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Maps, plates, charts, etc., may be filmed at different reduction ratios. Those too large to be entirely included in one exposure are filmed beginning in the upper left hand corner, left to right and top to bottom, as many frames as required. The following diagrams illustrate the method: Les cartes, planches, tableau;^, etc., peuvent Atre filmds A des taux de rdduction diff6ren;s. Lorsque Id document est trop grand pour 6tre reproduit en un seul clich6, il est film6 d partir de Tangle supdrieur gauche, de gauche A droite, et de haut en bas, en prenant le nombre d'images n6cessaire. Les diagrammes suivants illustrent la mithode. 1 2 3 1 2 3 d, R 6 if I ^^ I ; , bi ILLUSTRATIONS 01' THE SIGNIFICANCE OF CERTAIN ANCIENT BRITISH SKTJLL FORMS. ■> ' \ !' t m i From the Canadian Journal /or March, 1863. ILLT7STRATION3 OP THE SIGNIFICANCE OF OEETAIN ANCIENT BRITISH SKULL FORMS. BY DANXEZ. WltSON, tt.D.. PBOFBSBOE 0» HISTOBT ABD aHGXiSH HTJBAIUKB tT,T,,,»c « «-»y«HATU»B, ClUVBBSIXT COUBGB, TOHOHTO. i During a recent visit to 'Wnqlii'ncyf«« t m j facilities afforded me by vZlorZt°'l ^''^^^^'^'f "^ 'he the Smithsonian Institution/to eL^l^iih" ''T'^ '""*'"^ °^ liological collections p-eserved ther? inti i T"'" ""'^ *''° «">- United States ExplorinTEldMon „ I! ^"^ '^T ^"""'^ ^^ "" eating collection 'of huCctS„°' The Z?"^ ^ ? ^^""^ "'"^'• Esquimaux and Tchulitchi TT\ . '"''''"^^' *'"'«« "f disLed Chinook and ot; FlathL Thul /^''T"' ""^ ^^"^ those of other Indian tribp« h^r % at ', ^" "' examples of and of Piji, Kanatrand"'o:L' P ClfsU e^:" 'o"'" ^T™=" opent a short time in Philadelphia chMvt. tt ""y/e'"™ I .tudy of the valuable mater airof the M„rf-''"''°.f°'^'''""''^^ whUe there enjoyed the l^l^n^t II ■ ''°^^^''^''"' ' «■"* with Dr. J. AitkenMeigs!a series on25^ "^' '" """f^^ by Br. Hayes during I Arcrrurn^ ffirr """^ ""'"'"^^ invite to very diverse re,.„.„l,! t VT *''^"' ''"P'^'mmts ; and toafford. ItchaTeedTo?ete '^^ /'^^"^ recalled to an oU snbi Jt J' ,'»>'.»"''"*'»" tad been recently modification o^hefrmr„flrr«v I '''''"™ '" '''' P--"'" very causes which softer llTterthot'ffZ''^'-'' ""° "' «■" a.ection to some r^t^t:^^:;;^:'' "'" «'™ 2 ILLUSTRATIONS OP THE SIGNIFICANCE O, skull. But though on a ZZflit I tT" '"""• ^'""^ crania au object of special ITv tl ' ' ''' ""^ «■■'-■'«■'* ""^-""J the series wa'e u„t tllltoMel-^'T """ff » «''™i''' •' the original ior tl,e fir,t tim" tZ "0™^^/.,""'' ^ '"'" ''"""■''^'» to satisfy me that the remarkahl. f! ] * " '"""""tion «a> "e much more due rartml ilfl ""^ K""""'""' "^ «"" •''"11 .uppose from the views Xhtl in ThTv t" '•'"" *■"" '«* •» to Knowledge* The vert ^1 •^f"**»«'M Contribution, In the original it pres nis «! "T* ''f"^'^' » ^^'^ """""te. before desfgnatedrthe t:crdw!T™'T'^'''''"- broad Battened occiput to its eztreLTn ??,'? "'""P"' fr"™ • tapering with slightlateral swell ?»^ >°^ ''™^"'' •■"* *>=» immediately behind the^xtonr-n,'''''""'''' '" '^'«' '"^'"'th The occiput has been subTecrdtol;?r""' ''''■«'■'»'»' ''»<'• greater extent than is apparent f^m th/f ""^ ^""^^ '» » '»»"'' time it is accompanied by no 2117 ! T"^" ' ''""" the same .uch as inevitably r^snl frl T '"^°^'''''°""'*'''''"™''*«'''°»«. other Flathead tribes !m!r . T'''""' "^ ">« ^hinooks ani « effected by hircSrth'VT''/™™"' '''^'•°™*° modifying the frontaUs much °f , "'"'"' ""■* "o^e^uently On this account, eZTJi^t *' ""' P"™'"' ""^ occipital bones able skull, it is pr'oba rdu so^T* t '""^""^ '» *^'^ -""''k- the cradle-board acting on" h"!^,'" "■," ""'^'''ig-ed pressure of portions and great nafura? n ^ 1 '""''''""■^ brachycephalie pro- arched, the guct pS:t ;z^^^^^ .^'■'' '■"-■'-^ - '•""r bone is essentially d-W from rt T v "^"'""''' "^ "■« fr™*"' very much ossified rand even t! T '^P'" '^'^ ™'"^» «« as 18.«. when discos stg DrMoWsf "f"'^"'^"- '° ^"'^ tjpe pervading the whok ancienr, / . ^ °^'""' ""'fo™ mnial South America, with tie sZL "'?'''™ '"''^^ '"'North and remarked: I thnk it ex L f ^ T^F^'"'^ "^ *•=" ^-'quimaux, I «m tend to the conettn th'f'f"'"' "'"' ''""'" '"vestigaton instead of being Tt, pi al c ar! J • !• '"'"'' "' ^''"™^'' »«'?»'. olasa of artificial modfflSn,f!u"""' P^''"'"^ '""■•o'y *» the American ethnoWis a^ke " VVT'^ "™"'"» '■'"''*«^ *" the ^^1^^^ of ^idelyXfcd lliTrr;"'"' ''''''" "" p. zi, Canadian Journal, yoL ij. p. 40fl. nd nd of ed aa ill h 19 d. b >» I » I CERTAIN ANCIENT BRITISH SKULL FORMS. $ This idea received further confirmation from noticing the almost invariable accompaniment of such traces of artifioinl m. ifi T- with more or le«s inequality in the t.o side' of tt heTd^^'r^^^ extremely transtormed skulls of .he Flathead Indians and of tl Natche., Peruv:ans, and other ancient nations b/7hom the am! barbarous practice was encouraffed. thft extpn* nfV- T/ • ® 8kuU.fbrms,wa3au.llTf„r ' ""'''''""»> *» """^n' British pointing o,.; z sr iX:s rrMirzt '"• r^- Vmmetrical conformation, or irreeularL of fn ' ?''*^" S:=:"-; jrc^f S^^^^^^^^^^ tended, in iL^l^-^C uLT:^'' '''.'''^'''' » infancy, having longitudinal arjelJu^eonstHuraoT* I'r"''""'' ''' ''"' characteristics. eonst.tutea one ot the.r most remarkable of the British Association in 1 «7 .f '"' ^"'''"» "^^t'ng B.ada before leavi g Scotlnd in 1857 O ^^»"''. "^ ""-mtioxS *«»«..> Anna!, u/ .Scotla^^ U IfL to ".' d"°° "• ''^ ''"■ ethnological significance «( ,hJ " . ^ *" » discussion as to the .dding to the Ij^tZTmutZl cmTT" : "P""^'""''^ f" ment. In pursuing suIJ ? ^"' interesting depart- eknlls, andtoZfrZu'r truZTr "' °™'™' ^'-h/cephali^ mound skull of the sl t vX t ™'/"°°™P™'''^- "« ■" '^e occiput which I soon b ™n , ''"'^' Y "" "'"•"P' fl='tt^°i"g of the Sincethenlheiac HtL Z to suspect «as due to artificial causes. collections I,avrWarr»r"7'f^"r"''"™^^ of form of whll th" ZmTn h :, ""' ""'^ "'"' ">" «^"-'">'' varieties a 2 4 ILLUSTRATIONS OV THE SIGNIFICANCE OF pressure of the Indian cradle-board. The examination uud meaeure- ment of several hundred specimens of American cranio, as well as of the living head in representatives of various Indian tribes, have also satisfied me uot only of the existence of dolichocephulio and brachycephalic heads as tribal or national characteristica» but of the common occurrence of the same exaggerated brachycephalic form, accompanied with the vertical or obliquely flattened occiput, which bad seemed to be characteristic of the crania cf tfie Scottish tumuli. There are indeed ethnical differences apparent, as in the frontal and malar bones, but so far as the posterior region of the head it ccncerned, both appear to exhibit the same undesigned deformation resulting from the process of nursing etiil practised among many Indian tribes. The light thus thrown on the habits of the British mother of pre- historic times, by the flkull-form* found in ancient barrows, is replete with interest, from the suggestions it furnishea of ancient customs hifherf> undreamt of. But it has also another and higher Talue to the craniologist, from its thus showing that some, at least, of the pecu- liar forms hitherto accepted as ethnical distinctions, may le more cor- rectly traced ta causes operating after birth. The first example of this pecuUar cranial conformation which at- tracted my attention, as possibly traceable to other causes than inherj- ted characteristics, or natural deviations from the typical skull-form of an extinct race, occurred on the opening of a stone cist at Juniper Green, near Edinburgh, on the I7thofMay. 1851. Soon after the publication of tiie Prehistoric Annah of Scotland, in which the epecial characteristics of the crania of the Scottish tumuli were first discussed, I learned of the accidental discovery of an ancient tomb in a garden on the Lanark road, a few miles to the north-west of Edinburgh, and immediately proceeded to the spot. The cist occupied a slightly ele- vated site, distant only a few yards from the road ; and as this had long been under cultivation as a garden, if any mound originally mark- ed the spot it had disappeared, and no external indication distinguish- ed it as a place of sepulture. A shallow cist formed of unhewn slabs of sandstone enclosed a space measuring three feet eleven inches in length, by two feet one inch in breadth at the head, and one foot eleven inches at foot. The joints fitted to each other with sufficient regular- ity to admit of their being closed by a few stone chips inserted at the junction, after which they appeared to have been carefully cemented with wet loam or clay. The slab which covered the whole projected I i nortioQ n was eavy ; have CERTAIN ANCIENT BRITISH SKULL FORMS. f • over the sides, ho ns effectually to protect the sepulchral chamher from any infiltration of eartH. It lay in a sandy soil, within little more than two feet of the surface j but it had probahly been covered until a com- paratively recent period by a greater depth of earth, as ita iite was higher than the eurrounding surface, and possibly thus marked the traces of the nearly levelled tumulus. Slight ns this elevation was it had proved sufficient to prevent the lodgment of water, and hence the ciat was found perfectly free from damp. Within this a male skeleton lay on its left side. The arms appeared to have been folded over the breast, and the Vnees drawn up so aa to touch the elbows. The head had been suj)ported by a flat water-worn stone for its pillow i but from this it had fallen to the bottom of the cist, on its being detached by the decomposition of the fleshly *' rer and, as is common in crania discovered under similar ci; s, it had completely decayed a\' the part in contact with the - of tiie left side is thus wanting ; but with this exc( not only nearly perfect when found, but the bones are . and the whole skeleton appeared to ine so well preservt u admitted of articulation. Above the right jboulder, « neat ear ihen vase had been placed, probably with food or drink. It contained only a little sand aud black dust when recovered, uninjured, from the spot where it had been deposited by afl'ectionate hands many centuries before, and is now preserved along with the ekuU in the Scottish Museum of Antiquities. As the peculiar forms of certain skulls, such as one described by Dr. Thurnam, from an Anglo-Saxon cemetery at Stone, in Bucking- hamshire, • and another from an Indian cemetery at Montreal in Lower Canada, f as well as those of numerous distorted crania, from the Roman site of Uriconiura and other ancient cemeteries, have been ascribed to posthumous compression: the precise circumstances atten- dant on the discovery of the Juniper Green cist are important, from the proof they aiford that the body orij^inally deposited witnin it, had lain there undisturbed and entirely jnafFected by any superincumbent pressure from the day of its interment. Two, if not three, classes of skulls have been recovered from early British graves. One with a predominant longitudinal diameter, in the most marked examples difi^ers so essentially in its elongated and narrow forehead, and occi- put from the modern dolichocephalic head, that I was led to assign it to • Crania Britannica, Dec. I. p. 38, t Ediu. Philo8oph. Journal, N. S. XVI. p. 269. O ILLUSTRATIONS OJ THE SIGNIFICANCE OF « separate class under the title lcutnl)ecep!ialic.* Another has the Ion- gitudinnl diameter little in excess of the greatest parietal breadth, and is no less strikingly distinguished from the prevailing modem bead,, whether of Celtic or Saxon ureas, bjr its shortness, than thr nchor is by its length, when viewed cither in profile or vertically. Thk» Anglo- ^ Saxon type of skull appears to be intermediate between those two formr. with a more symmetrical oval, fluch ti if of common occurrence in modern English skulls. If cranial conformation has any ethnical eignificance, it appear* to me niconceivable that the two extreme forms above referr»:d to caa both pertain to the same face; and the circumstances under which the most characteristic examples of the opposite tv, es have been found, confirm me in the belief which I advocated when the evidence was much less conclusive, that the older doHchocephaiic or kurabecephalic skull illu?trates the physical characteristics of a race tvhich preceded the advent of the Celtee in Britain, and gradually disappeared before their aggressions. Ao, however, the opposite opinion is maintained by so high an authority as Dr. J. Barnard Davis, tho comparison of the tollowmg measurements, illustrative of the three tvpes of head will best exhibit the amount of deviation in opposite directions from the intermediaU; form. The mensurements arc taken from those furnish, ed in the Crania Britannka, and include the longitudinal diameter, frontal, parietal, and oceij)ital breadth, parietal height, and horizon^ tal circumferenee. No. 1, like the majority of the same class, is de- rived from a megalithic chambered barrow, and has been selected by Dr. Davis as a characteristic example of the class to which it belongs 4 though, according to him, that is on* of aberrant deviation from the typical British form. No. 2. obtained from a barrcM. at Codford m Wiltshire, has also been selected by i)r. D. /is as one of three typical British crania. It is of the same type as the Juniper Green skull, v.^^ Its strongly marked characteristics are thus defii^ed by him: "Itfl most interesting peculiarities are its small size, and its decidedly brachychepahc conformation. This latte* character, which commonly appertains to the ancient British cranium, and even to that form which we regard as typical, is seldom met with expressed in so marked a manner. J No. 3. is a skull from an Anglo-Saxon cemetery neaf Litlmgton, Sussex, one of two of tvhich Dr. Davis reuiarks : "There is . " - ^ ■ — • — - • -■- — -.. — -■- • Prehistoric AnmU of t^cotland, p 177 t Proceedings of the Acad. Nat. Sciences. PhUadelphia, 1857. p. 49. i Crania Jirttamca, Dec. a., pi li. * . r »- CXRTAtIf ANCIKNT BRITISH SKUIX FOIXMS. ••general indication of good .form in tlioae fine cnjjnclous skulls, which i# apparent In every aspect. . . On a review of die whole series of AngIo*Shxon crania which haTC comy midei- ui i* notice, we are led t9 conclude that this plea^.ng oval, nithe? dolichociplmlic form, may beat be dest^rving the epithet of typical among them."^ All the three examples ire male skuUs: 1. Fir/ Chambered Barrow Skull a. Co'lford Skull 3. Litlington Skull.. **•.. b. r. 8.1 6.8 T.5 V. a r. k. 4.» 6.» 4.6 5,T 4.7 5.3 0.il. 5. 5.1 4.6 r. K. S.I 4.7 4.9 B. «. 21. 20. 20.9 Each of the above examples presents the features of the type to ^hicfe it belongs with more than usual prominence, so that if the mea» of a large eeriea were taken, the elements of difference between the three would be less strongly defined. The diilerercea are, how- ever, those on which their separate classification depeaas } and they thus illustrate the special points on which anycrauiOi^sjic^i corrrarison for ethnological purposes must be based. Of the ttiree ska.is, the era and race of one of them (No. 3) are well determined. It is that of ft Sason, probably of the seventh or eighth century, of the race of the South Sa :on3, descended i'tom JE\h and his followers ; and recovered in a district where the permanenry of the same ethnic type is illus- truted by its predominance among the rural population at the present day. Another of the selected examples. No. 2, is assumed by Dr. Davis, perhaps on satisfactory grounds, to be an ancient British, i.e., Celtic Skull. It is indeed a difficulty, which has siill to be satisfac- torily explained, how it is that if this brachycephalic type be the true British head-form, no such prevalence of it rn modern Celtic areas •is to be found, as in the case of Saxon Sussex connects the race of its ancient pagan and christian cemeteries, by means of the characteristic ovoid skull, with the Anglo-Saxon population of the present day. The historical race and era with which Dr. Davis appears to connect the Barrow-builders of Wiltshire, is thus indicated in the Crania Britanruca.—-**Uegion of the Belgee, Temp. Ptolemsei, A.D. 120." The Belgse of that era— then apparently comparatively recent in- truders, and by some regarded as not Celtic but Germanic— were dis- placed, if not exterminated; but the modern Britons of Wales are • Crania Sritanieat Dec ir, pla. 3», 40. 8 ILLUSTRATIOIm.:^ OF THE SIGNIFICANCE OF undoubted descendants of British Celts of Ptolemy's age. Though doubtless mingling Saxon and Norman with pure British blood, they probably preserve the native type as little modified by such foreign adm xture as that of its supplanters in the most thoroughly Saxon or Anglish districts of England. It is therefore a question of some importance how far the extreme brachycephalic proportions of the so-called British type may be traceable to other than inherited ethnical characteristics ; whether in fact it is not entirely due to the unde- signed flattening of the occiput, and lateral expansion of the brain and skull, consequent on the use of the cradle-board. ^ Meanwhile, turning from this supposed British skull of Roman times, to the one derived from Uley chambered barrow, No. 1, the most ancient of the series, and assuming their chronological order to be undisputed, as it appears to be : we find no gradation from an ab- breviated to an elongated form, but, on the contrary, an extreme bra- chycephalic type interposed between the ovoid dolichocephalic Anglo- Saxon of the Christian era, and the extreme dolichocephalic, or kumbe- cephalic one belonging to a period seemingly so remote that Dr. Thurnam, when noting the recurrence of the same type in another chambered barrow at LittLton Drew. Wiltshire, remarked : '■ It is not necessary to admit the existence of any pre-Celtic race, as the skulls described may be those of Gaelic, as distinguished from Cymric, Celts; or the long-headed builders of these long, chambered, stone barrows, may have been an intrusive people, who entered Britain from the South-west. Can they have been some ancient Iberian or Ibero- Phcenician settlers ?"* Among the rarer crania of the Morton collection is one to which a peculiar interest attaches, and which may possibly have some signifi- cance in reference to this inquiry. Its history is thus narrated in Dr. Henry S. Paterson's Memoir of Dr. Morton : During a visit of Mr. Gliddon to Paris, in 1846, he presented a copy of the Crania ^gyp. tiaca to the celebrated oriental scholar, M. Fresnel, and exited his in- terest in the labours of its author. Upv.ards of a year after he re ^eiv- ed at Philadelphia, a box containing a skull, forwarded from Naples, but without any information relative to it. " It was handed over to Morton," says Dr. Paterson, "who at once perceived its dissimilarity to any in his possession. It was evidently very old, the animal matter having almost e ntirely disappeared. Day after day would Morton ♦ Crania Britannica, Doe. iil. pi. ai, (4.) "* CERTAIN ANCIENT BRITISH SKULL FORMS. be found absorbed in its contemplation. At last he announced his conclusion. He had never seen a Phcenician skull, and he had no idea where this one came from ; but it was what he conceived a Phoe- nician skull should be, and it could be no other." • Six months after- wards Mr. Gliddon received, along with other letters and papers for- warded to him from Naples, a slip of paper, in the handwriting of M. Fresnel, containing the history of the skull, which had been discovered by him during his exploration of an ancient tomb at Malta. Dr. Meigs refers to this in his catalogue of the collection, (No. 1352,) as an illustration of *♦ the wonderful power of discrimination, the tactus visus, acquired by Dr. Morton in his long and critical study of cranio- logy." Such was my own impression on first reading it ; but I confess the longer I reflect on it, the more am I puzzled to guess by what classical or other data, or process short of absolute intuition, the ideal type of the Phoenician head could be determined. I suspect, there- fore, if we had the statement in Dr. Morton's ovm words, it would fall short of such an absolute craniological induction. The following is the sole entry made by him in his catalogue : " Ancient Phcenician ? I received this highly interesting relic from M. F. Fresnel, the distin- guished French archseologist and traveller, with the following memo- randum, A. D. 1847 :— Crane provenant des caves sepulchrales de Ben-Djemma, dans Tile de Malte. Ce crane parait avoir appartenu k un individu de la race qui, dans les temps les plus anciens, occupait la eote septentrionale de V Afrique, el les iles adjaoentes." The sepul- chral caves of Ben-Djemma, are s series of galleries with lateral chambers or catacombs hewn in the face of the cliffs on the south- west side of the island of Malta. Other traces besides the rock- hewn tombs indicate the existence of an ancient town there, although no record of its name or history survives. M. Frederick Lacroix remarks, la his Malfe et U Ooze, ** Whoever the inhabitants of this city may have been, it is manifest from what remains of their works, that they were not strangers to the processes of art. The sepulchral caves, amounting to a hundred in number, receive light by means of little apertures, some of which are decorated like a finished doorway. In others, time and the action of the humid atmosphere, have obli- terated all traces of such ornament, and left only the weathered rock. The chambers set apart for sepulture are excavated at a considerable distance from the entrance, in the inmost recesses of ' Memoir of S. G. Morton; Types of Mankind, p. x\. 10 ILLUSTRATIONS OF THE SIGNIFICANCE OF I Ilii the subterranean galleries. The tombs are of admirable design and style of art and the details of their execution exhibit remarkable ingenuity and punty of t.ste The author of the Voyage pittores^ue de S^cde does not hesitate to declare that they surpass in elegance any that ne has seen executed on the same scale. What hand has hewn out these gloomy recesses in the rock ? To that we can give no reply. The chromcles of Malta are silent on this point. Time has defaced problem ''* ''^^'''^''' ^"'' ^'^^'^ *° *^' '^^^^^^^ ^^ ^^^^ JT. '"^'r ''"''^^1' r '^"' "^ ^"*^^"^^y «^°""^ i» Malta Tvtl V7 r^^^'T'^ 5/"°'^' ^"^^"'"'S the Cyclopean ruins *t> led La tourdes Qeants, which have also been assigned by some writers to a PhcBnician or Punic origin, as a temple dedicated to ABtarte ; and the Tadarnadur Isrira, a magalithic structure for which a Pelasgic origin is assumed. But in drawing any comparison between the chambered galleries of Bcn-Djemma and the megalithic cham- bered barrows or cairns of the British Islands, we are at best reason- mg from the little known to the less known indices of prehistoric races ; between whom the points in common may amount to no more than those which admit of a comparison being drawn between the Brachycephah of the British Stone-Period, and the corresponding physical form and rude arts of American gravemounds. Nevertheless the Ben^Djemma skull in the Mortonian collection it not improbably what it has been assumed it to be j and it is in many respectr a remarkable one. A deep indentation at the nasal suture gives the idea of an overhanging forehead, but the superciliary ridgce are not prominent, and the peculiar character of the frontal ' bone U most strikmgly apparent in the vertical view, where it is seen to retreat on either side, almost in a straight line from the centre of the glabella to the external angular processes of the frontal bone. The contour of the coronal region is described by Dr. Meigs as « a long oval, which recalls to mmd the kumbecephalic form of Wilson.*'t It it ia of more importance, perhaps, to note that the remarkable skull re- covered by Dr. Schmerling. from the Engis Cavern, on the left bank of the Meuse, buried five feet in a breccia, along with the tooth of • rhinoceros and other fossil bon.s. appears to be of the same elongatfd dolichocephalic type. Its frontal devel opment ia long and narrow | • Malte et le Gme, p. 21. tCitol»su6ofHumMCrM,l.ta(heic«l.m,rfN.t.Scl.o«..fPkita«.I|4lfc p. a, III CERTAIN ANCIENT BRITISH SKULL FORMS. H and its greatest relative proportions, in length and breadth, are 7*7 by 5*25 inches, so that it closely corresponds in those respects to the most characteristic British kumbecephalic crania.* Whatever be the final conclusion of ethnologists, as to the evidence which led me to adopt that name to indicate the characteristics of a preceltic British race ; the necessity appears to be acknowledged for some such term to distinguish this form from the ordinary dolichoce- phalic type. The Ben-Djemma skull is narrow throughout, with its great, est breadth a little behind the coronal suture, from whence it narrows gradually towards front and rear. The lower jaw is large and massive, but with less of the prognathous development than in the superior maxillary. The skull is, no doubt, that of a man, and the nose has been prominent ; but the zygomatic arches are delicate, and the whole face is long, narrow, and tapering towards the chin. The parietals meet at an angle, with n bulging of the sagittal suture, and a slight but distinctly defined pyramidal form running into the frontal bone. The occiput is full, round, and projecting a little more on the left side than the right. The measurements are as follows : ~ Longitudinal iliameter ,, 7,4 Parietal diameter..... , s.j Frontal diameter , 4, Vertical diameter , 5.3 Intcrmcatoid arch = , 12.3 Intermastoid arch , 15. (7) Intermastoid line » 4*3 (?) Occipito-froQtal arch 14.3 Horizontal circumference 20.2 I hive been thus particular in describing this interesting skull, because it furnishes some points of comparison with British kum* becephalic crania, bearing on the inquiry, whether we may not thus recover traces of the Phoeuician explorers of the Cassiteridei in the long-headed builders of the chambered barrows. When contrasting the wide and nearly virgin area with which Dr. Morton had to deal, with that embraced in the scheme of the Crania BriU mnica, I remarked in 1857 :— Compared with such a wide field of investigation, the little island home of the Saxons may well seem narrow ground for exploration. But to the ethnologist it is not «o. There, amid the rudest traces of primeval arts, ho seeks, and probably not in vain, for the remains of primitive El ^opean allophy* • Natural History Meview, vol. L 12 ILLUSTRATIONS OF THE SIGNIFICANCE OF lice. There it is not improbable that both Phoenicians and early Greek navigators have left behind them evidences of their presence, such as he alone can discriminate.* Before, however, we can abandon ourselves to the temptations of so seductive a theory,— which, after all, finds only such support as may be deduced trom a certain general analogy of cranial form ; and derives no confirmation from the works of art accoiu- panying the remains of the long-headed barrow builders ;— it has ta be borne in remembrance that the question ie still disputed with reference to this class of British dolichocepliflie crania: are they examples of an essentially distinct type, preserving evidence of the cbaracteristics ot a difierent race, or are they mere exceptional aberrant deviations from the supposed brachycephalic Celtic, or British type ? Much stress is laid on the fact that the two forms of skull have occasionally been recovered from the same barrow ; from which it may be inferred that the two races to which I con^ ceive them to have belonged, were for a ntore or less limited period contemporaneous. More than this t cannofc regard as a legitimate induction from such premiaes, ia relation to trania of such extremely diverse types. But this amounts to little; for the same is undoubtedly true of thy ancient British and the modern Anglo Saxon race ; and the discovery of Celtic and Saxon skulls in a common barrow or tumulus of the 6th century is no proof that th© latter race was not preceded by n.any centuries in the occupation of the country, by the Britons, among "-'loui they then mingled as conquerors and supplanters. But the elongated ekulla of the Uley barrow typo are no rare and exceptional forms. They have been most frequently found in tombs of a peculiar character, and of great antiquity Many have been recovered ta too imperfect a state to admit of more being deduced from the fragments than that these conform to the more perfect examples of this peculiar form. Nevertheless the number already obtained in a sujfficiently perfect state to admit of detailed measurement is remarkable, when their great age, and the circum- stances of their recovery are fully considered. Of this the following enumeration will afford satisfactory proof. Only two perfect crania from the chambered tumulus of Uley, in Gloucestershire, — of which the proportions of one are cited above,— have been preserved. But in the later search of Mr. Freeman, and Dr. Thurnam. in 1854, the fragments of eight or nine other skulls were recovered, and of these * OaiKidian Joitmat, vol. it. p. 419. CERTAIN ANCIENT BRITISH SKULL FORMS. 13 the latter remarks : " The fragments are interesting, as proving that the characters observed in the more perfect crania were common to the individuals interred iu this tumulus. Three or four calvaria are sufficiently complete to show that in them likewise the length of the skulls had been great in proportion to the breadth."* Again in the megalithic tumulus of Littleton Drew, North Wilts, at least twenty-six skeletons appear to have been found, from several of which imperfect crania were recovered, and of those Dr. Thurnam remarks; " Eight or nine crania were sufficiently perfect for compar- ison. With one exception, in which a lengthened oval form is not marked, they are of the dolichocephalic class."t So also the four nearly perfect skulls from West Kennet are described as "more or less of the lengthened oval form, with the occiput expanded and projecting, and presenting a strong contrast to skulls from the circular barrows of Wilts and Dorset."^ To these may be added those of Stoney Littleton, Somersetshire, first pointed out by Sir R. 0. Hoare ; || and examples from barrows in Derby, Stafi'ord, and York- shire, described by Mr. Thomas Bateman in his " Ten Years' Dig- gings in Celtic and Saxon Grave Hills;" including those from Bolehill, Longlow, and Ringham Low, Derbyshire ; from the galleries of the tumulus on Five Wells Hill ; and from the Yorkshire barrow near Heslerton-on-the- Wolds. Several of the above contained a number of skulls ; and of the last, in which fifteen human skeletons lay heaped together, Mr, Bateman remarks : *' The crania that have "been preserved are all more or leas mutilated ; but about six remain sufficiently entire to indicate the prevailing conformation to be of iha long or kumbecephalic type of Dr. Wilson."§ The crania occuring in graves of this class mentioned by Mr. Bateman alone, exceed fifty in number, of which the majority are either of the elongated type, or too imperfect to be determined. The others include between thirty and forty well-determined examples, besides a greater number in too imperfect a state to supply more than indications of their correspondence to the same characteristic form. Alongside of some of these are also found brachycephalic crania ; but in the most ancient barrows the elongated skull appears to be the predominant, and iu some coses the sole type ; and of the examples found in Scotland, several • Areheeot. Journal, vol xi. p. 313. Crania Sritannita, Dec. L pi. 5, (6). t Crania Britannica, Dec. lll.pl. 24, (3). j Ibid, Dec. V. pi. 60 (4.) B Archeaologia, vol. xix. p. 47. f Ten Year*' Diggings in Celtic and Saxon Crav* Uilit. p. SSO. I 14 ILLUSTRATIONS OF THE SIGNinCANCE OV have been recovered from peat boga, or others under circumstances more definitely marking their great antiquity. The variations of cranial form are thus, it appears, no gradual transi- tion, or partial modification, but an abrupt change from an extrem© dolichocephalic to an extreme brachycephalic type ; which, on the in- trusion of the new and essentially distinct Anglo-Saxon race, gives place once more to a dolichocephalic form of medium proportions. The three forms may be represented, reduced to an abstract ideal of their essential diversities by means of the following diagram :* Fig. L >Fiff.l Pi?.S. Leaving, meanwhile, the consideration of the question of distinct races indicated by such evidence, it will be well to determine first if such variations of skuU-form can be traced to other than a transmitted ethnical source. The Juniper Green skull, already referred to, pre- sents in profile, as shown in the full sized view ia the Crania Britan^ nica, the square and compact proportions characteristic of British brachycephalic crania. It also exhibits in the vertical outline, the trun. cated wedge form of the type indicated in Fig. 2. In the most stronglj marked examples of this form, the vertical or flattened occiput is a prominent feature, accompanied generally with great parietal breadth, from which it abrubtly narrows at the occiput. The proportions of this class of crania were already familiar to me before the discovery of the Juniper Green example j but it had not before occurred to me to ascribe any of their features to other than natural causes. But the circumstances attending its exhumation gave peculiar interest to what, ever was characteristic in the skull and its accompanying relics, handled for the first time as evidences of the race and age of the freshly opened cist, discovered almost within sight of the Scotish Capital, and yet pert aining to prehistoric time s. The skull was carried home in my • Owing to inaccurate copying on the p»rt of the wood enRriver. tU dia«r»ma. e»pecl»ll» nc. Si do not eorreapond oq opposits sideSj as ths" a«ght to d&» />^ CERTAIN ANCIENT BRITISH SKULL FORMS. 15 in * I* to 1* iB S. )f hand a distance of several miles, and its truncated outline, and still more, its flattened occiput attracted special attention, and gave rise to conversation with my friend Mr. Robert Chambers, who had accom- panied me on this exploratory excursion. With the temptation of a novel discovery, I was at first disposed to recognise the traces of art in this abbreviated form, not only as exaggerating the natural character- istics, but as a possible source of their production. But a comparison with examples of the true dolichocepha!" skull, to which I had already assigned priority in point of time, sufficed to dispel that illusion, and to satisfy me— of what the examination of the corresponding classes of Peruvian crania has still more strongly confirmed, — that no artificial modification can entirely efface the distinctions between two such diverse forms. At a subsequent meeting of the Society of Anti- quaries of Scotland, I accompanied the presentation of the cranium and urn with an account of the circumstances of their discovery, and gome remarks on the novel features noticeable in the skull. Unfor- tunately the printing of the Society's Proceedings, which had been fuspended for some time, was not resumed till the following season ; and no record of this communication was preserved beyond the title. Another skull in the same collection, found under somewhat similar circumstances in a cist at Lesmurdie, Banffshire, has the vertical oc- ciput accompanied by an unusual parietal expansion and want of height, fuggestive of the idea of a combin<'d coronal and occipital compres- iion.* A third Scottish skull, procured from one of a group of cists near Kinaldie, Aberdeenshire, also exhibits the posterior vertical flattening. But a more striking example than any of those appears in the one from Codford, South Wiltshire, selected above to illustrate this type.f Dr. Davis remarks in his description of it : — "The zygomatic arches are short, a character which appertains to the entire calvarium, but is most concentrated in the parietals, to which the abruptly ascending portion of the occipital lends its influence. The widest part of the calvarium is about an inch behind, and as much above the auditory foramen, and when we view it in front we perceive it gradually to ex- pand from the outer angular process of the frontal to the point now indicated." The entire parieto-occipital region presents in profile an abrupt vertical line ; but when viewed vertically it tapers considerably wore towards the occiput than is usual in crania of the same ulass. The cause of the vertical occiput, as well as the oblique parieto-oc- * Crania Britannica, Ikic. it. pi. 16. t/Md.]>ecU.pll4 M 16 ILLUSTRATIONS OF THE SIGNIFICANCE OF cipital flattening in this class of British Crania, I feel no hesitation io believing to be traceable to the same kind of rigid cradle-board as is in constant use among many of the Indian tribes of America, and which produces precisely similar results. Its mode of operation, in eifecting the various forms of oblique and vertical occiputs, will be considered, when describing some of the phenomena of compre'= which he ascribes that distortion. All experience shows that Buch usages are among the least eradicable, and long survive tho ehock of revolutions that change dynasties and efi'ace more important national characteristics. But now that attention has been directed to the subject of unde- •igned changes thus effected on the human head, its full bearings be- gin to be appreciated ; and there is even, perhaps, a danger that mor« cjay be ascribed to them than is legitimate. Such was undoubtedly the effect on Dr. Morton's mind from his familiarity with the results of artificial deformation on American crania; and were we to follow his ex- ample, we should be tempted to designate all the extreme varieties of the elongated dolichocephulio, acrocephalic, and brachycephalic skull* of British barrows, as mere modifications of the same ethnical form. I ILLVfTRATIONS OF TBS •lOlfiriCAltCK Or "1 ', Iq his latest recorded opioions, when commenting on iome of the ab* norni&l forms of Peruviaa crania* he remarks : " I at first found it diffi- eult to conceive that the original rounded skull of the Indian could be changed into this fantastic form ; and was led to suppose that the latter was an artificial elongation of a head remark:^ble for ita length and narrowness. I even supposed that the loug-headed Peruvians were a more ancient people than the Inca tribes, and distinguished from them by their cranial configuration. In this opinion I was mistaken* Abundant means of observaticn and comparison have since convinced ne that all these variously -formed heads were originally of the same ■hape, which is characteristic of the aboriginal race from Cape Uom to Canada, and that art alone has caused the diversities among them.*** The repeated opportunities 1 have enjoyed of examining the Morton- tan and other American collections, have satisfied me of the occur> rence of both dolichocephalic and brachycephalic crania not only as the characteristics of distinct tribes, but also among the contents of the same Peruvian cemeteries,— -not as examples of extreme latitudes of form in a common race, but as the results of the admixture either of conquering and subject races, or of distinct classes of nobles and serfs* most generally resulting from the predominance of conquerors.f Among the Peruvians the elongated cranium pertained to the domi- nant race ; and some of the results of later researches in primitive British cemeteries, and especially the disclosures of the remarkable class of chambered barrows, seem to point to an analogous condition of races. That the Uley and West Kennet skulls may have been laterally compressed, while the Codford barrow and other brachy- cephalic skulls have been affected in the opposite direction, appears equally probable. But auch artificial influences only very partially account for the great diversity of type ; and no such causes, even if brought to bear in infancy, could possibly convert the one into the other form. But as the cranial forms, both of the Old and ^ew World, betray evidences of modification by such artificial means ; so also we find in an- cient Africa a diverse form of head, to which art may have contributed, solely by leaving it more than usually free from all extraneous influ- ences. Such at least is the conclusion suggested to my mind from the examination of a considerable number of Egyptian ekuUs. Among famiJiar relics of domestic usages of the ancient Egyptians is the pil- * Physical Type of the Ameriean Indian, Schoolcraft : |>- 320. t Frthittorie if aw. vol it. |». 82A. canoK 4HCUIIT nmiB wrau. wmiM. » w .lM;