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P. S. Ihave found on comparison that I had come to wrong conclusions, with respect to some of the vertebrae, I had the honor to send with the last parcel, of which opportunity I availed myself to send all of which I had the least doubt. The teeth too, which I have hitherto . called camel’s, cannot have been rightly classed, as they bear not the least appearance of having belonged to the existing species, at least, the evenness of the crown differs entirely from any anatomical specimen to which I have access.

I should have forwarded the whole of the undermentioned specimens before, but obvious reasons induced me to wait the present op. portunity.

List of specimens illustrating observation: on the obstacles to navigation in tire . Jumna,_frn-worded from Delhi, 22nd October, 1834.

A. B, C, D, E. Specimens of the remains of a cluster of one pipal and four palms.

F. Parcel containing 10 specimens of petrified animal remains, viz. Nos. 2 and 3, teeth. Unknown. ,.,

,, 14 portions of Asiatic elephants’ jaw and tooth.
,, 38 and 39, upper extremity of femur and kneepan.

(Of these I had myself no doubt, as having belonged to a camel ; but some doubt
having been expressed in another quarter, I have left it to your decision.)
N05. 40, 4l, 45, 48. 49. Vertebrw.

z‘. Specimens of pipe kankar.

y. Supposed shale.

2. Rolled clay connected with the formation of conglomerate rocks.

a and b. Fossil remains of an elephant from Pachcowrie. Femur and enamel of tooth. Specimens of clay passing into or vitrified clay. Specimens of sandstone passing into ditto. 1. Fine sandstone from Burriarie. 2. Coarse ditto, from Mhow. 3. Specimens of vitrified clay from Murka. 4. Ditto of ditto, from Mhow. 5 6

9-."

Ditto of ditto, from ditto. . Cement formation of conglomerate rock.

7. Tufa ditto, of ditto, containing blade bone of camel and other animal remains.

, 8. Specimens of outer edge of beds of nodule kankar, conglomerated by carbonate of lime.

9. Specimens of petrified clay.

10. Composition shingle, in which sand predominates.

ll. Ditto ditto, in which clay ditto.

12. Ditto ditto, of separate formation, cemented into one mass.

13. Specimens of sandstone peculiar to the J umna.

Norn.-—-We intended to have given plates of the principal fossils forwarded by Serjeant DEAN, but the friend who had kindly undertaken to draw them has been prevented from accomplishing his task in time; we must therefore reluctantly postpone their insertion and notico.—En.

V.-Note on the Gold Washings of the Gu'mt1' River. By Lieut. CAUTLEY, Beng. Art.

In-the 18th volume of the Asiatic Researches (Physical Class), the occurrence of gold in the line of mountains skirting the‘ foot of the Himalayas has been brought to notice by Captain Hsmaawr, and as in his specification of the points where it has been found, he has drawn our attention chiefly to the Ranugunga, and its tributaries east-ward of the Ganges, and has not noticed the tract of mountains upon which the town of Nahun stands: and as in the system adopted by the natives in washing the sand, as described in the paper alluded to, there is some difference from that of the Nahun washers ; it will be perhaps interesting, not only to bring forward this new locality, but also to shew the simple means adopted in procuring the mineral.

The late grand discoveries of organic remains in the hills under Nahun, and the consequent desire of prosecuting the inquiry as far as means would allow, have like many other searches led to the discovery of an object of a totally different nature from that in pursuit ; nor may we be far wrong in agreeing with Captain Hnancar, that the ultimate discovery of gold in abundance in these regions will eventually either benefit some fortunate individual, or else come at once under the eye of the ruling power of the district.

I will however enter upon the subject of this note, previous to discussing the ‘probabilities of discovering the ore in situ. '

The rivers from the beds of which the sand containing the ore is procured derive their sources solely from this lower tract of mountains, and are not in any way connected with the Himalayas ! There does not appear to be any river free from the ore, although many of them are considered by the washers as more abundant than others, and consequently more worthy of their labor : that to which I shall particularly refer is named the Giimti river, which leaves the mountains at the village of Chfiran ; Giimti being the name of two villages on the right and left of the stream, about three miles in the interior, at which there is a main junction of tributaries ; the river opens into the plains opposite to the town of Sidoura, to the Westward, and parallel to the Choura Pani and Markunda river, which carry off the greatest; portion of the drainage from the hills directly under the town of Nashua.

The gold-washers are by no means numerous, and are of the poorest class, depending entirely on their trade for support. The Raja of Nathan levies a tax of a masha per annum on each trough ; but although there is no restriction to the number of people employed, as long as this

toll is paid, there does not appear to be any desire or competition on the part of the natives to carry it on, by which we may draw a tolerably accurate conclusion on the returns of the trade as it now exists.

The apparatus used by the washers consists simply of a trough, a sieve made of the Sirkunda grass, a flat piece of board, with an iron edge for scraping up the sand, a plate or dish for carrying it away, and triturating the sand with mercury, and a ladle or spoon made of a gourd, for raising water: with these and a little mercury in the end of a hollow bambu our gold-washer starts on his pilgrimage. Ihave endeavoured in the accompanying sketch Pl. XVII. to give some idea of the process, and this will perhaps be clear enough without much explanation. The gold washer, in the first instance, examines the soil by washing a small quantity in his hand, the smallest particle or particles of the metal are easily detected: the soil holding the greatest quantity appears to be that in the line upon which the drainage of the river takes place, for these mountain streams occupy but a small space of their channel during the dry months, or even at any time, with the exception of those periods, during the rainy months, when very heavy and successive falls of rain charge every channel with its full supply. The situation proving favorable, the washer then establishes his trough; the sand is placed on the sieve, and water thrown over it with the spoon : the coarser particles are thus separated and thrown away; the man still continues pouring water through the sieve over the sand in the trough, until nothing remains there but an almost impalpable blackish powder; in this powder the gold dust is perceptible. This powder is then collected and taken out of the trough, forming a mass capable of being held in both hands : this is triturated with a small quantity of mercury on the dish or basin B, and the whole is again subjected to a careful washing with the hand on this dish : this latter washing removes every thing, but a small piece of mercury and gold in amalgam. The gold-washer then lights a piece of cow-dung, upon which he places the amalgam, and (as far as I observed in their manufactories) his labor was repaid by the smallest piece of the precious metal imaginable. The rains are said to be the best and most profitable season: at this period, two rupees per day may be the return of one trough under a gold-washer and one assistant, the worst day's produce about two annas; the gold is either sold to the bum'a's at the large towns in the neighbourhood, or given to zaminclérs for an equivalent.

There is a great loss of particles of the gold in the system of washing adopted here, many of which must pass off through the trough; there is also a total loss of mercury : the latter might be easily reme

died, we should imagine, were the washers in the habit of giving the amalgam to their employer, who might complete the process in close retorts. It is evident that under the eye of an active and interested person, a trade might be carried on here of a description by no means contemptible: a much greater quantity of the mineral might be procured; and that on the adoption of a trade in the article,-an improvement of the apparatus might be etfected, tending much to that point. I have much pleasure in sending you three packets.

No. 1, containing the sand as found in the bed of the river.

2, the black powder, the result of the first washing in the trough.

3, the gold ore ; and shall hope to see your note on the quality as well as the natural state in which the ore exists : it would appear from the account of the washers that lumps or larger particles than those sent are not found, although it is by no means an easy matter to get correct information on points of this sort*.

That the gold exists in any other shape than that of the present specimen in these lower mountains is very improbable. The particles may difl'er in size ; and we may in all probability detect the stratum containing the gold dust, and so procure it before it has undergone further attrition in the river's bed ; but we must look to the Himalayas themselves for the auriferous strata. from the disintegration of which the sand of these lower hills have been supplied with the mineral. Captain HERBERT alludes to the occurrence of the ore having been traced up to a certain point in one of the tributaries of the Ramgunga, a fact corroborated by Mr. Rnvnnsunw of the Civil Service, in a note to the Society. My inquiries establish a similar limit in the Giimti river : this is a point, however, that would require very careful examination, and that examination under the eye of an experienced person, who, after all, in such a maze of mountains and rivers, would perhaps have to depend upon chance for successful prosecution of his labors.

The occurrence of gold in alluvial soil is common to every quarter of the globe, although South America and Africa provides the greatest supply of commerce, and in all probability there is no extensive chain of primary mountain that does not charge its drainage with the mineral in question ! Its incorruptible nature, and its not being subject to the

'* These have not yet reached us. The black powder is however doubtless similar to that which accompanies the gold dust in the rivers of Assam and Ava:—f0r the most part magnetic oxide of iron. Platina may also be found in it>but rarely. The use of a strong magnet would perhaps prove advantageous, before rubbing in the mercury for amalgamation.--E D. I

N N

effects of oxidation from common causes, is a suflicient reason for the presence of this mineral, unaccompanied by others*.

With regard, however, to the Néhun and Ramgunga gold, we are perfectly dccided on one point, viz. that the rivers bearing the dust have no connection whatever now with the great Himalayan chain, and therefore, that if the mineral exists in abundance at any one point, it will be found in the hills from which these rivers derive their sources: and it is to be hoped, that we may even look forward to the ultimate discovery of gold in comparatively as great abundance as the present fossils, the existence of which, six months ago, would have been as much doubted as the possibility of finding gold now may be.

Northern Dudb, April 10th, 1835.

[graphic]

VI.——N0tice qf the Nipdlese Spirit Still. By A. CAMPBELL, Esq. M. D. attached to the N épal Residency.

The accompanying (Pl. XVII.) is a rough sketch of the still in universal use throughout the valley of Nepal Proper, as well as its neighbouring hilly country ; and so far as I can learn in the portions of eastern Thibet, usually visited by Nipfilese traders, on the beaten commercial routes, by the Kerirn and Kuti passes of the Himalaya, to Digarchi and Lhassa. I believe it to be as different from that commonly used in the plains of India, as it assuredly is from any with which I am acquainted as existing in European countries, and as its use is confined here chiefly to the Newar population, it needs no apology for intrusion on the public attention.

~ In India, (so far as my recollection is faithful,) Nipalese men, menners, and things areregarded, as pertaining exclusively to the ruling class of the community, yclept Gurkhzis ; this arises partly from want of better information on, or curiosity regarding, Nepal affairs ; partly from the common habit of identifying the whole people of a country, with the few, who may for a time direct its destinies, but chiefly from Nepal being best known to us, as the theatre of a twoyears’ ‘war between one power and the afore-mentioned tribe.

The Newars, as is well known, were down to the Gurkha. conquest the rulers of this valley, and were, as far as at present ascertained, its

* In the specimens from the alluvial soil of the Brazils, the particles of gold are much larger than those found in the N ahun sand, appearing like little boulders, or rounded masses of the mineral. In my cabinet the Brazilian alluvium is clay, or argillaceous matter, with rounded pebbles of white quartz. Mr. MAWE having provided the specimen.

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