National Institute of Informatics - Digital Silk Road Project
| |||||||||
|
Scientific Results of a Journey in Central Asia, 1899-1902 : vol.2 |
522 | GENERAt. II1'DRtK;RAPIIY (W TUF TA•t;Ik <Y,i1!At. |
e>ire, — :--_~..~,..~.....~.. : -- - .. .. ~
w
r r o1 that drains . way to the Inch ~ n (. )c.c:an, name.. \ t i.,, • R
H~re, then it is tha we have, as al • pa • . c• '.,.•',
`teste g
afar e, ~ to the i.reat ',o„ . F
::
noir r c. .pression. A. for the catchn •. ;r ., ~
tivé. he catchmentl-area of the Sr : , > 1 \if , name , • t E t, I • 1r
the I,ir-darja and 'the .Amu-darja- ;-o,stn bettyrc• t1uso; 40. g ,
of i . Kaschgar-d . rja and the la. E : a on tl : one ,['14 /PI ..I~t ~~
"* , M,,. a coup e of sel <% • v .
dar a on the ot r, . 1
P ti.
the 1.; rg-e Kara-ku an t . Mn 'set!.
Though, as 1 h, c t : il • - . I 1 : c-rved, the b sin to th, •
, ti
zon:• of the Kwe -1 ingoioc~ b- c si _Ted as entir-h- Iacltin;
by i means t k) t B, ~ f~t ~ ~ region to the south of : in .~ .
()eel. on to show w ,~~ ~ . ~~. ~ ~,
will ifficiently cx rr !? to'', ot i ain and snow < +~ tall there. : r,.$ tT
sea• of the y a; ”
~ ;. _ . [ itlg ~ ur attention ic, the ~•it••%•exst,~. ~ ° ^• r-+'
the ighlands, it 1. , s~`i~~` <l. g•nerallh sI,.-.•icin , that tlx• ~,s fr,
qu. ; • • • n•rtl t(• , . ah an from east to est. The I;“r
meet namely th. tltq„ ' eeipitati.n increases fro east to wt. !-, ; ~ g
per p eral zone, ~;i r Hi • wn by he accomp;~yin sketch-m;ct • 'b I ;
(Pl. .7). True, .• . ch does It convey acg, di ect inform. N o~
the p ecipitatio _ ,~ ti e very fact! ,.,f steady decre se in the I>> ' i~~
- ~ ;^f Zn
fro~tti ~ • 1...._ . u .. . _ .. . . .
weyt we :r•_=h~ 1 ~
1<~; cnt-darja, the biggest str:am of all; ; dar a w► ch ~; rt;s c' es the Trim during abo it forty da• ~ lows th ' e ~a Lila. which h4s long been cu off and ci[-
artotrx of th : ~::. t,:: ; the remafning streams the Sour 1, k i a,
the 4'.: --::.,`::.... - •Ora , e `•(sc a, . ct OP 0 a
— a e all still : lle . 6/ ' c Ts hertschen-darja orms, i~ s ~).', :
the . ream. . e .~ tie• f 't, thajt flow north, a d of ~h âhc~' l ~
large~t, . e a . i • lpir. bly ss magnitude t an e c~' e ri ,pt filoo ~
No ,v'i alt Zou ~ 4 : xtt~m ea. terl stre . .. • - __ o • : -J ^
of ~~ . .t,~ve h ~
all alik: . : ch
.nent areas of ..e s ams,, o : oun ônclusion. he ra -a ~
to t ~ e preci on; bfo,t~ xoihile r ..► i& a ar a s 4
N ~
c; ~i ostan-tog 1 an ~ $e jIöld . ha to _ her ~.
the. , ea o. : . v '5.. N _ ~
N m
yet •~ ch of the t-mattt`Pe,n ..~ - . ~~t~~ as t' ~ s a~ ~
l ', • • ` ~ ,~ = -Icat et-it-area o •• • river. tragai , 's rat 6gre. - Ian that •,~ ~ =' °,'
3
dari:. and vet t e lat er is Inc •! . rably 1° eate i the '. ra s w ~~
scr l,~ion in vol. will cle. ' y sh • . 'h ctrcum. . nee is ho et-, ~ ~ ~ .ih`
two lrainage-area ~ are im ediatel cot mous th o • ~ - . ~ ~ ~ ~ ~
If now it isl tl • • : ' • , • • 1- ~, e d' •and the n N N ~ j
the #reshets formel by the thawin Y o thcO5 ow nd ice, that d. w 4
rert !magnitudes „f the rivers i[ • esti • it is equally the L. ô
cowE~ - • • l - • ~ •• •• • • ! a}l,
|
Copyright (C) 2003-2019 National Institute of Informatics and The Toyo Bunko. All Rights Reserved.