DOI Page / Citation link:
https://doi.org/10.11588/diglit.20836#0034
Drawn
ancL snrveyecL
bv iermann and liobert
de Sctiladintwelt.
Messrs.de ScMadintweits’Lxdia and Ili ili Asia.
Lypsometry, \rol.IT.
also oue o£ ttie lateral Tivers s h.ov's a
13 .
salt lake of
tVestern
Tibet .
The okiect
m a ckaracte
ristic fea
fcure of
tke s alt
13. PROFILE OF THE TSOMOGNALARI - PANORAMA.
serves as a £ood type of mixior elevations iu Tibet rntli coinparatively fevr snow peales. The former outlet of tlie iake, noxv dry, rs to Le seen aibove tlie present level of tke water,
rke sceuexv. Tke view takeu near a Takung, close to tke cousiieTakLe beucl. of tke loweT lake, embraces 250° Drawu aud. surveyed. ky iteruiaflii ( Or. 584 a585.)
Seale for tiorizontal ancl vertical de^rees
0 1 * 3 * 5
C' entral dire ctiou. : T ast.
Larimo, a peak easy of access, close ti
14. PROFILE 0F THE LARIMO-PANORAMA.
Lek, commaiuLs towards tke soutk a view of tke moimtains ketween tke Brima rauge aiul tlie Indus. Tke lower parts of tlie view inciude tlLe skores of tlie Iudus, witk fke towu of Lek, aud uumerous otker inhabited places. In tkis series of
representafions, kowever, we liave Iimited onrselves tlirougkont to tke orograpkic profile of tke mountain ckains only. It extends over 105°. Drawn ky Hermann, surveyed ky Lokerl (0i-. Nos.3G7 & 368.)
r
I 7 7 “|r th- >
J£.7xo Jiar 16,68ft,
JS Miirt Tso 15,5(7
The diagram. conJaining Lltjp.
heighis ix Lvaced, in. this ca-
sc. supcrposeiL orer a. inap
(jiring t/ue.■ LaliiiuLes anJL
Longiiudes ■ but, f'or rethtting
its sizcj, Uub districL of‘ thc
Gruxru Khorsujn, laktus f'orms
a parb for itscif.
pSK.Gr. IjO 8IO B|1
1 1 ‘: G E N E R A
or THE
L SKETCH
L A K E S
Tstr
4
jll« •,(
m I
1
a
I 1 1
«~J_ !_
n
Trr
^-f— 4-
D
Qajt
L
D I A G R A M
SHOWING T H C
HEIGHTS AND GEOGRAPHICAL POSITIONS
O F THE PRINCIPAL
LAKES o f WESTERN TIBET.
2'Raktis TaLl5flo(X JyAIansaTaur J,5,JS0
Tfuu laJces htJ'e, represenituL nre
^gradruUltj Lrying up, aniL iraces
are, yet extant inAicaiinq ihe.
cortsidertthly taryer surfaces co-
rercci, by tJiem. in, forrner limes
Thcy holxL a. tjrcMier quaniity of
salL, than, is usiutllij to be fotind
in, lakes, most of Ihcjn coniaj, -
niruj etn. amjrunt, trhich, renxlers
them, more. or less brtichish,.
The waier ofsome,, however, is
stilL (IrinJeabLe,, ajnang whLc,h
we, mtiy partLculary rneniinn. thc.
uppcr part of the, Tsomngrucla-
rL ajt-(L ilte. Jfdnle laJce .
slJesde. Chiiu (Lai.Ji. 3o ’
Jtm tjJZ. (jr. 77 °51‘ > xs the n ttme, of
a. la.Tce ttl- Trurkistdn. ( not zru-
tficateJL in, this nurp ), whjJh, is
ordj p e riotHcti flj fillcd.
fl e s -1 incli.
Engravel aniL puTjlisked "by E. A. Brockhaus , T.eipzi g , 1861.
See fhe evpfanations a.t tke foot of plate I of the .Panoraimc Profil.es.
ancL snrveyecL
bv iermann and liobert
de Sctiladintwelt.
Messrs.de ScMadintweits’Lxdia and Ili ili Asia.
Lypsometry, \rol.IT.
also oue o£ ttie lateral Tivers s h.ov's a
13 .
salt lake of
tVestern
Tibet .
The okiect
m a ckaracte
ristic fea
fcure of
tke s alt
13. PROFILE OF THE TSOMOGNALARI - PANORAMA.
serves as a £ood type of mixior elevations iu Tibet rntli coinparatively fevr snow peales. The former outlet of tlie iake, noxv dry, rs to Le seen aibove tlie present level of tke water,
rke sceuexv. Tke view takeu near a Takung, close to tke cousiieTakLe beucl. of tke loweT lake, embraces 250° Drawu aud. surveyed. ky iteruiaflii ( Or. 584 a585.)
Seale for tiorizontal ancl vertical de^rees
0 1 * 3 * 5
C' entral dire ctiou. : T ast.
Larimo, a peak easy of access, close ti
14. PROFILE 0F THE LARIMO-PANORAMA.
Lek, commaiuLs towards tke soutk a view of tke moimtains ketween tke Brima rauge aiul tlie Indus. Tke lower parts of tlie view inciude tlLe skores of tlie Iudus, witk fke towu of Lek, aud uumerous otker inhabited places. In tkis series of
representafions, kowever, we liave Iimited onrselves tlirougkont to tke orograpkic profile of tke mountain ckains only. It extends over 105°. Drawn ky Hermann, surveyed ky Lokerl (0i-. Nos.3G7 & 368.)
r
I 7 7 “|r th- >
J£.7xo Jiar 16,68ft,
JS Miirt Tso 15,5(7
The diagram. conJaining Lltjp.
heighis ix Lvaced, in. this ca-
sc. supcrposeiL orer a. inap
(jiring t/ue.■ LaliiiuLes anJL
Longiiudes ■ but, f'or rethtting
its sizcj, Uub districL of‘ thc
Gruxru Khorsujn, laktus f'orms
a parb for itscif.
pSK.Gr. IjO 8IO B|1
1 1 ‘: G E N E R A
or THE
L SKETCH
L A K E S
Tstr
4
jll« •,(
m I
1
a
I 1 1
«~J_ !_
n
Trr
^-f— 4-
D
Qajt
L
D I A G R A M
SHOWING T H C
HEIGHTS AND GEOGRAPHICAL POSITIONS
O F THE PRINCIPAL
LAKES o f WESTERN TIBET.
2'Raktis TaLl5flo(X JyAIansaTaur J,5,JS0
Tfuu laJces htJ'e, represenituL nre
^gradruUltj Lrying up, aniL iraces
are, yet extant inAicaiinq ihe.
cortsidertthly taryer surfaces co-
rercci, by tJiem. in, forrner limes
Thcy holxL a. tjrcMier quaniity of
salL, than, is usiutllij to be fotind
in, lakes, most of Ihcjn coniaj, -
niruj etn. amjrunt, trhich, renxlers
them, more. or less brtichish,.
The waier ofsome,, however, is
stilL (IrinJeabLe,, ajnang whLc,h
we, mtiy partLculary rneniinn. thc.
uppcr part of the, Tsomngrucla-
rL ajt-(L ilte. Jfdnle laJce .
slJesde. Chiiu (Lai.Ji. 3o ’
Jtm tjJZ. (jr. 77 °51‘ > xs the n ttme, of
a. la.Tce ttl- Trurkistdn. ( not zru-
tficateJL in, this nurp ), whjJh, is
ordj p e riotHcti flj fillcd.
fl e s -1 incli.
Engravel aniL puTjlisked "by E. A. Brockhaus , T.eipzi g , 1861.
See fhe evpfanations a.t tke foot of plate I of the .Panoraimc Profil.es.