that of 
A- 
fight £83 
early morning hoare before sunrise. 
This is true particularly of the more elevated parts of the infcfcr- 
re.ju.irod for sleop- 
\ whore woolen blankets 
/yi -0 
During the winter(rainy) season the atmos- 
A-r A t * 
phero is 
, | *tiw rui uy avatsvii cagxarc> utu'iug iiuo tuwuwu uj nyana ,k > 
Dur¬ 
ing this period the streams are ^ 11 t^O qdddf i®UTthe dry stream beds 
of the summer season are oonverte (JTnto rushing torrents impeded 
only by their tortaojfs character. So heavy is the rainfall at 
ing during the night, 
isi^eaingly humid o ften.¥ e »|r oppyetre tve. 
The rainy season Jagta^^during the month of 
■««8A^~S8y), and continues right through to about December 
•/ 
times that t 
rivers rise as much as 10 feet within a few hours: 
_ LaaaJa ) 
and the water oTEei^Sirries wi th J it '' 
-numerous uprooted trees which.render the use of 
4 ir: " 
the riveajfexoee&ingly dangerous to 393. navigate®*. During the 
vO frfi .txXJCXJ 0 ' ' fii,( * ..\ 
months c/f j/lepf^Fer ttui "'JjfitlSUwp-, H a j - #tsn eb ft oy^h» va»ycao V ow-yc ■ ■ . . 
yvw AJAJL J~\JkXau~jS, Jur€^ aaaj CCLuf \xatQ. >vA \rQ/ A 
-hTfrrn n 0/tfr--^vrtrt-ri—mn-fcfeqr-GSYpig TndXOuir to - T ,cntoy e - e- Ijrip' Up 
yfiz. 1 
The moisture-^adsn winds ar^, chiefly from the 
y* f} n t 
faiVJAv/' n Cut u<4 - 
which 
drive the rain clouds ase^ward o dsemf the southern slope of the 
Continental Divide, These winds impign on the southern slopes. 
which chill the clouds and cause the rain to fall excessively a.t 
the heads of the numerous streams draining into the riv'STT 
Droia December 15 to about the middle of April or first of May there 
aX'XaO 
is ww*almost »■ ' " la rain throughout the region of the “ 
river basin. The ground which during the rainy season is 
saturated, no' 
m bqq^ o » - ^ «e e o 4ing ' 3yn| fy-t 
a-using 
4w (jJJh 
QO ' ;Q 0 . to~- - beee s Kr tr 
J/tAJfr’ tut 
the 00 satisfy. 
~?€^TTtTrs^-~fTi : i4oxen 
mfr-fsw 
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