lower ]iortion lieing burietl in the dirt or ashes, and the fire built about it. (Fig- 3, 4, PI. I). Of two pots, one (Fig. 2, PI. II) is nearly round, its bottom is ill-defined, and its jjody walls are evenly ornamented with cord im)iressions. The other (Fig. 3, PI. II) is similar in form and size, but lias, besides a mouth, a single small liole, and that part which separates tlie mouth from this hole is slightly arched so as to form a sort of handle. Its body wall is rough and destitute of any impression. The material of this pot is reddish clay. The largest vessel which we have already described ( Fig. 9, PI. II) has the lower half of the body wall ornamented with incised lines and its upper half entirely smooth; and on the boundary line between these two different regions, four small knobs occur leaving a similar space between them. Biuses:— Those with matting impressions are compiiratively few, and their figures are more or less dillerent in ditterent ves.sels. (Fig. .'3, 7, PI. II). The majority of bases are smooth. A single lump of reddish material wivs found associated witli fragments of j)ots. This material which is detxirmined as Ferric oxide (Fe^ 0,) by our friend Mr. ri. Yoshida, seems to have been u.«('d as a mixtrn-e with the clay M 7r ^ PLATE III SHELL MOUND of OKADAIRA. C PLATE IV. Fig. 1. P>ro\vuish red. } natural size. Fi<;. 2. Ke(ldi.ody wall 11 nun. thick, blackish, i natural size. Fig. 5. Body wall 12 mm. thick, reddish, -i- natural size. Fig. (j. Body wall 9 mm. thick, reddish brown, i natural size. Fig. 7. Body wall 14 nun. thick, blackish. ^ natural size. Fig. S. Body wall 10 nun. thick, reddish yellow. !^ natural size. Fig. 9. Body Willi 8 nnn. thick, reddish yellow, z natural size. Fig. 10. Body wall 7 nun. thick, reddish. \ natural size. Fig. 11. Body wall 9 nnn. thick, reddish, i natural size. m i O SHELL MOUND of OKADAIRA. c PLATE VI. g. 1. Body Willi 12 mm. thick, reddish with some black patches. J natural size, g. 2. Body wall 14 mm. thick, reddish above blackish below, f natural size, g. 3. Body wall 10 mm. thick, reddish. J natural size. 4. Body wall 9 mm. thick, blackish, i natural size. 5. Body wall 9 mm. thick, blackish, i natural size. 6. Body wall 8 ram. thick, blackish, f natural size. 7. Body wall 7 mm. thick, brownish red. i natural size. 8. Body wall 11 mm. thick, blackish. J- natural size. 9. Body wall 10 mm. thick, reddish. 3 natural size. g. 10. Body wall 9 mm. thick, reddish above blackish l)elo\v. § natural size. g. 11. Body wall 9 mm. thick, reddish, natural size. g. 12. Body wall 10 mm. thick, reddish black. ?^ natural size. g. 13. Body wall 13 mm. thick, reddish black. J natural size. O' m ^"^ ^ m ^ m ^ PLATE VI i < • SHELL MOUND of OKADAIRA. PLATK VII. Fig. 1. Boilv wall 11 mill, tliiok, hhickish. r. iiatiiinl size. \'\<^. 2. I'oily wall S) iniii. tliick, iTtlilisli black, i natural si/,(\ l"'ig. .3. lioily wall 1) mm. thick, ledJisli. i natural size. Ki;j;. 4. Hotly wall 5> mm. thick, blackish, i uatural size. Vig. f). 15oily wall 11 mm. thick, yellowish grey, i natiual size. Vh^. ('). I'oily wall 12 mm. thick, blackish, w natural size. Fig. 7. Body wall 7 mm. thick, reihlish. Slaigin wavy, i natural size. Fig. 8. Body wall 12 mm. thick, reddish. Ornanieiiteil with a series of dots. ^ natural size. Fig. 0. Body wall 10 mm. thick, reddish. ^ natural size. Fig. 10. Body 9 mm. thick, blackish. ^ natural size. Fig. 11. Body wall II mm. thick, reddish, ^i n.itural size. Fig. 12. Body wall II imii. thick, reddish black. \ natm°al size. Fig. l'^ Mody wall 11 mm. tliick, reddish yellow. ^ natural size. Fig. 14. Body wall 1 1 mm. thick, blackish, i natural size. Fig. IT). Body wall 11 mm. thick, blackish. ?, natural size. Fig. 16. Body wall 13 mm. thick, blackish, h natural size. Fig. 17. Body wall 8 nun. thick, brownish rctl. A natural size. ^ SHELL MOUIMD of OKADAIRA. PLATE VIII. Fig. 1. l?o(ly wall 11 mm. thick, blackish above reddish Ik'Iow. i natural size. Fig. 2. Body wall 12 mm. thick, reddish above blackish below, i natural size. Fig. 3. Body wall 1) mm. thick, blackish. ^ natural size. Fig. 4. Botly wall 9 mm. thick, browuish red. i natural size. Fig. 5. Body wall 13 mm. thick, blackish above reddish l)elow. ^ natural size. Fig. 6. Ifody wall 15 mm. thick, reddish. ^ natural size. Fig. 7. Body wall 13 mm. tliiok, brownish red. i natural size. Fig. 8. Body wall 15 mm. thick, reddish, i natural size. Fig. 9. Body wall 12 mm. thick, yellowish red. i natural size. Fig. 10. Body wall 9 mm. thick, reddish black, i natmal size. Fig. 11. Body wall 10 mm. thick, reddish above, bltvckish below, i natural size. m A % Jj!^ -*■ « ^ ^ P^ PLATE VIII • SHELL MOUND of OKADAIRA. PLATE IX. Fig. 1. Body wall 9 mm. thick, brownisli red. ? natural size. Fig. 2. Ijody wall 13 mm. thick, light yellow. \j natnial size. Fig. .'5. Body wall 7 mm. thick, hlackish. A natural size. Fig. 4. Body wall !• nun. thick, hlackish above greyish helow. y; natural size. Fig. 5. Body wall 7 mm. thick, yellowi.^h grey. I natural size. Fig. G. Body wall 11 mm. thick, yellowish grey above reildish below, i natural size. Fig. 7. Body wall H mm thick, browish red. {. natural size Fig. 8. Body wall mm. thick, blacki.«h. l natural size. Fig. 9. Body wall 10 nmi. thick, reildish. i natural .si/.c. Fig. 10. Body wall 13 mm. thick, blackish aliove reddish below. .', natural size. Fig. 11. Body wall 10 nun. thick, reddish abnvc blackish IkIow. {, natural size. Fig. 12. Inside? surface of ditto showing eight parallel grooves, blackish. i natural si/.(>. Fig. l.'i. Fxidy wall !l uini. thick, brownish red. ^ natiu-a1 size. Fig. 14. Body wall 1 1 mm. thick, reddish. ? nattiral size. Fig. If). Body wall II nmi. thick, gr(\vish. i natiu'al size. Fig. IG. Body wall !• mm. thick, nMldish. -?, natural size. Fig. 17. Body wall >S mm. tiiick, blackish, h natural siz(!. Fig. 18. Body wall 7 imn. thick, lilackish above, reddish below. I uatinal size. Fig. 19. Bodv wall 11 mm. thick, blackish. ^ natural size. ^H A ^ *S % -i^ « ^ PLATE IX '# SHELL MOUND OF OKADAIRA, I'LATK X. Fig. 1. Hotlv wall 7 rmii. tliii-k, ivddisli ijiev. ••{ ii.itmul siw. Fig. 2. IJoily wall 11 nun. tliick, blackish almvt' leililisli bcldw. 3 natural sizi'. Fig. 3. l?roken piece of jiottery notehcd on opposite sides. A natnral size. ditto. i natnral size. ditto. i natural size. Broken piece of pottery with a round hole near the centre, i natural size. Drilled stone, i natural size. Worked stone with three holes communicating internally. § natural size, rt. top. view. Fig. 9. Rude adze made of Tufacious stone. § natural size. Fig. 10. Worked stone broken on either end. Chlorite schist. 5 natural size. Fig. 11. Worked sandstone. § natural size. I'^ig. 12. Ilude adze madi; of Igneous rock. § natural size. Fig. 13. Iiude adze made of (ircywacke sjuidstone. § natural size. Fig. 14. I!ude adze made of Tufa. § natural size. Fig. 15. Worked jnimice with a single perforation, natural size. Fig. 4. Fig. 5. Fig. 6. Fig. 7. Fig. 8. f>^ -r % Is % * « ^ ^ PLATE X SHELL MOUND of OKADAIRA. O Fi^'. 1. KiK .) iMg- 3. Fig. 4. Fig. "). Fig. C Fig- 7. Fig. 8. Fig. y. Fig. K Fig. 11 PLATE XI. Fragini.'iit ot" deer's autler (worked), iiatiiral size. Fragment of deer's antler sliowiiig rude cutting, natural size. Same as above, i natural size. „ ,, ,, natural size. Fnigiuent of deer's antler cut of on either end. natural size. Worked bone, natural size. I'rong of deer's antler, natural size. Os cjilcis of deer (worked), natural size. Fragment of bone witli one end pointed, natural size. KJ. Worked piece of deer's antler, natural size. 1 1 . Fragment of bone with a rude incision. § natural size. m ± w> *s % ifc- « ^ i^ 1^ PLATE XI 1 SHELL MOUIMD of OKADAIRA. LIBRARY UNIVERSITY OP CALIFORNIA SANTA BARBARA 6-/V THE LIBRARY University of California SOUTHERN REGIONAL LIBRARY FACILITY 405 Hligard Avenue. Los Angeles. CA 90024-1388 Return this material to the library Irofn which It wa* borrowed. i?il]tm,K?°''AL UBRABV „r,, ,T,. D 000 356 187 .nllfii 3^05 008113688 Univer; Soul Lit