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0656 Scientific Results of a Journey in Central Asia, 1899-1902 : vol.2
1899-1902年の中央アジア旅行における科学的成果 : vol.2
Scientific Results of a Journey in Central Asia, 1899-1902 : vol.2 / 656 ページ(カラー画像)

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doi: 10.20676/00000216
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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 wch ~; 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 .~ tief '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,