senha i ee capes tos Beles eaee - . Sen “te or tes: ay yee hee Wy wre arsitew See Ea 3 er Bhan: a ee Societe bode es -¥ ba ptiteed ee We Meme som % hg ht se tae aes A> ert 1m yer ge earpiece ra caer Dr cr wren Yea MP AM OVI ae ee ene ane) a A Dy cn, etary =. . . * 3 Pre Vargarepe me aneera! pee Ex. CM an Coe Saat ee ee es orearcoarn Yee a : ee ON Meter Lae NID OTD © peat ae ee ee cal ial afte ete apie ah ysemey tie, ore - nen de ¥ Tah oh Aer Ae ayo te OUR eee Se tte AS : Cee Badd " f Sah onde ASAE aS Male rtd Fa py Pb aatd . ak ioe SES SY ys teenage gee DE ten SUES © et ET oes rt te aep Rapes ea eae he bd ra whoo ng Nee Aaa F 8 me Non iew ne od ater ta mayne Shasta see pe Nethaied gman tent BORG TH ESP EO PIee FOR EDVCATION FOR SCIENCE LIBRARY OF THE AMERICAN MUSEUM OF NATURAL HISTORY J 0 URN Wok, OF THE ASTATIC SOCIETY OF BENGAL, VOL. XXXIV. PARLE IE Nos. I. to [V.—1865.. EDITED BY THE NATURAL HISTORY SECRETARY. RA ne “Tt will dourish, if naturalists, chemists, antiquaries, philologers, and men of science in different parts of Asia, will commit their observations to writing, and send them to the Asiatic Society at Calcutta. It will languish, if such communications shall be long intermitted: and it will die away, if they shall entirely cease.’ Sir Wn, JONES, PLDI IOI CALCUTTA : e PRINTED AT THE BAPTIST MISSION PRESS. 1865. eS Maes. Vere els te. ; 5 5 a eC ei The Editor requests that the reprint of Captain Basevi’s paper on the “Pendulum Operations” be substituted for the copy which appeared in Part II. No. IV. of 1865. Ae ae LIST OF ILLUSTRATIONS IN PART II. 1865. Plate. v I.—Asthenurus Atripinnis, “I.—Gegological sketch map of the ieee hte or en Gras: in Bunnoo, III.—Section across the above, TV .—Section near Buxa, V.—Map of the Yoonzalin Tretnen Vi. Boulder Temple at Kyik-hteo,... NVII.—Kyik-hteo-Galay boulder pagoda, VIli.—Kyik-hteo boulder pagoda, IX.—Paludine and Melanie, SAPP LPP LLP IIIS LLLP III INI Page 2 35 49, 43 106 146 146 146 146 274. CONTENTS. = BOQ OQce~ No. I. (Published 31st May, 1865.) Notes of a tour made in 1863-64 in the Tributary Mehals under the Commissioner of Chota-Nagpore, Bonai, Gang- pore, Odeypore and Sirgooja— By Lt.-Col. T. Darton, Description of a supposed new Genus of the Gadide, Arakan.— By Lieut.-Col. S. R. Ticket, Bengal Staff,................66 On the degree of uncertainty which Local Attraction, if not allowed for, occasions in the map of a country, and in the Mean Figure of the Harth as determined by Geodesy; a method of obtaining the Mean Figure free from ambiguity by a comparison of the Anglo-Gallic, Russian and Indian Ares; and Speculations on the constitution of the Harth’s Onist_biy, ARCHDEACON PRAUT 0. bs. cccse0ahs-rencinereue cece Notes to accompany a Geological map and section of the Lowa Ghur or Sheen Ghur range in the district of Bunnoo, Punjab: with analyses of the Lignites—By Aubert M. Mremermerie Discs ME Dy yo onecn sts endive gs aicee sees svoignape es Scientific Intelligence, ........ Abstract of the Results of the Hones Tideeobetelt Gua tions taken at the Surveyor General’s Office, Calcutta, for the month of January, 1865,..............., Me vela noses aras Baad No. II. (Published 22nd July, 1865.) Remarks on the Vegetation of the Islands of the Indus River.— By J. H. T. Arrenison, M. D., F.R.C.8.E., F.LS., Extr. Member, Royal Med. Soc., Hdin., &c., Asst. Surgeon, eH Meg soe aie gers (i iden etindi isan da paranenieesfes Page iv Contents. : Page Observations on certain Strictures by Mr. H. F. Buanrorp, on W. Tueopatp’s Jr. Paper on the distribution of Indian Gasteropoda in J.A.8., No. CCLXXXIX. Page 69.—By W.. THEOBALD SS tise cis shen Saeed woe sede s ose eee ae Pee 60 Note relating to Sivalik Fauna.—By H. B. Mepuicorv,......... 63 Contributions to Indian Malacology, No. V., Descriptions of new land shells from Arakan, Pegu, and Ava; with notes on the distribution of described species—Ry Witir1am T. Branrorp, AUR. S. Mel GS ..) y ccce sees cues cack cee eae Notes on the Sandstone formation, &c., near Buxa Fort, Bhootan Dooars.—By Captam H. H. Gopwin Austen, F.R.G.S., Surveyor, Topographical Survey. Plate IV.,... 106 Note on Lagomys Curzonie, Hodgson.—By Dr. F. Srotrozka, 108 Abstract of the Results of the Hourly Meteorological Observa- tions taken at the Surveryor General’s Office, Calcutta, for the months of February and March, 1865.,...............c0.08 1x No. III. (Published 23rd October, 1865.) Notes on Central Asia.—By M. Szemenor (Communicated by Lieut.-Colonel J. I. Wanker, WR. We 2. os. .-cenene sees Sonata Als Notes of a trip up the Salween.—By Rev. C. Parisu,............ 135 Notes of Observations on the Boksas of the Bijnour District. — By Dr) J. Uy Stewart, said lars cca eee 147 Religion, &c., among the Karens.—By Rev. F. Mason, a De Mee to the Karen people; Js..scncns seen eee 173 Wotes and Queries, 5.0 ie ciescsenes ocess ate see sa aieetteeee eae eee eee 189 Abstract of the Results of the Hourly Meteorologieal Observa- tions taken at the Surveyor General’s Office, Calcutta, for the month of April, 1865, ............. AreBcOdAdccmnabotade ade nat RON, No. IV. (Published 6th February, 1866.) Religion, Mythology, and Astronomy among the Karens. ia Rey. EF; Mason, D, D.,. .cisisssisascesisstipsass> ssctunne enya Contents. On the Pendulum operations about to be undertaken by the Great Trigonometrical Survey of India; with a sketch of the theory of their application to the determination of the earth’s figure, and an account of some of the principal observations hitherto made—By Capt. J. P. Baservt, R. E., 1st Assistant, Great Trigonometrical Survey of India, Notes on a collection of Land and Freshwater Shells from the Shan States—Collected by F. Frppren, Esq. 1864-65.— By W. THeopap, Jr. Hsq., ........s000. Sas ecbauieis aee'e sin serene RU seE NRE ME EIOMEERETIC OD: « 2occhc sae ec fiva vs cade cpascee dines ves ool sc agains ° Abstract of the Results of the Hourly Meteorological Observa- tions taken at the Surveyor General’s Office, Calcutta, for the months of May and June, 1865,........0006ccesecccsecsnes Meteorological Observations taken at Gangaroowa near Kandy, Ceylon, for the months of March and April, 1864,........... LILLIE Vv Page XXXL Or Gaow: Irom ie Me to Coren cs o.. S82" wihak DA en tatins ooriialhelT 1 2 ReTRENURUS ATRIPININE: Bia Th. —Geeboy ces Bee ae Power Chun “he mi owa by Pesan sr cigeagssuasene a o “Boxa- BRorkane Deora - livtod reat V. “M é Nactonasb dies” se ima ee whee Dovteey 13 Vee Neat kyik-Hhes ! ie W- Ky Lek Hren-Calay: ra ‘ar- Kk ne ies Rovldey a rt The Geological Map will be issued with Part II. JOURNAL OF THE meee tic SOCIETY —}— Part I.—PHYSICAL SCIENCE. No. I.—1865. NN a a Votes of a towr made in 1863-64 in the Tributary Mehals under the Commissioner of Chota-Nagpore, Bonai, Gangpore, Odeypore and Sirgooja—By Lr.-Cou. T. Darron. [Received 2nd September, 1864: | Bonai is a small hilly district lying very snugly isolated from all civilization, between Sarundah the wildest part of Singbhoom and the Tributary Mehals of Keonjhur, Bamra, and Gangpore. It is 58 miles in greatest length from east to west and 37 miles in greatest breadth from north to south, with an area of 1,297 square miles. It is for the most part a mass of uninhabited hills, only 14th. of the whole being under cultivation, but about its centre, on both banks of the Brahmini river, which bisects it, there is a beautiful valley containing the sites of upwards of twenty good, and for the most part cotermin- ous villages, the houses well sheltered by very ancient mango and tamarind trees, with a due proportion of graceful palms. The tal and date appear to grow very luxuriantly in the valley, and sugar-cane thrives there. Many of the villages lie close to the river and their luxuriant groves meet and form long undulating lines of high and well-wooded bank. On all sides, at the distance of a few miles, are hills, some nearly three thousand feet above the level of the valley, and thus a very pleasing and varied landscape is disclosed at every turn of the broad and rapid reck-brqken stream. I bo Notes of a tour in the Tributary Mehals. [No. 1, The Brahmini river in its progress from Gangpore has forced its way through the barrier of hills separating the two districts, and enters the valley I am describing, after a course of eight miles through a beautiful glen, in a succession of rapids and loughs, the latter swarm- ing with alligators. The shortest route from Gangpore to Bonai is by a rugged path through this pass; but is only practicable in the dry weather. Bonaigurh, where the Rajah resides, is in the valley, occupying a bend of the river in latitude 28° 49’ N. and longitude 85° H., being 508 feet above the sea level. It has the river on three sides, and is sur- rounded by a mud wall and moat, within which are about-150 houses, including those of the chief, his court-house, and jail: the village altogether, inside and outside the gurh, contains about 300 houses, but nothing that can be called a bazar. The inhabitants are the Brahmins and other retainers of the Rajah; his own family, including most of the collateral branches, legitimate and illegitimate; people practising trades workers in brass and pewter, potters, weavers, smiths ; and people of low caste, Gonds, Pahans, Ghassees and Domes. Ooriah is the language spoken, and the costume and customs followed are those of the Orissa provinces. This includes a lavish use of saffron in their ablutions, hair neatly dressed with silver ornaments, and a general tidy appearance. They have good features and rather fair complexion. The young girls, till they attain the age of puberty, are very scantily dressed. The only garment usually worn by them is a “ kopin’’—a scarf, round the loins and between the legs. This is national and classical, as we find from the images of the oldest temples, that it was the favourite costume of the Hindu goddesses, who thus enjoyed the full play of their limbs. The young people of both sexes are fond of adorning themselves with wreaths of bright yellow flowers. There are 217 inhabited villages in Bonai, and from the number of houses returned by the topographical survey recently completed, the population may be estimated at fifteen thousand six hundred souls. About one half of the agricultural population is of the “‘ Bhooya’ caste or race. They are doubtless the earliest settlers, and it was from their hands that the ancestor of the present Rajpoot Rajah first ob- tained his insignia as chief. The Bamra and Gangpore Rajahs are reported to have in the same manner derived their chieftainships from 1865. ] Notes of a tour in the Tributary Mehals. 3 the Bhooya aborigines, and when a succession to the Raj takes place in any of these districts, the acknowledged head of tho Bhooya clan goes through a ceremony of making over to the new chief the country and the people. The person who claims this prerogative in Bonai is titularly called “‘ Sawunt.’”’ He holds, at the very trifling quit-rent of Rs. 18 a year, twelve villages with their hamlets, and claims to be the hereditary Dewan of Bonai, but the chief neither employs nor acknow- ledges him as such. There are two other similar tenures with the titles of ‘ Dhunput’ and ‘ Mahapater,’ and subordinate to them are certain privileged heads of villages called Naiks. Under the Sawunt, Dhunput, or Mahapater, the subordinate officers of the Bhooya militia, —all the able-bodied males of the tribe are bound at the requisition of the chief or of the Government, to turn out for service fully armed and equipped. ‘There are no military tenures in the hands of people of any other caste. The Bhooyas thus have great power in the little state. Nor is it only in consequence of their being thus orga- nized as a military body; I find they have also charge of the oldest temples and shrines, and discharge the duties of Levites to the exclu- sion of Brahmins. Yet the temples are dedicated to Hindu gods. Whatever their origin may be, the Bhooyas are now completely Hin- duized. They have no peculiar language or customs of their own. In Bonai and the southern parts of Gangpore they speak Ooriah. In the northern parts of Gangpore and Jushpore, Hindi. They are a dark-complexioned race, with rather high cheek-bones, but with nothing else in feature or form to distinguish them as of extraneous origin. According to their own traditions, they were once a great peo- ple in Hastern India and had a king of their own, but were dispersed by invasion from the west. They are now found in all the districts between Cuttack and Behar, but they are most numerous in this and the adjoining estates, and here may be found the most civilized and respectable and the most primitive of the family. While in the low- lands, they dwell in villages, clothe themselves decently, and otherwise follow the customs, adopt the manners, and, I may add, the intriguing nature of the more civilized Brahminical races. In the hills of Bonai they are found as naked, as simple, as truthful and unsophisticated as the wildest of the Cole tribes. There are a great number of Bhooyas in the Singbhoom district, and it is said that they were driven out of the west portion of it, by the advance and spread of the Lurka Coles. 4 Notes of a tour in the Tributary Mehals. [No. 1, The Bhooyas call themselves ‘ children of the wind’ ‘ Pawun buns,’ this would establish their affinity to the Apes, as Hunooman is called “ Pawun-ka-poot,” the son of the wind.* The Bonai hills shelter some thousands of the race commonly called Coles, who all represent themselves as having at some period emi- grated from Singbhoom or Chota-Nagpore. They have not benefited by the change. Their brethren on the Chota-Nagpore plateau and in the plains of Singbhoom are better off and better looking. The emi- grants must be the most unimprovable of the race, who, finding that the old country is becoming too civilized for them, fly from the clear- ances they have made, hide themselves in the hill forests, and relapse into the condition of savages. Amongst the races of Bonai yet to be noticed, are the Kolitas, a very enterprising and respectable class of cultivators, that are found in these regions, Sumbulpore, and strange to say, Assam. A very large proportion of the purely Hindu part of the Assa- mese population are Kolitas, and in accounting for the different races that are found in that province, the antecedents of the Kolitas have always been a difficulty. They have none of the peculiarities of the Indo-Chinese stock. They are considered, in Assam, as of very pure caste, next in dignity to Kaists, and are on this account much in re- quest amongst the higher classes as house servants. Another difficulty in Assam was te account for what was called the Bhooya dynasty, of which traces are found all through the valley, and it is recorded in their history, that the north bank of the Brahmapootra above Bish- nath was known as the country of the Barra Bhooya, long subsequent to the subjugation of the districts of the southern bank by the Ahoms. It appears to me, that there is a strong reason for supposing that the purely Hindu portion of the Assamese Sudra population was originally from this part of India. There is, in idiom especially, a strong resem- blance between the Assamese and Qoriah languages, and though the Moriah written character did not take root in Assam, this may be owing to all the priestly families having been introduced from Bengal.+ * They very probably formed a division in Rama’s army, hence their adoption of Hunooman’s pedigree, and their veneration for “ Mahabir.”’ + In a paper in the Asiatic Society’s Journal for June 1848, the Assam Kolitas are described by Col. Hannay as‘having the high and reoular features of the Hindu, and many of them with the grey eye that is frequently found amongst the Rajputs of Western India. 1865.] Notes of a tour in the Tributary Mehals. 5 The appearance of the Bonai Kolitas reminded me very much of the Assam Kolitas, and I may mention that Ram Chunder, the seventh Avatar, is the favourite object of worship with both. Of the mineral and other resources of Bonai, I have not much to say. Iron is produced, but the hills are for the most part quite unex- plored, and their riches, if they possess any, unknown. The popula- tion, with so much room for expansion, does not increase. There are 83 deserted village sites, and what are now small hamlets appear to have been at one time large villages. The cause is not apparent, as the people of the more civilized class are well to do and content, and rent is very low, and as in all the Tributary Mehals, fixed. It is Rs. 2-8 for a hull of 17 khundees. Nevertheless the chief tells me he is obliged to grant all manner of extraneous indulgences to his ryots to induce them to remain. Wild beasts are very numerous, and in their ravages lies one great difficulty that villages bordering on or in the jungles have to contend against—the ryots complain not of loss of life but of the destruction of crops. They say they have to raise grain for the beasts of the forest as well as for their own families. On this account very little cotton is cultivated, though the soil is well adapted for it. The store of Sal timber in Bonai is immense, but the isolated and almost inaccessible position of the forests will prevent their being utilized for years to come, except for the resin, to obtain which, so many noble trees are girdled and killed. Together with the Sal, are found vast quantities of the Asan tree on which the tusser silk-worm feeds, and a considerable quantity ot the wild tusser is exported from Bonai, but it is not much cultivated as the mass of the population look upon it as an impure or unorthodox occupation, and none but people of the lowest castes, the Domes, Ghassees, Pahans and Gonds practice it. (The Gonds are out of their element in Bonai and are thus classed.) We meet with no Rajpoot or Khettree family except that of the chief. Nothing can be more absurd than the tradition handed down to account for this possession of power by one Khettree family over an alien population. The Nagbungsi family of Chota-Nagpore admit that they are sprung froma child found by and brought up in a “ Moondah’’* family, and that this child was made chief of the whole * Kole. 6 Notes of a tour in the Tributary Mehals. [No. 1, Moondah race. It is I think highly probable that the chiefs of Bonai and Gangpore were originally Bhooyas who becoming leaders of their people and Rajahs, and allying themselves by marriages with other Rajahs were gradually admitted into the fraternity of Rajpoots or Khettrees. It may be said indeed of both of them, that the inter- marriage with families of better certified Khettree descent has not yet obliterated their Bhooya lineaments, for they bear a very remarkable likeness to that race in feature. GANGPORE. This is a very extensive estate lying between Chota-Nagpore, Jush- pore, Oodeypore, Sumbulpore, Bamra, Bonai and Singbhoom. It is kidney-shaped. Its greatest length from east to west is about 97 miles, and in breadth from north to south it varies from 15 to 50 miles. The topographical survey of the estate is not yet complete and its area cannot therefore be computed with accuracy, but I estimate it at double the size of Bonai or about 3000 square miles. Of this area not more than a tenth is under cultivation. The Sunkh and Koel rivers from the plateau of Chota-Nagpore, unite near Gurjun in Gangpore and form the Brahmini. The Keb, another river of some magnitude, flows through Gangpore south on its way to the Mahanuddee. ‘The ordinary level of Gangpore is about 700 feet above the sea; the highest hill yet noted by the topographical surveyor is 2,240, not much above the general level of the Chota-Nag- pore plateau. The descent, however, from the plateau to the ordinary level of Gangpore is gradual, and there is a tolerable road. As in Bonai, the majority of the population are Bhooya, and they were no doubt the first settlers. All the zemindars under the Rajah are of that race, and hold their estates as fiefs at low fixed rates and terms of ser- vice. Consequently the Rajah is under the necessity of adopting a con- ciliatory policy towards some of them at least. There are generally one or two in opposition, but fortunately for the Lord Paramount, the great vassals are too jealous of each other readily to combine. The largest estate is held by the vassal who bears the title of Mahapater. It borders on Singhbhoom, extends to the Brahmini river and com- prises 100 villages for which the Mahapater pays only Rs. 200. This part of Gangpore was at one time more densely populated than it is at present, but all the more peaceably disposed of the old inhabitants 1865.] Notes of a tour in the Tributary Mehals. 7 including, it is said, several colonies of Brahmins, were slaughtered or driven out of the country by the Lurka Coles. To the south, another great vassal, under the title of Gurhoutea, holds the Hemzeer estate, consisting of 84 villages, and an unlimited run of hill and forest. Gungadhur the Gurhoutea, boasts that he can travel twenty-four miles in a direct line over his own ground without seeing a human habita- tion, all through hill and forest, which, united to enormous tracts of hill and forest of Raigurh and Sumbulpore, forms perhaps the most extensive uninhabited region in all India. The third of these vassals has his estate on the north-west of Gangpore and holds the passes into the country from Jushpore and Chota-Nagpore. This estate is in advance of the passes, and looks as if it had been filched from Jush- pore, to which from the geographical features it ought to belong. The chief is of the ‘ Seekur’ family and claims connectionship with the Rajah of Pachete. His ancestor the first Rajah of Gangpore, was, we are told, invited by the Bhooyas to take charge of their country ; from which, it is said, they had just expelled a Rajpoot family called the ‘‘ Kaiserbuns ;” but as I stated above, I think it more probable that the ruling family are descended from the original Bhooya chiefs. The traditions, assigning to them a nobler birth, are founded on the sup- position that the Rajpoots or Cshetryas were the only class qualified to rule, that where there was no one of this class over a nation or a people, “the Guddee”’ was vacant, and a Cshetrya had only to step in and take it. The Cshetryas must have wandered about like knights- errant of old, in search of these vacant Guddees, as we do not find in the country any descendants of the followers whom they must have had, if they came in other fashion to oust the native chiefs and seize the country. It was admitted to me that until these Tributary Mehals came under British rule, a human sacrifice was offered every third year before the shrine of Kali at Suadeeh, where the present Rajah resides. The same triennial offermg was made in Bonai and Bamra, Bhooya priests officiating at all three shrines. This fact appears to me to be confirmatory of the theory that the Hindus derived from the abori- ginal races the practice of human sacrifices. In the above named districts, the practice of widows going “ suttee”’ was also generally followed in the family of the chiefs and in Brah- 8 Notes of a tour in the Tributary Mehals, [No. 1, min families, up to a recent date; many of the grandmothers of the present generation of chiefs and Brahmins having so distinguished themselves. One man was pointed out to me as having lost his mother by the rite of suttee. He would not say ‘lost ;’ he no doubt regards her as canonized by the act. A rather romantic story of a suttee that occurred some fifty years ago in Gangpore is related. A Brahmin took a dislike to a girl he had just married, and turned her out of doors, a wedded maid. She took refuge with her parents who were poor, and who soon after died, leaving her destitute; then she wandered from village to village subsisting on alms and leading a wretched widowed life. Her husband married a second time, and sons and daughters were born to him and grew up about him, and in the fullness of years he died. His second wife had preceded him, so his corpse was placed alone on the funeral pile, and the torch was about to be applied to it, when a poor emaciated and meanly clad female stepped forward, and as the first, the faithful and only surviving wife of the deceased, claimed the right of suttee. Her request was com- plied with. Bathed, anointed, clothed, and adorned with flowers like a bride, she ascended the pile and clinging to the corpse of the hus- band who had so cruelly discarded her, and for the first time in her life pressing her lips to his, the flames arose and their ashes were mingled together ! There is no doubt still a strong sentiment in favour of suttee in the Tributary Mehals, and States under native government. Its prohibition has not been long enforced in the eastern parts of Rewa. Not long ago, in that territory, on the death of a Brahmin, his widow, notwith- standing the prohibition, was so vehement in her desire to join her husband on the pyre, that her relatives as the only method of restrain- ing her, locked her up. When the ceremony was over they proceeded to release her, but found that her spirit too had fled. She had attained her object, as my informant declared, by a special interposition of Providence in her behalf. Proceeding north-west from Nugra and the banks of the Brahmini river, you enter the Nuagurh division of Gangpore and come to Lainggurh, near the confluence of several streams, which was once the capital and promises to be so again, as the present Rajah is just now 1865.) Notes of a tour in the Tributary Mehals. 9 building there. It is very prettily situated, and the gurh ona little hill in the centre of the valley has a commanding position, but I fear it is not a healthy site, from the number of enlarged spleens and cases of skin-disease I observed amongst the people. There are many fine old village sites in Nuagurh, now occupied by impoverished squatters, mostly Oraons from Chota-Nagpore. The old inhabitants have died off or removed to more civilized and: securer regions further south. The shabby huts of the squatters hud- dled together under the shade of the grand old trees, the monuments oi the more civilized race that. preceded them, look as much out of place as mud cabins in a street of palaces. The Rajah and other zemindars give these new settlers, when they first come, three years of absolute immunity from demands of every kind. In the fourth year: they are called on to pay a light assessment. It is difficult to describe on what principle it is imposed, but in old settled villages of Oraons it does not amount, including rent and contribution, to more than Rs. 1-8 per house or family. The soil in this part. of Gangpore ap- pears very fertile, and there is still available much of the slightly swampy, rich looking land, that gives the best crops of rice. I find “ Sirosha”’ now in flower, growing in great luxuriance, It is sold here at one maund for the rupee. The Coles are evidently a good pioneering race, fond of new clear- ings and the luxuriant and easily raised crops of the virgin soil, and have constitutions that thrive on malaria; so itis perhaps in the best interest of humanity and cause of civilization that they be kept mov- ing by continued Aryan propulsion. Ever armed with bow, arrows and pole-axe, they are prepared to do: battle with the beasts of the forest, holding even the king of the forest, the ‘Bun Rajah,” that, is the tiger, in little fear. Mixed up with them are numbers of the Kherria tribe, who are as-yet a mystery to me, and I will say nothing more about them till I learn more. Jam. assured that they have no affinity with either Moondahs or Oraons, ¢. ¢. with those who are generally called Coles. Borgaon, near the Mahabeer hill on the borders of Bamra, is the largest village Gangpore possesses on this side. It contains 160 houses— 20 of Brahmins, 20 of ‘ Telis,’ oil-pressers, 22 of various Hindu Ooriah castes, and the remainder Oraons and Kherriahs, The two 2 10 Notes of a tour in the Tributary Mehals. [No. 1, latter coming in contact with Brahmins, have at once succumbed and become their farm labourers. It appears to make little difference in the condition of Oraon emigrants, whether they are farm servants or farmers on their own account : they have the same wretched huts, scanty apparel, and generally uncared-for appearance, as if they had in despair given up all ideas of rendering themselves attractive; but the wonder is that they remain in this dependent position, when they can get land on such easy terms and become farmers themselves. The village pays direct to the Rajah a rent of Rs. 34, magun or contribution Rs. 34!, and 64 maunds of rice. The price of rice is from one maund to two maunds for the rupee. On births, deaths and mar- riages in the Rajah’s family, the villagers are called on for additional contributions, and when that family, as it is just now, is a large one, the extra charge comes to from Rs. 30 to 40 a year. The total demand is therefore about Rs. 160 a year, and from the extent of land under cultivation, I do not think this would amount to more than 3 annas a beegah on the cultivated area. It is evidently a very old village site, surrounded by extensive groves of mangoes, and with several tanks of very insalubrious water overgrown with water lillies. Hills are seen on all sides, but the most remarkable feature in the landscape is the great Mahabeer hill; a mass of rock tilted up, and shewing towards Borgaon, an uneven wall of disrupted ends, forming a cliff of fantastic outline, nearly 2000 feet high. The tutelary deity of this hill is a favourite object of worship with the Bhooyas, and is more or less revered by all the country. The top of the hill or rock being difficult of access, Mahabeer has studied the convenience of his votaries, and entered an appearance down below in the form of a stone, in a sacred grove or ‘Surna’ at the foot of the hill. The idea of a ‘ Surna’ is pretty and poetical. It is or ought to be a fragment of the primitive forest left when the first clearance was made, as a refuge for the sylvan deities whom the clearing might have disturbed. The best villages and most thriving portion of the popu- lation in Gangpore are found on both banks of the Heb river, as we approach the boundaries of Sumbulpore. Here the very industrious and respectable looking caste called Agureahs are first met with. They are found in Gangpore, Sumbulpore, Raegurh, Raipore and Rutten- pore. They number about 5000 in the three first places named. 1865. ] Notes of a towr in the Tributary Mehals. 1 According to their tradition, they are called Agureahs from having, ages ago, come from Agra. They were a proud Cshettrya or Khettree family, a stiff-necked generation, and refusing, when making an obeisance, to bow their heads, the Rajah lowered some of them summarily by cutting them off. They therefore left Agra and wandered south through Central India till they came to Sumbulpore, and eventually settled in these regions. Acquiring lands, and determining to devote themselves entirely to the tilling of the soil, they divested themselves of their “‘ paitas’’ making them over to the Brahmins, and no longer styling themselves or being styled Khettrees, they became known as Aguriahs. They bury their dead, and for this departure from the usual custom of Hindus, they can assign no specific cause, but that they gave up the practice of incremation when they resigned their pretensions to be esteemed Khettrees. They nevertheless now profess to be Vishnoovis, divided into two denominations, ‘ Ramanundyas’ and ‘ Kubeer pun- thees.’ The Vishnoovi doctrines they have probably taken up, since their migration to tracts bordering on Orissa and approximating the great fane of Juggernath. They say they gave up the worship of Kali when they resigned their ‘ paitas’ and took to the plough. It is probable that they were Boodhists, obliged to leave the Gangetic pro- vinces for refusing to conform to Brahminism. Their physique decidedly supports the tradition of their Khettri extraction: they are distinguished amongst the dark, coarse-featured aborigines of this country, as a tall, fair, well-made and handsome race, resembling the Rajpoots in every thing but swagger. That went with’ the ‘ paitas,’ as a farewell offering to Kali. The women, who are not very jealously secluded, have good features and figures, and a neat and cleanly appearance. The latter are subjected to no field labour, their sole business being to look after the domestic arrangements, to gin cotton and to spin. They do not weave. Their spun thread is made over to the weavers, who are paid in kind for their labour. Their villages, laid out in streets, are comparatively well kept, and their own houses in these villages sub- stantial, clean, and comfortable. Munguspore, near the Sumbulpore boundary, is, 1 think, the largest. It contains 200 houses, those of the Aguriahs occupying the centre of the village, surrounded by huts 12 Notes of a tour in the Tributary Mehals. [No. 1, of Coles and others of the primitive races, whose services they have secured as their farm labourers, and who are not allowed to hold Jands, but are paid for their labour at the rate of three seers of dhan per diem, and a modicum of clothing doled out annually. The soil in this part of Gangpore is exceedingly rich, producing magnificent crops of sirosha, sugar-cane, and tobacco, besides the staple rice. The plants of the country tobacco grown by the Aguriahs are the finest I ever saw, and they grow more cotton than they require for their own use, though they do not stint themselves in raiment. J am certain the soil and climate is well suited for the finer kinds of cotton. Proceeding north up the Heb from this, the Arabia Felix of Gang- pore, we came again upon untidy Bhooya villages, and their patches of cultivation, separated by miles of the monotonous Sal forests, and there is no change in the features of the country or the population, till we come to the -estate of Bhugwan Manjee, which, as above mentioned, does not appear as if it belonged to Gangpore, as it is separated by a range of hills, and approached by a very narrow and difficult pass. We are still amongst Bhooyas, but here they speak Hindi instead of Ooriah, and the peculiarities of Ooriah cestume and decoration are rarely met with. J USHPORE. The small state of Jushpore, though specially mentioned as a cession to the British in the agreement taken from Appa Sahib, after his defeat at Setahbuldee in 1818, has hitherto found no place in any pub- lished map. In the very latest issued from the Surveyor General’s office, a few scattered villages of Jushpore are inserted as if contained within*the boundaries of Sirgoojah, but the name of the estate is not given, and the chief town, where the Rajah now lives, is not down. It is singular how old the information must be, from which some names have been inserted on the maps of the unsurveyed parts of India. Konkale appears in large letters in about the centre of the tract which should be called Jushpore. It is now an insignificant hamlet, but there is the trace of a fort, where resided an ancestor of the present Rajah. The present capital, Jugdispore, is about two miles to the north and west of it. Jushpore is bounded on the north by Burway of Chota-Nagpore ; south by Gangpore and Oodeypore ; east by Chota-Nagpore; and west 4865.] Notes of a tour in the Tributary Mehals. 13 by Sirgoojah. It is about 50 miles in length from north to south, and 30 in greatest breadth from east to west, and may comprise about 1000 square miles. It contains upwards of 200 villages, exclusive of the hamlets or detached huts of migratory hill savages; the population is about 30,000, and the total income of the Rajah from all sources may be estimated at about Rs. 6000. With this moderate income he maintains a very becoming state, and so rules as to be greatly beloved by all his people. Jushpore is about equally divided into highlands and lowlands, *Oopur Ghat’ and ‘Heth Ghat.’ The highlands consist of a mag- nificent plateau, a continuation of the great tableland of Chota-Nag- pore, averaging upwards of 2000 feet above the level of the sea, and fringed by hills, rising in places 1000 feet higher. The lowlands lie im steppes descending towards the south, broken by low ranges of hills isolated bluffs, and masses of granite, sometimes semi-globular in form, and without vegetation, bare and round as an old man’s bald pate, and hence the most conspicuous of them is called the ‘ Boora.’ The Heb river has its sources in the Jushpore highlands, and grows so rapidly into a respectable stream, that when it reaches the brink of the plateau, it bounds into the lowlands with a roar that is heard for miles. It is, shortly after, joined by another stream, the Maini, which also rises in the J ushpore heights. There is a story that, years ago, an invisible spirit in a visible light canoe ascended the Heb, water- fall and all, to its source, and there the boat is still waiting for the spirit’s return. I did not see it. It is also called the ‘ Heera’ river, as diamonds are found in its bed, and it is probably the source of the diamond stores of the Maha Nuddee, as I understand that none have been found above the con- fluence of the two streams. It is auriferous, and from time immemorial its sands and deposits have been explored by hereditary gold-washers, called ‘‘ Jhorahs.”” These gold-washers do not, however, confine their operations to the bed of the river. They find it more profitable to penetrate the soil some distance from its banks, and on both sides you find tracts honey-combed with shafts, sunk by successive generations of gold seekers. These shafts are from 10 to 30 feet in depth, and three in diameter. The Jhorahs excavate till they cut through the upper 14 Notes of a tour in the Tributary Mehals. [No. 1, ‘stratum of vegetable mould and the red soil beneath it, and come to a layer of pebbles and fragments, chiefly of quartz, forming a dirty damp gravel; this they remove and wash. I have watched their operations close along the banks of the river, and at some miles distant from the stream, and the process and result was much the same in both places. Near the river, five pits or shafts had been recently sunk by as many families of Jhorahs, for they work in families, women and children assisting. They had one washing trough, called a‘ dooin,’ to each family, andthewashing commenced in my presence. The stuff selected is either of a dirty drab or of a reddish colour, with occasional small white spots, little balls of particles of decomposed felspar, adhering together from moisture, and drying into powder. The Jhorahs regard these white spots as the surest indication that the gravel contains gold. The stratum of gravel which they were working on this occasion was not more than a foot in depth. It rests on decomposed granite, which crumbles when taken in the hand, and the gold-washers assured me that this contained no gold, but I insisted on having some of it washed, and found their statement not strictly cor- rect. It contains gold, but is less rich in the mineral than the gravel above. When the gravel immediately under the shaft is all removed, they scoop out from the sides all round, as far as they dare venture to penetrate laterally, and in this way sometimes connect the shafts, but they take no precautions, and sometimes, going too far, have to be dug out, not always alive! There appear to have been several accidents of the kind, but with all this danger and labour, the pursuit does not return sufficient to support them, and they are farmers as well as gold- washers. They are greedy and reckless in taking advances, trusting much, no doubt, to the facilities their remote situation gives them, of evading payment, and some of them are enormously in debt. One man was pointed out to me as owing Rs. 1000! He grinned as the sum was mentioned, asif exulting over his victim. The greed for gold and the gambling nature of the pursuit is surely a great corrupter of human nature, for in the midst of a population generally remarkable for honesty, truthfulness and simplicity, these gold-washers are menda- cious and unscrupulous rogues. Some years ago, a trader came amongst them whilst they were at 1865.] Notes of a tour in the Tributary Mehals. 15 work, accompanied by his wife, hoping to obtain some return for the advances he had made. He dunned and worried them, and to get rid of his importunity, they knocked him on the head and popped him into one of the 30 feet shafts, where he was told to seek gold for him- self! The unfortunate woman was similarly disposed of. The crime was, however, brought home to the delinquents, who were all transported. The yield of these pits in gold is of course very uncertain. The out-turn obtained in my presence from the five pits, in about four hours, would not have given to the individuals employed, more than half an anna a head, but they admitted that they sometimes obtained as much as half a tolah of gold from one ‘ dooin’ in a day, and this would give about Rs. 2 a head to the hands employed, and make up for many blank days. From their mode of washing, there must be great waste. I observed it is only very palpable particles of gold that are retained. The grains are irregularly shaped, with sharp angles, and do not appear to have undergone any disturbing process since they were evolved from their original matrix. There is no indication of flatten- ing or rolling out. The northern portion of Jushpore, bordering on Burway and Sirgoojah, is a wild mountainous region called Khooria, inhabited chiefly by Korewahs ; some, utterly savage and almost nomadic ; others, somewhat more civilized, living in villages; but all invariably armed with bow and arrows and a battle-axe. In 1818 when Sirgoojah and Jushpore were ceded to the British Government by Appa Sahib, the chief of Khooria, himself a Kore- wah, and claiming to be hereditary Dewan of Jushpore, was in rebel- lion against his Rajah ; and for several years, by savage raids at the head of his Korewahs, both on Sirgoojah and Jushpore, gave much trouble. In one of these expeditions, his son Muniar Singh was cap- tured and detained as a hostage by the British authorities till the death of the old chief, when a reconciliation was, effected, between the Rajah and Muniar Singh, who was restored to his possessions and hereditary office. The policy adopted on the occasion has proved very successful : the dewans Korewahs have ever since conducted themselves peaceably. Having expressed a wish to see some of the wild hill Korewahs, the present zemindar of Khooria, a nephew of Muniar Singh’s, ap- 16 Notes of a tour in the Tributary Mehals. [No. I, peared in camp with forty warriors of the tribe. Their costume way nothing in particular, except that they had very shaggy heads of hair, into which their store of spare arrows were stuck by the barbs. They each carried in one hand a very powerful bow and two or three arrows, and in the other the gleaming long edged battle-axe of the country. The arrows are carefully made with flat bright heads of iron, 9 inches long and 23 in breadth, with long barbs, the edges and points all carefully sharpened. These are attached to light reeds, the other ends of which are neatly spirally feathered. The men were mostly short of stature but with well knit muscular frames, springy and energetic in action, better looking and of lighter complexion than the Oraons of the plateau. There was no remark- able protuberance of the maxillary processes nor lowness of forehead. Those who were old enough had beards and moustaches. They evinced no timidity, but immediately on seeing me, gruffly vociferated that they had had nothing to eat all day, and they wanted immediately, rations of rice, dal, oil, salt, tobacco and pig, and expected as they had come so far to see me, that they were each to be presented with a cap, a coat and a waist cloth. I placed a small earthen pot on a peg, and offered it as a mark to those amongst them who wished to shew their skill in archery. In great excitement, all eagerly volunteered, bows were instantly strung, and though they did not once hit the small target, they all planted their arrows close to it, and aman in the same position would not have escaped. I tried them afterwards at a tree at 40 yards, and almost every arrow told. Their bows are very powerful, and arrow after arrow was delivered with a force and rapidity that made one feel a very profound respect for this, owr once national weapon. In bush warflare it is more formidable than the matchlock, and I do not doubt that the Korewahs could render a hostile entry ito their country, a difficult and dangerous task. There is every point of resemblance between them and the wilder section of the Lurka Coles, and so little do the languages of the two tribes differ, that my slight acquaintance with that of the Coles, enabled me to understand what the Korewahs, on first appearing, were demand- ing; and a Cole chaprassee of mine kept up a conversation with them. It is almost unnecessary to seek for further proofs of affinity, but they 1865.] Notes of a tour in the Tributary Mehals. 17 are to be found in the identity of many of their customs. Their sacrifices in eases of sickness, their songs, their dances, their mode of disposing of the dead—all these shew them to be of kin to the ‘ Ho’ or Lurka of Singbhoom, the Moondahs of Chota-Nagpore, and to the Sonthals. It is not possible to trace the similitude through all the relations of life. The Singbhoom Coles live in large communities and have an organization unattainable by the hill Korewahs, who prefer to dwell apart. Except on great occasions, when there is a ‘ gathering of the clan,’ the Korewah has only his own family to think of and associate with. The head of the family is chief and priest—the god to whom he sacrifices, the spirit of his father. The Korewahs are found also in the wildest parts of Sirgoojah, and in the ranges of hills between Sirgoojah and Palamow. Many of them have abandoned their free mountain life, and have formed settlements on the skirts of hills, near villages ; and where this is the case they appear to be losing their own language and peculiar habits, and becoming Hinduized. The Hill Korewahs live in wretched little detached huts, in the midst of the patch of hill forest they have partially cleared and are then cultivating, shifting every three or four years as the ground be- comes exhausted. They cultivate very little rice. Their crops con- sist of pulses, millet, pumpkins, cucumbers,* melons, sweet potatoes, and yams. They also grow and prepare arrow-root, and thereis a wild arrow-root which they use and sell. The grain they store for winter use is secured in small parcels of the leaves of a plant called ‘ muhoo- lain,’ sown together by fibres of the same, and these parcels they bury. The grain thus preserved remains for years unimpaired. They have no prejudices in regard to animal food, and they drink freely of an intoxicating beverage prepared by themselves from millet. They are as devoted to songs and dances as the Moondahs and Son- thals, and have the same steps and melodies. They bury or burn their dead, whichever they find most convenient, but the practice of mark- ing the spot where the body or ashes are deposited, iscommon to both. The Khooria Korewahs resort in large numbers to an annual fair held at Muhree on the borders of Sirgoojah, and give in barter for salt * They have a gigantic cucumber about a foot and a half in leneth and ten inches in diameter ! 3 18 Notes of a tour in the Tributary Mehals. [ No. 1, and other necessaries, wax, arrow-root, resin, gums, honey and stick lac, and excellent iron smelted by themselves. The Korewah iron, roughly fashioned as battle-axes, is greatly prized by the inhabitants of all the neighbouring States. Whilst conversing with the Rajah about these savages, he men- tioned to me that there existed a tribe called Birhores, whom he accused ofa sort of interfraternal anthropophagy, of feeding literally on their blood relations. They are alluded to by the late Col. Ouseley, in a paper that ap- peared in the Journal of the Society for January 1848, but he relates the story, as of the Korewahs, calling them inhabitants of Mynepat in Sirgoojah. The Korewahs repudiate all affinity with the Birhores, nor could I hear of either Korewahs or Birhores on the Mynepat: the latter are found in some of the wildest parts of Chota-Nagpore and Jushpore, but they are of rare occurrence. With much trouble some were caught and brought to me. They were wretched looking objects, but had more the appearance of the most abject of one of those degraded castes of Hindu, the domes or pariahs, to whom most flesh is food, than of hill people. Assuring me that they had themselves given up the practice, they admitted that their fathers were in the habit of disposing of their dead in the manner indicated ; viz. by feasting on the bodies, but they declared they never shortened life to provide such feasts, and shrunk with horror at the idea of any bodies but those of their own blood relations being served up at them! The Rajah said he had heard that, when a Birhore thought his end was approaching, he himself invited his kindred to feast on his body. The Birhores brought to me did not acknowledge this, but they spoke on the subject with a degree of reticence that made me think it might be true. I told the Rajah to enquire particularly about it, and gave out that if the horrid rite was still practised, it must be discontinued. But, query,—‘ would not Saturday reviewers regard my order as an injudi- cious interference with a time-honoured custom, on a point that natives the disposal of their dead 2?’ The Birhores speak a jargon of Hindi, which I found intelligible ; and have no other language. Nine-tenths of the population of the remaining portion of the Jush- pore highlands are ‘* Coles.” Chiefly Oraons, there are very few Moon- were so peculiarly tenacious of 1865.] Notes of a tour in the Tributary Mehals. T9: dahs amongst them ; the Jushpore Oraons are the ugliest of the race, and appear to me utterly destitute of all ambition to rise into respect- ability of appearance. With foreheads “ villainous low,” flat noses and projecting maxillaries, they approach the negro in physiognomy, much closer than do their brethren in Chota-Nagpore. Jushpore produces an excellent iron, much prized for making wea- pons and implements of husbandry. Amongst its exports may be included about ten thousand maunds of cotton. The lowland villages of Jushpore have a sprinkling of the tribes from all the surrounding districts. Of the Orissa type are ‘ Makoors”’ from Keonjhur, the most thriving people in these parts, well dressed, and occupying good houses. They have great herds of cattle, like the Aheers and Gwallas. Then there are a few of the Gangpore Bhooyas, intermingled with a good many Khairwars from Palamow, (of which. caste is the Rajah,) and Gours or Gonds from the south and west, and as we approach Oodeypore, we come for the first time on the Kawrs. The Kaurs form a considerable proportion of the population of Oodeypore, Sirgoojah, Korea, Chang Bhukar, and Korbah of Chutteesgurh, and there is this point of interest in them, that they claim to be the descendants of the ‘‘ Kooroos” who fought the Pandavas, who, when defeated and driven from the scenes of the war, found a safe retreat in these mountainous and densely-wooded regions. In appearance they more resemble the aborigines than the Hindu tribes. They are, in fact, next to the Jushpore Oraons, the ugliest race I have seen in the course of my tour: dark and coarse-featured, broad noses, wide mouths and thick lips. They resemble the Khair- wars of Palamow, especially that ill-favoured section of them called Bhogtahs, in features, but in nothing else, as the Kaurs are an exceed- ingly industrious and thriving people. Their houses are unusually neat and commodious, built ike bungalows, with verandahs on two or more sides. Of these there is one to each married member of the family, who, however, meet and eat together in the largest, belonging to the head. The houses are placed so as to form a small court-yard, which is kept scru- pulously clean. The Kaurs do not strictly conform to Hinduism: they rear and eat fowls, and have no veneration for Brahmins. The “ Nau,” the village barber, whom they sometimes call Thakoor, is their priest, and officiates as such at all marriages and other ceremonies, The 20 Notes of a tour in the Tributary Mehals. [No. 1, combination of priestly functions and operations with the easy shaving line, is singular; but it arises from the fact that the great ceremonial law of the Kaurs is all comprised in the act of shaving. At births, deaths and marriages, the parties immediately interested, and all con- nected with them, are clean shaven all round. In regard to the disposal of the dead by this tribe, they tell me that they bury those that die unmarried, while the bodies of married folk are burnt m orthodox Hindu fashion! I wonder if matrimonial interests are ad- vanced by this invidious custom. The tonsure of the males is ‘pecu- liar; the hair is allowed to grow long on the crown of the head and collected in a knot, but the forehead is shaven to the knot, and there is a shaven ring round it as if to facilitate the operation of scalping ; the back of the head is also shaven, but over the ears and temples the hair is worn long. They worship Shiva under the denomination of Mahadeva, and Parvati as Gouree, and they have a festival in the year for each, at which they dance and sing, men and women. In some villages there is a Baiga who offers sacrifices at these festivals ; but this Baiga is not a Kaur. He belongs to one of the aboriginal tribes, and it is a remarkable feature in the religious ceremonies of the people of the Tributary Mehals, that the aborigines should have a monopoly of such offices. The new settlers dread the malignancy of the local spirits, and to appease them, naturally rely on the aborigines, who have longest known them. The zemindar of Korbah in Chutteesgurh is a Kaur, and as far as I can learn is the most influential person of their caste existing: there was a Kaur zemindar in Sirgoojah formerly, called Kumol Singh, but he rebelled and came to grief. Most of the “ Khalsa” villages in Oodeypore are held in farm by ‘ Kaurs’ and two-thirds of the population of these villages are Kaurs. With one exception all the permanent service tenures of Oodeypore are in the hands of Gours, and the people in those estates are for the most part Gours. We find therefore, that the Gours have, in Oodey- pore, a position similar to that held by the Bhooyas in Bamra, Gang- pore and Bonai, and the right to the office of Dewan and to instal a new Rajah, claimed in those districts by certain Bhooyas, is in Oodey- pore claimed by one of the Gour zemindars, Bhowany Singh of Kourajah. Thus we find the Gours or Gonds, who in Bonai were 1865.] Notes of a tour in the Tributary Mehals. 21 classed amongst the most degraded of the people, (and in Gangypore not held in much higher estimation,) holding a high position in Oodeypore. I have insensibly glided into Oodeypore. In no published map are the boundaries of that district defined. It has to the north the great tableland of the Mynepat, as a massive barrier between it and Sirgoo- jah, to the west Korbah of Chutteesgurh or the Belaspore district, to the south Raigurh, and to the east Gangpore and Jushpore. It is about 64 miles in length by 40 in breadth, and contains about 1800 square miles. There are 220 villages. The population may be roughly estimated at 25,000. The only river of consequence is the Mand, an affluent of the Mahanuddee. It rises near Girsa in Sirgoojah, and re- ceives the streams that flow south from the Mynepat. Near Rabcope, which, though not much of a place, we may call the chief town, it has cut its way through a great mass of sandstone rock, and now flows without obstruction through a narrow pass with perpendicular or rather overhanging cliffs, on the highest portion of which the former Rajahs of Oodeypore, like Barons of the Rhine, had their castle. The site was occupied by the leader of the Oodeypore insurgents in 1857- 58, and had he not abandoned his position on the approach of a force sent against him, he might have given us much trouble, as the rock is or might easily be made as inaccessible from the land as from the river side. The river has generally a deep cut channel, flows in alternate rapids and pools, and is not navigable in any part of its course. The country north of Rabcobe rises in steppes to the base of the Mynepit, but the suriace is everywhere undulated by masses of sandstone rock, forming hills, dividing and enriching the culturable lands, as the rocks have many springs, from which fertilizing streams are ever flowing over the terraced plains. But with all these advantages the country is sparsely populated, the villages small and ‘ far between,’ and there appears little prospect of improvement, as the districts all round are in much the same condition. There is at present but one weekly market held in Oodeypore, at Dukree, 24 miles due south of Rabcobe. This is attended by people from Raigurh, Chutteesgurh, Sucktee, &c. The chief exports are lac, cotton, resin, oil seeds, rice, wild arrow-root, iron, and a small quantity oi gold. 99 Notes of a tour in the Tributary Mehals. [No. 1, The production of the precious metal is restricted by the limited number of gold-washers. There are now only six families of that pro- fession on the estate. The same cause may be assigned for the limited production of iron, as there are not more than ten families of smelters in all Oodeypore. I saw the gold-washers at work in pits similar to those I inspected at Jushpore. The deposit sought and the method of working it is the same in both mehals, but the deposit in Jushpore is supposed to be the richer of the two. In Oodeypore, the gold-washers produced, as the result of a day’s labour, only 3 grains of gold to each “‘ Dooin” or trough, but I am satisfied from what I saw of the quan- tity of gold exhibited at each washing-out of the trough, that they must have obtained very much more than they thought proper to pro- duce. The Rajah was with me; he wishes to obtain a monopoly of the gold trade; and it did not suit them that he should see a better yield. The export of ‘lac’ from Oodeypore is said to amount to about 2000 maunds annually. I have not been able to gain any information in regard to other produce, but the heavy expense of carriage and consequent low prices offered, are very discouraging to the producers. Amongst the mineral resources not yet utilized, is coal; seams have been observed at Baisi south-west of Rabcobe, and other places. Lime- stone is found under the Mynepat. SIRGOOJAH. I entered Sirgoojah from the north-west corner of Oodeypore, as- cending the Metringa Ghat and passing along a ridge, a cyclopean wall of sandstone that actually divides the sources of the Rehur, an affluent of the Soane, from some feeders of the Mand, an affluent of the Maha Nuddee ; and near the same point the boundaries of Sirgoojah, Oodey- pore and Chutteesgurh meet. Clear of the Ghat, which is very steep and difficult, I find myself at the western extremity of the great Myne- pat, which rises majestically fromthe plain in a succession of bold headlands and promontories, as our own proud islands rise from the sea; and as the eye follows what so much resembles a long coast line, the mind is filled with the idea that the ocean must once have rolled where the Sal trees now wave, and this is strengthened when we turn to the isolated bluffs having all the features of the mainland, from which they appear to have been cut off, rising abruptly like islands = 1865.] Notes of a tour in the Tributary Mehals. 23 from the sea, not less than 2000 feet above the plain, or appearing in the distance, from the parallel markings on the face of the rock, like huge casemated batteries protecting the coast. The country teems with architectural remains of a race who appear to have left no other trace of their existence. On the banks of the Rehur, in great heaps of carved stones, shafts, bases, capitals, friezes, architraves, lie the ruins of numerous temples of a very ancient type. (The Rajah’s cousin, Lall Mohessuree Persad Singh, on whose estate they lie, is very irreverently using them up in the construction of a sporting lodge). The fragments appear to have been put together as children build with wooden bricks, all in parallel courses, with nothing but their weight and adaptation of the parts to keep them in their position; and thus their overthrow, which from the studied mutilation of all the idols could not have been accidental, was easily effected. There is no indication of any kind of cement or of iron bindings having been used in the structures. Amongst the isolated hills mentioned above, the most conspicuous is that of Rama or Ramgurh, which rises from the plain about 8 miles west of the Mynepat. From one distant aspect, the upper portion of the hill alone appearing above the Sal forest, its resemblance to a monster fort with a cupola roof is very striking, so regular is its form and so abruptly precipitous are its sides. Approaching it, however, it is seen to have a variety of outworks of its own. The ascent commences from the north side, proceeding up and along narrow ridges of one of these outworks, till you reach nearly to the base of the great rock itself, and there are the ruins of a very ancient stone gateway. The lintel now lying on the ground is adorned with the image of ‘ Gunesh’ as the Janitor. Inside, between the gate and the rock, there is a level path both east and west. Proceeding westward, you come to an ample space of level ground affording room for a small encampment, in deepest shade, under a perfectly perpendicular portion of the huge rock, reminding one of the description of ‘ Sinai,’ the mount that could be touched with the hand but must not. The ap- proach to this spot from the gateway was originally protected by a stone breastwork now fallen, and the importance of protecting it is obvious, as here the rock sends out a jet of perfectly pure water, just such as one could suppose to have issued by Divine command at the 24 Notes of a tour in the Tributary Mehals. [No. 1, touch of Moses. The temperature of the water was, strange to say, much higher than that of the air, but cooled in a soraz it was delicious. A broad seam of coal is here seen underlying the sandstone. It burns well, but I say no more about it,as the Sirgoojah coal from this vicinity has been fully reported on by my predecessor Col. Ouseley. To continue the ascent of the hill, you repass the gate, and proceed by an easy path three parts round the hill to its southern face, and then as best you can wp, by an exceedingly difficult zig-zag path, some- times a mere ledge cut out in the rock. Just at the commencement of the difficult part of the ascent, you pass a large boulder of sand- stone with nothing to distinguish it externally from many others that are lying about, but which has been hollowed into a chamber of suffi- cient capacity to allow of a man sitting in it at his ease, and with an aperture just large enough fora slender man to creep in by. The open- ing is not seen from the path ; so that an unconscious pilgrim might find himself exhorted by a voice from the bowels of a rock in a manner truly awe-striking. Crowning the most difficult part of the ascent, so perched that you cannot obtain a good view of it without looking right up to the sky, from a position that makes it unpleasant to throw your head back to the necessary angle, isa second gateway, which is in better preservation, and is the best executed and most beautiful architec- tural antiquity of the entire region, Though its origin is equally unknown, it is unquestionably a more modern work than the other gateways and temples on the hill. It belongs to that description of Hindu architecture which bears most resemblance to the Saracenic. Tnstead of a flat lintel over the gate, we have an arch formed of three voussoirs of stone. The soffit of this arch is cut into a wavy scroll, terminating on the abutments, in heads of some animal not clearly discernible. There is an exterior and interior arch of this description, springing from fluted pilasters, and the space of about three feet be- tween them is covered in by another loftier arch similarly formed. Entering, you find yourself ina small court, at the bottom of a flight of steps. A projection of the rock has been scarped to form this resting place, and from it a most extensive view south and west is obtained. The steps are to the right as you enter, to the left there is a projection with stone breastwork used as a look-out. Opposite the entrance, there was a covered colonnade, but this has fallen in, 1865.] Notes of a tour in the Tributary Mehals. 25 In the thickness of the gateway wall, a niche four feet in depth and about eight feet in height and breadth, is divided by a column still in position, shewing how the fragments of the columns of the ruined colonnade should be restored. The shaft and base are octagonal and the bracket-like projections of the capital are crouching human figures, so placed, that head, arms, hands and back all appear to support the abacus. There is one well executed figure in this enclosure, of a man Imeeling on a coiled cobra, and with snake heads peering over each shoulder. A flight of 48 cut stone steps leads from this resting place to another mass of ruins which appear to have been a temple and gateway combined. There is here an image of Durga with 20 arms, another with eight, and a large figure of Hunooman, all more or less mutilated. We are now on the ridge forming the top of the hill. Bare as are the sides of the rock, there must be here a great depth of soil, as it supports a variety of large forest trees and shrubs, which are growing luxuriantly. On the highest part of the ridge and about the centre of the hill, is the temple, which contained no doubt the principal object of worship. It consisted of a small fane, the inner crust of which, constructed of parallel courses of roughly cut stone, is still standing, with a detached portico on columns. It is small and insignificant, but no doubt immensely old ; it is impossible to say to what idol or object of worship the temple was originally dedicated ; at present, on the old “argha” or stand, thereis a group of Vishnu with his wives, but the group does not fit the pedestal, is of more elaborate workmanship than the figures that are lying about, and whilst all the old figures are mu- tilated, this one is perfect. I conclude that it was placed in the temple aiter its partial destruction, and the mutilation of the original images. I found the air on the hill keen and invigorating. There is space for several houses on the saddle back ; and as it is an independent isolated mountain, it commands an extensive view, shewing that all this part of Sirgoojah, which the maps make out to be a mass of hills, from the foot of the Mynepat, as far as the eye from this elevation can penetrate westward, is, thus seen, a plain slightly undulating, but on the whole well adapted for the Railroad, which, I am confident, will some day be made through it, connecting, by the most direct route, Calcutta, Central India and Bombay. 4 86 Notes of a tour in the Tributary Mehals. [No. 1, The tableland called the Mynepat is 50 miles in length by 40 in breadth, with an elevation of 3,700 feet above the sea level. Its soil, like that on the Ramgurh hill, is deep and rich, and it possesses numer- ous springs and streams. It abounds in game; gaur, buffalo, tigers, leopards, and deer, and some of the streams are large enough to give the angler gentler sport. The day must surely come for the fructifi- cation of all these natural advantages, and the tract now occupied by a few herdsmen and savages, may become the head-quarters of a divi- sion, or the seat of a Government. Not iar from the summit of the Ramgurh hill, an attempt has been made to construct a tank, but it probably was not a success, and it is now nearly filled up with light vegetable mould, of not less than three feet in depth.and quite dry. In another direction, a descent of a few hundred feet brings you to a pool of good water percolating a seam of white calvareous clay. A party defending themselves on the rock could not be cut off from this supply, as it is perfectly maccessible from below, but it would not be adequate to the supply of a large party, and the next nearest source is the spring near the first gateway. But the great curiosity of the Ramgurh hill has yet to be described. Two of the spurs of the great rock, themselves rocky and precipitous, forming buttresses on the northern face, instead of gently blending with the plain like others, have their bases truncated, and then united by a vast natural wall of sandstone rock, 150 yards thick and 100 to 150 in height. A semi-circular or rather horse shoe shaped nook is thus formed, which, from the height and precipitous nature of the. sandstone rock enclosing it, would be almost inaccessible, had not na- ture provided an entrance by a natural tunnel through the subtending wall. This is called the ‘‘ Hathphor.” The waters collected from springs in the nook form a little stream that flows out through the tunnel. At its mouth it is about twenty feet in height by thirty in breadth, but at the inner extremity of its course of 150 yards, it is not more than eight feet by twelve. A man on horseback could ride through it. The sand of the stream in the tunnel was impressed with old and recent foot-prints of a whole family of tigers, who had taken up their abode in this pleasant and secure retreat, but we did not find them at home. The horse shoe embraces an acre or two of ground, well wooded and undulating, so that a considerable body of men could 1865.] Notes of a tour in the Tributary Mehals. 27 conveniently encamp there. In the face of the great rock opposite the entrance, two large caves have been excavated by human labour, the largest of the two, sufficient to afford accommodation for forty or fifty people. The entrance, about 30 feet wide, opens into a gallery of double that length, with recesses at the extremities, intended for more private apartments, probably for females. The excavation is made so as to leave a platiorm of stone, extending through its whole length, and also in the recesses, for the occupants of the cave to sit and sleep on. The floor is some fifteen feet above the ground, but is accessible by steps cut in the rock. In both caves I found inscriptions carved on the rock in ancient ‘ Pali’ character, and I made the best transcript of them I could : this is now in the hands of Babu Rajendra Lal Mitra, and it will, I trust, throw some light on the history of the retreat. Since writing the above, I have seen Col. Ouseley’s brief notice of the Ramgurh hill in the Asiatic Society’s Journal No. CLXXXVI. for January 1848. He does not appear to have observed the inscriptions, and I do not recollect having seen in the caves any of the stone figures that he noticed there. They may have been since removed. Col. Ouseley calls these antiquities cave temples, but there is nothing now to indi- cate that they were intended as places of worship. ' There are many other interesting collections of ruins in Sirgoojah. Those to the west, in the Pal Pergunnahs, noticed by Col. Ouseley, I have not seen, but he found there a stone with an inscription on it, which I think must be in the Society’s museum. On the banks of the Kunhur river in Tuppah Chulgalee, there is a large collection of temple ruins. Three distinct heaps of fragments were at my request opened out, till the foundations of three large temples dedicated to Shiva and Durga were disclosed. The object of worship in the largest, was a huge Lingum, five feet in length, which we found divorced from its appropriate ‘‘ Yoni” as if it had been blown up. The latter was smashed into several pieces by the destroying force, whatever it may have been, and the numerous sadly maimed gods and goddesses that were found in the debris, are further memorials of the barbarous zeal of some uncompromising iconoclast. I observed a Shib’s bull in good preservation, as large as life, a well executed figure of ‘ Parvati’ three feet high, and a grand, colossal, four armed figure with one foot resting on a broad-edged axe, not unlike what is still the national 28 Notes of a tour in the Tributary Mehals. [No. 1, weapon of the tributary mehals. Close to the temples there is a stone- faced tank. : Six miles to the west of the above ruins at Sirnidee there is another small temple which appears to have been overlooked by the destroyer. The dome over the fane is still standing, and part of the vestibule, the latter a pyramidal roof supported on columns. The stones forming the lintels and uprights of the entrance to the fane are elaborately earved with minute representations of all the principal Hindu gods. Shiva and his wife on Nandi occupying the place of honour in the centre of the lintel, The Ruksale Rajpoot family who now hold Sirgoojah, have no tradition regarding the antiquities Iam describing, but they tell me that under the Mahratta rule, their ancestors often availed themselves of the retreat of the Hathphor to save their property from pillage and their women from dishonour. The ruins of an ancient castle of the Ruksale Rajahs of Sirgoojah are to be seen on a hill near Bisrampore, and this appears to be the Sirgoojah, marked as the chief town on the map, shewing again the antiquity of the information from which the maps of these unsurveyed tracts had been filled in. ‘ According to the tradition preserved in the family, the first Ruksale was called into existence by a ‘Muni’ or sage, to destroy a demon that troubled the holy man in his devotions. The hero thus created was the ancestor of the lovely Rukmini carried off by Krishna. In about Samvat 251, a lineal descendant of Rukmini’s brother, Ruk- man, entered Sirgoojah and fought with and killed the Rajah of the place called ‘ Balind,’ and became Rajah in his room. The present Maharajah Inderjeet Singh has a family tree to shew that he is the 111th in descent from the conqueror of Balind ! but I have been told there is a popular tradition assigning to the family a local origin, and considering there are no Ruksales in any other country, it is not un- likely that it is the most truthful of the two. If so, it is probable that the family are derived from the same stock as the ‘ Gours,’ the most influential and numerous of the races now inhabiting Sirgoojah. In A. D. 1758, a Mahratta army in progress to the Ganges overran the district of Sirgoojah, and the chief was compelled to acknowledge himself a tributary of the Berar government, but 1865.] Notes of a tour in the Tributary Mehals. 29 beyond a fine imposed at the time, and engagements taken for the security of the roads from Mirzapore, Benares and Gya to the capital of Nagpore, no proofs of submission were exacted. In the year 1792, Sirgoojah first engaged the attention of the British Government, in consequence of its Rajah Ajeet Singh having invaded and taken possession of Burway, a Pergunnah of Chota-Nagpore. At the requisition of the Governor-General, the Rajah of Berar interposed; but ineffectually, as about this time, on the death of Ajeet Singh, his third brother Lall Sungram Singh usurped the chieftainship, murdered Ajeet Singh’s widow, and not only retained possession of Burway, but assisted a rebellion in Palamow against the British Government. This led to an expedition into Sirgoojah under Col. Jones by order of Marquis Wellesley, which resulted in the restoration of Burway to Chota-Nagpore, and Sirgoojah itself became a dependency of the British empire by treaty with Appa Sahib in 1818. Sirgoojah has not been surveyed, and it is therefore impossible to give its area with any degree of accuracy. It is about 90 miles from east to west and 80 from north to south; is divided into 26 tuppahs and contains 1197 villages, and according to a return of houses made some years ago, a population of 1,30,000, one hundred and thirty thousand souls. About one-sixth of the whole are of the Gour tribe: the Khairwars, Kawrs, Kisan Rajwars, Kore- wahs and Coles number from 5000 to 7000 each: there are about 2000 Bhooyas, and about as many of the hill tribe found in greater numbers further west, called Boyars : the remainder of the population are for the most part Sudras. The ruling race, Rajpoots, number only 505 souls, and there are only 369 Brahmins. Of the Gours, I have already observed that they are the same as the Gonds of the south. Of this there can be no doubt, as we find amongst the Gours of Oodeypore and Sirgoojah, blood relations of the Gonds down south; and they intermarry. It is only a different way of pro- nouncing the name of the tribe. They have always I believe been considered as amongst the aboriginal races of India, but in Sirgoojah and Oodeypore they are completely Hinduised, retaining neither the language nor any other characteristic of their own race. The Kaurs and Korewahs have already been disposed of; the Coles must have a chapter to themselves; the characteristics of 30 Notes of a tour in the Tributary Mehals. [No. 1, the Rajwars and Kisans I have not yet had an opportunity of study- ing, and shall conclude with a few words about the Khairwars. They are found in many parts of this province but are most numerous and have been longest resident in Palamow. They are said to have migrated from the hills west of Rhotas ; there is a place there, called Kyra, supposed to be named after them, and they are found about the Kymoor hills. The Rajah of Turki in that vicinity is a Khairwar. In this division several of our great men are said to be of Khairwar extraction, but they are all now undergoing that process of being refined into Rajpoots which I have described as likely to have occurred in other families, by intermarriage with Rajpoot maidens. They have to pay very high for the honour, but by giving large dowries with their daughters, they sometimes obtain for them also the distinction of Rajpoot alliances. The two races appear to blend well; a handsomer and more ener- getic stock is the result; so the aspiring families I allude to, have gained something by their outlay in marriages, as the ordinary or pure Khairwars are generally a dark, ill-favoured race, with coarse features and of lazy unimprovable habits, The people called Bhogtahs are a Khairwar tribe. There was a small clan of them in Palamow, who long defied the power of the British Government. They lived on a narrow plateau, with the Sir- goojah mountains behind them, and a range of hills with difficult passes in front of them; and with the cattle and property of their neighbours, they did very much as they pleased; and as they had wonderfully contrived retreats amongst the hills and rocks for them- selves and their plunder, they defied all efforts to capture them. At last the wild country they occupied was given to them at a nominal rent, on condition of their living honest and peaceful lives. This kept them quiet for many years, but when the mutinies broke out in 1857, the two chiefs, Lilumber and Pitumber, headed an insurrection in Pala- mow and came to unmitigated grief. Qne was hanged and the other was transported for life and died in the Andamans. The actual income of the Rajah of Sirgoojah from all sources is not more than Rs. 30,000 a year: the estates held by members of his family are worth in addition about Rs. 23,000, and other vassals hold estates worth annually about Rs. 20,000. A fixity of tenure is the 1865.] Notes of « tour in the Tributary Mehals. 3h predominating feature in the revenue system of all the Tributary Mehals, and will no doubt be found to prevail in all parts of Hindu- stan where ancient landmarks have not been swept away by the tide of conquest. In these mehals, the great mass of the cultivators are the descendants of those who first occupied and tilled the soil, and to them, (says Malcolm in his Central India,) according to the most revered texts of the sacred writers, the soil in the first instance belongs ; and where a monarchy or chieftainship is by some process eliminated, the peasant proprietor contributes for the support of the sovereign a moderate share of the produce of his land. This accounts for the lowness of rates of rents that prevail in these districts. The actual rent does not exceed 2 annas a beegah in Sirgoojah, and this is un- changeable. It probably represents the proportion of the produce first assigned to the chief, and both the cultivating classes and heads of villages in this province aré exceedingly tenacious of their right to pay no more than-one fixed rate of rent. The hereditary village head- man pays no more on this account, and collects no more than the old fixed rate, but it does not now suffice for the requirements of the chief, and as noticed before in treating of Gangpore, a practice has ‘arisen of giving as an ordinary contribution, a sum equal to the amount paid as rent, whilst extraordinary contributions are often exacted, and demands made for unpaid labour, which must greatly hamper the productive . industry of the cultivators.. In Sirgoojah I.asked the Rajah and zemindars if all these irregular demands could not be done away with > and a fair fixed rent taken in lieu. They expressed their willingness to abide by any arrangement of the kind that I could make, but refer- red me to the rent-payers and village headmen. They, with one con- sent, reiused to acquiesce in any enhancement of rent. 32 On a New Genus of the Gadide. [No. 1, Description of a supposed new Genus of the Gadide, Arakan.—By Lieut.-Col. 8. R. Trcexetn, Bengal Staff. Plate I. [ Author’s date, October, 1862. ] [Received 8th June, 1864. ] Order. MatacopreryGir SUBBRACHIATI. Family. Gapip&. Genus. AsTHENURUS (mihi). (acGerijs feeble and Ovpa Tail). Body rounded—very little compressed—head small, muzzle short, mouth wide with a single row of minute teeth in each jaw, and a band across the anteal part of the palate. Scales of a medium size. No lateral line visible. Fins; two dorsals and two anals, joined by intermediate detached rays, which are partially membraned. The anterior dorsal and anal, quadruple the height of their posterior fellows. Ventrals jugular and filiform. Caudal bilobed and very small. Brancheostegous rays 7. Astusenurvs Arripinnis. Tickell. Specimen 52” long. The largest of 4 or 5 observed, Akyab harbour. Avakan. October 15th, 1862. Structure. See above for Genus. Body lengthened in the portion of the tail behind the Ist dorsal. Head small; snout short and blunt. Gill plates smooth and smooth-edged, their divisions not very distinct : but suboperculum large: scales medium-sized, semitransparent and deciduous. Along the back, from occiput to Ist D, a mesial groove, with a ridge along each side for the whole length of the fish to caudal. A deeper groove along mesial belly, in which the ventrals can lie encased. Intermaxillary long and narrow, and set with a row of minute pointed teeth jammed close together. Mandibles with a similar row, smaller still. Rest of mouth smooth. Tongue short, round, tied down to floor of mouth. Scales round at free edge, concentrically furrowed; about 67 from gill cover to base of C and 14 tiers. Air bladder large. Its shape and that of the intestines could not be ascer- tained, as the specimen examined had been a long time in spirits. Fins. 1st D 20, detached rays 15—2nd D 20,—P, 21.—V 5.— A 20, detached rays 12—2nd A 26.—C 6-13-6, (714x914) “SINNIdId1Y = SMYNNAHLSY / 3ZIS :LWN 5991 AVW 'VLiIM91v90 9 S HLIWS WH AB SHLIT / WaZV¥S 1 4 AW UNOISNO VIET WON ATRIA -pEUsatang ay speuatar es LS BS Sars a e hice 1865. ] On w New Genus of the Gadide. 33 1st D and 1st A have their 5th and 6th rays as long as the greatest depth of the body, the fins decreasing rapidly to the first and last rays. The 2nd D and A are much shorter rayed and close to ©, and the space between them and their preceding fins is occupied by a row of short rays each with a basal membrane. Pectoral, small, broad, and pointed. C very small, and bilobed, the lower lobe blunter and shorter than the upper. Ventral, 3 first rays filiform, the 2nd reaching to the space between the two anals; Ist and 3rd a little shorter; 4th and 5th ordinary and membranous. Colowr.* Pale ochreous grey, or horn colour, blackish along back, from minute dots powdered along edges of scales. Snout and head, red earneous. Iris, greenish silver. Fins black, with whitish bases, except Vs which are fleshy white. A rectangular patch of black above gill plates. Gill plates nacreous. The specimen here figured is the largest of 4 or 5 obtained in the fish market of Akyab. The fish is not described by Cantor in his ichthyological catalogue of the Straits, and Cuvier and Valenciennes’ great work, which is incomplete, does not include the Malacopterygii Subbrachiati. None of the Gadide (Cod family) have as yet been noticed in India, and the present subject is one of peculiar interest on that account: that is, if my allocation of it should prove correct, of which I think there can be little doubt, on an examination of the structure of the fish. In the synopsis of Cuvier’s Regne Animal there is no genus amongst the Gadide which resembles it : but it may rank next to Phycis (Artedi.) It does not appear uncommon. In October 1862 I procured four or five specimens from the estuary of the Koladyn at Akyab, and from Kyoukphyoo. Two of these I do myself the pleasure of forwarding to the Museum of the Asiatic Society. The alcohol in which they are preserved, has very little affected their natural colour. * Fresh specimen, OO OOOO 34 On Local Attraction. [No. 1, “On the degree of uncertainty which Local Attraction, if not allowed jor, occasions in the Map of a Country, and in the Mean Figure of the Harth as determined by Geodesy ; a Method of obtaining the Mean Figure free from ambiguity by a comparison of the Anglo- Gallic, Russian, and Indian Ares; and Speculations on the Constitution of the Earth's Crust.” —By Arcupnacon Pratt. [Received 4th August, 1864. | To the Secretary of the Asiatic Society. Srr,—l beg to forward to you a copy of a Paper lately printed in the . Proceedings of the Royal Society (No. 64) on the topics notified at the head of this letter. Two years ago you accepted from me a “Series of Papers on Mountain and other Local Attraction in India,” and published in your Journal a memorandum, regarding the effect - of local attraction upon the operations of the Great Trigonometrical Survey of this country. The present Paper is not confined to India ; but appertains to the globe in general. But as the results of the Indian Survey occupy an important position in the calculations, you may deem it to be not irrelevant to the objects of your Journal to publish some account of it. The state in which the question of local attraction was left in my former communications to the Royal Society was this :—That in India the deviation of instruments of observation from the true vertical caused by the Mountains and by the Ocean is very great, far greater than had ever been supposed; that this deviation might be much increased or diminished by the effect of variations of density in the solid crust of the earth, but that of the amount of this we have no - means of judging, as we are entirely ignorant of the constitution of the crust: and that the effect of local attraction on the Map of India constructed from the Survey would fortunately disappear as far as regards the relative position of places laid down, but that the precise position of the Map on the terrestrial spheroid could not be discovered, as it would depend upon the unknown total resultant local attraction arising from all causes at the station from which the Survey operations commence. 1865.] On Local Attraction. 35 M. Otto Struve has lately called attention to similarly important deflections caused by local attraction in Russia—and especially to a remarkable difference of deflection at two stations near Moscow, only about eighteen miles apart, which is attributed to an invisible unknown cause in the strata below. Tt has become, therefore, an important inquiry :—What degree of uncertainty does Local Attraction, if not allowed for, introduce into: the two problems of geodesy, viz. (1) obtaining correct Maps of any country, and (2) determining the Mean Figure of the Harth. These matters are discussed in the present Paper; and I would. here observe, that the paper is complete in itself, and does not require a study of the previous communications. 2. With regard to the construction of Maps from. Survey operations. I show, as before in India, that no map in any other part of the world will be affected except in the way already stated, if the length of every measured arc of latitude is not greater than twelve degrees: and a half, and of every measured arc of longitude not greater than fifteen. Now in point of fact, however long the great arcs (such as: the Anglo-Gallic, the Russian, and the Indian) may be, they are. always broken up into much smaller portions, so as to bring them very far within the above-mentioned limits. Hence the maps constructed from geodetic operations will always be relatively correct, in themselves ; but the precise position of the map. on the terrestrial. spheroid will be unknown by the amount of the unknown deflection. oi the plumb-line in latitude and longitude at the place which fixes the map. In India the effect of the Himalaya Mountains and the Ocean, taken alone, would throw out the map by nearly half a mile. And, as already stated, there is no way of discovering with certainty how much this is increased or diminished by the effect of variations of density in the crust. If, however, the calculations which I give in the third section of this Paper are accepted, they show that the effect of variations in the density of the crust below almost entirely counteracts that of the mountains and ocean at Damargida in latitude 18° 3’ 15’, and the displacement of the map is almost insensible if fixed by that station. If fixed by the observed latitude of any other station, the map will be out of its place by the local 36 On Local Attraction. [No. 1, deflection of the plumb-line at that station. This, in the Indian Great Arc, will not exceed (supposing my reasoning as described below is accepted) one-thirteenth of a mile at any of the stations where the latitude has been observed. It appears also from these calculations, that, except in places evidently situated in most dis- advantageous positions, the local attraction is rarely of any consider- able amount. 3. In the second section of the Paper I proceed to ascertain the degree of uncertainty introduced, by our ignorance of the amount of local attraction, into the great problem of the Mean Figure of the Earth. Bessel was the inventor of the method now in use for solving this problem. His method enables us to bring all the ares which have been measured in any part of the world to bear simultaneously upon the solution. He made use of arcs measured in eight parts of the earth’s surface ; called the Anglo-Gallic, Russian, Indian II, (or Great Arc), Indian I, Prussian, Peruvian, Hanoverian, and Danish Ares, the first three of which are very long. For each of these ares he made use of an algebraical symbol to represent the unknown error of the precise position of the are on the meridian. In his method he treats these eight quantities as independent variables; which is tantamount to ignoring local attraction altogether. The calculations, therefore, of the Mean Figure of the Harth hitherto made have left this most important element out of consideration. T’o remedy this has been my object. By a change, I venture to call it a correction, of Bessel’s method I have succeeded in obtaining formule for the semiaxes and ellipticity of the Mean Figure, which involve expressions for the unknown local deflections of the plumb-line at the standard or reference-stations of the several arcs. Ii a and 6 represent the semiaxes and e the ellipticity, the following are the results arrived at :— a=20928627 + 1057:°8¢, + 342°9¢, + 152°3¢, + 27°3¢, + 93:6¢, + 8°8t, + 63°7¢, + 62:91, feet. b=20849309—3762-6t, — 334:3¢, —661:3¢, —101:5¢, —372'6¢, — 14:01, — 249°3t, — 249-14, feet. From these we may easily deduce the ellipticity 1865.] On Local Attraction. 37 { 1+0:06087, +0-0085¢,-+-0:0103¢,+-0:0016¢,++0-0059,, + 0:0003¢, + 0:0039¢, + 0:001639¢, }. where t, t, ... t, are the eight unknown deviations of the plumb-line from the true vertical at the standard stations of the eight ares arising =a50 9 from local attraction. These formule for the semiaxes and ellipticity of the mean figure of the earth show us, that the effect of local attraction upon the final numerical results may be very considerable : for example, a deflection of the plumb-line of only 5” at the standard station (St. Agnes) of the Anglo-Gallic are would introduce a correction of about one mile to the length of the semi-major-axis, and more than three miles to the semi- minor-axis. Ii the deflection at the standard station (Damargida) of the Indian Great Arc be what the mountains and ocean make it (without allowing any compensating effect from variations in density in the crust below, which no doubt exist, but which are altogether unknown) viz. about 1724, the semiaxes will be subject to a correction, arising from this cause alone, of half a mile and two miles. This is sufficient to show how great a degree of uncertainty local attraction, if not allowed for, introduces into the determination of the mean figure. As long as we have no means of ascertaining the amount of local attraction at the several standard-stations of the arcs employed in the calculation, this uncertainty regarding the mean figure, as determined by geodesy, must remain. The effect of our ignorance in this case is far more serious than that already noticed in mapping a country with minute precision. 4. The third section of the Paper is occupied in devising means for removing this ambiguity. Although it has been necessary to assume one step in the argument, I think that the sequel shows that a very high degree of probability exists that the process is a correct one. Each of the three great arcs—the Anglo-Gallic, the Russian, and the Indian—is divided into a number of subordinate arcs. I therefore take each of these three great arcs and apply the method described in the last section to find the semiaxes of the ellipse which best represents that arc. The expressions for the semiaxes involve one unknown quantity, viz. the amount of deflection at the standard station of the arc. In this way I obtain the semiaxes of three ellipses, 38 On Local Attraction. [No. 1, involving three unknown quantities. The assumption which I then make is, that the Mean Figure of the Harth is a spheroid; that is, that these three ellipses are all the same. The effect of this is to give me four equations of condition, involving the three unknown quantities. These I solve by the method of least squares. The result is that the unknown deflections all come out very small; and the semiaxes of the three ellipses come out remarkably near each other in value. The first part of this result shows, what I have intimated in para. 2, that the local attraction arising from invisible causes hidden in the solid crust of the earth must be such, as very nearly to compensate for the effect produced by visible causes at the surface existing in mountains and oceans. And the second part of the result gives a very satisfactory solution of the problem of the Mean Figure taking local attraction into account, making the semiaxes 20926189 and 20855316 feet ue 2953 5. In the fourth or last section of the Paper I enter into specu- and the ellipticity = lations regarding the Constitution of the Harth’s Crust, suggested by the result of the preceding section. The following extract will best represent my views on this interesting subject :— “The first thing I observe in the results given in the last paragraph is the very small amount of the resultant deflections at the two extremities of the Indian Are—Punnee close to Cape Comorin, and Kaliana the nearest station to the Himalaya Mountains ; whereas the effect of the Ocean and the Mountains has been shown to be very large. This shows that the effect of variations of density in the crust must be very great, in order to bring about this near compensation. In fact the density of the crust beneath the mountains must be less than that below the plains, and still less than that below the ocean-bed. If solidification from the fluid state commenced at the surface, the amount of contraction in the solid parts beneath the mountain-region has been less than in the parts beneath the sea. In fact, it is this unequal contraction which appears to have caused the hollows in the external surface which have become the basins into which the waters have flowed to form the ocean. As the waters flowed into the hollows thus created, the pressure on the ocean-bed would be increased, and the crust, so long as it was sufficiently thin to be influenced by hydrostatic principles of floatation, would so adjust itself that the pressure on any couche de niveau 1865.] On Local Attraction. 39 of the fluid should remain the same. At the time that the crust first became sufficiently thick to resist fracture under the strain produced by a change in its density—that is, when it first ceased to depend for the elevation or depression of its several parts upon the principles of floatation— the total amount of matter in any vertical prism, drawn down into the fluid below to a given distance from the earth’s centre, had been the same through all the previous changes. After this, any further contraction or any expansion in the solid crust would not alter the amount of matter in the vertical prism, except where there was an ocean; in the case of greater contraction under an ocean than elsewhere, the ocean would become deeper and the amount of matter greater, and in case of a less contraction or of an expansion of the crust under an ocean, the ocean would become shallower, or the amount of matter in the vertical prism less than before. It is not likely that expansion and contraction in the solid crust would affect the arrangement of matter in any other way. That changes of level do take place, by the rising and sinking of the surface, is a well-established fact, which rather favours these theoretical considerations. But they receive, I think, great support from the other fact, that the large effects of the ocean at Punne and of the mountains at Kaliana almost entirely disappear from the resultant deflections brought out by the calculation. This theory, that the wide ocean has been collected on parts of the earth’s surface where hollows have been made by the contraction and therefore increased density of the crust below, is well illustrated by the existence of a whole hemisphere of water, of which New Zealand is the pole, in stable equilibrium. Were the crust beneath only of the same density as that beneath the surrounding continents, the water would be drawn off by attraction and not allowed to stand in the undisturbed position it now occupies. I have, in what goes before, supposed that, in solidifying, the crust contracts and grows denser, as this appears to be most natural, though, after the solid mass is formed, it may either expand or contract, according as an accession or diminution of heat may take place. If, however, in the process of solidifying, the mass becomes lighter, the same conclusion will follow—the mountains being formed by a greater degree of expansion of the crust beneath them, and not by a less contraction, than in the other parts of the crust. It may seem at first difficult to conceive how a crust eould be formed at all, if in the act of solidification it becomes heavier than the fluid on which it rests; for the equilibrium of the heavy crust floating on a lighter fluid would be unstable, and the crust would sooner or later be broken through, and would sink down into the fluid, which would overflow it. If, however, this process went on perpetually, the descending 40 On Local Attraction. [No. 1, crust, which was originally formed by a loss of heat radiated from the surface into space, would reduce the heat of the fluid into which it sank, and after a time a thicker crust would be formed than before, and the difficulty of its being broken through would become greater every time a new one was formed. Perhaps the tremendous dislocation of stratified rocks in huge masses with which a traveller in the mountains, especially in the interior of the Himalaya region, is familiar, may have been brought about in this way. The catastrophes, too, which geology seems to teach have at certain epochs destroyed whole species of living creatures, may have been thus caused, at the same time breaking up the strata in which these species had for ages before been deposited as the strata were formed. These phenomena must now long have ceased to occur, at any rate on a very extensive scale, as Mr. Hopkins’s investigations on Precession appear to prove that the crust is very thick, at least 800 or 1,000 miles ; and this result has been recently confirmed by Professor W. Thomson in a paper on the ‘ Rigidity of the Earth.’” These results meet with some confirmation from an examination of the direction of the deflection of the plumb-line at several coast- stations where it is drawn towards the sea. The amounts of deflection are, however, so small that much cannot be built upon this. This, at any rate, may be said, that they present no obstacle to the theory so remarkably suggested by the facts brought to light in India, viz. that mountain-regions and oceans on a large scale have been produced by the contraction of the materials, as the surface of the earth has passed from a fluid state to a condition of solidity—the amount of contraction beneath the mountain-region having been less than that beneath the ordinary surface, and still less than that beneath the ocean-bed, by which process the hollows have been produced into which the ocean has flowed. These coast-stations do in fact in several instances tend directly to favour the theory, as they seem to indicate, by excess of attraction towards the sea, that the contraction of the crust beneath the ocean has gone on increasing in some instances still further since the crust became too thick to be influenced by the principles of floatation, and that an additional flow of water into the increasing hollow has increased the amount of attraction upon stations ‘on its shores, ‘T am, your’s faithfully, Calcutta, August 2, 1864. Joun H. Prarz, 1865. | On Local Attraction, 41, Postscrupt. [Received 29th April, 1865.] Ii the raw or uncorrected results of the Surveys in India and Europe (I mean uncorrected for local attraction) are made use of, they bring out meridians of a slightly different curvature in these different parts of the earth. If these were the true forms of the seve- ral meridians the result would be that the equator could not be a circle and the figure of the earth not a spheroid of revolution. A few years ago, General T. F. de Schubert calculated the form of an ellipsoid of three unequal axes which would best suit the observations. Captain Alexander Clarke, R. HE. (Memoirs Roy. As. Soc. Vol. XXIX, for 1860,) went through the same calculation, following Bessel’s method. His result was thatthe equatorial radius-in longitude 14° or there- abouts is one mile longer than that in longitude 104°. He speaks with hesitation regarding the result, on the ground that the data are far too scanty to lead to a conclusion to be relied upon. He appears, however, not to shrink from the hypothesis on which he works, from the true grounds of distrust, viz. (1) the @ priori improbability that the earth’s mean figure is not one of revolution, as the evidence of the fluid-origin of that figure is overwhelming* and (2) that the effect of local attraction is altogether overlooked by him. General de Schubert indeed in a subsequent paper (See Monthly Notices of Royal Astrono- maical Soc. for 1860, p. 264, where it is noticed) does anticipate that local attraction may modify and altogether destroy the data on which he rested the argument of an ellipsoidal figure. The Paper which I have sent to the Society and have noticed in this letter gives, for the first time, a method for estimating the effect of local attraction and proves (in the third section) that so very moderate an allowance as 1” or 2” for local attraction will altogether destroy the disparity between the curvature of the different meridians. When the arguments in this paper are impartially weighed I feel convinced that the improbable ellipsoidal theory will be abandoned altogether. * The evidence, with full details, is given in the third edition of my treatise on the “ Figure of the Harth” now passing through the press at Cambridge and a copy of which when published,J purpose sending to the Society. 6 42 On Local Attraction. [No. 1, From the above letter it will be seen, that I come to the conclusion that the earth’s crust below the mountains is somewhat less dense than below the plains; and still less than below the ocean-bed. Mr. Airy (Phil. Trans. for 1854, p. 101) came to the former part of this conclu- sion. But his argument requires that the crust should be thin—and so thin as to be influenced for its position by the principles of floata- tion. But Mr. Hopkins’ and Prof. W. Thomson’s results show that the crust cannot be thin. Moreover Mr. Airy’s line of reasoning does not lead to the latter part of the result, in that the crust is more dense below the ocean-bed. For these reasons I have not alluded to Mr. Airy’s hypothesis in my Paper. The argument therein explains both these phenomena without requiring that the crust should be thin, but rather the contrary. Notes to accompany a Geological map and section of the Lowa Ghur or Sheen Ghur range in the district of Bunnoo, Punjab ; with analyses of the Lignites—By Avert M. Vurcuzre, Ese., M. D. [Received 10th June, 1864. ] Description of the Section, Pl. ILI. 1. Hillocks or morraines formed by the pebbles and boulders of miocene conglomerates and sandstones which have been removed by the effect of the rains: the sand is carried away to the plain, but the boulders and pebbles are left behind and form a morraine. The stones have arranged themselves in layers resting against the miocene beds, with an inclination towards the plain (W) of 20°. 2. Miocene (?) sandstone, very friable, grey or rather salt and pepper ; calcareous and often so soft that it can be crumbled in the hand. It contains boulders and pebbles, well rounded and worn, generally arranged in bands. It is these boulders and pebbles which form No. 1, as No. 2 is being destroyed. The pebbles and boulders are greenstone, quartzite, quartzose porphyry, gypsose agglomerate, carboniferous and nummulitic limestone, etc. 3. Similar to 2, but a little harder, and contains occasionally bands of slate in a state of disintegration. Carbonized wood found here, (seldom,) in an iron-stained sandstone. Vol. XXXIV. Part I. Pl2. ve Gungee Wan —————— == Moral \la wan aa ee) ( / NN \ \ ad \\ Section, Soollan Khel er Surrnng PA (5 Miles from the tidus) as \ €0. opical Sheteh Map of THE LOWA GHUR on SHEEN GHUR, in the district of BUNNOO —— oe. —— [SSF Diluvial Talus Miocene(?) Sandstone [SSF Nummullitic Limestone Carbonaceous Shales with +) beds of “Rol” and lignite AM Verchere Seale: Two English Milea te One Inch. ee 8 e Vol xxxtv. Part 0. Plat. Journ As: Soc: Bengal x 1 fate 5. Section across the Lowa Ghur or Sheen Ghur false called lecally Srunya, Maidand, Meslakid er Mittah Rok or Puhar) from Snuwa to near Seoltankel Direction: WNW—-ESE (True Sectien) The Nummutilie Cermaticn is here’ will displayul; ik hat a tal thickness of #500 fist The Seocene? Sandstone anst Canglemirate ure! much: Vaulbyl the fults being parallel te the Strike: SCALE 2000 FEET TO 1 INCH Byes oe = F oe re ue 7 topes reer HALT? 4357 (® above the Sex mits U3 H in 3 aes Plain of Burmoo Valley 2 1 oy B30 F* akeve the Sex Soe a > eee LL ae Elent W.N.W. : a ——— Highest S e) = Summit of Range / / ‘ ‘ Datum Line, the Bank of the Indur a ioe ff ie 782 feet above the Sea. 20. f $6. 50. 5 7 5 On Transfer Paper by Shoik Munneeraddcen LTH) MY HM SMITH SUAVSCENES OFFICE CALCUTTA WAY Ihu6 1865.] Notes to accompany a Geological map. 43 4. Harder and greyer sandstone. The bed has been broken up and re-cemented by a coarser, more salt-and-pepper-like sand. The pieces of the original bed are seen sticking out at all angles like drifted ice. On the east side of the valley of Maidani, this breaking up is not observed. 5. Conglomerate composed of yellow limestone pebbles cemented by a very hard calcareous cement. The cement appears first to have coated the pebbles with two or three coats of various shades of yellow or brown, like a calculus of the bladder, This bed is seen always (west of the Indus) on the top of the nummulitic or bottom of the miocene beds. It is striking in appearance, especially when polished by a running torrent. 6. Flesh-coloured, hard, nummulitic limestone, weathering rough, pitted and grey. It contains a few nummulites of small size and a few small bivalves. 7. Limestone, argillaceous and yellow; it is arranged in concentric masses cemented by an earthy marly limestone. Both the rounded masses and the intervening earthy rocks are full of fossils ; N. Leevigata and N. Pushi are abundant; also a small flat species and two species extremely gibbose and always very abundant in muddy nummulitic limestone. Bivalves very numerous, Casts of Trochus very abundant. A large Spatanchus, 6 inches across, found here also. 8. Limestone, glaring-white like chalk and not much harder than chalk. It contains the same fossils as the preceding layer, but no Spatanchus. K is of very great thickness and forms a high white cliff facing the east and remarkable from a great distance. 9. Slate im a state of decomposition. It is interbedded with limestone and occasionally contains small nummulites; but it is generally without fossils. 10. Carbonaceous shale with beds of “Rol” or alum shale and of lignite. The Rol and the lignite beds are generally in contact with the nummulitic limestone above. 11. Shales of all colours, white, red, yellow, grey, olive, nearly black ; very calcareous, with thin beds of muddy limestone (very soft) containing debris of shells, rootlets and stems of plants. No nummulites in these beds. Some of these shales are a good fire-clay and are used to make crucibles. These shales are generally more or less wavy. 44 Notes to accompany a Geological map. [No. I, Examination of the Lignites. The following samples were given to me by Lieut. Lane, District Superintendent of Police, Bunnoo. No. 1.—From a seam newly discovered near Chushmea, north of Moolakhel, 8 miles from the Indus. Best quality, with a resinous fracture and lustre ; jet black in colour; Sp. gravity 1.25. Volatile inflammable substances, . : : : a5 Fixed carbon, Ash, ; : : ; : ; ; : ay 2 0t8) There is a partial caking when the lignite is burnt in a close vessel. The ash is a mixture of a reddish earthy powder, of hardened pieces of slaty shale (holding a little unreduced lignite) and of a fluffy white ash like wood-ash. The red earth and the pieces of shale are mechanical impurities. The white fluffy ash is the proper ash of the lignite. No. 2.—Best quality, as No. 1. Apparently a very little yellowish white clay adhering to the lignite which is 13 inch bedded. From the same locality as No. 1. Volatile inflammable substances, . “ : ou Fixed carbon, . : ; ‘ : : ; . 40 Ash, . , ; ; : ‘ ° : ; 5a ELD Same remarks as for No. 1. No. 3.—Middling quality, the usual quality of the bed. The lignite is in thin plates like leaf bed; each thin plate is sometimes resinous in appearance, but more frequently has the appearance and Iustre of charcoal. It contains a considerable amount of yellow clay between the plates. It crepitates in water like salt deflagrating on fire. Its Sp. gravity is 1.28, 1865.] Notes to accompany a Geological map. 45 From the same locality. Given by Mr. Lane. Volatile inflammable substances, . ; : , y) 25 Fixed carbon, . : . , . : : . AO Ash, ; : > . , ; : 35 100 NV. B—Some of the volatile substances were unreduced in the experiment, and consequently increased the percentage of fixed coal above its proper figure. The ash is mostly a reddish powdery earth with pieces of shale; very little fluffy ash. No. 4.—Middling quality like No. 3. Structure woody. Same locality. Given by Mr. Lane. Volatile inflammable substances, . : ; . 46.66 Fixed carbon, : - ; Sea : , 20:83 PE Nk oa a oy, ee aad yo OAD) 99:99 Ash, like No. 3. No. 5. Picked specimen, having the appearance of fine jet. Heavier than the preceding specimens and very resinous in appearance. . Obtained from a native who said that it came from a seam near Sooltan Khel. . : Volatile inflammable substances, . he ee Meus Himedearbon aims: ei ee ae iis ASH : . ; : , - ‘ ; ySEsd soEeg The ash was nearly entirely composed of white fluffy ash, like wood- ash. This lignite cakes a good deal in the close vessel, Average of four analysis of the Chushmea mine, Volatile inflammable substances, , : ~ 42.91 Fixed carbon, ; 5 : ; F . » 33.95 NSE a , E : m : : : pon kG 99.96 46 Notes to accompany a Geological map. [No. 1, I copy here Dr. A. Fleming’s analysis of the lignite of Kottree near the Chichalee Pass as it is evidently a continuation of the beds seen a few miles south of the Pass at Chushmea. Volatileinfammable matter, | . . . 86.421 Carbon, . : : ‘ ; : - pe o39)/() Ashes, z 5 3 - : . 380.000 100.000 The coal or lignite from Sooltan Khel (see No. 5) comes nearer to the Baganwallah lignite as analyzed by Dr. A. Fleming. Compare my No. 5 with the following analyses copied from Dr. A. Fleming’s report :— Baganwallah, No. 1. ° ' Baganwallah, No. 2. Volatile, . SNS AUGANT Volatibes 00). Up teaser ate Carbon, . : . 41.36 Carbon, . ; a) 2590'S Ashes, : . ls s00 Ashes, . : - 1.840 100.00 100.000 Average. Volatile, . 4 : : : : ‘ . 89.547 Carbon, ‘ ; ‘ A ; : : , 00.532 Ashes, : ‘ ! : : : : 5 OL 20) PSE) To conclude, I enter here a table of the composition of the lignites of the Lowa Ghur, of Baganwallah, and of the coal of Raneegunj and Sirsol in Bengal and of some coal in the British Islands. 4T Notes to accompany a Geological map. 1865.] “HURHOUEA “WW LYAaTV 166 og’ 769 OL'0L 69° O1t Vor 0266 €&'8 Tete ae a ae cS Sy 668 094 os79 OLLP 669 goa Tg G&S'0G 00°ST cess *"* oe *** Toqreg PeXhy 6871 0G'26 «6 9'8G—sC«OD TL ST Ss Gog G8& LVS'6& 99°97 T6'sp *"'f19}{VUL O[QVUIUIVBUL O[14BIO A, Ton Maye ‘OTeA MAT ‘SeMpog + “puasTem "poodkyuog "Joss *HOVTLV MA *SaTV AA. ‘GNVILOOD ‘SHIVA “IVONGG ‘SONVY LIVE “OONNAG, ‘spunjsy ys ay) fo pun jobuag fo 1009 ay) {0 pup qolung oy fo apubuy ayy fo worupsodiuos oyp fo 0790) arapouncdmoQ 48 Sceintific Intelligence. [No. 1, Screntiric [LyTrELLIGENCE. Mr. T. Tomlinson, late Superintendent of the Barrackpore Park, has recently succeeded in hatching an Ostrich by placing the fresh-laid egg in a box lined with straw and exposing it to the sun by day for some weeks, keeping it under a domestic fowl during the night. To prevent one side of the egg being more exposed than the other, it was occasionally turned over. ‘The new born bird is doing well. Col. Dalton from Chota-Nagpur announces the discovery of a vein of lead in a hill named Puttia near the village of Pelowa, Tuppeh Ramkola, in Sirgooja. From an analysis of the specimen forwarded by Col. Dalton, it appears to be pure galena with a small trace of silver and the ore is tractable. When fairly cleared, its value would be in England from 12£ to 13£ per ton. An attempt to work the mine was made, but the outturn not proving profitable, it was abandoned. The following is from our late Curator :— Belmont, St. Briavel’s, W. Gloucestershire, Dec. 2, 1864. My pear Grotre,—In the Reader for November 19th, you will read that a paper was read by me at the Zoological Society on November Sth; but I was not there, having left a short paper with Sclater. In the Proceedings, p. 335 of our Journal, I observe ‘ Kelis Jacquemonti’ mentioned. 'This I consider to be merely the longer-furred mountain variety of I’. chaus ; F’. ornata too, I now refer to F. torquata, F. Cur. ; and celidogaster turns out to be African, and distinct from vzverrina, F. torquata of Sykes being a striped domestic Indian cat,—at least identical with the latter, whether or not descended from domestic stock. A dead Tiger from Barrackpore is mentioned in the same page of the Journal. I hope this was skeletonized, because I could get you a Megaceros skeleton in exchange for it! Lastly, about the “ new species of Varranus” in the same page, I presume this to be the Hydrosaurus noticed by me from the Andamans and Nicobars, which I could not perceive to differ structurally from H. Salvator, I suppose 1865.] Scientific Intelligence. 49 you have received Giinther’s work on Indian reptiles, which will materially assist the study of them. I do not, however, agree with him in all cases ; for instance, his identification of the Bengal Emys ocellata with the Tenasserim £. Berdmorei.—He has certainly not seen specimens of the former, and I wish that some could be sent to him. The species is not very commonly brought to the Calcutta bazar, but by offering a slight reward to one of the museum servants a few might be obtained, and there is a good series of both races in the Society’s museum. I have written pretty regularly to Jerdon, communicating to him what I learn; but he has not largely availed himself of my notes in his Appendix, and I seldom hear from him. He never was a good correspondent. I certainly told him in good time for publication that the common Indian Curlew is not Numenius arquata, but N. major, Schlegel, figured in the Fauna Japonica ; and I sent British specimens of the former to the museum. He is quite wrong, too, in placing the Burmese Peafowl in Asim! The Indian species occurring so far round as Chittagong. The Gallus Tem- minckw, Gray (p. 541,) which he mentions as a peculiar species, is a most obvious hybrid between bankivus and furcatus, though differently coloured from the so-called G. aneus. In p. 481, he is quite wrong in identifymg Turtur chinensis with T. tigrinus : the former is much larger, with quite plain plumage on the back, and is correctly figured by Sonnerat. Both are in the Society’s museum. I cannot make out the middle-sized Indian Cormorant erroneously referred to sinensis in p. 862. P.870,1.3. For “ poliogenys,” read pyrrhogenys. P. 597. T. ocellatus, the Philippine species (/uzoniensis, Gm.,) is quite distinct from the Indian 7. pugnae, to which Jerdon’s other synonyms belong. Arboricola rufogularis, (p. 598) was sent by Tickell from Tenasserim, as noticed in one of my Reports. Another time I will annotate Jerdon’s work for you in detail. About the Darjeeling Kalij Pheasant (melanotus), these breed at the Gardens, and are distributed, but not any have died, to be promoted to the British Museum. A good pair of skins would accordingly be acceptable. Bruce has sent from China a noble pair of skins of Crossoptilon Mougolicum, Swinhoe, (auritum, Pallas, apud Sclater,) and ditto of a new species of Pucrasia, P. xanthospila, H. R. Gray, from the mountains N. W. of Pekin. The sexes of the former only differ in the male being larger 7 50 Scientific Intelligence. [No. 1, and spurred. Hodgson’s Cr. t2betanwm still remains unique, I believe. The localities assigned to many specimens in the British Museum are unreliable. Thus the Burmese lineated or pencilled Kalij is assigned to Bootan, and various Tenasserim squirrels, also to Bootan, all doubtless from the same collection, but received with the erroneous locality from the old India-house. The distinctions we recognise between Indian, Indo-Chinese and Malayan fawne are little understood by naturalists here who will have all alike, to be Indian. Giimther’s Indian reptiles, for example. About Sikhim and Asim monkeys. I look upon assamensis (original specimen in India museum,) as a mere variety (not unlikely an individual, var.) of rhesus, wanting the fulvous hue oi the hair on the hind-parts. JZ. pelops I know little of, but Jerdon should get this at Masuri. Of the Lungoors, I know nothing of more than one Himalayan species, which is Hodgson’s schistaceus. Does true entellus range, into Asém, and is it not the Hunuméan of the table-land of 8. India? Is not priamus peculiar to the ghats and mountainous country, as Johnii (verus) is certainly peculiar to the W. ghats? Ido not remember who wrote the Review of Jerdon’s work in the Annals, and cannot refer to it here. Smythe has yet to shoot the Shau, and perhaps the Tibetan Lynx. Is it the wild yak he thinks of sending home alive? The tame breed here as regularly as domestic cattle. A young bull was calved last year, and a cow this year, at the Zoological Gardens; both females hornless. Pallas refers to wild two-humped camels in the Mongolian deserts; and not many years ago the existence of wild yaks was doubted by Hutton and others. In the long stretch of desert country between the Red Sea and the valley of the Nile wild one-humped camels are numerous; and I see no reason why these should not be aboriginally wild, like genuine Asznus vulgaris in Africa (the a. tenispus, Henglin). There is a fine male of the latter now in the Zoological Gardens, a most decided and unmistakeable true donkey or Onager ; and the series of wild asinine animals (nclud- ing zebras) is complete, every known race or species being represented. All of the animals brought by Thompson were alive when I left London and the Hornbills in first rate condition. The Aceros nipalensis would be a grand prize; have not both semes the rufous plumage in the nest? Reversing the usnal arrange- ment, in Lhynchew and in Turma pugnax, the adult females are the 1865.] Scientific Intelligence. 51 more ornamented, and the young resemble the old males! The old she-rhinoceros soon made friends with the young ones, but is kept separate from them. Bos sondazcus did not die from the injury to the foot. That was a very slight affair and soon over; there was a ‘gathering, when the animal walked lame, and he recovered as soon as it was lanced. He grew much, and became in fine condition, and when he died the mass of thickened cuticle had begun to form between the bases of the horns; but the colour of the coat had not begun to blacken. Poor fellow, he is now admirably stuffed, in the B. MW. He died of inflammation of the bowels. In the Zoological Gardens, are one pair Arboricola torqueola, two pairs Ortygorms gularis, and one pair of each Indian species of Galloperdix, all in first-rate health and condition. The ‘blood-pheasant’ (thaginis cruentus) from interior of Sikhim, is a great desideratum. A young African wild boar (S. Scropha vera) has been put to S. Andamanensis, but I believe with no result as yet. I suppose there is no chance now of getting a boar of the Andaman race. Thanks for the Darjeeling Shrews and Bats, which I look forward with interest to see. F. More, when I last saw him, was mainly interested in insects of economical value, as honey-bees, &c. Has the hive bee of Kashmir ever been scientifi- cally examined? It is likely enough to prove as distinct as the Ligurian Bee. Just before I left London I saw, with Wolf, in spirit, a most curious new mammal, sent by Du Chaillu from Fernando Po. Tt is an Otter-like modification of the order Insectivora, and the most distinct new genus of mammal that has turned up for a long time. Tt will be figured and described in the forthcoming Number of the Tr. Z. 8. Size of a large stoat, but more bulky, with tail exceedingly tumid at base, laterally flattened for the remainder. Whiskers very copious, thick and coarse, as in Cynogale Bennettw. Eyes small. Two of the hind toes connected, as in so many marsupials. General appearance, colour and fur, very otter-like. Front teeth hooked, approaching to Sorex. Alphonse Milne Edwards has published a monograph on the Chevrotains, upon which part of my note bears. I have sent the particulars to Jerdon, and by the way I wish Jerdon would contribute to the Journal a selection from the many notes that I have sent him. There are two groups of Cheyrotains (united by A. Milne Edwards,) viz. Meminna of India 52 Scientific Intelligence. [No.-4, and Ceylon, and Tragulus of the Indo-Chinese and Malayan countries, —for Wf. malaccensis, Gray = I. indica. Of Tragulus, there are 3 large races and 3 small, as follow :— 1. Zr. napu, F. Cuv. = javanicus apud Gray and Cantor. One specimen in Calcutta museum. =o | 2. Tr. Stanle a4 4, yanus. = | 3. Ir. (like last, but with black sides of neck and breast-marks? n in Calcutta museum 6 ¢, and unknown here.) (4. Tr. javanicus (verus) = pelandoc, nobis, from Java only, L | suspect, and one $ only in Calcutta museum. Numerous 3 specimens in Liverpool museum. wa a Tr. kanchil. Extends to 8. Tenasserim. 6. Tr. afinis, Gray, placed as asynonym of Kanchil by Edwards, and the original specimen so named by Gray, from Malacca, is just a Kanchil wanting the medial breast-stripe ; but others sent by Mouhat from Cambodia appear to be a distinct race, whatever name it may bear. The Society's museum has all but the last, and the specimens should be re-labelled according to this present determination of them, 1865.] Contributions to Indian M alacology. 69 mouth. Aperture oblique, lunate, the breadth double the height, columella furnished with a spiral lamina which runs throughout the whorls, and renders the shell opaque around the umbilical excavation. Peristome simple, very slightly thickened inside, arcuate at the base oi the right margin ; margins distant, the columellar oblique. Millem. inch. Major diameter,...........s.scs00 10 0.4 Minarmcitios 2 Gelder. lost ee 9 0.36 Jy Sa Ret eet meee oe ee 7 0.28 Aperture 4 millem. broad, 2 high. Animal small with a very narrow foot, a very small mucus pore at the end, and a small lobe above. Habitat—Arakan hills near Prome; more abundant on the Arakan than on the Pegu side. This very pretty little snail, which is nowhere common, is re- markable for the screw like lamina on the columella, running up throughout the whorls. The indentation on the base of the lowest whorl is also peculiar; it varies considerably in position and form, being sometimes double, but it is almost always present. The animal bears a great resemblance to that of Nanina pylaica, Bs. | The subgenus Sesara was founded by Albers for Nanina infrendens, Gould, (supposed at first to be a Helix, ) a peculiar little Molmein shell with teeth inside the peristome. I have no hesitation in uniting to this species, besides the closely allied WN. capessens, Bens., the T’ridopsis- like NV. pylaica, Bs, and the present species, as well as the two fol- lowing. WN. pylaica, N. capessens, N. infrendens, and the present species are all distinguished by peculiar additions to the peristome, and form together a well marked group, all being more or less depressly trochiform, horny, with closely wound narrow whorls, arcuately costulate above, and smooth beneath. N. helicifera was found rarely on the road between Prome and Tongoop, and somewhat further south. In the Bassein district it appears to be replaced by N. Basseznensis. 6. N. MAMILLARIS, n. sp. Shell minutely perforated, very depressly trochiform, suborbicular, thin, horny; finely, closely and arcuately costulated above, the costu- lations passing over the periphery ; smooth, shining, and radiately 10 70 Contributions to Indian Malacology. [No. 2, striated beneath. Spire depressly conoid, with convex sides, the apex slightly acuminate and papillar; suture but little impressed. Whorls 73, convex, closely wound, slowly increasing ; the last sharply keeled, flatly convex beneath, marked in nearly adult and sometimes in full grown specimens, with two or three small pits of variable form, opaque from corresponding internal calli, and generally arranged in an oblique line opposite to the mouth. Aperture oblique, sub- rhomboidally lunate, 3 times as broad as high ; columella furnished in young specimens with a more or less rudimentary spiral lamina running up the whorls, which is obsolete in adult shells. Peristome thin, slightly curved forwards at the base ; margins distant, columellar margin very oblique. Millem. inch. Wayjpridiameter te se ceraced-cee 11 0.44 (Manor at toyita.c chon eee ee 10 0.4 BASKIS Su tea ree Are Was 63 0.26 Aperture 54 millem, broad, scarcely 2 high. Animal similar to that of WN. helicifera. Habitat—Akoutoung, Pegu—not rare. The close relation of this species to the last is unquestionable ; besides resembling it in general form, texture, and sculpture, and in the characters of the animal, young specimens possess a similar columellar fold, and indentations on the lower surface somewhat resembling those of NV. helicifera, though less deep and more opaque. Both these characters, however, appear to become obsolete in adult specimens of the present form. The two species are easily distin- guished by the absence of the columellar lamina in adults of WN. mamillaris, which may also be recognised by its acuminate apex, lower spire and flatter base. 7. N. Bassernensts, n. sp. Shell minutely perforated, globosely trochiform, subcampanulate, thin, horny, closely, sharply and arcuately costulated above, the costu- lations passing over the periphery to the under surface, which is smooth, shining, and radiately striated. Spire obtusely conoid, with convex sides; apex obtuse; suture slightly impressed. Whorls 7, slightly convex, closely wound, slowly increasing; the last not de- scending, flatly convex beneath, more tumid near the mouth, keeled 1865.] Contributions to Indian Malacology. | 71 at the periphery, the keel vanishing near the mouth. Aperture lunate, oblique, breadth more than double the height; peristome thin, curved forwards at the base ; margins distant, columellar oblique. Millem. inch. Major diameter,..............0008 11 0.44 Minor Gitio; oo ccten Soic less ss 10 0.4 JSS, pad ee Ae Me ea 73 0.3 Aperture 52 millem. broad, 2 high. Habitat—Southern portion of the Arakan range of hills near Bassein and Cape Negrais. This shell is distinguished from N. mamullaris by its non-acuminate apex, higher spire and more convex base, and from JN. helicifera by the absence of the columellar lamina, of which no trace appears in the present species. It appears to replace the last named shell in the southern portion of the Arakan hills. It is scarce, and I have met with but few specimens in good condition. I have never seen the animal, which, however, is doubtless similar to those of the two preced- ing species. Section Trochomorpha. 8. N. conrinis, n. sp. Shell minutely perforated, trochiform, very thin, whitish horny, smooth, shining. Spire conical, apex slightly obtuse, suture scarcely impressed. Whorls 7, flatly convex, marked above with 4 or 5 spiral ribs and fine oblique lines of growth; the last sharply keeled, flatly convex beneath, and very finely radiately striated. Aperture oblique subrhomboidal, twice as broad as high; peristome thin, acute, straight ; margins distant, columellar subvertical, briefly and triangularly reflexed. Millem. inch. Major diamicters. i... 00.00 55..0a es 104 0.42 Wirmormcdnitos, Vi. sk eae ; 4 0.38 ASUS. 3 bce con ee eee e 7 0.28 Aperture 5 millem. broad, 23 high. Habitat—near Thayet Myo, on the borders of British Burma; also near Ava. A near ally of N. arx, Bens., from Tenasserim, which, however, may easily be recognised by the concave sides of its spire. From other 72 Contributions to Indian Malacology. [No. 2, related species, as NV. enfula, Bens., N. cacuminifera, Bens., and N. attegia, Bens., N. confinis is distinguished by its sculpture. 9. N. cuLMEN, n. sp. Shell very minutely perforated, trochiform, very thin, horny, trans- lucent. Spire conical, apex obtuse, suture impressed. Whorls 6, convex above and ornamented with fine raised spiral lines, and oblique striz ; the last whorl sharply keeled at the periphery, not descending, swollen and minutely decussately striated beneath, Aperture but little oblique, subquadrately lunate; height less than the breadth; peristome simple, thin; margins distant, columellar vertical, slightly reflexed above. Millem. inch, Major diameters: 2... .cinsees. 6 52 0.23 Minor dittoel. aad ied peel 4 54 0.21 PAGS hfe Gems abe AM olsen al te os 0.22 Aperture 3 millem. broad, 2 high. Habitat—Akoutoung and banks of the Tsanda Khyoung, Henzada district, Pegu. Hasily distinguished from N. confinis and N. attegia by its smaller size and higher spire; from N. arx, by the sides of the spire bemg straight and not concave, and from the Bengal N. infula, Bens., by its sculpture, and its sharper keel. 10. N. @RaruLator, n. sp. Shell perforated, turbinate, thin, whitish horny. Spire conical ; apex obtuse; suture impressed. Whorls 5, slowly and regularly in- creasing, convex, spirally lirate and marked with oblique striz of growth above; the last whorl keeled at the periphery, convex and decussately marked with concentric and radiating strie below, not excavated around the perforation. Aperture diagonal, subtrapezoidal, breadth exceeding the height; peristome thin ; margins distant, united by a callus; basal deeply sinuate ; columellar vertical, forming a right angle with the basal, and briefly triangularly reflexed above; reflexed portion thickened and passmg half round the perforation. Millem. inch. Major diametersey. neues 5) 0.2 Minors itto, §.c:teets seamen see 4} 0.18 OAL ROE AERATED. BRR EP nH te Bate 4 0.16 —_ ss. 1865.] Contributions to Indian Malacology. 73 Aperture 5 millem. broad, 2 high. Animal with a small mucus pore, and very small lobe above. Habitat—Irawaddy valley, Pegu. This pretty little species abounds near Thayet Myo, and occurs throughout the Irawaddy valley in British Burmah. I do not re- member meeting with it in Arakan. It is easily distinguished from all others of similar form among Indian shells, by its very oblique mouth, by the peculiar columellar margin of the peristome, and by the strong lirate sculpture. I have much doubt as to whether it should be assigned to Zrochomorpha, the species of which group are larger, and the animals somewhat different. Section Kaltella ? 11. N. conuna, n. sp. Shell subperforate, turreted, white, horny, thin, translucent, marked with oblique sinuous subfiliform costulate striation, and, below the centre of the whorl, with very fine spiral lines, only visible under a powerful lens. Spire conical, apex rather obtuse, suture deeply sunk. Whaorls 6, very convex, keeled in the centre, the keel very fine, raised, thread-like, opaque and white; the last whorl bicarinate, the second raised spiral line being below the periphery ; flatly convex beneath, and marked by radiating strie and concentric impressed lines. Aperture oblique, tumidly and subangulately lunate, about equally broad and high ; peristome thin ; maigins distant ; columellar nearly vertical, very briefly reflexed at the penultimate whorl. Millem. inch. Diameter, ......... agel neat 13 0.07 Plevobt.).. 1) Wate ais ea es a 4 2 0.08 Habitat—Phoung ditto. Arakan. A minute species remarkable for its keeled and convex whorls. Only 4 specimens were found. Genus HELIX. Section Plectopylis. 12. H. Karenorvum, n. sp. Shell sinistrorse, very widely umbilicated, discoid, flat above, solid, white, with rather irregular oblique pale chesnut streaks crossing the whorls, transversely and sinuously striated with decussating spiral 74 Contributious to Indian Malacology. [ No. 2, lines above and below; epidermis thin, horny. Apex minutely granulate or sub-granulate, almost imperceptibly raised above the flat spire; suture not impressed, very narrowly marginate. Whorls 6, narrow and closely wound, flat above; the last angulate above the periphery, rounded beneath, descending close to the mouth, very slightly compressed behind the same. Umbilicus very shallow, exposing ail the whorls. Aperture, diagonal, truncately subcireular ; peristome white, reflexed throughout, margins joined by a raised bar, from the centre of which a lamina passes up the parietal side of the whorl to the plication, which lies at about + the circumference of the whorl from the mouth, and resembles that of Helix achatina, Gray ; the parietal transverse lamina being simple and oblique above, then bifureating, giving off the lamina which runs to the mouth, and two short basal supports. A thread-like lamina also runs along the extreme base of the parietal side of the whorl, and joins the aperture. Palatal teeth 5; the upper 3 and the lowest longitudinal, the upper- most very long and thin, the 4th vertical, corresponding to the fork in the parietal lamina. Millem. inch. Major, diameter’... 0.420 nae 13 0.52 Miamon nth O we ceet ch tse ae cee 11 0.44 Be 1 Samet ier Renae TAs SAI 4 0.16 Habitat—Banks of Tsanda Khyoung, near Kaintha village, in Henzada district, Pegu. Larger variety ; major diameter 18 millem. minor diameter 15, height 5. A very few specimens were found on the banks of the Nungatho Khyoung, Henzada district. This shell combines the external form of H. lecophis, Bens., and H. refuga, Gould, with the internal plication of Hl. achatina, Gray. From both the first named species, however, the present may be easily distinguished by its more perfectly discoid shape, by its smaller height, and more open umbilicus, as well as by its colouring. Exter- nally, it is a very different shell from H. achatina, being of not more than half the thickness of that species. The internal plication, however, is absolutely undistinguishable. Like many other shells in Pegu, this species has evidently a very local distribution. In the spot where it was found first, among some limestone rocks forming a low ridge skirting the right bank of the 1865.] Contributions to Indian Malacology. 75 Tsanda Khyoung, it was abundant, but it was not met with again until 3 or 4 specimens of the larger variety were found nearly 50 miles further south. The locality given by Mr. Benson for Helix leiophis is Kwadouk near Thayet Myo. The shell also abounds at Akoutoung, on the Trawady, below Prome. 13. H. pERarcta, n. sp. Shell sinistral, widely umbilicated, discoid, rather thin, white, transversely sinuously striated, with faintly marked decussating spiral lines above and below. Apex minutely granulate, slightly raised above the flat spire, suture rather deeply impressed. Whorls 6, convex above and at the periphery, the last a little compressed behind the mouth, descending suddenly to the aperture, which is oblique and roundly lunate ; peristome white, expanded all round; margins joined by a somewhat curved ridge, from the centre of which a lamella runs up the whorl towards the parietal plication, which, however, it does not join. The parietal vertical lamina is single, simple, rather short, slightly curved, with a rudimentary transverse plait at the top. Two free horizontal lamelle occur beneath that running to the aperture, the lowest being the longest and thinnest, and running back beneath the base of the vertical lamina. Palatal teeth 6, all horizontal except the 4th and 5th, which are slightly oblique. Umbilicus open, deep, exposing all the whorls. Millem. inch. Major diameter,...... Seat a A 11 0.44 WRG ORITEEOS ee Oe 9 0.36 Feta sae ee Sadan: 4 0.16 Habitat—Mya Leit Doung, near Ava. Distinguished from its allies, H. refuga, H. levophis, and H. Kareno- yum, by its deeper suture and rounded whorls, and internally by the shorter parietal lamina, and by the 5th palatal plait being less oblique than in /eiophis, and not backed by a second plait as in refuga. This species is the smallest known amongst those belonging to the Burmese types of Plectopylis. 14. H. Feppent, n. sp. Shell sinistrorse, very widely umbilicated, discoid, flat above, thin, dull white, marked by rather irregular oblique sculpture both above < 76 Contributions to Indian Malacology. [No. 2, and below. Spire quite flat, apex not rising above the surface, suture impressed. Whorls 6}—7, narrow and closely wound, slightly convex above ; the last much broader, rounded at the periphery and beneath, descending abruptly close to the mouth. Umbilicus shallow, exposing all the whorls. Aperture more nearly horizontal than vertical, sub- circularly lunate. Peristome slightly thickened, expanded throughout, margins joined by a rib, from the centre of which a lamina sometimes runs up to the parietal plication, but is frequently interrupted a short distance within the aperture, and is always thicker and higher near the mouth than further back. Parietal plication consisting of a verti- cal lamina in front, and a second, slightly oblique, just behind the first, giving out the interrupted lamina running to the aperture from the top, and a shorter horizontal lamella from the bottom ; the hinder with small re-entering supports above and below. Beneath both is a narrow free thread-like horizontal lamella. Palatal teeth 5: Ist, 2nd, 3rd and 5th horizontal, 4th vertical and stouter than the others; Ist and 2nd longer than the remainder. Millem. inch. Major diameter,........... disses 16 0.65 Mimorilititoyy ciek-tickniendeSeiuae + 13 0.52 cig bb risk. tis. 0% eal unde Salehe Au 44 0.18 Habitat —Prome : rare. Of this unquestionably distinct species but 3 or 4 specimens were found by Mr. Fedden and myself. Both the external form and_plica- tion differ from those of all allied species. It is especially distinguish- ed by its rounded periphery, wider last whorl, and its irregular non-decussated sculpture externally, and internally by the double parietal lamina. Section ? 15. H. potypLeuris, n. sp. Shell openly umbilicated, trochiform, rather solid, white, (probably horny in living specimens,) obliquely and closely costulated. Spire conoid; apex rather obtuse; suture impressed. Whorls 6, convex, slowly increasing ; the last not descending, surrounded by a raised *thread-like keel, convex beneath, and somewhat sinuously radiately costulated around the deep and pervious umbilicus. Aperture oblique, 1865. ] Contributions to Indian Malacology. 17 roundly lunate, almost circular; peristome thin; margins distant, columellar slightly expanded. Millem. inch. Major diameter,........... SENS 4 0.16 Mimor ditto, ....ccsccsecsessesees 3200 an? OMG J Sun" | 22 gn 3 0.12 Habitat—Arakan hills: rare. A prettily marked little species near H.. Bascauda, Bens., from which it is distinguished by its finer and closer sculpture, more open umbilicus, and less conical spire. It is very probably a Nanina, but the animal was not met with. f Genus BULIMUS. 16. B. scropicunatus, n. sp. Shell subobtectly perforated, turritedly ovate, thin, horny, yellowish white, marked with vertical, subarcuate, rather irregular, closely set, raised lines. Spire turrited, apex obtuse, suture simple, impressed. Whorls 6, convex, the last rounded beneath. Aperture vertical, truncately ovate: peristome simple, thin; right margin considerably curved forwards ; columellar vertical, curving to the left near the base, frequently straight, rather broadly reflexed. Millem. inch. LAD Tai eg cay MED Coan iN ee aE iT 0.28 ID RPAMCE EES 25 25,095 inacledsiesiea 3s 0.14 Length of aperture, :2.......0.5 34 0.14 Habitat—Pegu, west of the Trawady. The nearest ally of this species is its congener B. putus, Bens., which inhabits the same localities, and differs in its greater tumidity and less marked sculpture. There is, however, much variation in the first named character, and despite the great difference between the two forms in general, there is some appearance of a passage. T'wo speci- mens of B. putus which I possess, measuring respectively 7 and 8} millem. in length, are both 5 millem. in diameter. Both these species shew a tendency to a passage to Sprraais. 17. 3B. puicrrer, n. sp. Shell obtectly perforated, ovately conical, rather thin, horny, finely striated. Spire conical, apex obtuse ; suture marginate, scarcely Vd. 78 Contributions to Indian Malacology. [No. 2, impressed. Whorls 5, planulately convex above, the last longer than the spire, somewhat tumid, rounded at the base. Aperture vertical, truncately oval, subpyriform; peristome simple ; right margin cutved forwards ; columellar callous, subvertical, slightly curved, rather broadly reflexed ; margins united by a callus bearing a small re-entering lamella about the centre. Millem. inch. Hengiihy eegihs st eevercaccanioas 9 0.36 Diameterncd case, fis o2cilse 5d 0.22 Aperture 5 millem. high, 24 broad. Habitat—Thayet Myo, Pegu: rare. A more tumid shell than B. putus, Bens., and easily distinguished from all other Indian and Burmese forms of the genus by the re-enter- ing parietal plait. Genus SPIRAXIS. 18. 8S. PUSILLA, n. sp. Shell imperforate, ovate, thin, horny, yellowish white, costulately striated. Spire conically pyramidal ; sides straight ; apex rather acute ; suture impressed. Whorls 5, convex; the last longer than the spire (ratio = 4 : 3) and rounded beneath. Aperture rather oblique, subpy- riform ; peristome simple, acute, much curved forwards on the right margin ; columella scarcely twisted, reflexed, appressed on the whorl. Millem. inch. engine sem ccnces seers Bence 6 0.24 DIDMEChEU eae eeasunenaeceen eae 33 0.14 Length of aperture, ............ 3s 0.14 Habitat—Prome district, Pegu : rare. I am not quite sure if all of the few specimens I possess of this peculiar small form came from Akoutoung, or whether some may not be from Thayet Myo. The shell resembles young specimens of Bulimus putus, Bens., so closely, that it can only be distinguished by the absence of any perforation. Genus ACHATINA. 19. A. Prevnnsis, n. sp. ' Shell oblong ovate, rather solid, dark reddish brown, horny, marked with distinct and regular impressed lines. Spire convexly conical ; 1865.] Contributions to Indian Malacology. 79 apex obtuse; suture impressed, subcrenulate. Whorls 63, slightly convex ; the last ascending a little towards the mouth, and exceeding 4 of the shell in length. Aperture vertical, truncately semicircular ; peristome obtuse, slightly thickened; margins joined by a callus; columella very much curved, projecting forwards at the base,. subver- tically truncated within the peristome. Millem. inch, PDair es: SIE rae a tase ij 0.28 Jo STG ya a 34 0.14 Length of aperture, ........ te 2? 0.11 Habitat—Ivawady valley, Pegu : common. A pretty little species, darker in colour than any of its allies, except: perhaps A. gemma, Bens., and easily distinguished from all, by the columella being more arcuate, also by its more acuminate spire and blunter apex, and its much stronger sculpture. 20.. A. PERTENUIS, n.. spi Shell very slender, turrited, thin, light horny,. polished, closely, minutely, and rather wregularly striated. Spire subulate, somewhat. acuminate towards the blunt.apex; suture impressed, subcrenulate. Whorls 11—12, convex, the last about + the length of the spire. Aperture oblique, ovately pyriform, peristome thin, margins united by a thin callus, columella moderately curved, obliquely truncated, Millem. inch. 10 1) ee Rep aA 20 0.8 PPA CREE 2 5. 12eIo G8) wstiecs - 43 0.18: Length of aperture, ........... - 4. 0.16 Habitat—Tongoop, Arakan.. Var major, length 2634 millem. ; diameter 6; length of aperture 6. Oi another specimen ; length 23 millem.; diameter 53; length of aper- ture 5+. Habitat—Pyema Khyoung, Bassein district, Pegu: A much more slender species than A. tenuispira, Bens., (a variety of. which also abounds in partsof Pegu,) though there are signs of a passage. The present. appears to replace A. tenwisprra in Arakan and Bassein. Mr. Benson, to whom I sent a specimen, observes that it is intermediate between. A. tenuispira and A. hastula, Bens. 80 Contributions to Indian Malacology. [No. 2, Genus SUCCINEA. 21. S. PLicatA, n. ‘sp. Shell depressly subovate, very thin, irregularly, obliquely and more or less coarsely plaited, pale amber in colour, horny. Spire short ; apex minutely papillar. Whorls 23; the last about 4 of the entire length. Aperture oblique, curved backwards at the base, nearly oval, openly angulate above; peristome simple ; columellar margin regularly bow-shaped ; right margin rather straighter. Millem. inch. MICH OTR eA eens 17 0.68 MDE LED eee ected och 94 0.38 Height, when laid upon the mouth, 6 millem. Aperture 14 millem. long, 8 broad. Habitat coarsely sculptured, occurred also south of Bassein in Pegu. Tongoop, Arakan: one or two specimens, rather less This species approaches S. semiserica, Gould, but is distinguished from that and from all other Indian species by its coarse sculpture. It has also a larger spire than S. semzserica. It is not common : indeed species of the genus Succinea are generally but very locally distributed in India and Burma. Genus CLAUSILIA. 22. (C. FUSIFORMIS, n. sp. Shell not rimate, fusiform, horny, thin, white; obliquely, very closely and finely costulately striated throughout... Spire diminishing slowly at first above the middle, then rapidly attenuate towards the acute apex ; suture simple, scarcely impressed, deeper towards the apex. Whorls 9, convex above, flattened below, the last very little narrower than the penultimate. Aperture semioval, (nearly semicircular) ; upper parietal plait very fine; internal palatal teeth 7, the uppermost by far the longest. Peristome thin, expanded, not continuous, the margins being distant, and united by a thin callus ; columellar margin straight and very long posteriorly. Millem. inch. Vieng thy sstacccdtnndnsbiaapeeccpae 23 0.92 Diametetyesae) doceed eee ae aa) 0.24 Habitat—Arakan hills, west of Henzada. Very rare. 1865.] Contributions to Indian Malacology. 81 But a solitary specimen was met with belonging to this form, which is more tumid in the centre than any of its allies, C. imsignis, Gould, &e. The non-continuity of the peristome may be due to immaturity in the specimen found. The shape of the mouth may also possibly be slightly modified in older examples, but the general form doubtless remains the same, and is alone sufficient to distinguish the species. A solitary specimen of another new form, much smaller than the above, being only 17 millem. long, occurred at Moditoung Tsekan, on the road from Prome to Tongoop. It is unfortunately bleached and worn, though perfect. Genus STREPTAXIS. 23. S. Burmanica, n. sp. Shell ovately subglobose, umbilicated, thin, horny, white, marked throughout with fine and closely set sinuate costulation. Spire convex; sutures scarcely impressed. Whorls 6, the last 2 widely excentric, rounded at the periphery ; the penultimate broader than the last whorl; last flattened beneath, and angulately compressed around the umbilicus. Aperture oblique, irregularly semioval, with a single re-entering lamellar parietal ; peristome white, thin, expanded through- out, deeply sinuate above, at the junction with the penultimate whorl, compressed and curved forwards on the upper right margin, and some- times furnished with a very small internal tooth-like callous projection ; the two margins subparallel, distant, united by a thin callus. Millem. inch. Major diameters... 0.0... 2 o0de 10 0.4 Minter dkboy 2 2ss2aep Ile, 7 0.28 1S 013152 eee SE Ee SEE 6 0.24 Habitat—Tongoop, Arakan. This is a very near ally of the Molmein S. Petitz, Gould, but it is distinguished from that shell and from S. exacuta, Gould, by the rounded periphery and more globose form. It is larger and less slender than S$. Andamanica, Bens., and is distinguished from all the above species, and also from the Nilgiri S. Perrotteti, by the greater size of the penultimate whorl in comparison with that of the antepenul- timate, a character to which my attention was called by Mr. Benson. _In Dr. Gould’s original description (an imperfect one) of S. Petitc, 82 Contributions to Indian Malacology. [No. 2, as republished in Otia Conchologica, p. 183, no mention is made of the angulation of the periphery, which, however, is referred to by Pieiffer, (Mon. Helic. I. 8). The character is certainly variable: in specimens in my own collection there is a considerable difference. Orprer,—PROSOBRANCHIATA. Family Cyclophoride. Genus CYCLOPHORUS. 24. C. (Lagocheilus) tuvorinus. Shell narrowly umbilicated, conically turbinate, thin, dark horny, and ornamented throughout with oblique striz and with raised spiral lines, closer together at the periphery and within the umbilicus than elsewhere. Spire conical ; apex rather acute. Whorls 53, rounded ; the last cylindrical, not descending. Aperture oblique, subcircular, angulate above ; peristome simple, thickened, subexpanded, incised at the upper angle; columellar margin curved backwards. Operculum horny, greyish white, multispiral. Millem. inch. Major diameter, ) (si secacsie-tsin0 4 0.16 Minor ditto, ..... aol Stetaenanen Ate 34 0.14 PS RAS ari I hols ee hia ciel etodatha aeive ale 4 0.16 Habitat—Akoutoung, Pegu. This form is allied to Cyclophorus scissimargo, Bens., and C. tomo- trema, Bens., forming with them the group for which Mr. Theobald has proposed the name of Lagocheilus. 'There appears good reason for associating these shells as a distinct subgenus, which perhaps repre- sents, in Burma, the group of Cyclophort comprising C. halophilus and its allies in Southern India and Ceylon. The present species is smaller and higher in the spire than either of the others. The animal of (. leporinus is short, dark in colour, with small black tentacles, and resembles ordinary Cyclophort in most characters. The only specimen obtained living and examined, possessed, however, the peculiarity of a groove down the middle of the caudal portion of the foot above. The peristome is simple in the only perfect adult specimen which I possess, but ina broken barely adult shell, there is a rudimentary duplication. The two lips are probably united in the full grown shell. 1865.] Contributions to Indian Malacology. 83 I also met with a shell apparently belonging to this species, but not full grown, at Pyema Khyoung, south of Bassein. An immature specimen of probably a 4th species of Lagochezlus, with very fine and rather close equidistant spiral sculpture, was found by me in the neighbourhood of Ava. Gents PTEROCYCLOS. 25. Pr. Feppeni, n. sp. Shell widely umbilicated, convexly depressed, smooth, finely striated rather thin, elegantly marked with alternating transverse zigzag stripes of white and chesnut, and with a moderately broad submedian band of darker colour. Spire nearly flat; apex but very slightly protruded ; suture deep. Whorls 42, convex ; the last rounded, descending towards the mouth. Aperture circular, slightly oblique ; peristome double; the two portions separated by a shallow groove, the inner cut away into a moderate sinus above, and the outer turned up into a small vertical wing, free from the penultimate whorl. Operculum concave within, the centre flat ; flatly concave without, with lamellar free edges to the whorls, thickest at the circumference. Millem. inch. Major diameter,........ sete cay 3 11 0.44 IVENTLOT GELO} hese, ccpenslee dis aonss 9 0.36 Js STE Se ee 8 ea ee 4 5 0.2 Habitat--Thayet Myo, Pegu—rare. A smaller and more convex shell than Pt. cetra, Bens. from Molmein. Itis one of the most beautifully marked species of the genus; it resembles Pt. pullatus, Bens., in form, and in the peculiar characters of the operculum, and equals the handsomest specimens of Pt. rupestris, Bens., in its colouring. Named after the discoverer, Mr. Fedden, of the Geological Survey. Gents ALYC AUS. 26. A. POLITUS, n- sp. Shell moderately umbilicated, turbinately depressed, smooth, polish- ed, shining, amber-coloured. Spire depressly conoidal ; suture deep ; apex obtuse, rather redder than the remainder of the shell. Whorls 3g, convex; the last round, scarcely descending towards the mouth, very little swollen at the side, and ornamented on the inflated portion 84 Contributions to Indian Malacology. [No. 2, for a short distance with close fine costulation, which extends beneath to the umbilicus and renders the shell opaque in that spot. Constric- tion long, smooth, swelling considerably in front towards the mouth. Sutural tube short, about + to 4 of the periphery of the penultimate whorl. Aperture oblique, circular, deeply sinuate at the junction with the penultimate whorl, and at the lower right margin; peristome double, the imner lip projecting and continuous, outer lip retrorelict. Operculum horny, multispiral, externally concave. Millem. inch. Mayor diameters sce. se /awee c's «se 3 0.12 W/E eT eye (eel FORMS OR See SOR REMoR ABE 24 0.09 LASTS Sa eR Riana ene 1i 0.05 Habitat—Phoung do, near Cape Negrais, Arakan. Very near A. humilis, W. Blanf., from Pegu, but distinguished by its lower spire, wider umbilicus, more sinuous mouth, and especially by its high polish, in which it is only equalled by A. nitidus, W. Blanf. 27. A. GLABER, n, sp. Shell broadly umbilicated, conoidly depressed, solid, reddish white, the upper whorls darker, rather dull in lustre, smooth, except at the swollen portion of the last whorl, which is very finely and closely costulated. Spire depressly conoid; apex rather obtuse; suture im- pressed. Whorls 4, convex, the last obsoletely subangulate at the periphery, moderately swollen at the side, then constricted, descending a little near the mouth. Constriction of moderate length, smooth, slightly swollen in the middle. Sutural tube of moderate length, Aperture diagonal, circular ; peristome more or less distinctly duplex, thickened, moderately expanded. Operculum dark coloured, horny, externally concave, internally convex, with a prominent central nucleus. Millem. inch, Major mMameters os.) .cecceeues ; (e 0.30 Mimor auto, Suc ac cserseneee 6 (0.24 HAIG carer a eereckewae LP ELL se 4h 0.18 Habitat This species closely resembles A. Ingranu, W. Blanf., for which T Akyak, Arakan; the hills south of the harbour. for some time mistook it, but it is distinguished by the absence of any- sculpture on the upper whorls, and also by the more oblique mouth, 1865. ] Contributions to Indian Malacology. 85 Genus DIPLOMMATINA. 28. D. NANA, n. sp. Shell not rimate, dextrorse, subovate, rather solid, amber-coloured, very finely and closely filiformly costulated on the lower whorls, less closely on the upper, or, frequently, subdistantly costulated through- out. Spire conical, with sides scarcely convex above; apex rather obtuse, sometimes reddish, suture impressed. Whorls 6—6, rounded, antepenultimate the largest, the last rising considerably upon the penultimate. Aperture vertical, ear-shaped, nearly circular, columellar margin straight for a short distance and vertical, with an internal tooth. Peristome double, both portions expanded and appressed, the inner forming a thin callus upon the penultimate whorl. Operculum ? Millem. inch. 1 E12 pe ee ee 24 0.09 LTTE ge Belem si a pk Aa Ll 0.04 Aperture with peristome about 2 millem. in diameter. Habitat—Akoutoung, Thondoung and Yenandoung in Henzada district, Pegu. . This species approaches D. polypleuris, Bens., more nearly than any other. It is distinguished by its more regularly ovate form, blunter apex, less swollen penultimate whorl, and more marked and distant sculpture. The latter character, however, varies. The specimens from Thondoung, a hill about 20 miles south of Akoutoung, being either closely costulate throughout, or subdistantly sculptured above, closely below; while in Akoutoung specimens, the costulation is subdistant throughout. As, however, I can trace no other distinec- tion between the shells, and the costulation varies in different indivi- duals from each place, I do not think there is any specific distinction. A still more minute species than the present exists in Pegu, and I found two dead specimens at the base of the Arakan hills in the Henzada district. As these specimens were not very well preserved, I abstain from describing them for the present. Family Helicimde. Genus HELICINA. 29. H. ARAKANENSIS. Shell depressly turbinate, sublenticular, rather thin, obliquely striated above, radiately and very minutely beneath, polished, flesh-coloured, 12 : 86 Contributions to Indian Malacology. [No. 2, with a darker red band in the centre of the whorls above, and another on the last whorl, just below the periphery ; apex yellow. Spire con- vexly conoid ; apex acute. Whorls 4, the last compressed and sharply keeled, moderately convex at the base, furnished with a polished sub- granulate central callus; columella very short. Aperture diagonal, triangular; peristome white, slightly expanded. Operculum light grey, shelly. Millem. inch. Mayormiamebert iiss. 6 0.24 “ALTTEVC RS 26)5 50 Se IN Ae 5 0.2 BNGEGIS PE Cts GEL SHS ORE CGN 33 0.15 Habitat—Ramri Island, coast of Arakan. Rare. A smaller variety, measuring—major diameter 5, minor 44, axis 3 millem., was abundant in the southern portion of the Bassein district. Near H. Mergwiensis, Pir. and H. Andamanica, Bens., but smaller than either. It is mainly distinguished from the former by the absence of the close spiral striation, so marked in that species, and from the latter by different colouring, higher spire and closer sculpture. — The preceding pages contain descriptions of the greater portion of the previously unpublished species of land shells in my collections from Ava, Pegu, and Arakan; I have still a few remaining, the dis- tinctness of which is probable, but they belong, for the most part, to critical groups, and require comparison with the original types of species, described by Mr. Benson and others. The following addition- al notes, on the distribution of previously described species, may serve to supplement the papers on the subject, by Mr. Theobald, in Jour. As. Soc, Bengal, Vol. XXVI. p. 245, and Vol. XXVII. p. 313. Nanina. Nanina petasus, Bens., is common about Thayet Myo and in the Arakan hills. My largest specimen measures 12 millemetres by 11 in its two diameters. A smaller, closely allied shell, measuring 8 by 7 millem., I was inclined to refer to Mr. Benson’s Helix aspides, on account of the arcuate and labiate basal margin of the aperture, but [ learn from the describer that it presents differences, although not sufficient to prove it a distinct species. A third still smaller form, with the thickening and curvature of the peristome exaggerated, and 1865. ] Contributions to Indian Malacology. 87 a somewhat flatter spire, measures only 5 to 54 millem. in its largest diameter, and may be a distinct shell. It, also, is from the Arakan hills. Nanina honesta, Gould, originally described from Tavoy, is found throughout western Pegu and Arakan, as well as at Molmein, where it was collected by Mr. Theobald. Dr. Gould’s description is very imperfect ; he does not even note the great obliquity of the mouth, which is the most striking character of the species. In the Arakan hills near Prome, and about Thayet Myo, a larger variety occurs, in which the angulation of the periphery entirely disappears in the adult, although the other characters are the same. The sutural margination is sometimes, though rarely, obsolete. Large specimens measure 14 by 113 millem., and about 7 in height. NV. levicula, Bens., also first found by Mr. Theobald in the Tenas- serim provinces, is very common about Thayet Myo, Prome, and Akoutoung, and occurs also as far south as the Bassein district. It is frequently whitish in colour. It is allied to N. honesta, but easily distinguished, besides by its smaller size, by the fewer whorls and their more rapid rate of increase, and also by the total absence of sculpture, - There is much variation in size : my largest specimen measures 84 and 7 millem. in its two diameters. The animal has a very small lobe above the mucus pore in the tail, which is truncated. The mantle is rather large. A single specimen of a shell, apparently identical, was found by me, some years ago, near Balasore in Orissa. NV. teatvina was evidently described by Mr. Benson, Gn the Annals and Mag. Nat. Hist. 1856, Ser. 2, Vol. XVIII. p. 252,) from an immature specimen. When adult, the peristome is white and slightly thickened within, and the body whorl internally of a milky white colour. This handsome species is found west of the Lrawady, from Thayet Myo to Bassein, and varies considerably in size, in the height of the spire, and in the degree of angulation above the periphery, The greatest change takes place in the latter character ; specimens from the district of Bassein being sharply angled, and even subcarinate, the angulation diminishing, however, close to the aperture; while, in specimens from Thayet Myo and Prome, the periphery is round. In height of spire, the shell varies from depressed to subturbinate ; in two specimens before me, one has a major diameter of 30 millem., and height of 13; the other with a major diameter of only 27, measures 88 Contributions to Indian Malacology. [No. 2, 15 millem. in the axis, and this variation is seen in both rounded and subcarinate specimens. The largest specimen I possess, measures in its two diameters, 36 and 31 millemetres, and in height 18. N. pansa, Bens., was found near Akoutoung and Thayet Myo; and also, more abundantly, in the neighbourhood of Ava. N. (Lrochomorpha) attegia, Bens., abounds at Akoutoung below Prome. It is not common elsewhere, except about Prome, The animal has a mucus pore at the end of a truncated foot, and a lobe above, as in N, vitrinoides, Desh. A shell which Mr. Benson considers as probably identical with Helix diplodon, Bens., (a Khasi hill species) occurs rarely in the Arakan hills. It is a Nanina with a small lobe above the mucus pore near the end of the tail, which, however, is more flattened and less truncated than in species of the Trochomorpha section generally. No species of the Ariophanta section, so largely represented in India, has as yet been found in Pegu or Arakan ;* NV. retrorsa, Gould, being hitherto unknown N. or W. of Molmein. Macrochlamys and Trochomorpha (anless N, textrina and N, pansa belong rather to Hemiplecta than to the former,) comprise the great majority of the Nanine. The forms belonging to the first named section are so numerous, and distinguished by such minute differences, that their study is one of great difficulty. Helin, Amongst the true Helices in Northern Pegu, several forms assigned to the section Dorcasia, Gray, are conspicuous. They appear to re- present in Burma, H. fallaciosa, Fer., H. asperella, Pir., and their allies of the Indian peninsula, and they might all perhaps with greater correctness be classed together in the same section. Amongst these forms is H. similaris, Fer., of which H, scalpturita, Bens. and H. Zoroaster, Theobald, appear to be varieties. These shells oeeur in the drier portions of the Irawady valley, and are not found below Prome, but they extend northwards to beyond Ava. The variety named by Mr. Benson #. scalpturita sometimes wants the coloured * Nor is this section, so far as I know, represented in the Himalayas. N. Himolayana, Lea, being almost certainly N. interrwpta, Bens., and the assigned locality due to an error ; while H. cyclotrema, Bens., lately described from the hills N. of Tirhoot, is a sinistrorse member of the asperella group, and closely allied to that species, as may be seen from its expanded lip and granu- late surface, The animal is doubtless a true Heliw, and not a Nanina, 1865. ] Contributions to Indian Malacology. 89 bands, and passes into a shell closely resembling H. Peguensis, Bens., a more solid form, shells approaching which closely in every character except in being less solid, were found on the Shan hills, east of Ava, Mr. Benson considers these shells distinct from H. Peguensis, but there can be little doubt of their forming a link. The typical variety of H. scalpturita abounds near Mandélé. H. Zoroaster, Theobald, is a large H. similaris, and occurs abundantly at Thayet Myo and less so at Prome. 4H. bolus, Bens., abundant near Thayet Myo and Prome, is sometimes marked by a coloured band like that of H. similaris, and varies greatly in the height of the spire. The type is a well marked form, far more globose than the others, but yet it passes, by impercep- tible gradations, into simlaris. H. delibrata, Bens. is also allied to similaris although classed in a different section or subgenus by both Albers and Pfeiffer; it unites Dorcasia with the Trachea group, (Z. asperella and its allies). H. delibrata is not rare throughout Arakan; it occurs at Akyab, and in Pegu it is found at Akoutoung and other places; when fresh it has a subhispid epidermis, and fre- quently a rufous band above the periphery, like s¢mlaris and asperella. Somewhat allied to the semilaris group, but yet forming a distinct and well marked section, are H. tapeina, Bens., and its allies H. rota- tora, v. d. Busch, H. Oldhami, Bens., and H. Huttoni, Pir. To these, two other species have been added by Mr. Theobald, viz. : A. Phayret and H. Akoutongensis. The type appears almost peculiar to the Malay countries, one species only, H. Hutton:, occurring upon the Himalayas and other Indian mountains, and none in the plains of India. H. Oldham, Bens. is a well marked and easily distinguished form, with almost flat spire, very wide umbilicus, and the last whorl sub- angulate above the periphery and swollen beneath. The epidermis, when in good order, is subhispid, as in several other species of the group. This form was first found by Dr. Oldham at Mya Leit Doung, a few miles south-east of Ava, and I afterwards met with it in the Arakan hills, on the road between Prome and Tongoop. The other species pass into each other in the most perplexing manner, and there scarcely appears any choice between increasing their number indefinitely, and classing all together as varieties of one species. The little form known as H. Huttoni, Pir., is perhaps more easily distinguished than most of the others, as it is singularly constant in 90 Contributions to Indian Malacology. [No. 2, form. It is usually smaller than tapevna or rotatoria, and may gener- ally be recognised by its blunt periphery and the convexity both of the spire and base. Still, forms of H. tapeina approach it so closely that they may be said to pass into it. I found specimens of H. Huttoni in only one spot in Burma, viz. on Puppa hill, an isolated peak, nearly 5,000 feet high, in Upper Burma. The occurrence of a Hima- layan shell which is found as high as 6,000 and 7,000 feet in Sikkim, upon this solitary hill, where it is accompanied by peculiar species, as Alyceus Vulcani, W. Blanf. and Diplommatina Puppensis, W. Blant., and with a flora comprising plants, such as Pteris agwilina, belonging to a temperate climate, is very remarkable; especially as the same species was found by myself on the Nilgiri hills of Southern India, at an elevation of above 6,000 feet, and by Mr. F. Layard on the moun- tains of Ceylon. It is found both in the eastern and western Hima. layas, and has probably once enjoyed a far more general range in India than at present. Its occurrence, with go little variation, in isolated situations, is in favour of its being a distinct and natural species, a rank to which, morphologically considered, its claims are small. At Mya Leit Doung, the high limestone peak 15 miles south-east of Amarapoora, already referred to, and the locality whence Cyclopho- rus cryptomphalus, Bens., C. hispidulus, W. Blanf., Diplommatina exilis, W. Blant., Georissa frustrillum, Bens. sp., Hypselostoma Benso- nianum, W. Blanf., Helix perarcta, W. Blanf., and other peculiar species have been obtained, I found Mr. Theobald’s Heliw Phayrez, which appears to have some claims to be considered a distinct species. Mr. Theobald’s description (J. A. 8. B., 1859, Vol. XXVIII. p. 306) is very imperfect, and the following may serve to give a better idea of the shell. H. Puayret, Theobald. Shell moderately umbilicated, orbiculately conoid, rather solid, white, with a horny shining epidermis ; obliquely, coarsely and flex= uously plicately striated beneath the epidermis, bluntly angulate at the periphery. Spire depressly conoid; apex obtuse ; suture scarcely impressed. Whorls 6, slightly convex, slowly increasing; the last descending towards the aperture, where the angulation of the peri- phery dies out; convex beneath, compressed around the deep umbili- cus, which exposes all the whorls. Aperture subcircularly lunate, diagonal; peristome white, slightly expanded throughout; margins 1865. Contributions to Indian Malacology. Of WK approaching each other, and united by a callus. Major diameter 18, minor 153, axis 8 millemetres. 6 Habitat—Mya Leit Doung. Ava. This differs from all allied forms in its much coarser flexuous sculp- ture, and from most of them by its blunt angulation at the periphery. Tt is also, so far as I know, the largest form, belonging to this group, which oceurs in Burma.* H. tapeina is said by Mr. Benson to be distinguished from rotatoria, amongst other characters, by the greater regularity of the sculpture in the former shell, which contrasts with the irregularly flexuous stria- tion of the latter. I have never seen a typical specimen of H. rota- toria, which was originally described from Java, but Mr. Benson has identified with it a shell which abounds at Thayet Myo, Prome and Akoutoung, and a variety of which, with a flat spire, Mr. Theobald has called H. Akoutongensis. Of H, tapeina I possess specimens collected by Mr. Theobald at the original locality, the Khasi hills. These have a slightly more regular sculpture, an angulate periphery instead of the sharp compressed keel of the Pegu form, and a rounder mouth, but the spire is sometimes higher, sometimes not, and I can see no distinction in the umbilicus. In all the distinctive characters, varieties shewing gradation, occur in Burma. Leaving the question of specific distinction, the distribution of varieties of these shells in the Ivawady valley, so far as I have searched, is the following. On the Shan hills, east of the valley in which lie Mandélé, the pre- sent capital of Ava, and the older capitals, Amarapoora and Ava itself, I found a lenticular sharply keeled form, less swollen beneath, and, in general, higher in the spire than the Akoutoung form of rotatoria, with the sides of the spire straight, not convex. The epidermis, when in good order, and especially in young specimens, is hispid ; the sculpture rather variable, but flexuous. ‘This latter is also the case with the Akoutoung and Thayet Myo form of rotatoria. *Tn a letter received since the above was written, Mr. Benson informs me that H. Phayrez only differs from his type of H. tapeiina in its coarser sculpture. My specimens of the latter shell have a more angulate periphery. + In Pfeiffer’s Monogr. Helic. Viv., however, H. tapeina (Vol. IIT. p. 254) is said to be “ Subtiliter granulato-striata,’ while H. rotatoria (Vol. I. p. 208) is described simply as “ oblique striata.’ The former is said to differ from the latter in sculpture, higher spire, narrower umbilicus and rounder aperture, 92 Contributions to Indian Malacology. [No. 2, In the Tsagain hills, west of the Irawady, opposite Ava, I obtained two forms, one bluntly angled at the periphery and approaching 4. Oldhami, in which however the spire is lower and the umbilicus more open. The sculpture, form of the whorls and of the mouth, (which is rounded with connivent margins and expanded throughout,) and the angulation of the periphery, are precisely similar to the same characters in my specimens of H. tapeina: the umbilicus is slightly broader, and the spire lower, sometimes as flat as in Akoutongensis. The dimensions are 15} and 14 millem. in the two diameters; height 6. The other form is extremely sharply keeled and lenticular, with an angulate lunate mouth, and a narrower umbilicus than the last, or even than the Cherra tapeina, but it has the same simple sculpture, differmg in this from the Shan hills form, which it otherwise resembles. It mea- sures 174 millem. by 16, and 9 in height. The next locality to the south in the Irawady valley at which I obtained forms of this type was at Thayet Myo. I have already re- ferred to the variety prevailing there, as well as at Prome and Akou- toung. Asa rule, the shells are small, thin, horny, and more or less hispid, very variable in the height of the spire, sharply keeled and with very fine, flexous striation. The major diameter is about 10 to 12 millem. on an average. At Henzada, and in its neighbourhood, another form prevails. It is also met with at Akoutoung, but is rare, and it passes into the flatter form there prevailing. The Henzada shell has a much higher spire with very convex sides, and is, in fact, subcampanulate, the base, on the other hand, being flattened. It is sharply keeled, quite as sharply as the Akoutoung form, but it has the sculpture rather of H. tapeina than of rotatoria, and the epidermis, instead of being sub- hispid as in the latter shell, is merely granulate. A form, interme- diate both in height of spire and in sculpture between the Henzada and Akoutoung varieties, was found in the Arakan hills, between Prome and Tongoop. In the Bassein district, all the shells of this type are much the same. They have a sharp keel, moderate spire with convex sides, obtuse apex, and but little convexity beneath. They possess a granu- late epidermis and the sculpture of H. tapeina. The specimens with the highest spires, from Henzada, approximate 1865.] Contributions to Indian Malacology. 93 in form to the Cambodia H. repanda, Pir., and may perhaps be identical. Tt will be seen how variable the forms are. The spire varies from flat to almost bell-shaped, the periphery from sharply keeled to angu- late, the whorls from subconvex to flat or nearly so; nor is there great- er constancy in the form of the mouth, the sculpture, the epidermis, or the breadth of the umbilicus. Distinct as many of the varieties appear to be, they all pass gradually into each other, and with the exceptions already described, I believe all the forms are most safely classed as varieties of one species. Whether this should be called rotatoria or tapeina is difficult to say, without more precise acquaint- ance with the types of those shells.* Not far from the tapeina group must be classed H. castra, Bens., which, despite its thin horny shell and sharp peristome, is not a Nanina, but a true Helix. It occurs throughout the Arakan hills, wherever I have searched, but is everywhere scarce. It has the widest range in the Indian area of any known Helix, being found in the Himalayas, in Orissa, in Ceylon, and throughout Burma as far south as the Tenasserim provinces. | Hi. climacterica, Bens. is very probably a Nanina, but I have not had an opportunity of observing the animal. The shell was found by Captain Ingram on the road from Prome to Tongoop, and I found it again in the hills, at the southern extremity of the Henzada district, and in Bassein. It occurred also in Long island, in the Bassein river. It is much smaller in general than the typical Khasi hill shell; I possess specimens, apparently fully grown, but measuring only 13 or 14 millemetres in their major diameter. H., hariola, Bens. is a true Helix, and is found chiefly on trees near Thayet Myo and Prome. It isa rare shell. Near Ava it is replaced by a large sharply carinate form, which I found abundant at Thinga- dan, on the Irawady, about 80 miles north of Mandélé. This shell so closely resembles H. capitiwm, Bens., that I am much disposed to consider them identical, a view in which Mr. Benson, however, does not agree. At Puppa hill, near Pagan, already referred to as the * Mr. Benson, to whom I sent specimens, considers all the forms above men- tioned to be varieties of rotatoria, but some, especially that from the Tsagain hills, appear to me to be at least as nearly allied to tapeina. 13 94 Contributions to Indian Malacology. [No. 2, locality where H. Huttoni, Pir., is found, I met with an intermediate variety, between the carinate form and the typical H. hariola. The Plectopylis group is represented near Ava by H. perarcta, de- scribed above, and further south by H. leiophis, Bens. This shell occurs near Thayet Myo, but I found it abundantly only at Akou- toung. Another form, which may be a small variety of lecophas, but which shews some differences in the internal plication, also occurs near Thayet Myo. At Prome, close to the Pagoda, I found H. Fed- deni, (described above) which, however, appeared very rare, as I only obtained two perfect specimens, despite much search. 20 or 30 miles south of Akoutoung, I found H. Karenorwm in abundance, and 2 or 3 specimens of the large variety of the same shell still further south in the Arakan hills, nearly due west of Henzada. Elsewhere in the Henzada district and throughout Bassein, no species of the Burmese form of Plectopylis was met with, but the Himalayan and Khasi H. plectostoma, Bens. abounded south of the town of Bassein in sever- al places, Pyema Khyoung, Long Island, &. It was also found by Captain Ingram in Arakan, near Tongoop. Bulimus. A variety of the sinistrorse Bulimus Sinensis, Bens., measuring 26 millem. in length and 15 in diameter, occurs near Prome. It has generally two dark stripes round the body whorl, but some specimens have other stripes, usually 3, above the periphery. Occasional speci- mens were met with further south. At Tongoop in Arakan, I found a much smaller variety, measuring only 20 millem. in length, and 124 in diameter. At Akyab I also found this small variety ; some shells being entirely yellow without any stripes, like Mr. Theobald’s Mergui specimens, B. putus, Bens. is rather common at Akoutoung, less so at Thayet Myo, and scarce to the south : I found it, however, occasionally, in the Bassein district. B. pullus, Gray, occurs near Ava; but not, so far as I am aware, in Pegu. Specimens of B. cenopictus, Hutton, were also met with in Upper Burma. JB. gracilis, Hutton, occurs throughout Burma appa- rently. I have found a rather dwarf variety in Ava, Pegu and Arakan, and have received it from Molmein. 1865.] Contributions to Indian Malacology, 95 Achatina. Achatina tenwispira, Bens., of small size, is common at Akoutoung and further south. A small variety of A. crassilabris, Bens., occurs in Arakan, and another form, perhaps distinct, but closely allied, was found in the Shan hills near Ava. The species of Achatina do not appear to be numerous in Burma; they attain their maximum in the Indian area in the Western Ghats, and the hills of South India and Ceylon, and their numbers diminish to the eastward. Vitrina, Vitrina prestans, Gould, differing in no respect from the Molmein shell, and V. gigas, Bens., equally identical with the Khasi form, are both met with throughout the Arakan hills, though sparingly. A smaller species, which I had looked upon as the young of V. gagas, has been correctly separated by Mr. Theobald, and will doubtless be described by him. Ennea and Pupa. Ennea bicolor was met with near Tongoop in Arakan, and at one or two places in Pegu. Asin many other localities throughout its wide range, it is a scarce shell. Pupa Avanica, Bens. occurs near Ava. I found it abundantly on a small hill, a few miles north of Mandélé. Streptaxis. Besides the species above described from Arakan, a smaller form occurs in Pegu, which I consider a variety of S. Andamanica, Bens., the only difference I can detect being in the sculpture, which is some- what finer in the Pegu shells. Hypselostoma. I have nothing to add to the particulars of the distribution of the two species of Hypselostoma beyond those given in a preceding number of these contributions, CYcLOSTOMACEA, Cyclophorus. In the Shan hills east of Ava, I found two forms of large turbinate Cyclophort, one apparently a variety of C. speciosus, Phil., the other so closely allied that I doubt if it is wise to describe it as distinct. C’, speciosus does not appear to occur in Northern Pegu, but I found 96 Contributions to Indian Malacology. [No. 2, it at Rangoon, close to the Pagoda, abundantly south of Bassein, and at Tongoop in Arakan. At Akyab I found some dead specimens, which may possibly belong to this species, but they are thinner, with a rather narrower umbilicus, and less broadly expanded peristome, and one specimen is subangulate at the periphery. In these characters they appear to be intermediate between the Burmese C. speciosus, Phil., and the Khasi hill C. Pearsonz, Bens. At the base of the Shan hills, and also at Mya Leit Doung, I found the small species referred by Mr. Benson to C. cornu venatorium, Sow. Some living specimens at the former locality shewed the operculum to be normal. At Mya Leit Doung occurs also C. eryptomphalus, Bens. of which I obtained fresh specimens, with the colour and epidermis perfect. When in this state, it is the handsomest of the Burmese Cyclophori, and equal in beauty of colourmg to C. Svamensis, Sow., the dark blackish brown colour of the upper surface of the shell contrasting finely with the inregular zigzag white lines. The mouth, in my specimens, shews no distinct duplication: it is much thickened and expanded, as in C. speciosus or C. Svamensis, C. fulguratus, Pir., I did not find further north than Puppa hill. At Thayet Myo and Prome it is very abundant, and it occurs more sparingly throughout the Prome and Henzada districts, together with C. Theobaldianus, Bens, and C. patens, W. Blanf. C fulguratus is a handsome shell, varying greatly in size, my largest specimens from Thondoung, south of Thayet Myo, measuring 38 millem. by 30, the smallest, a dwarf specimen, also from Thayet Myo, only 20 millem. by 15}. ; Mr. Theobald, in a paper published in this Journal for 1863, (XXXIII. p. 376,) classes my C. patens asa variety of C. fulguratus. The types of both species occur together at Thayet Myo, and are very distinct, C. patens having a broad, rather thin disk-like expanded peristome, while the lip of C. fulguratus is much thicker but only moderately expanded. C. patens also is much smoother. However, intermediate forms may possibly occur, as they do between many other Burmese species. ; At Tongoop in Arakan, and on Ramzri island, I found a variety of the large C. aurantiacus, Schum. It approaches C. Theobaldianus 1865.] Contributions to Indian Malacology. 97 Bens., but has flatter whorls, a sharper keel, a more acute apex, and rather less strongly marked sculpture. A small turbinate species of Cyclophorus, which I found at a con- siderable height on the Arakan hills between Prome and Tongoop, with a rounded periphery and very narrow umbilicus, requires compa- rison with (@. scwrra, Bens. Another form, with a subangulate peri- phery, was met with in Bassein district, and a third, rather larger, but otherwise identical, in Ramri island. All of these may be varieties of the same shell. All possess a very narrow umbilicus, a thin white expanded lip, and minute sculpture. None of the small discoid Cyclophori, so far as I am aware, occur in Pegu. C. hispidulus, W. Blanf., I described in a previous paper as occurring at Mya Leit Doung, Ava. C. calyx, Bens. is stated by Mr. Theobald to occur at Akoutoung, Pegu, and that locality has been quoted for it by Mr. Benson in describing the shell, and repeated by Pieiffer in Suppl. Mon. Pneum. p. 56. I think some mistake must have been made by Mr. Theobald in arranging and labelling the very extensive collections which he made in 1854-55, for the shell abounds in Molmein, while, although I have repeatedly searched all round the Akoutoung hills, I have not met with it. Leptopoma. In a previous paper (J. A. S. B. for 1862) reference was made to the occurrence of the Tenasserim L. aspirans, Bens., in Arakan, near Tongoop, and in the Bassein district of Pegu. It was found in great abundance in Long Island in the Bassein river. I also found speci- mens close to Akyab, in the hills on the opposite (south) side of the harbour. Some of these last are rather larger than the typical form, and measure 14 by 103 millemetres in the two diameters and 12 in height ; they are also smoother, wanting the raised spiral lines, and the last whorl is rounded or subangulate near the mouth: but other specimens are scarcely distinguishable from typical shells from Tenas- serim, among which also some of the above characters, and especially the sculpture, are variable. Pterocyclos. Pt. pullatus, Bens., has only been found near Akoutoung. In Arakan, near Tongoop, and again at Akyab, I found a species closely allied to Pt. parvus, Pearson. The Akyab specimens possess their 98 Contributions to Indian Malacology. [No. 2, opercula, which is flat like that of Pt. pullatus, and not convex as in Pt. rupestris, &c. These shells also closely resemble a species collected by Mr. Theobald at Cherra Poonjee, and referred by Mr. Benson to Pt. Albersi, Pir., which has a convex operculum, and a peculiarly shaped wing. The specimens from Tongoop and its neighbourhood had a much thicker epidermis than those from Akyab, and were larger, but otherwise similar.* No form of Cyclotus is known from Burma. I have shewn, in a paper published in the Annals and Magazine of Natural History for June, 1864, that the Cyclophorus calyx group approaches very closely to the true Cycloti, and represents them; while the Cycloti of India (e. g. C. subdiscoideus, Sow.) are allied to Cyclostoma, haying the peculiar cleft foot and mode of reptation of that genus. I have pro- posed to place them in a new genus, Cyclotopsis. Alyceus. Much concerning the distribution of the numerous species of this genus has been communicated in previous papers. A brief recapitula- tion may be useful. A. Ave, W. Blanf., is the only form as yet found on the Shan hills, east of Ava. A. Vulcani, W. Blanf., occurs at Puppa hill, Pagan. About Thayet Myo, A. sculptilis, Bens., is abundant, especially on the hills a few miles south of the town, where also A. arnullatus, Bens., was found in very small numbers, its minute size doubtless rendering the search for it difficult. A few specimens of a small variety of A. wmbonalis, Bens., first appeared here. They have a “yetro-relict’’ outer peristome, and coarse sculpture on the upper whorls. The typical variety is rather common at Akoutoung, the original locality. I found this species again at one spot, a little north of Bassein, near the village of Kani. The older specimens obtained there, and others from the base of the Arakan hills, west of Prome, had the outer peristome retro-relict as in the Thayet Myo variety, a peculiarity I never observed in the typical Akoutoung form. % Since the above was written, I have heard from Mr. Benson, who has kind- ly compared the species with Pt. parvus. In the latter, the wing runs up the penultimate whorl, while the wing and sinus of the Akyab and Tongoop species resemble those of Pt. pullatus. In other respects the form resembles Pt. parvus. Tt may be distinguished as Pt. Arakanensis, n. sp. I have not specimens at hand, so cannot add a complete description. 1865. ] Contributions to Indian Malacology. 99 At Akoutoung I also found A. humilis, W. Blanf., and at the same place, at Thondoung and at Yenandoung, two hills about 20 miles further south, I found a variety of A. Ingrami, W. Blanf., rather larger than the type from Tongoop in Arakan, and measuring 7 millem. in the larger diameter. Another form of the same shell, with a less distinct subangulation of the periphery, and rather closer sculpture on the upper whorls, oceurred at Moditoung, on the Prome and Tongoop road, with A. graphicus, W. Blant, A. succineus, W. Blanf., neither of which has been found elsewhere, and one form of A. vestitus, W. Blanf. : A. nitidus, W. Blanf. and A. polygonoma, W. Blanf., were first found on the same road, but nearer to Tongoop. The latter I afterwards obtained in two or three places south of Bassein, the specimens being a little larger (6 and 5 millem. in their two diameters) than those first found. A. vestitus has only been found in the Arakan hills on the confines of the Henzada and Prome districts. Adding to these the two new species above described, A. politus from near Cape Negrais, and A. glaber from Akyab, we have 14 species described from Ava, Pegu, and Arakan, besides 3 more from Molmein and Tenasserim, altogether nearly half the known species of the genus. Pupina. A species of Pupina occurs at Thayet Myo, Prome, Akoutoung, &e., closely resembling P. artata, Bens. from Molmein, but rather stouter in form and with a somewhat thicker peristome, which is frequently but not always orange in colour, instead of white. These differences do not appear, however, to warrant specific distinction, especially as there is much variation in the form of typical specimens of P. artata. A variety from Ava is closer to the type. A small form, probably another variety, occurred upon the Arakan hills near Prome. It is only 4 millem. long, but the specimens are unfortunately not quite fresh. My own specimens of P. artata trom Molmein are but 6 millem. long. The operculum in fresh specimens is horny, not testaceous, the white appearance being produced by weathering, and I suspect the apparently paucispiral character to be due to the rapid increase of the interior whorls, which rest one upon the other, as in 100 Contributions to Indian Malacology. [No. 2, Cataulus. Near the}periphery, the whorls are more numerous, but their boundaries are indistinct. I have in this and other papers, already given all the details con- nected with the occurrence of the four species of Diplommatina as yet described from Burma. The only known Helicina from Northern Burma is also described above. Georissa. T have described (Ann. and Mag. Nat. Hist. for June 1864) as a distinct genus, under this name, the species of Burmese and Khasi shells referred to Hydrocena by Mr. Benson, both the animal and operculum differing from those in that genus. But one species is known to exist in Pegu, G. pyzis, Bens., and I have met with that in many places west of the Irawady, from Thayet Myo to south of Bassein. G. Frustrillum, Bens., I only met with at the original local- ity, Mya Leit Doung, Ava. Tt is evident that two very distinct zoological provinces exist in Burma, exclusive of Martaban and Tenasserim, which form a third, characterized by the appearance of several Malayan generic types, such as Raphaulus, Hybocystis and Rhiostoma, and others apparently pecu- liar, as Sophina. The two northern provinces are: 1st, Arakan, with the southern part of Pegu near the sea, enjoying a very humid climate. 2nd, Upper Burma, with, in many parts, a very dry climate. The boundary in the Irawady valley may be drawn roughly above Henzada, although species belonging to each fauna, as is usually the case, pass over the border. The first province, besides a considerable number of peculiar species, is especially characterized by forms common, on the one hand, to the Khasi hills, and even to the Hima- layas, and, on the other hand, to Tenasserim. Hxamples of the first are Helix plectostoma, Bens., H. delibrata, Bens., H. castra, Bens., &e. ; of the second, Cyclophorus awrantiacus, Schum., C. speciosus, Phil., Leptopoma aspirans, Bens., Nanina honesta, Gould, &e. In the Ava province, on the other hand, the forms which have also been found in India_are mostly inhabitants of the plains, such as Helia similaris, Fer., Bulimus pullus, Gray, and B. ceenopictus, Hutt. The genus Hypselostoma has as yet only been found within this province, or close to its borders. It is rich in species of Plectopylis, and in varieties or 1865.] Contributions to Indian Matacology. 101 allies of H. stmilaris. The Arakan Yoma north of Henzada separates the two provinces; the southern portion of the range, which is very low, rarely exceeding 1000 feet, is solely occupied by species belong- ing to the Arakan fauna. These provinces are also characterized by distinct forms of mammals and birds, and there is a great difference in their vegetation. In a list of Burmese shells, published by Mr. Theobald in J. A. S. B. for 1857, (Vol. XXVI. p. 251) occur the names of HI. petila, Bens., and H. mensula, Bens., from Thayet Myo, and H. precaria, Bens. from Tenasserim. These shells have never been described, and Mr. Theobald in this, as in other instances, has publish- ed lists of manuscript names communicated to him, some of which have subsequently proved to have been given in error. It is, I think, to be regretted, that in a recent paper J. A. 8. B. for 1863, Vol. XXXII. p. 374, Mr. Theobald has again included one of these aban- doned names, viz. H. petila, and he has also published the names of several of the species described above, and similarly communicated to him in manuscript. One of those thus published, Alyceus scepticus, has proved, on more careful comparison, and when additional speci- mens from other localities were procured, to be only a variety of A, Ingrami, and not a distinct species. Several of the names in Mr. Theobald’s paper are incorrectly given, e. g. Helix helicofera for Hi, helicifera, H. caussia for H. causia, H. pausa for H. pansa but these are probably errors of printing. The practice of including, amongst lists of species, manuscript names, without any reference to the fact of their being unpublished, and consequently of no authority, is much to be deprecated, as tending to confusion and the multiplication of synonyms.* Postscript —Since the above paper was penned, now nearly 6 months ago, I have received Mr. Theobald’s “ Notes on some Indian and Burmese Helicide, &c.” published in this Journal for last year, pp. * Besides the shells above mentioned in the Burmese list, the names of many other undescribed species occur in the paper, while many described species are omitted, 14 102 Contributions to Indian Malacology. [No. 2, 238, &e., which calls for a few remarks. Although I differ in many points from Mr, Theobald’s views as put forward in this paper and in the earlier one of 1863, especially those on the origin, migration, and distribution of specific forms, I see no object to be attained im answer- ing at length opinions long since refuted, as I believe, by far more competent authorities and far abler writers. The works of Hdward Forbes, Owen, Lyell and a host of others besides Darwin, will serve to shew the arguments relied upon by the great majority of hving natur- alists, to prove the doctrine of “ specific centres,” that is the theory that all members of the same species, whether existing or dead, have descended, not necessarily from one pair, but from one parent stock, living in one spot. To call this, however, the Darwinian theory, as Mr. Theobald appears to do. would be paralleled by calling the earth’s rotation round the sun the Newtonian theory. In each case the earlier theory is only a necessary step in the line of argument, and the hypothesis of the origin of species by means of Natural Selection is no more involved in the doctrine of specific centres, than was the theory of universal gravitation in that of the rotation of the planets around the sun. li I refer briefly to one remark of Mr. Theobald’s, (that im his first paper, J. A. 8. B. for 1863, Vol. XXXII. p. 376) it is because it appears to me the only argument of any importance which he has advanced in favour of his opinions. The question of the distribution of fresh water shells and especially of the bivalves, with their limited powers of progression, is a well worn argument in favor of the sporadic origin of species; that is, of the descent of each species from many parent stocks, existing in distinct and separate localities. But if all the facts of the case are fairly stated, there appears much, even in this instance, in favour of the doctrme of specific centres. The facts are briefly these. Many species of. Unio, e. g. U. marginalis, Lam. exist throughout a large tract of country, in almost every river and stream, and even in many ponds and marshes, although these rivers, &c. have no fresh water communication with each other what- ever, and the animal is incapable of living in the sea, or of traversing the land. On the other hand, the area inhabited by this species is continuous; that is to say, the same species does not occur in tropical Asia and tropical America, for instance. Other species are restricted 1865.] Contributions to Indian Mulacology. 103 to a single river and its feeders, as is the case, so far as is known, with U. olivarius, Lea. In other cases again, as in U. ceruleus, Lea, and its allies, one form is found over a considerable area, as Bengal, and in separate rivers, and is replaced at a distance, as in Scind and Western India, by forms which may either be considered as distinct species, or as local varieties, according to the value attached to specific rank. In the intermediate country of Central India, we find interme- diate forms. Now it is surely more philosophical to assume that we are only partially acquainted with the phenomena attending the means of distribution enjoyed by animals of low organisation, especially in the young state,* than to arrogate to ourselves complete knowledge of the subject, and to assert that no means of passage exist. If we sup- pose that facilities for migration exist, or have existed, with which we are unacquainted, all the facts above detailed are at once accounted for in the simplest manner, whereas on the theory that the species were originally created throughout the whole area, no explanation whatever is afforded of the limitation of that area, no cause shewn why the same species does not exist in other areas where the conditions are equally favourable for its existence, and still less is any explanation afforded of the gradual divergence of varieties at a distance from the typical form. Let it be distinctly noted that the case of mollusks and of other animals inhabiting fresh water is an exceptional one; in the vast majority of the members of the animal and vegetable king- dom, the phenomena are far more strongly in favour of the theory of specific centres. On another question, more especially treated in Mr. Theobald’s second paper, viz.: the impracticability of drawing a line between species and varieties in many cases, I entirely coincide; indeed in the preceding pages will be found remarks upon the varieties of H. sem- Jaris and its allies, and of H. rotatoria and its allies, similar in pur- pose to those of Mr. Theobald. LI must, however, object to the practice of publishing names, whether of varieties or species, without any description, or with such extremely inadequate details, as in the case of Helix Arakanensis and H. geiton. I can only say that, *Tt should not be forgotten that the ciliated fry of the Unionidae have very considerable power of locomotion, and that even the adults are amongst the most vagrant of bivalve shells, 164 Contributions to Indian Malacology. [No. 2, although I probably possess the former, I am totally unable to tell, from Mr. Theobald’s account, to which of the numerous varieties of H. rotatoria he has applied the name. Again, in this paper as in former ones, manuscript names are introduced without any reference to the fact of their being unpublished ; and, in two cases at least, I believe I can shew that these names would never have appeared, had they not been cited by Mr. Theobald. Ist. H. wnicincta was a manuscript name of Mr. Benson’s for a shell from Western India, described by Pfeiffer as H. propinqua. Mr. Ben- son’s name of course was never published, nor would it have seen the light but for Mr. Theobald, who, in his paper in 1863, gave H. uni- cincta as a species excluded from his list, without referring to the fact that no such name existed except in manuscript. In the present paper, H. propingua, Pir., is first given as a distinct species, and a few lines further on quoted as a synonym of H. wnicincta ; thus giving precedence to the manuscript name, in opposition to the laws of scientific nomenclature. 2nd. H. anoplewris was a manuscript name given by Mr. Benson to some shells sent by Mr. Theobald to England, I believe in 1860 or 1861. Mr. Theobald having kindly furnished me with specimens of the same shell, I found, on comparing them with the types of 1. orna- tissima, Bens., of which I had a good series, (the shell was first col- lected by my brother and myself and described from our specimens) that the species were identical in every respect. I wrote to Mr. Ben- son to tell him my opinion and on recomparing the forms, he found that he had been misled by an abnormal peculiarity in the solitary specimen of H. ornatissima which he had retained. Another name mentioned by Mr. Theobald, Helix submissa, Bens., is equally, so far as I am aware, undescribed. In the group placed by Mr. Theobald next after that in which the above shells are included, there is evidently a misprint, in the five shells from H. im/rendens, Gould, to H. sanis, Bens., being classed together. I have no doubt Mr. Theobald’s intention was to class together the three first, and, as a separate species, the two last.* * T am authorized by Mr. Theobald to notify that this error was due to a misinterpretation of his manuscript. His intention was that suggested in the text. Hp, 1865. Contributions to Indian Malacology. 105 As regards the new species described, Liman viridis, if it has no internal shell, and none is mentioned, can scarcely be a Limax. The characters given are mostly unimportant, while essential characters, such as the position of the mantle and breathing pore, surface of the mantle and body, carination or roundness of the back, form of the jaw and lingual teeth, are omitted. What advantage is gained by publishing names for a genus and two species of slugs, of which Mr. Theobald has unfortunately no notes, is not clear. Vitrina Pegu- ensis is the shell referred to above as undoubtedly a well marked and distinct species. Streptawis Blanfordi and Pupina Blanfordi are also mentioned above, they being, I believe, varieties of S. Andama- nica, Bens., and P. artata, Bens., respectively. Streptaxis Burmanica I have described above, and as my description is more detailed, and taken from a better and more typical specimen than Mr. Theobald’s, I have retained it. On the other species I have nothing to add. In Mr. Theobald’s 1863 paper, he referred my Cyclophorus patens, as I have before stated, to C. fulgwratus. I can scarcely believe that he is now serious in proposing to unite these shells, because one is searce and the other abundant, although that is the sole reason assign- ed. Even in this point, however, Mr. Theobald is not quite correct. T have found C. patens in some places the more common shell of the two. On the question of the restriction of the genus Nanina, I can only say that Mr. Theobald’s ideas are totally at variance with those of Pfeiffer, Adams, Gray, Albers, and other authorities. On the other hand he is probably correct in his opinion that HZ. pansa and some other shells do not belong to the section Macrochlamys of Benson, with which I had classed them. 106 Notes on the Sandstone formation, &c. [No. 2, Notes on the Sandstone formation, &c. near Buxa Fort, Bhootan Dooars.—By Captain UH. H. Gopwin Austen, £.2.G.S., Survey- or, Topographical Survey. Plate IV. [Received 26th April, 1865.—Read 3rd May, 1865. ] Having heard from Asst.-Surgeon Fergusson, R. A. at Buxa, that he had found several pieces of coal in the bed of a nulla below the position near Santrabari, I paid a visit to the spot accompanied by that officer. Buxa Fort, at 2,400 feet, is situated near the foot of the first range of hills, that rise above it on the north to a height of 6,000 feet above the sea; this ridge being the continuation of the western water-shed of the Tzinchu, the river from Tassi Chotzong in Bhootan. The rock of this range is a well stratified gneiss, thick beds of quart- zite occurring in it, being even schistose in places. The plateau on which stands the Fort of Buxa is composed of debris and talus from the hills above, and is situated in a valley formed by spurs from the northern ridge. The eastern of these spurs is of the formation mentioned above, but the western is found to be of sandstone, having a light ochre tint, coarse and micaceous, with here and there water-worn pebbles in strings; its stratification not being so well marked as in the sandstones of the Siwalik group. The ridges on the west of this are all of this same formation, but do not extend much higher than 5,000 feet. As one proceeds down the western spur to Santrabari, the sandstone is soon hidden by a surface talus of the older rocks, and the rock in siti is only to be seen by descending into the deep ravines. Crossing the stream at Santrabari, proceeding east and topping a spur covered with sal trees, I descended into another ravine, very precipitous on the western side: here the sandstone was well displayed, and several pieces of the coal were soon found in the bed of the ravine. The outermost beds of sandstone are very soft, with a light bluish tinge, and in them the coal, properly speaking lignite, was discovered, occurring in lumps and strings: these lumps shewed the woody structure well, splitting in the direction of the fibre. The form of a portion of a tree pressed into an elliptical shape, was well seen in one instance, but I could find no impression of leaves, im, ' panynaping: ‘ Journ, As. Soe. Bengal. Vol. XXXIV. Part 2, Pl. IV. Section near BUXA, BHOOTAN DOOARS. 6060 Fut, Bhootia Stockade, \ Fort. 2,400 FE Santrabart 1 of ( lignite)? t « Sie Na / f HF ‘ f i $ oy - aie i Lalas mise el koh \ id EE tet abe ‘ bho Breer) i if fp i ) ig j f ei i t b... JHeeTEe UD yeah Cees ales Ri 3 ted aii einale beuis addon Gaiiit Si teree) } 5 GALT D Aan atv ame De y des’ ‘ Plate IV. to illustrate Capt. Godwin Austen’s paper, will be issued with No. 3 of the Physical Science Part. ee ae erg he ak 3 SAN ngs wien son bata sd « és Myphed a dhs Wh ls ei JOURNAL OF TUE meal LO SOGiET Y. —}—. Part I1.—PHYSICAL SCIENCE. eee No. I1.—1865. ~ Remarks on the Vegetation of the Islands of the Indus River.—By J. H. T. Arrcutson, M.D., F.R.C.S.E., F.L.S., Hxtr. Member, Royal Med. Soc., Edin., dc., Asst. Surgeon, Bengal Army. [ Received, 18th March, 1864. } As much interest is being attached to the local production of fire- wood for the use of the steamers that ply on the Indus river, I have the honor to forward the accompanying notes taken during a passage made up that river and its tributary, from Kotree to Mooltan, on board the steamer ‘ Havelock,’ Capt. Davis, Commander, which left Kotree on the 29th of August and reached Mooltan on the 16th of September. The river at the time of starting was at its highest, inundating much of the country and causing an immense number of islands to be formed in its course. It is the vegetation of these islands I would describe. It is not very extensive, but what there is of it is turned to much account and might be to more, — The following is a list of the Flora met with, viz. :— Acacia Arabica, L. A. Arabica, var Cupressina, Prosopis spicigera, L. Populus Euphratica, Oliv. 8 54 The Vegetation of the Islands of the Indus River. [No. 2, Tamarix Indica (= T. Gallica, L.) T. Dioica, Roxb. T. Orientalis. Phenix Dactylifera, L. Saccharum Munja, Roxb. S. spontaneum, L. 8. eylindricum, Lam. Typha (angustifolia ?) Creeping amongst the above, climbing to the top of all, shewing off its lovely flowers, was Asclepias rosea, Roxb. in great beauty. Acacia Arabica, ‘Bubber’ (Scindee,) ‘Babool’ (Hind.) ‘ Kekur’ (Punjabee). A. A. var Cupressus, ‘ Caublee-bubber’ (Scindee). This tree with its variety grows in very great luxuriance and tolerably rapidly, and within 60 miles of Kotree it is in much greater abundance than further up the river; it here forms dense jungles and yields very fair timber. The tree itself is too valuable to be directly used for firewood, its chief timber being used for railway sleepers; the rest of the wood and branches only are converted into firewood or charcoal, and the bark and fruit reserved for tanning purposes, A tree (as it stands) that can yield from two to three sleepers, costs one Rupee, the buyer felling and carrying it away. White ants do not imjure the felled logs much, and the old wood is tolerably proof to their attacks. The timber of the Cupressiform variety is considered the better, being closer in grain, and harder than that of the common outspread- ing tree: being also of ‘greater length, and thus generally giving an additional sleeper. Prosopis spicigera, ‘ Kunda’ (Scindee,) ‘ Jand’ (Punjabee). This tree is not common-on the Balaas ; indeed it is scarcely to be seen in any quantity until we get above Sukker, and then chiefly on the mainland, where it is obtained largely, especially at one of the river wood stations called Jummalee. Its wood is good for fuel, but alas, too readily attacked by white ants. These insects seem to relish it:more than any other of the woods, and from the great loss it suffers from these destructive insects 1865.] The Vegetation of the Fslands of the Indus River. 55 whilst stacked, its collection for the supply of the steamers is prohibited. For the reasons. given against. its being stored for fuel, its timber is likewise not used by the natives for any purpose whatever, when other can be obtained. The fruit, however, called in. Scindee “ Singhar,” is.considered an excellent. vegetable, and is largely. eaten by the natives in. their thur- karies. Populus Euphratica, ‘Bahn’ (Scindee and Punjabee,) grows in great abundance on the Balaas, but more especially about a hundred miles above Kotree. It is a rapidly growing tree, producing very fair timber, with a white light wood, very useful for furniture and house- hold-work of a light nature, but which. does not, stand mueh. strain. It is a very dangerous. article as fuel in steamers, or when used for the railway, as the wood, owing to its lightness, flies up through the fiue when only half burnt. The officers commanding the steamers are very careful that none is ever taken on board, even by mistake, from the danger attendant on its use. The timber for furniture costs about 5 annas a cubic foot. Tamaria Indica, ‘ Laee’ (Scindee,) ‘ Jhao’ (Hind.) ‘ Furash’ (Pun- jabee). Yhis may be considered as the chief source of firewood from Mooltan to Kotree.. It grows in immense quantities, but above the union of the five rivers with the Indus, it becomes gradually replaced on the Balaa land by the Z. dzoica and it becomes more abundant on the mainland, where we find the 7. orientalis also occurring, but as a very much larger tree. These were all in blossom in September, presenting a very heath-like appearance just before the flowers expanded. The 7. Indica like all its congeners, grows very rapidly, producing in three or four years a deep red wood, very much like the Beef wood of. Australia. At this age it is best for fuel: the white and young wood makes but poor fuel, and is also rapidly destroyed by the white ant; whereas the red wood may lie for nearly four years without injury; but as it becomes completely dried and aged, it becomes more liable to the attacks of these insects. The cost of this wood at the river stations is 15 Rupees for 100 maunds. 56 The Vegetation of the Islands of the Indus River. [No. 2, Tamarix diowca, ‘ Pilchee,’ (Scindee and Punjabee,) first met with in any abundance on the Balaas near Bukree; above that station it gradually takes the place of Z. Indica. It is greatly used for all thatching purposes, basket-work, d&e. Tamarix orientalis, ‘ Asree-loua’ (Scindee,) is an unknown tree on the Balaas, but on the mainland it not unfrequently forms a prominent object im the landscape, generally near villages. The tree lives best in a dry and salt soil, where it very rapidly produces large timber, but this does not make such good fuel as the 7. Indica. The native names of these Tamarisks are much confounded even by the natives themselves. The name ‘ Furas’ in the Punjab is applied to all, but chiefly to 7’. Orzentalis. They are so very much like each other that this is not to be wondered at. Edgeworth, in his Flora Mallica, calls 7’. diowca, ‘ Lai,’ and 7. Galliica (= T. Indica) * Pilchi.’ I would consider the Scindee names as typical, from their being connected with something further than simply the tree as it grows, viz. in the one case the value of the wood for fuel, 7’. Indica, ‘ Laee,’ ‘ Jhao ;’ in another the use of the shrub for thatching purposes and the known fact of this kind never producing wood, 7’ dioica, ‘ Pilchee ;’ and lastly with the fact that it forms a large tree, the wood of which is not so good for fuel, 7. Orientals, ‘ Asree-loua.’ Pheniaz dactylifera, is occasionally to be seen on the Balaa land between Sukker and Mooltan, where it is very common on the main- land also. A splendid grove of these trees, surrounding Sukker, is seen from a long distance off. After leaving Kotree some forty miles, we see none of this tree until Sukker comes in sight, whereas round Kotree it is very abundant, and at and near Mooltan it is also very abundant. Saccharum Munji, ‘ Moonj, (Scindee and Punjabee). Thousands of acres of river land are covered with this useful grass, the value of which might be greatly raised by the introduction of machinery for converting it into pulp for the Paper Maker. And Sukker would be the place for starting such an establishment, as it grows chiefly above Sukker, to which place it could be floated down the river at little or no cost. This very floating down would aid in the treatment required by all fibres to bring them into a fit condition for working. The surrounding country yields immense quantities of an Alkali 1865.] The Vegetation of the Islands of the Indus River, 57 (Sugee-muttee) with which the material could be cheaply bleached, then to be forwarded to England, to be converted there into finer pulp and paper. The great outcry at home since the commencement of the cotton famine has been for material, capable of being converted at a cheap rate, into paper of a fine quality. Coloured materials require much bleaching, and this in England is the expensive part of the process. Now if such a material as Moonj, which costs at the place of growth little more than the labour of cutting, could be bleached thoroughly with the alkali produced on the banks of the river, this would supply the great desideratum of the paper-makers. Ksparto (Stipa tenacissima) has been very largely used in England within the last three years, but its great drawback is the expense of bleaching it. - The Moonj is largely employed by the native boatmen in making | ropes for their boats, which they manufucture for themselves. Saccharum spontaneum, ‘Khaus’ (Scindee.) This grass grows in great luxuriance. It is chiefly used for thatching purposes, and makes tolerably good grazing for cattle, although as it. ages it becomes a very rough coarse grass, when the cattle seem to leave it alone. It begins to flower early in September, and its flowering has just ceased, when the S. Moonja commences to flower, which is about the beginning of October. Typha (angustifolia?) ‘Pun’ (Scindee,) is very common in the back waters, but more especially above Sukker. I cannot say it is even common below Sukker. The leaves are largely used for making matting (chuttie) and the soft down attached to the ripe fruit is used for stuffing pillows. The pollen is said by Lindley to be converted into bread in Scind. Although I made many enquiries relative to it, I could get no information about it. On examining the wood brought on board the steamer, (about which Capt. Davis gave me every information and assistance in his power, ) I found that nearly’ the whole of it consisted of the wood of the Tamarix Indica, and the wood was called Jhao. We occasionally took on board that of the Acacia Arabica called ‘Bubber.’ But I had to procure specimens of that of the Prosopis Spicigera called ‘ Kunda,’ and of the Populus Huphratica called ‘ Bahn,’ 58 The Vegetation of the Islands of the Indus River: [No. 2; The Captain considered the billets that were large enough to be split into two, of the Jhao, when it was “as red as beef” as the best wood on the river. But his heart used to long for the wood he once got when up the Jhelum river. “ Cows, that’s the thing for driving the engines.” Olea Huropea, ‘Cow’ (Punjabee. ) Immense injury is done to the wood. after it is collected at the wood stations, by white ants, which will, in a very few days, if not carefully looked after, destroy a stack, leaving a mass of mud in place of the original wood. White ants will not attack the Jhao, if the wood is red, to the same extent that they do the other kinds of wood.. The soil of the Islands varies very much. It consists nearly altogether of a rich alluvial deposit at Kotree, gradually becoming more sandy as we ascend the river. This change to a sandy soil is very much more marked above Sukker, after which the soil really seems to be all sand with no earthy matter. Owing to this change in its composition as we gradually get above Kotree and approach ° Sukker those massings of the Acacia Arabica that we had down the river become less numerous and thinner: until at last by the time we have reached the junction of the five rivers with the Indus, we lose them altogether, as well as the Zamarix Indica, which is now replaced by the JZ. dioica. Moonj gets abundant above Sukker and the Islands are vety much less wooded, being more covered with grasses. I have no doubt that much of this river land which at present really lies waste, might be, with a little care and management, covered with trees capable of yielding both timber and firewood. We should look to timber as the ultimate object ; in doing so, we obtain firewood as a collateral result. In covering these islands with vegetation we aid in rendering them somewhat more permanent than they are at present, by the roots grasping and keeping together the soil. The following may be considered the history of one of these islands that may have remained permanent. In the month of September as the river falls, a mound of sand gradually appears, enlarging daily as the river becomes lower, and bare and barren. But as the September winds blow, they carry clouds of the seed of the Saccharum spontaneum from other islands; these iall on the soil and then readily germinate. Ina couple of months the 1865.] The Vegetation of the Islands of the Indus River. 59 S. spontaneum has sprung up, and its leaves now aid in catching the seeds of the Tamarix and S. Munja, which having ripened, are flying about at the mercy of the winds. The two latter lie dormant until the next year. In the meanwhile the S. spontanewm for a short time kept down by the cold season and eaten over by the cattle, has its growth stopped until March or April, when it springs up, and by September is in its full growth and blossom. The Tamarix and S. Munja being now, on the rising of the river in August, placed under favourable circumstances, begin to grow rapidly, and by the end of the second year cover the Balaa, killing out S. spontanewm to a great degree. Upon the island being flooded at the end of the second year, the vegetation on it catches the seeds floated down by the river, and these in their turn germinate and gradually develope a jungle. At very little expense, indeed, many of these Balaas might be sown broadcast with the seeds of timber trees, (Acacza or ‘ Sissoo’ are undoubtedly the best) about the beginning of August. When the river rose it would cover the islands and deposit sufficient alluvial soil to permit their germinating and taking root. The seeds would not be carried off by the currents, as they become entangled in the grass, which after an inundation is generally seen pressed flat to the surface: with a large amount of alluvial deposit keeping it down. Developing jungles on these islands, would not only supply timber, firewood, &c., but by making the islands permanent, would to a great extent assist in forming a permanent channel for the river, the absence of which is one of the great difficulties to be overcome at present by the navigator. 60 Indian Gasteropoda., [ No. 2, Observations on certain strictures by Mr. H. F. Buayrorp, on my Paper on the distribution of Indian Gasteropoda in J. A. S., No. CCLXXXIX. Page 69.—By W. Tuxosan, Jr. (Received 21st May, 1864.) (Read 1st June, 1865.) My iriend Mr. Blanford, loc. cit., after reading the above paper; among other remarks, expresses himself as follows :— The sporadic origin of species is not held by any eminent naturalist of the present day, and Mr. Theobald had advanced no instance in its favour.” Now the peculiar distribution of a few species over an enormous area, was the reason for my preferring the supposition of a sporadie origin for them at least as the only intelligible one, and if for the majority of species, this view is not so imperatively requisite, yet for such species as Bulimus pullus, B. punctatus, B. gracilis, B. coenopictus, and others, it naturally suggests itself, though I doubtless must have expressed myself so badly as to warrant Mr. Blanford in denying my having “advanced any instance in its favour.” Rejecting however, the obvious view, as I hold it to be, of sporadic origin, it yet remains to be seen what explanation consonant with the Darwinian hypothesis, can be offered, and I shall eagerly listen to Mr. Blanford’s suggestions on this point. I see of course, that in terming the origin of any species ‘‘ sporadic,” I explain nothing, and that it amounts to a confession of ignorance, still this is a negative evil and leaves the ground clear for any superstructure which fresh light may enable us to add, but not so a positive assertion of a law, which, however, applicable in some cases and true to some extent, does not meet all, and appears contradicted by some. I will now advert to the first portion of Mr. Blanford’s stricture to the effect that I held views which no eminent naturalist did, and certainly such a statement was not encouraging, but on returning to station within the last month, I accidentally came across a work which considerably reassured me; though how far Mr. Blanford will admit the names of A. A. Gould and Louis Agassiz to be eminent in their department, after the quotation I shall presently make, I cannot say. Any how I find in the , “Principles of Zoology” by those Professors, my identical theory 1865.] Indian Gasteropoda, 61 laid down, on precisely the same grounds of certain peculiarities in the distribution of Fish, which appeared to me (though unhappily not to Mr. Blanford) so convincing in the case of the Land Shells. of India. So identical are the results and the proofs in either-case, that I think it necessary to.say, that till the present month, I had never seen the work I am about to quote from, or any writings whatever of either Gould or Agassiz, and that my views of the sporadic origin of certain species of shells were deduced from considerations touching: their distribution, and in ignorance of similar arguments, derivable from the study of an entirely different class. The following quotation from page 211 of the Principles of Zoology will prove how closely the estimate I formed of the practical effects of accidental distribution, corresponds with that. held by Gould and Agassiz. “448. Other causes may also contribute towards dispersing animals. Thus the sea-weeds are carried about by marine currents and are frequently met with far from shore, thronged with little crustaceans which are in.this manner transported to great distances from. the place of their birth. The drift wood which the Gulf Stream floats from the Gulf of Mexico even to the western shores of Hurope is frequently perforated by the Larvee of insects, and may probably serve as depositories for the eggs of fishes, crustacea and mollusks. It is possible also that. aquatic birds may contribute in some measure to the diffusion of some species of fishes and mollusks, either by the eggs becoming attached to their feet or by means of those which they evacuate undigested after having transported them to considerable distances. (Still all these circumstances exercise but a very feeble influence upon the distribution of species in general, and each country none the less preserves its peculiar physiognomy so far as its animals are concerned. “449, There is only one way to account for the distribution of animals as we find them, namely to suppose they are autochthonoi, that is- to say that they originated like plants, on the soil where they are found. In order to explain the particular distribution of many animals, we are even led to admit that they must have been created at several points of the same zone, en inference which we must make from 9 62 Indian Gasteropoda. [No. 2, the distribution of aquatie animals, especially that of fishes. Vi we examine the fishes of the rivers of the United States, peculiar species will be found im each basin, associated with others which are common to several basins. Thus the Delaware river contains species not found inthe Hudson. But on the other hand, the pickerel is found in both. Now, if all animals originated at one point and from a single stock, the pickerel must have passed from the Delaware to the Hudson or vice versi, which it could only have done by passing along the sea shore or by leaping over large spaces of terra firma; that is to say, in both cases it would be necessary to do violence to its organisation.’ This last argument must of course stand for what it is worth, and were it alone, would not be worth much, but we have here, with fish, as I have shown to be the case with Gasteropods in India, the grand fact of certain few species of enormous range, compared with the limited extent of their more numerous congeners and the absurdity of supposing that they have been thus widely distributed by any physical agency, which has left the great majority unaffected by its operation. Hence my reasons for leaning towards the ‘sporadic’? theory, for some species at least, not singly at all events, I am glad to see, if however, in company with no other physiologist than Louis Agassiz. I cannot conclude these observations without quoting a passage from the vitriolic pen of Dr. Knox, in his work on Race, where, though he holds that ‘‘ Time and developement change all things” (page 94, ) yet is very bitter on the absurdity of supposing that accrpEnT has anything to do with such changes. Knox on Race, page 90, “‘ When Tam told that there is a short-legged race of sheep somewhere in America, the product of accident, my reply is simply, I do not believe it, even although to make the story look better, it has been added that from among the few short-legged sheep accidentally produced in the flock, the owner was careful to extrude the long- legged ones, and so at last his whole flock became short-legeed, and he had no more trouble with it.—It is the old fable of Hippocrates and the Macrocephali reduced to something like a scientific formula. Transferred from sheep, it has been made the basis of a theory of race of mankind, reducing all to accident. By accident a child darker than the rest of the family is born; when this happens in the present day, it is also by courtesy called an accident, but its nature is well 1865.] Note relating to Sivalik Fauna 63 understood—not so in former times. This dark child a little darker than the others separates with a few more from the rest of the family and sojourns ina land where a hot sun embrowns them with a still deeper hue. In time they become blacker and blacker or browner and browner. Should they travel north instead of south, it is all the same ; for extreme cold produces the same effect as extreme heat! This is ancient and modern physiology !”’ PP PLPILIPILPL LLP LPI LIPID PIP PPPS PPL DD, Note relating to Swalik Fauna —By H. B. Mepricort. [Received 7th September, 1864. ] [Read 7th September, 1864. | The notice I have to bring before the Society may be considered a continuation of a series of brief but important communications, com- menced more than thirty years ago, and continued during some twenty years, as recorded in the volumes of the Journal of the Asiatic Society for that period. Those communications formed a current chronicle of the discovery of the Fauna Sivalensis. Had the account of those discoveries ever assumed a more connected and complete form, the correction I have now to make, would never have been needed, as it is but the statement of a fact, of which the evidence was in hand and in mind, although never expressed. Indeed, for the same reason, this fact can now be only indicated, its value being still unknown. This fact is—the existence of two vertebrate faune, possibly quite distinct, among the fossils hitherto collected from the so-called Sivalik rocks. In a recently published number of the ‘ Memoirs of the Geological Survey of India, Vol. III. Part 2, I have given a somewhat detailed account of the geology of the Sub-Himalayan region in North-West India. I therein established a threefold division of the great series of deposits coming under the general title of Sub-Himalayan. Concerning the lowest of these groups (Subathu, etc.) little or no conflict- ing evidence presented itself. The two upper groups I described as in all respects more akin to each other, although still most clearly separable along a well marked boundary, at which the younger strata overlap the steeply denuded edges of the older, besides being 64 Note relating to Sivalik Fauna. [No. 2, largely made up of their debris. Such evidence is so immutable to the geologist, and, when on so grand a scale, entails such grave consider- ations of time, that I presumed to call in question the one published statement (in Vol. III. p. 527 of the J. A. S. B. for 1834) of vertebrate Sivalik fossils having been found within the area of the older groups, not having myself succeeded in re-discovering fossils at the locality indicated. My scepticism was of course based upon'the @ prior? consideration of geological time; and because, as I state at p- 105 of my Memoir, no corresponding distinction has as yet been suspected by the authors of the Fauna Sivalensis. I made due attempts to authenticate the observation which I had called in question by referring to the original discoverers ; .as, however, in every reply I received, there was some trace of ambiguity, not wishing to give further trouble to my correspondents, I published the whole case in its unsettled form, giving ‘full directions for the application of the verdict on either side (see pp. 15, 16, 104—6, of my Memoir). I have now the pleasure to announce this verdict ; and, notwithstand- ing the precaution I took to provide for its application, the fact cannot well be stated without a few words of explanation. Ina letter dated the 16th July, 1864, Sir Proby.Cautley tells me that he has himself collected fossils on the north side of Nahan 7. e. in the rocks of my middle group, the same in every respect as those he had found more abundantly at the south base of the Sivalik hills, east of the Jumna. ‘The peculiar mode of occurrence of these fossils in the nodular clays (‘ clay-conglomerate’ of Cautley), as compared with those found in the coarse gravel deposits, could. not escape observation. The former were all small and fragmentary. Large masses of the clay had to be carted from the hills and broken up at leisure in search of the fossil remains. I need scarcely, however, state that the Sivalik fossils have hitherto been given and received as one undivided fauna. Every one interested in these subjects will join in the regret expressed by Sir Proby Cautley that it is now impossible to work the question out, unless upon fresh materials. He informs me that the large collection of these smaller fossils, sent by him with the others to the British Moseum, is now not to be found. To paleontologists then, we may now announce that a most interest- ing case awaits their investigation, namely, the comparison of well 1865. ] Note relating to Sivalik Fauna. 65 represented vertebrate faune, occurring in a series of beds, closely related in point of geological conditions of deposit, etc., and yet distinctly separated (broken) in time. The application of the fact to stratigraphical geology may now take shape. The strata at the base of the sections visible in parts of the Sivalik hills are representations of the Nahun group—the middle group of the Sub-Himalayan series. The expression of this on a map must still be arbitrary : for the true Sivalik strata (though so strongly unconformable with the ‘ Nahun’ strata along their junction with the inner zone of these Nahun rocks,) appear to pass conformably and even by gradation into the representatives of the Nahun strata in the eater zone. It is of course to be expected that a very close study will reveal traces of this unconformability in the sections of the Sivalik hills also; but in such massive, banked strata, from twenty to two hundred feet thick, the determination of such a feature will be very dubious. In physical geology this feature will be only another example, on a larger scale than those given in my Memoir, of the supposition I have offered in explanation of the mode of disturbance of all these Sub- Himalayan rocks—slow contortion and upheaval along narrow zones synchronously, with more or less uninterrupted deposition im the ad- joining exterior area. 66 Contributions to Indian Malacology. [No. 2, Contributions to Indian Malacology, No. V. Descriptions of new land shells from Arakan, Pegu, and Ava ; with notes on the distribution of described species—By Wiuttam T. Buanrorp, A. &. S. I, Et. GS. [Received 11th March, 1865. ] Orprer,—PULMONIFERA. Family Helicide. Genus NANINA. Section Macrochlamys. 1. N. compiuvratis, n. sp. Shell perforated, subglobosely depressed, thin, light-coloured, horny, smooth, polished, diaphanous, very minutely striated. Spire convex ; suture ina deep and rather broad groove, which becomes obsolete at the apex. Whorls 43, convex, sharply angulate above at the edge of the sutural groove; the last not descending near the mouth. Aperture, oblique, irregularly lunate, of the same form as the whorls, nearly equal in height and breadth; peristome thin, in one plane, simple ; margins distant, columellar briefly reflexed at the perforation. Millem. inch. Major diameter, .......«..00. se 10 0.4 NUIT TEL O jy itpics ae sciencissene 9 0.36 PASSAB ath dacsciee sioiwans pas se ee 64 0.26 Aperture 5 millem. broad. Habitat —Arakan hills. This shell is closely allied to N. convallata, Bens. of the Tenasserim provinces, and replaces that shell in Arakan. It is distinguished by the smaller number of whorls, while the singular sutural channel is even more developed, but it varies slightly in size. 2. N. NEBULOSA, n. sp. Shell minutely perforated, conoidly depressed, thin, light horny, not polished, minutely striated, and possessing a dull greasy lustre. Spire conoidal ; apex rather acute; suture impressed. Whorls 6, convex above; the last rather broader, subangulate above the periphery rounded beneath. Aperture slightly oblique, lunate, the breadth greater than the height; peristome simple, thin; columellar margin vertical, slightly reflexed, 1865.] Contributions to Indian Malacology. 67 Millem. inch. Major diameter, 00.0. .0). 00000. 114 0.46 WOR GIELO, 2.020) le sis owas aes 10 0.40 2. SE. soca Oe REE ae oe eee 6 0.24 Aperture 6 millem. broad, 43 high. Habitat—Akoutoung on the Irawady, below Prome, Pegu. This species may be distinguished from its numerous allies of the Macrochlamys section by its blunt angulation at the periphery and its dull lustre. Its nearly vertical mouth amply serves to shew its dis- tinction from N. honesta, Gould, which shell moreover is more polished, and differs in several other particulars. 3. N. wypoLEuca, n. sp. Shell openly perforated, depressed, very thin, smooth, polished, horny ; dark brown above; lighter, frequently white below; faintly striated, obliquely above, radiately below, with extremely fine con- centric microscopic markings, which are frequently obsolete. Spire very little raised; apex rather obtuse; suture impressed, sometimes sub-marginate. Whorls 5, rather convex above; the last rather broader, rounded beneath, not descending. Aperture lunate, the breadth exceeding the height, nearly vertical; peristome acute, straight ; columellar margin descending with an oblique curve, scarcely reflexed. Millem. inch. Mayan diameter.) 5 sememnncaiqdoit- 12 0.48 Mit SEITE EO 6. 5 on: ninsbiciclds diced de 103 0.42 ISTE 2 Re ee ee ee aR 6 0.25 Habitat—Akoutoung, Pegu. Scarce. Near NV. causia, Bs., but larger, more depressed, and with far finer microscopic spiral sculpture ; so fine indeed that it is difficult of detec- tion even under a powerful microscope. H. hypoleuca may be re- cognised by its pale base, and dark horny colour above, and by its open perforation. A small form, perhaps identical with the above, but only 5 or 6 millemetres in diameter, is common in northern Pegu. I had con- founded it with N. causia, Bens., but Mr. Benson informs me that 68 Contributions to Indian Malacology. [No. 2 that species is very different. This small form differs from NV. hypoleuca in its more marked spiral sculpture, which, however, is still microscopic. Section Hemzplecta. 4. N. Unposa, n. sp. Shell narrowly umbilicated, depressed, rather solid, white (? horny when fresh,) peculiarly marked with irregularly sinuous close spiral sculpture resembling scratches, and crossed by oblique lines of growth. Spire very depressly conoid ; apex obtuse ; suture impressed. Whorls 5, rather rapidly increasing, somewhat convex; the last broader, rounded at the periphery and below; the spiral sculpture passing over the periphery and gradually dying out on the lower surface, which is marked by radiating striez. Mouth diagonal, broadly lunate, equally broad and high; peristome simple, acute; margins distant, united by a callus; columellar margin oblique, shortly reflexed above. Millem. inch. Major diameter,....... Le sha 36 1.45 Minor aittos UU. VR eee. 31 1.24 2S a1 sath) | bid ae AS bah a Reg 21 0.84 Aperture 18 millem. broad. Habitat—Shan Hills, east of Ava. Distinguished by its peculiar sculpture ; which somewhat recalls that of Nanina Hwmphreysiana, Lea. All the specimens found were dead and bleached; fresh speci- mens possibly possess a coloured epidermis. Section Sesara. 5. N. Wevicrrera, n. sp. Shell imperforate when adult, but with a deep umbilical hollow ; young specimens deeply perforate ; conoidly trochiform, subcampanulate, thin, horny, sharply and arcuately costulated above, the costulation continuing over the periphery; smooth, polished and finely striated beneath. Spire conoid, sides convex ; apex rather obtuse; suture im- pressed. Whorls 7—7}, closely wound, convex, increasing very slowly; the last angulate at the periphery in adults, sharply keeled in immature specimens, flattened beneath, more convex near the mouth, with one or two small, irregularly shaped indentations, (which are mostly opaque from a coating of white callus within the shell), on the lower surface, generally at a distance of about 4 a whorl from the JOURNAL OF THE DMowA TC. SOCLEDY. —— Part I1—PHYSICAL SCIENCH. ees No. III.—1865. Notes on Central Asia.—By M. SrMEnor. (Communicated by Lieut.- Colonel J. T. Watxer, R. LH.) [Received 15th April, 1865. ] [In the year 1856, M. Seménof was deputed by the Imperial Geographical Society of Russia, on a mission of exploration into Central Asia.—On his return to St. Petersburg, he published a trans- lation of Ritter’s ‘‘ Hrdkunde von Asien” into Russian, and gave in the preface to the 2nd volume, an account of the results of his own explorations—The following notes are taken from this preface. At my request they were translated from Russian into English by Mr. R. Michel, F. R. G.S., whose name will be familiar to all who are ac- quainted with the numerous papers on the geography and trade of Central Asia, which have appeared of late years in the Journal of the Royal Geographical Society of London. J.T. W.] 5 The second volume of the Russian translation of Ritter’s ‘‘ Asia” comprises a description of the North Western portion of the tableland of Asia, 7. e. that extensive region which stretches between the Altai and the Celestial mountains, from the Hastern extremity of the latter at Hami (Komul), to the Watershed of lake Balkhash. The range of country under consideration embraces the whole of the extinct kingdom of Djungaria, or the Chinese Province of Tian- 16 114 Notes:on Central Asia. [No. 3, Shan-bey-Lu (the region to the northward of the Celestial mountains, consisting of the districts of Ili, Tarbagatai, Gobdo, &c.) and like- wise the Russian districts of Alatavsk, Kopal and Ayaguz, which now constitute the new Semipalatinsk region. The whole of this country, including, both Chinese and Russian Djungaria, forms that most obscure and unknown portion of the interior of Asia which contains within it the very centre of the Asiatic continent, namely the gigantic mountain group of the Tengri-Tag, (a part of the Celestial mountains) situated at equal distances from the Black Sea, on the West, and the Yellow Sea on the Hast, the Obi Bight on the North and the Bay of Bengal on the South, and lying in the centre of the straight line connecting Cape Severovostochui in Siberia with Cape Comorin in India. : This region offers, moreover, special interest in physical as well as in ethnographical and historical aspects. Physically, it forms a dis- tinct limit between the highland and the depressed portions of Asia, and is remarkable for the contrast it presents between its gigantic mountain groups of the Bogdo and Tengri-Tag in the Celestial range, which tower far above the limits of eternal snows and are crowned with large alpine glaciers, and the low sandy and sterile steppe of the Bedpak-Dala, on the South West of lake Balkhash, which, in common with all the other sandy wastes of the Aralo-Caspian depression, bears the character of a bed of an inland sea, dried up during a very recent geological period. In ethnographical respects this region offers a contrast no less marked, between two numerically preponderating central Asiatic races—the Mongolian and Turkish,—whose rulers are Chinese and Russians, strangers from the far Hast and West, occupy- ing, in the same alluvial plain of the Balkhash, small populated oases in the midst of an indigenous population alien to themselves in speech and habits, and who are powerful not by reason of their numerical superiority, but by the weight of their civilisation, and the magnitude of their respective Empires, the most colossal on the face of the globe, Lastly, from an historical point of view this country presents features of a no less interesting character. It has served from time immemo- rial as the point of departure for migrating races from the highlands of Asia, the cradle whence they sprang, to the low arid steppes of the Aralo-Caspian depression, and to the still more distant and 1865.] Notes on Central Asia. 115 better favoured regions of the West. It was here, namely, in Djun- garia, and on the fertile and smiling banks of the Ili and Ittysh, that the migrating hordes lingered for some time, both, as it were, to venture out into the unknown plain stretching before them far away into the sandy ocean that separates Europe from Asia, until a new tide of popular migration forced them at last to strike their tents, and depart westwards from their mountainous halting grounds. It is also in the valleys of Djungaria that a few existing rude monuments, crude traditions, geographical names, and remnants of tribes who, in many cases, have lost their native dialect by intermixture with other races (the result of which appears in the name of Kassak or Kerghiz Kaisak), serve the scientific explorer as the only links for identifying the obscure and fragmentary allusions concerning these migrated hordes, which occur in Chinese and Russian chronicles. Although the physical and ethnographical characteristics of Central Asia have attracted the constant attention of some of the most learned men, such as Humboldt, Ritter, Abel Remusat, and Klaproth, the researches of these leaders of science could only be based on the most meagre data, namely on the dry and one-sided Chinese narratives which found a place in Chinese literature, from the period of the dismemberment of the Djungarian kingdom inthe middle of the last century, and also on the inaccurate, brief and conflicting accounts and itineraries of a few Asiatics, who succeeded in visiting Djungaria and Little Bokhara with caravans. All these materials were collected and carefully collated by Ritter and Humboldt; nevertheless. this region remained up to the most recent period, like the interior of Africa, completely inaccessible to Huropean science. Even Marco Polo, the most enterprising and reliable traveller of the middle ages, did not visit this region, but proceeded eastwards to China by a route that lay southward of the Celestial range. A few other travellers, it is true, passed through Djungaria; these were Plano Carpini (1246), Andre Songjumel (1249) and Wilhelm Rubriquis (1252) ; and they probably journeyed by way of lake Faisan to Karakorum the capital of the Mongol Khans. The same route was traversed by some of the subjugated Western princes, such as Yaroslof and Alexander Nevski of Russia and Getum of Armenia (likewise in the middle of the thirteenth century) tor the pur- 116 Notes on Central Asia. [No, 3, S| pose of paying homage to the great Khan ; they, however, either left no description of their journey, or else their accounts are so meagre and confused, as for instance, the narrative of Prince Getum, that very few of the places mentioned in them can be identified. Much later, in 1654, Fedor Isakonitch Baikof, the envoy of the Russian Tsar Aleksei Fedorovitch, proceeded past lake Faisan, and the upper course of the Black Irtysh, and traversed the whole of Djungaria, reaching the Chinese wall at Huhu-Hoton from whence he advanced to Pekin. Although Baikof’s marche-route (of course not in the form it is inserted in Wilson’s work from which it was derived by Ritter, but in the shape we find it in Spasskis’ “‘ Sibirski Vestnik’”) can, in the present state of our knowledge of the geography of Central Asia, be pretty readily applied to certain localities, still the information it contains is of a meagre character, and is greatly inferior to native Chinese accounts. The Southern border of the country now under consideration, 7. e. the gigantic Celestial range, has not been explored by any European traveller up to the present day. The destruction, how- ever, of the kingdom of Djungaria, by the Chinese, led to its being surveyed under the superintendence of the European missionaries Felix d’Arocha and Hallerstein, by whom astronomical points were determined, not alone in the towns of Djungaria and Little Bukhara, but also at the very foot of the Celestial range, as at Hongor Olen the modern Konur-Ulen, and on the Southern shore of lake Issyk- Kul. As the Jesuits have left no record whatever of their having visited any part of the Celestial range, it must be naturally concluded that they themselves did not diverge from the highroads of Central Asia, but detached a party of Chinese topographers, instructed by themselves, to the base of the Celestial mountains. The first learned Russian traveller who penetrated into the part of Inner Asia described in the present volume, was the botanist Sivers, who in his hazardous and venturesome journey to the Tarbagatai, in 1793, advanced as far as 47° N. Latitude. During the succeeding forty years, not one of the scientific explorers of Western Siberia succeeded in passing beyond the point previously reached by Sivers. The journey of K. A. Meyer in 1826, did not extend beyond the Arkat mountains, Chingiz-tan, and the Karkara district of the Kirghiz Steppe. The travels of Humboldt, and his associates, in 1828, did 1865.] Notes on Central Asia. aby | not embrace even Djungaria, Their extreme limit was the Chinese picket of Baty, on the Irtysh, in 49° N. Latitude, and Humboldt’s greatest service in connexion with the geography of the interior of Asia consists in the critical elaboration of the materials relating to this subject in his classical ‘‘ Asie Centrale.” Some of these materials, namely the itineraries of Asiatic traders, who had visited different parts of Asia with caravans, were diligently collected at Semipalatinsk by Humboldt, and another portion of his materials was derived from Chinese sources that had been elaborated by the European Sinologists, Abel Remusat, Klaproth, Schott, Neuemann, St. Julien, Father Hyacinth, and others. Among the few unscientific eye-witnesses who, in the pursuit of trade, penetrated into Imner Asia, were some Russians, and among these in point of lucidity, and accuracy of information, the first place is undoubtedly occupied by the interpreter Putinsef, who, in 1811, visited Kuldja and Chuguchak, the most flourishing towns of Djun- garia. The narrative of this journey was published in the ‘“ Siberski Vestnik” translated by Klaproth, and served Ritter as one of the most valuable sources in elucidating the geography of this region. In addition to Putinsef, we may mention the miner Snegiref, who, towards the end of the last century, proceeded from the Altai to the neighbour- hood of Chuguchak, in search of gold; also the noble Madatof, who, in the early part of the present century, successfully reached India, starting from Semipalatinsk, and traversing lake Issyk-Kul, the Celestial mountains and Little Bokhara. A short account of Snegiref’s journey was printed in the ‘“ Siberski Vestnik,” but with Madatof’s expedition I am acquainted only through official documents preserved in the archives at Omsk, and as no original narrative was discovered by me, it must be presumed that none ever existed. I also found a short marche-route at Semipalatinsk, drawn up by the merchant Bubeninof, who, in 1821, proceeded from Semipalatinsk to Kashgar. This itinerary will be printed in due season, but from its brevity and scantiness of information, it is in no respect more valuable than the itineraries already printed and digested by Humboldt and Ritter, Such was the unsatisfactory condition of our knowledge of the geography of Central Asia in 1831, at the time of the appearance of that part of Ritter’s work which relates to it. It was only in 118 Notes on Central Asia. [No. 3, the fourth decade of the present century that we became more familiar with Central Asia, from the side of the Djungarian and Kirghiz steppes, after the foundation of the Russian town Ayaguz, on the upper course of one of the rivers of the Balkhash basin, and aiter the submission of a portion of the great Hordes under Sultan Sik, son of Ablai Khan. These events gradually rendered not only lake Balkhash, but also the mountainous districts of Djungaria, more accessible to travellers. In 1834 the astronomer Fedorof was enabled to reach the embou- chure of the Lepsa, and determine its geographical position, under 46° 23’ North Latitude. He also succeeded in visiting the southern shore of lake Faisan and in making a trigonometrical measurement of Tarbagatai. A little later, the relations of Russia with the Kirghiz Hordes became more satisfactory, and in 1840, 1841 and 1842 the learned travellers Karelin and Schrenk, penetrated into the moun- tainous portions of Djungaria or the Snow-clad Djungarian Alatau. Karelin explored the wild valleys of the upper courses of the Lepsa, Sarkan and Baskan rivers, as high as the snow-line. Alexander Schrenk visited, and it may be said discovered to science, the lake Ala-Kul, crossed over the Djungarian Alatau to the Chinese side, attained the upper course of the Tentek, and reached the snow line on several occasions. The extreme limits of his journey on the plain bordering lake Alakul, were the Chinese town of Chu- guchak, in Alpine Djungaria,—the hills skirting the banks of the Koksu river, and the river Chu (or Tzu) in the hungry Betpak- -Dalor desert, South West of lake Balkhash. Subsequently the voluntary submission of the remaining portion of the so-called Great Kirghiz Horde, in 1844, led to the Russian occupation of that rich and fertile portion of Djungaria, which is known under the name of the Semipalatinsk region, from the seven tributaries of the Balkhash that water it. The Russian town of Kopal was founded by Governor General Prince Gorchakof, in 1846, on a fertile plateau at the base of a snow-capped spur of the Djungarian Alatau. The establishment of this town ensured the development of the already existing relations of Russia with the neighbouring Chinese province of Ili. Although rapidly increasing, the trade with the Western Chinese region, through the towns of Kuldja, and more especially Chuguchak, encountered 1865.] Noles on Central Asia, 119 obstacles in its legitimate development from its transitive and contra- band character, as the Chinese of the Western region (Si-yui) were only able to have secret dealings with the Russians under a semblance of traficing with the Kirghizes. It was this disadvantageous state of things, that led to the mission, with objects partly diplomatic and partly geological, of H. P. Kovalefski accompanied by Vlangagli, an officer of mining Engineers. This expedition started from Kuldja, and skirting the Russian side of the Djungarian Alatau, traversed the valley of the Koksu, as far as the upper sources of this river, while, on the Chinese side, it reach- ed the town of Kuldia, on the Ili. The most important results of this mission in commercial, as well as in scientific respects, were the establishment of Russian trading factories at Kuldja and Chuguchak. The opening up of the Western Chinese region contributed largely to the increase of our knowledge of the geography of Asia, inasmuch as it threw two learned Chinese scholars into the commercial centres of Djungaria in the capacity of consuls. The local researches of these sinologists has opened a wide field to science. Mr. Fakharof, one of the consuls, has already collected materials of great value relating to the physical geography and cartography of Inner Asia; these mate- rials he has obtained during his stay at Pekin, from rare geographical works (namely the reports of the Survey made during the reign of Tsian-Sun) and from information supplied him by natives of the Western region. The foundation of the town of Kopal, which was in a satisfactory and flourishing condition, owing to the rapid develop- ment of agriculture aided by artificial irrigation, could not, however, secure the great Hordes, now under Russian dominion, against the bold attacks of the Buruts, or the so-called Black or Dikokamenni Kirghizes, who infested the valley of lake Issyk-Kul, and the neighbourhood of Tekes on one of the sources of the Ii. This was naturally to be expected from the position of Kopal which stood on the northern confines of the Hordes, whose southern boundary, beyond the Ili, remained completely unprotected. The unguarded condition of the frontier of the Russian Empire on this quarter induced Governor General Hasford to occupy the so-called Trans-[li country extending between the river Ili, and the snow-line of the gigantic Trans-Ili Alatau, with a view of securing the left flank of the Kirghiz Steppe 120 Notes on Central Asia. [No. 3, which was under Russian protection, by making it conterminous with the peaceful frontier of China and the natural snowy mountain boun- dary. This well conceived plan was carried out with complete success. In 1853 the first Russian detachment, under the command of Colonel Gulkofski, was despatched: beyond the Ili; it, however, met with serious opposition from a strong body of Kirghizes belonging to the hostile tribes of the great horde who supported themselves on Fort Trichubek on the river Kesen. But in the following year the whole of the region was occupied by a force under Lieut.-Colonel Peremy- shelski, who razed the Kirghiz fort to the ground; after this some of the tribes submitted to Russia, while the most inimical fled into Kokanian territory, and to the banks of the Talas and Syr- Darya. The Russian detachment passed the winter in the sheltered valley of the Talgar, and in the ensuing year of 1855, General Hasford founded Fort Vernoé, at the base of the Trans-Ili Alatau, at the head of the Almatynka valley, which is picturesquely wooded with apple and apricot trees. The occupation of the fertile Trans-Ili region, well adapted for agricultural and gardening purposes, and in all respects bountifully endowed by nature, had the effect of protecting the great Hordes from the attacks of the Buruts, but placed its nearest tribes in the same position as that occupied ten years previously by the Great Kirghiz Horde. The powerful and numerous tribe of the Bogus, who occupied the picturesque valleys and table-land between the Celestial mountains and the Trans-[li Alatau, received neither countenance nor support from the Chinese, to whom they were nominally dependent, in resis- ting the fierce attacks of the Sary Bogish tribe; they had at the same time to repel, on another quarter, the depredatory incursions of some of their neighbours of the great horde. Consequently, soon after the occupation of the Trans-Ili region by the Russians, the High Manap of the Bogu tribe, the old Burambai, claimed the assistance of General Hasiord against the attacks of the neighbouring tribes, and volun- tarily tendered the submission of himself and his tribe to the Russian government. This led to the despatch of the first Russian detachment from Vernoé to lake Issyk-Kul, for the purpose of pacifying the two contending tribes, and making a reconnaissance of the hitherto unex- 1865.] Notes on Central Asia. 121 plored valley of lake Issyk-Kul. Colonel Khomentofski, the officer in command of this force, and General Siverhelm who was in charge of the Survey of the newly organized Semipalatinsk region, were the first educated Russians who beheld this extensive lake and the snowy summits of the Celestial range. Unfortunately this detachment in consequence of its critical position amidst the wandering mountain tribes, the animosity of one of which against the Russians was decided, while the friendliness of the other was open to much suspicion, was soon recalled, and the surveying parties were unable to penetrate into the interior of the Celestial mountains. The southernmost point attained at the foot of the Tian Shan, by Ensign Yayooski the topo- grapher attached to the expedition, was where the Fauku rushes out if its narrow defile on the Issyk-kul plateau. In the same year of 1856 I was sent by the Imperial Russian Geo- graphical Society on an expedition to explore those more accessible portions of Central Asia, which had previously been but little visited. Naturally the great object of attraction for me on this journey was the Tian-Shan or the Celestial range. The signification of this stupendous chain in position the most retired in the whole continent of Asia, had already been pointed out by Ritter and Humboldt ; but the labyrinth of the Celestial mountains had not as yet been penetrated by any scientific traveller.* All the learned and critical researches of Ritter and * Atkinson, the Hnelish artist, in his travels, which were published in 1858, gives an account of his journey from the river Kurchum, in the Southern Altai, across the Black Irtysh to lake Ubsa-noor, thence southwards, past Ulusutai, to the neighbourhood of the Chinese town of Barkul, at the base of the Tian-Shan ; travelling then parallel with this chain, though at a considerable distance from it, as far as the meridian of Bogdo O’la mountain, and finally proceeding in a North Westerly direction, past lake Kyzyl-bash, until he reached Jake Ala-kul in Russian territory. Unfortunately so extraordinary a journey, unprecedented in the history of the exploration of the Asiatic Continent, has had no beneficial scientific results. The narrative, which occupies 115 pages of text, so little characterises the explored region, that it might with equal fitness be applied to any portion of the Kirghiz Steppe. The critical enquirer finds nothing throughout the whole narrative, to satisfy him of the genuineness of the deseribed journey, which extends over no less a distance than 3,000 miles of Chinese territory. This is the more striking as undoubted proofs of the actual performance of journeys of which descriptions have been given, may easily be found in the short itineraries and accounts of travellers of different ages and nations; as for instance in the travels of Huc and Gabet, in the marche-rontes of Tartar traders, collected by Humboldt, and in the more ancient accounts of Baikof, Marco Polo, the Armenian prince Getum, in the marche-ronte of the army of Gulagu Khan, (compiled by one of his officers in the 13th century) and lastly in the narrative of the travels of the Buddhist Missionaries Fa-Hian EG 122 Notes on Central Asia. [No. 3, Humboldt respecting this range partook, even by the admission of the latter, of the character of conjectural geography, founded on a comparison of the obscure and confused narratives and descriptions and Huan-T'san, in the 4th and 7th centuries. Concise though these accounts doubtless are, the learned critic soon discovers in them such local peculiarities as can only be descriptive of particular spots and localities, and as we become more intimate with the geography of the country to which such accounts apply, the more readily and clearly do we identify the points given in these marche-routes. To our great regret we do not find this to be the case in that part of Atkinson’s work which relates to Chinese Djungaria. From the com- mencement, in calling the Tian-Shan Sayan-Shan, he confounds, in name at least, the two principal mountain systems of Inner Asia; and in all the other portions of his narrative, where he does not confine himself to descriptions of the Steppes, the chase of wild animals, and the social customs of the nomads (descriptions which would apply with equal force and truth to the whole of Central Asia) but wishes to communicate something more definite and locally characteristic, he falls into numerous incongrnuities, Thus, to cite some exam- ples, he speaks of the Kara-Tyn snowy range, at the upper course of the Black Irtysh, as of a level steppe intersected by low ridges; again, from the Tannu mountains, situated at a distance of 120 milesto the N. HE. of Ubsa-noor, he sees the Bogdo-Ola in the Tian-Shan, which is about 750 miles away from this point. Lastly from the plain at the base of the Celestial range, he simul- taneously sees not only the Bogdo mountain, but also the Baishan or Pé— Shan (emitting smoke by Atkinson’s account), which is about 300 miles beyond to the westward, notwithstanding that the snowy Bogdo-Ola group stands out as is well known, considerably in advance of the main chain of the Celestial mountains, and the Baishan mountains rise on their southern slope, that is to say beyond its gigantic snowy ridge, in the neighbourhood of the Little Buk- harian town of Kucha. Similarly as little confidence do those inconsistencies inspire which occur in his account of the time occupied in performing the various journeys, and in his description of the distribution of the nomad Kirghiz population, throughout Chinese Djungaria. As regards ourselves personally, the inyoluntary doubts respecting the abovementioned portion of Atkinson’s travels are still further strengthened from information we gathered on the spot regarding his journeys, from the Cossacks who accompanied him, and from the commanders who provided him with escorts. Atkinson, during his many years’ residence in Siberia, visited the neighbourhood of Kopal, that had then just been founded, many valleys of the Djungarian Alatau, the lake Ala-Kul, Tarbagatai, the rivers Narym and Kurchum in the Southern Altai, the Teletsk Lake, Tunkinsk mountains of the Sayan range, Irkutsk Kiakhta, &c. but as regards his travels over an extent of more than 4000 verts in Chinese territory, accompanied by three Narym or Kuwrchwm Cossacks, I regret to say that I not only could not gather anything to confirm this fact, but I was con- vinced of its utter impossibility, from existing local conditions on the Russian as well as on the Chinese side, On the Russian, because the protracted detachment of these Cossacks, or their voluntary absence from the corps, is a fact that would leave behind it some record in the official archives, while on the Chinese side, the journey lasting more than six months, of a party unac- quainted with the local dialect, and passing through inhabited districts, along established routes, and across the picket and frontier lines, could scarcely escape the vigilant eyes of the Chinese authorities. Under all these circumstances, and in the absence in Atkinson’s narrative of any new data relating to Chinese Djungaria, this work cannot be considered as an acquisition to science, until the author adduces more definite information and stronger proofs, in corrobora- tion of his accounts which involuntarily inspire certain mistrust. 1865. ] Notes on Central Asia. 133 of Chinese and other Asiatic travellers, commencing from the Buddhist Missionaries Fa-Hyan and Huyan-Tsan of the 4th and 7th centuries, to the brief itineraries of the Semipalatinsk Tartar traders of the present century. Numerous questions, replete with interest to the seience of geography, could only be possibly solved by actual investi- gation on the spot. The configuration of the country, the direction of the upheaval of the mountain chain, its mean height, the altitude of its mountain passes, the height of the snow-line, the distribution of animal and vegetable organisms, the existence of Alpine glaciers or of volcanie action,—points all requiring either investigation, or confirmation. So far back as 1851 and 1852, during my stay at Berlin, I acquainted Humboldt and Ritter of my intention of proceeding into the interior of Asia as far as the Tian-Shan range. They both encouraged me in my difficult enterprise, but did not conceal their doubts as to the possibility of penetrating so far into the interior of the Asiatic Continent. The result of my deliberations with these leaders of science, strengthened me in my determination of attempting to reach the eternal snow-line of the Tian-Shan at all hazards. Hum- boldt attached so much importance to the investigation, even a cursory one, of this range, that I could not look at the undertaking but in the light of a holy mission, marked out for me by the Nestor of Huropean: savans. By the end of the summer of 1856 under the auspices, and with the co-operation of the Russian Geographical Society, I was already in Vernoé. Unfortunately, however, I arrived two months after the visit of a Russian detachment to lake Issyk-Kul. With a small escort of twelve cossacks, I succeeded, on the ,9- September, in reaching the eastern extremity of the lake, and had an opportunity of surveying from point Kuké-Kul-usun, the imposing range of the Tian-Shan, from the Djirgalau to the opposite extremity of the lake. To visit the chain itself was that moment impossible. My escort being so small, I was obliged to proceed very carefully, and passed the night among inaccessible defiles, anticipating every moment to be attacked by hostile bands of Kara-Kirghizes. Returning to Vernoé, and procuring a larger escort (40 cossacks) I proceeded through the wild Biam defile, at the upper course of the Chi, and emerged on the base of the Celestial range, near the Western 124 Notes on Central Asia. [No. 3, extremity of the lake Issyk-Kul. Here I came upon numerous encampments of the hostile Sary-Bagysh tribe, who shortly before my arrival, had had a fierce engagement with a Russian detachment ; which had been sent out from Vernoé, to punish these mountaineers, for acts of violence and plunder. Notwithstanding that, I met with a hospitable reception from the Sary-Bagyshes who were comme- morating the death of many of their kinsmen who had fallen in the recent conflict, I was not able to penetrate beyond the first exposed rocky spurs of the Celestial range, nor to visit its wild defiles, being apprehensive of treachery from the revengeful mountaineers, who had lately been so severely punished by the Russians. However, in the spring of 1857, thanks to the escort kindly fur- nished me by Governor-General Hasford, who displayed great zeal and energy in furthering the organisation and exploration of the newly acquired region, I was enabled to realise all my plans. The deadly strife between the two Kara-Kirghiz tribes was then at its height, and the valleys of the Tian-Shan seemed quite inaccessible. A happy combination of circumstances, however, removed this apparently insurmountable obstacle to my journey. A rumour, that had spread with extraordinary rapidity, through almost the whole of the Mustag (the Turk name for the western portion of the Tian-Shan) of the approach of a strong Russian detach- ment, armed with terrible instruments of destruction,* for the purpose of assisting the Manap Burambai, produced a sudden panic among the Sary-Bagysh tribe, inducing them to relinquish, not only the camping grounds they had seized from the Bogus, but even their own native pasturages, from the upper course of the Djirgalan, along the whole border of Issyk-Kul, for an extent of more than 200 versts and to migrate to the upper course of the Syr-Daria (Marym). The Bogn tribe who had been previously attacked by the Bagyshes in the spring of 1857, and driven into Chinese limits, expected their complete destruction; the sudden flight of their enemies dispelled their fears and enabled them to re-occupy their former camping grounds, and * The exaggerated accounts respecting the strength of my escort were owing to my having really reached Burambaisatls accompanied by 800 horsemen; but tnese consisted of a body of Kirehizes of the Great Horde under the Sultan Tezek who had voluntarily joined my detachment. My own personal escort consisted of only 25 cossacks. 1865. | Notes on Central Asia. 125 even to reap the harvest that had been left standing in the fields by the Sary-Bagyshes. Attributing this favourable turn in their affairs to my approach, they rendered me every assistance for my journey. With such material assistance, I was able in July of 1857 to wind round Issyk-Kul from the south side and to reach the summit of the imposing and terrible Fatki-Davan mountain pass; I also sueceeded in gaining the sources of the Narym, which forms the system of the Syr-Daria or Jaxartes. Shortly after, I penetrated in a more easterly meridian, much farther into the heart of the Celestial range, and ascended one of the most elevated mountain groups of Inner Asia, that of the Tengri-Tag, which is crowned with a circle of alpine glaciers, and covered with a dazzling mantle of eternal snows. In the glaciers of the Tengri-Tag I discovered the source of the Sary-Djaza, which belongs to the system of the Tarym- gol or Erget the most remote of the considerable rivers of the Asiatic Continent. On my return to St. Petersburg in 1858, the Imperial Russian Geogra- phical Society, taking into consideration the great scarcity of asironom1_ cal points in the region I visited, organised at my recommendation, and with the co-operation of the Military Topographical Depét, a new ex- pedition, under Captain Golubef, for the purpose of determining astro- nomical points in Russian Djungaria, and on the Lake Issyk-Kul. By last accounts, Golubef had ascertained the position of three points in the valley of Issyk-Kul lake (on the Tekes river, and at the eastern and western extremities of the lake respectively), but he had not succeeded in penetratmmg into the interior of the Tian-Shan, owing to adverse circumstances, as the southern shore of the lake of Issyk-Kul was at that time occupied by the hostile Sary-Bagysh tribe; under such a state of things it would of course have been extremely rash to advance into the mountains, leaving hostile tribes in his rear. All the journeys and researches, since the year 1834, enumerated above, have considerably advanced our knowledge of the portion of Asia which we are now considering, and have removed it from the region of hypothetical speculation, to a certain basis of scientific investigation. On this account, therefore, the 2nd volume of the Russian version of Ritter’s Asia ought to be accompanied by copious and well established addenda, Unfortunately all the materials that 126 Notes on Central Asia. [No. 3, might be used for such an amplification are as yet but little digested. The travels of Fédorof, Kardin, Schrenk, my own, the observations of Golubef, the data collected and elaborated by Fakharof, have not yet appeared in print, and only short notices of them have been presented. I am consequently necessarily obliged to withhold the supplementary matter to the 2nd volume, at all events until the publication of my travels which is now delayed by all my time and attention being engaged on questions of pressing and vital importance to Russia. With regard to the 3rd volume of the Russian edition of Ritter’s Asia, containing a description of the Russian Altai, the not unim- portant materials relating to these mountains, which were collected by me on my journey, have been partly digested since my return, and Tam therefore in a position to proceed at once with the publication of this volume with its supplementary portion. I think it necessary to allude briefly in this place to some of the general results of my visits to the Celestial mountains. They embrace three questions of the utmost importance to the geography of Asia, namely the height of the snow-line in the Celestial range, the existence of alpine glaciers, and the existence of volcanic phenomena in this region. ) On the first of these points I consider it incumbent on myself to dwell at length in reply to the doubts expressed by Humboldt as to the correctness of the elevation of the snow-line in the Celestial range, as determined by me. The height I fixed it at, namely 11,000 to 11,500 feet, was ascertained by Humboldt from a letter I wrote to Ritter, which attracted his particular notice. This letter was pub- lished in the “ Zeitschrift fix Hrdkunde” with some explanatory remarks hy Humboldt. The method I adopted for ascertaining the height of the snow-line was not known to Humboldt, who grounded his supposition of an over-estimation of the elevation of the snow-line on certain theoretical and analogical considerations. Inaccuracies in the determination of the height of the snow- line may arise from two sources first from what is taken to be the snow-line, and secondly from an imperfect method of measuring heights. In the first instance the observer may be deceived either by taking dissolvable for eternal snows, or by fixing their limit of height in 1865.] Votes on Central Asia. 127 sheltered ravines or defiles which are hardly reached by the rays of the sun. Had I fallen into these errors in my determination the results-would have been to lower instead of to raise the height of the snow-line, as compared to its true limits. But these sources of error were fully anticipated and averted; my observations were made at points where regular layers of eternal snow occurred, and moreover on mountain-ridges and not in hollow depressions, in some of which I really did find eternal snows in some cases several hundred feet below the limit of 11,000. With regard to the other point, I must observe that the method of determining heights by the temperature of boiling water, is certainly one which is far from being perfect ; and leads only to approximate results ; but the inaccuracy of these results becomes more inappreci- able, the greater the height which is being measured. For inconsi- derable elevations this method of measurement cannot be adopted. I may, however, observe that the other method, namely that of commer- cial determination, can scarcely be expected to give more accurate re- sults when the conditions are unfavourable, as for instance on a journey through an extremely wild and dangerous region, where the traveller is obliged to form his own track, and stands every moment in danger of an attack; under such circumstances all simultaneous observations oi the barometer, at the base and summit of mountains, or a series of observations at any one point, are quite out of the question. Experi- ence has also shewn me the complete impossibility of keeping the barometers (I had two with me) from breaking, in a country so mountainous as that I traversed, where, on each expedition, the pack horses and camels stumbled repeatedly, and were occasionally dashed to pieces by falling over precipices. Hence travellers (Humboldt amongst the rest on his famous journey in the Andes and the Cordilleras) have invariably had recourse to the method of determining heights by the temperature of boiling water. The results obtained in this manner are regarded by science merely as approximations, until they are superseded by more accurate data, obtained when the region is more accessible to scientific exploration. Although incomplete, these results are nevertheless of undoubted value to science, as the magnitude of probable errors even under such an imperiect method, cannot exceed certain limits. 128 Notes on Central Asia. [No. 3, But Humboldt could not have taken exception to the method used in measuring the height of the snow-line, in the Tian-Shan, because he at that time did not know what means were used for this purpose, and also because he himself adopted the same method on his journey | in the New World, which was so prolific of scientific results. Hum- boldt’s doubts respecting the probability of the height of the Tian- Shan snow-line (as fixed by me), being considerable, were based on considerations of comparative geography, and their soundness or other- wise may be easily tested, for they were founded on a comparison of their height of snow-line, 11,000 to 11,500 feet, with its well ascertained limits in nearly the same meridian (in the Altai, 6,600 feet) or in the same parallel, (the Pyrennees, 8,400 feet and the Caucasus, 10,170 feet). In examining the observations made by any traveller respecting the elevatious of the snow-line, the most accurate scientific criticism must test their correctness, by the following theoretical investiga- tions. The height of the snow-line in a given range, must be calculated theoretically on the basis of a comparison with other ranges, on the same meridian, and the same parallel; the obtained results should then be compared with the figures arrived at by actual observation, and it must then be carefully considered whether the discrepancy that may occur can be at all attributed to considerations of climate, and local peculiarities. Humboldt, in his classical work ‘ Asie Centrale,” supplies us with the requisite figures for arriving at a definite conclusion. In the same meridian with the Celestial mountains we find that the height of the snow-line is as follows, In the Altai (Tigerski Belki) iat. blr Nor p aa lec ade 6,600 feet. On the Northern ee of the seen eeane range, Lat..32, North, (epee eee cece. | / LOMO OOBIEEES The Celestial mountains extend at the part visited by me, between Lat. 41° and 42° North which is consequently mid-way between the Altai and Himalayas. Taking the mean of the figures given above we shall get 11,100 feet for the height of the snow-line of the Celestial 1865.] Notes on Central Asia. 129 range. Inthe same zone, parallel with the Celestial mountains the height of the snow-line is as follows : In the Pyrennees ; (between Lat. 424° and 43° North), ... 8,400 it. On mounts Elburuz and Kazbek in the Caucasus (43° N. Ba eee re see esate: leawedeed bane all Mawel ues 10,170 ft. ni anennt) Ararat! (lat.;39% North), (22... 050. 2000 sc eieeeees es 13,300 ft. In the Rocky mountains of N. America (Lat. 43° N.)...... 11,700 ft. Humboldt, in his observations on my letter to Ritter, refers exclusively to the Pyrennees and to the Elburuz mountains. With regard to the first they cannot be taken at all into account in determining the height of the snow-line in the Celestial range, as they are situated in a moist sea atmosphere, where the snow-line must be considerably lower than in the continental climate of the interior of Asia. The Caucasus, however, supplies a better point of comparison, if treated with proper discrimination. The height of the snow-line of the Kazbek and Hlburuz occurs at 10,170 feet, under a latitude of more than 1$° to the northward that that of the Tian-Shan, and with a climate consi- derably more humid. On mount Ararat, where the surrounding atmosphere is drier, and the latitude 25° more to the south, we find that the height of the snow-line is 13,300 feet above the level of the sea. Ji a range of mountains existed between the Elburuz and mount Ararat, under climatic conditions of an imtermediate character as compared to those characterising mounts Ararat and Hlburuz, and situated under the same parallel as the Celestial range, the height of the snow-line of these mountains would be determinable at 11,300 feet. All these figures, computed theoretically by comparing the heights of the snow-line on different parallels of the same meridian with the Celestial mountains, and on different meridians of the same parallel, coincide very nearly with my determinations. The considerable elevation of the snow-line of the Celestial mountains is to be explained by the peculiarity of their geographical position, and the character of the surrounding atmosphere. It is generally admitted as a fact that a dry atmosphere has the effect of elevating the line of eternal snow very considerably. Thus for instance the snow-line on the southern slope of the Himalayas occurs at 12,180 feet, while on the northern side it rises to 15,600 feet. This anomaly is only to be accounted for by the southern side of the range being exposed to winds 18 r 130 Notes on Central Asia. [No. 3, charged with the humid vapours of the Indian Ocean, which settle on the cold mountain slopes in the form of snow, while the winds on the northern slopes of Thibet are completely free from moisture. The extraordinary dryness of the atmosphere of the Celestial mountains, compared to the Altai and Caucasus, is strikingly exemplified by the following instances. In the neighbourhood of Riddersk, in the Altai mountains, the dew falls so heavily that the horseman is completely drenched, when riding through the high grass, while in the sombre forests of the North-Western Altai, called locally Taigi, the atmos- phere is still more humid, and rain, during some summers, falls inces- santly. Now during the two years I spent in the Celestial mountains and Trans-Ili-Altati I positively saw no dew; notwithstanding that the summer of 1857 was remarkably wet, and the Altai was rendered impassable from this cause, the fall of rain was very small. In addi- tion, the very vegetation of the Tian-Shan bears evidence to the dryness of the surrounding air. While the slopes of the Caucasus are clothed with dark and impene- trable forests, which proved so troublesome in the military operations of the Russians, the wooded surfaces of the Tian-Shan are of limited extent, and rhododendrons, which are so widely spread in the moist climates of the southern slope of the Himalayas and of the Caucasus, do not grow at all in the Celestial range. Ii to this extraordinary dryness of the air in the Celestial mountains, be added the intense heating of the broad plateau by the scorching rays of the sun, accompanied by cloudless skies and a rare atmosphere, a natural explanation will then be found for the height of the snow- line being at 11,000—11,500 feet. The few measurements of heights made by other travellers in Djungaria, and moreover by other methods, serve to confirm the accuracy of my figures. Fédorof determined trigonometrically, that is by the most accurate process, the altitude of the highest point in the Tarbagatai at about 9,900 feet. The Tarbagatai range extends under Lat. 47° N. and is consequently nearer by 1° of latitude to the Tigeretski Belki, than to the Celestial range. Com- puting the elevation of the snow-line of the Tarbagatai theoretically, by a comparison of the heights in the Altai and Tian-Shan, we should obtain a result of about 8,600 feet, while in reality the true elevation is considerably greater, as throughout the Tarbagatai range the existing 1865.] Notes on Central Asia. 131 snows with the exception of two patches, are only sporadic, and the snow-line is not below 9,500 feet. This case proves that the snow- line rises rapidly from the Altai to the Tarbagatai, owing to the greater dryness of a continental atmosphere. Lastly, the barometrical observations of Schrenck, in the Djungarian Alatai, in Lat. 45° N., fixed the limits of eternal snows at 10,700 feet. Calculating then the height of the snow-line in the Tian-Shan by a comparison of that of the northern slope of the Himalayan, and of the Tarbagatai ranges, we obtain 11,700 feet and 11,950 feet, if we take in the Djungarian Alatat. In this manner all the facts of the case, not alone those supplied us by comparative geography and climatology, but likewise those derived from the exact observations of other travellers, tend to confirm my figures, and prove them to be rather understated than magnified ; Humboldt’s doubts therefore as to the possibility of the snow-line of the Tian-Shan exceeding 11,000 feet elevation, are disposed of not only on theoretical considerations, but also by ocular demonstration. The interesting questions relating to the existence of fine alpine glaciers in the Tian-Shan, which is in intimate connection with that of the height of the snow-line, I solved in complete accordance with the previously expressed opinions of Humboldt and Ritter. I set out without any foregone conclusions on this point, but having experienced the remarkable dryness of the air in the Tian-Shan mountains, and having ascertained, on ascending the Fatiku Davan, that the height of the snow-line was higher than 11,000 feet, involuntary doubts entered my mind as to the possibility of the existence of real glaciers in the Tian-Shan. These doubts were, however, soon dispelled. At the sources of the river system of the Sary-Djaza, I came across five magnificent alpine glaciers and a “‘ Mer de glace” exceeding in size that of Chamounix. Notwithstanding some of the peculiarities of the Tian-Shan glaciers, owing principally to their prevalence at not more than about 2,500 feet below the limit of the snow-line, while in Switzerland they descend as low as 5,000 feet, their existence in the form anticipated by Ritter and Humboldt, on the strength of Chinese accounts, was fully confirmed. It now remained for me to prove, by actual observation on the spot, the existence or otherwise of volcanic phenomena in Djungaria, and 132 Notes on Central Asia. [No. 3, in the Celestial mountains, to which Humboldt in his works so often alludes. I started on my journey firmly persuaded that I should find the conjectured volcanoes, or at all events some volcanic forms, and I sought diligently (as Schrenck did on lake Ala-kul) to establish the correctness of Humboldt’s surmises, with respect to the existence of volcanic phenomena in Central Asia, by which confirmation I knew a traveller would gain greater credit than by an incomplete refutation of the hypothesis. I was even aware that Humboldt was rather displeased with the researches of Schrenk who clearly showed that the island of Aral-Ttibe on lake Ala-kul was not of volcanic origin. The opinions entertained by Humboldt on the subject of the existence of voleanoes in Djungaria were favourite ones with him, and I regret that I was not able to confirm his cherished theory. Kullok peak, another of Humboldt’s mistaken volcanoes, was found to have no volcanic origin whatever. The hot springs, and the non-congelation of the waters of lake Issyk-Kul, were not accompanied by any voleanie forms in the Tian-Shan, and furthermore all the native accounts of phenomena which from their descriptions might be supposed to be volcanic, proved unfounded, and were at once disposed of on my examination of the localities where they were declared to occur. The result therefore of my researches on this point was that I became convinced of the complete absence of volcanoes, distinct volcanic phenomena, or even volcanic forms throughout the Celestial mountains. It is true that there existed in Djungaria at one period some “ Solfaters” or smoking cavities from which there was a discharge and deposit of sulphur, and that some of these fissures, out of which the Chinese obtain sulphur, emit smoke even at the present day. But a careful inspection of one of the extinguished pits satisfied me, that at all events in that case, there was no volcanic affinity. In the neighbourhood of the pits which I discovered in the Katt mountains, and in the Ili valley, I could trace no volcanic forms, but ironstone occurred, and owed its formation, as far as I could judge, to the pyrites that were widely spread in the vicinity; there was at the same time a discharge of sulphur emitted in the form of vapour out of numerous fissures and which left a deposit on the sides. It is to be taken into consideration that I found a coal formation largely developed throughout the Ti basin, and that coal is obtained by the Chinese in 1865.] Notes on Central Asia. 1383 the neighbourhood of Kuldja, in large quantities, from very deep seams. The whole process of the formation of sulphur can then in my opinion be reasonably explained by the combustion of some coal seams in this basin, which would at once set at rest the question of supposed volcanic agency. I cannot positively affirm that the origin of the other smoking pits of Djungaria, and particularly Humboldt’s famous ‘ Solfater’’ of Urumchi, is susceptible of the same explanation, although the analogy between all the Djungarian “ Solfaters’’ would appear to be confirmed, native accounts excepted, by the circumstance that the Chinese, who are very expert in recognising such sulphur formations, procure sulphur from the “‘ Solfaters” of Katt which I visited. With still less certainty can I deny the existence of volcanic pheno- mena or volcanic forms farther eastwards in the Celestial mountains. Humboldt in his observations on the letter I addressed to Ritter, which was published in the “ Zeitschrift fir Erdkunde”’ says that the Sangai, rising in the centre of the Ando-Cordilleras range, the most active of all the volcanoes in the world, forms around itself an island of trachyte, not more than two geographical miles in diameter. From this I must of course conclude that the observation of a single portion of the Tian-Shan visited by me cannot serve as a positive evidence of the absence of volcanoes and volcanic forms in other parts of this mountain system. My conclusions on this question generally have already been made public, in the letter here referred to, but I must likewise observe in addition, that all Asiatic accounts of phenomena which might be volcanic in appearance, should be treated by men of science with great circumspection, as many of these accounts have already proved fallacious. I would here also remark that the impres- sion produced on me personally by Djungaria and the Tian-Shan leaves great doubts in my mind as to the existence of volcanoes in this part of Asia, and as I am the only traveller who has visited the Tian-Shan, I cannot accept the belief in their existence, as an axiom requiring no proof or confirmation. My conclusion on this point, though negative, is one of the most important results of my journey. Ii, in aspiring after the truth, I have been compelled to express opinions on two points of such vast importance to the geography of 134 Notes on Central Asia. [No. 3, Asia, which differ completely from those entertained by Humboldt ; whose faith in the existence of volcanoes in the Celestial mountains was as firm as that of Columbus in the existence of the New World, it does not necessarily follow that I cast a shade (in itself impossible) on the spirit of the great scientific genius of the age. Science is the eternal aspiration of the whole human race towards truth, and truth can only be grasped at out of a multitude of errors and misconceptions. No one moreover is more liable to fall into such errors than the pioneers of thought, who marshal their fellow creatures to the great goal of truth, and call into existence words of new thoughts and conceptions. These giant minds are followed by a train of disciples, for whom the path of investigation, and the final solution of great scientific problems, is rendered comparatively easy. Thus there are the men of genius in science, or the master minds, who conceive great thoughts, and the workmen who follow up such of these thoughts as are sus- ceptible of elaboration. Hach has his separate functions, but on the most humble labourer in the field of science devolves the sacred duty of pointing out and rectifying any error into which the eminent master may have fallen. And in such a case, the obscure advocate of truth should not be crushed by all the height and authority of genius, science being a problem open to solution to all humanity, and recognising no individuality or oligarchical superiority. The science of geography has lately been deprived of two of its most brilliant leaders— Humboldt and Ritter. To follow in their footsteps, to extend the circle of their researches, to strive after that eternal truth which they eagerly sought during their mortal careers, to correct the few errors which are inter- spersed through the wide field of their enquiries, these are the duties of every votary of science, even of the most humble grade, and will serve as the best testimony of admiration and respect to our great masters. May the present effort be taken as such an expression, and as one of the many proofs, that dying, Humboldt and Ritter have bequeathed to humanity a living record of their great genius. OO aaa 1865. ] Notes of a trip up the Salween. 135 Notes of a trip up the Salween—By Rev. C. Parisu. [Received 39th June, 1865.] In March last, as I had never travelled on the Martaban side of the Salween, and as I had been promised by Captain Harrison, the Deputy Commissioner of Shway-gyeen, that, if I would pay him a visit, he would accompany me through the Fir forests of the Yoonzalin, which I have long wished to see; I availed myself of a month’s privilege leave to take a trip northwards. Col. Fytche was going, at the same time, on his official tour to Shway-gyeen. His company was an additional inducement to go in that direction. The road to Shway-gyeen lies through Beling and Sittoung, and affords good riding ground all the way in the dry season, as it keeps to the plain, leaving the mountains on the right hand, that is, on the east. These mountains, which, N. HE. of Shway-gyeen, cover a great breadth of country, divide themselves towards the south into two narrow ranges, one of which separates the Yoonzalin and Salween rivers, terminating at their point of confluence: the other and longer range terminates at Martaban, and is the watershed between the Sittoung and Beling rivers on the west, and the lower Salween on the east. Westward of the latter range stretches a vast plain; and it is along this plain, parallel with the mountains, though at some little distance from them, that the road from Martaban to Shway-gyeen lies. While at Beling, on the way, I rode out in company with Ool. Fytche and Capt. Harrison to a place called Kothanaiong, about 7 miles off, to see the Amherstia trees there. This place had often been mentioned as one where the Amherstia was to be seen in great perfection, and where, indeed, it might perhaps he wild. I was well rewarded, for a prettier little spot I never visited. The Amherstias, growing in a well-shaded place and watered by a perennial stream which tumbles down a steep granite hill, and is ingeniously directed hither and thither in large bamboo troughs, were, indeed, to be seen in the wildest luxuriance of growth. But Kothanaiong is a sacred spot. Here are Pagodas, Pongyee-houses, Zayats all around, A flight of stone steps leads from the bottom to the top of the overhanging 136 Notes of « trip up the Salween. [No. 3, hill, which is about 600 feet high, and on which are more sacred buildings. The Amherstias, seen only round the principal Pagoda, were undoubtedly planted, although they are left now to take care of themselves, and have a wild appearance. Evidently, this is not a native habitat of the tree. From Beling we went on to a place called Kyik-hto. Hastward of this place and distant about 14 miles, is a remarkable mountain, called Kyik-hteo. Capt. Harrison, one of the very few Huropeans who had been there, assured me that it was well worth a visit, as there was, on the summit, a very singular hanging rock, surmounted. by a Pagoda. We went accordingly, riding the 14 miles to the foot of the mountain in the morning, and walking up it in the middle of the day. We reached the top 3,650 feet at 3.30 ep. m. The view from the sumunit is very fine, as all views from great heights are; but the many granite boulders which are scattered about, some of them perched and balanced in the strangest manner on the most prominent peaks, constitute the most remarkable feature of this mountain. On all the most striking of these boulders small Pagodas have been built; in several instances, I should say, at the extreme risk of life to the builders. As the only way of conveying a true idea of the appearance of these rocks, I send a rough sketch of two or three of them. There are two principal ones.—The one at the very summit is called Kyik-hteo ‘par excellence ;” the other, some little way down the hill is, Kyik-hteo galay, or, “ little Kyik-hteo.’” We could not ascertain for certain what their names signify, further than that “ Kyik” is “rock” or “ mountain-peak.” I have observed that the Burmese never know the weaning of the names which the mountains and prominent rocks in the country bear; the names being older than the Burman occupation of it. They are, I believe, generally Valaing, but sometimes Karen. The chief rock of all, which gives the name to the mountain, is simply a wonder. It is a huge rounded granite boulder perched on a projecting and shelving tabular rock at the very summit. This tabular rock is itself reached by a small foot-bridge, for it is separated by several feet from the mountain by a rent or chasm; and on the farther side it drops down perpendicularly, I do not know how many hundred feet, into a valley below. On the extreme verge of this flat sloping rock-table, and actually over- 1865.] Notes of a trip up the Salween. 137 hanging it by nearly half, is perched this wonderful boulder, which is about 30 feet high, and is surmounted by a small Pagoda about 15 feet high. A rude bamboo ladder is leant against it on the inside, which enables an adventurous person to ascend. Every native will do this, but we, being both heavier and more awkward, preferred to remain at the bottom. Viewed on one side, it is difficult to understand why this rock does not slide off its shelving support into the valley below! As one looks at it, it appears as if, assisted with a little grease and a slight push, it must go! But there it hangs, as it had hung, and I suppose, will hang yet,—one might indeed almost say, there it s/zdes and will s/zde,—for many an age : “Labitur et labetur in omne volubilis evum;’ unless some earth- quake (and a very slight one surely would do it) should rudely shake it from its precarious foundation. This place is annually visited for the purpose of worship by people from all parts of the country round ; many, I am informed, going to it even from Moulmein. Many were already there, and very many more shortly expected, as was shewn by the temporary booths of grass which had been erected, and were calculated to hold several thousand people. Altogether, this is a remarkable place, very little known, and well worthy oi the trouble of visiting it from a long distance. I was disappointed, however, here, in a botanical point of view. I expected great things from a high mountain in a totally new part of the country; but I gathered scarcely anything. There were no Orchids at all. The Ferns, if any, were dried up; one or two new Acanthaceous plants alone rewarded my search. At this season the mountain is arid, and vegetation on it scanty. On the top there is little else besides long grass. We passed the night on the top; and descended on the opposite, or north side the next morning. Our ponies had been sent round, and were found waiting for us at the appointed place; and a ride of 18 miles brought us by evening into Sittoung. From Sittoung to Shway- eyeen the distance is about 40 miles. After two or three days spent at Shway-gyeen in making preparation, Capt. Harrison and I started upon our walking trip to the Yoonzalin district. The Yoonzalin river is a tributary of the Salween and takes its rise in (about) Lat. 18° 30’ and flows in a very tortuous course, but in 19 138 Notes of a trip up the Salween. [No. 3, a general southerly direction until it joins the Salween at Kankareet, a little below the Hat-gyee. It draims a very mountainous district, and during the rainy season, rolls down a considerable body of water, but during the dry weather, it is a shallow rocky stream, full of rapids and scours. It takes small boats 15 or 20 days to ascend from Kankareet to Pahpoon, about two-thirds of its course. It took us 5 days to descend that distance. The valley of the Yoonzalin is an extremely wild and almost uninhabited district. All the way from Bangatah in the valley of the Sittoung to Panpoon we did not meet with a single village. The Karens, the only inhabitants, are very few and scattered ; and they have been so harried during the last few years, by the incursions of the Shan Pretender who styled himself Aing-lowng, on the one side ; and by us, in our attempts to drive him out, on the other, that they have hidden themselves away in the most inaccessible places. Occa- sionally only we saw a stray house or two perched up on the top of some distant mountain, or on its almost perpendicular side, with no visible way of approach from the spot where we stood. When the inhabitants become reassured and gain confidence in the permanency of peace, they will no doubt increase, and settle down in more accessible places. IT will not attempt any description of the scenery of this district, because mountain scenery in one place is very like mountain scenery in another place; and because I have rarely found that attempted descriptions of the kind convey any definite picture to the mind.. All that needs be said is, that it was extremely wild and beautiful, and afforded all that endless variety of view which a chaos of mountains rudely thrown together, might be expected to afford. Neither shall I give the length of the stages which we performed, nor the names of the places where we halted ; for these places were not villages, only well imown spots conveniently chosen for the purpose, as combining the advantages of level ground and water. And the stages, if measured by miles, might appear small; though measured by labour, by no means so. A more laborious, at the same time thoroughly enjoyable, walking tour I never took. It is ceaseless ascent and descent, to the extent of several thousand feet a day, all the way. There are two words in Burmese for hill: Towng, and Kon. A Toung, hereabouts, is 1865.] Notes of a trip up the Salween: 139 a good stiff hill, in fact, a regular mountain. The word Kon seemed to be applied to any thing under 1000 feet. Two or three Kons go for nothing, no account is taken of them in the prospective march; if you should ask what it is like. After two or three days, one learnt oneself to despise a mound of 1000 feet. In this sort of travelling; one counts hours not miles; and, beginning to walk at 5.30 or6 a. M., a man has generally had enough of it by 11 or 12 o’clock, and rejoices to hear that the “tszkan” or halting-place is near at hand. And this is the country through which some enterprising person has, T believe, proposed to make a Railroad to China ! The extremely low temperature of the upper part of the: Yoonzalin district is remarkable. Immediately you get in among the moun- tains, even before crossing the watershed which divides the Sittoung and Yoonzalin, it becomes very much colder. It was the beginning of March; yet, at a place called Thayet-penkindat, on the west of the watershed, the nights and mornings were uncomfortably cold, and: the water in the stream excessively so. Before reaching this place, an elevation of at least 4,000 feet, has to be made from. Bangatah. Thayet-penkindat is the name given to a stockade which we have placed here. It is beautifully situated at the head of a fine valley, and is 2206. feet above the sea, and closely surrounded by mountains 2000 or 3000 feet higher. The stockade is guarded by a Police force, and the site appears tobe well chosen, as it is situated at the entrance of the Pass into this part of the Yoonzalin. This Pass is called: Kyouk- taga or Rock-gate, and is a narrow defile, two or three miles long, The head of this pass is 3343 feet above the sea.* A small stream runs through it, and the vegetation consequently is very rank. I was told that I should probably find some new ferns here, but though. there were many species, there was nothing which I had not seen before. Near the head of the pass, however, I discovered a new species of Bulbophyllum, and one or two other orchids. Through this pass, we were in the Yoonzalin district, and, to my great delight, thenext day, among the Hirtrees. The sight and the fragrance of a Fir forest to me, who had not seen one for a long time, was most refreshing. The trees are all of one kind, Pinus longifolia; * The heights given have been furnished by Col. Blake, and are from his own measurements by an aneroid. 140 Notes of a trip up the Salween, [No. 3, and cover the mountains from top to bottom. In many places it is the only tree visible. It attains a considerable height, 80 to 100 feet, and are, (the full grown ones) 8 to 9 feet in girth. The temperature of the tract or belt of country where the Fir grows, as I said just now, is extremely low. In the month of January, Capt. Harrison informs me, (for he had been here in that month) there is hoar frost, and a thin covering of ice forms on a basin of water by the morning. Even in March we found the nights and mornings so cold, that we were glad of thick over-coats and a blazing fire of Pine logs. At 11 and 12 o'clock in the day, and while walking in the sun, the heat was not unpleasant. The vegetation gave indications of low temperature. I gathered violets in the valleys. Rubus was met with ; and instead of the Acanthacee and Zingiberacee, which cover the hills to the south but which were not seen here at all, Composite (among them a large Carduus) abounded ; many of them attaining to the dimension of large shrubs. The Composite, however, were not confined to the Fir tract. Of Epiphytic Orchidee, there were none: though I dare say that, in the rainy season, the terrestrial kinds would be numerous. As the forests were dry, ferns were scarce, though I was gratified at finding that singular little tree fern “ Brainea imsignis” in large quantities. IT had never met with it before. I gathered also Adiantum flabellulatum and Lindswa tenwifolia. Immediately we crossed the watershed to the eastward, though still among the mountains, the Fir trees ceased, and it became very hot ; and so it continued when we turned southward and crossed again into. the Yoonzalin valley. It is only in the upper Yoonzalin. that the tem- perature is so remarkably low, and that the Fir forests exist. Strange, however, to say, the Fir reappears in the Tenasserim provinces at Myawaddee, on the Thoung-yeen, some 50. miles due east of Moulmein, and thence stretches southwards for several miles, as I have myself seen. The tree there does not form forests, but is sparsely scattered among other trees; nor does it grow so large. But, and this is most *emarkable, in the Thoung-yeen valley, it is found on hills only about 1000 or 1500 feet high, and descends nearly to the river; therefore in many places, cannot be more than 300 or 400 feet. above the level of the sea; and this in N. Lat. 16.°! Shortly after passing out of the Fir forests I was delighted to come 1865.] Notes of a trip up the Salween. 141 upon a truly splendid Bauhinia, which I discovered for the first time last year in the Thoung-yeen valley. Then, however, I met with but one tree—here now I found many, and all in flower. The flowers are very large, about 4 inches in diameter, of the purest white, save the single coloured petal which is streaked with purple and gold. It far surpasses B. Richardiana in beauty, for the petals of that plant are very narrow, consequently the flower looks poor, whereas, those of the species I am describing, are broad and meet at their margins, and this adds immensely to its beauty. The flowers also are of the sweetest fragrance, and are produced in profuse abundance all over the tree. I hope to get seedsof it. I left particular instructions with the head- man of that part of the district, to gather some when ripe and forward them to Capt. Harrison, who kindly promised to remember me in the matter. The most northerly point to which we went was Kanlado, another police station, and our frontier out-post. It is but some 15 miles from our boundary on the North, and not far from the Salween. There is a strong block-house here besides a stockade. It is situated on the top of a small cleared hill, and 1881 feet above the sea; it is surrounded on all sides by higher hills. This is the lively abode of the officer who has the honour of serving Her Majesty in the capacity of Assistant Commissioner of the Yoonzalin district. He, at least, if no one else, will rejoice at the completion of the projected Railway ; but he is likely to be the only passenger ! The vegetation of the hills round Kanlado is very different from that which is seen in the Tenasserim Provinces. The forests consist almost wholly of what the Burmese call Hngyen a species of Shorea, a middle-sized tree, at this season of the year in flower and without a leaf. The forests consequently have a bare wintry look, a condition of jungle never seen in the Tenasserim Provinces, where the whole country is densely green throughout the year. There are, of course, a few other trees mixed with the Shorea, such as Careya, Dillenia, Hugema, and Anneslea fragrans ; but not in sufficient quantities to alter the character of the jungle which is given by the prevailing Shorea. Orchids grow sparingly on the trees here, but some good kinds; Dendrobium Dalhousianum, formosum, and eburneum. The only other locality known for the last plant is the valley of the Shoung- 142 Notes of a trip wp the Salween. [No. 8, yeen. Besides these, I collected two or three other species familiar to me, but not yet described or named. There was nothing absolutely new to me here; indeed, the whole expedition only yielded two new Orchidex ; the Bulbophyllum already mentioned as found in the Kyouk-taga ; and a Dendrobiwm with the flowers of D. aggregatum,. but with short, erect cylindrical pseudo-bulbs. From Kanlado, after a day’s halt, we bent our steps southwards and homewards ; as my limited time would not allow me to go further, not even to visit the banks of the Salween which is within an easy day’s march of Kanlado on the east. About half way between Kanlado and Pahpoon, we turned aside from our path to visit a water- fall on the Yoonzalin river. I had often noticed on a map made by a local surveyor, professing to be a map of this district, high up on this river, the words, “‘ Waterfall, 400 feet ;” but I could never find any one who had seen the waterfall. Now, a waterfall of 400 feet is a very unusual feature in the scenery of any country and a grand sight ; and I had long formed a secret resolution to find out this waterfall some day, and verify the statement as to its height. We were now at the very part of the country whence, if visited at all, it must be visited. I determined, therefore, not to return home without seeing it. Capt. Harrison, happily, was of the same mind; so, notwith- standing the assurance of the natives that the place was very difficult of access, and the mountain side very steep and slippery, we sent on a party in advance to find out a way forus and toclear the jungle sufficient- ly to make it passable. Arrived at the point of our road whence it was necessary to diverge from it to go in search of the waterfall, we struck off, and had certainly as hard a morning’s work before we reached the object of our search, as any man could desire: but we reached it about noon, and that was enough. On arrival we were at once gratified and disappointed : gratified at finding ourselves in a most romantic spot, and at the preparation made for us: disappointed at seeing no waterfall, although we were told that all that was to be seen lay before us. We had come prepared to rough it and sleep on the ground ; we were, therefore, agreeably surprised at finding a very capacious and exceedingly pretty structure built, and all ready for us. The site was selected with great taste, for on stepping up out of the thick jungle 1865.] Notes of a trip up the Salween. 143 by a small ladder on to our house, and on going to the front of a broad baleony or verandah ornamented with a balustrade, the whole made of bamboo, we found that the boughs of the trees had been cut away in front, and that we stood over a large circular pool of water into which the Yoonzalin poured itself on one side, and out of which it flowed on the other, and we had the best view that it was possible to have. We were in a perfect punch-bowl, shut in by almost perpen- dicular mountains on all sides. Before us lay the still pool, 60 feet deep and about 150 yards across: we heard the roar of the water rushing in and rushing out, but, so hemmed in with rocks is the spot that we could neither see the course of the river above or below. As I said, we were charmed with the place, but where was the waterfall of 400 feet? The reply was, that this was the “ Yaytagon” (so the Burmese call a waterfall) and that there was nothing more to be seen than this! A raft of bamboos was made for us, and on it we went close up to the ‘ ‘embouchure” of the stream, the mouth of the passage through which the water from above pours into the pool. It was a singular sight. The whole of the waters of the Yoonzalin at this point are poured through a long, straight, and very narrow street of rock. The passage, or street as I call it, through the rock is perfectly straight, about 14 feet wide only, and having exactly the same width throughout its whole length, which is about 20 or 80 yards. The rock, granite, rises on either side of this passage to the height, in the centre, of about 50 feet in perpendicular walls with smooth faces, as straight and smooth as if measured with a plumb line, and cut with a hay- knife. As the water enters the upper end of this passage at a right angle, we could see no more of the river than the length of the passage, but we could hear the roar of the water as it boiled and bubbled in its tortuous and bouldered channel above. But though lashed into foam above, so smooth and polished is the narrow passage that the water glides through it with a surface like glass, and sinks at ounce to the bottom of the pool, causing little or no commotion init. I climbed to the top of the overhanging rock on one side to get a sight of the river above, but it takes so many short and sudden turns and the gorge in the mountains is so narrow, that I could see but a few yards upwards. Thinking that we had seen all that was to be seen, and having already spent a day and a half here, we determined to set out 144 Notes of a trip up the Salween. [No. 3, on our return the next morning; but towards evening, some of our party, who had been exploring, came and informed us that they had discovered a way to get up the rocks on the opposite side, and that having ascended that way they had come upon a waterfall. As we wished not to leave the plaee without being able to speak positively on the subject of the fall, and thinking that there might yet be one higher up the stream but hid from our view, we resolved to stop another day, and explore on the morrow. We did so, and climbed the way pointed out to us; and thus, taking the passage before mentioned in the rear, we got a good view of the river for a mile or so above it. As far asthe eye could see, the course of the river lay through an extremely narrow valley and was impeded the whole way by huge granite boulders. The fall of level also was considerable ; and near the spot where we stood, it took a sudden perpendicular leap of some 30 feet, into a deep and very confined square hole, which at once turned the water at a right angle, whence it rushed on, and after 2 or 3 similar sharp turns within the length of a hundred yards, dashed through the beforementioned passage into the pool. We had now seen all certainly and could positively assert that the greatest perpen- dicular fall the Yoonzalin makes here, is not more than 30 feet. Though disappointed of a grand sight, we yet considered ourselves well repaid for our toil by the general beauty of the spot and by the very remarkable character of that natural feature in the scenery which I have attempted to describe; the narrow street with perpendicular walls through which the whole river, as well when at its height in the rainy season, as in dry weather, has to make its way. Several_persons have thought that Pine logs might, in the rains, be floated down this river to Moulmein: but no one who had visited the Yay-tagon would allow it to be possible. No log could, I am convinced, pass this part of the river’s course without being broken to pieces. It is unfortunate that all the Pine forests should be above the fall. There was one drawback to our full enjoyment at this place. There is a pest here in the shape of a very small fly, met with happily no where else, which attacks every exposed part of the body most viru- lently. Its puncture immediately raises a blood pustule and causes considerable irritation for several days afterwards. I could scarcely sketch for these tormentors; and when we bathed, especially, their 1865.] Notes of a trip up the Salween. 145 attacks were so vigorous, that we wasted no unnecessary time in putting off and in resuming our garments. On the third day after our arrival we started for ‘‘ Pahpoon.” It was not far from “ Pahpoon”’ that, for the first time in the whole journey, we heard the cry of the Gibbon. Its cry was totally different from that of the Gibbon of the Tenasserim Provinces. The latter is a wailing, plaintive, and, to me, not disagreeable cry: but the cries of the Gibbon here were most discordant, and not unlike that of a pack of jackals. They can hardly be the same species. From Pahpoon, an obscure village on the Yoonzalin, we dropped down to Moulmein in boats. Onthe second day after leaving Pahpoon I noticed unexpectedly on the bank of the river, in one of the wildest spots, a fine Amherstza in full flower, about 30 feet high. I saw but one; for it was the middle of the day and hot; I had been, therefore lying down in the boat under cover, heedless of what I passed. I looked out of the boat casually, and saw this tree; so there may have been others which I did not see, both on the bank and in the adjacent jungle. I am sorry to say that my companion Capt. Harrison was a long way behind in another boat, so that I could not point it out to him; and he did not notice it, because, not caring for the character of the vegetation, he did not look out from his boat at all. Now, my reasons for saying that this was a bona fide wild tree are these: in all this district, the valley of the Yoonzalin,—there are no Pagodas or Pon-gyee houses, or spots sacred to the Burmese where they have erected buildings. The inhabitants of the district, in fact, are Karens and not Burmese; and these Karens are exceedingly few and scattered. After leaving Pahpoon, we did not see a single village on the banks all the way until we came to the junction of the Yoonza- lin with the Salween. There are, indeed, no doubt, a few villages a little way from the bank, here and there hidden among the trees, but these generally consist of but 2 or 3 houses: neither are they settled villages, for the custom of the Karens is to change the site of their houses continually. Besides the regular Karens, not being Buddhists, do not build Pagodas, nor do they ever trouble themselves to plant ornamental trees, as the Burmese always do. in their sacred places. Besides, the spot where this Amherstia was seen, was not at all a likely place for an Amherstia to have been planted by any one; but 20 146 Notes of a trip up the Salween. [No. 3, one of the wildest places imaginable. Had it been on & rismg ground on a high bank alone, or on any prominent point on the river, 1 should have suspected that a hand had planted it : but it was on a low and sloping part of the bank, struggling for life with Calamus, Bauwhi- nia and tall grasses and such other tangled stuff as forms the common vegetation of our river banks in the wildest places; and behind again was dense jungle of the tallest trees. However, notwithstanding alk this, had it been seen in a fairly peopled district, I should have doubted; but in such a wild uninhabited country as the Yoonzalin is, LE see no reason for suspecting that it was not a genuine native.” Had Wallich’s first tree been here, I am satisfied that the idea of its not bemg wild would never for a moment have occurred to him. If am perfectly satisfied that the tree seen by me was a wild one. That the Amherstia in a wild state may be very scarce is not improbable, but that it should not exist any longer in that state, though possible, is, to say the least, very unlikely. Probably it is confined to a small area; and I am inclined to think still, as I always have thought, that its habitat is the banks of the Salween, and of the Yoonzalin, which runs nearly parallel with the Salween in about the latitude where I suppose it grows. Very. few Europeans, who would care to notice the vegetation of the country, have ascended either the Yoonzalin, or the Salween above the Great Rapid, that is to say, have been conti- nuously along its banks, so that a rare tree may, mot improbably, exist there, although it has not been seen on the latter river at all, nor on the former, except by myself, as I have described. I append a rough but tolerably accurate map of the country, * The Amherstia has never been found wild before. Wallich discovered it, i. e. first saw it, at a place called Pagdt, some twenty or thirty miles up the Salween. The trees which he savy are still there, at least some of them, and, are manifestly planted trees, being near an artificial tank, at the entrance to some sacred caves, I have long had an idea that the native habitat of the Amherstia would be, found to be somewhere high up the Salween, This is not at all unlikely, be- cause very little, indeed almost nothing, is known of the banks of this river: above the Hat-gyee, or Great Rapid, which is about 100 miles up the river. COLD ALLL PIP LLL LLDPE Journal As: Soc. Bengal: Vol: XXXIV PartII Plate V. p jeToungoo MAP ILLUSTRATING M® PARISHES NOTES OF A TRIP UP THE SALWEEN )) Zpah-Chioung ( Feundery (5: way -goore ‘ é Journ. As. Soc. Bengal. ; as Vol_ XXXIV. Part. I. Pl. 6- On stone by Kristohurry Doss. Sketched by C. Parish. BOULDER TEMPLE AT KYIK-HTEO Journal As. Soc. B emma) As. Soc. Bengal. Vol. XXXIV. Part). Pl. Skelched hy C. Parish. On stone by Kristohw KYIK-HTEO-GALAY BOULDER PAGODA. LITH) BY Hof SMITH. S.G.0.CALCUTSA. 307 1kes. a Iogrn al As: Soe ourmal Ax: Soc Sketched hy C Parish. KYIK-HTEO BOULDER. PAGODA. LTH ORY Hoot SMITH, 5.6.0, CALCUEER OFF. Nes fh Vol XXXIV. Part Tl, P} On stone by Kristohurry De 1865. ] Ox the Boksas of Bijnow'. 147 Notes of Observations on the Boksas of the Bijnouwr District —By Dr. J. Ya. Stuwaret. [Received 10th January, 1865. | Travellers in Central America tell us that the phrase quien sabe (“ who knows?) stops them at every step, when they seek to inquire into the past history of the natives, and some analogous expression is probably in frequent use, in similar circumstances, among all barbarous or hali-civilized races who have no literature. In this country gwen sabe is fully represented by khabar nahin and Khuda jdne, and of these I have had much more than was pleasant, in trying to discover some- thing of the past history of the Boksas of the Bijnour district. My attention was first directed to the existence and peculiarities of these peo- ple, while making some investigations as to the food of the inhabitants of the district, and various circumstances subsequently led me to be some- what curious about them. And altheugh I have miserably failed in making out anything definite as to whence the Boksas came or from whom they sprung, a few facts have been elicited regarding the habits, mode of life and health of these who inhabit the Bijnour Forest and the Patli Doon, which may have some interest as relating to a section of this tribe, the last of which, it seems not unlikely, will be seen by a few more generations. This information was only acquired by a good deal of patient digging among these Boksas themselves, during several weeks of the cold season of 1862-63 when I visited a considerable number of their villages, and conversed with many of their inhabitants, including some of the most intelligent headmen among them. No detailed description of the Boksas, or of any section of them, has hitherto been published, but there are many scattered notices of those who inhabit the eastern portion of the Rohilkhund forests, in the reports and papers of Traill, Batten, Jones and Madden; and Sir H. M. Elliot, in his supplement to the Glossary, gives some interesting traditions as to their origin. Frequent reference will be made to these notices hereafter, but, meantime, a few general facts gleaned from these and other sources may be given regarding the distri- bution and characteristics of the eastern Boksas. Since our occupation of 148 On the Boksas of Bijnour. [No. 3, Rohilkhund they would appear not to have extended in any numbers to the eastward of Kilpoory, beyond which the Tharoos, a similar race begin to prevail, and their chief settlements were near Guddurpoor and Roodurpoor. On the rearrangement of the canal system of that part of the Rohilkhund Tarai, the Boksas were concentrated to the north of Guddurpoor, where their settlement is now known by the name of Boksdr. Nearly 300 years ago this term was applied to a tract a little further to the eastward, in which, at that time, probably the greater number of the tribe resided. Captain Jones, about 1845, gave the number of inhabitants of (the present) Boksér as 2,293, and I have no information, subsequent to that date, shewing what proportion of the Boksas of the neighbourhood may still inhabit scattered villages. The Boksas inhabiting the forest to the east of the Ramgunga, who are called by those of Bijnour Paurbid Boksas, and sometimes Khalsé, ave described as mild, inoffensive and truthful, but indolent, fickle and unthrifty, and extremely ignorant; and, ere they were taken in hand by British officers, they are said to have been kept in grinding poverty by the usurers and their own Pudhdn. They are stated also to have shewn an invincible disinclination to settle down for more than two years on one spot, yet never to emigrate outside of the Forest and Tarai, to be excessively partial to the flesh of game, especially wild pigs, and to exhibit a “‘ wonderful immunity from the effects of malaria.” The Tharoos or Tharwi above alluded to, present many points of resemblance to the Boksas, though neither will acknowledge any connection with the other. But the former cover a much greater extent of country than the latter, as from the point a little west of the Sardah where the two tribes dovetail, the settlements of the Tharoos stretch eastward through the forests of northern Oudh and Goruckpore to the river Gunduck. I can find no evidence that on the east the Tharoos meet the Meches, who are called by Dr. Hooker ‘“ decidedly Indo-Chinese,” and who occupy a similar position abreast of Darjecling, to that held by Tharoos and Boksas to the west, and to whom they appear to possess a considerable resemblance. The fact of different segments of the Sub-Siwalik forest being \ 1865. ] On the Boksas of Bujnour. 149 inhabited by three tribes which acknowledge no relationship, and which, at the same time, have many peculiarities in common, is deserv- ing of more attention than it appears to have hitherto attracted. To the westward of the Ganges, there are some Boksa villages inside the Siwaliks, in the Dehra Doon, but I can discover nothing certain regarding their numbers, nor as to whether any of the tribe inhabit the forest outside the Siwaliks in the Saharunpore district. These western Boksas are called by those of Bijnour, Mehras or Meri, and are acknowledged by them as in every respect of the same caste with themselves. But isolated statements by ‘members of such ignorant tribes can hardly be accepted without check, for the Patli Doon Boksas repudiated all bardddré with the Merz, as well as with the Purbid, whom they asserted to be nothing but Tharwi, and to eat frogs and lizards. We need not, however, suppose ther ignorance to be strikingly exceptional, for, at an early period of my inquiries, I was informed, upon what would ordinarily be called “good authority” in the Bijnour district, that the Boksas were chiefly remarkable for living in houses built on poles, for the indifference of their women to decent clothing, and for mainly earning a livelihood by gold-washing. As will be seen by and bye, there is some little truth in the last state- ment, while the two first are baseless. But this is beaten by the characteristics attributed to the Boksas of Dehra Doon by the other inhabitants of the district, who say that the former are famous for dealings in witchcraft, for successful treatment of insanity and syphilis, and for their pot-bellies, all which peculiarities probably originate in the imagination of the narrators. The number of inhabited Boksa villages in the Bijnour district outside the Siwaéliks, including two in the Patli Doon within the outer hills, is fifteen, of which the thirteen outside are pretty equally distributed over the Forest, but are rather more numerous towards its western end. Of these, four are situated near the base of the Siwaliks on the inner edge of the Forest, five on canals at some distance from either border of the latter, and four—all in the eastern part—on or near its outer edge in the Taréi proper. It is out of my power to give aught like a correct census of these, but the number of inhabitants in single villages, ranges 150 On the Boksas of Bijnour. [No. 3, from twenty to at least two or three hundred in one or two of them. Having found out the exact number of persons in a few families, and made a good many inquiries, about most of the villages, bearing on the poimt of population, I should put down the total number of Boksas in this tract as at least two thousand, and possibly nearer three thousand. Of the fifteen villages, eleven were visited. All are built on the same plan of one straight street generally of considerable width (in some cases as much as forty to fifty feet) and kept very clean, in both respects, differing remarkably from the ordinary villages of the plains. The huts are placed end to end with intervals after every group of three or four, and the walls are, for the most part, built of wattle (of split bamboo) and dab, but sometimes of chhuppar, of which latter the roofs also are constructed. The houses are window- less, but each has a door in front and another behind, the latter affording access to the sheds for cattle, &e. The doorways and roofs are very low, and the floors of beaten earth are considerably raised above the general level of the ground, and are kept scrupulously clean. The only “furniture” in the houses, besides an occasional charpaz, or more frequently small chhappars (which are often used to sleep on, as cheaper than the former), consists of a few cooking vessels and one or two barrel-shaped utensils three or four feet high and fully as much round, made of wattle and dab, and used for storing grain. There is no change made in the houses or household arrangements during the rains, so that these western Boksas do not at any time “Jive in houses built on poles,” as is stated to be the case with those opposite Kumaon. The members of the tribe are of short stature and very spare in habit, in both respects, somewhat exceeding the ordinary Hindoo peasant of the district, from whom, however, they do not differ much in general build or in complexion. No measurements of their crania were made, but so far as ordinary inspection goes, their features are marked by several of the Turanian peculiarities. Thus,. the eyes are small, the opening of the eyelids being narrow, linear and horizontal (the inner angle not inclined downwards so far as I observ- ed), the face is very broad across the cheekbones, and the nose is depressed, thus increasing the apparent flatness.of the face, the jaw 1s 1865.] On the Boksas of Bijnour. 151 prognathous and the lower lip thick, and the moustache and beard are very scanty. Some of these peculiarities are much more marked in certain individuals than in others, but most of them were notice- able in almost every man’s face I saw, and it seems certain that a Boksa will at once recognize another to belong to his tribe even if he never saw him before, although some persons (Kumaonis) said they could not recognize one of the tribe until he spoke. The features of the few women that I had an opportunity of seeing closely, were comely enough and of the same general character as those of the men; but, as might be expected, in the children of both sexes and even in a descendant the above peculiarities were but little noticeable. Indeed, some lads were remarked in whose features could be discovered no difference from those of the ordinary peasant of the district. I cannot say, whether or not, it was owing to the Boksa peculiarities of feature striking one less after a time, but in the western part of the forest, which was visited last, “ features hardly so marked here” are noted more than once. As will be seen presently, I am inclined to lay considerable stress on the fact of the Boksas having features with so many points of resemblance to the Turanian type so well-marked, that they have in a general way been commented on by all previous observers. The dress of the men is the same as that of the ordinary native of the North West Provinces, but, except in one or two cases where the Pudhan may be presumed to have put on his “ Sunday clothes” for inspection, none of them wore turbans over the thin cotton cap which generally covers the head. The little boys run about 7 puris, or nearly so, the girls wear a scanty rag. The women’s dress consists of a petticoat, generally blue or of an orange-red, with a dirty-white or orange-red chaddar. The proper names, in use by the Boksas, are almost always the same as those of Hindoos generally, with a few exceptions such as Pili, Dhanni, Mangi and Kakha, which may be supposed to have been corrupted from Hindoo names. All of those, who were questioned on the subject, were quite positive that their language is quite the same as that of the other inhabitants of the district, and I heard of no words peculiar to these people, with the exception of some names of trees. The most remarkable of these is Kanddr for the Sal tree, 152 On the Boksas of Bujnour. [No. 3, which, however, was only heard locally. Singular enough, the Tharoos as Madden mentions, apply a special name Koron, to that tree. But little stress, however, can be laid on any, specially in the names of plants, which, with the natives of other parts of India, are often found to alter within a few miles, even among the same or closely allied tribes. There are some peculiarities in the boli of the Boksas by which one of them is at once recognized by members of their own or other tribes. Thus 2 is constantly substituted for, as sdn for sdl and nath for lath, and less frequently changed into r, and 7 into J, as dari for dali and thalela for thanela. Two of these changes are often met together, as Baglana, which is very often substituted for Bagnala, the name of their chief village. One is struck also by a dialectic manner of pronunciation, which alters the short a, and occasionally the long a@ of Hindustani, into a sound approaching that of the French eu. Thus, Boksa is called Boksuh, and achha sukha rahtéd hai is pronounced achhuh sikhuh rahtuh hac. The earliest historical indication of the existence of the Boksas consists in the circumstance of a certain division of the Chourassi Mull in Rohilkhund, nearly 500 years ago, having been called Boksdér, a term which is now, as then, applied to a tract of country thickly inhabited by them (as well as to the tribe, and sometimes to a single village of the Boksas). With regard to the traditional origin of the race, the clear and connected statements given by Elliot and Batten on this head are by no means borne out by the discrepant and, in some cases, absurd scraps of information which only these western Boksas, and the three pwrohits who are their spiritual guides, can impart. The writers mentioned, state that the traditions of the Boksas make them out to be Powar Rajputs descended from Oodya Jeet, (or his relative Jug Deo) and his followers, who in the 12th century left his native place in Rajputéna on account of family quarrels and came, either mediately or directly, to settle here. In reply to the inquiries I made on these points, instead of frequently, or at all getting a connected account like the above, the only assertions that most of these Boksas agreed in, were two, viz., that they are of Rajput origin, although they confess that the Rajputs of the plains hold them impure on account of their less cleanly 1865.] On the Boksas of Bijnour. 153 habits, &c., and that they had come from the Dakkan, but even in this they were not unanimous. When they came to details, and many professed to know none, their statements were more varied than satisfactory. Thus, several of them agreed that they came from Dharanaggari, which, however, one man declared was close to Kangra Devi. One stated that they came from Delhi, and another that they had been driven from their original home in the Dakkan by the Marhattas; one pudhdn stated that they came from Chittorgurh, “beyond Delhi” in the wars of the old Rajas, and the most intelligent pudhdn of all, the only man among them that I met who could read, affirmed that they originally came from “‘ Boondee Kolah” having been ? exiled thence “ by the king.” On this subject I found the three puro- hits quite as ignorant as the members of their flocks. A still more curious statement, than any of these was made by an intelligent old Bengali Baboo, who has held a village in the Boksa district for many years. He solemnly affirmed that, before the com- mencement of British rule, the Boksas were Mussulmans in faith and ceremonials, and that, in his time, they had Hosseini Brahmins as pwro- hits, and used verses of the Koran in their pwa. This is a very suspicious story, at the same time it is difficult to see what motive the man could have had in narrating it. It is not easy to reconcile the clear statements made to Elliot, especially regarding the origin of the tribe, with the above discordant and fragmentary information which alone is current among the western Boksas, and the explanation of the difficulty may be the following. Ii the story about Oodya Jeet is the true one, it would be more likely to be retained by the numerous and concentrated Boksas to the east oi the Ramganga, than by the few and scattered members of the tribe to the west. Or, if that tradition is, as there seems reason to suspect, a mere concretion, resulting possibly from the original conversion of the tribe by Rajputs, and their centuries of contact with Hindoo castes and traditions, it may, ina similar way, have more readily assumed a definite form, where the tribe was most numerous and united. Still less than my inclination to theorize definitely, are my quali- fications to dogmatize on such a subject, but the suspicion has grown on me, since commencing inquiries regarding these people, that their origin may be very different from what has ordinarily 21 154 On the Boksas of Bijnowr. [No. 3, been supposed. It seems exceedingly unlikely that, had they been a tribe of Rajput extraction whom mere accident had driven to take refuge in this inhospitable tract six or seven hundred years ago, they would have, for such a length of time, remained so isolated as they undoubtedly have been, from other sections of Rajputs. But thisis a minor difficulty, compared with the necessity to account for the very decided Turanian characteristics of feature which have been mentioned in detail, and which appear to be quite incompatible with a descent from any Indo-European race. It may be objected that the language of the Boksas, barring slight dialectic differences, is identical with that of the ordinary inhabitants of this part of this country. But, not to lay too much stress on the circumstance that, in a case of this kind, positive is much more valuable than negative evidence, it is a recognized principle in ethnology, that the physical structure of a tribe, and the nature of their language, may change at very different rates, the possible alterations, in each, depend- ing on yery different conditions, and supposing that the Boksa originally sprang from a source different from that of the ordinary Hindustani, and that the physical circumstances in which he is placed are not such as, even in the course of centuries, greatly to alter the peculiarities of feature, @&., by which he was at first distinguished, it is difficult to conceive any position in which his language would be more likely to be rapidly and, at last, completely changed, than that in which he is now placed. Scattered in scanty colonies, over a very narrow strip of country, the language of the inhabitants, on both sides of which (we assume), differs wholly from that in use by him,— when each successive political or social convulsion in the neighbouring tracts, and, for hundreds of years, we know that these were neither few nor slight, was seen to be followed by an influx of these outsiders, what more likely than that his language should, at last, become completely assimilated to that of the latter ? f The fact of the Boksas holding the Hindoo faith, and performing its rites, seems to me to present no stumbling-block in the way of adopting the view that they are of non-Aryan derivation. A race so few in number, and occupying so circumscribed a position, surrounded by Hindoos, and brought into close and frequent contact with them, would be likely to adopt the dominant religion almost as readily as 1865.] On the Boksas of Bijnour. 155 the dominant tongue. It is evident that, if my supposition is correct, all the traditions which assign to the Boksas a Rajput origin are baseless, but precedent are not wanting of tribes, assuming traditions in accordance with the history of their new co-religionists. Indeed, such traditions sometimes arise even where the smaller tribe has not adopted the religion of those who surround it. This is the case of the Nilgiri Todas whose ancestors are now represented to have been the palanquin-bearers of Kunya-Swami, a Hindoo deity, though the Todas, far from being Hindoos, seem to have no religious beliefs or ceremonies whatever. To the question, whence the Boksas came, and, if they are of Turanian origin, to which of the great tribes of that race are they nearly allied, the information at my disposal does not enable me to offer any definite answer. It may be, that they sprang from the same source as the Bheels, Gonds, Coles, and other so-called “ hill tribes” of Peninsular India, relics of the original Tamulian inhabitants of the country, still subsisting in the out-of-the-way corners into which they were driven by the Aryan influx. But it appears to be indicated by the fact of a series of analogous tribes occupying segments of the Sub-Himalayan forest-belt from Assam to the Jumna, and seems on the whole more probable, that the Boksas are the furthest authors of the stock whence sprung the aborigines of the northern part of the Malayan peninsula. In any case, if they are really non-Aryan, the complete substitution of Hindustani for their original language, and the thorough assimilation of their faith and customs to those of the surrounding race may form insuperable obstacles to their true relation- ships ever being found out. Here, however, I shall leave this subject to be discussed by those who are better qualified to handle it, in order to revert to less theoretical matters. The Boksas conform to the Hindoo religion in an ignorant, un- meaning way, ®nd the usual rites of that faith are performed on the occasion of births, marriages, and deaths. Marriage, as among the Hin- doos, takes place at 8to 10 years, and at this ceremony the pwrohit receives afee of about four annas. After a birth, he gets from four annas to one rupee four annas. The bodies of the dead are burned at the Ram- gunga, or other neighbouring large stream, and the phdl (ashes) are carried to Hurdwar, there to be consigned to Gunga ji, by a Brahmin ‘ 156 On the Boksas of Bijnour. [No. 3, who gets a rupee or two for his trouble. Besides his special fees, each purohit receives a general contribution from-every village in his beat, apparently amounting to about 5 maunds of grain each crop, which is allocated among families according to their means. In small matters also the Boksas adhere to Hindoo customs. Thus, they do not wear their shoes (when they have any to wear) during cooking, and they kill animals to be used as food, by ghatka a blow or cut on the back of theneck, and not by the throat-cutting haldl- karna of the Mussulmans. A good many of the tribe are said to profess special devotion to particular deities, the only ones named to me being the spouse of Siva; under her designations Bhowani and Devi, with Baba Kalu and Surwar Sakhi. Of the personality of the last, I could learn nothing. Kalu Saiyid is a local saint, who, curious enough, they state to have been a Mussulman, as indeed the appellation Saiyid, if it be not a corruption, would indicate, Some traditions about his life and death are current, and before his shrine, at the entrance to the main pass through the Siwaliks into the Patli Doon, Hindoos of all sects make offerings, and his name “ Kalu Sacyid ki jav’’ is invoked in the neighbourhood of the tomb on entering upon an undertaking, or when engaged in severe exertion such as heaving up a load, &e. The Boksas only marry among their own tribe, but there does not appear to be any restriction within its limits. In this tract they will have nothing to say to intermarriage with the Tharoos (who, they declare, ‘‘ eat frogs and lizards”), and there is some authority for believing that Elliot must have been misinformed, when told that some of the eastern Boksas, “in Kilpoory and Subna, occasionally vy} intermarry with the Tharoos.”’ The wife always follows the path of her husband, and the children that of their father, in regard toa difference to be presently mentioned. Their purohits are Gour Brahmins who hold the office here- ditarily. They do not live among their flock, but outside the forest tract, one residing at Afzulghur, towards the eastern end, and two in Nujeebabad towards the western end of the hathi. One of those of Nujeebabad has the six most westerly villages in his charge, the other has the three in the centre, and the Afzulghur man has the four easternmost with the Path Doon villages. I conversed with all 1865.] On the Boksas of Bijnowr. 157 of these pwrohits, and found two of them apparently most ignorant and stupid, while the third was fairly intelligent, sensible and com- municative. A considerable proportion of the tribe follow Ndnak Matha, 1. e. have adopted the Guru of the Sikhs as theirs, indeed they are called Sikh by their brethren, and not Ndnak shdhis as followers of Nanak are in Hindustan generally. The ordinary Boksa does not “take Nanak’s name” at all. In some of the villages, including Bugnalli which is by far the largest of all, the proportion of Sikhs to the others is very nearly or quite equal, but in some especially of the western villages, there are few or no Sikhs. Among so rude a people as the Boksas, it would be vain to expect to find any elaborate set of religious tenets either held or understood by such a sect as these Sikhs, and accordingly their one distinctive mark is avoidance of spirituous liquor, opium and charras, which the Boksas in general use freely. The Sikhs will not even smell spirits vo'uvtarily, nor will they use the hookah or eat in the house of one wko has smoked on the same day. It is said that the purohits also adhere to the latter rule. Tobacco is lawful to the followers of Nanak, and they, and the rest of the tribe intermarry without restriction, the wife and children as above mentioned invariably following the man’s sect. The Boksas bear an excellent moral character. I have no definite information as to their intimate domestic and social relations, but for three years at least, not one of the tribe had been a party in either a civil or criminal suit in the district courts. Any disputes that occur are referred to the village elders, and in extra- ordinary cases, it would appear that the pudhdn of one of the more important villages (Bagnulli or Chuttroowali) is called to adjudicate, but such quarrels of any moment are extremely rare. Their indolence and ignorance are fully as remarkable as their inoffensiveness. They have a strong objection to all labour which is not absolutely essential to provide means for subsistence ; for example, near some villages immense quantities of manure, of which they well know the value, were lying unused, the trouble of taking it to their fields being too much for them; and they assigned as the reason for not collecting Kino (Mrakkigond) in the forest that it. would be barri mehnat, although it is really very hght work, 158 On the Boksas of Bijnour. [No. 3, They seem to have no spirit of inquisitiveness whatever, even in regard to points in which one would naturally suppose they might be interested. Thus it was frequently found, that they did not know who was the pwrohit of villages within half-a-dozen miles of their own: and several said that there were no Boksas beyond Nawab- poora, which is the most easterly village of this section of the tribe. As a specimen of their combined ignorance and credulity, I may mention, that a pudhdn of one of the largest villages having brought up his sick child, for some time declined to answer any questions, believing that by merely feeling its pulse the details of the disease would be discovered, and that any information from him would be superfluous. They have among them no arts or manufactures whatever, all clothes, leather, &c., being imported ; nor do they, so far as could be learned, use a single medicinal substance. I only met one Boksa who could read, and heard of one other. They are much more frank in manner than the villager of the plains of the North West Provinces, speaking their mind pretty freely, and they appear to have some sense of humour, which if the latter possesses, it never comes out in his intercourse with Huropeans. One of the Boksas when asked what remuneration he got for being pu- dhdn, answered with a grin ‘‘ Nothing but dzkkat ;” the question, ‘‘ What will you get, for having guided me, if you do not wait till my servants come up?” elicited “‘ Plenty of kdntd on my way back ;” an old fellow on seeing me examining under the ribs of some of the others for spleen, complacently patting his lank abdomen said with a droll expression such as is often seen to accompany some stroke of ‘‘ Scotch wut,” ‘ Do you think I’ve got spleen?’ And I had a hearty laugh, one intensely cold morning, when on my suddenly stopping to ask the old guide who, with chattering teeth, was panting up an acclivity after me, some question about their traditions, he replied ‘ I may remember by and bye, but its so bara jaara just now, I can recollect nothing.” Their only amusement seems to be the pursuit of game, terrestrial and aquatic, and they complained bitterly that the recent carrying out of the Disarming Act had deprived them of a chief means of ivelihood. They are excessively greedy after animal food, and 1865.] On the Boksas of Bijnour, 159 Mr. Batten informs me Boksas have told him, that without wild pigs a Boksa would die. This statement has probably something to do with their fondness for sporting, but, independent of this, wild pig is said to be almost a passion with them. The Boksas are undoubtedly restless in their habits, and there are more migrations from village to village than would appear to be absolutely necessary. Still, this propensity doubtless shows more strongly when contrasted with the generally extreme adhesiveness of the Hindustani agriculturist to his native village. Here, among the western Boksas, there is nothing like the “ Never stay in a place more than two years” which Jones and others state to be the case with their eastern confreres. On the contrary, most of the former appear never to shift their village at all, and the most exten- sive changes going on of late years among them, seem to arise from the Government orders to clear the Patli Doon. With the minor development of the nomadic instinct, shown by their restlessness, they evince unconquerable adhesiveness to their natale solum among the swamps and jungles. I could not hear of a single instance of a Boksa having emigrated from the forest belt, and they mentioned the existence of a tradition that no Boksa had ever gone abroad for service. Although they are so fond of flesh, they keep no goats or sheep, and in only one instance did I find that a few fowls were kept. Agriculture may be said to be almost their sole employment, but one or two others, which are followed by a few of them at times, may be here noted. A very small number of them ever engage in cutting bamboos or timber for export, and the collection of drugs and gums, which are largely produced and gathered in the forest, affords employment to almost none of the tribe. In some parts, however, they collect a few of these (viz. gum of jingan, Odina wodier, and sohanjan, Hyperanthera pterygosperma, kamela powder from the Rottlera tinctoria, aorila, fruit of Hmblica officinalis, and harra immature fruit of Terminalia chebula) for sale to the bunyas, who come hither to buy such things. I have already here mentioned, that the collection of the kino of the dhak they object to as being too laborious, and probably we must attribute to sheer laziness the fact, that they do so 160 On the Boksas of Bijnowr. [No. 3, little in availing themselves of the natural products, which are literally scattered around them. But the most important and interesting of the extra-agricul- tural avocations the Boksas ever engage in, is gold-washing, and it deserves a somewhat more extended notice. Within the last 25 or 30 years, the first part of the course of the Ganges, outside the Himalaya, furnished gold from its sands, but at present the Sona naddi in the Patli Doon, and the Ramgunga, below the junction of the former, are the only streams in this neighbourhood, whose sands are regularly or frequently washed. Little is done on the Ramgunga outside the Siwaliks, but there appeared every indication that the gold-washing was a regular employment of the Boksas on the Sona naddi, and there is reason to believe, that the proceeds derived- from that minor Eldorado -had a good deal to do with the manifest reluctance of these people to leave the Patli Doon, on the occasion of its being shut up for the preservation of the timber. In the aggregate, however, the amount annually collected does not seem to have been very large, for some years ago, the sum paid to Govern- ment by the contractor of the Doon as gold-dues was only 25 rupees yearly. The Boksas say that there is nothing in the appearance, of the gold-bearing sand to let them know if it will be productive or not, and only “ prospecting” by a trial will shew this. The sand itself is dug from the bed of the stream at many places extending over several miles, and the superficial layer generally contains much less gold than some of those a few inches below. In the sand, there seems to be a good deal of ferruginous matter, and there are iron-markings along many parts of the borders of the little stream, which here runs down an intra-Siwalik valley similar to, but very much smaller than the Dehra Doon. The soil, in and near the bed of the stream, is mostly gravel, and soft gray sandstone, similar to that of the Siwaliks, frequently crops out. Three or four people, often members of one family, work in a gang, each having a separate part ofthe process assigned to him.