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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
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1 2 ReTRENURUS ATRIPININE: Bia
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W- Ky Lek Hren-Calay: ra
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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
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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)?
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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
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JOURNAL
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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.
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ILLUSTRATING M® PARISHES NOTES
OF A TRIP UP THE SALWEEN
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Journ. As. Soc. Bengal.
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On stone by Kristohurry Doss.
Sketched by C. Parish.
BOULDER TEMPLE AT KYIK-HTEO
Journal As. Soc. B
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Skelched hy C. Parish. On stone by Kristohw
KYIK-HTEO-GALAY BOULDER PAGODA.
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Vol XXXIV. Part Tl, P}
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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. Thou arrivest at Khu-the;
thou goest unto Tha-ma [7. e. Yu-ma, the judge of the dead].. Thou
goest through the crevices of rocks, thou goest through the crevices of
precipices. At the opening and shutting of the western gates of rock,
“thou goest in between ; thou goest below the earth where the sun travels.
Temploy thee, I exhort thee. I make thee a messenger, I make thee
an angel. Good, thou revealest; evil, thou revealest. Arouse thee
fowl, arouse ; reveal what is in thee. Now I exhort thee, I entreat
thee, if this man is to live to an old age, if his head is not to be bent
down, ii he is not to come down crash, like a falling tree, let the
right hand bone come uneven, let the bones be short and long. Thou
art skilled in the words of the elders, thou knowest the language of
old men. The good, thou fully knowest ; with the evil thou art -
perfectly acquainted. Fowl, I exhort thee, I entreat thee; reveal
whatever is in thee. And now, if this man’s head is to bend down, if
he is to come down crash, like a falling tree, if he is to be unable to
rest himself from incessant trouble; if unable to overcome obstacles
which shall meet him on every hand; if unable to rise up or lie down,
if his life is not to be prolonged, if he cannot live, then, fowl, come up
unpropitious, come up with the tendon short on the right side, come
wrong end foremost. If he be able to obtain sufficient to support life,
if he be not overcome by feuds, fowl, come up even, Thie-keu’s fowl,
Mo-khie’s fowl, I pull out thy feathers, I pull at thy skin, I dip thy
head, I dip thy feet. Arouse fowl, reveal what is in thee.”
Hyery one in succession is then besmeared on his forehead with the
blood of a separate fowl; and then every one marks his own fowl by
tying a string to it that he may recognise it after being cooked.
Some tie a string on the neck, others on the leg, others on the wing,
and others elsewhere. They next scorch off the feathers, and boil
them.
The hog is taken if the gall bladder be deemed a good one, otherwise
it is rejected. When the rice and meat is cooked, they bring the rice,
234 Religion &c. among the Karens. [No. 4,
and the pork, and the fowls, and the threads, and the bamboo tubes to
suck up the drink and the spirits; and all are placed together.
The master of ceremonies then goes and puts two bamboo tubes
into the left hand of one, and the gall bladder of the hog and the
head of the fowl into his right hand; and then the elder of the family
takes the thread and ties his wrist. Hach one in succession takes the
articles in his or her hands mentioned above, and the elder ties every
one’s wrist, at the same time praying with each: ‘‘ Mo-khe, the hand-
tier, the good-to-do, we offer thee food and drink, spirits well prepared,
a great hog. Defend us; when we go to and fro, look after us. If we
fall, raise us up. When we go or return, when we walk on a branch
or a beam, when the branches or creepers break down, when we
go among the Burmese or other tribes, when we climb trees or descend
into the waters, when we go up into the house, or return to the paddy
field, may no accident befal us! Stretch forth thy hand, and help
us; put forth thy foot and assist us. Go before us, follow behind us.
Deliver us from demons, deliver us from ghosts.”
After this the person whose wrist is tied, changes the things in
his hands from right to left and left to right. Then each one tastes
the spirits; after which each one tastes the fowl; and when this is
done, an elder is called upon to pray, who prays thus :
“ Mo-khe of mountain Kie-ku, Mo-khe of the seven heavens, Mo-khe
of the seven earths, assemble together, even the blind, the deaf and
the lame; and eat and drink the valuables.”
A libation of spirits is then poured out; and after this the drama
closes with spirits being served out for all to drink.
ASTRONOMY.
CosmoLoey.
“There are seven heavens and seven earths.” This expression
occurs frequently in Karen stories, but the people have no definite
ideas on the subject. The sun is supposed to go round the earth. In
the west are two massive strata of rocks which are continually opening
and shutting. Between these strata the sun descends at sunset, but
how the upper stratum is supported, no one can describe.
1865.] Astronomy among the Karens. 235
In the western ocean is an immense volcanic mountain, which is
continually fighting with the water. They have a story which must
be of common origin with Sinbad the Sailor.
The Elders say there are fish in the sea as large as mountains, with
trees and bamboos growing on them as on land. Voyagers have to be
careful where they land to cook. They carry axes, and cut into the
ground to try it. If juice springs up where it is cut, they know that
they are on a fish ; but if the ground seems dry, they are on land, and
go to cooking.
It is related that a man landing on an island, went to cooking with-
out trying his ground, and it proved to be a fish which sunk with him
into the sea, and then swallowed him. When the man was in the
fish’s belly, he said to the fish: ‘‘ When males acquire large game,
they shout, and cry out in exultation, but you are silent. Are you not
amale? Qn hearing this, the fish opened his mouth to scream, when
the man leaped out and escaped.”
The Elders say that when people kill one of these fish, it is impos-
sible for them to eat it all up, and they burn its fat. With its bones
they can make beams and rafters for houses.
CoNSTELLATIONS.
The Karens have names for a few of the most prominent constella-
tions. The great Bear they call an elephant, and so do the Burmese
and Hindus. The pole star is a mouse crawling into the elephant’s
trunk.
The southern cross they call Mai-la-ka, a name whose derivation is
not obvious, but they regard it as some kind of animal ; for they say
that Mai-la-ka and the elephant once dwelt together in the middle of
the heavens, but they quarrelled and fought. Mai-la-ka seized the
elephant by his tail, and the elephant took Mai-la-ka by his thigh,
and in the struggle which ensued the two were thrown to the opposite
extremities of the heavens, where they remain to this day.
The Pleiades is called ‘the great house,” and is regarded as a family
of persons, consisting originally of seven persons, but one has been
lost, and there are only six now. Two men, one of their myths states,
married here two sisters. The names of the men were Lan-to, and
To-phau ; and of the women Tha-bgheu-mu, and Tha-bgheu-bghai,
31 ;
236 Astronomy among the Karens. [No. 4,
While the men were out fishing, “the wife bearer,” or Orion, came
and carried them off on his shoulder. The women cried out to their
husbands :
“ Lau-to, oh, Lau-to dear,
Snatch up thy bow and spear,
To-phau, oh, To-phau come,
We’re carried away from home.”
After calling a long time, their husbands heard their cries, and
returned home, when they discovered that their wives had been carried
away. They seized their bows and spears and followed on after “‘ the
wife bearer.’”’ When they came within a spear’s throw of him, Lau-to
poised his spear or javelin to throw it at ‘ the wife bearer ;” but his
younger brother came behind Lau-to unobserved, and struck the
handle of the javelin, so that it flew against his father-in-law’s house,
and knocked a part of it down. To encourage their wives, the men
sung :
“ Tha-bgheu-mu, suffering dear,
Tha-bgheu-bghai, have no fear.
The bow’s bent, the string tight,
Arrows ready, you in sight.”
Then they followed on silently, and “ the wife bearer” thinking he
was not pursued, stopped and set down his burden to rest; but while
he was gone down into the water to bathe, the husbands arrived and
carried their wives back home, and repaired their father-in-law’s
house.
Though the resemblance is remote, yet this story must have had a
common origin with the Greek myth of Orion and the daughters of
Oenopion.
Some of the Karen constellations, to judge from their names, are of
Karen origin. One is called the “ Burmese yoke,” from the resem-
blance the stars are supposed to bear to the yoke a Burman carries on
his shoulder,
Some names are local and vary in different places. For instance,
the Karens in the south call the Milky way the “Paddy Bin af
while the Bghais denominate it the “ Bazar. street,’ because the
streets in the bazar are usually an undistinguishable mass of people.
1865.] Astronomy among the Karens. 237
Comets.
Comets are sometimes called ‘ Tailed-Stars,” sometimes “ Fire-
Stars,” and sometimes ‘‘ Smoke-Stars.” In common with all other
unenlightened nations, the Karens regard their appearance as indi-
eating approaching war, famine, pestilence, or other public calamities.
PLANETS.
The Karens do not seem to recognize any planet, excepting Venus.
They know the evening and morning star to be one and the same, and
by some process not clearly understood, she is sometimes before, and
sometimes after the sun. When a morning star, she is called the
“Star receiving the morning ;’’ and when an evening star, the “ Star
receiving the evening.” |
SHootine Srars.
Shooting Stars are said to be “ Youth Stars,” going to visit the
“ Maiden Stars.” When a Karen girl sees one she exclaims, ‘“‘ May
my hair grow as long as the path thou fliest !”
Meteors.
Meteors, the Karens say, are the animals that produce gold and
silver, and when seen in the heavens descending to the earth, are sup-
posed to be returning home. When a report is heard, as the Karens
say there often is, itis the roar the animal makes.on entering the
earth. Wherever they fall, gold or silver is certainly to be found in
the neighbourhood.
Division oF THE YEAR.
The Karens divide the year into twelve lunar months, and, like
occidental nations, they begin it with January, and end it with De-
cember. This is contrary to the usage of all the nations that surround
them; the Burmese, the Talaings, and the Shans commencing the
year in March. “ The civil year,” says the Journal of the Asiatic
Society of Bengal, “‘ commences differently in different parts of Thibet,
varying from December to February. At Asadakh, it begins in De-
cember. The months have several names expressive of the seasons,
&c., but they are usually denominated numerically ; first, second, &c.”
The Karens would seem then to have derived their calendar from
Thibet, for while they make now the year to begin in January, yet
238 Astronomy among the Karens. [No. 4,
the months corresponding to June and July are designated numeri-
cally ‘‘ the seventh,” and “ the eighth’? months, which must have
originated from a system that made December the first month ; as our
September and October must have been named, when the year was
made to commence in March.
The names of many of the months show that they were given when
the Karens had the same habits that they have now. Thus January
is “the searching month,” from the habit of going about in search of
a suitable locality to clear a field. And February is “the hewing
month,’’ because in this month the trees are cut down. Other names
show that the seasons were the same when and where the names were
given as they are now. Thus April is “the seed month,” because in
this month the seed is sown; and August is “the month of gladness,”
because the corn is then in the ear; like the month of Abib among
the Hebrews; but that corresponded to April, indicating a different
climate from the Karen. May is “‘the Crinum” or holy month, be-
cause the Crinums, popularly called lies, are then in flower ; while
December is denominated ‘‘ the month of the shades,” because in this
month the Karens make their annual offerings to the shades of the
dead. |
The Red Karen names are usually coincident, but a few of the
months have different names. July is not with them “ the eighth
month,” though June is the seventh ; and August is not “the month
of gladness,’”’ but is named from a feast that is made this month, and
which is peculiar to themselves.
A correspondent writes: “ In the month of Ai-du, the Red Karens
kill hogs, and fowls, and oxen all at once, and make a feast in which
the whole village eat and drink together. They beat drums, and fire
off muskets, and have sham fights, firing at each other with nothing
but powder in their guns, Accidents often happen, and houses are
frequently set on fire. The feast is kept up for three days, and during
their feasting the people send food and drink to their friends and
relatives in other villages. The origin of the feast is not known.”
239
Karen Vocabulary.
1865.]
"aIny-DF “DIT
‘ONT “ULING,
"SOT
“hol EU
nour “wry
"yany pure “yny “UIT
ey eS)
“Yow
8 SOIUSIS Jo[dnoo sup,
“AvT AL “Ung,
AMS AGU
‘any J, “WING,
‘jortinbs B soylUsis a7
"ng “OUuIry
‘uag weyg
“DID “OUL0OYT
‘unybury, “SudIOyy
OT TRL
‘hoy wang
"UorTT “ULRIG
ey ANU 8
IK
BUC
noyd
oosN
eu-v gq
4OS FT
oly
orn,
CMV
ed
Sunyyy
eal
Ol]-® T,
OTM FT
NON
BM-BG
Hoy
Ae
CU-Bq
qIOMSFT
noy
omy FT
nil
Bd
ney
nA-WOry
“OY YUDE)
sywouay “nyjbunoz wo hosp
OTM} FT
°N
BM8-89
nod
NVZ-O1]y.
CU-GIT
ory
eA
OH
qoaig
avy
no,
Id
uo}
Ary
MAL
‘pybdoyy
oIMys Cue eli
SIN oNG
eT Aer-neg
NS] ng Od
eAU-BUL-009F]
ned-Uld TL ‘oorHT
eu-eq vue Aeu-eq
OIMT YT OIMA YT
suneyyy Avd-v J,
OTM FTE Meaqy,
TL SENN
ony a
OT OT al
ed vig
SunjiyT no J,
Suey
ory Ss« ATA
‘NWOT, ‘Ong ‘Uawny poy
OL TT OIM IFT
®IN ®IN
BM-0g eyyeaneg
val
neg pue nepy
ned-orpned-olul-e yy J,
Aeu-eg eued
rea iDal ory
Aed-eyy ol
SHES Crh
oI, omy,
or hall
eq-D9F oH
Auld "Id
ney, nay,
viyy-Av AA neysnerpy,
ETE | EDT
“wmyog “noby
‘SHWANONAG ‘O27 ‘IvaDg ‘AVG “ASITONG, HiIM ‘SdYOM NOUV] OLMSGNOG #0 TAPOTVIVO YW
Soy
keg
MOLD
MOO
te)
oreyng
ouog
‘dnog (<4
yeog
poolg
‘dnog “
pag.
MOLLY
quy
‘dnog “
VW
“ysypbugy
LNo. 4,
Karen Vocabulary.
240
‘wary “URYyg
‘uary “WING,
“Uarry “URYG
DANY) “CS
SEMAN LUO)
‘OFT “uRYg
hunoyy “wang
‘nligy “OK
DI “uUByg
‘bun “POLL,
‘my “Yury
‘ayy “eog.
DY]. “weyg
"yon ULI)
‘Bunigy uryy)
‘buns, “weyg
‘DAT ‘OYSUTG
“SY LDUA LT
Oak
aryye
UBT
SUL
SUNN
OV
ny-e yf
ng
OOT-B YL,
keg
uey sy
ney
OW
Bd
Ae
uesyy
Ue4-We FT
vB N
‘ny jbUuno, 7,
eyyy od-vy-vy,
ory
Bry
ay |
wing
oly,
Suny
no
oouyy
Ss
Suey
suryg
8 AN
vd
Avy
a | a |
B-B1F7 Bl-B IT
oT bal
FOYT, oys-ery
DN nent
ynoyL OH
NeMY-O¥T nol
88 HOS)
YNO]-OY S{OoY-Noq Ney-ooyy
Avy
oA q -00F-01g
ny-ny =| Mey
old NET
SIA IN O=2 1K
ial ed
om = Av
Sues} pT
nypy-Avpy
O-ON tN
‘OY YD)
olny nybdory
osy-ey SunesyT Sunesy-vy
Noy-nvpLOYY-oue Py oOyy-suvyy
BN
“Nl DD
suey gq ovy, ory ned-vyy
ery Aery Aery a |
ey, Avqy-09 77 B-VIAy ey
Surety) oH °H ol
TEST EMRE TD tlh EMBEDS
HUON nen nd N noN
on a 8 | neiT On
OY NeIY-00FT noyy-ooyy ous,
ie ng ng ng
como = BAT-OY YT OOT-NOYE 0049-0 YF
: oq Ae qAvy-oy-Av g Avy-Avq-AR
MU DY abil SUBS LAL
suryg oud ney ney
Sun-oy, OW OW 00-0]
wud keyg ey, » ‘eq td
OW AvpOop-v]-noyy AvW
RYS-B
nypy-Av py
nN SunON
Avpeyy-noAy-o
BN ‘AV]-BY yy
‘Ong
“Wad DST ped
VYS-VY]
NOP] -V'T
ney-At Ny
ooy-Av NY
LU ybg
UBSY-BY
OU - UV
ON
UN
“roby
qsvy
yeory
uoly
asnoy
Os10 AL
WO FT
Soy]
proxy
puryy
UVAL
yRox)
4007
TOMO]
ally
TOIL]
oA
queydoalq
Yegy
‘dnog “
It Wf
“yspbugr
241
“nedd-vtmy) ‘WING,
“DAU ET “ueys
(6
TAM)
‘buy eyoyg
Karen Vocabulary.
‘D]-UDY YY “URIS
“NOY ST UIT)
“hu ueyg
“Nay “uByg
Apyuowt OF W110}
‘OMloues OU SI oto,
‘bunoy yy uryg
‘007 “wang
1865.]
eyy-ey, «- A’Y}-eG-—-&Y-Ylog.
uvy-Avpy Avpy,—-By-neg
ney Oory
eZ
BULY) SIM SIM Y-vry
NVUL-¥ NT hog noez-Aeny
ey ae | vy
ON @N
CL
Suey ONO THY
o£
VI-v.L-¥}-00d-ey nes-ery
sunoig vy yy noy-eaqT
NV]-VT
SUNOY = neMYY, nos-ery
ney nod-W ny wy
ery Bry vy
nod, = Oru~ery
od-v]-noy
nex o7,
sunoAy-e 7 ne] gq
suok nez-o7
ney -vy-vig ‘op-log
sunodpy
POMEL
vyy-oung
oT
Lae
vuy) oIMy-eyp,
OuL
Mtg)
tN
RU
Sule]
eH
08-tq
esl
-B AIT) On
O[-3un07 FT
SUNBY Sy Sunvy-oyyy
OW
wT
OW
OT
oul
-VMB-NOIFT
vyd
~nod-v yy
00-nos fy]
SUOTY-NO FT
ni q{suopyd-nopy
Aeys-9 7,
Jo ‘Avyy-0f «= Avq4-0T v1]}-0T(unou) Jeg
ey
vdTyy -ood-AvT yy AUT peoy
ODI ney = Oy ‘oT TOATYT
°X PEM “
OA EKT! CA PIMY-VYY, | Ulezaelg
vA
Jo ‘oouy, nou, oul 0)
Avy ACH BP SUIMOATT
Aen Aen ®N SIN
Aeyy, Aeqy, eyy, ‘dnog “
STIL STAL STN Sue NN
alys-ny O8-tq os-eq ojmbsnyy
OO-RY YT «= WVU-vTON-eIY QUO
BATT NT-nVy yy oy-eyy “dnog “
oyg nu ney Nos-vyy UrILzUNOPT
no hoy OW oYPIOP
Aery Avy a | MOO]
OlU-vy, «= OTU-Byy_— BANJ-B,
Avyd
ny-ne_ = -ey-no_ vyd-nd-vy_
nea nox n-vg, Aayuoyy
nojd
nof-o1g -eyj-eysgq ‘dnog “
vi-vy-AVI vd-orquvduy-eysg uty
[No. 4:
Karen Vocabulary.
242
“WAT “URI
PS OTD
“pay y, “Wang
“phy ‘wing
‘buy nquary
‘fuoryT “eyodery
bung Ur)
“moreyy UL ys 1Oy
plOM O[SUIS OU ST O10] T,
tq =)
“sy oulaeyy
BM NY
oH
ens-ey,
aL
OYA
‘SUNT
BSE
TLL
oly d
‘nyjbunoy, «0 hoy
Kemyy = AVANT
mows) -=127E
nyy-Avyy nog
eT i
ON OL
om] BU Led BAS
oy yp yrop-ed-e yy,
noAT(l ney
ynoy yuo
BSL VS
coy = ny
oyd-oyde
vyj}-noy-vg -oAY-Nv I,
Sia SNe
Suey ney
“OYSVO-F)
‘py bdo pr
AN NT
nosy]
Suray,
oN
Ssuniqq
Suny
vs]
OO
"NDT,
KEMNT
SUNON
ial
SUBM-¥T,
Surly],
Av
oS
ni
Suory
vus
ooyy
Suoy
-od-ooy
oud
Suvyy
‘ond
nory ARMY ARAN
neu-Vyy ON
oAI on eH
ug neq nevA-vyy,
neuh nod eT
oyy-oyy Avut-noyy, AvW
ot-ood-Aey, —0-BY}-0G
oy so ‘oyyy = 10 “oy
OOUI-v'T ny NI
ney no'y ney
Avyg keyg VsFL
00% 00, nip)
O]-ouL vy-ned OT
-Vpy-nepy « -ey-neyy -od-vy-oopy
od oud old
Avy Av ney]
"UalD YT poy “anybo *noby!
Ulva
. dnog cc
Oye MA
asey[tA
aol],
oo,
TOOL,
ung
ouo}g
IRA
oyRug
ANS
ulyg
(qaoa) “
yspbuyy
1865.]
Karen Vocabulary.
243
The following table exhibits the pronouns in all their forms, in the
various dialects.
Case Absolute. Nominative. Objective.
I, as to me.
Sgau Ya, or yay
Pwo Yeu, or yawe
Bghai Yay
Mopgha Za
Toungthu
Red Karen
Kay or Gai-
kho
Taru
Thou, as
to thee.
Sgau Na, or nay
Pwo Neu, or nawe
Bghai Nay
Mopgha Na
Toungthu Na
Red Karen
Kay, or Gai-
kho
Taru
As regards
éc.
Away
Awe
Sgau
Pwo
Bghai
Mopgha
Toungthu
Red Karen
Kay, or Gai-
kho
Taru
32
if, me.
Ya, yeu seu Ya or yay
Ya, or yeu Yeu
Ya Yay
Za Za
Khwa
Va
Khye Khye
Va
Thou. Thee.
Na, orneu Na
Na, or neu Neu
Na Nay
Na Na
Na Na
Na
Na
Na
Poss. Pron.
my.
As nominative,
As nominative.
Thy.
As nominative,
He, she, ut, Him, her, it, His, her, ts,
they. them.
A,orway Au
A, or we Ku
Seu
O, or wo
Wa
A
their.
244 Karen Vocabulary.
Case Absolute. Nominative Objective.
We, as re-
gards us. We. Us.
Seau Pa way Pa, or peu Pgha
Pwo Pa we Pa, or peu Peu
Bghai Kay Ka,orwa Kay
Mopgha Kay Ka Wau
Toungthu Ne
Red Karen Pay
Kay, or Gai-
kho Pa, or ka
Taru Pa
You, as re- You. You.
gards you.
Sgau Thu way Thu Thu
Pwo Nathie Nathie Nathie
Behai Thie Thie Thie
Mopgha Nay Nay Nay
Toungthu Nathie Nathie Nathie
Red Karen Thie
Kay, or Gai-
kho Thu
Taru
[No. 4,
‘Poss. Pron.
Our.
As, Nomin.
7
)
Oo, or Hi.
As nominative.
Your.
As, Nomin.
245
Karen Vocabulary.
“a0. (a4
gasp
“yoy “
“py “UBys
1865 J
NOYS-T9t14)
noys
-OLMT
noys
ney],
nou-neyg
nvjzY-®y,
vodyey, ed-vy,
sISETN] NOYS-No9 yy
By
vyoIsey, -noys-wy,
“AU SI 400.1481],
Oo Vs ‘UYD oIsey, neys-vy,
noy noy wey 400%F AC MYT
noyoy Byodeary yeu, neyg
Yysnu NOW JOMNT AGM NT
NYT, oug
DUB Mg yeu) TOU)
ysy “MULTE = yaary OLA]
Uns “JOqTT, SUNY, nowy,
bunosyy ueyg ot N noNy
D-NUb "TRY, BT, ®L,
ny? §—“oysr)
“syunuary -hunoyz wo ‘ho
Wh
“A
oTys
-keuy
S1Ys-9InG
o1ys-Ny,
noyyos
“ory
O7gR'T orlV
ATA | vhVy
arys
-neyyog
orysery nosyy
OIMT ST OTM NE
ouyT OOS}
uw) Ke NT
NYY OST]
Avy, Avr
OL TT OMT
Noy, Ny,
noyyo no NT
Bry Ne,
‘wybdoyy = =" nua 7
x
orsy-Ae i
MENTE
o1sy]
go.
-SunY I,
ou
-910Y-v'T
Ssunejzye'T
vhery
OUEMEUINY
BlSISyery
OISye'T
OTAT YT
ous
OMN
ooy yy
Aex
ory
sung,
SINT
eal
Oe
eyy-eyy ois-vAnNy omms-kv x orsy-fkr Ayr s
HL SFys-taN o1ys-ABx orsy-Ae FUT
SY -Oly[, OLYS- OTA], OTYS-OL MIT OISY-OTM!T 44105
P-L, OLys-noyy, orgs-noyy,
orl
SOUR EH I
Oll-@y,
Kek-ey,
09-BU)
By
“OY -
BYY-B YL,
Ney]
vkd-ey,
ds)
OL
Cink
O}-8 J,
MLL
OWL,
@L
“ULLO fT
pug ‘uae
er aiee td:
ou
-TYS-
Oly
-O1ys-B
OLle T, NYT,
AeXey,
OYSON
BIOYSe y,
Ose y,
BY
-OUJOTANT
OYJOTMT
By
-OT NOY J,
oy Noy],
eAN
OIM'T
noy,y,
©N
BL
"Udl
see Rea g
Avkeye y,
SUUTSEUNY|
BIOS,
SEL
By
-OUJOTMT
OYJOLAT
ey
-OY MoT T,
oyjnoy J,
ACK
OLM'T
noy
10 “nou,
ory
"WL
‘wmybg
oIsy]
“noyy, Ary,
ory
-9ISY-By, OATOM,
pues
oyyeyey -noyy,
pop
ekeyey, -unyy
44
sso] -WAA y,
BJoISyB], UAH
oIsyey, Uday,
LIS CUNT
ou FSET
SIME wWeAeg
LIDS =
AvX eal
SIATT = MOY
noyy, oe,
oIYy{. —-OAN,
GL oud)
‘nob “ysapbug
[ No. 4s
Karen Vocabulary.
“urotpt we Aq
possaidxyy =“ wa.le yy
ut piom sodord oy
“sy dpouiaay
nou = oT-aTU
-B\Vsqy-NP. —--B [BJT
eUl-nodg
Key-Avyd
Nh EMBIENY
ney ‘NY,
Aeyq neypd-v]
-84-NU-Ly, -NU-ne} FT
ot-ACU
of-eYSy — -NeY YT
noyy-nog oy-neg
o0yf 00g
neq. ‘Vad nory
nog nory
eMC]
‘es nog
eM (T nary
V Vv
ee)
‘nyjbunoy, olny ‘wybdoyy
BN LUG p
or
~B}-VY-N]
BL]
-Sune yy
-AVYy-W
Sune} yy
sueyq
-e]-neu
orkut
“8}-00-V
99-01Aq,
~Avwpy-V
nofy,
noy.od-v4
-suneyz FT -nedu-nod Ty,
oA-SUL
atAU-v}
~ABYS-B IM
Aep-aq
~Avyy-W
ney,
vyd
-e}-NU-®y,
no&
-vu-suog ov-vAU-OT Sy “NoUu- NvY NY
oyy-sury.g OOTY y-NeL yy Hoyy-nVq
sunyd
keg
Arg
nary
Surryg
@L
Avy
nory
V
‘ON
OON,
NY
ney
neg
nog
v
“Ud WT Poy
00g
Aery
Aery
neg
nary
‘neg
V
‘Ww yb
oTUe4y
“OIN-CHL
Kep-Avyqd
“BIp-V
Dy,
neyq
-8)-NU-1y,
ero
“ey-Avy yy
oyy-neyg
00g
neq
neg ‘ no'y
oosy]T
no'T
Vy
*noby
kep-oy,
é TOT M
WoT MA,
uot],
MON
uo
Us
MOTTA
TUTM
Ag
OL
WONT
1U
*yse pbug :
247
Karen Vocabulary,
1865.]
CUL-Vy «A -O1Z,
nok-ey —s«OL-917,
BU-oyoq o]-06g
Vv awd
eryg es
ny d nog
nox ok
ood
— OOFY-No, -B-o'T
OF-nvypy
nvyy nog -No'T
nosjy-noyy Nosy-neq
Uy Rl-OW
noyy-noqy—- Oy-neg
GUI-DO (7,
‘eu-vgq Avy-AvTg
euc-nog nu-Av]q
oA
noA-BM(T
nodA-og
‘ok-og¢ ot -ART
nou oru-vy
~BY-BUY- CTA -BUL Uy
OA oo
-B-O8-AV]T — -BUL-OFF
e]-sury
© OW-oury
Avy]
a as
-SUNvY FT
neu
-BUNvY FT
oA-SUNv) TT
Oru
Avy]-Nv]S
Avy-0g
Avy-oyy-Avgy oy-oygq Avj-ex
of-og nodu-oyg
oA-Av ov-oyg nof-ex
Avy-@-O1S FT oy-egq Avy-oy.sg
Vv AV Ay
Av Joy-B4-o1q-Vq aryg
00g ooud, og
Sure X aK ox
sunyd
-B-O'T ooy ood-x-nery
SUNVIP] noyy
-no'T NEY -RVY-No'T
Sunosy,
-8u0g ooy-neg nos-noq
Avy]-nV yy
OOY-VV]ST Noy y,-nV @.
09-01hq
nodu-org
ov-o1d
arcu
Avy-ne
nou-ne(y
nou-ogq,
nod-neg
‘noA-ogf
o1u-v
-ey-vy.s-nqy vy-Avys-ey -Avy-oopy
OTAU-B} OLU-R4-NVY,
-niu-Avy -O1-nd-o1yg -oowm-ney -ney.s-Avyy~MoLOU-o 7,
oy-ney.d
Avy-o1,
‘Key-ne K 4 MOF
oT HCE
‘OT-1e K snyy,
Av]-8-OIS FONUL MOFT
Vv gon
eal LAL
00g IVON
15,0 Ie
ood-v-nory = UIT A
OYy-Ney ynoypyrAA
nesy-noeq uwooajoge
vary MOTO
oyy-neyg oaoqy
Avy-Avgq 3, @IOTL Ah,
ou-Avg O10],
o1-Avy ol TT
ort
-vy-ey-vy, Avp.109so 7X
OTU-
[No. 4,
Karen Vocabulary.
oO
“ULOTPT
ue Aq posseidxe st
aad
‘Udleyf UL LO
A0J plOM OU STL O10 T,
Pig meacienite |
“SH LDUOYT
"11Qbuno ZL,
Suneyy
ned sq
OTT
‘OM FT
Ay
Sury,
Q
ould
CAV
evad-vid-v}
-v.id-vd-opi
003-003
Bj-VUl-no(y
BULO-No
kery
nag. ‘vA (T
00y
-oMUI-neg
BI-OA\ TAT
ni
1-8}-B
‘O YU)
40 ny
neu
-98-ny g
SOTA
Te)
ny
TO]-VIL.6
~B]-T8]
-ed-ay\y
To[-eY.5-8]
To]
-SUIV} FT
nU-V
ok
Ke-oT
OU-9OTAL
oq-01
ng
Tou
-BUL-B
‘pybdopy
OTL
BY}-B-SUe NT
eral
TOW:
Ssuy
Aey-eys
-v]-neyg
Avyj-vys
-eY.o-8T
NeU-V
keg
o-AV MT
o-AVI
ynod
-AVMIT
ynoA-Av yy
Sunny
AG]
-neu-Avg
“ONT
seu
sony} 00 di
akT eru-neyg
O HN
CE CE
neu-Avysd
-BneU
-eysd-oyf,
neu
oy-Avid -Avysd-vy
-e}-0j-01hg -Av]-neg
Avad
-ey-nedu-V nou-V
Nv A. Svry
O}-VIA NVU-OUU-R FT,
‘OL, nen
ney-v]Ay eq-O]K
auc NOL
neu
04-01}-Arg
“Ua. DM PPL
-vu-AvgT
“0 yl
new
oy} NY
aril
ny
ny
Aey-eys
-E}-V}-VYY
Key-vys
-Avy-Avy
ou-V
neq
2-°W
‘eq-oUl-By,
nod-op
0
Avy
-NU-BUU-B
“nob
dye M
doayg
SULT
wy
60UTM
6 TOM
WUE
10
osye ‘puy
jou ‘oN
Sox
gAUM
‘ysebugr
SH "Joo. outes nek-neg _—os-ar'T
N ay} wor; epru oe
AVMB oye} pue Sung noA-nIT OS-O'T
‘Yap ayou AT[e1oyvY = OTY-RPT «= AUY-eL-le7-e PY
“Dy, “WYO
nyynvg “wRYg ACM, 109 FT neg
noyy ou-dIg ZIG
“pp “SURG
‘Ang wing
‘ “NOT “WRYG Rad ad oH
>
~ Nosy, “UIQ ney BMG o1g
= ‘hoy Wang Kery esq eH
S A Ln
za Ne-ouf) Sueu-oy neu-nesy;y
> noqy,
Ss SUNY-sUp) neyy-neyy, -neyg
‘NOT “TRMBUNG KOA ory oT
“ATJOOATpUT
Ajuo = poysinsurystp
ale SPo]VIp sy} Jo
OULOS UL OS pu oULOK) uory ory Avyy
OLMS-B od
‘burvahh xy ung, SULSNT —-O0S-OT NT neg
rm ‘OON “ULI, 83 NT oT
ne ‘adid 10 RON 83 NT ON,
my deoos @ yung ‘wT “BMV -OMET -00
OSy-SUleI TT
osy-Aer4)
Or SIN = OFT SIN
og
oid
-sunoyd
Uv A
ed
SUIR]
~€}-SUIRG
sureg ‘ey
ny,
SnVu-ospT
suny
-UNOSFT
eal
°d
key
AvP)
OTA YS
-8UNy, sure[q yy
SUBUL-SURrT
Suvyy)
oTN
oul-ny
BUY)
ny-nig 88-93]
Avi-neg vS-@rT
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+ This circumstance was most clearly pointed out by the Chevalier du Buat
in 1786, who made a number of experiments with pendulums formed of different
substances, but his researches, which created a great sensation at the time,
appear to have been completely lost sight of, and to have been unknown even
to Borda, who was conducting his experiments, little more than ten years after
the publication of Du Buat’s results.
The true correction for buoyancy Mr. Baily has shown to be (Phil. Trans. 1832)
B A f
aX i .0023 (£329) where f, is the height of Barometer, and ¢, the tem-
perature during the interval of observation.
pendulum, and is determined from the formula
Ne Ne
gp” [1 + .0023 (t°—32°)]in which N’ is the number of
C is a constant for the same
(Ch
vibrations in a mean solar day, B’ and t’ the barometer and thermometer read-
ings, im oir; and N,” B,” t’’ the same quantities in a highly rarified medium,
Pie xt’)
pres:
1865.] The Proposed Pendulum Operations for India. 255
called, depends also on the state of the atmosphere, it is necessary for
its calculation, to record the readings of the barometer, when the
observations are taken in air.
The last correction is for the height of the station of observation
above the mean sea level. The force of gravity varying inversely as
the square of the distance from the earth’s centre, a pendulum swung
at a certain elevation above the sea, will make fewer oscillations in a
day than at the level of the sea, and a correction has to be added on
this account. Dr. Young, however, demonstrated that the correction
computed on this consideration alone, was too large, as it neglected
the attraction of the elevated mass itself, and he showed how this
might be approximately allowed for.*
The general principle followed in determining the length of the
seconds pendulum, is to observe the number of vibrations made by a
pendulum of known length, in a mean solar day ; then the length of
the seconds pendulum is found by multiplying the length of the given
pendulum, by the square of the number of its vibrations in a day, and
dividing by the square of the number of seconds in a day.
The number of vibrations is generally determined by the method of
coincidences. The detached pendulum is placed in front of a good
clock, and adjusted to such a length as to gain or lose, (the latter
generally) two beats upon the clock in some convenient time, 5 to 10
minutes. Suppose the pendulums to be started together, then the
longer one of the two will be left behind by the other, the distance
between them continually increasing, until at length they will be at
opposite extremities of their arcs of vibration at the same moment:
the longer pendulum has now lost one oscillation on the shorter one,
and both are apparently going at the same rate, but in opposite direc-
tions; after a short time they will begin to approach each other, the
distance between them gradually diminishing, until they both appear
to coincide. It is clear that between two consecutive coincidences the
* This correction is given by the formula — h zw, where n denotes the num-
r
ber of oscillations in a mean solar day, 7 the radius of the earth at the given
station, h the height of the station above the mean level of the sea: wis an
unknown quantity determinable from theory; on the assumption that the mean
density of the earthis 6.5 and that of the surface 2.5 Dr. Young (Phil. Trans-
actions 1819) showed that the correction for a station on a tract of table land
would be reduced by ird or that the correction = 2 nh.
256 The Proposed Pendulum Operations for India. [No. 4,
jonger pendulum will have lost two oscillations on the shorter one.
Hence all that is requisite in practice, is to observe as accurately as
possible the intervals between the successive coincidences ; the number
of vibrations made by the clock pendulum is determined by obsery-
ations of the sun or stars, and then the number made by the detached.
pendulum is computed by simple proportion.*
The first pendulum observations of which any account is preserved
are those made by Picard at Paris and Uranienburg (Tycho Brahe’s
observatory) and those by Richer at Cayenne in 1672. These last
observations are said to have attracted Newton’s attention, as they
proved the variation in the length of the seconds pendulum in different
latitudes, and it is generally stated that Richer made the discovery by
accident. But it appears from Picard’s address to the French academy
in 1671, that a variation had been already observed, and it is probable
that Richer’s mission was undertaken partly with a view to throw
light on the subject. Picard stated that ‘‘ from observations made at
London, Paris, and Bologna, it would seem as if the seconds pendulum
required to be shortened in approaching the equator, but that on the
other hand, he is not sufficiently convinced of the accuracy of those
measurements, because, at the Hague, the length of the seconds
pendulum was found to be quite the same as at Paris, notwithstand-
ing the difference of latitude.’’+
Near the end of the 18th century, Borda made his celebrated expe-
riments for determining the length of the seconds pendulum at Paris.
His apparatus, whichis named after him, consisted of a spherical ball of
platinum attached by grease to a brass cap which had been truly ground,
so as to fit it perfectly. The object of this attachment was to enable
the observer to turn the ball round in the cap at pleasure, so as to
destroy the effects of unequal density in different parts of it. A fine
wire carrying the cap was fastened to the lower end ofa small
cylinder, passing through the knife edge, which carried on its upper
end a small moveable weight, by adjusting which the knife edge
and cylinder could be made to vibrate independently in the same
* If + = daily rate of the clock and I the mean interval of the coincidences,
then the number of oscillations made by the pendulum in a day = 1
— = (86400 + r) the lower sign is to be used when the
clock is losing.
+ Cosmos Vol. IV. page 25, Sabine’s translation.
1865.] © The Proposed Pendulum Operations for India. 257
time as the pendulum, so that their effect might be neglected in com-
puting the length of the simple pendulum. When in use, the knife
edge rested upon a steel plate. The number of vibrations per diem,
were ascertained by means of a clock, but Borda made a great improve-
ment on the old method of counting the coincidences. He fixed a
straight edge vertically, so as to coincide with the pendulum wire at
rest, when seen through a telescope placed opposite. A cross was
made on the bob of the clock pendulum, and the observation consisted
in noting the times when the wire and cross disappeared together
behind the edge. After a series of coincidences had been observed
the length of the pendulum was measured by means of a horizontal
steel plate, which was screwed up from below, so as just to touch the
ball: then the pendulum was removed, and a bar, whose length had
been carefully compared with a standard, inserted in its place. The
bar had a 7 head, of which the lower surface rested on the upper steel
plate, and a graduated rod, sliding on the bar, was adjusted to contact
with the lower plate. The diameter of the platinum ball was then
measured by means of the same slider, by placing it on the steel plate
for the purpose; the brass cap and wire were then weighed. The
apparatus was enclosed in a glass case, and the temperature was care-
fully recorded. All necessary corrections were applied, excepting the
true one for buoyancy. The whole process, which required very great
delicacy, had to be repeated, and the length of the corresponding
simple pendulum computed after each series of observations. Borda’s
pendulum was about 12 feet in length.
His method was followed by M. M. Arago, Biot, and Chaix, at
Formentera, the southernmost station of the French arc, with this
exception that they used a pendulum of only 3 feet in length. These
observations were extended by Biot in 1817°to Leith, and Unst in the
Shetlands, and in conjunction with M. Mathien, he observed at
Dunkirk, Paris, Clermont, Bordeaux, and Figeac. From these opera-
tions, Biot deduced an ellipticity of 33;.
In about 1809, Captain Warren made some observations at the
Madras observatory with a pendulum formed of a leaden ball suspended
by a fibre made from the plantain leaf. The vibrations were counted
and an assistant noted the times, from an astronomical clock. In order
to measure its length, he attached some glass plates to a wall, and set
258 The Proposed Pendulum Operations for India. [No. 4,
off on them a scale, transferred from Colonel Lambtons’s scale; the
length was then measured by a pair of beam compasses. The length
of the seconds pendulum was found to be 39.0263 inches of this
scale in air.
In 1818, Captain Kater published his determination of the length
of the seconds pendulum in London at Mr. Browne’s house, Portland
Place, taken for the purpose of fixing the standard of English
measures. His method was founded on the dynamical theorem due to
Huyghens, that the centre of oscillation, and axis of suspension, are
reciprocal in the same body; that is, if the body be suspended at its
centre of oscillation, the former axis of suspension will pass through
the new centre of oscillation, and the body will vibrate in the same
time as before. The distance from the axis of suspension to the point
called centre of oscillation, is equal to the length of the simple
pendulum.
In 1822, the English Government sent out an expedition under
Captain, now General, Sabine, for the purpose of extending the
enquiry commenced by Captain Kater; for both Kater and Biot had
come to the conclusion, from a discussion of their experiments, that
no decisive result of the earth’s ellipticity could be obtained from
them, on account of the smallness of the comprised are, and the
variations of local density. Captain Sabine visited thirteen stations
between Bahia, S. Lat. 12° 59’ to Spitzbergen N. Lat. 79° 50’.
He had with him three pendulums of Kater’s invariable pattern,
which were all swung at each station. Besides these he had the two
clocks and attached pendulums which he had already used on his
arctic voyages. His method of observation was similar to Captain
Kater’s; all the pendulums were swung in London at Mr. Brown’s
house, both before and after the expedition.
Captain Sabine subsequently determined the difference in the
number of vibrations made by an invariable pendulum between London
and Paris, London and Greenwich, and London and Attona. He also
determined the true buoyancy correction for Kater’s convertible
pendulum.
In 1825 M. Bessel made his experiments for determining the length
of the seconds pendulum at Konigsberg, with an apparatus constructed
and partly designed by Repsold the celebrated artist of Hamburg
1865.] The Proposed Pendulum Operations for India. 259
The apparatus was contrived so as to avoid any uncertainty in the
centre of oscillation of the pendulum, as well as any error in the
measure of its length, by observing the times of vibration of a pen-
dulum ball suspended alternately by two wires, whose difference in
length was known.
A toise was set upright on a narrow horizontal plane firmly fixed to
a perpendicular iron bar, and the contrivance by which the pendulums
were suspended could be placed either on the horizontal plane, or on
the top of the toise itself, so that the effective lengths of the wires
differed in the two cases by an amount exactly equal to the length of
the toise. The wires, which were of steel, were attached to a thin
strip of brass which unwound itself over a small cylinder. The pen-
dulum, thus suspended, described the curve called the evolute of the
circle. At the lower end of the iron bar, there was a micrometer
serew for measuring small differences in the height of the ball.
The system of observation was as follows. At the commencement
of a series of coincidences with the longer pendulum, the thermometers
attached to the toise were recorded, and the reading of the lower
surface of the ball was taken with the micrometer screw ; the pendulum
was then set in motion, and after a sufficient number of coincidences
had been observed, the readings of the ball and thermometers were
again taken. Exactly the same process was then gone through with
the shorter pendulum: then from the times of vibration of the two
pendulums, whose absolute lengths were unknown, but whose difference
in length was accurately known, the length of the seconds pendulum
was easily computed.* There were a great many minute details to be
attended to, all of which were carried out with the greatest ingenuity
* Let t, &1, be times of vibration and length of longer pendulum.
to le ” ) 3” shorter 9
1, — 1, = difference in length = a
L =length of seconds’ pendulum,
1 L
a a i We er
Pee
Peas bes Gon L, oF $2 — t,?
peg L ee UM ae a
Again me pion G75 278
260 The Proposed Pendulum Operations for India. [No. 4,
and nicety, and all conceivable sources of error were considered and
their effects computed and allowed for.
The coincidences were observed in a slightly different way from any
preceding method. ‘The pendulum was enclosed in a wooden case,
faced with glass to keep out currents of air, as well as to preserve as
constant a temperature as possible; the clock was placed about 84
feet in front of the pendulum, and between the two, the object glass
of a telescope was adjusted to form an image of the detached pendulum
in the plane of the clock pendulum, to enable them both to be seen
simultaneously through the observing telescope, which was set up at a
distance of about 15 feet. On the wire of the detached pendulum
was fixed a small brass cylinder, painted black and called the coinci-
dence cylinder; it weighed something under 4 grains, and could be
brought exactly opposite the scale for measuring the arc of vibration.
Captain Kater’s pendulum consisted of a bar of plate brass 1.6
inches broad and }th of an inch thick: two knife edges of the hardest
steel, attached to solid pieces of brass, were fixed to the bar at a dis-
tance of rather more than 39 inches from each other ; when the pen-
dulum was in use, these knife edges rested on horizontal planes of agate.
At one end of the bar, immediately below the knife edge, was a large
flat brass bob firmly soldered to it ; and on the bar, between the knife
edges, were two sliding weights. The plan of operations was to
observe the number of vibrations per diem, made by the pendulum
when suspended, first, by one knife edge, and then, by the other ;
and if these numbers were not identical, to make them so, by means
of the sliding weights. The distance between the knife edges, that is,
the length of the corresponding simple pendulum, was then measured
by a micrometric arrangement. The method of observing the number
of vibrations was as follows; to each extremity of the pendulum, a
light deal tail-piece, well blackened, was attached ; and on the bob of
the clock pendulum a white paper disc, equal in diameter to the
breadth of the tail-piece, was fastened; the detached pendulum was
now placed in front of the clock, and both pendulums being at rest,
a telescope was alined, so that the blackened tail-piece exactly covered
the paper disc. The telescope was also fitted with a diaphragm, con-
sisting of two perpendicular cheeks, which could be adjusted so as to
become tangents to the disc. Now, if both pendulums be set in motion,
1865.] The Proposed Pendulum Operations for India. 261
the detached pendulum vibrating slower than the clock one, the tail-
piece will be seen to pass across the diaphragm, followed by the
white disc; at each succeeding vibration the disc follows closer and
closer, first touching it, and at last becoming completely eclipsed by
(4
it. The exact time of this event, called a ‘“ disappearance,” is noted ;
aiter a few more vibrations, the dise will reappear preceding the tail-
’ is also noted ;
piece ; the time of this event, called the ‘‘ reappearance,’
and the mean of the disappearance and reappearance, is taken as the
true time of coincidence. It is immaterial in this method of observ-
ation, whether the detached pendulum vibrates faster or slower than
the clock pendulum, but it is a sine qué non that its arc of vibration
be less. The result, introducing all corrections, except the true one
for buoyancy, was 39.13929 inches, which is still the received length,
although General Sabine in 1831, showed, by swinging the pen-
dulum in air and in vacuo, that the buoyancy correction was different,
according as the heavy weight was above, or below, the plane of
suspension.
Captain Kater, in the following year, 1818, made a series of expe-
riments at the principal stations of the English Survey, from Shanklin
in the Isle of Wight, to Unst in the Shetlands. He used in these
observations a pendulum of a different pattern, known as “ Kater’s
invariable pendulum.” With it, it is not possible, nor was it intended,
to determine the length of the seconds’ pendulum, but it is essentially
a differential instrument, and is used for measuring the differences
in the number of vibrations at different stations. With these dif-
ferences, ii at any one station the length of the seconds’ pendulum
has been already determined, the corresponding lengths at the other
stations can be ascertained. The invariable pendulum, is of the same
dimensions as the convertible one, but is without the second knife
edge, and tail-piece, and the sliding weights. The mode of observation
is exactly the same. Captain Kater deduced values of the ellipticity,
from consecutive pairs of stations; he considered 1, as a probable
value (the same as M. Biot’s); but he remarks on the difficulty of
deriving a satisfactory determination, unless the extreme stations
comprise an arc of sufficient extent to render the effects of irregular
local attraction insensible.
In 1821-22, some very good observations were made by Mr,
262 The Proposed Pendulum Operations for India. [No. 4,
Goldingham, at Madras, and afterwards at a small island called Pulo
Gaunsah Lout, lying nearly on the equator in Hast Longitude 98° 50’.
The pendulum used was an invariable one, and observations were first
taken with it in London, by Captain Kater. Fyrom the observations
at Madras and London, Mr. Goldingham deduced an ellipticity of 54,.
Captain Basil Hall, assisted by Captain (then Lieutenant) Henry
Foster, made a series of experiments with an invariable pendulum in
1820-23, at Galapagos, San Blas (Mexico), Rio Janeiro, and London
(Mr. Browne’s house). Comparing the results at each of his own
stations, with each of Captain Kater’s, he deduced ellipticities of 34,,
=. and =|.
314) 302°
In 1822, Sir Thomas Brisbane took with him to Paramatta (near
Sydney,) an invariable pendulum that had previously been swung in
London, at Mr. Browne’s house. He deduced ellipticities of 51, and
rhe comparing his observations with those of Kater in Tose and
t Unst.
In 1817, the French Government fitted out a scientific expedition
under the command of Captain Freycinet, who was furnished with
three invariable brass pendulums, one of which was similar to Captain
Kater’s pattern, and the other two had solid cylindrical rods instead
of a flat bar. He had also a fourth pendulum, with a wooden rod
formed of two plates of deal firmly clamped together. Instead of a
clock he used an astronomical counter, (“‘ compteur astronomique’’)
whose beats could be adjusted to synchronism with those of the pen-
dulum. The counter had a dial, which showed hours, minutes, and
seconds, so that by comparing the time shown by this ‘ compteur”
with that of a chronometer, he obtained the number of vibrations
made by the pendulum in a certain interval, generally an hour or 40
minutes. The pendulums were first swung at Paris, and afterwards
at Rio Janeiro, Mauritius, Guam (one of the Ladrone Islands), Mowi
(one of the Sandwich Isles), Cape of Good Hope, Port Jackson,
Kawak (an island under the line, north of New Guinea) and Malouine
or Falkland Isles. Rejecting the determinations at the Mauritius,
Guam and Mowi, as they appeared affected to a remarkable degree by
local influences, Captain Freycinet deduced an ellipticity of 545 from
all four pendulums.
On the return of Captain Freycimet, the French government sent
1865 ] The Proposed Pendulum Operations for India. 263
out another expedition under Captain Duperrey. He was supplied
with two of Captain Freycinet’s brass pendulums, viz. one with a
cylindrical rod, and the one on Kater’s principle. He observed at six
stations, viz. Ascension, Mauritius, Port Jackson, Falkland Isles,
Toulon, and Paris. In deducing the ellipticity, he combined his
results with those of Freycinet only, and obtained values varying from
zee to on 0 0°
During Ross’s voyage to Baffin’s Bay in 1818, some observations
were taken at Brassa, in the Shetlands, and at Hare Island, with a clock
fitted with an invariable pendulum vibrating on a knife edge, which
rested on hollow agate cylinders. Observations were repeated at these
stations, and a further set taken at Melville Island, on Captain Parry’s
first voyage to the North Pole in 1819-20. Captain Sabine conducted
both these experiments, using the same instruments.
The ellipticity deduced from the experiments at Captain Sabine’s
stations was 51,.z, from the same combined with Kater’s ,1,., and
combined — with Biot’s 51,., and from a general combination of
all of these, 54,.z. The observations of the detached pendulums only
were used in these determinations ; for though the clock pendulums gave
closely coinciding values of ellipticity, still being acted on by other forces
than gravity, their results are less reliable, and are only valuable in so
far as they afford an independent corroboration of the other results.
Captain Sabine was not at first aware of the strict expression for the
reduction to a vacuum, but after the publication of Bessel’s observ-
ations in 1828, he had an apparatus specially constructed, and ascer-
tained the proper correction practically, by swinging his pendulums
In air, and in vacuo.
The error from this cause, however, proved to be trifling, owing to
his observations being strictly differential, so that only the differences
between the corrections by the old and new formule entered.
The most widely differing buoyancy corrections at any of his or
Captain Kater’s stations of observation, computed by the old formula
were + 5.75 vibrations at Sierra Leone and + 6.27 vibrations at
Spitzbergen, in a mean solar day. These corrections, multiplied by
the proper factor, 1.65, to reduce them to the new formula became ++
9.52 and + 10.38 vibrations, so that the number of vibrations in a
mean solar day at Sierra Leone required to be increased by (9.52 — 5.75)
264 The Proposed Pendulum Operations for India. [No. 4,
3.77, and at Spitzbergen by (10.388 — 6.27) 4.11 vibrations. But the
acceleration between the stations would only be increased by the
difference between these numbers, or by 0.44 vibrations. It so happened,
however, that even this difference was too large, for in the deduction
of the temperature correction, the old buoyancy formula had of course
been used; on applying a correction on this account, the above dif-
ference required to be reduced by 0.36 vibrations so that the whole
error on the acceleration of the pendulum between Sierra Leone and
Spitzbergen was only + .08 vibrations.
On this scale a black streak was painted, in the middle of which a
space was left white, equal to the diameter of the coincidence cylinder,
so that when the pendulum was at rest, the cylinder exactly covered it.
Again, to the bottom of the clock pendulum a piece of blackened
paper was attached, in which a hole had been cut of such a size that
when both pendulums were at rest, it exactly coincided with the image
of the white space on the black streak: hence when the pendulums
were moving im coincidence, the coincidence cylinder was visible
through the hole, and completely eclipsed the white space. Bessel’s
result was expressed in lines of the toise of Peru, the standard used in
the measurement of the Peruvian arc.
In publishing these experiments, M. Besse! pointed out the true
correction for buoyancy, which he had investigated by swinging in air
two spheres of equal diameters, but of different densities, one being of
brass and the other of ivory, suspended by a fine steel wire; and again
by swinging the same brass sphere first in air and then in water.
These experiments showed that the old formula for reducing obsery-
ations in air to a vacuum gave too small a correction, and that it should
be multiplied by a factor.
Mr. Francis Baily made a long series of experiments on the cor-
rection for buoyancy, which were published in the Philosophical
Transactions for 1832. He used about 80 pendulums, all differing in
form, weight, and mode of suspension. From these experiments he
deduced factors for pendulums of almost every description that have
ever been used, and computed also the weight of the air adhering to
each, in other words deduced the wibrating specific* gravity of the
* “The vibrating specific gravity of a compound pendulum is ordinarily found
“a follows; Let d’, J” d/” ... denote the distance of the centre of gravity of each
, ee
1865.] The Proposed Pendulum Operations for India. 265
pendulum. He concluded from all his results, that even if a pendulum
is formed of materials having the same specific gravity, yet if it be
not of an uniform shape throughout, each distinct portion must be
made the subject of a separate computation, in order to determine the
correct vibrating specific gravity of the whole body, since each part
will be differently affected by the surrounding air.
The last extensive series of experiments were those taken in
1828-31 by Captain Henry Foster, who was sent out on a scientific
mission by the Board of Admiralty. He took out with him four
invariable pendulums of different metals, two of Captain Kater’s
pattern, and two of Baily’s convertible pattern. These last consisted
of a plain straight bar, 2 inches wide, $ inch thick, and 5 feet 24
inches long, having two knife edges 39.4 inches apart, but no heavy
bob or sliding weights, as in Captain Kater’s pattern ; the synchronism
was adjusted by filing away at one end of the bar; Baily’s intention
was, that the pendulum should either be used as two different invari-
able pendulums, or applied as a single convertible one for absolute
determinations, at any station. The objection to the form is, that both
the knife edges must be exactly perpendicular to the bar, or error is
entailed, as the bar is not flexible like Kater’s. Captain Foster
swung pendulums at all his stations, 14 in number, which were chiefly
in the southern hemisphere. He made a set of observations at Mr.
Browne’s house before the voyage; on the return of the pendulums
to England, they were again swung at the same place, but by Mr.
Baily, Captain Foster having been most unfortunately drowned in the
River Chagres, in February 1831, just as his mission was completed.
His observations were reduced by Mr. Baily, who obtained from them
an ellipticity of 5,4.5-
About this time the Russian government sent out an expedition
under Captain Liitke, who used an invariable pendulum, formerly used
by Captain Basil Hall. He swung it first at Greenwich, and after-
* body respectively from the axis of suspension : w’, w’”, w’, ... the weight (in air)
* of each body: s’, s’, s’”’, ... the specific gravity of each body determined in the
“usual manner. Then will the required vibrating specific gravity of the pen-
* dulum be
wd wld? + wd” +...
S=w’ d Oe oee idan ae
Tagua W See
U sf?’ s
s
(Philosophical Transactions, 1832.)
266 The Proposed Pendulum Operations for India. [No. 4,
wards at Ualan, in the Caroline islands, Guam, Bonin island (to the
south-east of Japan), at Sitka in Russian North America, at Petro-
paulowski, Valparaiso, St. Helena, and St. Petersburg. He deduced
an ellipticity of 53, from his observations.
Schumacher, the celebrated astronomer of Altona, conducted in
1829-30, a series of experiments with Bessel’s apparatus, at the castle
of Guldenstein, in order to determine the Danish standard, which was
to be a certain fractional part of the length of the seconds pendulum,
at the level of the sea, in latitude 45°. In order to estimate the in-
fluence of the air, he used, instead of a ball, a hollow cylinder of
platinum, made by Repsold, inside which a second solid cylinder,
also of platinum, fitted perfectly true. The outer cylinder was closed
by covers of the same diameter screwing on to it, which were both
perforated ; the clamp holding the wire was fastened on to the top,
and into the bottom was screwed a point with which the contact was
made in measuring the height of the cylinder by the micrometer
screw.
The pendulum was swung under four different circumstances, viz.
the long pendulum, with and without the inner cylinder, and the short
pendulum, also with and without it; and as exactly the same surface
was exposed to the air in each case, the influence of it could be
computed, which was done by a formula deduced by Bessel. The
reduction of the observations was made by Professor Peters. One
novelty was introduced, viz. that of computing out the attraction of
the ground on which the observations were taken. A square space
having a side of 600 toises (1279 yards), in the middle of which the
observatory was situated, was subdivided again into 36 squares of 100
toises (213 yards) a side; in each of these borings were made, and
specimens of the earth removed and their specific gravities determined ;
as these were very nearly the same, a mean of the whole was taken.
The height of the floor of the pendulum room was 343 toises (220.6
feet) above the mean sea level, and the attraction of this plateau of
the earth’s crust introduced a change in the length of the second’s
pendulum of 0.000215 English inches.
Carlini, whilst measuring the Piedmontese are in 1821-23, took a
series of pendulum experiments at the Hospice on Mount Cenis, with
the view of determining the density of the earth. His pendulum was
1865.] The Proposed Pendulum Operations for India, 207
formed of a heavy sphere suspended by a wire, which was attached to
a kind of inverted stirrup ; in the part corresponding to the foot plate
there was fixed a wheel with a sharp edge turning on its axis. This
wheel was placed on a grooved plate and formed the knife edge for
suspension ; the arrangements for observing were similar to Bessel’s,
Corresponding observations, though not with the same apparatus, were
taken by Biot and Mathien at Bordeaux. The result was a density
of 4.95.
One more attempt to determine the density of the earth by means
of the pendulum was made in 1854 by the Astronomer Royal, Professor
Airy, at the Harton Colliery pit. Two invariable pendulums were set
up in the same vertical line, one at the top, the other at the bottom of
the pit, and their coincidences with the pendulums of two clocks were
simultaneously observed, the relative rates of the clocks being deter-
mined by a galvanic apparatus. After each series of coincidences the
pendulums were interchanged. The distance between the upper and
lower pendulums was 1256 feet ; a careful description of the interven-
ing strata was prepared and specimens submitted to Professor W. H.
Miller who determined their specific gravities. The acceleration of
the seconds’ pendulum below was 2.24 seconds per diem, and the
resulting mean density of the earth was 6.565.
The best value oi the earth’s ellipticity as yet deduced from pendu-
lum observations is undoubtedly that of Mr. Baily’s. He combined
all the observations taken with invariable pendulums, and aiter apply-
ing to them all corrections, obtained a mean ellipticity of ;f;.5. The
latest value of the same, from geodetic observations, is Captain
Clarke’s, R. E. which includes the new Russian arc and is zgh55-
The ellipticity obtained from observations of precession and nutation is
sos5 (Aiy’s tracts).
The apparatus for the Indian experiments, consists of two invariable
-pendulums on Kater’s principle, a vacuum apparatus with air pump
for exhausting, an astronomical clock by Shelton, a good battery of
thermometers and a transit instrument. Both pendulums have already
done good service: one having been used by General Sabine in his
extensive range of experiments, the other by Professor Airy in his
Harton pit experiments ; they cannot be considered, however, to have
retained their original length, as their knife edges have been reground,
39
268 The Proposed Pendulum Operations for India. [No. 4,
Each is composed ofa bar of plate brass 1.6 inches wide and rather less
than an ith of an inch thick; a strong cross piece of brass is rivetted
and soldered to the top to hold the knife edge, which consists of a
prism of very hard steel, passing through the bar and adjusted at right
angles to its surface. The prism is equilateral in section, but the edge
on which it vibrates is ground to an angle of about 120°; the length
of the bar from knife edge to the extremity is about 5 feet 14 inches.
At 3’ 22” from the knife edge, a flat circular bob, also of brass
nicely turned and pierced in the direction of its diameter, is firmly
soldered on; the part of the bar beneath the weight, called the tail-
piece, which is about 17” in length, is reduced to a breadth of 0.7 of
an inch and is varnished black, in order to contrast better with the
white disc on the clock pendulum, in the observation of the coinci-
dences.
The knife edges rest on agate planes set in a solid brass frame,
which is provided with three levelling screws. On the outer side of
each plane are Y’s, which are moveable in a vertical direction by
means of an eccentric ; the knife edges rest in them when the pendu-
lum is not in use, and by their means the observer is enabled to lower
the pendulum down gently so as to bear always on the same parts of
the agate planes. Each pendulum has its own set of planes, and will
give different results if swung on any others.
It has been decided to swing the Indian pendulums in vacuo, in
order to secure the following advantages. When the pendulum has
been set in motion, it will vibrate for a whole day ; its temperature
will be more equable; it will not be disturbed by currents of air;
and errors in the formula for the correction for buoyancy are unimpor-
tant. The vacuum apparatus consists of a cylinder of sheet copper
about 1 foot in diameter and rather more than 5 feet long, with
hemispherical caps, the upper one of glass and moveable, the lower
one of sheet copper and soldered to the cylinder. The upper end of
the cylinder carries a strong brass plate, to which are attached the
frames containing the agate planes and a bar of the same metal and
shape as the pendulums ; placed side by side with a pendulum inside the
apparatus, the bar and pendulum will be of the same temperature, and
it is evident that thermometers attached to the former will give the
required temperature of the latter. ‘Two delicate thermometers are
1865.] The Proposed Pendulium Operations for India, 269
attached to the bar, their bulbs being sunk in the metal. at points
equidistant from. each other and the ends of the bar. The stem of the
upper thermometer is inverted, and placed side by side with that of
the lower thermometer, in order that. they may both be viewed
through a moderate sized glass plate let into the cylinder. In the
lower part of the cylinder there are four other windows, two on the
line of the pendulums, to enable their coincidences.to. be observed ;
the other two at right angles to these, to. give additional light and
enable the observer to ascertain whether the detached pendulum is
vibrating truly without wabble. There are two scales fixed at right
angles.to each other, inside the cylinder, on a level with these windows,
ene of which is used for measuring the arc of vibration of the pen-
dulum, and the other to measure the distance of the pendulum: from
the former scale, which is necessary to furnish the correction for
parallax in the readings of the are of vibration: it is useful also in
placing the pendulum at a constant distance from the clock, which is
found convenient in practice.
The upper 4’ of the cylinder is made of greater thickness than the
rest, and at top is-a strong projecting flange which is intended to rest
en a strong cast iron frame made in two pieces, so as to grip the
cylinder round the thicker part just below the flange;: the halves of
the frame are then firmly bolted together with nuts and screws. The
upper surface of the flange is ground perfectly true to. receive a bell
glass, the cap. already mentioned, which is like the receiver of an.
ordinary air pump. ‘The eccentric for raising and lowering the pen-
dulum. on to the agate planes passes through a stuffing box in the
upper part of the cylinder. Motion is imparted to the pendulums by
means of a fork and crutch turned by a spindle which passes through
another stuffing box.
The clock with which the vibrations are compared is firmly secured.
to a wall, and the vacuum apparatus is erected in front, at a distance,
of about 2 feet from it. The diaphragm for limiting the view of the
disc is fitted inside the clock case.
The telescope for observing the coincidences is placed on a small
masonry pier at a distance of about 8 feet from the vacuum apparatus
and is mounted so-as to slide laterally on a graduated horizontal bar ;
it has also a slight vertical motion. The thermometers and barometers
270 The Proposed Pendulum Operations for India. [No. 4, -
are read from alongside of this pillar by means of a cathetometer, viz. ’
a telescope sliding up and down on a vertical rod. The object of this’
is to obviate the ill effects of any defect in the isolation of the appara-
tus, as well as the influence of the observer’s person on the thermo-
meters.
As the disc on the bob of the clock and the tail-piece of the de-
tached pendulum are too far apart to be viewed simultaneously by the
telescope, a lens is placed between them, so as to throw the image of
the white disc upon the tail-piece of the pendulum. The vacuum
cylinder and all its adjuncts, air pump, &c. were made by Adie, and
are the only new portions of the apparatus.
The method of operation is as follows. After setting up the clock,
the vacuum apparatus is inserted in the iron frame and suspended.
either on wooden trestles or masonry piers; the frame is roughly
levelled; the temperature bar is fixed in position; the agate planes
are screwed on firmly to their bed plate, and are very carefully levelled
by means of delicate spirit levels provided for the purpose. A pen-
dulum is now inserted and let down upon its planes, but the clock
must not yet be set in motion. The telescope is next set up on the
prolongation of the line which passes through the two pendulums,
when both are at rest. For this purpose it is moved laterally on its
graduated support, until a very small portion of the paper disc, on the
bob of the clock pendulum, is visible on one side of the tail-piece of
the detached pendulum. The reading is noted, and the telescope is then
moved in the opposite direction, until an equal portion of the disc is
visible on the other side of the tail-piece ; the reading is again noted,
and the telescope is set to the mean position. The pendulum is then
removed, andthe diaphragm in the clock case adjusted, until its cheeks
are tangents to the disc. The pendulum may now be replaced, and
nothing remains to be done but to exhaust the air out of the apparatus
and to set the pendulums in motion.
The observations are made in exactly the same way as already de-
scribed in the account of Captain Kater’s apparatus; the times of the
disappearance and reappearance are both noted, and the mean taken as
the true time of coincidence. The arc of vibration is then determined
by noting the reading of the arc, when it is cut by the same edge of
the tail-piece on each side of the vertical line. The thermometers and
1865.] The Proposed Pendulum Operations for India. 271.
barometer are read by means of the cathetometer. It is usual to
observe not every coincidence, but the first three consecutive coin-
eidences, and then the 11th, 12th, 13th, then the 21st, 22nd, 23rd, and
so on; aiter observing the first two or three, the times of the after
coincidences can be easily computed with sufficient accuracy to intimate
when the observer should be ready to note them.
Tt is intended to have observations made generally along the Great
Are at stations 2” apart in latitude, and at other points where it may
be desirable to obtain data regarding local variations in the intensity
of gravity.
The pendulum experiments in this country will afford an independ-
ent value of the ellipticity of the Indian are. It is also hoped that
they will throw some light on the existing discordances between the
astronomical and geodetic latitudes of the Indian survey.
The amount of the deflections of the plumb line, due to the Hima-
layas and elevated table lands to the north of India, have been computed
by Archdeacon Pratt for the different terminal stations of the Indian
ares; but these determinations are so much in excess of the results of
the survey, that it is evident that the effects of the mountain attraction
must be in a considerable degree compensated, either by a deficiency
of density in the strata to the north, or by an excess of density in the
strata to the south of the survey stations.
Now the peudulum can undoubtedly be made the means of showing
whether the compensation is to be attributed to either of these causes ;
for, whilst the effect of a distant range of mountains on the vibrations
would be quite inappreciable, any local variation in the density of the
underlying strata would show itself most unmistakably ; so that by
taking observations both at a normal station, and at a few points in
its vicinity symmetrically situated around it, should there be any con-
siderable excess or defect in the density of the strata to counteract
the disturbance due to the mountain mass, the pendulum observations
would not fail to point it out.*
_
* Professor Stokes remarks in his letter on these operations: ‘‘ The pendu-
“lum no doubt indicates only the vertical component of the disturbing force,
© whereas it is the horizontal component in the plane of the meridian that aftects
“the measures of arcs ; at any one station, of course, a horizontal disturbance
“may exist without a vertical disturbance, and vice versa ; but in a system of
© stations disturbances of the one kind must necessarily be accompanied by dis-~
272 The Proposed Pendulum Operations for India. [No. 4;
The Indian operations will eventually be combined with those taken
previously with similar instruments in other parts of the world, to
deduce the ellipticity of the earth’s mean figure. Both Sir Jokn
Herschel and Professor Stokes have remarked, in their letters on the
proposed Indian operations, that almost all observations hitherto made
have been taken at stations either on islands or coasts, so that a series
along the centre of a continent is very much needed. A complete set
of observations has been already taken at the Kew observatory by.
Mr. B. Loewy, with the Indian apparatus; and on the completion of
the experiments in this country it will be returned to Kew, in order
that final observations may be taken, to show whether the pendulums
have undergone any change in the interim.
It is to be hoped, however, that so good an opportunity will not be
lost cf extending these observations to stations easily accessible from
India, though not included within its limits. On this head Professor
Miller’s opinion may be quoted at length, “Much would be added to.
the value of the observations made at the stations of the Indian
survey, if, before the pendulums were brought back to England,
observations could be made with them at some other points, especially
points nearer to the equator, such, for stance, as the south coast of
Ceylon, Singapore, or on the coast of Borneo. Another accessible
point, interesting from being in a long line of depression, where a
Jarge gravitation might be expected, is Aden.”
The intention of the Russian government, to have similar obser-
vations made along the Russian arc, has already been alluded to-
Ii, aiter the return of the pendulums to England, they were to be
swung at one of the Russian stations, it will be possible to. combine
the Russian with the Indian operations, and deduce a value of the
earth’s ellipticity from exclusively Continental observations, extending
from Cape Comorin to the northernmost part of Finmark.
*‘+urbances of the other kind. Indeed it is theoretically possible, from the ver-
“tical disturbances, supposed to be known, actually to calewlate the horizontal
“ disturbances, and that without assuming anything beyond the law of universal
“ sravitation. Actually to carry this out, would probably require observations
“to be made at stations more numerous than can be thought of, but the fact of
“its possiblity shows how severe a check pendulum observations are capable of
“ exercising on the results of geodetic observations.”
——
1865.] Land and Freshwater Shells from the Shan States, 273
Notes on a collection of Land and Freshwater Shells from the Shan
States —Oollected by F. Fuppnn, Esq., 1864-65.—By W. Turoxatp,
Junior, Esq.
[Received 17th July, 1865. ]
Mr. Fedden having kindly placed in my hands for examination a
small collection of shells from the Shan states, I am led to offer the
following brief remarks, though I have not the requisite time at
my disposal at present, to describe the many novelties which the
collection contains, most of which, however, Mr. Benson will shortly
describe in the Annals of Natural History. Although the condition
of many of the specimens is very poor, for purposes of describing
specific characters, and many species are represented by a single
individual, still the collection affords conclusive evidence of the great
richness in terrestrial mollusca of the region where it was made, and
interesting proof of the distribution of some shells, hitherto rather
scarce in Indian collections.
Fam. MeLanrapa.
1. 1 Melania tuberculata, Mull. Species.
Large and fine ... 1.90 0.60.
2. 2 WM. variabilis ... Common. Melania, 2.
Of this melania there are five marked varieties, some of which
could doubtless be separated specifically by many systematists.
8. 1 Glabra. A smooth var. from the tepid springs of Nam-moo.
This var., in common with all the others, has the apex but
little eroded, and differs but little from the ordinary smooth
var. found in Pegu and Bengal.
An average specimen measures 2.00 0.75, the measurement being
taken along the long axis of the shell, and the transverse diameter of
the last whorl.
Qnd. Vittata. This var. is also smooth, but with more convex whorls
than the last. The shell too is paler, with a dark median stripe becoming
obsolete on the last whorls, but well marked on the earlier ones.
Average size 2.00 * 0.75.
3rd. Turrita. A black turrited var. sometimes slightly eroded at the
extreme apex, and with the whorls ornamented with two or more,
274 Land and Freshwater Shells from the Shan States. [No. 4,
usually three, series of prominent tubercles, ranged in symmetrical spiral
order with four non-tubercular spiral keels on the last whorl towards the
mouth. The tubercles form oblique transverse ribs, but the ribs are
a subordinate feature to the spiral ornamentation. 2.00 0.75.
4th. Pyramidalis. Ornamentation like the last var. but form very
squat, with rapidly increasing whorls. The shell is slightly ccerulescent,
with four dark brown stripes visible in the interior, corresponding with
the spiral keels outside. Columella slightly yellowish, apex but little
eroded. 1.90 *& 0.85.
Grotto in Nam-mah stream.
2nd. Baccifera. This var. is intermediate in its character between
vars. 2 and 3. Its whorls are ornamented with four or five rows of
beaded keels, the transverse ribbing being often well marked likewise.
Most of the specimens were dead shells. 1.90 0.75.
It is noteworthy that the ordinary type of M. variabilis, or the huge
specimens of the race met with inthe Arakan hills, are not represented
in the collection, though the abundance of calcareous rocks and cale tuff
would, prima facie, lead us to expect shells of similar, if not greater,
dimensions. Climate and a lower average temperature of the streams
in the Shan country may possibly explain the small size JZ. variabilis
there attains, since I have a Maulmein shell which measures 4.00
1.30, and Arakan specimens not rarely attain (decollated shells).
8.00 «-1.3
3. 1 Paludomus.
A single specimen of a large paludomus, which I have not
yet identified, occurred in the collection.
Fam. Patupinipa.
4. 1 Paludina naticordes, n. s.
Two marked varieties of this shell occur. A smooth one with one,
two or three filiform keels, and a strongly keeled var. with prominent,
rugose keels. The species is probably undescribed and may be thus
characterised.
P. naticordes, Th.—Testa turbinata, sub-polita, solida, pallide flaves-
cente cornea ad peripheriam cariné munita; marginibus callo junctis,
callo columellari non raro valde incrassato, umbilicum obtegente.
Varietas fasciata, fasciis duabus castaneis ornatur, hae superperipheri-
ali, illé juxta suturam posité. Anfractu ultimo tertia notest a carina
Vols Dex av, Ptoll Pi: IX
4 Paludima naticoides n.s. var fasciata.
a BoB d° d2 var. carinata. — :
4. Melamia, v arial 8, Benson var vittata.
A 2 ae .war. baccifera
6 - d® var. turrita.
“1 a? de
aaa
var. pyramidalis.
BRAWN BY T.W. TURNER AND ON STONE BY KRISTOHURRY BOSS GOV" SCHOOL oF ART.
LITH: BY H.M.SMITH, $.6, 0, CALCUTTA NOV: 1865.
Rit,
pe
1865.] Land and Freshwater Shells from the Shan States. 275
panlum remota. Callo flavescente, ore interiori ccerulescente. Anfrac-
tibus 64. 1.45 x 1.10
Var. carinata, Carinis quatuor fortissimis supra munitur, et infra
peripheriam sex vel quinque levioribus; colore albido; epidermide
flavescente ; fasciis nonnullis castaneis interdum ornata. 1.40 « 1.00.
These two varieties pass into each other, but the peculiar columellar
eallus is pretty constant inall specimens. But for this character, some
of the smooth variety might be referred to P. Bengalensis, which
is an extremely variable species.
The strongly corded var. is well marked, but I have preferred taking
the smooth shell as the type of the species, and have regarded the
keeled individuals as hypertrophied, placing the greatest value, as a
specific character, on the columellar callus, occurring in both varieties.
2. P. melanostoma. Paludina...... 2.
1. Bithinia nassa, n. s.
Testa elongata, turbinata, polita, diaphand, solidiusculé. Labio
expansiusculo, plica callosé extern’ munita. Anfractibus quinque.
0.45 < 0.25.
This is the only species of Bithinia in the collection, and it is well
characterised by the strong rib-like fold strengthening the lip outside,
somewhat as in “ nassa.”’
1. Ampullaria, sp.
A small species similar to that found at Maulmein, but distinct
from the smaller species met with in the Arakan hills.
An ordinary specimen measures, 1.75. Aperture 1.25. A very large
specimen of the Arakan species. 1.45. Aperture 0.95.
Fam. Hexicip2.
Of Helices -of all sections, the collection comprises twenty-three
species, nearly one half of which seem undescribed.
1 Helix, n. s.
A large dextral species of six whorls partaking the characters of H.
interrupta and H. senidecussata, but very distinct from either. All
the specimens are unfortunately dead shells. Lat. 1.55 & Alt. 0.75.
2. HA. Blanfordi, Th.
This species was originally founded on a single shell from Darjiling
in wy cabinet, which, from its sculpture, I had no hesitation in separat-
36
276 Land and Freshwater Shells from the Shan States. [No. 4,
ing from its nearest ally H. cycloplaxw. It appears to be a common
shell in ths Shan states, though not so in the Hastern Himalayas, but
all the specimens are dead shells. They agree well with the type,
though a trifle larger and more convex.
3. Helix ansorinus, n. s. (MSS8.)
A very marked form, but all the shells dead ones.
The sculpture is very ornate and well marked. Shape somewhat as
in H. Peguensis. 1.20 X 0.60.
4. H. delibrata, B.
Deak EIT
6
7
Pe ee
Ys Beer (approaches H. Guerin).
9. H. sanis, B.
Though a trifle larger than the type, I can see no sufficient reason
a
for separating this from the Andaman shell. A few dead specimens
only are contained in the collection.
10. #. infula, B. one or two specimens.
11. #. attegia, B. one specimen.
AGE eels
cha ee ale GO ae
els Bae
15. H. similaris, Fer. var.
This shell is somewhat variable. It is usually banded, but occasion-
ally the band is obsolete. It tends to unite H. Zoroaster, Th. and
H. bolus, B., closely approaching the former, but being less depressed
and more tumid, though not so globose as the smaller sized H. bolus,
B. 0.75 & 0.40. Another variety occurs which might be ranked as a
large H. Zoroaster, Th., but it is not larger than the type of that shell,
bnt shows a tendency to approach H, delibrata, B. in form and expanded
peristome. 0.80 x 0.40.
16. A. Oldhami, B.
A little larger than the type which was from near Ava.
17. H. Hutton, Pi.
A single specimen of this widely spread species was in the collection.
18. H. Avrakanensis, Th. A single specimen of this shell also
accompanied the last, a trifle flatter that the type.
1865.] Land and Freshwater Shells from the Shan States. 277.
Lt 27 Rap gh a gan VL
i. Pleciopylis,...... sp. Plectopylis, ...... 1
A described species, but not identified with certainty.
1. Nanina vitrinoides.
Abundant.
2. N. consepta, B. NOMA, v0.2... seule outa cate 3
Closer armed and one more whorl than the type, which was from
near Maulmein.
2 gs een ee
1. Streptaxis Birmanica, Th.
The variety wanting the marginal tooth.
2. S. Blanfordi, Th. Three specimens, ............ 2
1. Vitrina (Cryptosonea, Th.) prestans, Gould.
Tolerably common..
22 ere
ype as the last. A small species of the same, .....5........--. Die
1. Bulimus Sinensis.
A single specimen of this species which is tolerably common in the
Pegu forests.
3 A of the ‘‘ Gracilis” type, common, with deciduous
epidermis.
2. 2 ee eae ditto, common.
PUENTE ECUISS ivooc.es00s common.
SBE ses st
6. B. Niligiricus.
The occurrence of this shell is very interesting. It has eight
whorls and differs slightly from the type, but not to a greater degree
than Nilghiri specimens do from one another. Bulimus, ...0+- 6
Achatina...four species.
apes
it etre
All of the ordinary Indian type. Achating, vo 1c: 4
Pupa.........In species with new.
Eee eons I, PU Keeiet ent amet
1. Clausilia, a large species, not rare.
2. €..,.... a small species, rather rare.
278 Land and Freshwater Shells from the Shan States. [No. 4
3. C....... a larger species, common.
All three seem new species. Claustlid, .c.ccscne 8
Fam. Limnz1pz.
Lymnea, a small species, Lijec
Planorbis Coromandelianus, Fab.
Very common, rather small Planotbis: 2o.-ae ae
Fam. DrrromMMatInipa.
Diplommatina, five species.
As far as a cursory examination enables me to judge, all five seem
undescribed : two are sinistral, the others dextral shells.
Diplommatina,... 4
Fam. CycLostomip2.
1. Pteroeyclos.
Probably a new species. Of the type of P. pullatus, B., but three-
fourths larger.
" 9. P. insignis, n. 8.
Forma typica. Testa albid&; epidermiide flavescente sive castanea,
decidua vestita, castaneo-fasciaté. Peristomate duplici, antice valde
expanso. Operculo intus concavo, extra planiusculo, margine valde
radiate hirsuto. Lat. 1.20. Lat. oris intus 0.65,
This handsome shell seems tolerably abundant.
EL CHOCY CIOS: ae) teem
1. Cyclophorus speciosus, Phil.
A common species, specimens of medium size.
2. ©. cornu-venatorium, Sow.
A single specimen occurs in the collection, rather more tumid thar
Ava specimens. ;
S iC ars.
A distinct but not very well defined species, approaching near to
C. excellens, but wanting the funiculate keel of that species. Only a
few dead shells were collected.
A ie AUS:
A single broken specimen, but evidently a new species, recalling in
form C. involvulus, only larger, and for its size a lighter shell.
5. C. n.s. avery minute shell, smaller than C. Sczssemargo.
Cyclophorus, ... 5
1865.] Land and Freshwater shells from the Shan States. 279
1. Pupina arula, B. Two specimens.
2. P. artata, B. Two specimens. Pwpind, ii... Scene ad
1. Alyceus, n.s. type of A. Ingrami, Bl.
2. A. n.s. type of plectocheilus, B.
= ae
4. A.
5. A. amphora, B. Two small specimens.
Gas RA PMTs proce ens |
i) Pomateas,~ 0. sz
2. P. n.s. near P. Peguense, but with more convex whorls..
TE OUEC bocce 2
CONCHIFERA,
Fam. Unronipa.
1. Unio ceruleus. Very fine.
2. U.marginalis. Fine.
3. Sp. fine. WO Bei eS
One specimen occurs of a unio, remarkable for having two rounded
osculating teeth, one in each valve, very near the anterior end. These
teeth are smooth and apposed without interlocking. The species is
also found in the Pegu Yoma hill streams.
Fam. CycLapipm.
Pe Coriculd 2.2.4.3. Common.
A small species with yellowish epidermis. Corbicula,........ L
Genera 24, species 77.
Screntiric INTELLIGENCE.
London, Sept. 17, 1865.
My pear Grors,
As you will doubtless print much of my last letter, I will add a
few more items of intelligence concerning matters ornithological, as
I have still been steadily engaged in my commentary on Jerdon’s work.
This has now grown so extensive that I have divided it into four
parts, which will probably spread over the Jdvs for next year. The
first three, treating respectively of Jerdon’s three volumes, and the
fourth, of Ceylon birds, not included by him, and a final tabular expo-
280 Scientific Intelligence. [No. 4,
sition of the Orns of the Indian special province of the Indian region.
This I divide into 24 districts, and give one to four asterisks to each
square, according to the amount of commonness of the species, and a
cross where I regard it only as a casual straggler. So that consider-
able information is conveyed at a glance. I next take up the Indo-
Chinese or Ultra-Indian province, for which I have a fair amount of
material. You will have received from Col. Phayre a short note from
me respecting the middle-sized Indian Cormorant and one of the
Ring-plovers. I now tell you about them more in detail. No. 1006
of Jerdon will stand as G. fuscicollis, Stephens: Syn. sulczrostris,
Brandt (figured in Gould’s B. Austr.), sulcirostris et stictocephalus,
Bonap., leucogaster, Meyer (apud Jerdon), leucotis, Blyth, albiventer,
Tickell and purpuragula, Peate,—Sinensis (apud Jerdon), G. K. Gray,
cat. of Nipalese birds, Jerdon,—a somewhat formidable array of
synonyms. Also, one common small Cormorant is the true pygmeus of
Pallas. Next, about the Ring-plovers. No. 849. This is, as I mentioned,
4B. curonicus, (Beseke), minor, Meyer, and Jndzcus, Latham : distinct
from AZ. philippensis, (Scop.), which is a species intermediate to
AZ. curonicus and 47. cantianus, obtained by Wallace in Borneo, Z.
philippensis in nuptial dress, has the usual white forehead surmounted
by a black band, also a black loral streak and auriculars in part ;
crown rufescent-brown with a more rufous periphery; some black
behind the nuchal collar above ; the black pectoral streak narrow or
interrupted in front ; and the tail unbanded, with the outermost three
feathers white ; legs pale in the dry specimens: length of wing 4 inch;
of tarse 14 inch. It should be looked for in S. India. Of No. 850,
there are two specimens in the India museum, one of which is the
philippensis of Sykes’s list. After learning of the distinctness of phi-
lippensis from curonicus, I re-examined Horsfield’s type specimen of
his pusillus ; and though in bad condition, especially about the nape,
I now recognise it as distinct. It is in winter dress, and has not the
white collar seen at all seasons in others of the present group. As
compared with ewronicus, the tail is more cuneated, with the dark
band considerably less developed, shewing only as a narrow cross
stripe on the outermost feathers. Perhaps it is Ch. Peroni, Sany., the
description of which I have not yet seen. It should also be looked
for in 8. India. Jerdon omits to include the Ch. nigrifrons, (Cuy.), v.
jj ice
1865. ] Scientific Intelligence. 281
melanops, (Vt.), his russatus, an Australian species, of which he obtain-
ed a single specimen near Madras in the month of June (7. e. during
the southern winter), and which is now in the Society’s museum:
of course an exceedingly rare and accidental straggler. The Indian
Neophron turns out to be distinct and new, N. orientalis, nobis. It is
not the Vuliwr meleagris of Pallas, which he describes as a rarity in
the Taurian Chersonesus, and which is the black-billed N. perenop-
terus. Four of our rarest alconide I have made out to be Japanese
species, all priorly named by us ‘insulars.’ 1. Accdpiter nisoides,
nobis (gularis, Schl., of which he notes a specimen from Nipél !)—2.
Buteo aquilinus (v. leucocephala), Hodgson (hemilasius, Schl.),—3.
B. plumipes, H. (Japonicus, Schl.),—and 4. Poliornis pygmeus
(Buteo pygmeus, nobis, B. pyrrhogmys, Schl.), of which Helfer obtain-
ed a specimen in the Tenasserim provinces. Athene castanotus, nobis,
of Ceylon, is recognised as distinct, from castanopterus of Java by
Schlegel. Jerdon’s No. 145 is not Zockus gingalensis (verus), but
T. griseus (Buceros griseus, Latham, B. cineraceus, Sem.), as distin-
guished from T. gingalensis of Ceylon, which, together with the other,
inhabits that island. The two were discriminated by Layard (Ann.
Mag. N. H. 1854, XIII, 260), though he describes both under cinga-
lensis ; and he also indicates a second-Hydrocissa (akin to H, albiros-
tris and H. conoisus) as inhabiting the mountains of Ceylon. Spzlor-
nis bacha inhabits Ceylon in addition to Sp. cheela ; and the Parda-
lotus pipra of Lesson is a second Cinghalese Prionochilus (seu
Piprisoma) unknown to Layard. The large crimson Chrysocolaptes of
Ceylon will rank as C. Stricklandi (Layard, v. carlotta, Malherbe),
erroneously figured by Jerdon in his J//. Ind. Orn. as Brachypternus
Ceylonus! No. 197 should be Megalaima Hodgsoni, Bonap, of N. E.
India and the whole Indo-Chinese provinces, as far at least as Cambo-
jia; where the species is mistaken by Schlegel for the Javanese
corvina, which is wholly unknown in those parts: and M. viridis
(apud Schlegel), of Java is quite distinct from J. viridis (verus) 0
S. India, and is probably the true lineata, Vt., as Schlegel himself
suggests. He also recognises the identity of No. 42 with the leuco-
rypha of Pallas. The latter holds just the same relationship to
H. rustica, which H. hyperythra (of Ceylon) holds to H. Daurica ;
also Falco rulen apud Schlegel (the Shdhia) to F. peregrinus,
282 Sctentific Intelligence. [ No. 4,
Hypotriorchis severus to H. Subbuteo, Tinnunculus rupicolus (of
Africa) to 7. Alaudarius, and Athene castanotus (of Ceylon) to A.
radiatus. In all these cases the deeper coloured bird is more subtro-
pical, less migratory (or even permanently resident), and does not visit
temperate latitudes. Schlegel, with much probability, refers F. pert-
grinator, Sundevall, to F. macropus, Swainson (v. melanogenys,
Gould), the Australian Falcon which occurs in the Malayan province.
I think I mentioned that I found a fine female Falco Babylonicus in
the Worcester Museum; and this is probably the ‘ Red-naped Fal-
con,’ L. peregrinoides apud G. K. Gray, of his Catalogue of the Birds
of Nepal. The specimen in Worcester is like an adult female Pere-
grine, only much paler, with all the markings.considerably less developed ;
nape light cinnamon-rufous marked with dusky; the moustachial
streak small; the upper parts cross-banded as in adult Peregrines:
this rare Falcon belonging to the Peregrine subgroup, as distinguished
from that of the Sakir, Lanan, and Lugger. About Zurnix, I stated
(in Ibis, 1865, p. 33) that Ortygis luzoniensis of Horsfield’s list of
Javanese birds was the species I now recognise as Z’. tanki (B. Ham.,
vy. joudera, Hodgson); and such a distribution rather puzzled me, as I
knew no instance of 7’. tanki out of India proper. It is, however, of
a nearly allied but smaller species proper to the Malayan province, de-
scribed by Wallace from Timor as 7’. rufescens. Thus are here three
allied species, Z’. maculosus in the Indo-Chinese province with China,
7. tanki in the Indian special province, and 7. rufescens in the Ma-
layan province. The proper name for the Indian Curlew will be
Numenius lineatus, Cuy.: Syn. N. Major, Schlegel.
D. G. Elliot of New York was here the other day, and picked up a
few new Polyplectrons from Cochin China at Paris. He is about to
bring out the Phasianide in grand style, from drawings by Wolf,
some already made, and which you would most heartily admire.
Now for some intelligence about what is doing in the Zoological
Gardens, Regent’s Park. There are two small female African ele-
phants now in London, one of which is safe in the Zoological
Gardens. Also a pair of the superb Gazella Dama. A fine healthy
Buceros Abyssinicus (Abba Gumba of Appendix to Bruce’s Travels),
the long-legged ground Hornbill, a most curious kind, which stalks
about in a style that would puzzle you altogether to make out
Beni.
1865.] Screntrfie Intelligence. 283
what it was, if you were to see it stepping about at a distance. Hm-
phatically a snake-devourer. Two young Wapitis came to light this
week, the daughters of the fine Californian buck ! A lot of Ammoperdix
Hleyr; and different species of Pterocles. Pt. alchata (I may have told
you) has bred, and I saw the newly hatched chick, precox of course,
but inactive, from the shortness of its legs. The Felis macroceles and
two Ursus Malayanus which I brought doing well. A pair of common
house Mainas at last; and I wish I could see a pair of common Indian
crows, and the two common Indian vultures, Gyps indicus and G.
bengalensis. Although the temperature has been extraordinarily high
all this September, and people are panting and languishing as if they
were in Sierra Leone, I observe with terest and considerable surprise
that the Arctic Foxes are rapidly re-assuming their white winter coat |
I hear of some extraordinary discoveries up one of the great tributaries
of the Amazons, where the few scattered human inhabitants had never
before been visited, and were unacquainted with the use of metal,
using stone implements; and the animals quite tame and unscared
by man—herds of Tapirs, which would allow their coats to be rubbed
by a stick and enjoyed the titillation. I just lost a fine thing the
other day at Stephens’s auction, a splendid skull of Dubalus brachyceros
had been knocked down for eight shillings; and the purchaser would
not part with it. You would otherwise have had it.
P. S.—1 have been thinking that you would do well to re-publish
my commentary on Jerdon’s Birds of India, if you could get Jerdon
himself to annotate it, and thus afford him a convenient opportunity,
of making known all that he may have to add, in order to complete
our information on the subject up to the date of publication in the
J. A.§. I much wish to know how his book has sold, and also what
progress he is making with the other classes.of vertebrata. WN. B.
Felis rubiginosa of the Coromandel Coast extends to Ceylon (Cingha-
lese specimen in Belfast Museum); and my Cinghalese Secwrus Lay-
ardi is in the Worcester Museum from Malabar, sent (with Presbytis
Johnit, verus, &c.) by R.Cole of Madras. Also, in the Worcester
Museum, a fine adult female of the rare Falco Babylonicus, alleged to
be from Java, which I do not believe. Ihave seen a kitten of my
Felis Jerdoni from Malabar, and I have little doubt that this jungle-
cat there takes the place of L. rubsginosa of the Coromandel side of
aT
284 Screntific Intelligence. [No. 4,
the Peninsula. I adda list of desiderata for the Zoological Gardens.
You may smile at my enumerating common Vultures, Kites and
Crows, Frogs and Toads; but these are just what are wanted—
what nobody thinks of sending. The Batrachia might be sent in
damp jars, and would endure the. voyage without food, though
cockroaches might be given to them if available. WN. B. There are
Australian Rallide and Pelicans in the Zoological Gardens; also
Varanide, Scincide, and Snakes. Why’ not also Indian ? and
operculated Shells (sent with opercle closed) as Ampullaria and Cert-
thium telescopiwm ; even our big Achatina with its pseud-opercle
closed.
Mamuatta. Gibbons—Hunumin Monkey and other species of
Presbytis—Wild Dog—Indian Wolfi—common Bengal Fox, one in
Dublin Zoological Gardens, labelled—Jackal, C. aureus !—Viverra
Zibetha—Arctonyx—Jungle-cats—4-horned Antelope—Gaydls and
common Buffaloes (fine, as those of Burma)—Tapir—Rhinoceros
Sondaicus (from Sunderbans or Burma) and kh. Sumatranus—any of
the Himalayan ruminants— 7wpaia—Melogale—Pteromys—Atherura
—Porcupine from Chittagong or Tippera.
Avzs. lLories (any),—common Kites, 2 or 3 (not Brahmini)—
Limnaétus niveus (of Serdon’s work)—Pontoaétus icthyaétus—Spilornis
cheela (especially, to contrast with Sp. Hlgint)—Poliornis teesa—
Aquila fulvescens (2 or 3 to contrast with the allied African species)
—Agq. hastata—Ketupa Ceylonensis—Urrua bengalensis—U. Coro-
manda—Ninox scutellatus—Gyps Indicus and G. Bengalensis (not Oto-
gyps calvus. With the exceptions of the two common Bengal species
of Gyps, the series of Old World Vultures is complete. WN. B. Neo-
phron percnopterus of Africa has a black bill, in India a flesh-colowred
bill !)—Barbets—Centropus rufipennis (very desirable. WN. B. ‘The
two Indian Coéls are doing well)—Corvus splendens*and C. culminatus
(pair of each, especially the former)—Dendrocitta rufa (very accept-
able—Bhimraj—Shama—Sdt Bhai (Malacocircus)—Bdyas (Ploceus, 2
or 3 pairs of each, which would doubtless breed)—Mainas of each
species, Sturnopastor, and especially Temenuchus, pagodarum (2 or 3
pairs of each)—Dengal Jungle-fowls, with white ear-lappet—A djutants,
bothspecies— Ciconia leucocephala—Geronticus papillosus—Threskiornis
melanocephalus; one already from Siam!—Gallicrea cristatus—Gallinula ~ ;
-
1865.] Scientific Intelligence. 285
phenicura—Sarkidiornis melanonotus—A nas pecilorhyncha—A. caryo-
phyllacea—Fuligula rufina—Pelicanus Philippiensis (small Indian
Pelican, common in South India). If Pelicans can be sent from
Australia, why not from India? I have mentioned that we have
Australian Rallide alive, and also Gdienemus grallarius. By the
way, the middle-sized Indian Cormorant still remains an enigma. I
haye seen no specimen in England, nor is any such species recognised
in Schlegel’s elaborate notice of the genus. Specimens (skins) of
this bird would be most acceptable! It appears to be common in
Kashmir.
Tickell’s supposed new Gadidous fish is precisely what I told you it
would be. There should be a plentiful supply in the museum, several
dozens, which I procured in the Akyab bazar. It was- described and
figured by Richardson, and since by McClelland (who associated it
with the Gadide). I cannot refer just now, but the synonyms in my
hand-writing should be on the label attached to the bottle; and that
bottle I leit near the specimens of Polynemus, which Jerdon agreed
with me.in considering the nearest ally. It just holds that sort of
relationship to some of the Gadide, which the Scopelide do to the
Salmonide ; only the latter are really more nearly allied, I think.
There is a most interesting Australian Seal on exhibition at Cremorne,
which I am anxious to see, and will do so soon. Vide a notice of it,
in a letter from Bartlett to Gray, ina late No. of the Annals. So
high a price is wanted for it that the Zoological Secretary has declined
to purchase hitherto; but I fear that the exhibition of it brings in
some £11 or 12 per. week to its proprietor! Of course I have been
to see the African Elephant, which differs very much from the Asiatic.
It is equally docile, but much more energetic and active, and Bartlett
considers it the more intelligent of the two! Moreover it is very
salacious, which the Asiatic is not (unless when regularly must). It
was rather in bad case when it arrived, but is now in capital condition. A
small African female Elephant is expected immediately ; and with it one
of the long-leeged African ground Hornbills, Bucorvus Abyssinicus, or
Abba Gumba of Bruce. The other Hornbills are doing admirably, viz.
3 Homrai, one B. rhinoceros, 1 albirostris, and one small African
Tockus. Two or three more of albirostris would be acceptable, and as
many more species as possible, especially the large kinds; for they
286 Scientific Intelligence. [No. 4,
shew well in the spacious aviaries allotted to them. The yellow-
quilled Porcupine (M/alabaricus, Sclater,) turns out to be my A. Ben-
galensis, the yellow colour of the quills being only temporary. The
3 handed Armadillo is a most interesting form, very different from
Dasypus, and considerably akin to Glyptodon. There are a fine
healthy pair of Chimpanzees, and female Orang-utan ; but no Gibbons,
which are particularly wanted; especially as there seems every pros-
pect now of these Apes living, as they are so very much better accom-
modated. The Gazella dama lately added to the Garden is a fine
acquisition ; and Burchell’s Zebra has bred. The Hagle you sent has
assumed the mature plumage; and I think I may say that all, which
you have sent, are doing well, the 2 Mycterie, 2 Tantalz, also pair of
Hematornis Elgint, and pair of Hudynamys orientalis &e. Gallo-
phasis lineatus has bred; and there is a young hen $ Swenhoer; also a
half-bred Ocellated Turkey. Males of Phenicura Reeveswi and Diar-
digallus, Also the Heliornis or ‘ Sun Bittern’ (a very curious form) ; and
the black-necked Swans. Bengal Floriken in first-rate summer dress.
It was sent by Babu Rajendro Mullick in 1857. How is he getting on,
and his store of live-stock ? Three living Apteryx ! Sturgeon Still doing
well. Garrulax Sinensis from China, quite lively and well: the same
as the Tenasserim species. The new Cassowary which J described
turns out to be the finest of them all. A living female at Amsterdam ;
and its egg quite different from that of common Cassowary, or of
Mooruk. I have seen the magnificent fossil head in the British Museum
of Elephas primigenius lately dug up near Ilford in Essex, with superb
tusks in socket—not curled up as in the Siberian specimens so often
figured. Head very different from that of H. Indicus, more ike A/fr-
canus, but the grinders are of the same type as the former. Another fine
accession to the B. M. is an enormous aérolite from Australia.
I must now tell you a few results of interest at which I have arrived
concerning Indian birds. The paper is a very long one, and will probably
spread over the Lis for all next year. When I have quite finished
it, I contemplate working out the birds of the Indo-Chinese province
or sub-region, and then those of the Malayan Peninsula. You may
begin by expunging from your list Cotyle sub-soccata (identical with
Sinensis), Luticilla pheniewra (as distinct from phonicuroides), Phyl-
loscopus trochilus (disavowed now as Indian by Gould), and I suspect
~1865.] Scientific Intelligence. 287
also Sturnus unicolor (for which I believe old spotless specimens of
S. vulgaris have been mistaken); Rhodophila melanoleuca, Genus
quite identical with Oreicola, Bonap., as founded on two Timor
species, melanoleuca and luctwosa ; and therefore I now call the Indian
one QO. Jerdoni, and do not agree that Pratincola ferrea should range
with it. (Vide Jerdon’s Appendix). The Horornis and Horestes
series puzzled us much. Horornis fulviventer = Phylloscopus fusca-
tus, nobis !—H. fuliginiventro, also a Phylloscopus, akin to last.—H.
flaviventris a true Dumeticola ; and H. fortipes, I suspect, another
Dumeticola, (to judge from my description of Hodgson’s specimen in
J. A: S. XIV, 585, for I cannot find a specimen in the museums
here.) This disposes of the four species admitted by Jerdon; but
both in the British and India museums, I find numerous specimens
marked Horornis assimilis, Hodg., and these are identical with the
bird I formerly described as Drymoica brevicaudata. Afterwards I
thought that this was the adult of Neornis flavolivocea, Hodg., of
which I had only seen the young ; and this view is accepted by Jerdon.
It turns out that the two are allied species, and Horsfield’s Sylvia
montana constitutes a third; so I bring these three together under
Neornis, and sink Horornis altogether. As for Horeztes, I know but
of two species, the large H. major, and-the small H. brunnezfrons,
(v. schistilatus), of which pollicaris is the young! Jerdon sends me a
new Dumeticola ; making 3 Gf not 4) of this form, which I think
might be very well merged under Locustella. Jerdon tells me that
my Accipiter nisoides is common in the interior of the Himalaya; I
can find no specimens, and two that he has sent me (as I presume for
this) are decidedly A. Virgatus, which he should know well. His new
swallow, Hirundo Tytlerx (Gn Appendix), I cannot distinguish from
HZ. cahirica of Palestine and Egypt; but Adam’s species (referred to
by Jerdon and H. fluvicola) is distinct, and Gould has named it
empusa. Two species of Woodpecker are confounded under Chryso-
colaptes sultaneus, viz. true sullaneus, H. (strenwus, Gould), which is
considerably larger, rare, and known only from Nipal; and C. Deles-
serti, Malherbe, from all India, Indo-China, and Malayan Peninsula.
Zoothera imbricata, Layard—Oreocincla Nilgiriensis, nobis. Of Cuc-
koos, our Himalayanus is the canoroides, Muller, and optatus,
Gould; and this species is accepted as striatus, Drapeiz, by Schlegel.
288 Scientific Intelligence. [No. 4,
Tt would seem to be the commonest species of the archipelago.
Wallace has also C. poliocephalus from Java. In the British Museum
there is a Nipél specimen of what seems to me a small race of #.
sparverioides, which I have named nisoides: wing 74 in.—Of H.
nisicolor I have now seen several specimens. H. strenuus, Gould
(B. As.), I think doubtfully separable from sparveroides ; and his
hyperythrus is just the adult of Horsfield’s fugax, which I consider to
be distinct from the Indian varius. The fugax I now recognise as
HI. flaviventris, (Scopoli. Syn. C. radiatus, Gm. ; H. pectoralis, Caba-
nis, and H. hyperythrus, Gould,—the adult; and C. fugax, Horsf.,
sparveroides apud von Schrenck,—the young.)—From China, Philip-
pines, Borneo, and Java. My Geocichla dissimilis is Turdus chrysolaus,
Temm., nec cardis (Jerd. No. 358). The Zragopan Duvaucelii, Temm.,
is Pucrasia castanea, Gould; and its true habitat probably Kashmir
(Kdfiristan being altogether out of the question). I suspect that
nipalensis, Gould, is merely a hybrid between it and the common
Himalayan species, Arboricola. I have made out a list of 12 species
of this group! Turnix Dussunvierit (vERUS) = Sykesi; and T. Dussu-
mieri apud Jerdon must stand as tancki, B. Ham. (v. joudera, Hodg-
son). Casarca leucoptera, nobis, is Anas scutulata, Mitller.
This must do forthe present. I may add that the large striped
Derbian Eland has a very different form of ear-conch from the common
Eland, broad like that of the Kandoa, instead of lanceolate as in the
humped cattle. This is a notable distinction.
Nore on tue Pevra Parrivers (Arboricola, Hodgson). This groud
of hill Partridges, with long (or moderately long) straight claws and
spurless, is greatly developed in the jungle-clad hills of 8. EH. Asia
and its islands, where probably, several species yet remain to be
discovered. I think we can already enumerate—
a. With the throat well feathered.
1. a torquerors. (Tem., p. c. 462-3.) The only species known to
me in which the sexes present a marked difference of plumage.
Himalaya.
2. Aa. nvFoGcuLARIS, nobis. S. E. Himalaya (at a lower altitude
than the preceding race,) and also the Tenasserim mountains. (J. A.
S. XXIV, 276.)
x
t
Ne
4
of
1865.] Scientific Intelligence. 289
3. A. BRUNNEOPECTUS, Tickell. (J. A. S. XXIV, 276.) Tenas-
serim mountains.
4. a. gavanica. (Brown, J. A. Zool. pl. XVII; Temm., p. c-
1488 : but guere—the red surrounding the eye?) Java.
5. A. (?) Aigueinosa. (Hyton. P. Z. S. 1839, p. 106.) Malayan
peninsula.
b. With the throat thinly clad with feathers, shewing
the crimson skin beneath.
6. a. peRsonaTa. (Horsfield, Zool. Pes.in Java, fig.; Tr. Lum.
Soc. XIII, 184.) Sumatra (?) and Java.
7. s pe | Se | Sec. | co oe lees
Ih We A ) a = Mamet KS cor ae
0 t) “@ ty) Inches. |Troy grs.|Troy grs.
xe 609 | 46°) 572) 8.8 | 0.476 |} 5.28) | 170) ome
a 60504 431) 57.4. 747 ANTS Oy 56 Wir
2 60.1 | 4.0 | 56.5 WG\e) (AGS 18 AQ 78
3 59.7 | 3.9 | 56.2 7.4 | AGL 14 AB 78
4 59.0 | 3.7 | 55.7 7.0 | 453 06 33 79
5 59.1 | 3.5 | 55.9 6.7 | .456 09 28 .80
6 58.5 | 3,6 | 55.3 6.8 | .447 00 27 .80
7 58.3 | 3.5 | 55.1 6.7 | 444 | 4.97 24 80
8 60.1 | 4.5 | 56.5 Bal) WA6au Bais 60 76
9 62,2 | 68 | 568 | 122 | .4’70 18 2.58 67
do Gea) SAnl 570) dod Ne A7e 18 3.35 61
ll 650) | 981 SSL) Gy) aor 34 92 5S
Noon.| 65.5 | 10.7 | 580 | 182 | .489 81 4.35 BS
1 65.8 | 11.7 | 57.6 | 19.9 |. .483 122, 82 52
2 66.3 | 12.1 | 57.8 | 20.6 | .486 25 5.06 51
Brill) Gea mean O57 4 PLM 280 18 a7 50
4 65 B04 Wile) Wy 57200) 17, 76 16 4.70 52
5 65.1 | 10.2 | 580 |17.8 | .489 82 08 BT
6 | 653 | 75 | 59.3 | 13.5 | J511 58 3.13 64
"7 647 | 64 | 59.6 |115 | (516 66 2,62 .68
@) | 639))| Beri’ 598) "| 104M, (bit 63 30 vl
9 | 631 | 53 | 589 | 9.5 | 504 56 .06 73
20 | 62.4 | 49 | 585 | 88 |. .498 50 1.87 75
AP Ne Glo | Aa 57.8 o | Bb ss 39 78 45
}
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations. Vv
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
an the month of January, 1865.
Solar Radiation, Weather, &c.
He | So Ss
68 |2ad
.| 2 |© = S| Prevailing direction General Aspect of the Sky.
S| 43 18389 of the Wind.
oe! ss os
Shen jp
| o |Inches
ER. .. | Sunday.
2) LEU epee Cloudless: also slightly foeey at midnight,
3,137.4) ,.. |S. E.&8.&N. EH. | Cloudless: also slightly foggy at 7 a. M.
4; 139.0}. ... | NW. &N, Cloudless: also slightly fogey at 10 & 11
5| 136.2) .... | N.& N.W. Cloudless. [P. M.
Sikes. | N. Cloudless till noon: “i till5 p. w. cloudless
afterwards also fogey at 10 Pp. mM.
2) igh)... | Ho & N- ~ | Clondless: also fogey from midnight to 2
A, M.
8 ee ... | Sunday.
9; 1382.4)... N, Cloudless.
TOU ESAO |... N. &N. W. i till 4 A. uw. cloudless afterwards.
41) 131.8) 2. | N.W. GN. Cloudless tilll p.m. \i & “i afterwards.
PASSO} 3: W.&N. W. i till 7 A. mM. cloudless afterwards.
13| 131.4) 1. |N.W.&W.&N. | Cloudless : also slightly fogey at 9&10 P.M.
PA bao... | N. Cloudless.
11) eee Pe Sunday.
16| 132.4)... N.W.&S.&N. Cloudless till noon: Scatd. clouds till 6
p. M. cloudless afterwards.
A) '36.0) 2. | Wo & N. W. Cloudless till8 a. m. i till 5 p. uw. cloudless
afterwards: also fogey from § to 11 P. M.
18] 138.4:| ,.. W. Cloudless : also fogey at 7 a. um. & from 9
to 11 P.M,
19) 142.4) ... nf & N. W. Cloudless.
20| 127.45 ... Ni & i till 7 a. M, cloudless afterwards.
Palit.) 2. e & EH. &N. Cloudless.
vows “oe Sunday.
on eaaeOl | ou N. Cloudless til 5 a.m,—-i& “i till 6 Pp. uM.
cloudless afterwards ; also foggy at 6 &
7a.M. Gat8&9 P.M.
PALANAN} ce. | Ni. We & N. Clondless till 4 4. um. “i till 7 ep. mw. cloud-
less afterwards.
25) MADD | ove N. W. & W. Cloudless tillnoon: i & “itill 7 P. mu.
cloudless afterwards.
26) 140.0| ... Ss. Cloudless till11 a. mw. ~itill 8 P. um. cloud-
Jess afterwards.
77 Ne aor 0.16 |S.W.&S8. - | Cloudy : also raining at 34.m.8 & 9 P. M,
& thundering & lightning at 8 P. M.
ABP LSS) 3, Ss. W. Scatd. clouds till 10 a. mw. “i afterwards.
ah | ee ws | Sunday.
30} 133.0; ... |N.&S.&N. W. Cloudless till 9 A, Mm. Scatd. clouds till §
P. M. cloudless afterwards.
31) Soe 0.32 |S. & N. W. Cloudless till 5 a. M. cloudy afterwards :
also thundering & raining at noon.
“S Cirri,—i Strati, 91 Cumuli, “i Cirro strati, ~i Cumulo strati, i Nimbi
ade Cirro cumuli,
vi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of January, 1865.
Montuty REsutts.
Inches
Mean height of the Barometer for the month, .. eo es 930.066
Max. height of the Barometer occurred at 10 A. M. on the 5th, so» 90.238
Min. height of the Barometer occurred at 5 Pp. M. on the 27th, e- 29.844
Extreme range of the Barometer during the month, 30 ee =: 00.8 9.4
Mean of the Daily Max. Pressures,.. eo eo ee 30.143
Ditto ditto Min. ditto, .. fe os 2» 30.008
Mean daily range of the Barometer during the month, .. ee =: 0135
i o
Mean Dry Bulb Thermometer for the month, .. ee ee 69.5
Max. Temperature occurred at 2&3 P.M. on the 26th, .. oe 83.2
Min. Temperature occurred at 7 A. M. on the 11th, Bye oe 57.0
BDaxtreme range of the Temperature during the month, .. c° 26.2
Mean of the daily Max. Temperature, 50 ee eo 78.9
Ditto ditto Min. ditto, .. 30 60 50 61.7
Mean daily range of the Temperature during the month, .. 33 17.2
Mean Wet Bulb Thermometer for the month, .. 50 a0 62.7
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 6.8
Computed Mean Dew-point for the month, .. oe oe 57.3
Mean Dry Bulb Thermometer above computed Mean Dew-point, ee 12.2
Inches
Mean Elastic force of Vapour for the month, .. ee ee =: 0478
Troy grains
Mean Weight of Vapour for the month, ee ee ee 5.26
Additional Weight of Vapour required for complete saturation, es 2.62
Mean degree of humidity for the month, complete saturation being unity, 0.67
Inches
Rained 2 days, Max. fall of rain during 24 hours, oe ee 0.382
Total amount of rain during the month, 60 oo ee 0.48
Prevailing direction of the Wind, .. oe ee N.& N. W.
Meteorological Observations. vil
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
an the month of Jaunary, 1865.
Montruty REsvtts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
1
Hour. |
g = E = 5 a BI S| : Si 5 |
elle atl] |SiF ls! sie |siala|a
NJ Siz |S) E. |slalels.iclalete lela eis iG\a
No. of days
Midnight. Se el Ue | By eG)
1 8 if 1 1 3 1 7| $4
= Ae lie Seal alts 3
Of 8 2 2 2 4| | 4 4
3 i 7 1 il 9 3 2) | 4 4 2
9 12 Does aoe ane bh Lie fe
10 10| | 2 8) yl) pa yl f 3) | 2
11 Lu) |e ft Fa 73 73) fe
Noon. 10) | 1 3 1) | 4 11) a) 6
1 9 |2 1 Ab Sai
2 13 al 2 1 9
3 10) | 1 1 cl ele |S
j 5 1} J 2} fil Psi fio
2 ale liq 1) }al f2 10 2
"7 7 ai 1 1 5 1 4 6
8 6 1 2 1 4, 2) 175 5
a 6 2) | 1) [4] fal [4 4 2
Meteorological Observations taken at Gangaroowa near Kandy,
Ceylon, in the month of January, 1864.
Alt. 1560 ft.; E. Long. 80° 87’, N. Lat. 7° 17’.
All the Instruments have been compared with standards.
The tension of aqueous vapour, dew point and humidity, have been
found from the readings of the dry and wet bulb Thermometers by
Mr. Glaisher’s Hygrometrical tables (Hd. 1863).
The dew is the weight in grains deposited on a square foot of
ordinary woollen cloth exposed on a board from 6 P. M. to 6 A. M.
or for as many hours as there is no rain.
The rain guage is 45 feet above the ground.
The ozone cage is hung about 25 feet above the ground.
The direction of the wind given, is that of the lowest current by the
vane, and of the currents above this by the direction in which the
Nimbi and Cumulo-Strati clouds are moving.
In this column a“ calm” signifies that the clouds are apparently
motionless: “ variable,” that the clouds apparently in the same or
nearly the same stratum move in no fixed direction, but their parts
move as if in vortices, or different masses of them move up from
different quarters as if into a vast vortex, this beg nearly always the
ease before thunder storms.
Entries, such as WS W and NN W or ESR ve signify that
NN W tocalm,
the clouds are evidently in strata of different altitudes, that those
in the lowest stratum move from W S W;; those in the next higher
from N N W; those in the next are apparently becalmed, and so on.
The velocity and distance in 24 hours are given by Robinson’s
Anemometer.
In the column for Lightning and Thunder
L —“ Lightning” when the flash is near enough to be visible.
LR=“< Lightning Reflection” when the flash is so distant that
only its reflection on the clouds or in the air is visible.
“Morn,” is6 a. u., “ Even,’ 6 P. w. and “ Night,” 12 Pp. Mm. and
“ fore’ and “ after” are prefixed to these, as ordinarily to “ Noon,”
to denote the 3 previous and 3 following hours.
R H. Barnes.
il
Meteorological Observations.
GANGAROOWA NEAR Kanpy, CEYLON.
| January, 1864,
STOO ON
Barometer
reduced to 32°
A. M. P. M. P. M.
9.30 | 3.30 | 10.0
28.393) 28.265] 28.362
.870| .254| .376
372| .256| .371
.406) .269} .349
.865| .229 2
.360| .268 ss
892 *. a
3° bP) °°
2? 33 3)
be) bP) be)
be) 5) 9
410} .284. 4
.420) .279 r
.874| .266] .372
.378| .238] .343
369} .239] .3845
.382| .254/ .369
.375| .247| .865
.893| .254| .380
419} .290| .396
442) .294) .404
.400| .291) .408
.880| .262] .380
880; .268] .378
401| .277| .383
.887| .263| .374
.383| .268) .373
.881| .260) .371
.403| .284) .3879
.395| .289) .398
.403| .286) .404)
28.390) 28.267 28.376
Pressure of
Thermometer.
Dry Air: Dew Point.
M. P. M. P. M. |A. M.|P. M.|P. M.|A. M.|P. M.|P. M.
9.30 | 3.30 | 10.0 | 9.80} 3.30; 10.0/ 9.80) 3.30} 10.0
27.769] 27.677) 27.780] 72.8) 75.1] 70.2) 65.3) 63.6] 63.3
.757| +.606] .782!| 72.5) 76.8] 68.8) 64.8) 66.4! 63.9
-765| .666] .840| 70.0) '75.0| 66.1| 64.5) 63.7) 60.7
.828] .628| .714| 70.2] 73.4| 69.0} 63.1] 66,1| 65.8
.717| 498 » | 71.5|75.7| 5, | 66.4) 69.9) ;,
776} = .728 5 | 73.5] 79.0] 4, | 63.4) 61.4) ,,
.783 ”? ” 72.0 29 Ey) 64.6 2 29
29 99 99 99 9 99 99 29 29
? ” ” ” y) 29 ry) 5) 3
2 ” bP) 39 99 29 by) by) bP)
5) By) 29 ” 9 DD 39 39
“795! 597 » | 73.6)'75.0] ,, | 64.9]/68.1] 5,
.736| .599 >> | 72.0| 73.7] ,, |68.0]67.8] ,,
-788| .665] .808) 72.1] 75.0) 68.2) 63.5] 64.2) 62.4
-767| 623} —.773) 70.7) '76.5| 68.3) 64.7| 64.9] 62.7
843} .653) .791| '70.0| 77.3] 65.0) 60.4) 63.5) 61.9
804] .653]} 785! 69.7| '7'7.8| 69.4) 63.1] 64.2] 63.4
772) .749) 898] 70.5) 76.8] 69.7! 64.3) 58.9] 57.1
-928] .692) .879| 67.6] 76.0] 67.7|57.0| 62.3] 59.1
-937| .799| .905| 69.2} 75.0) 67.6| 58.0| 58.5] 58.5
28.011; .782| .929]71.1| 76.3) 68.7) 54.9] 59.7) 57.6
27.957| .745| .933] 71.9] 76.0) 68.1] 55.6] 61.5] 57.6
.868| .733| .856]'71.5| 76.0) 70.4] 59.7| 60.6] 60.3
810] .633| .765] 72.0| 77.2, 70.8 62.7| 65.8] 64.8
-833| .715) .848] 73.0) 76.3) 69.8, 62.6) 62.3] 60.9
-882} .689) .802| 71.4) 76.4) 68.9, 59.3) 62.91 62.8
823) .646) .842)72.9|'77.1| 69.6 62.2] 65.2) 60.7
872) .748} .906] 72.0) 75.2 Oral 59.5] 59.7| 57.0
-942) .792!| .881]'71.0)76.8 69.1) 56.7] 58.6 58.9
.877| .830] .895|'71.6|77.9 69.5 60.0] 56.6] 59.2
911} .797| .9381]71.2\76.9 68.9 58.6} 58.4) 57.5
27.835) 2'7.690] 27.843] 71.4) 76.0 lee 62.9| 60.7
Meteorological Observations.
itt
GANGAROOWA NEAR Kanpy, CEYLON.
nm
m
oS
Humidity. Si
ty “ 2
2 3
ea| 2
| EE
a.m.|p.u.| Pu. | ao] &
SOUS
9.30/ 3.30 | 100/29 | ‘2
Be
779 | 672 | 785 | 5, |62.1
774 | 706| 888] ,, |56.0)
825 | 676 | 830] ,, | 55.6|
780 783 892 |} 5, | 51.0]
835 820 » 3 | 64.7
708 624 ” » =
780 > Ee) 33 39
33 39 2 33 23
3? 32 22 23 29
32 22 33 33 2
33 39 3) 29 22
ae aeotp. | e155
Sa seo a ty le ss
maga GSS) S20 7 3. | ss
s10 | 678 { 824] 4, |55.8
728 634. 910 9 |o2.7
796 | 631] 813} , | 55.1
805 563 636 | 136.5) 54.1
685 | 630 | 740 | 135.8) 50.8
668 | 562 | 725 | 132.4) 50.0
563 | 565 | 670 | 134.1/53.3
561 | 610 | 685 | 136.0) 54.4
662 | 590 706 | 131.9) 52.2
725 | 682 810 | 139.6) 59.6
700 | 624 | 732 | 135.9| 59.0
654 | 636 | 833 | 135.2/ 56.2
694 | 670 | 760 \ 137.4) 59.9
646 | 582 | 650 | 141.6) 55.9
606 530 | 696 | 133.2) 51.2
666 | 536 695 | 136.6) 51.2
642 523 660 | 132.7) 53.2
721 | 647 | 760. | 135.6) 59.2
| Maximum in Air.
76.2) 62.2
| Minimum in Air.
b= a
i= | Difference.
=)
i
x
bho
15.0
| 18.3
2
°
10.6
NORM ys Oo NN
Oe tO-T oO oO
Rain,
A.M. | P. M.
Total.
9.30 | 10.0
Meteorological Observations.
iv
GANGAROOWA NEAR Kanpy, CryLon.
P. M. 3.30
A. M. 9.30
BhROOWROCO COOODSOD HNOSOSOSH FOORRGSGQ AWS | wo
"TRIO, BODSH S Bower ASH WSSHAGSBS Mw ~
ne ri
Si ee SS
SOSOONSOS SOTSOSSS SCSOSSSSSO SSSWSSSD 999 S
‘gnqVayg W SMqUITyy Sa an) | qi
| Seq SSs SS SOOO qann~ TOW TaNMSODSS S a
“snyeryg-opnUIND i) eSonHAS SG TOM OW NaN | a
SOOOO00O CO5000090 OSOSSSS CSO095S909 999 S
‘snumg | ro)
Soo a ee ee
SOOOOOO SCOOSCON SOSOSSSS SSSSHSS AWS rc]
*sn[MUIN?-O4AT() iS A =) on | fo)
SOOOOOO OCOO0000 SCSOSDSSDSS SSOOHSD9SS CSS a
*g4yV14G-OLILD | CR | ri
eee
RRDHONSO SOSSCSSOOR WONSSSOS SOMOSSS Eoo =
‘snartg | Oor S G6 Gow BSH Aro x ~ | xi
SIG MISIOIS IO MSS IOS lS Cl nm Ceona et So SS See Xe)
: BOON a SBASHSS SSHranS nS 19S
TPO.
SOOONSO GCOOO500 SCSOS0S095 SSSS999 S99 | g&
“SNYVAIA D SNCUIT NT | S | 3S
BHOoSeOoCoO SCOSCSSCON SOOOCSCO ONONOWHS ON —
‘SHyBAPS “ONIN | Ro a So ® S 2 - © oR | 3S
‘snug | SCOCDOCOCO CODOSSDOo COCO OSDSDo C99090099 99° | 2
| eocogcs Soocses MOOOOOS SSOSOSCSSS 9290 Ney
*SMMUINY)-O4ATC) | er) ros) = ros)
“enqusg-o.ttg | oooooo°o ooooo0e oooooco MEME BCIEMEME) ooo | =
SamMoeoe GVOOOooCo Gowns (_Secrors ooo ry
sent | HOS SBASASOS SaOrK FO x
: Lond = ——
° oan oO aA MmOMm~OoRDOrs Mo in co re © aon
post ‘Krenwe | AAD WOOD DR ARMA AAN ANAAANAN NOM |
Meteorological Observations.
GANGAROOWA NEAR Kanpy, CEYLON.
mossg | BZOQSSLSSS SOSSSOH HKSAHHR BOOANRA was 19
p SHANNA SG ARRHHOH HOHMASCM NAOH a}
ied yooy Ur aOoTe | DOAN S H DNONH OE SCBNGFOOGS SHH 19
a :
=
3 oe ye 5
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= ‘S) slsbje (se 8 8 9 8 3 eo SR Eh stchel= fe dei eh Sl dela) 3
S 4 By o8s ti Piri:iz £202,969 ,9 SA 5% 07,0 oF 3
de shite aie seasptcaee :
OE 2 oa7a AAAZAZA44Z4A Apa"4g4 AA
eel ° Z
Meteorological Observations. X1
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of February, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
© 2 . | Range of the Barometer = oO Range of the Temperature
oOo +
i for each hour during me for each hour during
H Pom the month. bo the month,
our. | = So 5 2
Bee = 2
S52 | Max. | Min. | Diff.| 36 | Max. | Min. Diff.
= =
Inches. | Inches.| Inches.| Inches.| 0 cy) 0 0
eS eng 53 70.2
night. 967 | 30.058 | 29.873 | 0.180 0. 74.6 66.6 8.0
1 957 051 .863 188 | 69.5 | 74.6 69.6 - 9.0
2 947 044 | .853 191 | 69.1 | 73.6 64.6 9.0
3 .937 .035 845 | .190 68.7 720 64.0 9.0
4, 937 -036 | .842 194} 68.1 72.2 63.0 9.2
5 951 044 | .854 190 | 674) 71.8 62.7 9.1
6 969 068 |} .862 206 | 66.8 | 71.1 62,2 8.9
7 994 086 | .888 1198 | 66.7 | 71.6 61.2 10.4
8 | 30.023 112; .913 199 | 69.4 | 74.8 66.0 88
2 048 | .141]} .945 196 | 72.8 | 78.6 67.8 10.8
10 .059 157 | .953 .204 | 75.8 | 81.0 69.0 12.0
il 048 ~| .157 | .917 240 | 77.1) 83.2 70.6 12.
Noon. 020 | .184 | .904 2380 | 79.3 | 85.5 71.4 14.1
i | 29.985 081 | .867 214 | 80.6 | 86.4 72.2, 14,2
2 951 048 | .843 2050 (eS C Onl S 720 75.2 11.8
3 .932 025 | .843 182 | 81.9 | 87.8 76.0 11.8
+ Sel 015 | .826 189 | 81.3 , 86.8 75.6 11.2
5 922, 019 | .822 197 | 79.9 | 86.0 74.0 12.0
6 927 033 | .802 231 | 77.5 | 83.0 73.0 10.0
7 943 047 | .824 .223 | 75.5 | 80.6 72.2, 8.4
8 .958 055 ; .858 197 | 74.0 | 78.8 71.1 7.7
9 974 .070 | .858 PALA 7S Nps) 70.1 7.2
10 983 077 .866 211 | 71.7 | 76.4 68.6 7.8
il .980 073 | .878 195 | 70.8 | 75.2 67.4 7.8
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther.
mometer Means are derived from the Observations made at the several hours
during the month,
xii Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of February, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
2 3 as 5 3 BO So Ss S a
3 ermluite: Wie ge pes |252)Hes
2 Come & eames 2) 2 2
oe ° o S) oO » Ss 55 Umeha
Hour. eS 3 a S ae Oo a 2 a E, = =
| 3 2 = ay (unseat a4" 2 | @ ocr
| = AS = = 5 i= a 75 2
22 S Ss Sih mahi, iegeiion te ees |e
o & ce a. As Sie | eles) |S Seer aeeeme
= 5 >. E pe | ee | sie | eo oe eee
a A S A S pay ene) ff) SSS Es
o ry 0 o Inches. |Troy grs./Troy grs.
Mid- | gga | 41 | -e28 | 74 | 0574 | -692 | 1493 | oe
eaniit Ne a. ] . O04 5 .
aa 65.8 3.7 | 62.8 6.7 B74 82 56 .80
2 65.6 3.5 | 62.8 6.3 BTA 33 A5 i
3 65.3 3.4 | 62.6 6.1 570 2 AO 82
A, 64.8 3.3 | 62.2 5.9 563 2 134 82
5 64.3 3.1 | -61.8 5.6 1555 14 25 83
6 63.6 3.2 | 61.0 5.8 AL 5.99 27 83
7 63.6 Ba MG al 5.6 543 6.01 122 83
8 64.8 4.6 | 61.1 8.3 548 5.98 88 76
9 65.8 70 | 60.2 | 12.6 527 76 2.95 .66
10 66.7 8.6 | 60.7 | 146 536 82 3.58 62
ll 67.3 98 | 604 | 16.7 .530 75 4.17 58
Noon.| 67.9 | 11.4] 59.9 | 19.4 521 63 96 53
1 68.1 | 125 | 59.3 | 21.3 bl 50 5.51 .50
2 68.5 | 131 | 593 | 22.3 11 49 85 48
3 68.3 |136 | 588 | 23.1 503 239 6.05 AT
4 68.0 | 13.3 | 58.7 | 22.6 501 38 5,86 48
5 67.9 | 12.0 | 59.5 | 20.4 515 5D 2RU ae
6 68.1 94 | 61.5 | 16.0 550 96 4.08 .59
7 68.9 7.5 | 62.7 | 12.8 572 | 6.22 3.24 .66
8 67.5 6.5 | 62.9 | 111 576 29 2.75 .70
9 66.8 6.0 | 62.0 | 10.8 559 sitrl .60 70
10 66.5 5.2 | 62.3 9.4 2565 .20 23 74
il 66.1 4,7 | 62.3 8.5 565 .20 .00 76
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations. xiil
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
an the month of February, 1865.
Solar Radiation, Weather, &c.
Ps | OO
SE i265.
eee ia | Pee go
-| = |S & & Prevailing direction General Aspect of the Sky.
- Pia aoc of the Wind.
Ala” jared
| o |Inches,
1) 130.9 | S. W. & variable. ‘i & “i till 3p. m. cloudy afterwards,
also drizzling at 3 a, M. 10 & 11 P, uM.
2} 139.0) 0.10 | N. & N. W. Cloudy till 8 a. mw. Scatd. clouds till 5 P.M.
cloudless afterwards also drizzling from
midnight to5 a. M. & foggy from 8 te
10 P. M.
ot 140.40 =, W. Cloudy till 3 Pp, wu. cloudless afterwards.
4 tee O eo lN. Wie Ws Clondless till 3 a. m. cloudy till8 a. M.
Ni & i afterwards.
Spies ce Sunday.
6) 145.5 |W. &N. W, i.
7 140.0 IN. W. & W. Cloudless till 10 a. um. “i afterwards.
8) 137.2 |S. W.&S. Cloudless till 8 a. mw. 91 till 6 pv. m. cloudy
afterwards also drizzling at 8 & 9 Pp. M.
731i nee at Ss. W. &N. W. Clondy till 6r.mM. \i & i afterwards ;
also drizzling atl &9a.uM. Gat 1, 5d
& 6 P. M.
10) 134.8) 0.72 |S. & N. W. ‘i & i till 4 a. u. cloudy afterwards,
also thundering at 10 a. uM. & raining
between 10 G11a.u. Gat4,5&11?, mu.
cH ae 0.20 | 8. &58. H. & i. Cloudy : also drizzling after intervals.
13| 140.4| ,.. |N.W.&N. &N. E.| i till 4 4. wu. cloudless afterwards: also
slightly foggy at 11 P. u.
G4) 141.27 oe N. W. Cloudless.
15 139.5; ... | N.W.& W. Cloudless till 2 a. uw. Seatd. clouds till 11
A. M, cloudless afterwards.
16) 138.0 W. & WN. W. Cloudless.
17| 139.2 W.&S Cloudless till6 a. mu. ‘i till 10 a. uM, “i
&
till 6 P. uM. cloudless afterwards.
W. Cloudless till 7 a. um. “i till 6 p. mw. cloud-
18} 140.7; ,.. |S.
less afterwards, also fogey ato & 6 A, M,
iL ww. | Sunday
20| 143.0 S.&S8. H. Cloudless.
2M FAVA) C. N. W. & W. Cloudless.
22) ’3NG|.. 3. 8. &N. W. Cloudless till 5 a. mu. Scatd. clouds till 2
p. M. cloudless afterwards, also slightly
drizzled between 10 & 11 a. u.
.W.&N., Cloudless.
s. Cloudless till 11 a, m. 1 till 6 Pp. uy, cloud.
less afterwards.
Mi Cirri, —i Strati, \i Cumuli, -i Cirro strati, ~i Cumulo strati, W-i Nimbi
\ i Cirro cumuli.
4
XIV Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
on the month of Kebruary, 1865.
Solar Radiation, Weather, &c,
Ba |PS
os lees eye
.| 2 |S S | Prevailing direction General Aspect of the Sky.
S| xs 1259 of the Wind.
BS) Ss jax 3
Ala = jas
| o [Inches
25| 139.5| ... | HE. & variable, Cloudless till 7 a. m. Scatd. clouds after-
wards, also fogey between 4&7 A. M.
& slightly drizzling at 94. uM. & 4 P. M.
Z26it es 0.66 | Sunday.
27; 1386.0} 0.18 | N. W.&N. Cloudy nearly the whole day; also thun-
dering and raining between 1 & 2 a. uM.
2B ASRON TING Wi. Cloudless till 5 a. mM. “i till9 a. Mu. cloud-
less afterwards.
Meteorological Observations. XV
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of February, 1865.
Montruty Resvrts.
Inches
Mean height of the Barometer for the month, .. oe -. 29.972
Max. height of the Barometer occurred at 10 & 11 4. u. on the 15th & 28th, 30.157
Min. height of the Barometer occurred at 6 Pp. M. on the 10th, «- 29,802
Extreme range of the Barometer during the month, ae ee =: 0.85
Mean of the Daily Max. Pressures,.. oe ee ee 930.062
Ditto ditto Mime ditto © ee 36 -- 29.907
Mean daily range of the Barometer during the month, .. ee 0,155
cy)
Mean Dry Bulb Thermometer for the month, .. ee ee 73.7
Max. Temperature occurred at 3 p. M. on the 20th, Ac ote 87.8
Min. Temperature occurred at 7 a. M. on the 7th, it aid 61.2
Extreme range of the Temperature during the month, ee 00 26.6
Mean of the daily Max. Temperature, SC oo AO 82.1
Ditto ditto Min. ditto, .. ae «eo ate 66.5
Mean daily range of the Temperature during the month, .. 40 15.6
Mean Wet Bulb Thermometer for the month, .. Ste 50 66.5
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 7.2
Computed Mean Dew-point forthe month, .. de as 61.5
Mean Dry Bulb Thermometer above computed Mean Dew-point, oC 12.2
Inches
Mean Elastic force of Vapour for the month, .. ae ae 0.550
Troy grains
Mean Weight of Vapour for the month, nc ve Ac 6.01
Additional Weight of Vapour required for complete saturation, Ae 2.95
Mean degree of humidity for the month, complete saturation being unity, 0.67
) Inches
Rained 10 days, Max. fall of rain during 24 hours, uh a 0.72
Total amount of rain during the month, cn at Be 1.86
Prevailing direction of the Wind, .. ae ith N. W. & W.
XVi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of Hebruary, 1865.
Monruty Rersvrts.
Vables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
= = =| a s S Ss I site
° o ° ° ° ne) e ro)
afal=| letile! (slele! lelEls|al ale
N. S17 [2 | B. [ot foi ce |S-la loi [aE |e ta lea 1S |e lS
No. of days.
Midnight. 1) 1 , 8 3 4) 1 6 2
1 1 11 | 8] 2) 4 4, 6} 1
2 1 1 H 5 4) 1} 6 gy il
3 1 1 fe) | 3) | 9} a7 1
4 iL We a 2 6) 1410} 1 3
5 3 1} yl 2 OM TU | 8 A 3
6 3 1 1 1 2 1 8 li
J 5 2 1 1 1 3 4 8
8 6 2 2 1) 47 2 3 2 6
9 5] 11 3| 2) |2| fai apal ail fe
10 3 5 2 3} Ij A 3 4,
11 3] | 4 4) }2, fa} aal fel fala
Noon. 4, 4, 2 3] ff 2 3 2 4
1 5 4 1 bh | Pet 3/ If 4 5
2 1 1 2 2) 473 3 4 8
3 1 1 1 2 1 3 7 8
4. 4) 1} 1} 2) 9 2 2 4 9} 1
5 3 1 1) 9 5) 1) 2 6| 1] 6
6 1 1 2| W 4) 1} 5) 116 5
7 1 1 5 6 6 5
8 2 1 } 4 6| 1} 6 5
9 2 il i) 5) A) 1 7
10 2 1 | 7 4) 1} 4 6
11 1 | 8 2 6| 2) 7
Meteorological Observations.
Xvi
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of March, 1865.
Latitude 22° 33’1” North. Longitude 88° 20’ 34” East.
Feet,
Height of the Cistern of the Standard Barometer above the Sea-level, 18.11.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
Date.
|
OCOntn anhwone
27
28
29
30
31
Mean Height of
the Barometer
at 32° Fabt,
Inches.
30.017
29.966
.923
-909
Sunday.
927
-930
-929
924
948
962
Sunday.
937
951
987
39.004
29.998
961
Sunday.
.948
-946
893
859
838
848
Sunday.
851
828
852
859
.880
Range of the Barometer
during the day.
Max.
Inches.
30.094
.040
.000
29.971
992
30.021
29.996
30.005
043
:023
.009
057
029
094,
.090
039
-032
-039
29.975
948
908
2920
-932
912
21
940
.965
Min.
Inches.
29,957
.907
.832
-820
852
867
580
874
888
914
2893
887 |
-900
952
937
886
894 |
881
819
ATA:
790
795
781.
765
.790
813
828
Diff,
Inches.
0.137
lio
168
allie
140
154
116
131
155
109
ANE
170
129
142
153
153
138
158
156
174
118
130
151
147
131
LPT
135
Mean Dry Bulb
Thermometer.
a
gt 8 ©
oo
73.4
Range of the Tempera-
ture during the day.
Max.
)
82.3
85.4
84.4:
83.8
78.4:
81.2
76.0
83.0
85.4
85.8
86.7
83.8
843
86.6
87.8
91,4:
93.2
91.2
94,8
94.4
94.7
96.3
97.6
97.8
94.3
93.8
95.0
Min.
63.6
66.8
70.0
68.8
68.0
68.1
68.7
69.2
72.4
71.5
72.8
70.8
70.6
68.0
64.9
69.2
73.6
75.2
76.8
71.8
74.6
74,0
76.8
76.2
78.4
76.9
76.7
Diff.
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther~
mometer Means are derived from the hourly Observations made during the day. .
xvill Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of March, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—(Continued.)
s i E S 5. |ag 16
2 3 z a 2 a eee ane
Seo A | gS ee eee
= o S) = an) £o42|s62°3
3 CS E 2 © pyc = De
Date.| 7. 2 a) $$ fo = Bee ihc = on
| 83 2 z = Si | BS || Seales
| Bs a 2 ee Meee eN eels) os — =
Hees a a. 5 aS Mite ese sts) | se =
$A a 5 po | > | 88 |2ag] S38
| 2 a) os) a) = = S =
| o 0 o 0 Inches. | i gr5 | Wier:
1 64.5 8.5 57.7) 15.3 0.485 5.30 3.46 0.61
2 69.3 6.6 64.7 | 11.2 611 6.65 2.92 70
3 69.6 7.3 64.5 | 12.4 .607 .60 3.26 .67
4 68.7 6.7 64.0 | 11.4 97 -00 2.93 69
5 Sunday.
6 68.5 3.1 66.0 5.6 .638 7.00 1.40 83
Af 69.9 3.2 67.3 5.8 .666 .28 51 .83
6.4 68.5 3.1 65.5 6.7 .628 6.88 67 81
9 | 70.9 5.5 | 67.0| 94 | .659| 7.17 | 255 | 74
10 | 72.0 5.9 67.9 | 10.0 .679 .36 .80 72
1k 72.3 6.0 68.1 | 10.2 684 -40 88 72
12 | Sunday.
13 70.6 8.5 64.6 } 14.5 .609 6.58 3.95 .63
14, 69.6 7.2, 64.6 | 12.2 .609 62 21 .67
15 69.0 eg 63.6 | 13.1 .090 -40 40 .65
16 65.9 11.0 58.2 | 18.7 493 5.34 4,52 04:
17 65.1 ult? 56.9 | 19.9 A72 Al 72 02
18 66.9 13.1 57.7 | 22.3 A85 «22 5.59 48
19 | Sunday.
20 0) 700 13.3 | 60.7 | 22.6 536 72, | 6.20 48
21 70.5 12.4 61.8 | 21.1 .500 .95 5.84 col
22 72.4 11.3 64.5 | 19.2 .607 6.50 .57 4
23 72.4 102 65.3 | 17.3 .623 .69 499 Yi
24 | 72.4 10.9 (eye! || alfeys 619 63 5.40 .55
25 73.7 10.6 66.3 | 18.0 644 .89 a9 56
26 | Sundoy.
27 74.6 11.7 66.4 | 19.9 .646 88 6.14 08
28 74.3 11.4 66.3 | 19.4 644 88 5.92 04
29 778 6.7 73.1 | 11.4 .803 8.60 8.75 -70
30 75.7 8.1 70.0 | 13.8 027 7.78 4.32 64
31 | 74.4 10.2 67.3 | 17.8 666 12 5.27 08
All the Hygrometrical elements are computed by the Greenw ich Constants.
Meteorological Observations. X1x
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of March, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
°c =; | Range of the Barometer = 3 Range of the Temperature
age for each hour during Ag for each hour during
He: = 2 = the month. Po the month,
= tees RE 7
2 Ge eS |
= | Max. Min. Diff. Sc) Max. Min. Diff,
= | &
Inches. | Inches.; Inches.| Inches. ty) 0 0 °
Mid- a "5
night. 29.919 § 30.054 | 29.822 | 0.232 0 81,3 68.0 13.3
if; .910 .043 813 .230 74.3 80.8 67.0 13.8
2 .898 .033 .805 .228 Wall 79.4: 65.8 13.6
3 .888 .018 -798 .220 73.2 78.8 65.2 13.6
4, .888 -003 .802 201 72.7 78.8 64.4 14.4
5 .905 .019 813 | .206 W221 78.6 64,0 14.6
6 .926 .031 .832 .199 AL e/ 78.6 63.8 14.8
7 .948 .042 854 .188 72.3 78.4 63.6 14.8
8 .975 .065 .888 Gal 75.4 81.3 68 2 13.1
9 .993 -083 -906 177 78.8 86.0 68.4 17.6
10 .998 .094 .905 189 81.7 89.4 68.1 21.3
11 .987 | .088 .896 192 84.2 93.2 74.0 19,2
| |
Noon. | .963 071 | .872 199 | 85.9 | 95.0 | 74.2 20.8
1 .934, .040 .851 189 87.1 96.2 75.0 21.2
2 898 | .005 811 194. 88.0 97.6 76.0 21.6
3 877 '29.977 -776 .201 88.1 97.8 75.6 2222
4, 867 | .965 TEA) | ells 87.7 97.6 74.9 22.7
5 .865 .959 76d 194 86.4 96.1 72.6 23.5
6 872 .957 177 .180 83.4 91.6 71.8 19.8
7 .888 .969 791 178 89.9 88.0 70.8 17.2
8 .906 -988 | .812 176 79.2 85.2 70.2 15.0
9 .918 (30.001 .831 170 78.0 83.8 69.6 14.2
10 ee \ 1015 1 837 LTB Wa 82:9 70.3 11.9
11 924. .008 823 185 76.1 81.4: 70.0 11.4
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several hours
during the month.
20:< Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of March, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
2 3 3 E S 23 (sone
oc nk MiMi ues = |= 22
@ fs @ & o-8 mle | oss
Se ie Se 2 Bees | 2s
Hour. eS 3 a s wo “eO Om tenes oe
ee Oe IOC he 2S | 2 22
EO 3 3 Ee Foo 5 & oS a2 a 2
ai tre Pee So oMeleai2 25 | 22s
Ss |b) £2 | pa | ge | 8 6... BS 8 leis
= a) ‘S) fa = SSCs ra gs
1
0 to) 7) () Inches. |'Troy grs./Troy grs.
a 69.7 | 53 | 660 | 9.0 | 0638 | 695 | 236 | 0%
il 69.55) 4:81. 66.0 8.2 | .640 99 13 17
2 693 | 44 | 66.2 hes Wp Gee | GON 1.95 78
3 69.2 | 4.0 | 66.0 He | NBS GOS 84 79
4 68.9 | 3.8 | 65.9 6.8 | .636 96 72 .80
5 685 | 3.7 | 63.5 6.7 | .628 88 67 81
6 682 | 3.5 | 68.4 63 | 1626 87 eG 82
7 686 | 3.7 | 65.6 Gi | ERO .90 68 80
8 70.0 | 5.4 | 66.2 92 | .642 .99 2.4A 74
9 70.9 7.9 65.4 13.4 .626 17 3.67 .65
10 Fala OlON | G4e7) orn ona BT 4.80 58
11 72.0 | 12.2 | 63.5 | 20.7 | .588 27 5.97 bl
Woon, | F200 13.9) ||) 62.3)! 123.67) 565 01 6.86 AT
1 79.1 | 15.0 | 631 | 240 | .580 16 717 46
2 49.4, | 15.6 | 63.0 | 25.0 578 13 55 45
3 793 |158 | 62.8 | 25.3 574 10 62 45
4 792 |15.5 | 62.9 | 248 576 11 AS 45
5 TG), PUB Eh APO AN ee. es 17 45
6 ral dale |) 63.5) 1 1910) |) 5ssinl yao 5.67 53
7 719 | 9.0 | 65.6 | 15.3 | .630 79 4.31 61
8 is hE ak Was yy GAO 92 3.64 66
9 Ty | BS |) Gea | ie 646 | 7.00 19 68
10 71.0 | 60 | 66.8 | 10.2 | .655 11 2.78 72
ll 70.7 | 5.4 | 66.9 9.2 | .657 15 AS 74
_
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations.
XX1
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of March, 1865.
Solar Radiation, Weather, &c.
zd jms
Sey) See ae
see jO = 9 | Prevailing direction General Aspect of the Sky.
=| #3 |282| ofthe Wind.
n= = = 10 ©
0 _|Inches,
1) 137.6 Ee Wer cnNi See Cloudless.
2| 136.0 Per Se Cloudless till 9 a, mu. Scatd. clouds after-
wards.
ap fae OPP, 1S. Cloudy till 7 4. mu. Scatd. clouds till 8
i Pp. M. cloudy afterwards.
4 135.0 8. &N. 4. Cloudy till 10 a.m. ni & “i till 4p. mu.
cloudy afterwards.
7 eee 1.08 | Sunday.
Gls 0.54 | H. GN. Cloudy also raining at midnight & 2 a. M.
& drizzling from 4 to 8 P.M. & at 11
p.M. & thundering at midnight & 5
P.M. & lightning at 1 a. uM. & at 8 P.M.
7| 135.4) 0.25 | N.& N. W. Cloudy till 10 a. mu. i till 3 P. wm. cloudy
afterwards: alsoraining at9 & 10 A. M.
& drizzling from 5 to 9 P. M.
Sie --- S.W.&W.&S. Cloudy: also drizzling at 2,5 & 7 P. u.
9} 137.0} ... |E.&W Cloudy till 7 a. um. i & “i afterwards.
10) 141.0} 0.09 | H.&N. H.G&N. W.| -itill 6 a.m, thin clouds till 10 a.m.
“i & 11 till 5 p. um. cloudy afterwards ;
also drizzling from 7 to 10 p.m. &
lightning at 7 P. M.
11; 139.8 . |W.& N.W. Cloudless.
2) ee . | Sunday.
13| 145.8 N.WG&N. Cloudless till 3 a. mM, “itill3 P. Mm. Scatd,
, clouds afterwards.
14| 134.9) ,. |N.W.&GW.O&N, Ni & +i till 2 p.m. Scatd. clouds after-
wards.
15; 135.0; ... | N.W.&N. i till 4 P. uw. cloudless afterwards.
16, 140.1) ... | W.&N. W. Cloudless.
Abs AO) |e eel Nei Wi. GoW Cloudless till 11 a.m. “i il38 em Ni
till 6 p. mM. cloudless afterwards.
18, 141.0} .,, | W.& N. W. itil 7 a.m. “i till 6 Pp. M. cloudless
afterwards.
BON 50 Sunday.
20 146.4 W.&S.&N.W. | Cloudiess till10 a.m, i & Yi till 2.
cloudless afterwards.
ZAL NAL OW)... S.W.&N. W. G&S.) -i till 1p. uw. 9i afterwards,
22| 142.2) ... |S.W.&W.&S. i till 4 p.m. cloudy afterwards, also
slightly drizzled at 8 ep. um. & lightning
at 7 P. M
23| 142.0 ye S.&N. W. i till 6 a. uw. cloudless afterwards.
24) 141.0] ,,, |W. &S. W. Cloudless: also foggy from 3 to 6 A. M.
\ i Cirro cumuli.
}
“Mi Cirri, —i Strati, \i Cumuli, -i Cirro strati, ~i Cumulo strati, -i Nimbi
XXil Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
wm the month of March, 1865.
Solar Radiation, Weather, &c,
ts Oe)
+ 2S Oe 5 Prevailing direction General Aspect of the Sky.
S| 4s 1839 of the Wind.
S| Sse fan -
Ala jped
==}. — —_ ——
| 0 |Inches
25) 142.0} ... |S. W. & W. Cloudless: also fogey from 5 to 8 A, M.
26] vee =| Sundoyy.
27| 141.6) ... |S.GW.&S. W. Cloudless.
23) T4IOUs 27. 4) Se Cloudless,
29| 137.0 aa Ws Cloudless till 3 p. mu. \-1 afterwards.
30} 137.6) ... |S. &58. W. Cloudless till 8a um. i & “i till 4p,
Scatd. clouds afterwards, also raining,
thundering and lightning at 8 P. mM,
31) 144.0; ... |S.W.&S. Scatd. clouds till 6 a.m. “i & i till 6
p. M. cloudless afterwards.
Meteorological Observations. XXili
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of March, 1865.
Montuty ReEsvuts.
Inches
Mean height of the Barometer for the month, .. oe e. 29,920
Max. height of the Barometer occurred at 10 a.m. onthelst & 16th,.. 30.094
Min. height of the Barometer occurred at 5 Pp. M. on the 28th, e- 29.765
Extreme range of the Barometer during the month, ee e- 0.329
Mean of the Daily Max. Pressures,.. ae eo ee 30,000
Ditto ditto Min. ditto, .. oc 50 «- 29859
Mean daily range of the Barometer during the month, .. oo §«©«.: 01 41.
Oo
Mean Dry Bulb Thermometer for the month, .. 50 AB 79.4
Max. Temperature occurred at 3 P. M. on the 28th, 56 50 97.8
Min. Temperature occurred at 7 a. M. on the Ist, 5c 00 63.6
Extreme range of the Temperature during the month, .. Be 34.2
Mean of the daily Max, Temperature, oe eo oe 88.5
Ditto ditto Min. ditto, .. ae AC os 71.6
Mean daily range of the Temperature during the month, .. Ad 16.9
Mean Wet Bulb Thermometer for the month, .. a an 40.7
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 8.7
Computed Mean Dew-point for the month, .. ae my 64.6
Mean Dry Bulb Thermometer above computed Mean Dew-point, Bs 14.8
Inches
Mean Elastic force of Vapour for the month, .. 50 e- 0.609
Troy grains
Mean Weight of Vapour for the month, ae se ee 6.58
Additional Weight of Vapour required for complete saturation, mA 4.04,
Mean degree of humidity for the month, complete saturation being unity, 0.62
Inches
Rained 6 days, Max. fall of rain during 24 hours, we oe 1.08
Total amount of rain during the month, Ae a ee 1.96
Prevailing direction of the Wind, .. a S.&W.& N, W.
XXIV Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of March, 1865.
Montuty RESULTS.
Wables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
3 § VS SS MN SH ens teehee
cite eials] |sielel | stElsts) ale
NJ 217 || EB. |elaleiS.claleielelaleiSigle
No. of days
Midnight. 2 Sa Hel 2 5} 1 3
1 ay |i a fs| | 5] | 7 Ja
2 ib) || Bil a isi | 5) Joel | 4
3 i 2 1 H 5 5 8 4 i
4 2 1 1 H 5 A, 8 4. 2
5 2) [a 1| fs sl Pal 74 1
6 2 1 Uy) 6 9 3
7 2 1 1 7 3} fll 3
8 ml 2 }5) je) [4 17
9 3 2 i 1) 5 5 6 A
10 A 2) 2| 1} 1) Yl 7 5 5
11 A, 1) 3 ab egy 2 7 5
Noon. 3 1 2 1 4 2 5 9
1 1 NU Pepe Ta VPI) il
2 3, [1 2 15) | 2} | sj apa
3 2 1 2 1 6 7 9
4, Teal foal i 5 4. 8 7
5 2,111 2a fe | 3) ifs) | 5
6 Li a 2) 2 1 9 3 5 6
7 2) 1} 2) 2 1 110 2) 1} 5 5
8 2) 1 3) 2 19) | 3lap7) ys
9 i Th} AL 2 1} $10) 13 4 4 4, H
10 2 1 f2; ita) 4) | 4
All 3) 1 1 Aid 5) 4, |
|
|
Meteorological Observations. XXV
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of April, 1865.
Latitude 22° 33’ 1” North. Longitude 88° 20’ 34” East.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in,
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
oo 2s
2 E = Range of the Barometer eB 3 Range of the Tempera-
oS during the day. ba ture during the day,
cre ee
Date. | _ e S 3
S22] Max. | Min. | Dif, #& | Max. | Min. | Diff.
a =
Inches. | Inches. } Inches. | Inches. o (a) to) fa)
1 | 29.885 | 29.974} 29.802 | 0.172] 849 96.4 | 75.0 | 21.4
2 Sunday.
3 843 .908 189 119 83.6 94.6 78.4) 16.2
4, 842 918 7/85) 183 83.8 98.2 73.4 | 248
5 .885 94:7 211 136 80.4 90.0 72.4 | 17.6
6 814 888 HET 151 | °83.6 93.0 | 77.0 | 16.0
7 -786 878 BD 163 85.3 94.6 79.0 | 15.6
8 788 .853 731 122 87.5 96.5 81.6 | 14.9
9 | Sunday.
10 S811 .885 746 139 87.5 96.8 80.4 | 16.4
11 .825 .908 rT 137 86.2 96.6 80.2 | 16.4
12 872 949 £785 164 \ 85.1) 93.6 | 78.2 | 15.4
13 .897 .985 .833 «152 84.3 92.1 75.2 | 16.9
14, 877 964, «794 170 85.4 94.6 79.2-| 15.4
15 .816 .885 Jol 154: 85.7 95.2 79.6 | 15.6
16. | Sunday.
ily! £729 795 .675 120 81.5 90.8 76.4 | 14.4
18 824 -905 .716 189 82.6 92.4) 75.4 | 17.0
19 879 -969 .809 .160 84.4 92,5 78.2 | 14.3
20 761 .852 -664: | 188 85.4, 93.6 79.6 | 14.0
21 701 778 622 .156 86.2 94.8 80.6 | 14.2
22 J74A: -795 .673 122 79.6 91.1 3A | 17.7
23 | Sunday.
24, 714 -786 647 139 82.5 91.0 76.2 | 148
25 .706 .786 629 Abi?) 85.7 93.8 79.8 | 14.0
26 736 .808 653 155 86.4 92.6 81.4 | 11.2
27 782 845 .693 152 84.6 91.4 Mine alias
28 .729 .802 637 165 85.6 91.6 80.6 | 11.0
29 .639 WS .526 .189 85.0 90.6 75.8 | 148
30. | Sunday.
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Meaus are derived from the hourly Observations made during the day,
XXxvi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of April, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
: Re S peau eh ala a2
A ey ee eee (oS | 22
S S co) a is © C8 2) Sa a
= é i 5 = 3: |e Sil ee
=) > io 2 ie aS) 08'S = oe S
Date. |). B= a i 3 Bo |228) $e x0
Bou 3 a. coe = Ze x Es
cf | Sl 8 | 8. | a: | £2 eee
ee Ee S| @2 |" 2 eo. eae
Ho = ‘5 2 nee Gules Sil Sse =
5 A ae 8 Pa Ss Sf 2s aieap bese
e a S) Q = = ee =
0 te) 0 0 Iiaelnveys4 || NS are, || GEL eae
1 78.2 6.7 73.5 | 114 0.814 8.70. a9 0.70
2 \ Sunday
3 74.8 8.8 68.6 | 15.0 .695 7 4A 4.59 62
4 75.5 8.3 69.7 | 14.1 720 71 at) .64
5 72.6 7.8 67.1 | 13.3 .661 13 3.8L .65
6 77.8 5.8 Moet Oe) 819 8.78 .25 73
7 79.3 6.0 75.1 | 10,2 .857 9.15 AID 12
8 80.8 6.7 76.8 | 10.7 .905 61 .88 vi
9 | Sunday
10 78.0 9.5 ripepy |) Ris? 183 8.32 B17 62
Oe ee 76 8.6 71.6 | 14.6 766 15 4.84 .63
12 «| TT 7A 72.5) 1) 12.6 787 AL 16 67
aS) ie ego OFZ 68:7 i 1bsG 697 | 7.44 84 61
14, 77.6 7.3 TWAM, We 33533 778 8.381 Bi .66
15 77.8 1.9 72.3 3.4 6783 .30 AA .65
16 Sunday.
il7/ 74.9 6.6 70.3 | 11.2 6134 7.90 3.41 -70
18 75.9 6.7 71.2) 11.4 756 8.12 56 .70
19) © 77.8 6.6 12: 11.2 .806 .63 .68 70
20 | 78.3 dew exe) | Weal 809 63 4.05 .68
21 199 5.3 75.5 | 10.7 868 9.25 3.74 71
22 75.2 4A 72,1 7.5 178 8.39 2.30 79
23 Sunday.
24 78.8 3. 76.2 6.3 .887 9.54 10 82
25 80.8 4.9 77.4 8.3 922 85 95 dl
26 80.8 5.6 76.9 9.5 .908 .66 3.40 7A
27 78.9 5.7 74.9 9.7 851 .09 30 713
28 79.3 6.3 74.9 } 10.7 851 08 68 Affil
29 78.6 6.4: 74.1 | 10.9 .830 8.87 66 71
30 Sunday.
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. XXVIl
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of April, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
Hour.
fet
HOMO MOST OI Co DO HE
A
°
iS}
=)
RPOMOOTA ABR we
ae
the Barometer
Mean Height of
at 32° Paht.
Inches.
29.806
793
-780
-770
oe
790
804
.826
848
.863
864
804
.830
199
769
744
129
725
Tk
763
784
805
815
81L
Range of the Barometer = 2 Range of the Temperature
for each hour during Ae for each hour during
the month. bo the month.
ams
=} &
Max. Min. Diff, Se | Max. Min. Diff.
=
Inches.} Inches.| Inches. Cy) 0 0 oO
29.904 {29.700 | 0.204 80.3 83.4 73.6 9.8
.899 .686 213 79.9 83.0 73.8 9:2,
884 673 211 79.9 82.6 TA 8.6
.878 642 236 19 2 826 73.8 8.8
.875 .646 229 79.1 82.8 72.8 10.0
.898 651 247 78.5 82.6 72.8 9.8
EOS .652 261 78.5 82.4 72.4 10.0
.930 .659 271 79.6 84.0 72.6 11.4
.962 .675 287 8 85.4: 76.0 9.4:
O74 697 277 85.2 87.8 79.4 8.4
.985 .686 299 87.6 89.6 82.0 7.6
oral: .673 298 89.7 92.7 84. 8.7
953 LOS eaO2 91.2 94.6 85.7 8.9
-936 .623 313 92.3 97.0 86.4 10.6
.917 598 319 92.8 97.4 83.4 9.0
.883 558 325 92.6 98.2 84.0 14.2
855 043 312 91.0 ; 97.8 75.0 22.8
.836 -b26 310 89.6 96.2 73.8 2.4
843 .039 304 86.6 93.4 73.6 19.8
.900 099 301 84,2 90.8 72.8 18.0
927 647 280 82.9 86.8 73.8 13.0
931 694 PBY/ 81.7 85.0 73.8 11.2
.906 648 258 81.4 84.4 73.6 10.8
.919 648 271 80.5 84.4 73.4 11.0
The Mean Height of the Barometer,
as likewise the Dry aud Wet Bulb Ther-
mometer Means are derived from the ‘Observations made at the several hours
during the month,
XXVill Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations —
taken at the Surveyor General’s Office, Calcutta,
in the month of April, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
= +3 3
s Ss ae!
Q eS °
eae
eves ° o
Hour. | = S e A
g 2 1
i=) S
S38 Fa 5.
eine | E
= e >)
Oo 10) 0)
Mid- | 766 | 347.) 74.0
night.
1 76.6 31) 74,3
z 76.3 3.2 TAL
3 76.1 ay l 73.9
4 "6.4 27 74.5
5 75.6 2.9 73.6
6 75.8 27 73.9
7 76.4 3.2 44,2
8 TESTI 4.5 74,5
9 78.7 6.5 TAL
2 8.4 74.2
Woon. 79.7 ii) 728
1 79.8 2S 723
2 79.6 lies TA,
3 79.5 Meyil 71.6
4 78.8 12.2 (AN)
5 78.5 TAAL 71.8
6 78.0 8.6 72.8
7 77.6 6.6 73.0
8 77.0 5.9 72.9
9 76.8 4.9 13.4,
10 76.8 4.6 73.6
11 76.5 4.0 Bri
/
eee EEenEEaneed
Point,
J
Dry Bulb above Dew
0)
6.3
5.6
5.4
5.3
4.6
4.9
4.6
5.4
doll
Lou
13.4
16.2
18.4,
20.0
21.1
21.0
19.5
17.8
13.8
11.2
10.0
8.3
7.8
6.8
f
Mean Elastic force o
Vapour.
Inches.
0.827
.835
-830
824
-840
819
824
832
.840
830
832
614
795
783
768
766
763
oh
£795
801
SST
811
817
0519
pour in a Cubic foot
Mean Weight of Va-
of air.
Troy grs.|Troy grs.
8.93
9.01
8.98
Vapour required for
complete saturation.
Additional Weight of
1.98
al
68
64
4.4:
1
Mean degree of Hu-
midity, complete satu-
ration being unity.
All thle Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. XXIX
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of April, 1865.
Solar Radiation, Weather, &c.
22| 127.5| 1.67
1.36
.| @ |© & 8 | Prevailing direction General Aspect of the Sky.
=| HS (282 of the Wind.
5 3S
Als aed
o Inches
EN t40.0)) 3. |S: Cloudless till 1 p.m. ~i & “i afterwards.
Be w. | Sunday.
3| 188.4) ... Ss. H.&S. Cloudy till 9 a.m. Scatd. clouds till 6 P.M.
i afterwards drizzled at 4 Pp. uM.
4) 141.0} 0.73 |S. W.& 8. E. i till 9 a. mM, “i till 4 Pp. . cloudy after-
| wards, thundering, lightning, raining at
6-7-9 & 10 p. mu. & hailstones fell between
5 & 6 p. M.
5) 132.0; ... |W. &S. GN. W. Citill1l vp. um. cloudless till 7 Pp. mM. i
| afterwards.
GietS6:0)}).. 2c S.&S. E. Seatd. clouds till 9 a. um, “i till 3 P. Mu.
cloudy afterwards, thundering, lightning
& raining between 6 & 7 P. M.
eT AST2) 2. |S. aS H Cloudless till 4 a. uM. cloudy till 10 a. mM.
| cloudless afterwards.
8 139.0 S.&8, W..& W. Cloudy till 8 a. m. i till 8 Pp. u. cloudless
| afterwards,
eee Sunday.
10) 136.0; ... |S.W.&S. Cloudy till 9 a. mu. cloudless afterwards.
i 141.0 =o \asH cose MVE Flying clouds till 6 a. mu. cloudless after-
wards.
12) 133.5 eres Cloudless till 5 p.m. cloudy afterwards,
#1 137.0|"... | S.&8 W. \ till 7 a. M. 91 till 38 Pp. M. \-i afterwards.
14] 184.5| ... |S. &S. W. Cloudy till 7 a. m. -itill6 pP. u. cloudless
afterwards,
15} 136.0; ... |S. &S. W. \—i till noon, cloudless afterwards.
1a ee ae Sunday.
17| 186.5| .. |S. H&S, i till 10 a. m. cloudy afterwards,
lightning at 9 & 11 P. u.
18} 132.0| 0.17 | E.&8.&S8. EH, Cloudy till 4 a. mu. Scatd. clouds after-
wards, raining & thundering at 4 P. M.
19) 131.0; ... |S.&S8. W. Cloudy till 7 a. wm. Yi & itil8 p.m,
clondless afterwards.
ZOWUSTOW ic Ss. &S8. W. Cloudless till 2 a. wm. “i afterwards.
21! 132.8' ... | S.&S. W. Ui till 4a. uw. cloudy till 8 a. Mm, “i till 4
p. M. cloudless till 7 Pp. mM. cloudy &
lightning afterwards.
8. &S. H. Scatd. clouds till 1p. m. cloudy afterwards,
raining between midnight & 1 a. Mu. &
from 4: to 7 ep. M. thundering & lightning
from 5 to 7 P. M.
Sunday.
Mi Cirri, —i Strati, 9i Cumuli, -i Civro strati, ~i Cumulo strati, -i Nim)b*
\ i Cirro cumuli,
Raax! Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Caleutta, ,
in the month of April, 1865.
Solar Radiation, Weather, &c,
~ Qe
eg (25.
o.S9 [ss
.| 28 |S © 8] Prevailing direction General Aspect of the Sky.
S| 43 1888] ofthe Wind.
S| GCs (ae
S))| 2S let
o |Inches
24) 128.9 S. E. & 8. Cloudless till 34.mM. 71 & “i till 7 P. uw.
cloudless afterwards.
25 LASS Sian else Cloudless till 5 a. mM. i & “i afterwards.
26] 131.0 Sant: Vitil4a.m. “ié “itil 2m. itil 6
p. M. cloudy afterwards, lightning at 7,
10 & 11 Pe. u.
WA TIBI Oy S Cloudy till 11 a.m. %1 till 7 Pp. m. cloud-
less afterwards, drizzling at 2a. a. & 1
p. M. lightning at midnight.
28| 124.0] ... |S. (high.) i till 8 a. m. “i afterwards.
2 313), || Se Scatd. clouds till6 P.M, cloudy afterwards,
raining between 9 & 10 P. uM. lightning
& thundering from 8 to 10 Pp. mu,
4)
co
—
SS)
N
(on)
i=)
(uy)
Or
BUT eae .. =| Sunday.
Meteorological Observations. XXX1
Abstraet of the Results of the Hourly Meteorological Observations
‘taken at the Surveyor General’s Office, Calcutta,
Qr
in the month of April, 1865.
Montruty Resvunts.
; Inches
Mean height of the Barometer for the month, .. oe 56) ALS
Max. height of the Barometer occurred at 10 A. mu. on the 13th, -. 29,989
Min. height of the Barometer occurred at 5 p. Mm. on the 29th, se) | 2902
Extreme range of the Barometer during the month, fe e- 0.459
Mean of the Daily Max. Pressures, .. ae ee oe 29/871.
Ditto ditto Wha, | ating. 955 ie 55 oq SHEN
Mean daily range of the Barometer during the month, .. cei OMIA;
0
Mean Dry Bulb Thermometer for the month, .. ae ne 84.5
Max. Temperature occurred at 3 P. M. on the 4th, a4 od. a whe
Min. Temperature occurred at 6 A. M. on the oth, 50 ye 72.4
Extreme range of the Temperature during the month, ate es 25.8
Mean of the daily Max. Temperature, ole ee ae 93.5
Ditto ditto Min. ditto, .. ate oo 50 77.8
Mean daily range of the Temperature during the month, .. iy 15.7
Mean Wet Bulb Thermometer for the month, .. 20 50 77.7
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 6.8
Computed Mean Dew-point for the month, .. 50 Ae 72.9
Mean Dry Bulb Thermometer above computed Mean Dew-point, Bag 11.6
Inches
Mean Elastic force of Vapour for the month, .. Be we 0.797
Troy grains
Mean Weight of Vapour for the month, ue a ox 8.52
Additional Weight of Vapour required for complete saturation, a 3.83
Mean degree of humidity for the month, complete saturation being unity, 0.69
Inches
Rained 8 days, Max. fall of rain during 24, hours, An ah 1,67
- Total amount of rain during the month, ie Ls a 4.28
Prevailing direction of the Wind, .. ee ae S.&8. W.
XXXiL Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of April, 1865. -
Montuty RESULts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
Be eT 1st /6] 16) (S0-leh iste
eidle| leldlel lelelel |slelstsisl2
Nuc; ce) Ee |e fon |ea |S. ee fos foo 1 a bs |e 1S |e
No. of days.
Midnight. 1 3) } 1 1 2
1 il A) 1$18 1 1
2 2 Br | 2 1} 1
3 1 2 alt 2 il
4, 2 2 2 1 3
5 2 4, 7 2| |1 4,
6 1 3 a il
7 i 5 i 1
8 2 5 7 1 1
9 1 4, 9 1 1
10 1 3 7 3 1
11 1 1 8 A,
Noon. Sia 5 5 1
1 6) | 6 3
2 1 6] | 8 3
3 9| | 6 3
4 5) 1) | 7} apa) fala
5 1 4, 1f16| | 3) J
6 2) 1 5) 2116 2
7 1 4) 1118 1 1) 1
8 1 1 yi} 1j 2 1
9 aby ab) Bl} 1 2
10 ALi ae 2) H 1j 1 1
11 1] | 3) | 1
a eel
Meteorological Observations. XXXII
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of May, 1865.
Latitude 22° 33’1” North. Longitude 88° 20’ 34” Hast.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
os aS
= E = Range of the Barometer Pa 2 Range of the Tempera-
oe during the day. Le ture duving the day.
220. ER:
Date.| _ a & = z
| $22 {1 Max. | Min. | Dif. aa Max, | Min, | Diff.
a =
| Inches. | Inches. | Inches. | Inches. 0 (0) (0) 0
1 | 29.542 | 29.609 | 29.452 | 0.157 | 849 92.0 | 77.6 | 14.4
2 .608 673 | 551 122 85.6 92.6 79.4 | 13.2
3 057 ~.625 438 187 85.9. 92.6 78.4 | 14.2
4 506 .589 447 142 87.4 92.6 83.2 | 9.4
§ ) «045 .657 .476 ASD. 87.0) 1) 94'8 ) 80:30) 14.5
6 -682 806 590 216 | 81.9 93.4 | 73.0 | 20.4
7 | Sunday.
. |
8 80 745 SSS 52) oe8e | 85.6.0 77.0) | 2S.6
2 619 .678 584: | 144, 81.9 89.8 74.9 | 14.9
10 643 “7iBS) | 089 NEO | Pee ll Bes 73.0 | 13.3
KE 610 .669 21 148 84.0 90.5 78.0 | 12.5
12 729 624) 16389 .185 4 Sae a 80:6) 1 1e.0) es 6
13 .799 854 | .725| 129) 88.3 89.0 | 77.0 | 12.0
14 | Sunday.
| |
15 .707 781 598 | .183 | 86,1 92.5 | 80.2 | 123
16 -712 775 639. | 136 84.1 92.0 75.6 | 16.4
ii 754 .826 | 684 | 142 84.0 92.1 76.8 | 15.3
18 -764 823 TOL. | 122 86.4 92.4 79.6 | 12.8
19 -786 851 116 | 135 86.6 93.2 82.0 | 11.2
20 167 844 | 674 | .170 85.2 92.6 78.4 ; 14.2
21 | Sunday.,
22 -787 .831 750 .081 79.8 87.8 76.6 | 11.2
23 His 844 709 135 82.4 90.0 Tie UPS)
24 -705 -785 605 | .180 82.1 88.2 76.8 | 11.4
25 .639 692 543 149 78.8 84.6 76.8 7.8
26 .622 681 582 .099 81.1 86.3 78.0 | 8.3
27 617 .652 565 .087 82.3 88.5 79.0 9.5
28 | Sunday.
29 487 049 427 122 | 84.6 92.2 81.3 | 10.9
30 459 001 415 .086 85.1 91.5 80.6 | 10.9
31 486 .520 42 .078 83.4 87.8 $1.4 6.4
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the hourly Observations made during the day.
XXXIV Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
wn the month of May, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
. Se 2 u Fy
: 1 So Bade | 2
5 2 Ea hye 2 Roce 2s
2 Aan a ieee ke
2 5 E 7 ) Sue SS | °@s
Dateigc 2 a 5 So |S28) SE x
| @ 6 3 2 a IE E er el ea
28 2 & FS = S Cee Sse
a) = s ae Rée Sey Meow ell cst 4S
= faa} = A 2. a nts soe | ates
=i = S Gs ae me S| £26
5 & ce 5 an o> of |Sas) Sus
= a S) a) = = S =
0 O OL Pale © Iba || EG eae, |) ANE ea
1 798 5.1 | 76.2) 8.7 | 0.887 | 9.49 | 3.00 | 0.76
2 79.9 BT 75.9 5907 879 .38 38 74
3 80.4: 5.5 | 76.51 9.4 .896 BY 80 74
4 Bee et een) Gulch ee3 .973 | 10.36 .09 UG
5 81.0 6.0| 77.4] 9.6 922 | 9.81 48 74.
6 76.6 53 | 72.9 |» 9.0 HOT || BH | DSF 16
7 Sunday. ,
Sid ln 1 G8 3.5 | 73.8] 6.0 822 87 | 1.88 83
OV ities AG ava Voges .830 1925 eae 78
10 75.2 Ah 23a aeTO 783 46 13 80
aT a cou2 BES M Ai TeD pro 925 | 9.90 27 BE
a2 1) eal Zeal erp ltl Nee VO Tal esol Ad, BT)
TB eo ea | C74 Oe .830 91 -| 3.02 ie
14 | Sunday.
15 79.3 6.8 | 74.5 | 11.6 840 .96 .99 .69
16 78.8 5.3 | 95.L al 9.0 857 | 9.17 04, 5
17 79.4 46 | 762| 7.8 .887 bl | 266 78
18 | 80.4 HO WARAN) LOR 1887 AZ | 859 is
19 80.1 65 || (762 \) 10.4 .887 AT 67 72
BO 789) 1 G3 | 74.p) 1) 10-7 840 | 8.98 63 J
21 | Sunday.
22 77.0 BBN 7.0) ole geass 854 | 9.22 | 1.58 .86
23 | 4785 | 3.9] 758| 66 .876 Al | 2.20 81
24 Feo eS Ou W760 saa 882 48 .03 82
25 G68 Ve ee 7b ch oey 857 by dame ia O71 89
26 | 778 3.3( 75.5 | 5.6 868 | 85. |). 2282) 0) ane
BF 789s gael 782 hea 946 | 10.17 Ad 88
28 Sunday. | | |
29 | 81.0 26. apie 955 2.3 | 216 83
$0) 4) (80.9.4) 4:2 780 7, 0 940 .05 2 .80 :
31 | 80.8 2.6: 79.0 | 44 .970 42 | 1.54 .87 #
All the Uygrometrical elements are computed by the Greenwich Constants.
Meteorelogical Observations. XXXKV
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of May, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
i 2 wz | Range of the Barometer = 2 Range of the Temperature
=& 4 | for each hour during 2a) for each hour during
ice | = ae | the month, Po the month.
meee EE tea acl Qs
| 5 2 = N : | 4 & = " 7
33 | Max. Min. Diff. Be | Aller Min. Diff.
Ee S
| |
Inches. | Inches.| Inches. Inches.; 0 ry 0 0
Mid- ‘50.661 | 29.827 |29.465 | 0.362 | 80.6| 85.0| 768 8.2
night. } . ed aid. . a ~ . . A
1 .651 811 458 .000 80.2 85.0 75.4 9.6
2 .635 804 ANT Nor e-BS0/ 79.8 85.0 73.0 12.0
3 | .642 -806 | 463 043 796 848 73.6 11.2
4 .630 808 445 .863 79.7 83.8 hore 10.6
5 651 824 449 .o10 19.5 84.0 73.6 10.4
6 .667 .826 468 | .398 79.7 83.8 73.6 10.2
U 681 | .832 A777 .000 80.7 | 84.6 73.0 11.6
8 .693 842 AT5 | 367 82.7 87.0 74.2 12.8
9 .705 854 | 492 | .362| 84.7 | 88.8 74.3 14.5
10 702 | .831| .497 | .354| 862! 903] 76.0 14.3
11 .692 843 A482 61 87.5 92.0 77.9 14.1
eon, || G7) | 827 | .473 354 | 88.6 | 92.6 80.8 11.8
1 650 | .806 |. .445 361 | 88.7 | 93.6 77.3 16.3
2 | 625 | .784: A427 oor 88.8 94.3 77.5 16.8
3 .605 UPF/S: 418 | .895 88.5 94.8 76.4 18.4
4 587 .700 415 | .830 878 94.8 77.3 17.5
5 092 .7d9 423 2320 86.5 94.4, 78.0 16.4
6 601 De 429 B24 84.6 90.2 77.8 12.4
ent) 626 teh A46 .o20 82.7 87.9 75.6 12.3
8 645 | .773, 454 319 | 81.6 | 87.7 75.6 12.1
9 661 | .786 A69 317 81.3 86.7 76.3 10.4
Oe | 678 | |.815 486 .229 811 | 85.6 75.8 9.8
11 G74 | .824| 473 |. .351 | 80.6 | 85.0 73.0 12,0
| |
|
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
miometer Means are derived from the Observations made at the several howrs
during the month.
XXXV1 Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
inthe month of May, 1865.
Huurly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
2 ies 3 E =
S | o = o
| Ble 2
| 5 e Oy o 5
Seances S 5 6 3
Hour. | = = S a "S 3.
| 2 3 ole =e
= o by E boy eS
a a iS) A =
0 fe) fe) (0) Inches.
oni W726 | 3.0 | 755 | BA | 086s
| "7.5. | 2.9 | 75.6 AGB, || sey
2 "7.2 2.6 | 75.4 4A 865
3 77.0 2.6 | 75.2 4,4 .860
4 77.3 2.4 | 75.6 A 871
5 m73.| 22 | 75.8 3.7 876
“Suh CS: 2.4 | 756 4 871
ea Wai || 2 BE len 759 4.8 879
8 789 | 3.8 | 76.2 6.5 887
9 79.9 48 | 76.5 8.2 896
io | S04 | 58) 76:3 9.9 890
ll 80.9 | 66 | 76.9 | 10.6 908
Noon.| 812 74 | 76.8 | 11.8 .905
a7) 813 74 | 769 | 11.8 908
B94) S12 76 | 766 | 12.2 1899
3 80.9 ipa 76.3) 122 890
4 80.6 DO NH || ah G 890
5 79.9 | 66 | 75.9 | 10.6 879
654 TO |) Sa 75.9 8.7 879
q 73.4 | 43 | 75.4 73 865
8 77.6 4.0 | 74.8 6.8 849
9 77.7 3.6 | 75.2 6.1 .860
10 77.9 3.2 | 75.7 5,4, .873
Te Pacey 2.9 | 75.47 4.9 873
}
pour in a Cubic foot
Mean Weight of Vas
of air.
Troy grs.
9.37
39
315)
.30
40
46
40
AT
02
.59
.00
64
Additional Weight of
Vapour required for
complete saturation.
Troy grs.
1.64
A9
40
.o9
.o2
20
on
7
2.20
.83
3.49
85
Mean degree of Hu-
midity, complete satu-
ration being unity.
}
a
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. XXXVI
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of May, 1865.
Solar Radiation, Weather, &c.
8 |g22
-| 2s |S & 2! Prevailing direction General Aspect of the Sky.
2| #3 gee of the Wind.
Al =~ led
| © |Inches
1 125.8} 0.48 |S. (high.) -ito8 a.m. Scatd. i & -ito4pP. M.
| | overcast afterwards, Rain from 7 to 9
P. M.
2 129.0; ,.. |S. &S8. W. (high.) | Overcast to 8 a.m. i to 5 Pp. mM. Seud.
afterwards. Thin rain at 1 a. M.
3 123.0) 0.39 | 8. &S. W. (high.) | Overcast to 4 a. um. %i to 10 a. m. Seud to
2 Pp. M. Overcast afterwards. Rain be-
tween 5 &6p.mM. Thunder & lightning
| from 7 to 9 P. M.
4) 127.8| ... |S. (high) &S. HE. ito 4 a.m. Scatd. 91 & “i afterwards
lightning at 8 P. M.
5| 132.7) ... |S. &S8. W. Overcast to 9 a. mM. Scatd. "i & \-i to 5
Pp. M, overcast lightning & thunder after-
| wards. Thinrainat6a.u.&7&8P.M.
6 127.0)) .. |\S.E&S.&E. Overcast light rain at 6, 7 & 11 Pp. u. thun-
| 1,46 der at 6 & 11 p. u. lightning at 11 P. u.
74 qlee | Sunday.
8) 124.0; 0.36 |S. HE. & N. Overcast to 7 a. mM. Scatd. "i & “i to 6
Pp. M. “iafterwards. Rain from 1 to3
| Pp. M. thunder at 2 P. M.
9 125.0| 0.62 |8.&8.H.&8.W.|-i& ito5 Pp. mu. overcast afterwards.
| Rain, thunder & lightning at 8 P. M.
10; 126.0; 1.65 |S. &8. W. Overcast to 11 a. um. Scatd. 91 & “i to 6
P. M, overcast afterwards. Rain from 2
to 7 a. uM. thunder & lightning from 1 to
7 A.M.
11} 120.0] 0.97 |S. Scatd. 91 & “ito 5 Pp. M. overcast after-
wards. Rain at8 & 9p. m. thunder &
lightning from 7 to 10 P. M.
12; 121.6| 0.98 |S. H.& H. &N. W.| Overcast to 7 a. um. Seatd. oi & “i after-
wards. Rain from 2to 7 A. M. lightning
at midnight & 2 a. M. thunder at 2,6&
: 7 A.M.
13] 128.0| .,, H.& N. H. Scatd. 911 & ito 4a. mM, “i to 9 a, M.
1 to 5 Pe. M. cloudless afterwards.
12) ee ... | Sunday.
£5) 135-01 5,, S. H. &S. Cloudless to 4 A. M. “ito8 A.M. i after-
| wards,
16; 133.0| 0.71 |S. &S. HE. Scatd. 91 & “ito 6p. mM. overcast after-
wards. Rain from 6 to 8 P.M. lightning
from 8 to 10 P. M.
PA toe! 3. |S. & 8. W. Seatd. i & “i to9 a. M. Oi to4P, M.
| overcast afterwards, lightning at 9 Pp, M.
Mi Cirri, —i Strati, %i Cumuli, “i Cirro-strati, ~i Cumulo-strati, i Nimbi
Wii Cirro cumuli.
XXXViil Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
wm the month of May, 1865.
Solar Radiation, Weather, &e,
{3 Srre |
| & 3 Pe
|o8 |gacd
.| 23 |S & 8) Prevailing direction |
GS] ps laos
43| Bra |. o © of the Wind.
2 = Eat at 12 ©
18} 126.5; ... |S. &S8. W.
19) 128.0) ... |S.&S W.
20} 130.0; ... |S. &S. E.
pada ... | Sunday.
22| 116.0, 2.77 |S. & 8. H.
23| 181.0| ... |S. E.&S8. 4&5,
24| 118.0| 1.50|S.E.&8.
25) ... | 1.08 | E. & variable.
26) 121.0| 0.10 |E.&S.&8. E.
27| 130.0| 1.02 | E.&S.E. &8.
LA WR ... | Sunday.
29) 130.0] 1.81 | 8, £.& 8. & W.
30} 130.6 ere E. & variable.
oli ... | 0.54 ,8S.&H.&S. H,
|
General Aspect of the Sky.
ee a
Overcast almost all day: Lightning from
7 to 10 p. M. thunder at 8 & 9 ». mM. light
rain at 11 Pp. M.
Scatd. 91 & “i to 6 P. M. overcast after-
wards.
Overcast to 6 A. u. 11 & i afterwards.
Scatd. "1 & i whole day, Rain at 6, 8,
10 a. Mu. 2 & 3 Pp. M. thunder at 10 a. mu,
lightning at 9 P. M.
Scatd i & “ito 7 p. m. cloudless after-
wards. Thin rain between Noon & 1
P. M.
Cloudless to 8 A. mM. Scatd. \i& \-ito noon
overcast afterwards. Rain at 10 A. mM.
1,5,6,8 &9 pe. m. lightning & thunder
from 5 to 10 Pp. mM.
Overcast allday. Rain from noon to 5 P.M.
i to 5 a, M. overcast to 7 P. M. “i after-
wards, rain between 9 & 10 A. M.
Scatd. 91 & -ito7 Pp. m. cloudless after-
wards. Rain at 3 A. M. noon to 2 P. M.
Scatd. i & ito 2 P. M, overcast to 7 P. M.
cloudless afterwards. Rain atl a. mM.
& at 4,5 P.M.
Scatd. 91 & i drizzled at 3 P. M.
i to 8 a. M. overcast to 5 P. M. Scatd. 71
& —iafterwards. Rain from 10 A. m.
to 2 P. M.
Meteorological Observations. XXXIX
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of May, 1865.
Montuty Resvutrs.
Inches
Mean height of the Barometer for the month, .. oC og RGB
Max. height of the Barometer occurred at 9 a. M. on the 13th, -. 29.854
Min, height of the Barometer occurred at 4 P. M. on the 30th, «. 29.415
Extreme range of the Barometer during the month, oe «- 0.439
Mean of the Daily Max. Pressures, .. 6c ae es 29-719
Ditto ditto Min. ditto, .. A bo oe | 29:51
Mean daily range of the Barometer during the aout Ke e- 0,141
Co)
Mean Dry Bulb Thermometer for the month, .. oo oe 83.4:
Max. Temperature occurred at 3&4 P.M. onthe 5th, .. os 94.8
Min. Temperature occurred at 7 a. M. on the 10th, Be A BD
Extreme range of the Temperature during the month, ne 2 o =
= 8 ee yee 2 go |e a eee
z Pale) eo) BA ee eee
| oe E 2 68 |mepe| Css
pa E 2 3 = eee Dees | ye, =
Date. . 2 A mn 3 = a5 Sees
2h 2 co om oye =
23 2 3 So eB | © 2) eee
Soe 3 s 3 ES =O 22 ma 29
g 3 Aa ia En © =
AG on ay S Sai SiGe sn! ee =
3% S a a bay Se a8 |s ee.| Sos
= fa) os) aa) = = = =
° Oo 0) ft) Inches.| I. er. _| Der.
1 80.9 3.0] 788} 5.1 | 0.964] 1034 | 1.79 | 0.85
2 81.1 SB. ly FSONay 58 .967 87 87 185
3 82. 4.4} 80.0} 7.0 | 1.001 66 | 2.63 .80
4 | Sunday.
5 82.5 5.8 | 79.0| 9.3 | 0.970 81 | 3.49 75
6 82.6 BiB Weal jae O38 973 34 50 75
7 82.7 56] 793| 90 979 .40 .40 75
pe pe ay Bi Ne FO bul Oa .986 AT 45 75
BR. 1h 84:0 ABN BLA) 70) 047 |) asia Boyz .80
10 | 82.9 Ab \ 80.00 74 .005 | 10.69 .80 79
Bg 80.8 44) 4472) 475 | 0.916) 9.79 63 79
12 | 816 48] 782] 8.2 946 | 10.09 97 i,
13> |, B08 AO} 78.0 \ 68.) ‘940 05 AL 81
ERS ery che c AS | 48.7) 47.8 961 24 86 78
15 81.4 25 |, 4916)| 48 989 60 | 1.53 87
16 80.0 2 li Rl e.8 £946 az AT 87
ig. | 97 18) 278 4e ness 1952 25 .06 91
1s | 785 WV preg Vs oA) :931 06 | 0.66 94
19 79.3 AEN tripe Nt ATS 922 | 9.91 | 1.56 86
20 | 82.2 26 OTe ioal .992 | 10.59 | 2.24 .83
21 83. A2| 80.71 6:7 | 1.024 89 56 81
22 | 838 4.4 | 81.2] 7.0 040 | 11.05 71 .80
pa) | B45 A Ne Si Bile eS .050 13 95 79
24 | 83.2 5B1| 801] 8.2 005 | 10.67 | 3.13 Ty
25 84.4 46 | 816] 7.4 053 | 11.18 | 2.90 79
26 83.3 45] 806] 7.2 .021 | 10.86 74 80
27 83.3 5.6| 79.9! 9.0 | 0.998 59 | 3.45 75
23 | 83.1 Bi. 80.9 |. 163) W080 99 | 2.00 | .85 ;
29 | 81.8 3.4] 79.41] 58 | 0.983 AQ 12 83 :
30 | 815 | 25) 796)\ 46 989 58 | 1.66 .86 é
|
—_——_—________,
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations.
lili
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of June, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
| =; | Range of the Barometer
| =sz for each hour during
| -=— oe the month.
Hour, | 2 <0
| 3.32 |Max. | Min. | Dif,
| &
| if
Inches. | Inches.; Inches.| Inches.
Mid- =
night. 29.564 | 29.684 |29.416 | 0.268
Ei Dod .682 404 278
2 543 677 398 279
3 27 .667 391 276
4 53d .653 2099 .264
5 AZ .669 .095 L274
6 50D .689 417 272
G 072 -706 429 277
8 582 Tie AZ8 299
§ |} .b9L -740 A432 .308
10 .090 728 | .429 299
Tl 084 122 426 .296
Noon. 570 .710 .405 .308
te 502 .685 084 OL
ied Se 659 | .369 .290
3 513 698 .000 282
4 | 497 | 614| .352.| .262
5 496 .616 .366 | .200
6 508 .613 .870 .243
ts 525 .627 .380 242
8 548 | .609 | 394 .265
9 567 | .683 405 .278
10 578 .688 426 262
il 575 692 AB2 266
|
Mean Dry Bulb
Thermometer,
Range of the Temperature
for each hour during
Max.
the month.
Min.
Diff.
°
Bs OID wT
MROONBDA™ &
=
Q's
NO
11.6
| |
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the ‘Observations made at the several hours
during the month.
xliv Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of June, 1865.
Huurly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
f
| 2 3 ae: 5 23 | Sse) #2
Bool B ils BA LS och Sin | aie me
2 Ae ee & S82 | EE | Sex
oe S Bae iale 2 as | 282 | oie
Hour. | = ic A & a pce cede 2 eS pau
a | 2 3 SSS EBS) 2 e.28/sE6
ES S = 2 = Boo | Se | iseshe a epee
me 4 a As e 3 epS"a (Sus. at ees
a 3 z z SiR iee walls Gera ce S| [ss -=
oie a ee ei) 2 = Seema l= &
° fe) te) Ce) Inches. |Troy grs. Troy grs.
aa 81.6 | 2.3 | 80.0 3.9 | 1.001 ! 10.72 1.41 | 0.88
at 81.3 22 | 798 3.7 | 0.995 66 BA .89
2 81.2 | 2.0 | 79.8 3.4 | .995 69 20 .90
3 81.0 | 19 | 79.7 3.2 | .992 66 13 ‘90
4 BLO.Y\ | Lion avo 3.2 | .992 66 13 '¢ |) So
5 80.9 | 2.0 | 79.5 3.4 | .986 60 19 ‘90
6 81.1 | 1.9 | 79.8 3.2 | .995 69 13 90
" 81.2 ] 2.5 | 79.4 4.3 | .983 BA 58 87
8 81.8 310 79.5 5.6 .986 D3 2.04, ok
9 822 | 43 | 79.6 6.9 | .989 BA 56 ‘Sl
10 82.7 51 | 79.6 8.2 | .989 i) 3.08 17
11 83.1 57 | 79.7 9.1 992 58 ‘AT 75
Noon.| 83.1 67. 179.0 Ol oF, 973 30 4.12 71
1 83.5 | 68 | 79.4 | 10.9 | .983 39 2A 71
2 83.4 7.0 492, 11,2 .976 00 04 .70
3 63.4..\ Foo | 179.2) ) | 1am, .976 33 34 70
4 S84. | 650|.079.2) 4) 10.40), S76m\) ap 3.98 72
5 82.6 | 6.0 | 79.0 9.6 | .970 129 63 Th
6 82.0 533 78.8 8.5 964 125 16 76
"7 82.0 | 41 | 79.1 70 | .973 38 2.57 .80
8 81.7 | 3.5 | 79.2 6.0 | .976 AB 118 .83
9 81.7. | 3.1 | 79.5 53 | .986 (55 1.91 85
20 81.7 | 27 | 79.8 46 | .995 64 67 86
ll 81.6 | 26 | 79.8 4,4 | .995 66 58 87
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations. xly
Abstract of the Results of the Hourly Meteorological Observations
- taken at the Surveyor General's Office, Calcutta,
in the month of June, 1865.
Solar Radiation, Weather, &e.
4 {| oOo od
25 |23_
.| 2 |© = & | Prevailing direction General Aspect of the Sky.
= be = |S 2.2 of the Wind.
S |r ef
Q = > ips 189 ras)
Oo |\Inches,
1 123.0} 0.30 | EH. &S.E.&S8. Overcast nearly the whole day. Lightning
howaese S. from 7 to ll p.m. Rain at
: Tel hee
2 0.09 |S. & 8S. W. 5 oe Light rain between Noon & 1
P.M, Thunder & Lightning at abdarghe
&1A.M.2,5&8 P. mM.
Shee} 2.) |S. & SS. WwW. Overcast to é A. M, Scud afterwards.
A eas as =| Sunday.
Het 296... 8. &S. W. Cloudless to 7 A. M. i afterwards.
Gr takOy oS Sh Kito6A.M. %ito2pP. mM. ~“i& %ito7 ». uM,
Cloudless afterwards.
7| 131.0} S Cloudless to 2 a4. mM, “ito 6 A. M. i to
6 P. M. overcast afterwards.
8 1380.0 s. Scud to 9A, M. “ito 5 P.M. Scud after-
wards,
9| 124.2) .., Ss. Seud to 2 A.M. overcast to8 A.M, 71 &
—i afterwards.
i 0) ie B70 S. &S8. E. | Overcast to 3.4, Mu. 91 & ito 1 P. M. overs
cast afterwards. Thin rain at 1 A. uM.
55) See Pree S.8.&H.&8. Overcast. Drizzled at 1 a. mu.
12) 134.0; 0.91 | S.W. & H. Light clouds to6 a.uM.“-i& %ito4 Pp, mM.
overcast afterwards. Rain at 6,8 & 9
P.M. Thunder at 6 Pp. mu.
13] 129.6| 0.10 |S.W.&N.& W. Overcast to8 A. M. 91 & “i to 6 P. M.
Overcast afterwards, light rain from 7 to
10 Pp. M.
Ae Se Wao GS. Wis, Light clouds to 2 4. M. “-itoll a. mM, ni
& \—i afterwards.
15) aes 0.53 |S. &8. W. ito 3 A. M. overcast afterwards. Rain
| at 6 & 7 A. M. noon, 3 & 4 P.M.
BG)... 1.16 |W. &S. W. Overcast. Rain from 1 to3 A.M. light
: rain at 1 pv. mM. & from 7 to 10 P. M.
17 0.14 |W. & S58. W. Overcast. Light rain after intervals.
» is| ... |*262|W.&S.W. . Overcast. Rain whole day. Lightning at
; 10 P. M.
mag) ... |4126 |S. W.&s. Overcast, Light rain from Midnight to
A.M. :
20) 129.0) 0.41 |S. &S. W. Overcast to 7 a. mM. iG “-itoll a, uw, “i
& Oi afterwards. Rainatl & 4 a. um.
& at 5 P. M.
Ni Cirri, —i Strati, \i Cumuli, i Cirro-strati, ~i Cumulo-strati, -i Nimbi,
“ni Cirro cumuli.
* Fell from 9 p. M. of the 17th to Noon of the 18th,
+ Fell from 1 vp. m. of the 18th to 7 a. m. of the 19th,
xlvi Meteorological Observitions.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of June, 1865.
Solar Radiation, Weather, &c,
be 2
| 28 [os S 5 Prevailing direction
2S) es 18 30 of the Wind.
SB) Sea fate
Q = m foe! In ©
fe) Inches
21) 137.5 s.
22) 130.2 Ss
25) 133-0) Gens
24; 188.0} 0.12 |S
25| 128.0] ... s.
26| 127.0| ... 8S. &S8. H.
IW MOTO) | eiices S.E. & E.
sliniees oe EK. & 8. & variable.
29| 120.8] 0.28 | E.& N. E.
30| ... | 0.71 |S.H.&N.E. & E.
General Aspect of the Sky.
Light clouds to 8 4. M,. “ito 4P. M, “ito
7 p. m. cloudless afterwards.
Cloudless to 4 A. M. i afterwards.
ito 4a,.™M.; light clouds to noon, i
afterwards.
Overcast to 10 a.m. Mi & “i to 4P. uM. Yi
& Oi afterwards. Rain at6&7 a. mu.
Lightning towards W. at midnight.
Cloudless to 5 A. M. %i to 8 P. M. overcast
to 8 Pp. M. 91 & ~i afterwards.
-id&é %ito3P. M. overcast afterwards ;
Lightning towards 8. at 8p. mu. Light
rain at 9 P. M,
i & \-ito 8 a. M. Mito 7 P. m. cloudless
afterwards.
Cloudless to 3 A. M. overcast to 3 P. M. Mi
& i afterwards: Light rain from noon
to 3 P, M.
“i & ito 8 A. M. overcast to6 P. M. Oi
& -iafterwards. Rain at 3 P.M.
Overcast. Rain after intervals from noon
to 1l Pp. M.
Meteorological Observations. xl vii
Abstract of the Kesults of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of June, 1865.
Montuty Resvuprts.
Inches
Mean height of the Barometer for the month, .. ee -. 29,550
Max. height of the Barometer occurred at 9 A. M. on the 7th, ». 29.740
Min. height of the Barometer occurred at 4 Pp. M. on the 80th, e- 29,352
Extreme range of the Barometer during the month, i na 0.388
Mean of the Daily Max. Pressures,.. ee ee 2. 29.607
Ditto ditto Min. ditto, .. ate ate ee 29.489
Mean daily range of the Barometer during the month, .,. se) OnkES
fo)
Mean Dry Bulb Thermometer for the month, .. ae ee 86.1
Max. Temperature occurred at 4, P. M. on the 24th, ee as 96.0
~ Min. Temperature occurred at 5 A. M. on the 19th, an ee mn AO)
Lixtreme range of the Temperature during the month, oe oe 19.0
Mean of the daily Max. Temperature, $3 sie 60 91.3
Ditto ditto Min. ditto, .. D6 oe ae 82.2
Mean daily range of the Temperature during the month, ., He 9.1
Mean Wet Bulb Thermometer for the month, .. BE ar 82.1
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 4.0
Computed Mean Dew-point for the month, .. O6 AG 79.3
Mean Dry Bulb Thermometer above computed Mean Dew-point, AR 6.8
Inches
Mean Elastic force of Vapour for the month, .. ds ee 60.979
Troy grains
Mean Weight of Vapour for the month, ae ae ut 10.44
Additional Weight of Vapour required for complete saturation, Ae 2.51
Mean degree of humidity for the month, complete saturation being unity, 0.81
, Inches
Rained 17 days, Max. fall of rain during 24 hours, ae Se 2.62
Total amount of rain during the month, a ae aa 8.63
Prevailing direction of the Wind, ., oe oe S.&S. W.
are
xlvili Heteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of June, 1865.
Monruny RErsvnts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour, | ;
3 2 S iS 8 sl] Vsti is e|_:
of .|o (o) ° ° of Ofs|Oof .lols
sia) £\a)e] | S|F |S el siais|2
N.S} |] EB. |e [oi (ch |S.)c8 fos |e IE ee te es dS |S lS
No.of days
Midnight. 1) 1 il 4 #3! 2) 1) & 1
] “A: faa 1] | 4 } 4) 2) 2) a
2 1) | 1 fi] alee f 3| 1) 3] 2)
3 1 Ble 2] 1) 2) 2 6
4 1 3) 42 f 2) 1) 4) 7
5 1] 12 4, f 3] 1) 4) 2
6 i) | 1 3| 1) 3 3) 1) 2) 1] 1/7
7 1 Bld HG) 2) 5] 2] 2) 1
8 3 eae 16) | 6) 1] 1
9 1] | 1 3, 1 PES ea ih
10 se fib) 4) 12 A 4) 1) 4) 1) 1
11 B 12 3} 42 6] 1) 1] 1) 1
Noon. i 2\ 1 A) 2) 2) {12 Dl ine
1 Lf ect 2| { 8] 2113] 15] 2f 2] | ald
2 2| 3} 1| 4) 1110) | 5) 1) 4) a
3 1) 1 5) 2) 2) Sito) 4) Gee) at
A, 5 2| 913) 1) 6) Ly 3) 1
5 2 3) 138) fla) 2 7) 2h d
6 1 4| | 2) |15) | 5) 1f 2) 1
7 1 8] | 4) 1)16) | 4) 2 Hl
8 1 A) 1518) 1) 4) 2) 1) 1 1
) 1] | 3] 1,19] 2) 4) 37 1/1 1
10 1) | 3] {18} | 5} 8b a} 1 1
a4: i 5) 1417] 1} 3) 2) 1 1 ib
- —$<—<—<—<—— ee ee
Meteorological Observations. xlix
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of July, 1865.
Latitude 22° 3371” North. Longitude 88° 20’ 34” East.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in,
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
= 3 e Range of the Barometer a S |Range of the Tempera-
m5 5 during the day, D2 ture during the day.
i ae = ~
Date. = A x i A ;
| 224 | Max. | Min. | Dif. | $4 | Max. | Min. | Dif.
= A
| Inches. | Inches. | Inches. | Inches. oO o 0 0
1 | 29.523 | 29.584 | 29.465 0.119 84.3 88.6 80.8 7.8
2 | 090 | -090 A87 103 85.2 90.8 81.7 9.1
3 048 | 596 ATT 119 85.5 92.6 82.0 | 10.6
4 494 073 ALT 156 85.0 89.5 82.0 7.5
5 445 484 381 103 84.6 88.5 SIA ek
6 455 .490 410 .080 | 84.6 88.3 8G | 637
7 440 484, 380 | 104 | 83.7 86.9 81.6 5.3
8 434 483 .398 | 095 83.4: 88.0 80.2 7.8
9 457 .506 ALL 095 84.2 89.0 81.0 8.0
10 AQ 047 | 456 | 091 85.4 | 91.4 81.6 9.8
1 539| 605| .482| .123| 838 | 90.1 | 78.0 | 12.1
12 022 577 444 | 133 81.4 85.0 78.4 6.6
: 13 512 | .553 465 | 088 84.2 91.2 | 81.4] 9.8
14 537 092 | 483 109 84.8 90.6 79.0 | 11.6
15 58d | 087 | 482 | 105 82.6 85.6 79.6 6.0
16 2024 562 | A486 | .076 825 87.1 UD 7.9
17 536 587 495 092 82.7 85.6 80.0 5.6
18 598 097 003 094 84,2 87.4 81.8 5.6
13 540 585 | 479 -106 85.4 90.5 81.4 2B
20 .082 631 2036 .095 85.2 88.6 82.6 6.0
21 598 .656 007 ALY, 85 3 88.9 82.9 6.0
22 604 655 2007 .098 85.7 90.8 82.5 8.5
23 .640 .699 085 114 85.2 89.6 80.2 9.4)
24 687 739 .628 eat 83.5 89.0 79.8 9.2
25 -725 717A 566 108 81.7 83.8 80 2 3.6
26 “719 Pee 678 094: 83.4 88 4 79.5 8.9
27 708 158 659 .099 83.2 87.7 79.8 1.9
28 “749 803 .700 1038 83.3 87.6 79.4 8.2
29 £759 198 707 O91 82.1 85.2 78.5 6.7
30 714 AT2 646 126 $2.0 88.4 77.4 | 11.0
31 678 726 601 125 82.6 88.6 78.8 9.8
|
| |
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
_ mometer Means are derived from the hourly Observations made during the day,
1 Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
an the month of July, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
‘ : E S SeaeeG sh | 4s
B S| eee | ee) ee
5 2 © B > So | 2 oe eis
= © 5 ma % 6 fa2/ 8624
s > i= Q o°o os os
| ° o 3 a on Be Sl ay Te
Date.| 7 2 A 3 ye (Ss ee sg S
| 38 iB 3 = @| 5S |S Sieulpeetiens
| B® 3 s ae | S| 6 o> ean cee
ives pa Bs 5 | gs | e¢% |2238| Bs
3 & Pe g PAY oe of |S ae| aos
= a 3) Qa a Pushes =
| o ) o 7) Ibnelnesy, | ME, re, |) ALL ete. .
1 81.4 2.9 79.A, 4.9 0.983 | 10.51 Wee 0.86
2 81.9 3.3 79.6 5.6 .989 .06 2.05 84
3 82.1 3.4) 797 5.8 .992 09 13 83
4 B98 in pS Lil ee Ol Tale 1:8 .992 {6 )\| mag? 85
5 81.8 | 28] 798) 4.8 .995 64 75 86
6 Si4y Me 8 2iloe VO 2uli 34 976 A5 94 84
7 | 80.7 B:0n | 78.Gnln ol .958 .28 79 85
8 80.1 3.3 77.8 5.6 934 OL 95 84
Ot lee 79.8 4.4) 76.7 7.5 902 9.64 2.60 79
10 BLO. gi) Vado ies TON 7-5 .937 | 10.00 68 79
A) HeeOOi: AN) PS Sales ZS: ule ONG .946 13 | 1.97 84
12 79.5 19) | ZS 2a (302 946 19 .08 .90
13 BLS) ae 2:9) 79. 3uly 9 979 A8 76 86
14 BLS) Gt) 8 ulin 7SiSwiy 6:0 964 31) ||P 205 83
25 Ho vS04) We 2.2c le, 78.900 8,7 967 39 | 129 .89
16 79.9 26] 781) 4.4 943 14 .50 87
a7 79.9 28| 77.9| 48 937 .06 .66 .86
18 81.4 2.8 79.4 4.8 983 ol 73 .86
19 81.3 4.1 | 784) - 7.0 1952 7 alee .80
20 81.8 3.4] 794] 5.8 .983 AQ 12 83
74 Ie 81.8 3.5 79.3 6.0 719 AG 18 .83
22 81.5 WF as) (3) |: siren 958 28 57 .80
23 81.1 41} 78.2) 7.0 .946 ailil 50 .80
24, 80.8 2.7 78.9 4.6 967 Ol 1.63 .86
25 79.7 20) a 783al) 34 .949 122 “Ls 90
26 80.7 27| 788] 4.6 964) 134 .62 87
27 80.4 2.8 | 784] 4.8 952 21 68 .86
28 80.7 2.6 | 78.9 | 4.4 .967 39 54 87
29 79.6 23 Ne Ti Sialay Ae ie OBA .05 AG 87
30 79.6 DA Noo TON Ant .937 .08 39 88
3 TN Pes) | TNT 4.9 931 .00 .68 86
|
ll
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations. li
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of July, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
S Pe a | Range of the Barometer = o Range of the Temperature
Sas = for each hour during ea) & for each hour during
H ee the month. bs the month.
ao? 3 r Sees 5 P
$4 | Max. Min. Diff, Se || Wiley Min. Diff.
| =|
Inches. | Inches.} Inches., Inches, Co) 0 tv) C1)
* Mid- (99.587 | 29.778 | 29.432 82.1
night. | 72° 29.7 29.432 | 0.346 2. 84,0 77.4 6.6
1 BYE! .761 AQZ1 .340 82.0 83.8 77.9 5.9
2 563 756 .410 846 81.9 83.8 77.8 6.0
3 504 737 .395 042 81.7 83.4 77.8 5.6
4 564 -740 .393 AT 81.6 83.5 478 5.7
5 561 752 .388 364 81.5 83.4 77.9 5.5
6 yi! -765 409 .300 81.6 83.0 78.0 5.0
Z) BL shld A221 1806 82.2 84.0 79.2 4.8
8 604 .790 438 1352 83.6 85.4 80.2 5.2
9 .615 .803 476 827 84.7 87.5 81.8 5.7
10 .615 .803 469 84 85.8 88.9 81.9 7.0
11 .608 198 457 AL 86.5 90.4: 80.8 9.6
Noon .595 788 A44 844 86.8 91.4 82.2 9.2
1 .576 .768 431 BON. 87.4 92.6 82.6 10.0
2 .008 Mesill 413 824 87.2 91.4 83.2 8.2
3 se fh 29 .380 349 87.1 91.2 83.1 8.1
4 825 711 381 .300 86.2 90.0 81.4 8.6
5 p27 -708 ool 327 85.8 89.4 80.2 9.2
6 535 739 384 .000 84.4 87.6 79.4 8.2
7 553 753 | A414 8389 | 83.2 | 86.4 79.8 6.6
8 DEL Ts | AZL 340 82.9 85.8 | 79.4 6.4
9 3594 | .789 445 044 82.4 84.8 78.6 6.2
10 .606 193 458 .3839 82.3 84.6 78.0 6.6
il .606 784: 468 O16 82.2 84.4 78.1 6.3
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several howrs
daring the month.
li Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of July, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
ics 2 3 B S 46 $5 6 | ale
3 5 3 fa S = ese |Fes
Sy ole e| o|, Saolh Sek sae
se) 8 Sha ine E 22 | ee eee
Hour. | FS ce a 3 ‘wal 6 “ap O ome mg 2
E = 3 SS sulle 2 @.8|/ 333
| &°o 3S =} a4 Fo Sehpeee sy | a 28
[Pee iia a |e] «= 2 | Soe | Ea
[ee i) ao Ss sa moog o£ 5
| 23 2 E pou | S> | Sou | B85 | Sas
eres A 3S A = Sete ieee as
o 0 0 0 Inches. |'Troy grs.|Troy grs.
Mic | s01 | 20 | 7e7 | 84 | 0.961 | 1085 | 116 | 090
"h?| 80.055) 2.0 FS878.6 3.4 | .958 182 We .90
2 \ 79.9 2.0 78.5 3.4, .955 29 15 -90
3 79.7 2.0 78.3 3.4 949 22 15 .90
4 79.6 | 2.0 | 78.2 3.4 946 19 15 .90
5 79.6 19 | 78.3 3.2 949 22 .09 .90
6 Wo V 1.921) 97814 3.2 0952 125 .09 .90
” 80.1 21 | 78.6 3.6 958 .30 24 189
8 BOG 2.8 alee 7 518 4,8 964 184 69 86
9 81.2 B50 1007817 6.0 .961 29 2.13 83
10 81.6 Ae P78h7 rial 961 .26 57 .80
age) BUS 4.6 | 79.1 74 973 38 72 79
Noon. 82.0 4.8 79.1 7.7 973 .36 .85 .78
1 82.5 4.9 | 79.6 7.8 .989 52 93 78
2 82.4 48 | 79.5 Weil .986 49 .88 79
3 82.4 4.7 | 79.6 7.5 .989 52 81 a)
4 82.0 42 | 79.1 7.1 973 .38 61 .80
5 Ly) 41 | 78.8 7.0 964 .29 4° | 80
6 80.9 3.5 | 78.4 6.0 952 19 12 83
7 80.4 2.8 | 78.4 4.8 1952 pall 1.68 .86
8 | 80.3 2.6 | 78.5 4A 955 Bil 52 87
9 80,1 BB ViiN78.5 3.9 955 A] 134 .89
10 80.1 PN ME all -958 .30 .28 89
11 80.1 21 | 78.6 3.6 .958 .30 24 .89
}
All tle Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. hi
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of July, 1865.
Solar Radiation, Weather, &c.
Be leo &
fae, | se
j Sika = 7: : :
-| “= | & 2 Prevailing direction General Aspect of the Sky.
S| #2 (s3e f the Wind
$\ ss /38 S| of the Wind.
Ala” ipso
a ss fs es eS SS
E. 1 & i. Rain after intervals.
H. & 8. o1& i. Rain at 1 A. uM. noon 4, 6 &
Ss
H
Ne
i
bo
=
oe
oS
i
w
8 P. M.
wilde i& i. Rainat2 &4 p.m.
4 Overeast to 10 A. M. Siafterwards. Thin
rain after intervals.
Overcast to 3 Pp. M, i afterwards. Rain
occasionally,
Scud from 8. to 5 a.m. Overcast tol
Pp, M. 1 & “iafterwards. Thin rain
at 6 A. M. & noon.
Metres 10:25. |S ei & -itoll a.m. “~ito5p.u,i& ri
afterwards. Thin rain at 5 a, um. from
noon to3 Pp. M. & at 11 P. mu,
ae, S. VWitolla.m.%ito7 p.m. “-iafterwards.
Light rain from 6 to 8 A. M.
SED Giles Ss. VWito 4p. uM. “iafterwards. Thin rain
| at 10 a.u, & 4 P. mw.
10} 127.5; 0.18 |S. &S. W. Mito7 a. mu. “i & 71to4 p.m. WWiafter-
wards. Rain from 7 to 9 Pp. Mm.
a 1 eager S.&S. W. ito 6 A.M. —i & oi to noon: “i to 7
P.M. Overcast afterwards. Rain be-
| paee* tween 1 &2p.mM. & from 4to1l1 Pp. m.
Lightning towards W, at 11. p. u.
11 eee J iS. & S. EH. \-i nearly the whole day. Rain after
intervals. Lightning towards W. at
| midnicht,
| 114.0] 0.57 |S. ni& -ito2p.M. V-iafterwards, Rain
from 3 to 6 P.M,
14) 119.0| 2.79 | 8. ni& “ito 9 a.m, ito 7p. M.\~iafter-
wards. Rain from 6 to 9 P. M.
ES ene 0.35 |S. & 5S. W. Overcast nearly the whole day. Rain from
: 5 to 8 A. M.
Lig | ee 0.31 |S. Overcast nearly the whole day, Rain after
: intervals.
| or 0.11 |S.H.&S§. Overcast nearly the whole day. Thin rain
at 8 a. mM. & from 10 to 1 P. mM.
TSE ELAS | S. H. Overcast to 5 A.M. 11 & “i to 6 P.M.
Cloudless afterwards. Light rain at
midnight, 1 & 9 a. M.
Mi Cirri, —i Strati, %i Cumuli, i Cirro-strati, ~i Cumulo-strati, i Nimbi,
‘ni Cirro cumuli.
* Well on the 11th & 12th,
liv
Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
| Date.
Bg [Be
oo aed
ws |5'S 3
i374 |g oO =
a's fase
Sx lpg 1 ©
o |Inches
TAAL] — 553
115.0) 0.33
121.5) 0.39
iby cy ees
124.4) 0.15
119.0} 0.52
5 Jl 0:15
130.1| 0.53
121.0 |
112.6| 0.25
in the month of July, 1865.
Solar Radiation, Weather, &e,
Prevailing direction General Aspect of the Sky.
of the Wind.
S. &S. H. Cloudless to 5 A. mu. 91 & Ni to 3 P, M. WE
| to 7 P.M, cloudless afterwards.
S.&S. H. Cloudless to 4.4. mM. “i & Ni to7 A. M. Wi
to2p.M.—i& i afterwards Rain at
lla.u.1&7 Pv. uM.
S. &S. EH, \i & “ito 9 a.m. 91 & Seud. from § to 4
P.M. Overcast to8 Pp. M. cloudless after-
wards. Rain at 5 P. M.
Ss. Cloudless to 44. M. 91 & “i to 7 Pp. wu.
Overcast afterwards.
Ss. Overcast to 5 aA. M. 91 & Seud from S. to
5». uM. “iafterwards. Thin rain be-
tween 7 &8 a.m. Gat9 &10P. mu,
|S. Wito2 a.m. \i& Scud from 8. to 10
A.M. Overcast afterwards. Rain be-
tween noon &1 Pp. um. & from 4 to 11 P. uM.
Ss. Overcast. Rainfrom7 to 11 a.m. & from
3 to ll P.M.
8. Overcast nearly the whole day. Rain at
midnight & 1 & 10 a.m. & from 5 to 9
P. M.
s. Overcast to2 P.M. 91 & “i afterwards.
Light rain from 7 to 10 a. u. & between
6&7 P.M.
Ss. Overcast to 9 A, M. 9ito5 P.M. Overcast
afterwards, Light rain at 4, 6, 7 A. M.
4p. mM. & from 6 to 10 P. M.
-» 124 01| Ss. Overcast, drizzled after intervals,
TUS) ped 8. & W. Overcast to8 A.M. V-iafterwards. Light
| rain from midnight to3 A.M. &at3&
6 P.M. ‘
en 8. & W. Overcast nearly the whole day, Lightning
& Thunder from5to9Pp.M. Rain from
2 to 11 P. M,
* Well on the 29th & 30th,
Meteorological Observations. ly
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of July, 1865.
Montutny ReEsvrts.
Inches
Mean height of the Barometer for the month, .. ee oo PREETI
Max. height of the Barometer occurred at 9 & 10 A. M.on the 28th, .. 29.803
Min. height of the Barometer occurred at 3 p. M. on the 7th, e- 29.380
Extreme range of the Barometer during the month, oc ee 0.423
Mean of the Daily Max. Pressures,.. O0 oo e. 29.625
Ditto ditto Min. ditto, .. cc se co | ZRLELS
Mean daily range of the Barometer during the month, .. e» 0.106
0
Mean Dry Bulb Thermometer for the month, .. 0 GO 83.9
Max. Temperature occurred at 1 P. mM. on the 8rd, oe ee 92.6
Min. Temperature occurred at Midnight on the 30th, G0 OG. 77 A,
Extreme range of the Temperature during the month, 50 ey 15.0
Mean of the daily Max. Temperature, 00 ate Se 88.5
Ditto ditto Min. ditto, .. 50 a 50 80.5
Mean daily range of the Temperature during the month,.. ee 8.0
Mean Wet Bulb Thermometer for the month, .. oye Ad 80.8
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 3.1
Computed Mean Dew-point for the month, .. OC Sei 78.6
Mean Dry Bulb Thermometer above computed Mean Dew-point, Ae 5.3
Inches
Mean Elastic force of Vapour for the month, .. be a 0.958
Troy grains
Mean Weight of Vapour for the month, oe ae vA 10.28
Additional Weight of Vapour required for complete saturation, Ae 1,85
Mean degree of humidity for the month, complete saturation being unity, 0.85
Inches
Rained 29 days, Max. fall of rain during 24 hours, ac ae 279
Total amount of rain during the month, re mit ane TOE
Prevailing direction of the Wind, .. oo oe 8. &S8. EB,
lyi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of July, 1865.
Monruny REsvtts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
|
Hour. h
S| .|6 SHS WES es els cols. =
alae elale| |slels] .|siBlsisia|2
|
No.of days.
Midnight. 1 1) | 5) faz) 4) al a
1 1 1] 1| 7| 2]20] 3) 2| 1
2 1 1} | 6 1421) 11 1
3 1 7 [21 1 i) aL
4 1| | 6 118] 21 5
5 1 8) 1/21) 21 1) 1
6 1 Q| | 4) }22) 3] 21 1
7 2 1] | 7 |19] 4) 2) 1
8 2) 1 8) 1117] 5) 3) 1141
9 2 6 1/20) 41 2) [4
10 2) 1 6 2)20| 3] 2| Ja
iat 2 6| 2118] 3) 4) 1) 1
Noon. 2) 1 1) 1) 7) 120] 5} 1
1 | 1) 0) 4) Gi il2a| sha
2 2) 14 2) 1| 5] 1/20) 2} 2] 1
3 hen ie 1| | 5| 2/21) 6} 2
4 ea 2| 1] 6] 1}20} 6} 1
5 1 1| | 7| 2:22] 7
6 1 2| 1] 6| 1/18] 6) 1 3| 3
7 1 1| | 4) |20] 8{ 3] 2f 2| 2
8 it 1| | 3] {23/7 3/3
9 1 1| 1) 6| 2119] 5! 2] 2f 2) 2
10 1 1] | 7] 29] 511) | 2) 2
11 2 5} 3/21| 3) 2) 1) 2] 1
|
|
|
Meteorological Observations. Ivii
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of August, 1865.
Latitude 22° 33’1” North. Longitude 88° 20’ 34” East.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in.
Daily Means, &c. of the Observations and of the Hygrometrical elements
os.
hes eo
23
| 3 se
; Son
Date. ee <3
ors
=
| Inches.
1 | 29.647 |
2 | 689 |
2. ey 2
4 .701
5 -700
6 .688
7 AAD
8 .700
9 665
10 646
iat .678
12 .718
13 .719
14 .675
15 .666
16 724
17 .733
18 .638
19 008
20 488
21 419
22 AAS
23 .068
24 ' 584
25 .568
26 om
27 470
28 439
29 634
30 .624
31 59L
Range of the Barometer
during the day.
dependent thereon.
Max.
Inches.
29.705
-766
chi
761
wf45
.746
164
£767
125
.692
122
.770
°762
2127
ay
coz!
779
724,
.606
.539
494.
.Dd3
622
.636
.608
p93
p40
O91
.685
690
640 |
Min.
) Inches.
29.577
627
.640
.629
631
617
.656
.613
.590
587
.635
.656
654
20998
.610
.678
672
447
400
.330
11
009
AGS
.080
ll
| 2083
548
2002
2
048 |
388 |
p24.
aS
5 3 Range of the Tempera-
>= ture during the day.
a:
eae
Diff. Sie Max. | Min. | Diff.
a
Inches. (0) 0 0
0.128 83.0 87.2 79.8 |
2139 81.3 84.9
alg3 83.3 89.4: 79.7 |
132 $4.6 89.4: 80.8 |
114 86.0 92.6 81.4. |
129 84.6 89.0 §2.0
108 | 84.5 89.0 80.0 |
lad 85.8 90.8 82.0
ao) 85.5 90.2 81.7
2100 86.6 91.5 82.4
.087 85.4 90.6 826
114 86.3 92.2 81.8
108 | 86.1 92.1 82.4
134 : ,
142 85.4, 90.8 81.6
.093 83.4 89.0 80.8
107 83 8 87.9 80.6
181 84.5 92.1
| 159
139
164: 83.3 87.0 80.8
165 82.6 86 2 80.2
098 84.4: 91.0 80.4:
125 85.1 90.8 81.0
103 84.0 89.2 81.6
~J
~T
to
cos1I STO
ry
.
ABROWENTAOWNNENTEROHPUMAOCONANYVE
(0.2)
ie
Lo
—
—
NAA HACIA ACOOIWNOODS HOH DO IE
125 85.4: 92.6 81.6 | 11.0
.160 84.7 89.8 $2.2 | 6
-280 81.2 84.4 79.0 4
102 82.5 85.5 80.2 3
142 | 85.1 | 90.0 81.2 8.8
108 | 895.6 90,6 81.4 92
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Thers
mometer Meaus are derived from the hourly Observations made during the day.
Vill Ifeteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta, —
in the month of August, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—(Continued.)
* : E S BR log = 6
2 3 = a 2 SSS) )| = 2
= mas oO oo) Satis ei =,
= Ee 2 5 po (2s —e)/ ae
| = © 6 “A ee cee Se | Se
la! Sees 3 E a © ae 28'S = ¥ © 3
ato de a = a i 6 rs 2 = “Sieo| to veten
es 2 3 a S| Se) 53 |S eee
a = = eu | 6 | Bo peee ogee
Fl o - oy iS r= os a 8 ae SB rs) S re a
$8 Pp a PAY Se Iams eure |) ce =
= Qa S) Q a = S =
o to) o o Inches: | @. gr. || O gn.
A 80.8 2.2) 79:3) 93.7 || 0:979.| 10.51. |e oss
2 79.2 2. TT 3.6 931 02 DP .89
3 80.2 Sl e780) ih wei 940 .09 84 85
4 81.1 SES WEN! AO .958 26 o2aK8 83
5 82.0 4.0 | +792) 6.8 976 Al 50 81
6 81.5 S1 WO ine be 979 48 | 1.91 85
7 80.9 SG a wero peu 952 19 |) 256 .83
8 81.3 ASA ae Mee Tr 943 .06 dig 78
9 81.8 3.7| 79.2) 6.3 .976 A8 .29 82
10 | 82.0 46 | 792) 47.4 .976 Al 73 79
11 | 82.0 3.4| 79.6] 5.8 .989 56 aD .83
12k BUS ASD eS. O alee ai, 2958 21 81 78
13 82.0 Zell EN EO 973 38 BT .80
14. 81.7 42 | 788) 71 964 29 58 .80
16 | 813 4.1] 78.4) .'7.0 952 a7 51 .80
16 80.7 227s 2718.8) ay AiG 964 384 | 162 87
17 80.8 3:0n| wufeenal wall .961 81 79-| 85
18 81.3 B25 FOU Mayo .973 42 93 84
19 81.9 29 | 79.9 | 4,9 .998 67 79 .86
20 81.7 3.4 | 79.3 | 58 979 AG. | 2a 83
21 80.7 26] 789 | 4,4 967 39 | 1.54 87
22 80.7 1.9) 79.4932 .983 56 ae .90
23 81.4 04\ uf 3 Heeoel 979 A8 83 85
24. 82.0 Api ieee AEB) 2995 64 93. | .85
25 81.7 PHEW \ewerelobil te YS). dk aL Gro} 15 AQ 88
26 81.8 3.6 | 79,3 | 6.1 | 0.979 AG) | zeae 83
27 81.5 2M 79.3 uma 979 A8 | 1.94 84
28 79.5 U7) aS 8 ee .949 22 | 0,99 91
29 80.5 ZO 791 | 34 978 AT Ne Glee .90
30 81.7 34 | 79.3) 5.8 979 sAG Banal 83
21 81.5 Aan 78 Cale 720 958 .26 58 .80
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. lix
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Ouleutta,
in the month of August, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
r S | Range of the Barometer = 3 Range of the Temperature
= aS for each hour during fafa) Ss for each hour during
Hour = £ ol the month. ca) the month.
=o) at aS ena
so? z : si 2
S22 | Max. Min. Diff, Be |) Wiles Min. Diff.
= asi =
Inches. | Inches.; Inches.| Inches. Oo) 0 o 0
Mid- |, ee :
night. 29.646 ' 29.764 {29.396 | 0.368 82.6 84.8 49.8 5.0
1 .633 758 319 see) 82.4 84.6 80.2 4.4,
2 .620 744, eS iul! A433 82.1 84.4 80.2 AZ,
3 611 734 .016 418 81.8 84.1 80.2 3.9
4, 607 734 .325 409 81.6 84.2 79.4 4.8
5 .615 146 1334 412 81.3 82.8 78.3 4.5
6 630 .756 AT A409 813 82.8 77.6 5.2
% .646 -765 1009 406 82.1 83.8 172 6.6
8 .660 -767 405 .062 83.6 85.8 77.6 8.2
9 .668 BACALL 431 046 85.1 87.6 78.0 9.6
10 .668 776 AAZ Pao) 86.4 89.2 78.6 10.6
ET 661 779 A439 040 87.6 90.6 79.4 11.2
Noon. 642 J735D 417 .208 88.4 91.4 80.6 10.8
1 .620 J734 402 302 88.5 91.6 81,2 10,4
2 595 .710 -360 .850 | . 88.3 92.2 81.4 10.8
3 576 .698 344 1304 87.7 92.6 82.6 10.0
4 .063 .686 «2393 .8090 87.1 91.4 82.8 8.6
5 063 691 ,830 261 86.3 90.4 82.8 7.6
6 LOWE 697 eal .366 85.3 88.2 83.0 5.2
7 .590 .716 .oD9 .863 84.5 86.8 81.6 5.2
8 617 736 | 2379 Sea 7/ 84.1 86.4 81.9 4.5
9 640 755 409 046 83.8 85.6 81.1 4.5
10 604 -766 | 424 342 83.4 85.0 80.7 4.3
il .658 - 771 A416 1305) 83.0 84.8 81.0 3.8
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several hours
during the month.
Ix Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of August, 1865.
Huurly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
2 3 3 E = Ze S.5 eae
| @ =e 3 /é 2 Pace oe | Has
| e | @ |e) S$. | 32 (Seger
fy Bptes i) 5 io) ° »'s OFSes yeas
Hour. | = S 3 a r ee a0 a 3% Se 2
3 2 3 & . Se os aoe cas
i) 3 = Be Flo ea. ae = a2
ga | a B |me| «= | eee | 282] Ba
s 5 p g pu | SE | $30 | 528 | sae
= A Ss) A = SESS | ates as
|
0 0 0 0 Inches. |Troy grs.|Troy grs.
ae 80.8 | 1.8 | 79.5 3.1 | 0.986 | 10.60 1.08 | 0.91
1 80.8 1.6 | 79.7 2.7 992 | .66 0.95 92
2 80.6 15) 7915 2.6 .986 .60 91 92
8 80.4 1.4 | 79.4 2.4 .983 .58 82 .93
ae | RDS 130 zo 2.2 .983 58 16 .93
5 80.0 Sh |e 7 9E: 2.2 973 49 nD 93
6 80.0 11-33 79,1 DR?, 973 49 15 93
7 80.5 16 | 79.4 Df .983 56 .95 92
8 81.1 25 | 79.3 4.3 979 51 1.52 87
9 81.6 3.5 | 79.1 6.0 .973 .40 2,17 83
10 81,8 46 | 78.6 7.8 958 21 85 78
ll 82.3 5.3 | 79,1 8.5 973 34 3.18 77
Noon 82.4, 6.0 | 78.8 |.9.6 964 23 61 74
1 82,5 6.0 | 78.9 9.6 967 .26 62 74
2 82.4 5.9 | 78.9 9.4 .967 28 52 75
3 82.2 5.5 | 78,9 8.8 967 28 28 .76
4 82.0 | 5.1 | 78.9 8.2 967 30 03 7
By 1 BLY 4) Ali 78.5 7.8 955 18 2.84 78
eh] Bie 3.9 78.7 6.6 961 26 38 gi
y | 81.2 2.3 | 78.9 5.6 967 34 01 84
g | 81.2 2.9 | 79.2 4.9 976 5 1.76 86
94 81.1 27 | 79.2 4.6 976 AS 65 86
10 81.0 2.4 | 79.3 41 979 51 AD .88
11 81.0 2.0 | 79.6 3.4 .989 63 19 90
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. Ixi
dbstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of August, 1865.
Solar Radiation, Weather, &c.
————— |
Pas Se
So | 2 O:
Seaete te S|
-| 2s © & Prevailing direction General Aspect of the Sky.
= ge: 8 2 2| of the Wind.
Q S = to 10
|
131.7| 1.72*| 8. & 8. HE. Overcast to2 P.M. “i & “i afterwards,
Rain from Midnight to 9 a. m.
0.75 |S. &S8. H. Overcast. Rain at midnight & 3 4.M, &
from 5 to 1] a. mM.
126.0 is “i & “ito2 P.M. Overcast afterwards.
ele acca AS Ni & Oi.
TS T(9 1) Sel SS “i to 8 a. M. Scud. from S. to 7 a.m. i
afterwards.
| 122.4, | Ss ito 7 Pp. M. “i afterwards. Thin rain at
| | 2&4-.M.
7| 124.0 Ss Overcast to6 A.M.%ito5 p.m. Cloud-
less afterwards. Thin rain at-1 & 3
e A.M. & 5 P. M,
S. & S. W. Cloudless to4 a4. uM, —-ito3 P.M. i & 71
afterwards.
Ss Yi&é “ito2P.m. Overcast afterwards,
| Rain at 24. uM. & 3 P, M,
70) 129.0) _ ... Ss. “i to 6 A, M. Mi afterwards,
iS}
iS)
S
8 128.4
9| 125.0, 0.22
11| 131.4 | Vito7 A. M. %i to 3 P. mM, Cloudless
afterwards. Light rain at 2 & 3 ep. M.
i to 6 A. M. Ni to 2 P, M. Vi afterwards.
12| 1316]...
13} 127.0 | Cloudless to 5 A. M. Xito9 P.M. Clouds
| less afterwards. Light rain at 8 Pp. uM.
P40). s. Cloudless to 5 A.M. “ito 6 P.M. “i to
the HE. afterwards. Thin rain at 1 Pp. u.
15| 137.0| ... |8.H. GE. &S. “ié Sito 10 a.m. “iafterwards, Light
rain between 2 & 3 P. M.
16) 126.0, 020|S.E.&E.&S. Cloudless to 2.4. M. Overcast to 7 Pp, mM.
Cloudless afterwards. Rain at 2, 3,5
& 6 P. M.
17; 129.6; 0.13 |S. Overcast to 7 aA. mM. W-itol P.M. Overcast
to6 P.M. Cloudless afterwards. Rain
at1,5&6 A.M.
WStse) ., | |S. & B. Cloudless to 4 4.M. ito 7 Pp. mu. Cloud.
less afterwards. Light rain at 3 P. M.
19) 132.0} 0.18 |S. &S. E. Cloudless to5 a.M. %ito8 P.M. Cloud-
less afterwards. Thin rain at 2,3 &6
p, M.
4 129.0\ 0.12 E.&S.E. si, iiGaein et 2 See
|
Ni Cirri, —i Strati, \i Cumuli, i Cirro-strati, ~i Cumulo-strati, i Nimbi,
‘ni Cirro cumuli.
* Fell from 2 Pe, M, of the 31st July to 9 A. mM. of the Ist,
Ixii Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
wn the month of August, 1865.
_ Solar Radiation, Weather, &e,
Bene | as
See
.| 22 |& & §| Prevailing direction General Aspect of the Sky.
2| 83 1/838] ofthe Wind.
A|a% (gus
| oO |Inches|
2M eee 0.51 | N. E. & H. Overcast to 1p. mu. “~ito9 p.m. Over-
cast afterwards, Rain at10 A. Mu. noon,
1,3 &11 P, u.
22] ... 0.44 | S. H. & EH. Overcast to 4 P.M, V-ito 8 p.m. Cloud-
less afterwards. Drizzled after intervals.
23) 120.0} 0.13 |S. Cloudless to 38 a. M.°1 to9r. mu. Thin
rain at 4 & 8 a. M. noon & 5 P. M.
24) 129.8) ,.. |S.&S8S. HE. Overcast to 7 A, M. Mito 8 P. mM. VW-iafter-
wards. Light rain at 2 4. M.
29 126.5) 0.22 | Variable. Overcast to 7 Pp. M, W-i & Lightning after-
wards. Thunder at 9 A, M.
26 137.4; ... | N.E.&S. Clouds of various kinds. Lightning at
midnight & 1 a. uM.
27, 122.4) ... | N.& N.E. Overcast to 2 Pp. M. V-iafterwards. Light
rain at 3,5 & 11 P.M.
28)... 0.79 |S.H.& EH. & 8. Overcast. Rain from midnight to 2 P, u.
& at 7 P. M.
29) ase 0.58 |S. E. &S, Clouds of various kinds. Rain at 3, 6, 10
& 11 A. M.
30 129.0 A Ss. & W. Cloudless to 5 A. M. i afterwards.
31} 129:0))) Ss. & W. \-ito7a,M. ‘ito 10a.mM. Overcast to
| 4p.mM. Cloudless afterwards.
Meteorological Observations.
Ixiii
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of August, 1865.
Moyrury Rusvurrs.
Mean height of the Barometer for the month, .. ee
Max. height of the Barometer occurred at 11 a. M. on the 17th,
Min. height of the Barometer occurred at 2 a. M. on the 28th,
Extreme range of the Barometer during the month, Be
Mean of the Daily Max. Pressures, . wa we
Ditto ditto Min. ditto, .. 56 ao
Mean daily range of the Barometer during the month, ..
Mean Dry Bulb Thermometer for the month, .. = 40
Max. Temperature occurred at 3 Pp. M. on the 5th & 26th, ..
Min. Temperature occurred at 7 A. M. on the 2nd, ne
Extreme range of the Temperature during the month, te
Mean of the daily Max. Temperature, oe nie
Ditto ditto Min. ditto, .. oC ate
Mean daily range of the Temperature during the month, ..
Mean Wet Bulb Thermometer for the month, .. i
Mean Dry Bulb Thermometer above Mean Wet Bulb Diicriioweite,
Computed Mean Dew-point for the month, .. ae
Mean Dry Bulb Thermometer above computed Mean Dew-point,
Mean Elastic force of Vapour for the month, .. hs
. Mean Weight of Vapour for the month, is ae
Additional Weight of Vapour required for complete saturation,
Inches
29 623
29.779
29.311
0.468
29.685
29.553
0.132
°
84.5
92.6
We
15.4
89.7
81.1
8.6
81.3
3.2
79.1
5.4:
Inches
0.973
Troy grains
Mean degree of humidity for the month, complete saturation being unity,
Rained 22 days, Max. fall of rain during 24 hours, as
Total amount of rain during the month, ay ay:
Prevailing direction of the Wind, .. nic Ae
10.4.2
1.93
0.84
Inches
172
5.99
S.&5S. 8,
Ixiv Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of August, 1865.
Montruny Rersvrts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
Rain on.
Rain on.
Rain on.
Ss. E
Rain on
W.
Rain on
Rain on.
Calm.
es
|
|
|
|
|
|
:
|
|
|
|
|
|
Midnight.
pay
We)
NW w wre
iS)
BWW wOrhNE
fe
ae
FPOoOwMONOQOBWNE
HERP WN NH EE Eee
02 00
=
WHwWANTNAE Ee Pw
bo bo
DBONRHAUMUMANE Pe
bo eo
_—
oo
—
Ep wpe
pee
Noon.
PH ww
bo
bw oo
eb
pam
rc
a
—
Oy
—
Be} Or
ENED HH
wDe Bre Db
—
—
Ww wndH
~
c=
—
BPOOODVTANL WH
wwNwnNwrbenwrwmwanwDy
—
eS
to
Or
ell eellendlae
Meteorological Observations. i
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of September, 1865.
Latitude 22° 33’1” North. Longitude 88° 20’ 34” Bast.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in,
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
| id 2 = Range of the Barometer z 3 Range of the Tempera-
mes during the day. ae ture during the day
peas S 3
Date. | "93 e 5
| 352 | Max. | Min. | Dif. SG Max. | Min. | Diff.
= =
Inches. | Inches. | Inches. | Inches. Co) 0 0 0
1 29.645 | 29.705 | 29.596 0.109 85.2 87.7 83.4 4.3
2 .680 027 .625 102 83.9 88.8 79.2 9.6
ee) .663 125 584 141 84.5 89.8 81.0 8.8
4 .629 .692 551 141 84.4 89.4 81.8 7.6
5 599 -665 027 138 85.2 89.8 81.4 8.4
6 620 -701 .006 135 84.5 88.0 82.2 | 5.8
7 673 128 .604 124 85.4 91.8 82.4 9.4
8 .629 .696 553 143 82.3 84.8 80.4 44
9 580 .638 013 125 81.3 83.8 79.6 4.2
10 .580 .620 019 101 81.5 85.0 80.2 48
11 .570 .629 014, 115 81.7 86.4 79.6 6.8
12 601 .667 045 122 81.0 86.6 78.2 8.4
13 .669 «145 614 | ollB3} 78.5 81.2 76.8 4.4
14 .756 .809 701 .108 79.3 84.6 75. 9.2
15 770 .833 .694, 139 83.4 88.6 78.6 | 10.0
16 -733 .806 634, 172 85,2 90.3 80.4 9.9
17 -702 072 .619 153 86.7 91.4 81.8 9.6
18 .689 «759 084 175 87.1 93.0 82.2 | 10.8
19 -686 Bape .603 148 86.6 92.8 82.4 | 10.4
20 .656 Bliss 584, | 129 83.8 89.0 79.0 | 10.0
21 .624; .670 549 | 121 85.2 90.4 81.1 9.3
22 645 .696 604 .092 85 4: 90.2 80.8 | 9.4
23 .673 127 .630 .097 85.5 89.6 82.2 74
24 723 789 .676 113 84,0 896 79,2 | 10.4
25 | .784 .638 727 111 84.9 91.2 79.2 | 12.0
26 1D S00 855 732 123 85.8 91.6 81.9 9.7
27 -761 £932 .689 143 86.1 90.7 82.2 8.5
28 707 784 .638 146 85.8 90.4: 82.2 8.2
29 .696 754 .635 119 85.3 90.6 83.4 7.2
30 .718 780 .660 .120 86.6 91.8 §3.2 8.6
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the hourly Observations made during the day,
il Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of September, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.— (Continued.)
is Sua se S A | 2 See
la s = a 2 a. | eee
S Ps iS) OR oi A Ss
| aes ow Ss & Ps | Seeie ries ase
| aa Co) ° SO ao aa a) = 2 “=
1 3 5 E 2 © Le | Pee =:
Dptedl wae = Q 6 a9 Secs] SS) Ss
| 22 2 0 eS FSS) 288
| 23 2 3 a ca os |zo8t| Pls
| Bo = s Ae BS | Os | ees ec meee
9 Q 3 Ais a ofS Sa
a6 Ru =) As as As (© sig
® A 2 5 a ee | $8 |cs ave.) Seas
= a) i) a = = cS =
EEE eS
| o to) O) oO limes, | 2s re, | M. ee,
a 4, P23 2.9 80.3 | 49 | 1.011 | 10.80 | 1.81 | 0.86
5.1. (8.4 2.5 79.6 | 4.3 | 0.989 .60 nae .87
3 B15 |. 8.0 79.4, | |5.1 .983 pik 84 85
4 81.9 | 2.5 80.1 | 4.3 | 1.005 JB 56 87
5 S18 034 79.4) 5.8 | 0.983 49 | 2.12 .83
6 B22) eS 80.6 | 3.9 | 1.021 Be | 1a 88
7 | 82.4 3.0 30.3. Bil O11 .80 .88 «85
s | 80.9 1.4, 79.9 | 2.4 | 0.998 74 | 0.84 93
y 79.7 1.6 78.6 | 2.7 .958 .32 92 .92
10 797 1.8 78.4 | 93.1 952 PS | TOG 91
il 79.8 19 Wish) | Be 955 .29 .08 91
12 79.1 1.9 77.8 | 93.2 934 On .07 90
13 77.5 1.0 GSS) Le 905 | 9,79 | 0.56 95
14 V7 9 Wael 76.9} 24 .908 82 ae .93
15 80.4 | 3.0 FE | Be 949 | 10.18 | 1.78 85
16 81.5 a7 78.9 | 6.3 .967 84 | 2.27 82
17 82.2 4.5 HISD I” eho 986 51 67 .80
18 82.4 4.7 79.6 3) .989 52 81 79
19 81.8 48 78:90 aie: .967 .30 84 .78
20 80.5 3.3 78.2 | 5.6 946 3) 9 BEST 84
21 Bless eso 78.6 | 66 958 23 | 2.38 81
po 2706 Nes Ty |p G8) 868.| 9.27 | 3.41 a3
23 80.0 | 5.5 6A oA 885 46 .26 74:
DA | 79.2 4.8 Tpsie) | 876 39 | 2.78 77
25 | 80.6 4.3 Bi.6 | e738 928 .93 56 .80
26 | 81.3 4.5 78.1 a .943 | 10.06 an 78
27 B02 jenn 76.1 | 10.0 885 | 9.44 | 3.51 73
28 80.4 | 5.4 76.6 9.2 .899 .59 24, 75
29 | 80.8 4.5 TON TK .928 Ign! \ 2i7e 78
30 | 80.9 5.7 | 77.5) 91 .925 .86 | 38.28 1D
| |
| |
| |
es,
All the H7gvometrical elements are computed by the Greenwich Constants.
Meteorological Observations. lil
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of September, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
c s a | Range of the Barometer | s o Range of the Temperature
= g= for each hour during oS for each hour during
Hoe = = aa the month. aS) the month.
. oo a (= I
= ect eo |
S23 | Max. Min. Diff, se | Max. Min. Diff.
= =
Inches. | Inches. Inches.) Inches. Co) Oo) (0) o
Mid- 29.69 yi : 5 pe
night, | 7°: 93 | 29.815 |29.599 0.216 82.5 84,6 78.0 6.6
1 .683 811 584 227 82.3 84.2 78.0 6.2
2 .670 .796 563 230 82.2 84.0 78.4 5.6
sep 200k -786 003 233 82.0 84.2 78.6 5.6
4, .657 792 DAT 245 81.7 84.4 | 78.0 6.4,
5 .665 .798 Ad 249 81,5 84.5 77.5 7.0
6 .678 812 DOA .258 81.2 84.6 75.6 9.0
Zi 694 .832 .569 .263 82.0 85.2 75.4 98
8 714 Sol 1587 264 83.4 86.8 Go 11.3
9 726 .850 098 202 84.7 88.1 75.4 12,7
10 727 .855 594, 261 85.7 89.8 76.1 13.7
11 7138 1854 586 .268 86.7 91.2 76.9 14.3
Noon. 691 835 567 .268 87.4 92.0 78.4 13.6
1 .669 .807 DAT .260 87.5 92.8 80.5 12.3
2 645 TES -528 247 87.5 93.0 79.6 13.4
3 | 622 | 748 | 1593 | 295 | 874! 9201 795 12.5
4, 614 UES 013 222 87.0 91.6 79.6 12.0
5 .618 132 O14 218 86 6 91.4 79.2 12.2
6 633 “744A .039 .205 85.3 89.4 76.8 12.6
7 .655 .767 D9 .208 84.5 88.2 774 10,8
8 .678 .796 OTA 222 83.6 87.4 77.4 10.0
9 697 .806 588 218 83.L | 86.0 77.8 8.2
10 707 | .808 601 .207 82.8 | 85.4 77.8 7.6
ED 704 .810 611 199 82.5 | 84.8 78.1 6.7
| |
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several hours
during the month,
iv Meteorological Observations.
Abstract of the Results of the Hourly Meteoroloyical Observations
taken at the Surveyor General's Office, Calcutta,
in the month of September, 1865.
Hourly Means, Xe. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
ae) Sf) 8) |) Bisilinve ae eile seamen
mf BS 8 8 he eels
S| Ek bp Soecet Ss eee
> Bepiss ° ° Sis 56 5
Hour. | BS = a Se $ : anO" ae: Se
5 2 3 SUE) Site eS a,2/|3S68
Eo 5 = SS Ao Eni eee || a Boe
2s oe a As Ga | 6 53 | Sosa moeee
| as b g py oe & Ow See ats
B fa) s) Qe len meme edn oe as
0 ty) ty) ty) Inches. |Troy grs.|Troy grs.
}
as 807 | 1.8 | 794 7) 8a) | 0.983) 10.56 1.08 | 0.91
1 BOGi yy) 79.4, 2.9 .983 .56 .02 91
2 80.5 | 1.7 | 79.8 2.9 979 53 01 91
3 BoB NY 1 79.1 2.9 973 47 .00 91
4 80.2 ese omy cane | 2.6 978 AT 0.90 92
5 80.0 15 | 78.9 2.6 967 Al .90 92
Se ne ee 78.8 2.4 964, .40 81 .93
mo) BOIL ey ye 7 ot 2.9 973 47 1.00 91
gs | 80.4 3.0 | 78.3 5.1 949 .18 .78 .85
9 80.7 | 4.0 77.9 6.8 937 .02 2.40 81
10 80.9 | 48 | 77.5 8.2 925 9.88 .92 Sek
11 81.3 5.4 | 78.1 8.6 .943 | 10.04 3.14 76
Woon.| 81.3 | 611] 77.6 | 98 | .928 | 9.87 58 73
qi]. (sie 64) 7785 102 919 78 AA di
Bi} (8100 6.5 Pinel 10.4 913 72 ail 72
3 | 809 65.1 770s) tod 910 .69 76 72
4 80.9 6s 772, 9.8 916 75 54 73
5 81.1 5.5 | 77.8 8.8 934, 95 19 76
6 81.2 | 4,1 78 7.0 949 | 10.14 2.50 .80
7 Sl. | Sd. 787 5.8 961 .29 .06 .83
me |) S09. P27 79.0 | 4.6 .970 40 1.63 87
H | 807 5| 2A4F 790 41 .970 2 44, .88
10) 10/805 4 23780 3.9 967 .B9 .36 88
ll 80.5 | 2.0 | 79.1 3.4 973 AT il .90
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations. Vv
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
an the month of September, 1865.
Solar Radiation, Weather, &c.
2) 137.0| 1.76 |S. & W.
3) 138.0; .. |W.&8S.&8. W.
seneatietsh. ig alts Op
ar Yeo 0) °c. tH,
6 een 76s || ONS
(3 aan 0.21 | N.
ee O42 He de NG. Hs!
HON. Parra 8. Hea Ny he
LA Soper 0.78 | H.&N. EH. ON.
12| 123.5) 0.12 |N.E &E.
Le er 2.36 |H. & 8. H.
4)... 111 |H. GS. EH.
15| 124.0; ... | E. &&.
16, 132.8) .. |S.&N.E.
|
. . oo
tS oo >
=osd Ses
eos Fah aang
3 2's © § € |Prevailing direction General Aspect of the Sky.
=| #3 18.32| ofthe Wind.
Ss S = eH
A | = eod
=| ee ae ee a
| o {Inches.
1 |S. Overcast.
Overcast nearly the whole day, Rain from
3to7 a. um. & from noon to 2 P. M.
Thunder towards N. at 9 p. m.
i & Nito7 A.M. 91 to5e. mM. Overcast
afterwards, Thin rain at 10 & 114. m.
&6P.M. Thunder towards N. W.at7
p. M. Lightning towards N. from 7 to 9
P. M,
%1t06 A.M. Overcasttolla mu. i &
“i afterwards. Thin rain at 10 & 11
A. M.
\Wito5a.M. ito 3 Pp. mM. Clouds of
different kinds afterwards. Light rain
between 7 & 8 P. M,
Li1& oi to7 a M.c1to3P.M. Overcast
afterwards. Rain at5 a.u.& 4 Pp. m.
ito2Pp.M. Overcastafterwards. Thin
rain between midnight & 1 A. uw. & at4&
& 7 P.M.
Overcast. Scud. from N. at 6 & 7 a. M,
Thin rain from 9 a, M. to 9 P. M.
Overcast nearly the whole day. Light rain
after intervals.
Overcast to 7 p. M. Cloudless afterwards.
Thin rain at 74. M. & from 10 to 1 P.M.
& at 4 Pp. M.
Overcast nearly the whole day. Rain from
38 to8 a. M. & from 1 to 8 P, M.
Overcast. Scud. from EH. from 8 to noon,
Thin rain after intervals.
Overcast. Scud. from 8S. HE. from 6 to 10
P.M. Rain from 4 A. M. to 11 Pp. uM.
Overcast to 5 P. M. Seatd. “i afterwards.
‘Rain from 5 to 11 a. mM, & between 4 &
5 Pp. M.
Overcast to 8 A.M. %ito 6 Pp, M. Clear
afterwards. Thin rain between 3 & 4
P. M.
Clear to’7 A.M. %ito6e.mM, Clear after-
wards. Lightning towards S. H at7 P.M,
Mi Cirri, —i Strati, %i Cumuli, i Cirro-strati, ~i Cumulo-strati, i Nimbi,
“i Cirro-cumuli.
Vi
Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of September, 1865.
Oo od
ms S
3) es |on
a 126 :
99 |sQlsg
so Bre
~ Ree \2 5
S| xs 1a 3s
8S) Sea laws
Ala = |jpoo
|
fe) Inches
17) 187.4
1
18) 144.0
19) 143.9} 0.47
23) 130.0
24) 140.4) 0.41
25| 141.8| 1.16
26| 142.0) ...
27| 140.0)
28 135.4
29) 130.0
30! 139.4
Solar Radiation, Weather, &c,
Prevailing direction
of the Wind.
8S. & HK.
8. & E.
N. W. & variable.
N. W. &N.
N. & N. W.
N.W.& W.&N.
W.
S.& EH.
|S. &S. W.& HE.
General Aspect of the Sky.
Clear to 7 A, M. “iafterwards, Lightning
& Thunder at 8&9 Pp. uw, Light rain
between 8 & 9 P. M.
Clear to 5a. M. Siafterwards. Lightning
towards N, W. at 7,8 & 9 Pp. uM.
Clear to 4 a. mM. ito 7 a. M. “ito 6 P. M,
Overcast afterwards. Lightning from
Midnight to 8 a. u. & at 7 Pp. M. Rain at
8&9 P.M.
Clear to 5 a.m. Clouds of different kinds
afterwards. Rain & Thunder at 1,2 &
3p.M. Lightning at 7 P.M.
Clear to 8 A.M. “ito 6 p.m. Clear after-
wards, Rain between 3 & 4 P. M,
Clear to9 4.M. 71 & -ito7 P.M. Clear
afterwards.
Clear to 5 a.m. i to10 a.m. “ito 5 P.M.
Vi afterwards.
Overcast to 10 a. M. Si afterwards. Rain
at 2, 3-10 & 11 P. uM.
MWito4 a.m. “ito 4 Pp. uw. clear after-
wards. Thunder & lightning towards
S. W. at 3 a. M. rain from 2 to 4 A, M.
Clear to 5 a. M. “ito 2 Pp. M. ‘i to6P. M.
clear afterwards,
Clear nearly the whole day.
Ni to 7 a. M. %i afterwards.
Vito 3 A.M. 1 to3 Pp, M. -i afterwards.
Thin rain at 4 vp. M.
Overcast to 5 A. M, Cito 5 P. M. clear after-
wards.
ee
Meteorological Observations.
Vil
Abstract of the Results of the Hourly Meteoroloyical Observations
taken at thé Surveyor General’s Office, Caleutta,
in the month of September, 1865.
Montuty Rursvuprs.
Mean height of the Barometer for the month, .. ac oe
Mas. height of the Barometer occurred at 10 A. M. on the 26th, a.
Min. height of the Barometer occurred at 4 P. mu. on the 9th, Re
Extreme range of the Barometer during the month, Be nas
Mean of the Daily Max. Pressures,.. 06 66 AG
Ditto ditto Min. ditto, .. ale 00 ae
Mean daily range of the Barometer during the month, .. ote
Mean Dry Bulb Thermometer for the month, .. ee 00
Max. Temperature occurred at 2 P. M. on the 18th, oe aie
Min. Temperature occurred at 7 a. M. on the 14th, ae ae
Extreme range of the Temperature during the month, 00 -
Mean of the daily Max. Temperature, ate se ae
Ditto ditto Min. Gibvonmes AA O06 ee
Mean daily range of the Temperature during the month, .. ae
Mean Wet Bulb Thermometer for the month, .. 50 Ao
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, ..
Computed Mean Dew-point for the month, .. ee He
Mean Dry Bulb Thermometer above computed Mean Dew-point, oc
Mean Elastic force of Vapour for the month, .. aie Pee
Inches
29.676
29.855
29.513
0.3842
29.737
29.609
0.128
80.7
3.5
78.2
6.0
Inches
0.946
Troy grains
Mean Weight of Vapour for the month, ate ate 56 10.13
Additional Weight of Vapour required for complete saturation, ee 211
Mean degree of humidity for the month, complete saturation being unity, 0.83
Inches
_ Rained 21 days, Max. fall of rain during 24 hours, Ae ne 2.36
- Total amount of rain during the month, «e se es 10.25
Prevailing direction of the Wind, .. eo eo E.&N.&S,
q
viii Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Caleutta,
in the month of September, 1865.
Monruny Resuptrs.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
°o lo} lo} ° OF -| oO Ci he
siAls elle] |e|ele| .|stel.
Note [oh EB. |g S.\ce la |e (EF lata
No, of days.
Midnight. 3) 4 4 6 | 3) Js) fil | 4) pa
if 3] 1 4 A Ea (A Pe ZS pe if!
2 5) 1 3 SI Gl Zeeland alo amano
3 6) 1] 4) 1) 4) | 2) | ap 2) a 4) 4 2
4, 7) 1j 2) 1) 7 2 6| 1) 1) | 5] 1} 2
5 6| 21 2 "il @ 6) yall 5) 1S!
6 5| 47 2) 1 5] 1) 2) 4 G| Fa) 7 5] a4
7 5| | 3] 2f 6] 3] 1] | 5] Fa) 7 5) a4
8 6} | 6) 2) 4) 1) 2) 1) a) Fe) We 3|
9 PALA Pees el Shea tall || 2:
10 7| 1) 4 7 2) 21 2) 2 5| 213
11 5 1) 5 Way
Noon. 2) 3] 8) 1) 4 1 2 4, 6) 1
1 5| | 3] 1h’ 8| 3] 2| 2 4) at 2) 4) [a2
2 5| 1] 3| 5| 3] 3] | 4) af 1} 1] 4) 5
3 3| 1) 2) 1 5] «| 4 1t 6] if 1) a 3] 6
4 8 bf 1) 6| 2) 4) | 6) at) 94
5 TAA iol 6) | 3) 1) 6) 138 Bi a
6 7 Wd 7| 1/ 3) 1] 5) 172) J 4) fa
7 al al 1| 6) 1) 2) | 5) 73) Pal
8 7| 1 8| 21 3/115) |2l tal qi
9 5| [1/1 9] 2] 3} |e) api) | 4) f2
10 Ele bl 10| 2} 2; | 7; f 2) 14) F2
can 3| | 4 6/1] 2| | 8) | 2] 114 1
Meteorological Observations. ix
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of October, 1865.
Latitude 22° 33’ 1” North. Longitude 88° 20’ 34” East.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
% 2 = Range of the Barometer B S |Range of the Tempera-
S 5 = during the day. BA ture during the day.
cen As
Date. |" me sS iB
5 23 Max. Min. Diff. & a Max. Min. | Diff.
= =
Inches. | Inches. |} Inches. | Inches. 0) 0 a) 0
ie 29.727 | 29.796 | 29.656 0.140 87.2 92 2 83.3 8.9
2 718 LOG -640 BB 86.7 92.2 81.2 | 11.0
3 | .763 al 716 115 87.4 93 2 82.2 | 11.0
aii 1153 824 692 »Lda 87.2 93.1 81.3 | 11.8
5 “751 812 692 120 87.2 | 92.8 82.2 | 10.6
6 wip: .807 687 120 87.4 93.0 82.5 | 10.5
7 2788 842 736 .106 86.9 92.6 81.2 | 11.4
8 .855 912 801 ll 87.1 92.8 82.6 | 10.2
9 864 931 788 143 86.8 93.4 82.0 | 11.4
10 873 944, .823 «121 85.8 92.1 81.4 | 10.7
11 .882 951 815 136 85.9 91.8 81.6 | 10.2
12 -884 951 821 .130 84.7 91.2 79.8 | 11.4
13 .890 .962 2839 alize 83.4 90.8 78.2 | 12.6
14, 914 .999 .863 136 85.3 92.2 80.0 | 12.2
15 922 | 30.005 854: 151 84.8 92 790 | 13.6
16 .887 | 29.953 824 “L229 84 4 91.4 78.5 | 12.9
17 859 .929 -807 122 83.8 90.2 77.4 | 12.8
18 .855 915 794 2h 83.6 89.8 77.4 | 12.4
19 .876 943 Ter 166 $4.3 99.0 79.0 | 110
20 .918 987 867 .120 83.8 90.0 78.0 | 12.0
21 904 .969 846 123 83.0 87.6 798 7.8
22 853 922 -799 123 83.8 90.6 78.9) |) JIR7
23 842 915 .808 107 84.0 91.4 79.0 | 12.4
24, O47 JS 7L .807 110 81.3 $2.0 74.8 | 14.2
25 .856 .935 .O15 120 80.5 89.6 72.6 | 17.0
26 .857 SEE 804 29 81.0 89.8 72.8 | 17.0
27 .009 904 786 118 81.9 90.2 74.0 | 16.2
28 . 873 .935 -830 105 82.9 91.4 76.6 | 148
29 918 998 .863 ABB 82.4 89.6 76.2 | 13.4
30 904 983. | 833 145 81.5: 88.8 75.6 || W32
31 .875 a2 .807 145 79.5 86.6 73.4 | 13.2
: .
: Sp ARSE Ee AR
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Meaus are derived from the hourly Observations made during the day,
x Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of October, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
2 Pea 2 Pee) 2 =
= 4 £ a 9 2 | eel eee
= 2 © 3 pS 9 2 eae
S 5 5 a 2 i S| yace =
Date | oe | 2 | aS| 2.) #2 (eee
| OD 2 no) = — MH O's —-o @ 2 o's
fae 3 Seon eee =
a fa . = ae | 6 3. |-ReSsocl cee
® A fe S ae oF S48 |san| S55
= fa) S) a = = - =
eee
o o 0) 0 Ihn@lngs, || “MU, fare, | AL, fete.
1 81 2 6.0 77.6 9.6 0.928 9.87 *| 3.50 0.74
2 79.9 6.8 75.8 | 109 876 .39 .85 71
3 80.0 74 75.6 | 11-8 871 .20 4.20 .69
4. 80.0 7.2 Mowe belies 873 28 -09 .69
5 79.8 7.4 75.4 | 11.8 .865 .20 oll'7/ .69
6 79:9) ae d.d 75.4 | 42.0 .865 .20 25 .68
7 79.9 7.0 Teal |) Wile 873 30 3.95 70
8 199 Sse 75.6 | 11.5 871 25) 4.08 .69
9: 9 80.9 5.9 77 A, 9.4 922 83 3.38 74
10 80.6 5.2 77.0 8.8 .910 71 12 76
11 80.1 5.8 76.0 9.9 1882 AL 46 13
12 79.6 5.1 76.0 8.7 882 43, 2.99 76
13 78.8 4.6 75.6 7.8 871 30 63 78
14 Tsp 6.2 74.8 ) 10.5 849 06 3.08 72
15 76.9 7.9 71.4) 18.4 761 8.13 4,33 65
16 76.7 Gi GAs8y ea 758 alll .20 66
17 76.3 7.5 71.0 | 12.8 751 04 .06 .66
18 76.3 7.3 71.2 | 12.4 756 .10 3.93 .67
19 | 76.7 7.6 71.4 | 12.9 761 13 4.15 .66
20 77.7 6.1 73.4 | 10.4 igoll .69 3.41 72
21 784 4.3 eet 1.8 873 9.38 2.44) 79
22 78.6 5.2 75.0 8.8 854 14 -96 76
23 75.7 8.3 69.9 | 14,1 725 7.76 A.A 64
24 | 71.5 9.8 64.6 | 16.7 609 6.55 .69 08
25 70.7 9.8 63.8 | 16.7 093 09 09 08
26 | 71.8 9.2 65.4 | 15.6 .626 73 AL .60
27 73.9 8.0 68.3 | 136 .688 7.39 .05 65
OBEN ides 6.8 (ales |) wets) 758 8.13 3.66 .69
29 76.2 6.2 71.9) | £O%5 7173 29 182 sf
30 74.3 7.2 69.3 | 12.2 711 7.64 67 68
31 72.1 74: 66.9 | 12.6 657 09 7 67
|
I
Ail the Hygrometrical elements are computed by the Greenwich Constants,
— a
Meteorological Observations. xi
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
an the month of October, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
S 3 | Range of the Barometer = 3 Range of the Temperature
mages for each hour during As for each hour during
Hour = g i the month. bo the month.
“| oa & aq 8
so : : S| | 0 9
Zoe Max. Min, Diff, BS Max. Min. Diff.
= =
Inches. | Inches.} Inches.| Inches. Co) 0 0 0
Mid-
night, 29.847 ' 29,923 (29.732 0.191 81.1 85.0 76.4 8.6
1 .839 .918 719 oh) 80.7 84.3 76.0 8.3
2 .832 .908 .709 199 80.3 84.0 75.2 8.8
3 .828 .903 -706 197 80.0 83.6 TAA, 92
4 831 914 -708 .206 79.6 83.4 73.6 9.8
5 844 931 722 .209 79.2 83.3 72.8 10.5
6 861 949 .138 Pal ||) YO) 83.5 72.6 10.9
Zi .882 974 154 .220 80.2 85.0 73.8 11.2
8 901 .997 773 224: 82.8 86.4: 77 A 9.0
9 915 |39.004 OL 227 84.8 88.2 79.8 8.4.
10 914 -005 766 239 86.7 90.0. 83.0 7.0
il 897 {29.988 747 241 88.5 90.8 83.6 7.2
Noon. 871 975 -716 259 89.4 92.0 86.6 5.4
1 -840 .919 .695 224, 90.0 92.8 85.2 7.6
2 .813 .889 664 225 90.4 93.0 85.3 EE
3 798 871 648 223 90.8 93.2 85.0 8.2
4 “791 .863 .640 .223 90.2 92.8 84.4: 8.4
5 -798 .873 649 224 89.8 93.4 83 1 10.3
6 .807 879 671 .208 86.5 89.6 81.6 8.0
7 2824 894 .690 204 84.8 88.4 80.2 8.2
8 .846 -920 | 712 .208 83.8 87.2 78.8 8.4
9 .857 .930 AUS .203 82.9 86.6 78.0 8.6
10 .863 .932 733 .199 82.1 86.0 77.0 9.0
1 807 934: 1734 -200 81.4 85.6 76.2 9.4:
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several hours
during the month.
xil Meteorological Observations.
Abstract of the Resuits of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of October, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
To) 45 = = ay ae) Ga one nee
= o =| 3) ° SiS 2) ge S = eS
| 2 = 5 |A 2 ieee
Pook | Bee Sod ce eee eee
a | a1 =
Hour. S = = a “Ss 5 4 O E o a 5 a oP
z =| 3 2 Sots Ss alicla a2 2 ees
|} &°o 3 = aya Fo eS eS a ees
= 8 b 8 pay oF oo | SS os een
& a) 5) Qa = = igeeen we gé
0 to) oO ty) Inches. |Troy grs.|Troy ers.
He "7.7 | 34 | 753 | 58 | 0862 ! 929 | 188°] 088
an 77.6 SP al) ioe 5.3 865 134 .70 685
9 \ 77.4 2.9 | 75.4 4.9 865 34 57 86
et ay Be 2.8 75.2, 4.8 .860 28 53 .86
Aa) 2700 2.6 | 75.2 4.4) .860 .30 39 87
Bi 3Bie 2.5 | 74.9 4.3 851 21 135 87
6 76.5 2.5 74.7 4,3 846 16 BY el| | sir
"7 76.9 3.3 | 74.6 5.6 843 .09 79 84,
Rol Bish 5.7 73.1 9.7 .803 8.61 3.14 are
9 a7 2 61719) 1,12.9 773 .26 4,20 .66
10 97.5 912 | 7210 14,7 776 125 93 63
1 76.) WO 712 Wf 756 .02 5.78 58
|
Noon.| 77.5 | 11.9 | 70.4 | 19.0 .736 7.79 6.46 Rats4
Coil See aleee a 697 we eos 720 61 89 53
el Bo deem Gos) | oni 711 50 7.17 51
3 | "7.0 | 13.8 | 68.7 92,1 697 3D 49 50
Ao WEL aed 69.2) 2110 708 48 iil 51
Bel 97%. | ASA OA 10/4 .736 19 6.63 54
6 Pea lo S44 73 si 803 8.56 4,54 .65
7 783 6.5 AWipe (alta .819 76 3.70 70
8 78.2 5.6 | 74.3 9.5 835 94 .16 74
9 78.0 4.9 | 74.6 8.3 843 9.05 2.74 Sehr
10) 7 4.4, 74.6 75 843 05 46 79
11 77.7 3.7 75,1 6,3 857 “20 04 82
}
ane
All the Hygrometrical elements are computed by the Greenwich Constants,
° ‘ opt
Meteorological Observations. xi
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of October, 1865.
Solar Radiation, Weather, &c.
= S| So 2
Sots ss
.| 2 |O & = |Prevailing direction General Aspect of the Sky.
= ce 3 = oe of the Wind. i
A,S7 jewd
0 {|Inches.
1) 142.2 ‘ N.W.&S8S Clear.
2) 139.4 N. W. Clear.
3) 140.0 W.&N. W. Clear.
4) 140.0 NV Clear to noon, Scatd. “i to 5 p. M,, clear
afterwards.
Bi 144.5] ... W.&N. Clear.
6 138.0 N.W.&N.&W. | Clear.
7| 139.9 | Be leWeyds Ne Wi Clear to 7 a. um, ‘ito the H. to 3 P. u.,
- clear afterwards,
8} 189.7| ... W. Clear.
9} 138.0 W.&S. Clear to 11 a. M. “i to 5 P. M. clear after-
wards.
10} 189.0} ,, 8. &58. W i to 5a.M. “ito noon, clouds of various
kinds afterwards.
31} 142.0| ... s.&8S. W Clear to 11 A. M, i round the horizon to
6 Pp. M., clear to 9 P. M. i to the N.
afterwards.
1G) IS fea eee S.&S. W.& EH. Mnitoll a.m. .%ito5p,mu.“~itothe S.
W. afterwards.
13} 139.0} .... S.GS. W.&S. H. | Clear to 44, m. Overcast toll a. mM. i
to 6 Pp. M. “~i to the W. afterwards.
$4 142-0)... H. & W.&S. W. “itol0 a.m. i to5 Pp. m., clear after-
| wards.
45) 149.4)... W.&S. Clear to noon, %i to 4 P. m., clear after-
wards.
EG LSSS i)... N. W. Clear to 10 A. M. Xi to 4 P. M., clear after-
wards.
i GAZ. Nod No W. Clear to 9 A. M. Sito 5 P. M. olear after-
wards.
oSt42G | 22 oN. & N. W: Clear to 9 a.M. Mito 6 P. mM, “i to the
.
H, afterwards.
19} 143.0) «.. | N.&W.&N. W. i to 8 a. M. clear to 10 a. m. Scatd. 11
EB afterwards.
20} 144.4| ,.. | S.&H, Clear to 9 a.m. Scatd. 9i to 5 P. u., clear
afterwards.
FAV UB ENG | TSM Clear to 5 a. M. Wi to 7 P, M., clear after-
wards.
221 139.0| ... | W.&S. E. Clear to 7 A. M. Seatd. i to 4 P. u., clear
afterwards,
_ ~NiCirri, —i Strati, \i Cumuli, ~i Cirro-strati, ~i Cumulo-strati, W-i Nimbi,
- Wi Cirro-cumuli.
X1V
Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
wn the month of October, 1865.
to
w
Sh ty
®D TS Ole
wwe
| Date.
Solar
Max.
Rain Gauge
5 feetabove
Ground.
oa
6
ie)
=
(@)
a
ee
tee
Solar Radiation, Weather, &e,
|W. & 8S.
E. & N.
N.GN, E.
Prevailing direction
of the Wind.
Vivo @o SS VIM
W.&S. W.
General Aspect of the Sky.
a Eg ST
“Wi to the KE. & N. W. to 4 a.m. “-ito8
A. M., clear afterwards.
Clear.
Clear,
Clear.
Clear.
Clear to 4.4.M,“i to5 p. m., clear after-
wards, ~
Clear to 10 a. mu. Scatd. ito 9 P. M.,
clear afterwards.
Clear to 4.4. mM. “i & ‘i tonoon. Seatd.
oi to 6 P. M., clear afterwards.
Clear to8 A.M. Stratonus to 3 P.M, “i
afterwards,
Meteorological Observations. XV
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of October, 1865.
Montuty Rusvurrs.
Inches
Mean height of the Barometer for the month, .. a0 eA ZoISAS
Max. height of the Barometer occurred at 10 a. mM. on the 15th, s» 380.005
Min. height of the Barometer occurred at 4 P. m. on the 2nd, -. 29.640
Extreme range of the Barometer during the month, we Ano OSes
Mean of the Daily Max. Pressures,.. 50 ae se 2ST
Ditto ditto Min. ditto, .. 56 60 ae 298790
Mean daily range of the Barometer during the month, .. So OE)
oO
Mean Dry Bulb Thermometer for the month, .. 50 ee 84.4
Max. Temperature occurred at 5 P. M. on the 9th, 50 BS 93.4
Min. Temperature occurred at 6 A. M. on the 25th, ay Ae 72.6
Haxtreme range of the Temperature during the month, ate ms 20.8
Mean of the daily Max. Temperature, Ubgierars oe 50 91.0
Ditto ditto Min. ditto, .. ae oe se 73.8
Mean daily range of the Temperature during the month, .. nif 12.2
Mean Wet Bulb Thermometer for the month, .. ae ae Wr 4
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 70
Computed Mean Dew-point forthe month, .. ae a 72.5
Mean Dry Bulb Thermometer above computed Mean Dew-point, we 11.9
Inches
Mean Elastic force of Vapour for the month, .. ae So OGY
Troy grains
Mean Weight of Vapour for the month, ac oe ee 8.42
Additional Weight of Vapour required for complete saturation, ee 3.89
Mean degree of humidity for the month, complete saturation being unity, 0.68
Inches
Rained No days, Max. fall of rain during 24 hours, at Wi Nile
Total amount of rain during the month, os oe ae Nil.
Prevailing direction of the Wind, ,. on oo wo WL & 8S.
Xvi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of October, 1865.
Montruty REsvyts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
5 5 §| .|6 elishic 6 el Sed Sites
2/4 | 2 ells] |sie\sl .|.Sielsislel2
No Siz [ce Bok [os |e 18.8 a (SIE lela leis sia
No, of days.
Midnight. A 1 3 5 5) 43 8 2
1 5 1 3 4, 6) 13 7 2
2 4 1 2 5 6| 43 i 3
3 A 1 2 4 17] 13 7 3
4 4, 1 3 3 "| 43 i 3
5 A 1 3 2 8| | 3 7 3
6 4 1 if 3 7| 9 4 7 4
7 A, 2 2 "| 5 7 A
8 5 2 4) | 8 9 3
9 5 1| i 5] # 5! (10 4
10 2 3] 6| #3] #11 6
11 2 1 2 1 Wy Gah 6
Noon. 2, 2 2 3| 12! [10
1 A 2 2 5 8| }10
2 4 1 1 1 4| 413 Z
3 2 1 4| 14) $10
4, 3 1 3 4, 9| fil
5 4 1 1 3 4) 412 6
6 5 2 5 2| 412 5
7 4 2 1 5 PA | (2 5
8 2 1 6 1 3 2| (12) 14
9 2 1 7 1 3 2) fil 4
10 2 1 6 2 4| | 3] [10] | 38
11 3 1 5 A Al 13 8 3
i A SE A
——
Meteorological Observations. Ixxxi
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Caleutta,
in the month of November, 1865.
Latitude 22° 33’1” North. Longitude 88° 20’ 34” East.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft. 11 in.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
o5 pasa
2oxv Range of the Barometer a 2 |Range of the Tempera-
"ep 5 Ss during the day, eae: ture during the day.
| oe E °o la 3 a
Date. | “~ E s 3
252 { Max. | Min. | Dif. SE Max. | Min. | Diff.
= =
— oo Cael ——~—=
Inches. | Inches. | Inches. | Inches. to) ry 0 o
1.6 | 29.802 | 29.863 | 29.732 0.131 78.6 85.7 BO) | Wz7/
2 801 .867 745 a2, 79.5 87.3 72.5 | V4.8
8 878 .953 817 136 81.0 88.2 73.8 | 14,4
4, 925 | 30.006 .853 LEE 79,7 86.8 71.4 | 15.4
5 .923 | 29.989 .876 A) 80.5 85.8 74.8 | 11.0
6 -931 | 30.007 873 | .184| 79.6 86.8 | 74.6 | 12.2
7 .899 | 29.965 8427) Gk23° [5976.5 85.4 | 67.0 | 18.4
8 .860 .918 “791 27 77 A 86.4, 68.6 | 17.8
9 .866 .929 822 | 107 78.5 86.4 70.5 | 15.9
10 .851 .920 .802 118 80.7 87.4 (5.6 HES
aa [2 .863 -929 822 | 107 80.6 87.2 VIKO) |) We
12 874 941 818 123 | 79.4 85.1 | 74.7 | 10.4
13 887 .964 .839 | 125 \ 77.4 85.7 71.8 | 13.9
14 -926 | 30.008 850 | PLS Si ees90 87.8 72.2 | 15.6
15 .970 051 921 | .130 80.0 86.8 Hees | UE
16 30.018 .094 .953 141 79.3 86.5 T2 Si loen
17 ,063 .133 | 30.005 128 77.8 86 0 71.5 | 14.5
18 .085 156 021 UBS 78.0 86.4 71.2 | 15.2
19 .092 164 .034 130 77.0 84.8 70.4 | 14.4
20 043 126 | 29.976 .150 75.4 83.6 69.0 | 146
21 29.984, .050 911 | 139 73.8 82.2 66.6 | 15.6
22 .997 ,068 948 .120 73.6 82.2 66.0 | 16.2
23 30.036 118 .979 .139 Wout 82.2 66.3 | 15.9
24, 024, .108 954 154: 72.8 81.6 66.0 | 15.6
25 29.974, .058 -900 158 71.8 81.0 64.5 | 16.5
26 .949 .014 .888 126 70.2 774: 63.6 | 18.8
27 -980 .060 919 141 69.7 78.2 62.3 | 15.9
28 30.008 .075 .960 Ne 69.5 78.2 61.6 | 16.6
29 ,008 .084 941 143 70.6 81.1 61.6 | 19.5
30 29.984, .059 908 151 71.2 82.0 63.0 | 19.0
°
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Thers
mometer Means are derived from the hourly Observations made during the day,
Ixxxii Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Obacknaianns
taken at the Surveyor General's Office, Calcutta,
in the month of November, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
2 , 5 S Bs aE Ag
2 3 3 a a ae |>3 | BE
& t _ [S) oe tS et A = <
= rs) 5 Sa) 6 Sty RON) ere ees
3 iS 3 oa 2 2S) | ISto ea eeoees
Date.| ©. 2 a 3 2eo |SE5| 2os
35 = 2 SB Gas Se | bog
= Ss = ® Bo: Qs > 2 |e oe She
a8 a 5 | ae 2 |) BO | ee eu ee
faa) Sh — ay 3 os ma
2S : iS) Ais = we) SSS
® A Lee g Peay oF ® sae} ots
| = a S) a = = 3 =
° ( t) oO Inches.| T. gr. | T. gr.
1 719 6.7 67.2 | 11.4 0.664: 7.19 3.19 0.69
9) 72.9 6.6 68.3 | 11.2 .688 43 .23 70
3 74.1 GON ae F693) ule 7 ay lth 64 50 69
4 72.8 69 68.0 | 11.7 681 .oD ABi/ .69
5 75.0 5.5 (lees 9.4, 1753 8.13 2.85 74
6 70.2 }) 9.4 63.6 | 16.0 590 6.36 4.33 .60
7 67.4 | 9.1 61.0 | 15.5 AL 5.87 3.88 .60
8 69.4 | 8,0 63.8 | 13.6 093 6.42 59 64
S| | 71.6 6.9 66.8 | 11.7 .655 7.09 .26 .69
10 74.6 6.1 70.3 | 10.4 734 92 Ale 72
rial 738 | 6.8 69.0 | 11.6 704 FeSr/ Ad: 69
12 (eRe Tp 98: 67.0 | 12.4 659 12 50 .67
13 70.4 7.0 65.5 11.9 628 6.81 .20 68
14 VPP NW Teper We tafe Tle .668 7 21 29 .69
150 PM ET2.0) Ae 67.9 | 12.1 679 33 48 63
16 71.7 | 76 | 66.4 12.9 646 6.98 61 .66
17 70.2 | 7.6 | 649 | 12.9 .615 67 AG .66
18 | 70.3) Biman 64.9 | 13.1 .615 67 52 .66
19 69.4 76-| 64.1 | 19.9 599 50 89 66
20 67.8 726, Wi G25 12.9 .068 18 25 .66
21 | 66.0 7.8 60.5 13.3 032 5.81 17 .65
22 66.0 | 7.6 60.7 | 12.9 536 84 .09 .65
23 67.1 6.6 62.5 | 11.2 .568 6.21 2.75 .69
24, 65.6 { 7.2 | 59.8 | 13.0 2520 5.68 3.03 65
OF 1) 268.40 Ul ps4 56.7 | 15.1 469 13 .B2 61
26 62:8. | 074 56.9 13.3 AT 2 18 2.87 64
27 6UGy Haves Sail 14,6 444) 4.89 3.04 62
28 | 62:3° fo Wie2 56.5 | 13.0 A465 5.12 2.76 .65
29 | 62.5 8.1 | 56.0] 146 58 302 | Sue 62
30 (| 63.9 (hee 58,1 13.1 AQ1 9) 2.91 .65
| |
|
|
= Gi) ee
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations. ixxxili
_ Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of November, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
ue .
S 3; | Range of the Barometer = 8 Range of the Temperature
P= for each hour during Ag for each hour during
Hour 2 the month. Pan) the month.
ay or 8 As
xo : = =i & n 4
S54 | Max. Min. Diff. Sc | Max. Min. Diff,
= =
Inches. | Inches.| Inches.| Inches. 0 0 0 0
Mid-
nicht, {29-949 | 80.099 [29.787 | 0.812 | 73.8] 79.4) 65.4 | 140
i 942 095 774 .o2L 72.6 78.6 64.8 13.8
2 933 .088 768 .020 W211. 78.4: 64.0 14.4
3 .927 -084 .769 2015 71.4 77.8 63.4 14.4
4, .926 08l 773 .308 70.7 76.8 62.6 14,2
5 939 .089 778 pole: 70.1 76.3 61.6 14.7
6 954, 106 .800 .306 69.6 75.6 61.6 14.0
% .978 126 815 Rolal 70.0 76.2 61.6 14.6
8 30.001 146 -036 .oL0 72.8 79.6 65.0 14.6
9 O21 164 052 012 76.0 83.0 67.7 15.3
50 019 161 861 .300 78.9 84.6 G2 13.4
11 | 29.998 140 838 .302 81.9 86.4 74.6 11.8
Noon. 966 13? li 302 82.5 86.2 76.6 9.6
1 934 074 .768 .006 83.5 86.8 772 9.6
Z .910 -050 740 .oL0 84.3 87.8 77.0 10.8
3 897 | .084 739 295 84.1 88.2 77.0 11.2
4; 895 .035 3732 003 83.0 87.0 76.8 10.2
5 904: .039 LV 292, 81.5 86.2 75.0 11.2
6 915 055 aT .298: 79.3 83.8 72.8 11.0
i, 933 -067 776 291 77.8 82.4 70.5 11.9
8 -952 091 801 .290 76.6 81.8 69.2 12.6
93 .966 Algal 811 000 75.5 80.8 67.9 12.9
10 970 | .109 .815 2294 74,5 79 A 67.0 12.4
il .966 104 810 294 73.6 79.3 66.2 13,1
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several hours
during the month.
Ixxxiv Meteorological Observations.
Abstiact of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of November, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
| 2 3 3 E = we S68) a8
a = Sy Ie 8 Fe |see | Hee
< Ay a) 5 3 a) “8p 2e re) 2g =
2. z E e Ss 2 o's 8 2 Oo 5
|} oO S o ° Ss) = =I = o =
Hour. | 28 B Qa B 2 “=O E Bm Sp a oP
A LE ht See Sled 2 Sloe ae ee
=a 3S = el Alo Bue. Be 2 = 22
> 8 ian) 2 FA-s Ss eis Becee Ie
= 3 b g po | E> | $5. |S 6 | Seas
Le hes A 3 A S se | Be oT ec
O) ee ) 0) Inches. |Troy grs.|Troy grs.
a | 686 | 47 | 648 8.5 | 0.613 | 6,71 2.13 | 0.76
“4 | 67.9 4.7 | 64.1 8.5 599 55 al 76
2\ 674 | 47 | 63.6 8.5 | .590 A5 .08 76
3 | 66.9 4.5 | 63.3 Bul 584 AL 1.94 Jefe
A 66.4 | 4.3 63.0 etl 578 85 83 78
5 | 66.0 41 62.7 7.4, 572, 30 43 a
6 | 65.6 | 4.0 62.4) 72, 567 24 .66 279
7 | 65.8 4.2 | 62.4 7.6 567 23 17 78
s | 669 | 5.9 | 622 | 10.6 563 615 2.56 Til,
a) | 68a 79 | 622 | 13.4 570 20 3.40 65°
10 | 69.4 | 9.5 62.7 16.2 572 19 4.28 59
7) | «702 | 108 | 626 + 184 570 14 5,00 5D
Noon.| 70.7 | 11.8 | 62.4 | 20,1 .567 .08 56 52
1 70.9 | 12.6 | 62.1 | 21.4 561 O01 99 .50
2 71,5 | 128 | 62/5 } 2118 568 .07 6.21 49
3 FAO, whist |) 6l:8ie Nye2i2 55D 5.94 27 .49
4 70.9 | 12.1 | 62.4 | 20.6 567 6.06 5.76 51
Ser FS) IOS 642 e738 601 AG 4.85 57
6 FG), etal 9166.2 AY ii 642 93 3.66 .65
7 | 71.3 6.5 | 66.7 | 111 653 7.07 .06 70
8 70.7 5.9 | 66.6 | 10,0 651 .07 2.70 Ure.
9 70.1 5.4 | 66.3 9.2 644 .02 AA 74s
10 | 69.5 5.0 | 66.0 8.5 .638 6.95 23 76
il 68.9 4,7 | 65.6 8.0 .630 .89 04 Tee
)
All the Hygrometrical elements are computed by the Greenwich Constants.
en
=_
Meteorological Observations. Ixxxv
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calewtta,
in the month of November, 1865.
Solar Radiation, Weather, &c.
Oo oO
28 |23 |
| 23 |O & & Prevailing direction General Aspect of the Sky.
‘SAS Begs of the Wind.
a s = |e isd
: o_ _|Inches.
a} 133.0)... |.N. Ni. :
2| 137.8 N.& N. W. ‘ito lp. mM. clear afterwards. Slightly
fogey from 9 to 11 Pp. M.
31 141.8} .. |N.&N.W.& W. Clear to 10 4. uM. “i & Xi to 3p. m., clear
afterwards.
4| 138.7 N.&N. W Clear to noon, Scatd. “i to 5 p. m., clear
afterwards.
EPtAd Oi tee, bl, N. Gy N. Woe Clear to 6 a. M. Mito 5 P. M., clear after-
wards.
GPa40.0| ... | N.&N. W. Clear. Slightly foggy at midnight.
7| 140.2 ' N.W.&N Clear.
SIge law | Ns We GN. Clear.
9) 131.8 N.&N.W.& W. | Clearto6 a.m. ito6 Pp. m., clear afters
: wards.
10} 120.0| «. | N. fito8 a.m. Wi to 6 P. M., clear after-
wards.
11) 129.0| .. | N. \i nearly the whole day.
12} 131.90 | aoa MNT 2 \n ito 6 Pp. M., clear afterwards.
13° 139.9 N. Scatd. \i to 5 a. M. light clouds to11 a.m.
Ni to 5 Pp. M., clear afterwards,
PA TAG A. ae. 2) N. & IN. 1. Clear to 4 a. M., clouds of different kinds
to Noon, ‘i to 5 P. M., clear afterwards.
15| 1848| . N Clear to 4 a. Mm. Scatd. ‘i to 6 P. u., clear
afterwards.
1G 136-2 |). | Ne Clear to 104, M., “ito 7 >. M., clear after-
wards.
17) 137.0 N. Clear.
18 139.0 ee Ns Clear.
79| 139.4; ... |N. Clear.
PLO | ic) Ne Clear to 6 A. u. Scatd. \i to 6 Pp. M., clear
| afterwards. Slightly fogey at 9 & 10
P, M.
21) 135.0| .. | N.&E Clear. Slightly foggy to 1 A, mM.
22 1260). ... | N.& E Clear.
23| 135.0; .. |N.W.&N.&E, | Clear.
2 HBGZ eat (ON. Clear to 5 A. M, Scatd, ‘i to 6 P. uw, clear
afterwards.
25) foe aise | N. Clear to 4 A. M, Scatd. “i afterwards,
26, 127.0| .. |N. Clear to 3 4, M, “i afterwards.
Ni Cirri, —i Strati, 0i Cumuli, i Cirro-strati, 11 Cumulo-strati, i Nimbi
“ni Cirro-cumuli,
Ixxxvi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
wm the month of November, 1865.
Solar Radiation, Weather, &c,
= {se
Se ae
.| 23 |S & §| Prevailing direction General Aspect of the Sky.
2| we 188 of the Wind.
a; Sse @ SH A
Al AF jad
| o |Inches =
247) 1290) 3... | NoW.G WN. Ni to 1 A. Mm. clear to 5 a. mM. “i to6 P. M.,
clear afterwards. Slightly fogey at 7
P. M.
ys IS{0s) I 355 NI orem ne Clear to5 A.M. ‘ito 7 P. M., clear aftere
wards.
29) 13620), 5, |) Wie Clear. Slightly fogey at 1 A. mM.
30} 138.8; ... | W. Clear. Slightly foggy at 10 P. M.
Meteorological Observations.
Ixxxvii
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of November, 1865.
Montuty Resvutts.
Mean height of the Barometer for the month, .. AC 60
Max. height of the Barometer occurred at 9 A. mu. on the 19th, oe
Min. height of the Barometer occurred at 4 P. M. on the Ist, Hes
Extreme range of the Barometer during the month, AR Be
Mean of the Daily Max. Pressures,.. ee eo oe
Ditto ditto Min. ditto, .. ce oo A
Mean daily range of the Barometer during the month, .. ee
Mean Dry Bulb Thermometer for the month, .. a0 ae
Max. Temperature occurred at 3 P. M. on the 38rd, o° ae
Min. Temperature occurred at 6 & 7 a. M. on the 28th & 29th, ae
Extreme range of the Temperature during the month, wih AR
Mean of the daily Max. Temperature, oo eo 20
Ditto ditto Min. ditto, .. oe 2° ee
Mean daily range of the Temperature during the month, .. 06
Mean Wet Bulb Thermometer for the month, .. ac we
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, ..
Computed Mean Dew-point forthe month, .. SS ee
Mean Dry Bulb Thermometer above computed Mean Dew-point, 50
Mean Elastic force of Vapour for the month, .. te as
Inches
29.950
30.164
29,732
0.432
30.623
29.890
0.133
69.1
Tce
64.0
12.4
Inches
0.597
Troy grains
Mean Weight of Vapour for the month, oo ee ai
Additional Weight of Vapour required for complete saturation, Bia
Mean degree of humidity for the month, complete saturation being unity,
Rained No days, Max. fall of rain during 24 hours, ale aa
Total amount of rain during the month, Se de BY
6.49
3.23
0.67
Inches
Nil.
Nil.
Prevailing direction of the Wind, ., oo oe N. & N, W.
IXXxViii Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of November, 1865.
Montruty REsvyts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
Rain on.
Hy.
Rain on.
SS)
Rain on.
Rain on.
N.
s.
N. W.
Rain on.
Calm.
Rain on.
Missed.
Rain on.
WwW
Rain on.
inal
|
|
|
|
|
|
No, of days.
Midnight. 17
a
bo bo
_
ve)
RSPNwmNNwNNWh
eS
WOO Ode
a)
w)
a
Rr Ooo
bo
ie
oo out
WNNNNWWWWWwWWwWwWLh
Re wOoW EOE OUD
Noon. 23)
ES
WE
a
paar
NTCOCOONTNTNTOOUOE
a
FPOUOOMONOA UHL WHE
_
con)
NNWWNRHEHEE DPD
WwkePeREWWNWNNHDNWW
e
eS
Re eee ee
ay
|
|
|
Meteorological Observations. Ixxxix
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of December, 1865.
Latitude 22° 3371” North. Longitude 88° 20’ 34” Hast.
Height of the Cistern of the Standard Barometer above the Sea-level, 18 ft, 11 in,
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
—_— tN
is = Range of the Barometer & 3 |Range of the Tempera-
th 2 = during the day. ba ture during the day.
= 20 Be
Bates: = Fe ss =
s22 | Max. | Min. | Dif, a Max. | Min. | Diff.
te a
Inches. | Inches. } Inches. | Inches. Co) te) 0 0
1 29.970 | 29.049 | 29.906 0.143 72.9 83.5 65.1 | 18.4
2, 984 .051 928 123 72.7 82.6 66.0 | 16.6
3 | 30.011 .079 955 Mia) 752 85.6 | 67.4 | 18.2
4; — .020 114 .960 154 | 74.9 83.6 | 67.8 | 15.8
5 29.999 O71 :929 142 74.0 82.2 68.2 | 14.0
6 30.031 .093 .934: 109 | 72.8 81.4 64.8 | 16.6
7 .013 .098 957 BUA 27229 81.8 65.0 | 16.8
8 29.972 051 927 124 75.3 83.4 69.4 | 14.0
9 30.010 .090 964. .126 74.3 82.2 67.8 | 14.4
10 .042 134 .995 (US) || CB) 78.8 61.4 | 17.4
11 .060 164 975 .189 67.6 76.3 59.5 | 16.8
12 .062 154 | 30.005 149 | 64.9 74.5 | 56.8 | 17.7
13 ,029 .107 | 29.950 157 66.3 76.2 58.0 | 18.2
14 .054 .139 .993 146 67.1 77.4 58.6 | 18.8
15 .066 .150 995 | 155 68.3 77.8 60.0 | 17.8
16 053 abe BT | 133 68.3 77.8 60.2 | 17.6
17 031 .103 985 118 68.3 78.7 60.0 | 18.7
18 021 .082 at | Auinl 69.0 79.0 60.6 | 18.4.
19 .037 «112 974 138 69.5 79.4 60.2 | 19.2
20 .092 185 | 30.048 137 70.4 80.6 61.5 | 19.1
21 101 172 043 5129 72.0 82.6 62.8 | 19.8
22 .126 196 064 182 71.9 81.2 63.6 | 17.6
23 101 178 043 135 71.0 80.4 62.8 | 17.6
24, .068 139 .005 134 71.7 81.0 64.3 | 16.7
25 | .060 156 | 29.975 181 71.9 81.8 63.8 | 18.0
26 015 .096 94,0 BSG edzed 82.0 64.8 | 17.2
27 29.974: 052 909 143 74.2 81.7 67.0 | 14.7
28 .940 .016 .883 133 Ups \\ > teil) 66.5 | 14.5
29 30.011 .070 965 105 71.5 76.2 68.4: 7.8
30 .050 146 .976 170 68.1 VEG) 62.6 | 12.0
31 .035 134: .966 168 68.5 78.0 60.0 | 18.0
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther«
- mometer Meaus are derived from the hourly Observations made during the day,
xé Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of December, 1865.
Daily Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
5 E i epee ee be |b
CMC eee es es
BB 2 = ro) me ww 9 Ss
= to) zy a > lo) ° 5 . Ha = >
lites > E § ons ess) Sos
a 2 2 % = OREO 2) tore =
Date. | = 2 QA Sb ao SB El |, © BP en
~~ s To) 3 Oo 80:5, = a8 ~ g S
22 2 @ ae Sl euloe ls 2 H | e 25
eo 3 = pa 3 AS ae) Fen lh rs eees
| = faa) 2 a= = on bd
| =e) a fo) Aaa as Bo L Ss £°6
eg bs g bay SS SS Po oon
= A o) a = = 3 =
0 r) o fy) Inches.| T. gr. | T. or,
1 66.2 6.7 60.8 | 12.1 0.537 5.88 2.85 0.67
2 68.3 4 64.8 7.9 613 6.72 1.96 sit
3 67.8 7A 62.6 | 12.6 .570 20 3.17 66
4 68.0 | 6.9 63.2 Wilde 082 Ais) 2.95 68
5 68.9 5.1 65.3 8.7 623 81 23 75
6 66.2 6.6 60.9 | 11.9 539 5.90 81 .68
q 65.9 7.0 60.3 12.6 .028 78 95 .66
8 70.1 5.2 66.5 8.8 .648 7.06 34 75
9 66.1 8.2 60.4 | 138.9 530 5.78 3.34 63
10 61.5 8.4 54.8 | 15.1 440 4.83 15 61
11 58.9 8.7 AS) |) ilayae 398 .40 04 59
12 57.4 (43) 51.4 13.5 892 1380 2.50 64
13 59.9 6.4 54.8 15 44.0 .86 29 .68
14 610 FPG DOva peel 0 A59 5.09 20 79
15 | 62.6 5.7 58.0 | 10.3 489 40 20 aff
16 62.0 | 63 57.0 ( 11.3 A73 22 38 69
17 62.0 6.3 57.0 11.3 473 22 38 69
18 62.4 6.6 57.1 11.9 A75 23 53 67
19 62.7 6.8 57.3 12.2 A7B 126 62 67
20 63.8 6.6 98.5 11.9 498 47 63 68
pi | 648 | 7.2\ | 59.0 | t80 506 | .54 | .96 | .65
22 65.3 | 66 60.0 | 11.9 523 73 75 68
23 65.0) 4 98G:0 60.2 | 10.8 27 78 AIT 70
24 65,3 | eo 61.1 10.6 DAB 95 48 71
25 66.8 5,1 62.7 9.2 572 6.27 21 74,
26 67.5 5.2 63.3 9A 584 09 29 7A
| 68.5 Dei 64.5 9.7 607 62 AT 73
28. | 68.5 | 4.3 65,1 7.7 619 78 1,93 78
29 ‘| 67.9 | 3.6 {| 65.0 6.5 617 Atle 61 SL
30 | 62.1 6.0 57.3 | 10.8 478 5.27 2.28 70
31 61.8 | 6.7 56.4 | 12.1 464, ne A 67
|
}
All the Hygrometrical elements are computed by the Greenwich Constants,
Meteorological Observations. ‘ xel
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of December, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.
=) =; | Range of the Barometer. = 5 Range of the Temperature
aaa for each hour during m2 for each hour during
Hak = = a the month. Po the month,
"(rag Aa
zo? 5 é s & -* ,
Z24 | Max. Min, Diff. Se | Max. Min. Diff.
= S
Sse — Sy
Inches. | Inches.| Inches.| Inches. 0) C0) 0 0
|
Mid- y
nicht. 30.035 30.153 {29.954 0.199 67.3 72.8 60.8 12.0
1 .028 148 .936 le, 66.5 72.8 59.8 13.0
2 -020 elise 912 221 66.0 42,2 590 13.2
3 012 124 .905 219 65.3 72.0 58.8 13.2
4. .010 107 8388 219 64.6 71.2 58.4 12.8
5 021 114 899 215 64.1 71.0 58.0 13.0
6 .035 126 .910 2216 63.6 69,4 57.0 12.4
&i .058 145 945 .200 63.5 70.0 56.8 13.2
8 .087 174, 991 1838 66.3 2.3 60.4 11.9
9 -109 194, |30.005 189 69.8 75.3 63.0 12.3
10 ot: 196 .016 180 73.3 49.2 67.8 11.4
aE .092 182 004 178 75.8 81.8 71.0 10.8
Noon. -058 144 |29.974, So: Ih lease 83.0 72.2 10.8
1 .022 116 93 180 79.0 84.7 TAL 10.6
2 | 29.995 -088 907 181 79.9 | 85.6 74,2 11.4
3 -980 .066 887 wZ9 79.9 84.8 74.5 10.3
4 -976 .064 083 181 78.5 83.5 73.4 10.1
5 .985 .067 .886 181 76.9 81.3 71.8 9.5
6 996 084 901 183 7A.2 78.3 68.2 10,1
7 '30.014 104 924 .180 72.3 76.2 66.0 10.2
3 ,030 123 953 .170 71.0 75.2 65.0 10.2
9 043 ,150 974 176 69.8 74.1 63.4: 10.7
10 048 159 .979 180 68.8 738 62.6 11.2
il 044: 0157 972 185 68.1 73.0 61.8 Tee
The Mean Height of the Barometer, as likewise the Dry and Wet Bulb Ther-
mometer Means are derived from the Observations made at the several hours
during the month.
xii lileteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General’s Office, Calcutta,
in the month of December, 1865.
Hourly Means, &c. of the Observations and of the Hygrometrical elements
dependent thereon.—( Continued.)
= S E S 28 ose 33
| 3 5 3 A 2 Pe ess |Fes.
| : ip aiee & S62 | EE | See
Be Bol eee 8 | eS See
How. | FS = a S Bae llc eg | mea
| iw 2 S12 sill 2 Sap 2 Seas) Seeee ees
eS Ej = 33 Flo Be. sak = 2
SE a a aecieiere ie Ghers es Re | Bee
= 3 P 8 aoc ac) oe S| Ses
= a) 'S) Q =) Se Se. | enim as
|
| o o oO Inches. |Troy grs.|Troy grs.
s |
Mi | 688 | 85] 61.0 | 68 | 0541) 5.69))) Lea iioes
a | 63.3 3.2 | 60.7 58 | .536 .93 26 83
2 63. 3.0 | 60.6 5.4 | 584 92 16 |, 84
3 | 62.5 2.8 | 60.3 5.0 528 87 .06 "85
a) 6S 2.7 | 69.7 4.9 518 76 .02 85
5B | 614 | 2.7 | 59.0 ig 506 .63 04 S84
6 61.0 | 26 | 58.7 4.9 | .501 5S 0.99 85
” 61.0 | 2.5 | 58.7 Zick Mn ASO) 58 97 85
8 62.8 | 3.5 | 60.0 GR ees .80 1.35 81
9 64.3 | 5.5 | 59.9 a9 521 73 2 22, 72
Ip | 656 | 77) bos gel iets .60 3.24 63
11 66.5 | 9.3 | 60.0 | 15.8 | .528 68 .86 .60
| |
Noon. | 66.6 | 111] 588 | 18.9 | .503 4A 4.66 5d
1 66.9 | 121 | 58.4 | 20.6 | 496 85 5.15 51
2 67.0 | 129 | 580 |} 21.9 | .489 27 51 49
3 668 | 18,07 |) 57.6) 4) 22/38) 483 .20 58 48
A 66.6 | 119 | 58.3 | 20.2 | .494 34 01 2
5 67.0.) (910 6040 4 T6Be 2525 .69 4.17 58
6 | 67.0 | TZ 62/0) 22 ta) 550 mala 2.99 67
7 | 664 | 59 | 61.7 |10.6 | .554 205 58 71
8 65.8 | 5.2 | 61.6 iA ly pee .06 19 74
9 | 65.3 4.5 | 61.7 8.1 Bb4 09 1.86 77
10 | 65.0 | 38 | 62.0 6.8 | .559 16 BD .80
il 645 | 3.6 | 616 6.5 | .552 .08 AT 81
All the Hygrometrical elements are computed by the Greenwich Constants.
Meteorological Observations.
KCl
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of December, 1865.
Solar Radiation, Weather, &c.
Max. Solar
Rain Gauge
vacation.
|
5 feet aboy
Ground.
\i Cirro-cumuli.
| Prevailing direction
of the Wind.
a ES
fe)
Be &
Estee
eee
W. & variable.
N. W.&N.
W.&N.&N. W.
W.&N.W.&S, W
N.
N.&N.W. & W.
W.&N. W.
S.& W.
S.
WwW.
General Aspect of the Sky.
Clear : slightly foeey from 2 to 7 A. M.
Clear: slightly fogey from 1 to 9a. m,
Clear to 5 a. mM. ‘ito ll a. mw. Scatd. Wei
& -ito3 p,m. “i afterwards.
Scatd. i to 6 a. Mm. Scatd, ‘i to 2 P. M.
Scatd. ito 6 vp. mM. “i afterwards.
Scatd. -i to3 a.m. “ito 9 A, M. Ni to
5 p. M. clear afterwards.
Scatd. \i to 6 a. M, clear afterwards.
Clear, foggy at 11 Pp. M.
Clear nearly the whole day, Slightly
fogey at 4 A. M.
Clear.
Clear to 3 A. m. “Wi to 11 A. mM. clear
afterwards,
Clear.
Clear, slightly foggy from 9 to 11. p.m.
Clear, slightly foggy from 9 to 11 P. Mm.
Clear, slightly foggy at Midnight & 1
A. M. & from 9 to 11 P, M.
Clear, shock of an earthquake at 6 h. 45 m,
P. M.
Clear, slightly foggy at 10 P. M.
Clear, slightly foggy from 4 to 7 a. M. &
from 8 to 11 P. M.
Clear, slightly foggy at Midnight, 6 A.M.
& from 8 to 11 P. M.
Clear, slightly foggy from 9 to 11 P. M.
Clear, slightly foggy at Midnight.
.| Clear, slightly fogey at 10 P, M.
Clear.
Clear, slightly foggy from 8 to 10 rv. Mm,
Clear, slightly foggy from 7 to 11 p. M,
Clear, forey from 5 to 7 A. M.
Clear, fogey at 5 & 6 A. M,
Clear to 11 4. M, i afterwards,
NiCivri, —i Strati, 9i Cumuli, i Cirro-strati, ~i Cumulo-strati, i Nimbi,
X¢Clv Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of December, 1865.
Solar Radiation, Weather, &c,
Sums o ®d
.| 2 |O & = |Prevailing direction General Aspect of the Sky.
2| 2 ae & of the Wind.
ale lqed
o \Inches, z
29| 138.0 Ww.&S Clear to 7 A. M. i afterwards.
29| 128.0 F N. & W. Overcast to 6 Pp. M. clear afterwards, fogey
at 9 P. M.
3032.0) = N Clear, foggy at 11 P. mu.
31| 130.0| |. |N.& W.&N.W. | Clear, fogey at Midnicht &1 a. u. & at
8 P. M.
Meteorological Observations. xcv
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of December, 1865.
Montuiy REsvtts.
Inches
Mean height of the Barometer for the month, .. ee o. 30,034
Max. height of the Barometer occurred at 10 a. M. on the 22nd, -- 980.196
Min. height of the Barometer occurred at 4 p. mM. on the 28th, e- 29.883
Extreme range of the Barometer during the month, ee ee §=«.: 00.18
Mean ofthe Daily Max. Pressures,.. 30 ae Sou Opleles
Ditto ditto Min. ditto, .. se ee e- 29.973
Mean daily range of the Barometer during the month, .. ee 0.140
Co)
Mean Dry Bulb Thermometer for the month, .. oo 20 71.0
Max. Temperature occurred at 2 P. M. on the 3rd, ee oe 85.6
Min. Temperature occurred at 7 a. u. on the 12th, ne Se 56.8
Extreme range of the Temperature during the month, 50 be 28.8
Mean of the daily Max. Temperature, ee eo oo 801
Ditto ditto Min. ditto, .. be oo oe 63.4
Mean daily range of the Temperature during the month, .. we 16.7
Mean Wet Bulb Thermometer for the month, .. BB ee 64.7
Mean Dry Bulb Thermometer above Mean Wet Bulb Thermometer, .. 6.3
Computed Mean Dew-point for the month, .. se Se 597
Mean Dry Bulb Thermometer above computed Mean Dew-point, we 11.3
Inches
Mean Elastic force of Vapour for the month, .. oe ee «0.518
Troy grains
Mean Weight of Vapour for the month, ee ee ee 5.69
Additional Weight of Vapour required for complete saturation, « 2.56
Mean degree of humidity for the month, complete saturation being unity, 0.69
Inches
Rained No days. Max. fall of rain during 24 hours, 56 re Nil,
Total amount of rain during the month, ae ae ie Nil.
Prevailing direction of the Wind, ., ee ee N.& W.&S8.
xevi Meteorological Observations.
Abstract of the Results of the Hourly Meteorological Observations
taken at the Surveyor General's Office, Calcutta,
in the month of December, 1865.
Monruty Rrsvuts.
Tables showing the number of days on which at a given hour any particular wind
blew, together with the number of days on which at the same hour,
when any particular wind was blowing, it rained.
Hour.
5 5 Sey ie) ae) balls! Kelsi Ei
aiels slale| |elele| | ste lsisial2
|NS (A (2) B le lala Selo lee leialals sie
No. of days.
Midnight. 10} | 1 2 }11) | 2' | 3) 2
1 9} | 2 3 si f 4) | 2] 2 1
2 10} | 2 il | 9) J 3l P3l y2 ih
3 9 2 1 1} | 9} ¢2| f4 2 1
4, 11 Wa | oh ake i 3} 3 1
5 11 f11) Jl) 73} | 4 iL
6 10) | 1 i) 72) 74) 13
7 11 PAU Gp ey 1 2
8 ast of 2 ee eb TN 3
9 11 1 3 2) | 4) fl} 25 4
10 11) | 3 1 | 6; fl) 75) | 4
11 9) | 2) 2 1S) ayes) iy
Noon. 11) 1 » 2 1 5 i10 2
1 5) | 6 13| 17
2 7| 14 72) | 9| [9
3 6, 1| | 3 13} | 8
4 5! | 4 11| fil
5 7 1} | 2) fF 2) 7s fil
6 7 1 1) Wa es 9} |9
Gi 7 1} | 2) | 4) | si 79
8 8} ta! 15) | 2! 7 8| 16
9 12) is} Ja TAP
10 cH) (a ashe iereshv) fyal Ii a!
ar 8| 1 3 19} 72] Fal [4
2 SN Bae OU) 1 Bee ee
INDEX I.
—=
PART IIL.—NATURAL SCIENCE. .
Page,
Aitchison, Dr. J. E. T., on the vegetation of the Islands of
dass.) 2. a aa das 53
Analysis of Lowa Ghur Lignites, a oy) AEBTOR 42
Arakan, description of new = seins THON ea ca ae 66
Asia, notes on Central, _... Eh Daas SES
‘Asthenurus Atripinnis, a new Gonna ai Gadi! na ee 32
Astronomy among the Karens, ae jh SATS LOD
Attraction, on Local, . Bat 2/
Austen, Capt. Fer Godwin, on Aare Bios Sandstone... OMT OG
Ava, description of new land shells from,. 66
Basevi, Capt. J. P. Pendulum operations of Trigonometrical
Survey, 251
Barnes, R. H. "Meteorological observations at Gangaroowa,
Kandy, bas one bee bce iE seg
Bijnour District, Boksas of, 147
Blanford, H. F., W. Theobald’ s Obecmeiiene on el ohne by,.. 60
2 gah Wee T., Contributions to Indian Malacology, ... ... 66
a ” Note on Syepoorite, ... fs caaenlige
Blyth, Edward, on Innus Assamensis, H.. WET Sime ge teed [19 ) 7.
Pee | On Indian Rats gnd Mice, ue At) deh
es Fe Letter from, : Hy, BSS ope 48
5 Ps: 4A QRS
Note on fee eae Partridges, ahs CEAUCLASS
Boksas of the Bijnour District,.. ua. ie , gO eeRIET
Buxa, Bhootan, Sandstone of, ri) ae ou: Seats eG
Calcutta, Meteorological observations, ate tit apes
Central ‘Asia, notes on, .. ee Odo dih. Haars
Contributions to Indian Malacology, Neh 66
Dalton, Lt.-Col. T., Tour in 1863-64 in Tributary Mehals. Ht. 1
ere "On discovery of lead at mele Ram-
kola, ae 48
Dorylus, Dr. T. C. Jerdon on, J5e6k UUs ESS
Karth’s Crust, 2 aa on Constitution of, 500 as 34
Fire-flies, Flashing of,.. . ake ale sue iees TanEeOU
Gadide, Description of new Genus, : 32
Gangaroowa, Kandy, Meteorological Observations at, i, seq.
Geological Map of Lowa Ghur range, notes on, : 42
Indian Malacology, contributions to, aes Coo 66
li Index.
Page
Indus river, vegetation of Islands of the, ... Se bia 53
Tnnus Assamensis, a 60 so 55, Goole
Jerdon, Dr. J. C., on Dorylus, ae ae bee ee 868
Lagomys Curzoniz, ¥ S00 sos ae 9 WN
Lead at Tuppeh Ramkola, ‘Sirgooja, ee a 48
Local Attraction and its relation to mean ficure of earth, ae 34
Lowa Ghur, Geology and Analyses of Lignites; sieie ae 42
M: ilacology, contributions to Indian, joa 66
Mason*D. Ds Rey. F., Religion &e. among the Karens, . 178, 195
Mean Figure of Earth, Bele Ses B4
Medlicott, HajBs Note on Steal Fauna, Nas 23 aS 63
Mchals, Notes of tour in 1865-66 in Tributary, ae 1
Meteorological Observations at Gangaroowa, Kandy, Ceylon, 1. seq.
a Calcutta, he soe 1, SEQ?
Mice, Indian Rats and, oats one Fee oo SEO
Notes and queries, .. ate oe Ber peclains kes)
Ostrich, Artificial hatching of eggs of, See 48
Parish, "Rev. C., Notes of a trip in Yoonzalin District, Pied
Partridges, Note on Peura, 288
Pendulum operations of Government ‘Trigonometrical Survey, 251
Pegu, description of new shells from, _... ee aoe 66
Peura Partridges, note on, So wie. Iploke SURI
Pratt, Archdeacon, on Local Attraction, &e., Be ae 34
Rats, "Indian, 3e4 555 see sae see
Salween river; Trip down ‘the, sie oo2 Sad 2. AE
Sandstone, at Buxa fort, Bhootan, ... sete cect hee ate! eee
Scientific Intelligence, OMe 500 2 2 Oe
Semenof, M., Notes in Central Asia, ue ding © cejee ee ml gliss
Shan States, "Land and Freshwater shells of, 1k sah hanes
Siwalik Fauna, Note on, ... ate eaen ee 63
Stewart, Dr. ip L., on the Boksas of Bijnour, at oa eh
Stoliczka, Dr. Note on Lagomys Curzoniz, 108
The obald, Jur., ae W., Land and Freshwater shells of Shan
States, ... Me 213. &
Observations on certain strictures by
H. F. Blanford, Lan eee 60
Tickell, Lt.-Col. S, lity AN New Genus of Gadide, i mer 32
Tt rigonometrical Survey, Pendulum Operations of, soa ae
Tuppeh Ramkola, Discovery of lead at, ... ue ae 48
Vegetation of Islands of Indus river, 53
V erchere, Dr. A. M., on Geology, Map of Sheen Ghur range,. 42
Yoouzalin District, notes of a tpn, Naeee a vaginal
DL LLLLILLIPLOPLLIFLILLIIIIIII
Index.
INDEX. II.
—a= fe
ii
New Genera and species described in this Volume.
Asthenurus,
Pterocyclos
Alyceus
Diplommatina
Helicina
Nanina
Helix
Pisces.
Order, Malacopterygii Subbrachiati.
Family, Gadidee.
Atripinnis, (Tickell,) ues fon by
Mollusca,
Order, Prosobranchiata,
Section Holostomata.
Family, Paludinidae.
Paludina naticoides, W. Theobald, Jnr. . 274
Bithinia nassa. . sf s See)
9
Family, Cyclophoride.
Feddeni, W. T. Blanford, : 83
Insignis, W. Theobald, ane 278
Politus, be aoe 83
Glaber, ae ben Pe es 84
Nanas 0 ss ay 85
Arakanensis, W.T. Blanford, 85
Order, Pulmonifera.
Family, Helicide.
Compluvialis, W. T. Blanford, 66
MNebulosa 2. ..s: “i Sect. Macrochlamys, 66
Hypoleuca, eames “6 if 67
Winvdlosa yo) ie. oie 6 - "Hemiplecta, 68
Helicifera,....... PBK
Mamillaris, mel - “fs rF Sesara, 69
Basseinensis, ...... 70
Woliniss:), saat eee Od
Wulmien, ces. osc: ‘ 35 ,, Trochomorpha, 72
Gratulator, ......... sev uantees
Conula, Soh aes: ys = » Kaliella, 73
Karenorum, Sa erhes
IPE AMC UA, 5) ap'vice d's 2c re Ef Plectopylis, 75
Beddent, ...s.s00ss ose.
Polypleuris, 3 (Ree 76
Ansorinus, W. Theobald,” ee Pemre (
iv Index.
Page
Bulimus Scrobiculatus, see sie Seen) ee
Plicifer,... a a5 ae voce SE
Spiraxis _ Pusilla, a56 505 500 PN Shes
Achatina Peguensis,- ae 5.09 ws aaa)
Pertenuis, ... oe mS ae tliat: Some aie
Succinea _Plicata, ae Boe sae we FEO
Clausilia Fusiformis, W. T. Blanford, ... don ate Oe
* Streptaxis Burmanica, un ee ers ip OIL
ERRATA.
rr O@ owe ome
Page 135, seq. for “ Notes of a trip up the Salween” read ‘‘ Notes of
39
a trip in the Yoonzalin District.”
273, below M. variabilis for ‘ could” read ‘‘ would” for ‘“ 3-1”
read “var. Ist.”
274, for “ naticordes” read “ naticoides” for ‘‘notest” in last
line, read “‘ subest.”
276, for “it is not larger,” read ‘it is not only larger.”
277, for “armed” read “wound.” For “‘cryptosonea’” read
“eryptosoma.”’ For “in species with new’ read “two
species, both new.”
278, “ Diplommatina 4” read ‘‘ Diplommatina 5,”
5
é